EX-99.3

Probable Reserve

millions of tonnes

Proven Reserve

millions of tonnes

Total A Zone Reserve =

millions of tonnes

The scientific and technical information included in this report has been prepared under the supervision of persons who are ‘‘qualified persons’’ under Canadian National Instrument 43-101. Craig Funk, P. Eng., P. Geo. is the qualified person who supervised the preparation of the information presented in this report and who verified the data disclosed herein.

The scientific and technical information included in this report has been prepared by, or under the supervision of, persons who are ‘‘qualified persons’’ under Canadian National Instrument 43-101.

is the qualified person who supervised the preparation of all information presented in this report and who verified the data disclosed herein.

The team of persons who conducted the majority of the work presented in this report consists of:

Unless otherwise noted, figures for which a source and / or date are not provided are current as of the effective date of this report and were prepared by the Company.

The effective date of this report is December 31, 2018, other than where otherwise noted.

Effective January 1, 2018, Potash Corporation of Saskatchewan Inc. (“PotashCorp”) and Agrium Inc. (“Agrium”) completed a court-approved plan of arrangement (the “Arrangement”), involving, among others, PotashCorp, Agrium and Nutrien Ltd. (“Nutrien”) the new parent company of PotashCorp and Agrium. As a result of completing the Arrangement, PotashCorp and Agrium are wholly-owned subsidiaries of Nutrien. References to “the Company” means Nutrien, indirectly through PotashCorp, or, for references prior to the completion of the Merger, PotashCorp, as the context requires.

Nutrien is the world’s largest provider of crop inputs and services, with operations and investments in 14 countries. It produces the three primary plant nutrients: potash, phosphate, and nitrogen. It also has a retail network that services over 500,000 growers worldwide.

Nutrien is a corporation organized under the Canada Business Corporations Act, the common shares of which listed and publicly traded on the Toronto and New York stock exchanges (symbol NTR).

The Company owns and operates a potash mine at Allan, Saskatchewan, Canada (Allan Potash, or Allan mine, or Allan). An aerial view of the Allan surface operations is shown in Figure 1. The Allan Crown Subsurface Mineral Lease is numbered KL 112R A, and was expanded in October 2017. Production of potash from the Allan mine began in 1968.

As of December 31, 2018, annual nameplate capacity for Allan was 4.0 million tonnes and annual operational capability is 2.6 million tonnes of finished potash products (concentrated KCl). Estimates of nameplate capacity are based on capacity as per design specifications or Canpotex entitlements once these have been determined. Operational capability is the estimated annual achievable production level at current staffing and operational readiness (estimated at beginning of year), not including any inventory-related shutdowns and unplanned downtime.

While the term potash refers to a wide variety of potassium bearing minerals, in the Allan region of Saskatchewan, the predominant potash mineralization is sylvinite, which is comprised mainly of the minerals sylvite (KCl / potassium-salt) and halite (NaCl / rock salt), with minor amounts water insolubles. Carnallite (KMgCl₃ · 6H₂O) occurs only in trace amounts at Allan. Potash fertilizer is concentrated, nearly pure KCl (i.e. greater than 95% pure KCl), but ore grade is traditionally reported on a % K₂O equivalent basis. The “% K₂O equivalent” gives a standard measurement of the nutrient value of different potassium-bearing rocks and minerals. To convert from % K₂O equivalent tonnes to actual KCl tonnes, multiply by 1.58.

The Allan mine is a conventional underground mining operation whereby continuous mining machines are used to excavate the potash ore by the stress-relief mining method, with continuous conveyor belt transport of ore from the mining face to the bottom of the production shaft. In addition to hoisting potash ore to surface, the production shaft also provides fresh air ventilation to the mine and serves as a secondary egress. The Service Shaft is used for service access, and exhaust ventilation from the mine. Raw potash ore is processed and concentrated on surface, and concentrated finished potash products (near-pure KCl) are sold and shipped to markets in North America and offshore.

Virtually all Allan underground mining rooms are in the potash mineralized zone situated approximately 14 m below the top of the host evaporite salt, the Prairie Evaporite Formation. More specifically, the Allan mine is located within the Patience Lake Member of the Prairie Evaporite Formation. In this Member, there are two potash seams named A Zone (the upper seam) and B Zone (the lower seam); at present, only the A Zone is being mined at Allan. Mine elevations range from approximately 980 m to 1120 m, averaging approximately 1010 m. These depths to A Zone potash mineralization are anticipated over most of the Allan lease area. Mine workings are protected from aquifers in overlying formations by salt and potash beds which overlie the mineralized zone. Conservative local extraction rates (never exceeding 45% in any mining block) are employed at Allan to minimize potential detrimental effects of mining on overlying strata; this is common practice in flat-lying, tabular ore bodies overlain by water-bearing layers.

Part of the normal surface infrastructure associated with operating the potash mine in Saskatchewan includes waste disposal on the land and disposal of salt brine into deep subsurface aquifers. The Company stows salt tailings within an engineered and licensed

Tailings Management Area (TMA) and operates two brine disposal wells near the surface plant of the Allan mine.

Over the 50-year mine life, 150.239 million tonnes of potash ore have been mined and hoisted at Allan to produce 52.949 million tonnes of finished potash products (from startup in 1968 to December 31, 2018). The life-of-mine average concentration ratio (raw ore / finished potash products) is 2.84 and the overall extraction rate over this time period is 33%. Actual production of finished potash products at Allan for the last 10 years is shown in Figure 2.

Figure 2: Actual finished potash products production from the Allan mine over the past 10 years (in million tonnes per year).

Over the past three years (2016, 2017, 2018), actual potash production at Allan has totaled:

The Canadian Institute of Mining and Metallurgy and Petroleum (CIM) has defined Mineral Resources and Reserves in The CIM Definition Standards for Mineral Resources and Reserves (2014). Based on these guidelines, all mineral rights owned or leased by the Company at Allan can be assigned to Mineral Resource categories (Inferred, Indicated, and Measured) and Mineral Reserve categories (Probable and Proven). Mineral Resources (reported as in-place tonnes) and Mineral Reserves (reported as recoverable ore tonnes) for Allan as of December 31, 2018 are outlined in Table 1. Mineral Resources reported are exclusive of Mineral Reserves.

Table 1: Potash Mineral Resources and Reserves for Allan, as of December 31, 2018.

The average mineral grade of the Allan A Zone Mineral Resource and Mineral Reserve is 24.8% K₂0 equivalent, and was determined from 6,738 in-mine samples at Allan to the end of December 2017 (discussed further in section 11.2). The average mineral grade of the Allan B Zone Mineral Resource and Mineral Reserve is 20.3% K₂0 equivalent, and was determined from 20,230 in-mine samples at the Lanigan mine to the end of December 2017, where the B Zone has been extensively mined (discussed further in section 11.2).

Potash production in any given year at the Allan potash mine is a function of many variables, so actual production in any given year can vary dramatically from tonnages produced in previous years. The Mineral Reserve tonnage and historic average production are used to estimate remaining mine life. If the average mining rate seen over the past three years (6.198 million tonnes of potash ore mined and hoisted per year) is sustained, and if Mineral Reserves remain unchanged, then the Allan mine life is 56 years from December 31, 2018.

The mining of potash is a capital-intensive business subject to the normal risks and capital expenditure requirements associated with mining operations. The production and processing of ore may be subject to delays and costs resulting from mechanical failures and such hazards as: unusual or unexpected geological conditions, subsidence, water inflows of varying degree, and other situations associated with any potash mining operation.

The purpose of this document is to give a formal reporting of potash Mineral Resource and Reserve for Allan Potash, and to provide a description of the method used to compute Mineral Resource and Reserve tonnages. Sources of geological and geotechnical information analysed

All data and reports are archived at Nutrien corporate offices in Saskatoon and at the Allan minesite. In addition, drillhole data (well-log data, drilling reports, drill-stem test results, etc.) are archived with the Saskatchewan Ministry of the Economy, Integrated Resource Information System (IRIS), and surface seismic data (shot records and stack) are archived through an offsite commercial data storage service.

All geological and geophysical data and information presented in this report were personally reviewed and inspected by Nutrien technical staff under the supervision of Craig Funk (P. Eng., P. Geo., Director, Earth Science). All historic mining and mineral rights data and information presented in this report were personally reviewed and inspected by Lisa MacKenzie (GIS Cert.) and Jodi Derkach (GIS Cert., P. Geo.). Jodi Derkach (GIS Cert., P. Geo.), Tanner Soroka (P. Geo.), and James Isbister (G.I.T) conducted or were involved with geological studies and investigations at Allan, and Randy Brehm (G.I.T.), and Matthew van den Berghe (G.I.T) conducted or were involved with geophysical studies and investigations at Allan. Each of these staff visits the Allan mine numerous times every year. Additionally, geological and geophysical data and information pertaining to the Allan mine are regularly presented to and discussed with technical and engineering staff from the Allan mine.

The authors of this report would like to acknowledge former staff, Arnfinn Prugger and Terry Danyluk for their past contributions to this report. The authors would also like to thank the many staff who provided information and expert reviews on portions of this report.

Responsibility for the accuracy of the technical data presented in this report is assumed by the authors. Outside experts were not used in the preparation of this report.

The Allan mine is located in central Saskatchewan, approximately 45 kilometers east of the city

of Saskatoon, Saskatchewan. The general location is shown on the map in Figure 3.

The Legal Description (Saskatchewan Township / Range) of the Allan surface plant is Section 22 Township 34 Range 01 West of 3^rd Meridian.

The Company owns approximately 3,212 hectares (7,938 acres) of surface rights required for current Allan mine operations, including all areas covered by the existing surface plant and Tailings Management Area, and all surface lands required for anticipated future Allan mine and expanded milling operations.

All permits and approvals required for the operation of a potash mine in Saskatchewan are in place at Allan.

Figure 4 is a more detailed map showing the location of Allan Potash relative to the potash deposits in Saskatchewan.

Figure 4: Map showing Allan Potash relative to Saskatchewan potash mineralization (pink). Also shown are Company (green) and other (purple) Crown Subsurface Mineral Leases (Saskatchewan Mining and Petroleum GeoAtlas).

Mineral rights at Allan are mined pursuant to mining leases with the Province of Saskatchewan, Canada (the Crown), and with non-Crown (Freehold) mineral rights owners. Crown mineral rights are governed by The Subsurface Mineral Tenure Regulations, 2015, and Crown Leases are approved and issued by the Ministry of the Economy. The original Allan Crown Subsurface Mineral Lease, numbered KL 112, was signed and executed in September 1962. In the following years, minor amendments were made to the Lease, resulting in Crown Subsurface Mineral Lease KL 112R. In October 2017, a large area of land totaling 20,784 hectares (51,359 acres) was added to the Lease resulting in Crown Subsurface Mineral Lease KL 112R A.

KL 112R A covers an area of approximately 75,112 hectares (185,605 acres), as shown in Figure 5. At Allan, the Company has leased potash mineral rights for 45,484 hectares (112,393 acres) of Crown Land and owns or has leased approximately 17,932 hectares (44,311 acres) of Freehold Land within the lease boundary. The Allan Crown Lease term is for a period of 21 years from September 2004, with renewals (at the Company’s option) for 21 year periods. Freehold Lands also remain under lease providing, generally, that production is continuing and that there is a continuation of the Crown Lease.

Within the Allan Crown Lease area, 19,183 hectares (47,403 acres) are mined pursuant to Unitization Agreements with mineral rights holders (Crown and Freehold) within two Unitized Areas shown in Figure 5. Allan Unit Area #1 includes 9,888 hectares (24,343 acres), while Allan Unit Area #2 includes 9,295 hectares (22,969 acres).

When underground workings of a potash mine are designed, there are inevitably regions that are mined with higher mining extraction (e.g. production panels) and other regions where mining extraction is lower (e.g. conveyor-belt development rooms). To treat mineral rights holders in both low extraction and high extraction areas fairly, and to promote good mining practices, a Unitization Agreement is the preferred method for determining royalty payouts. Under a Unitization Agreement, each mineral rights holder is paid a royalty based on their proportional share of the entire Unit Area regardless of whether or not their lands are actually mined. For example, if one mineral rights holder owns rights to 4,000 hectares within a 40,000 hectare Unit Area, they would be paid 10% of the total monthly royalty payout from that Unit Area.

Figure 5: Map showing Allan Crown Lease KL 112R A (blue), Unit Area #1 (green), and Unit Area #2 (orange).

The Allan mine surface facilities are accessed by an existing paved road that is part of the Saskatchewan Provincial Highway System. All potash product is shipped by rail over existing track. Location of the Allan Potash with respect to the features described in this section (major road and rail infrastructure, as well as nearby river systems) is shown in Figure 6.

The Allan mine is served by a number of villages within 50 kilometres of the minesite. The nearest city is Saskatoon (45 km distant).

Allan is situated near the northern extent of the Great Plains of North America. Topography is relatively flat, with gently rolling hills and occasional valleys. There are no rivers or other major watercourse channels near the Allan minesite. Climate at the Allan mine is typical for an inland prairie location at latitude 52º North (often characterized as “mid-latitude steppe” climate).

Part of the normal surface infrastructure associated with operating the potash mine in Saskatchewan includes waste disposal on the land and disposal of salt brine into deep subsurface aquifers. Facilities to carry out all aspects of these tasks are in place at Allan (see Section 20.0).

Figure 6: Map showing infrastructure (City of Saskatoon, towns, rivers, roads, and railways) near Allan Potash. Allan shaft locations are shown by red markers.

Ten potash mines were brought into production in Saskatchewan in the period 1962 through 1970. With 50 years of production history, most potash mines have contracted or expanded production in response to the demand for potash. No new mines had been commissioned until 2017, when a solution mine and production facility near Moose Jaw, Saskatchewan began production. At present, eight of the eleven operating mines are conventional underground mines, and three operate using solution mining methods.

Exploration drilling for potash in the Allan area was carried out in the 1950s and 1960s. The Allan mine was built by a consortium of companies (U. S. Borax, Homestake Potash Company, and Swift Canadian Company) in the 1960s. Potash production began at Allan in April 1968 and the mine has run on a continuous basis since then (other than short-term shutdowns taken for inventory management purposes or occasional plant maintenance and construction work).

PotashCorp acquired a 60% ownership of the Allan mine in 1978 (through purchase of the U. S. Borax and Swift Canadian interests), and became the operator of the mine in 1981. In 1990, PotashCorp purchased the remaining 40% interest.

Effective January 1, 2018, PotashCorp and Agrium completed the Arrangement. As a result of completing the Arrangement, PotashCorp and Agrium are wholly-owned subsidiaries of Nutrien.

Both flotation and crystallization methods are used at Allan to produce granular, standard, and suspension-grade potash products. Debottlenecking and compaction expansion projects were completed at Allan during two phases of construction in 2005 and 2007. A major refurbishment and expansion of the Allan mine was completed in 2013, increasing nameplate capacity to 4.0 million tonnes of finished potash products per year.

Much of southern Saskatchewan is underlain by the Prairie Evaporite Formation, a layered sequence of salts and anhydrite which contains one of the world’s largest deposits of potash. The potash extracted from the predominantly sylvinite ore has its main use as a fertilizer. A map showing the extent of the potash deposits in Saskatchewan is shown in Figure 7.

Figure 7: Thickness of the Prairie Evaporite Formation and area of potash distribution within these salts (from Fuzesy, 1982).

The 100 m to 200 m thick Prairie Evaporite Formation is overlain by approximately 500 m of Devonian carbonates, followed by 100 m of Cretaceous sandstone, and 400 m of Cretaceous shales and Pleistocene glacial tills to surface; it is underlain by Devonian carbonates (Fuzesy, 1982). The Phanerozoic stratigraphy of Saskatchewan is remarkable in that units are flat-lying and relatively undisturbed over very large areas. A geological section representing Saskatchewan stratigraphy is shown in Figure 8. A geological section representing the Prairie Evaporite Formation stratigraphy in the Saskatoon area is shown in Figure 9.

Figure 8: Diagrammatic vertical section showing basic layered-Earth stratigraphy in a typical Saskatchewan potash region (from Fuzesy, 1982).

Potash mineralization in this region of Saskatchewan is predominantly sylvinite, which is comprised mainly of the minerals sylvite (KCl) and halite or rock salt (NaCl), with trace carnallite (KMgCl₃ · 6H₂O) and minor water insolubles. Potash fertilizer is concentrated, nearly pure KCl (i.e. greater than 95% pure KCl), but ore grade is traditionally reported on a % K₂O equivalent basis. The “% K₂O equivalent” gives a standard measurement of the nutrient value of different potassium-bearing rocks and minerals. To convert from % K₂O equivalent tonnes to actual KCl tonnes, multiply by 1.58.

Over the past three years (2016, 2017, 2018), the average, measured potash ore grade of the mill feed at Allan was 25.3% K₂0 equivalent. The average ore grade reported from 18 historic surface drillhole intersections, all within Allan Subsurface Mineral Lease KL 112R A, is 26.65% K₂0 equivalent (discussed further in Section 10.0). The average ore grade observed from 6,738 in-mine samples collected to the end of December 2017 is 24.8% K₂0 equivalent (discussed further in Section 11.2).

Figure 9: Diagrammatic vertical section showing basic stratigraphy of the Prairie Evaporite Formation in the Saskatoon area (from Fuzesy, 1982).

There are three mineable potash members within the Prairie Evaporite Formation of Saskatchewan. Stratigraphically highest to lowest, these members are: Patience Lake, Belle Plaine, and Esterhazy. A geological section showing potash members that occur in Saskatchewan is shown in Figure 10.

The Allan potash deposit lies within the Patience Lake Member of Prairie Evaporite Formation. There are two potash seams named A Zone and B Zone within this Member; at present, only the A Zone is being mined at Allan. Some test mining has been carried out in the B Zone, but no mining is done in this layer at present. Neither the Esterhazy nor the White Bear Potash Members are present in the Allan area. The Belle Plaine Potash Member is not well-developed, and therefore is not mined.

Allan potash mineralization occurs at about 1000 metres depth below surface. The A Zone is approximately 3.35 metres thick and occurs near the top of the Prairie Evaporite Formation salts. Salt cover from the ore zone to overlying units is approximately 14 m. The Allan mine operates as a conventional, underground potash mine.

Figure 10: Schematic cross-section across southern Saskatchewan of the Prairie Evaporite Formation showing relative position of potash members. At Allan, potash is mined from the Patience Lake Member, labeled “PLM” (from Fuzesy, 1982).

Before the Allan mine was established in 1968, all exploration consisted of drilling from surface and analysis of core from these drillholes; drilling results are discussed in Section 10.0. Since mining began in 1968, there has been just one exploration drillhole; this drillhole was completed in 1969. A map showing potash exploration coverage at Allan (drillholes, 2D and 3D seismic coverage) is shown in Figure 11. A detailed air photo showing the area around the Allan surface operations is shown in Figure 12.

In most of southern Saskatchewan, potash mineralization is in place wherever Prairie Evaporite Formation salts exist, are flat-lying, and are undisturbed. Since the surface seismic exploration method is an excellent tool for mapping the top and bottom of Prairie Evaporite salts, this has become the main potash exploration tool in any existing Saskatchewan Subsurface (potash) Mineral Lease. Historically, 2D seismic, and now the more accurate 3D seismic methods are used to map continuity and extent of potash beds in flat-lying potash deposits. Seismic data are relied upon to identify collapse structures that must be avoided in the process of mine development since these structures can act as conduits for water. As a result, isolation pillars or mining buffer zones are left around these anomalous features. This practice reduces the overall mining extraction ratio, but the risk of inflow to mine workings are effectively mitigated.

A total of 248 linear kilometres of 2D seismic lines have been acquired at Allan. Between 1988 and 2015, 3D seismic has been acquired over an area covering 363 square kilometres. The most recent seismic survey was conducted in 2015 and accounted for 49.5 square kilometres of the total square kilometres stated above.

Figure 11: Potash exploration at Allan (2D & 3D surface seismic and potash drillholes).

Figure 12: Air photo showing the Allan surface operations and Tailings Management Area.

A typical seismic section from the Allan area is shown in Figure 13. This is a fence section extracted from the “Allan 2004” 3D survey. A 2x vertical stretch has been applied to these data. The vertical scale is in metres relative to sea level (SL). The seismic section is coloured by rock velocities computed from the seismic data: blues are slow (shales), reds are fast (carbonates), and pinks / whites are intermediate (sand, salt). Note that the reflectors at both top and bottom of the unit marked Prairie Evaporite (salt) are continuous. This indicates an undisturbed, flat-lying salt within which potash is likely to be found based on 50 years of mining experience at Allan. The reflection from an Allan mine panel also shows up.

Figure 14 is a detailed (zoomed-in) view of the data plotted in Figure 13. In this figure, mine elevations from the in-mine level survey are added into the seismic data volume; the seismic data were acquired in 2004 and the room plotted in the figure was cut before seismic acquisition.

Experience has shown that the potash mining zone is continuous when seismic data are undisturbed and flat-lying, as shown in Figure 13. Surface seismic data are generally collected three to five years in advance of mining. Any area recognized as seismically unusual is identified early, and mine plans are adjusted to avoid these regions.

Figure 13: Seismic section from the Allan 2004 3D seismic data volume showing relative rock velocities. Vertical exaggeration is 2X. Sea level (SL) is marked in metres and major geological units are labeled.

Figure 14: Detail of seismic section from the Allan 3D seismic data volume (see text for explanation). Actual mine room reflection is marked in yellow. Ground surface is at approximately +500 m above Sea Level.

For the original Allan potash test holes drilled in the 1950s and 1960s, the primary objective of this drilling was to sample the potash horizons to establish basic mining parameters. Seismic surveys (2D) were done sparingly in those days, so the drillhole information was relied upon heavily to evaluate potash deposits. Test holes would penetrate the evaporite section with a hydrocarbon based drilling mud (oil-based or diesel fuel) to protect the potash mineralization from dissolution. Basic geophysical well-logs were acquired, and in many cases, drill stem tests were run on the Dawson Bay Formation to help assess mine inflow potential. Core samples from the targeted potash intersections were split or quartered (cut with a masonry saw) crushed and analysed to establish potash grades.

Relatively thin interbeds or seams, referred to as clay seams in the potash industry, are an ever-present component of the A Zone and B Zone at Allan. Figure 15 shows the basic stratigraphic relationships. These seams, along with the clay or clay-like material disseminated throughout the rock, make up the water insoluble portion of the mineralized horizons. The same sequences of clay seams can be correlated for many kilometres across the central Saskatchewan potash mining district.

At Allan, a particular sequence of three clay seams marks the top of the A Zone, as illustrated in Figure 16. These seams are used to guide the vertical positioning of the mining machine. The uppermost portion of the sequence of three seams is maintained at the top of the mining cut to keep the cutting “on grade”. Cutting too high above this upper seam or top marker results in dilution, as halite (rather than sylvinite) immediately overlies the production zone. In practice though, the top marker seam is slightly overcut (between 10 cm to 20 cm) to prevent an unstable condition from being created. Clay seams are often planes of weakness, and if they are undercut, material immediately below the clay seam becomes a hazard as it may separate and fall. Since the hazard must be remediated prior to proceeding, thus slowing production, the moderately diluted mineral grade that results from the overcutting is preferable from a safety point of view.

The A Zone mining interval was historically fixed at 3.35 m (11’). Recently acquired mining machines cut at a fixed height of 3.65 m (12’). At present, seven older mining machines cut at a height of 3.35 m (11’) and four new mining machines cut at a height of 3.65 m (12’). These mining heights allow for comfortable working headroom and efficient extraction of potash ore. It is difficult to determine at which mining height certain Mineral Resources and Reserves will be cut in the future, so the more conservative mining height of 3.35 m (11’) was applied to Mineral Resource and Reserve calculations.

Figure 15: Stratigraphic section showing local nomenclature for potash zones and approximate position of prominent clay seams (modified from Robertson 1978).

Figure 16: Typical stratigraphic section correlated with composite photos covering the A Zone production interval.

The original exploration area was explored with a number of test holes spaced at intervals of 1.6 km to 6.4 km (1 – 4 miles). Assays from most of these original test holes were studied by independent consultant David S. Robertson and Associates (1978) and are found in Table 2. An additional six historical test holes were studied by Nutrien staff in 2018; these drillhole assays are also listed in Table 2 below. In each case, the best 3.35 m (11’) mining interval intersected in each drillhole was determined from the assay values, using clay marker seams as a guide. Note that one of the above-mentioned test holes was omitted from the assay calculation due to a section of missing core in the ore zone; one was omitted due to erroneous assay data which could not be resolved; and, another two were omitted due to an ore grade of less than 15% K₂O. With 50 years of mining experience at Allan, it is the opinion of the authors that areas of low grade (i.e. <15% K₂O) are localized with a relatively small lateral extent.

Drillhole assay data for the A Zone at Allan gives an estimated mean grade of 26.65% K₂O with 4.96% water insolubles.

B Zone mineralization is indicated by gamma ray geophysical log response in each of the exploration drillholes listed in Table 2 indicating a potash Mineral Resource. Some test mining of the B Zone has been done. However, sustained production from that zone has not been established. Assay results for the B Zone are not presented here.

Table 2: Assay results for all potash test holes within Allan Lease KL 112R A.

Due to the remarkably consistent mineralogy and continuity of the resource, as experienced through 50 years of mine production, no potash exploration drilling has been done at Allan since 1969. Instead of exploration drillholes, seismic surveying has been relied upon to explore ahead of mine development. Where normal Prairie Evaporite sequences are mapped in the seismic data, potash beds have unfailingly been present. Localized, relatively small mine anomalies, not mapped in seismic data do occur. When they do, they are dealt with in the

normal course of mining and extraction through these anomalous areas is typically minimized. Anomalies associated with possible water inflow problems, which are mapped in the seismic data, are avoided.

Exploration in the Allan area was conducted in the 1950s and 1960s. Sampling and assaying of potash core samples was done using methods considered consistent with standard procedures for potash exploration at these times.

Drillhole sampling methods have remained essentially the same over the years. Potash core samples are acquired as described in earlier sections of this report. Short segments of core usually about 1 foot (0.3 m) in length are labeled based on visible changes in mineralization, and sometimes based on more or less fixed intervals. Each segment of core is then split using some type of rock or masonry saw. The split portion of core is then bagged and labeled and sent to a laboratory for chemical analysis. Historical potash samples remain stored at the Subsurface Geological Laboratory (Regina, Saskatchewan) of the Saskatchewan Ministry of the Economy. Most of these have deteriorated substantially.

An assay plot for drillhole PCS Allan 09-27-034-01 W3 is shown below in Figure 17. Similar data were compiled for all historical potash test holes. The best 3.35 m (11’) mining interval intersected in each drillhole, as discussed in Section 10.0, is determined from the assay values, using clay seams as a guide. Table 3 lists the assay values plotted in Figure 17.

Figure 17: Potash assay plot for PCS Allan 09-27-034-01 W3 indicating the best 3.35 m (11’) mining interval.

A total of 6,738 in-mine ore grade samples were collected at Allan to the end of December 2017 (discussed further in section 11.2). All in-mine samples were analysed in the Allan mill laboratory using analysis techniques that were up-to-date for the era in which the sample was collected.

Regarding quality assurance for analytical results of in-mine samples, the Company participates in the Saskatchewan Potash Producers Association (SPPA) Sample Exchange Program to monitor the accuracy of analytical procedures used in its labs. In the early 1970s, the SPPA initiated a round-robin Sample Exchange Program, the purpose of which was to assist the potash laboratories in developing a high level of confidence in analytical results. This program has continued up to the present, and participants include all major Canadian potash mine site labs, the Nutrien Pilot Plant Lab, and an independent surveyor lab. The Sample Exchange Program provides the participants with three unknown potash samples for analysis four times per year. Results for the unknown sample analysis are correlated by an independent agency that distributes statistical analysis and a summary report to all participants. Completed SPPA

samples can be used for control standards as required in QA/QC sections of standard analytical procedures.

The Nutrien Pilot Plant is secured in the same way as modern office buildings are secured. Authorized personnel have access and visitors are accompanied by staff. No special security measures are taken beyond that. Currently, no external laboratory certification is held by the Nutrien Pilot Plant. On occasion, product quality check samples are sent to the Saskatchewan Research Council, a fully certified analytical facility.

In the opinion of the authors, the sampling methods are acceptable, are consistent with industry-standard practices, and are adequate for Mineral Resource and Reserve estimation purposes.

At Allan, in-mine grade samples are taken from the floor approximately once per week per active mining face. This is roughly equivalent to a sample taken every 68 m to 74 m in production panels, and a sample taken every 85 m to 128 m in development panels. Since start-up in 1968 through to the end of December 2017, a total of 6,738 in-mine potash mineral grade samples were collected from the Allan A Zone, the main potash horizon at Allan. In-mine samples collected and analysed in 2018 contributed no meaningful change to the overall mineral ore grade. All samples were analysed in the Allan mill laboratory using analysis techniques that were up-to-date for the era in which the sample was collected. Figure 18 shows a histogram of A Zone in-mine grade sample results from the Allan mine.

Figure 18: Histogram of potash ore grade from 6,738 Allan in-mine grade samples (data from 1968 through to end of December 2017).

The median ore grade for this family of in-mine samples is 25.5% K₂O equivalent and the mean ore grade is 24.8%. This is considered to be a more representative estimate of expected potash ore grade at Allan than drillhole assay results presented in Section 10.0.

For the B Zone at Allan, mineral grade is reported to be 20.3% K₂O equivalent, the grade observed from 20,230 in-mine samples at the Lanigan mine where the B Zone has been extensively mined. Even though Allan mine is some distance from Lanigan, this is considered the best estimate of expected mineral grade for this potash layer because the deposit is known to be regionally continuous from west of Cory to east of Lanigan (Fuzesy, 1982 and references therein). Although it is possible that once mining proceeds into the B Zone the reported grade could change from what is reported, it is expected that any such change would be minimal.

An estimate of in-situ rock density is used to calculate potash mineralization volumes in Mineral Resource and Reserve assessments. A common approach is to determine in-place Mineral Resource and Reserve volumes (m³) to a certain degree of confidence, then multiply this number by in-situ bulk-rock density (kg / m³) to give in-place Mineral Resource and Reserve tonnes. However, establishing an accurate bulk-rock density value is not an easy or trivial task. Well-log data from drillholes can be used for this if accurate and calibrated well-logs are acquired during exploration drilling. In practical terms, modern well-logs tend to meet these criteria, but historic well-logs (collected before the 1990s) do not. In Saskatchewan, almost all potash exploration drilling took place in the 1950s and 1960s, well before density logs were accurate and reliable.

Another approach is to look up density values for the minerals which constitute potash rock – values determined in a laboratory to a high degree of accuracy and published in reliable scientific journals / textbooks – then apply these densities to the bulk-rock in some way. Given that the density of each pure mineral is quantified and known, the only difficult aspect of this approach is determining what proportion of each mineral makes up the bulk-rock at a particular sample location. This is the methodology that was used to determine an estimate of bulk-rock density for the Allan ore zone. An obvious benefit of this approach is that a mean value computed on the distribution shown in Figure 18 (6,738 sample points) has a much greater confidence interval than a mean value computed from 18 drillhole assays.

The main mineralogical components of the ore zones of Saskatchewan’s Prairie Evaporite Formation are:

All Nutrien potash mines measure and record the in-mine % K₂O grade and insoluble content of the mined rock. The magnesium content is not measured at Allan, since carnallite is not a significant component of the ore here. From this set of measurements, the density of the ore can be calculated. The required composition and mineral density information for each mineral component is given below (Webmineral Mineralogy Database):

The value for insoluble density is based on known densities of the constituent parts of the insoluble components of the mineralization and the average occurrence of these insoluble components, which is known from the 50 years of mining experience at Allan. Assuming the lowest plausible density of insolubles known for Saskatchewan potash deposits of this nature, the effect upon overall bulk-rock ore density and Mineral Resource and Reserve calculations would be negligible.

The mineral composition of potash ore is halite, sylvite, and insolubles. From 6,738 Allan A Zone in-mine grade samples, raw ore composition is:

Applying this methodology, and using these mean grade data gives a mean bulk-rock density for Allan A Zone potash of:

RHObulk-rock

= (Halite density * % Halite) +

(Sylvite density * % Sylvite) +

(Insol. density * % Insol.)

= (2170 * % Halite) +

(1990 * % Sylvite) +

(2510 * % Insol.)

= 2110

This method is as accurate as the ore grade measurements and mineral density estimates.

To date, not enough B Zone mining has been carried out at Allan to permit a bulk density calculation based on Allan in-mine grade samples. The mining of 3.537 million tonnes of the B Zone represents a relatively small amount of material for a potash mine. The historic mining that was conducted in the B Zone at Allan was localized in only one geographic area, so data from this mining is not considered representative of what will be seen once mining proceeds in this layer. Although it is possible that once enough mining has occurred in the B Zone to give enough samples with all constituent minerals measured, the reported proportions of the various mineral constituents could change from what is reported. It is expected that any such change would have only a minimal effect on bulk-rock density used in tonnage calculations.

Instead, the potash bulk-rock density is calculated using 20,230 in-mine grade samples from Lanigan B Zone:

This estimate is considered acceptable since both Allan B Zone and Lanigan B Zone are the same potash seam. Should the Allan B Zone bulk density change from the predicted value of 2120 kg / m³, the later defined Allan B Zone Mineral Resources and Reserves in Sections 14.2 and 15.2 will also change, albeit, insignificantly.

Most of the original drillhole assays were studied by independent consultant David S. Robertson and Associates (1978). In 2018, six historical drillhole assay results were studied by Nutrien technical staff, Jodi Derkach (GIS Cert., P. Geo.) and Tanner Soroka (P. Geo.).

The original assay results for core samples from historical drillholes were taken as accurate in these studies, as there is no way to reliably reanalyse these samples. Most of the remaining samples in storage have long since deteriorated to the point where they are not usable.

Ore grades of in-mine samples are measured inhouse at the Allan mine laboratory by Company staff using modern, standard chemical analysis tools and procedures; an independent agency does not verify these results. However, check sampling through the SPPA program, discussed in Section 11.1, does occur.

It should be noted that assay results from historical drillholes match mine sample results closely – within approximately 0.9% – even though sample spacing is obviously much greater in the case of wells. This fact is a validation of the methodology. Based on 50 years of in-mine experience at Allan, historical assay results are considered acceptable and provide a good basis for estimating ore grade in areas of future mining at Allan. However, the mean mineral grade of 24.8% K₂O equivalent determined from 6,738 in-mine grade samples is thought to provide the most accurate measurement of potash grade for the Allan mine.

The purpose of any mineral exploration program is to determine extent, continuity, and grade of mineralization to a certain level of confidence and accuracy. For potash exploration, it is important to minimize the amount of cross-formational drilling, since each drillhole is a potential conduit for subsurface groundwater from overlying (or underlying) water-bearing formations into future mine workings. Every potash test drillhole from surface sterilizes potash mineralization; a safety pillar is required around every surface drillhole once underground mining commences. This is the main reason that exploration drilling has not been carried out at Allan in recent years.

Initial sampling and assaying of cores was done during potash exploration at Allan in the 1950s and 1960s. Methods were consistent with standard procedures for that era. The mine began production in 1968 and, with the exception of a single potash test hole in 1969, no further core drilling has been carried out since then. This approach to potash sampling is in accordance with widely accepted industry practice for areas adjacent and contiguous to an existing operating potash mine.

Assay of physical samples (drillhole cores and/or in-mine samples) is the only way to gain information about mineral grade, but extent and continuity of mineralization are correctly determined using data collected from geophysical surveys correlated with historic drilling information. To date, surface seismic data at Allan have been collected, analysed, and verified by Company staff, at times, in cooperation with an independent consultant. Ultimate responsibility for final analyses including depth conversion (seismic depth migration), as well as the accuracy of these data, rests with Nutrien qualified persons.

Data for the Mineral Resource and Reserve estimates for Allan mine reported in Sections 14.0 and 15.0 were verified by Company staff as follows:

This approach to data verification of potash mineral grade and surface seismic information is in accordance with generally accepted industry practice for areas adjacent and contiguous to an existing operating potash mine.

At Allan, potash ore has been mined and concentrated using flotation and crystallization methods to produce saleable quantities of high-grade finished potash products since 1968.

Over the 50-year mine life, 150.239 million tonnes of potash ore have been mined and hoisted to produce 52.949 million tonnes of finished potash product (from startup in 1968 to December 31, 2018). Given this level of sustained production over 50 years, basic mineralogical processing and prospective metallurgical testing of Allan potash is not considered relevant.

The Canadian Institute of Mining and Metallurgy and Petroleum (CIM) has defined Mineral Resource in The CIM Definition Standards for Mineral Resources and Reserves (2014) as:

CIM defines Modifying Factors as “considerations used to convert Mineral Resources into Mineral Reserves. These include, but are not restricted to, mining, processing, metallurgical, infrastructure, economic, marketing, legal, environmental, social and governmental factors.”

In south-central Saskatchewan, where geological correlations are straightforward, and within a (potash) Subsurface Mineral Lease with an operating potash mine, Mineral Resource categories are generally characterized by PotashCorp as follows:

The mine began production in 1968 and, with the exception of a single test hole in 1969, no further core drilling has been carried out since then. Instead, exploration involved collecting surface seismic data, which became better in quality over the years. Exploration drilling has demonstrated the presence of the potash horizon, and seismic coverage shows the continuity of the Prairie Evaporite Formation within which the potash horizon occurs.

Along with this approach, analysis of in-mine samples for potash grade has provided an observation-based understanding of the potash mineralized zone at Allan that is far superior to the level of understanding provided by any surface drilling based exploration program. The authors believe that this approach provides a body of information that guides and constrains exploration inferences in a much better way than could be achieved from any conventional exploration investigation in areas immediately surrounding, and contiguous to, the Allan potash mine.

Exploration information used to calculate reported Mineral Resource tonnages at Allan consist of both physical sampling (drillhole and in-mine) and surface seismic (2D and 3D) as discussed in earlier sections. Based on the definitions and guidelines in Section 14.1, all mineral rights leased or owned by the Company, and within Crown Subsurface Mineral Lease KL 112R A, are assigned to one of the three Mineral Resource categories.

Mineral Resources are reported as mineralization in-place and are exclusive of Mineral Reserves. In-place tonnes were calculated for each of the Mineral Resource categories using the following parameters:

The average mineral grade of the Allan A Zone Mineral Resource is 24.8% K₂0 equivalent, and was determined from 6,738 in-mine samples at Allan. The average mineral grade of the Allan B Zone Mineral Resource is 20.3% K₂0 equivalent, and was determined from 20,230 in-mine samples at Lanigan mine where the B Zone has been extensively mined. See Section 11.2 for more detail.

The tonnage reported in the Allan A Zone Measured Resource is comprised of the potash that is within 1.6 km (1 mile) of physically sampled location (i.e. drillholes or mine workings). Also included as Measured Resource is the potash that is left behind as pillars in mined-out areas of the Allan mine. In a potash mine, it is common practice to consider mining remnant pillar mineralization using solution methods after conventional mining is complete, or after a mine is lost to flooding. The Patience Lake mine was successfully converted from a conventional mine to a solution mine after being lost to flooding in 1989. Since conversion to a solution mine is not anticipated in the near future at Allan, in-place pillar mineralization remains as a Mineral Resource rather than a Mineral Reserve at this time.

Figure 19: Map showing Allan Mineral Resource with mine workings to December 2018.

The Canadian Institute of Mining and Metallurgy and Petroleum (CIM) has defined Mineral Reserve in The CIM Definition Standards for Mineral Resources and Reserves (2014) as:

For Saskatchewan, in regions adjacent and contiguous to an operating potash mine, Mineral Reserve categories are characterized by PotashCorp as follows:

Along with this approach, analysis of in-mine samples for potash grade has provided an observation-based understanding of the potash mineralized zone at Allan that is far superior to the level of understanding provided by any surface drilling based exploration program. An understanding of the amount of ore that can be conventionally mined from the Measured Resource category using current mining practices comes from 50 years of potash mining experience at Allan.

Using the definitions outlined in Section 15.1, part of the Allan A Zone Measured Resource has been converted to Mineral Reserve. The assigned Mineral Reserve category is dependent on proximity to sampled mined entries also described in Section 15.1. An overall extraction rate

for the Allan mine has been applied to the qualifying areas outlined as Measured Resource in Figure 19. This extraction rate is significantly lower than the local extraction rate described in Section 16.1, as it takes into account areas which cannot be mined due to unfavorable geology.

The overall extraction rate at the Allan mine is 33%. It was derived by dividing the total tonnes mined to date by the tonnage equivalent of the total area of the mine workings (i.e. the perimeter around the mine workings) less future mining blocks. Since an extraction rate has been applied, Mineral Reserves are considered recoverable ore, and are reported as such.

The average mineral grade of the Allan A Zone Mineral Reserve is 24.8% K₂0 equivalent, and was determined from 6,738 in-mine samples at Allan.

Figure 20: Map showing Allan Mineral Reserve with mine workings to December 2018.

All conventional potash mines in Saskatchewan operate at 900 m to 1200 m below surface within 9 m to 30 m of the top of the Prairie Evaporite Formation. Over the scale of any typical Saskatchewan potash mine, potash beds are tabular and regionally flat-lying, with only moderate local variations in dip. At Allan, potash ore is mined using conventional mining methods, whereby:

Sinking of the two original shafts (Shaft #1 and Shaft #2) from surface to the potash zone was completed in early 1968, and the first potash ore was hoisted by in April of that year. The Allan mine has run on a continuous basis since the first ore was hoisted in 1968, other than short-term shutdowns taken for inventory management purposes or occasional plant maintenance and construction work.

In recent years, the Allan mine underwent a major expansion which brought the nameplate capacity up to 4.0 million tonnes of finished potash products per year. The operational capability at the Allan facility as of December 31, 2018 is 2.6 million tonnes per year.

Virtually all Allan underground mining rooms are in one potash mineralized zone, the upper layer (or A Zone) of the Patience Lake Member of the Prairie Evaporite Formation (the host evaporite salt). In contrast, some potash mines further east in Saskatchewan mine in a different potash layer, the Esterhazy Member of the Prairie Evaporite Formation. Saskatchewan potash geology is illustrated in Figure 21. At Allan, mine elevations range from approximately 980 m to 1120 m, averaging approximately 1010 m. These depths to A Zone potash mineralization are anticipated over most of the Allan lease area. Mine workings are protected from aquifers in overlying formations by approximately 14 m of overlying salt and potash beds, along with salt plugged porosity in the Dawson Bay Formation, a carbonate layer lying immediately above potash hosting salt beds.

The Allan mine is a conventional underground mining operation whereby continuous mining machines are used to excavate the potash ore by the stress-relief mining method. Continuous conveyor belts transport ore from the mining face to the bottom of the production shaft. Mining methods employed in Saskatchewan are discussed in Jones and Prugger (1982) and in Gebhardt (1993). The highest mineral grade section of the Allan potash seam is approximately 3.35 m (11’) thick, with gradations to lower grade salts immediately above and below the

mining horizon. The actual mining thickness at Allan is dictated by the height of continuous boring machines used to cut the ore. Seven older borers are designed to cut at a thickness of 3.35 m (11’) and four new borers are designed to cut 3.65 m (12’).

As discussed in Section 10.0, Allan cuts to a marker (clay) seam that is slightly above the high-grade mineralized zone to establish a safe and stable mine roof. The top marker seam is slightly overcut by 10 to 20 cm. Clay seams are often planes of weakness, and if they are undercut, material immediately below the clay seam becomes a hazard as it may separate and fall. Since the hazard must be remediated prior to proceeding, thus slowing production, the moderately diluted mineral grade that results from the overcutting is preferable from a safety point of view.

Figure 21: Typical stratigraphic section correlated with composite photos covering both the Patience Lake Member and the Esterhazy Member potash production intervals. At Allan, mining takes place in the Upper Patience Lake Member (A Zone).

Conservative local extraction rates (never exceeding 45% in any mining block) are employed at all Saskatchewan mines, including Allan, in order to minimize potential detrimental effects of mining on overlying strata; this is common practice in flat-lying, tabular ore bodies overlain by water-bearing layers.

From the shaft-bottom, potash ore is hoisted approximately 1000 m from the potash level through the vertical shafts to a surface mill. In addition to hoisting potash ore to surface, the production shaft also provides fresh air ventilation to the mine and serves as a secondary egress. The Service Shaft is used for service access, and exhaust ventilation from the mine.

Actual potash production tonnages for the Allan mine, along with concentration ratios (tonnes mined / tonnes product), are plotted for the past decade in Figure 22.

Figure 22: Actual mining, production and concentration ratio for the Allan mine over the past 10 years.

The mining of potash is a capital-intensive business, subject to the normal risks and capital expenditure requirements associated with mining operations. The production and processing of ore may be subject to delays and costs resulting from mechanical failures and such hazards as unusual or unexpected geological conditions, subsidence, water inflows of varying degree, and other situations associated with any potash mining operation.

Potash beds in all regions of Saskatchewan are overlain by a number of water-bearing formations, and there are water zones underlying the potash beds as well. A water inflow into mine workings is generally significant in a potash mine since salt dissolves in water; an inflow can lead to anything from increased costs at best to closure of the mine at worst (e.g. see Prugger and Prugger, 1991).

When sinking of the Allan Shaft #1 was near the bottom of the Blairmore Formation at approximately 570 m depth, a breach developed in the ice wall and the shaft was flooded (Prugger and Prugger, 1991). A concrete plug was installed in the shaft bottom (underwater), and two additional freeze holes were drilled to seal the area of the breach and allow recovery of the shaft. The shaft was completed in 1968. In the mid-1990s the concrete shaft liner in an area of the Allan production shaft had deteriorated to the point where it required replacement. The concrete in the 671 m to 750m (2203’ to 2463’) level was replaced with iron tubbing segments in 1999, successfully repairing the shaft through this area. Further shaft repairs were made just below this zone in 2017. At present, inflow into the existing shafts is estimated at 25 litres / minute (6 US gallons / minute) for the Service Shaft and 145 litres / minute (38 US gallons / minute) for the Production Shaft.

In 1996, a connate potash seam brine was encountered in an area that had recently been mined; this was the first inflow into underground workings at Allan. This inflow, initially estimated at approximately 20 litres / minute, did not require active intervention, and the flow eventually diminished to virtually nil. There have been a few similar occurrences of brine in underground workings at Allan; all of these have been minor occurrences that were addressed without any impact to mine operations. There has not been any significant water ingress into underground workings at Allan since production began in 1968. At present, brine ingress into underground mine workings at Allan is effectively nil (not measurable).

At Allan, potash ore has been mined and concentrated to produce saleable quantities of high grade finished potash products since 1968. Products include granular, standard, and industrial grade potash used for agricultural applications and industrial purposes.

Both flotation methods and crystallization methods are used to concentrate potash ore into finished potash products at the Allan mill. A simplified process flow diagram is shown in Figure 23. Raw potash ore is processed on surface, and concentrated finished potash products (near-pure KCl) are sold and shipped to markets in North America and offshore.

2016: 2.380 million tonnes finished potash products at 61.16% K₂O (average grade)

2017: 1.832 million tonnes finished potash products at 61.39% K₂O (average grade)

2018: 2.410 million tonnes finished potash products at 61.17% K₂O (average grade)

Over the past decade actual mill recovery rates have been between 81.5% and 87.0%, averaging 84.6% (see Figure 24). Given the long-term experience with potash geology and actual mill recovery at Allan, no fundamental potash milling problems are anticipated in the foreseeable future.

Quality control testing and monitoring geared towards fine-tuning and optimizing potash milling and concentrating processes are conducted on a continual basis at all Nutrien minesites and at Nutrien research facilities. At Allan, this is no exception; test work to optimize circuit performance and ensure product quality is carried out on an ongoing basis.

Infrastructure is in place to meet current and projected requirements for transportation, energy (electricity and natural gas), water and process materials at Allan. See also Section 5.0.

The Allan mine is served by a number of villages within 50 kilometres of the minesite. The nearest city is Saskatoon (approximately 45 km distant).

The Allan surface facilities are accessed by existing paved roads and highways that are part of the Saskatchewan Provincial Highway System. All potash product is shipped by rail over existing track.

At present, high voltage power capacity at the Allan is 32 MVA. The ten-year projection of power utilization indicates that the utility can meet all foreseeable future demand.

The Allan operation requires a sustained fresh water supply for the milling process which is provided from a local reservoir called the Bradwell Reservoir operated by SaskWater (approximately 6 km distant). This water supply provides a sustainable source of process water for Allan milling operations without having any impact on other users of water in the area.

Potash from Company mines (including Allan) has been sold on a continuous basis since mining began in 1968. At present, Nutrien products are sold in more than 50 countries, to three types of end-use:

The Company owns and operates six potash mines in Saskatchewan and owns one potash mine in New Brunswick, Canada. The potash mine in New Brunswick is currently in care-and-maintenance mode and is planned to be permanently shut down. Over the past three years (2016, 2017, 2018) the Company had potash sales of 30.959 million tonnes¹. Historical Company potash sales data for the past 10 years are plotted in Figures 25 and 26¹.

Potash is mainly used for fertilizer, which typically makes up approximately 90 percent of the company’s annual potash sales volumes. By helping plants develop strong root systems and retain water, it enhances yields and promotes greater resistance to disease and insects. Because it improves the taste and nutritional value of food, potash is often called the “quality nutrient.” Industrial applications of potash include use in soaps, water softeners, de-icers, drilling muds and food products.

Potash fertilizer is sold primarily as solid granular and standard products. Granular product has a larger and more uniformly shaped particle than standard product and can be easily blended with solid nitrogen and phosphate fertilizers. It is typically used in more advanced agricultural markets such as the US and Brazil.

Most major potash consuming countries in Asia and Latin America have limited or no indigenous production capability and rely primarily on imports to meet their needs. This is an important difference between potash and the other major crop nutrient businesses. Trade typically accounts for approximately three-quarters of demand for potash, which ensures a globally diversified marketplace.

The most significant exporters are producers with mines in the large producing regions of Canada, the Middle East and the former Soviet Union, which all have relatively small domestic requirements.

World consumption of potash fertilizer has grown over the last decade, with the primary growth regions being developing markets in Asia and Latin America. These are countries with expanding crop production requirements, where potash has historically been under-applied and crop yields lag behind those of the developed world. Although temporary pauses can occur in certain countries, the underlying fundamentals of food demand that encourage increased

potash application are expected to continue the growth trends in key importing countries. See Figure 27 for world potash production and demand in 2017.

Figure 25: Historical Company potash sales 2009 to 2018 in million tonnes / year².

Figure 26: Historical Company potash net sales 2009 to 2018 in million USD $ / year².

Potash is used on many agricultural commodities. Wheat, rice, corn, oilseed, and sugar crops consume over half of the potash used worldwide. Fruits and vegetables are also important users of potash fertilizers, accounting for about 19 percent of the total consumption. The remainder goes to other consumer and industrial crops such as oil palm, rubber, cotton, coffee, and cocoa. See Table 4 for primary potash market profile. This diversity means that global potash demand is not tied to the market fundamentals for any single crop or growing region.

Global potash shipments surpassed 66 million tonnes in 2018, an increase of more than 1 million tonnes from the previous record set in 2017. Potash demand has grown at an annualized rate of more than 4 percent over the past 5 years, well above the long-term average

of 2.5 to 3.0 percent. This growth is driven by strong potash consumption trends in all major potash markets.

North American and South American growers applied significant amounts of potash to replenish soil nutrients removed by large harvests. Potash application rates are increasing in China and Southeast Asian countries as a result of increased soil testing and improved agronomic practices. Growers in these countries are also increasing acreage of potassium-intensive crops such as fruits, vegetables and oil palm. India continues to face political barriers to significantly growing potash demand, however, the agronomic need and willingness of farmers to improve yields persists. The Company believes that supportive agriculture fundamentals and the need to address declining soil fertility levels will enable strong demand growth in the years ahead. World potash shipments and consumption in recent years is shown in Figure 28.

Canpotex Limited (Canpotex), the offshore marketing company owned by the Company and other Saskatchewan potash producers, handles all sales, marketing and distribution of potash produced by its member companies to customers outside of the US and Canada (including the potash produced at Allan).

In North America, Nutrien sells potash to retailers, cooperatives, and distributors, who provide storage and application services to farmers, the end-users. This includes sales to Nutrien’s retail distribution business, which has the largest retail distribution network in North America. Typically, the Company’s North American potash sales are larger in the first half of the year. The primary customers for potash fertilizer products at the Allan operation are retailers,

dealers, cooperatives, distributors and other fertilizer producers who have both distribution and application capabilities.

Nutrien’s market research group provides management with market information on a regular basis including global agriculture and fertilizer markets, demand and supply in fertilizer markets and general economic conditions that may impact fertilizer sales. These may include specific market studies and analyses on different topics as may be required. This information is reviewed on a regular basis and the author of this report takes this information into account in understanding the markets and the assumptions within this report.

Plans and arrangements for potash mining, mineral processing, product transportation, and product sales are established by Nutrien and are within industry norms.

The tailings management strategy at all Nutrien potash mines in Saskatchewan, including Allan, is one of sequestering solid mine tailings in an engineered and provincially licenced Tailings Management Area (TMA) near the surface plant site. The Allan TMA currently covers an area of approximately 600 hectares (1,483 acres) of land owned by the Company. Solid potash mine tailings typically consist of 85% to 95% rock salt (NaCl) and 5% to 15% insolubles (carbonate mud = CaCO₃, anhydrite mud = CaSO₄, and clays like chlorite, illite, and so on). An engineered slurry-wall (in some portions, a compacted earth trench barrier) has been constructed where required around approximately half of the Allan TMA. In future years this wall can be expanded if required for operational needs. The slurry-wall provides secondary containment for any saline mine waters, minimizing brine impacts from the TMA to surrounding surface water bodies and near-surface aquifers. Areas surrounding the TMA are closely monitored: this includes everything from daily visual perimeter inspections to annual investigations and inspections of surrounding groundwater and aquifers.

Allan currently operates two brine disposal wells near the surface plant of the Allan mine (marked in Figure 12) where clear salt brine (i.e. no silt, clay slimes, or other waste) is borehole-injected into the Winnipeg / Deadwood Formations, deep subsurface aquifers approximately 1500 m to 1700 m below the surface (marked in Figure 13). The groundwater in these extensive deep aquifers is naturally saline.

Emissions to air (mostly salt dust and potash dust) are kept below regulatory limits through various modern air pollution abatement systems (e.g. dust collection systems built into mill processes) that are provincially licensed. This same procedure is followed at all Nutrien mines in Saskatchewan.

The Allan operation requires a sustained fresh water supply for the milling process which is provided by a waterline from the Bradwell Reservoir (approximately 6 km distant). This water supply is provincially licensed and provides a sustainable source of process water for Allan milling operations without having any impact on other users of water in the area.

In Saskatchewan, all potash tailings management activities are carried out under an “Approval to Operate” granted by the Saskatchewan Ministry of Environment (MOE), the provincial regulator. The Allan mine is in compliance with all regulations stipulated by the Environmental Protection Branch of MOE. The current Allan Approval to Operate has been granted to July 1, 2028, the renewal date.

In terms of long-term decommissioning, environmental regulations of the Province of Saskatchewan require that all operating potash mines in Saskatchewan create a long-term decommissioning and reclamation plan that will ensure all surface facilities are removed, and the site is left in a chemically and physically stable condition once mine operations are complete. The Company has conducted numerous studies of this topic, and the most recent decommissioning and reclamation plan for Allan was approved by MOE technical staff in October 2016. Because the current expected mine life for Allan is many decades into the future, it is not meaningful to come up with detailed engineering designs for decommissioning at present. Instead, decommissioning plans are reviewed every five years, and updated to accommodate new ideas, technological change, incorporation of new data, and adjustments of production forecasts and cost estimates. Any updated decommissioning and reclamation reports generated by this process are submitted to provincial regulatory agencies. For Allan, a revised decommissioning and reclamation plan is required in July 2021.

In addition to the long-term decommissioning plan, provincial regulations require that every potash producing company in Saskatchewan set up an Environmental Financial Assurance Fund, which is to be held in trust for the decommissioning, restoration and rehabilitation of the plant site after mining is complete. This fund is for all mines operated by Nutrien in the province of Saskatchewan (i.e. Allan, Cory, Lanigan, Patience Lake, Lanigan, Rocanville, and Vanscoy).

The Allan mine has been in operation since 1968; in the years immediately preceding this, major capital investment was made to bring this mine into production. Since then, capital expenditures were made on a regular and ongoing basis to sustain production, and to expand production from time to time.

A major refurbishment and expansion of the Allan mine was completed in 2013, increasing nameplate capacity to 4.0 million tonnes of finished potash products per year. This work involved enhancement of hoists and shaft conveyances, major expansions of both mine and mill, improvements to loadout facilities, and some infrastructure improvements. All construction was carried out without significant disruption to existing potash production from the site.

The Company conducts ongoing and detailed economic analyses on each of its operations and on all aspects of its business. While the Company considers its operating costs and results on a per mine basis to be competitively sensitive and confidential information, the Company is confident that the economic analysis conducted routinely for each of the Company’s operating potash mines is complete, reasonable, and meets industry standards.

On a cash flow basis, the Company’s potash segment generated USD $5,702 million in net sales over the past three years (2016, 2017 and 2018) based on sales volume of 30.959 million tonnes of finished potash products³. The annual average realized potash price for manufactured products (includes North American and offshore sales) over a 10-year period (2009 – 2018) is plotted in Figure 29.

Over the past three years (2016, 2017, and 2018) the Allan mine produced 6.621 million tonnes of finished potash products. In the past three years (2016, 2017, and 2018), the Allan mine accounted for 18% of total potash production at the Company over this time period. Allan is currently making a positive contribution to the Company’s potash segment.

Given the Company’s previous history (including 50 years of mining at the Allan operation), recent market conditions, and extensive reserve base, the economic analysis for Allan has met the Company’s internal hurdle rates.

Royalties are paid to the Province of Saskatchewan, which holds approximately half of the mineral rights in the Allan Crown Subsurface Mineral Lease. Royalties from non-Crown lands are paid to various freeholders of mineral rights in Saskatchewan. The crown royalty rate is 3% and is governed by The Subsurface Mineral Royalty Regulations, 2017. The actual amount paid is dependent on selling price and production tonnes.

Saskatchewan potash production is taxed at the provincial level under The Mineral Taxation Act, 1983. This tax, governed by The Potash Production Tax Regulations, consists of a base payment and a profit tax, collectively known as the potash production tax. As a resource corporation in the Province of Saskatchewan, Nutrien is also subject to a resource surcharge that is a percentage of the value of its resource sales (as defined in The Corporation Capital Tax Act of Saskatchewan).

In addition to this, Nutrien pays federal and provincial income taxes based on corporate profits from all its operations in Canada.

The Company’s Allan Lease KL 112R A is adjacent to the following potash dispositions (Figure 30).

For up-to-date information on Crown Potash Leases and Exploration Permits, see the Saskatchewan Mining and Petroleum GeoAtlas which is available online at the Government of Saskatchewan website.

Mosaic Potash Colonsay (Mosaic) operates a mine with extensive underground workings within Crown Subsurface Mineral Lease KL 108, which are immediately adjacent to Allan Lease KL 112R A. The Company and Mosaic each have a safety buffer between the two companies’ lease areas, where it is agreed that no mining will occur. This buffer ensures that mine workings in one company’s lease area will not impact workings of the other company.

PotashCorp has a long history of successful potash mining at Allan, where potash has been produced for the past 50 years. The authors believe that the experience gained mining and milling potash for this length of time has produced a reliable body of information about potash mineralization, mining and milling at Allan.

In a Saskatchewan potash mine that has been producing for many decades, reduction of mine life through increased production is counter-balanced by development mining into new mineral land parcels. This increases mine life through increasing the potash Mineral Reserve.

For Allan, mine life can be estimated by dividing the total Mineral Reserve (Proven + Probable) of 349 million tonnes by the average annual mining rate (million tonnes of ore hoisted per year). For Allan, the mining rate is defined as equal to the actual three-year running average (consecutive, most recent years). The average mining rate at Allan over 2016, 2017 and 2018 was 6.198 million tonnes of potash ore mined and hoisted per year.

If this mining rate is sustained and if Mineral Reserves remain unchanged, then the Allan mine life would be 56 years.

This estimate of mine life is likely to change as mining advances further into new mining blocks, and / or if mining rates change.

Companion Policy 43-101CP to National Instrument 43-101 Standards of Disclosure for Mineral Projects (2011). Retrieve this and related documents from many websites (e.g. CIM: http://web.cim.org/standards/documents/Block484_Doc111.pdf).

The CIM Definition Standards for Mineral Resources and Reserves (2014). Retrieve this and related documents from many websites (e.g. Committee for Mineral Reserves International Reporting Standards, http://www.crirsco.com/national.asp).

Fuzesy, Anne (1982). Potash in Saskatchewan (44p). Saskatchewan Industry and Resources Report 181.

Gebhardt, E. (1993). Mine planning and design integration, CIM Bulletin, May 1993, pp. 41 – 49.

https://gisappl.saskatchewan.ca/Html5Ext/index.html?viewer=GeoAtlas. Accessed Jan 2019.

Government of Saskatchewan. The Corporation Capital Tax Act of Saskatchewan. Available online at http://www.qp.gov.sk.ca/documents/English/Statutes/Statutes/c38-1.pdf.

Government of Saskatchewan. The Mineral Taxation Act, 1983. Available online at http://www.qp.gov.sk.ca/documents/English/Statutes/Statutes/M17-1.pdf.

Government of Saskatchewan. The Subsurface Mineral Royalty Regulations, 2017. Available online at

Government of Saskatchewan. The Subsurface Mineral Tenure Regulations, 2015. Available online at

Jones, P. R. and F. F. Prugger (1982). Underground mining in Saskatchewan potash. Mining Engineering, 34, pp. 1677 – 1683.

Nutrien Pilot Plant (2018). Personal communication on density of insoluble minerals in different ore zones.

Prugger, F. F. and A. F. Prugger (1991). Water problems in Saskatchewan potash mining – what can be learned from them? Bulletin of the Canadian Institute of Mining and Metallurgy (CIM Bulletin), Vol. 84, No. 945, pp. 58 – 66.

Robertson, David S. and Associates (1978). Summary Report on Evaluation of Potash Assets for Potash Corporation of Saskatchewan. Unpublished consultant’s report to Potash Corporation of Saskatchewan Inc.

Webmineral Mineralogy Database (2014). http://webmineral.com. Accessed Jan 2018.


				/s/ “Craig Funk”
Signature				Craig Funk, P. Eng., P. Geo.
				Director, GeoServices & Land
				Nutrien Ltd.

Date				February 20, 2019


DATE AND SIGNATURE PAGE		2

AUTHOR PAGE		3

TABLE OF CONTENTS		4

LIST OF FIGURES		6

LIST OF TABLES		8

1.0	SUMMARY	9

2.0	INTRODUCTION	12

3.0	RELIANCE ON OTHER EXPERTS	13

4.0	PROPERTY DESCRIPTION AND LOCATION	13

4.1	GENERAL	13

4.2	MINERAL RIGHTS	17

5.0	ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY	19

6.0	HISTORY	21

7.0	GEOLOGICAL SETTING AND MINERALIZATION	21

8.0	DEPOSIT TYPE	26

9.0	EXPLORATION	27

10.0	DRILLING	33

11.0	SAMPLING METHOD AND APPROACH	37

11.1	BASIC APPROACH	37

11.2	MEAN POTASH MINERAL GRADE FROM IN-MINE SAMPLES	40

11.3	POTASH ORE DENSITY FROM IN-MINE MINERAL GRADE MEASUREMENTS	41

12.0	DATA VERIFICATION	43

12.1	ASSAY DATA	43


12.2	EXPLORATION DATA	45

13.0	MINERAL PROCESSING AND METALLURGICAL TESTING	46

14.0	MINERAL RESOURCE ESTIMATES	46

14.1	DEFINITIONS OF MINERAL RESOURCE	46

14.2	ALLAN POTASH RESOURCE CALCULATIONS	47

15.0	MINERAL RESERVE ESTIMATES	50

15.1	DEFINITIONS OF MINERAL RESERVE	50

15.2	ALLAN POTASH RESERVE CALCULATIONS	50

16.0	MINING METHOD	53

16.1	MINING OPERATIONS	53

16.2	RISKS TO POTASH MINING OPERATIONS, WITH EMPHASIS ON WATER INFLOWS	57

17.0	RECOVERY METHODS	57

18.0	PROJECT INFRASTRUCTURE	59

19.0	MARKET STUDIES AND CONTRACTS	59

20.0	ENVIRONMENTAL STUDIES, PERMITTING, AND SOCIAL OR COMMUNITY IMPACT	64

21.0	CAPITAL AND OPERATING COSTS	65

22.0	ECONOMIC ANALYSIS	66

22.1	FUNDAMENTALS	66

22.2	TAXES	67

23.0	ADJACENT PROPERTIES	68

24.0	OTHER RELEVANT DATA AND INFORMATION	70

25.0	INTERPRETATION AND CONCLUSIONS	70

26.0	RECOMMENDATIONS	70

27.0	REFERENCES	71


Proven Mineral Reserve (millions of tonnes recoverable ore)	99
Probable Mineral Reserve (millions of tonnes recoverable ore)	250
Total Mineral Reserve (millions of tonnes recoverable ore)	349

Measured Mineral Resource - A Zone (millions of tonnes in-place)	1,006
Measured Mineral Resource - B Zone (millions of tonnes in-place)	1,506
Indicated Mineral Resource - A Zone (millions of tonnes in-place)	366
Indicated Mineral Resource - B Zone (millions of tonnes in-place)	367
Inferred Mineral Resource - A Zone (millions of tonnes in-place)	2,678
Inferred Mineral Resource - B Zone (millions of tonnes in-place)	2,691
Total Mineral Resource (millions of tonnes in-place)	8,614

Average % K₂O Grade - A Zone (from Allan in-mine samples)	24.8	%
Average % K₂O Grade - B Zone (from Lanigan in-mine samples)	20.3	%
Years of Remaining Mine Life	56


—	Latitude:	51 degrees 55 minutes 55.56 seconds North
—	Longitude:	106 degrees 04 minutes 18.84 seconds West
—	Elevation:	524.26 metres above mean sea level (SL)

—	Northing:	5,754,028.978 m
—	Easting:	426,303.225 m
—	Projection:	UTM
—	Datum:	NAD83
—	Zone:	13


Figure 1: Aerial photo of Allan surface operations, fall, 2012.			9

Figure 2: Actual finished potash products production from the Allan mine over the past 10 years (in million tonnes per year).			11

Figure 3: Map showing location of Nutrien Operations, including Allan.			14

Figure 4: Map showing Allan Potash relative to Saskatchewan potash mineralization (pink). Also shown are Company (green) and other (purple) Crown Subsurface Mineral Leases (Saskatchewan Mining and Petroleum GeoAtlas).			16

Figure 5: Map showing Allan Crown Lease KL 112R A (blue), Unit Area #1 (green), and Unit Area #2 (orange).			18

Figure 6: Map showing infrastructure (City of Saskatoon, towns, rivers, roads, and railways) near Allan Potash. Allan shaft locations are shown by red markers.			20

Figure 7: Thickness of the Prairie Evaporite Formation and area of potash distribution within these salts (from Fuzesy, 1982).			22

Figure 8: Diagrammatic vertical section showing basic layered-Earth stratigraphy in a typical Saskatchewan potash region (from Fuzesy, 1982).			23

Figure 9: Diagrammatic vertical section showing basic stratigraphy of the Prairie Evaporite Formation in the Saskatoon area (from Fuzesy, 1982).			25

Figure 10: Schematic cross-section across southern Saskatchewan of the Prairie Evaporite Formation showing relative position of potash members. At Allan, potash is mined from the Patience Lake Member, labeled “PLM” (from Fuzesy, 1982).			26

Figure 11: Potash exploration at Allan (2D & 3D surface seismic and potash drillholes).			28

Figure 12: Air photo showing the Allan surface operations and Tailings Management Area.			29

Figure 13: Seismic section from the Allan 2004 3D seismic data volume showing relative rock velocities. Vertical exaggeration is 2X. Sea level (SL) is marked in metres and major geological units are labeled.			31


Figure 14: Detail of seismic section from the Allan 3D seismic data volume (see text for explanation). Actual mine room reflection is marked in yellow. Ground surface is at approximately +500 m above Sea Level.			32

Figure 15: Stratigraphic section showing local nomenclature for potash zones and approximate position of prominent clay seams (modified from Robertson 1978).			34

Figure 16: Typical stratigraphic section correlated with composite photos covering the A Zone production interval.			35

Figure 17: Potash assay plot for PCS Allan 09-27-034-01 W3 indicating the best 3.35 m (11’) mining interval.			38

Figure 18: Histogram of potash ore grade from 6,738 Allan in-mine grade samples (data from 1968 through to end of December 2017).			40

Figure 19: Map showing Allan Mineral Resource with mine workings to December 2018.			49

Figure 20: Map showing Allan Mineral Reserve with mine workings to December 2018.			52

Figure 21: Typical stratigraphic section correlated with composite photos covering both the Patience Lake Member and the Esterhazy Member potash production intervals. At Allan, mining takes place in the Upper Patience Lake Member (A Zone).			54

Figure 22: Actual mining, production and concentration ratio for the Allan mine over the past 10 years.			56

Figure 23: Simplified flow diagram for potash flotation and crystallization milling methods used at Allan.			58

Figure 24: Allan mill recovery rate over the past 10 years.			59

Figure 25: Historical Company potash sales 2009 to 2018 in million tonnes / year (from Nutrien Financial Reporting).			61

Figure 26: Historical Company potash net sales 2009 to 2018 in million USD $ / year (from Nutrien Financial Reporting)			61

Figure 27: World potash production and demand for 2017.			62

Figure 28: World potash shipments and consumption, 2013-2018E.			63

Figure 29: Historic annual average realized potash price in USD / tonne (from Nutrien Financial Reporting).			67

Figure 30: Potash properties adjacent to Allan Potash.			69


Table 1: Potash Mineral Resources and Reserves for Allan, as of December 31, 2018.			12

Table 2: Assay results for all potash test holes within Allan Lease KL 112R A.			36

Table 3: Values for potash assay plot in Figure 17.			39

Table 4: Primary Potash Market Profile			62


Average in 3.35 m (11’) mining interval (undiluted)
Drillhole	Year Drilled	% K₂O		% Water Insolubles
04-10-033-01 W3	1954		*		*
12-32-034-02 W3	1956		28.74		5.76
16-11-033-01W3	1956		*		*
04-29-034-01 W3	1957		25.79		4.74
01-25-034-01 W3	1957		28.05		4.74
16-11-034-02 W3	1957		29.05		3.40
13-11-034-01 W3	1957		28.75		4.54
13-11-034-03 W3	1957		21.97		1.74
16-09-035-01 W3	1957		25.04		5.11
05-26-035-01 W3	1957		16.78		*
09-29-033-02 W3	1957		*		*
09-28-034-01 W3	1961		29.53		5.26
09-27-034-01 W3	1961		30.63		4.52
09-26-034-01 W3	1961		27.71		6.33
09-33-034-01 W3	1961		23.95		5.89
08-34-034-01 W3	1961		26.31		5.76
09-35-034-01 W3	1961		25.89		8.64
05-22A-034-01 W3	1961		26.47		3.19
16-14-034-01 W3	1962		26.78		5.25
01-17-034-01 W3	1962		28.63		5.29
01-12-034-01 W3	1962		*		*
14-23-034-03 W3	1969		29.56		4.18
Average (from 18 usable values):			26.65		4.96


#	From (m)	To (m)	Interval (m)	% K2O Total	% Insolubles	% Carnallite
22	1016.36	1016.63	0.27	30.61	1.70	0.00
23	1016.63	1016.72	0.09	4.12	12.29	0.00
24	1016.72	1016.84	0.12	7.51	30.77	0.00
25	1016.84	1017.24	0.40	2.83	1.10	0.69
26	1017.24	1017.76	0.52	7.33	0.68	0.34
3.35 m (11’) Mining Interval Top of Cut 1017.76 m

27	1017.76	1018.18	0.43	22.31	1.99	0.46
28	1018.18	1018.25	0.06	4.40	24.49	2.06
29	1018.25	1018.52	0.27	20.55	0.51	0.11
30	1018.52	1018.73	0.21	23.13	7.12	0.80
31	1018.73	1019.25	0.52	37.25	1.52	0.34
32	1019.25	1019.83	0.58	35.79	3.05	0.69
33	1019.83	1020.29	0.46	32.02	4.76	1.14
34	1020.29	1020.68	0.40	35.06	1.76	0.91
35	1020.68	1020.87	0.18	34.75	0.47	0.57
36	1020.87	1021.11	0.24	30.06	8.15	1.71
3.35 m (11’) Mining Interval Base of Cut 1021.11 m
37	1021.11	1021.23	0.12	14.80	7.79	2.29
38	1021.23	1021.38	0.15	2.46	20.73	1.26
39	1021.38	1021.54	0.15	0.47	28.53	0.80
40	1021.54	1021.72	0.18	2.63	11.99	1.83
3.35 m (11’) Mining Interval Weighted Average				30.63	3.43	0.75


• Na		39.34%
• Cl		60.66%
• Oxide form Na₂O		53.03%
• Mineral density		2170 kg / m³

Sylvite – KCl

• K		52.45%
• Cl		47.55%
• Oxide form K₂O		63.18%
• Mineral density		1990 kg / m³


Mining Height:		3.35 metres (11 feet)
Ore Density:		2.110 tonnes / cubic metre (A Zone)
Ore Density:		2.120 tonnes / cubic metre (B Zone)


Inferred Resource	2,678	millions of tonnes
Indicated Resource	366	millions of tonnes
Measured Resource	1,006	millions of tonnes

Total A Zone Resource	4,050	millions of tonnes


Inferred Resource	5,369	millions of tonnes
Indicated Resource	733	millions of tonnes
Measured Resource	2,512	millions of tonnes

Total A Zone + B Zone Resource	8,614	millions of tonnes


Probable Reserve		nil
Proven Reserve		nil

Total B Zone Reserve =		nil


Country/Region	Growth Rate*		Key Consuming Crops
China		8.1%	Vegetables, rice, fruits, corn
India		4.9%	Rice, wheat, vegetables, sugar crops
Other Asia		4.1%	Oil palm, rice, sugar crops, fruits, vegetables
Latin America		3.4%	Soybeans, sugar crops, corn
North America		2.1%	Corn, soybeans
*5-year CAGR for consumption (2013-2018E)