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Potash


   About Potash

About Potash

Potash and Potash Fertilizer Potash core sample

Potash (K2O) refers to a group of potassium bearing minerals, the most common being potassium chloride (KCl). Potassium (K) is the seventh most common element in the earth’s crust, and is found in every cell of plants and animals and is essential to their growth.

Potash has been used throughout history in the manufacture of glass and soap, but is used primarily as a fertilizer, with 95 % of all potash produced being used in this way, as there is no known substitute that rivals its effectiveness in this capacity. Potash contains one of the three most important nutrients to plants, which are nitrogen, phosphorus and potassium. Potassium helps produce healthier, higher yields, and without potassium fertilizer, world production of food, feed and fiber would drop by one-third or more.

Under severe potassium deficiency, plants will often develop visible symptoms including discoloured leaves, declining quality and lack of food crop yield. Potassium is necessary for eight primary plant functions including: enzyme activation, efficient use of water, photosynthesis, transport of sugars, water and nutrient movement, protein synthesis, starch formation and crop quality.  Potassium helps to slow crop diseases, reduces water loss, and aids in cellular respiration. Nitrogen use efficiency is also improved when potassium is readily available. In food production, potassium creates crops with a better appearance, more pleasing flavour, enhanced feed value, improved harvest ability, or longer shelf life. This produces better food and better profit potential for farmers.

Potash fertilizer is often necessary to provide adequate amounts of potassium and represents the most cost effect method of increasing crop yields despite escalating prices. Commercial production of potash in the U.S. began when supplies from Germany were stopped due to military conflicts. Carlsbad, New Mexico, became the hub of American production. Other production was subsequently developed in Utah and California. In the 1960s, vast, high quality potash reserves were also discovered in Canada and as a result, Canada now supplies about three-fourths of the potash used in U.S. crop production.

Potash Production

Potash ore prior to being milled
Potash is mined from naturally occurring ore deposits which can often be covered by several thousand feet of earth. Potash bearing deposits occur in many regions of the world including The Dead Sea in Jordan and the Great Salt Lake in Utah, as well as in underground evaporate structures such as those in the Holbrook Basin in Arizona, and were created when ancient seas evaporated millions of years ago leaving minerals and compounds behind.

These evaporates are essentially made up of a mixture of sylvite and halite called sylvinite, which is the most frequently mined mineral compound due to its potassium-rich composition, with  Sylvite containing 63.2% K2O equivalent. Halite (NaCl), or sodium chloride, appears as a mass of interlocking crystals. It is transparent, colorless or sometimes has a smoky grey or brownish hue. Sylvite (KCl), potassium chloride, is similar in appearance to halite but has the characteristic of relatively greater solubility. Sylvite crystals are clear or cloudy and can vary in color from white to pink, light orange or red.

Fertilizer potash is mostly derived from these potash rocks. It requires only separation from the salt and other minerals. Potash is generally mined in two ways: conventional underground mining and solution mining.

Conventional Underground Mining

Borer Mining Machine
Most potash occurrences are too deep underground for open-cast mining and thus this type of mining is therefore called underground mining. In deep mining, the "room and pillar" method progresses along the potash seam, while pillars and timber are left standing to support the potash mine roof.

Blasting methods utilize explosives to blast and break down ore, and are most often applied in cases where potash seams are extremely variable or other limiting factors make continuous mining techniques impractical. Blasting is most effective in managing mine sites with large variances in ore thickness, and requires less initial capital and maintenance than continuous mining, though generally results in higher costs overall.
Continuous mining is used when the potash seam is sufficiently thick, stable and uniform. This allows miners to calibrate and apply continuous mining machines economically, despite their high initial cost and substantial maintenance, because they are incredibly efficient, are able to cut smoothly, provide low disturbance entry, and possess a high capacity. In addition, continuous mining allows for the use of conveyor belt ore haulage, allowing for the automation of the entire ore extraction process.

In general, two types of continuous mining machines are used: Borer miners and Drum miners. Borer miners apply uniform cutting pressure, have fixed cutting heads, and possess a higher capacity though they only cut a fixed seam thickness and width.  Drum miners have rotating cutting heads that cut sideways against the face and despite their lower capacity, are better able to adapt to changing thicknesses.

Solution Mining

In contrast, solution mining is used when underground mines are very deep, have irregular deposits, or have become flooded and

Typical layout for a potash Solution Mine
(click to enlarge)
unworkable. The  primary reasons to  utilise  solution mining is based on the thickness of mineralization, the grade of the potash bed, the depth of burial, the presence of faults, and the dip of potash beds, as an excessive dip can limit recovery.

In solution mining, heat brine, a salt water solution, is injected into the mine and circulated throughout to dissolve potash and salt from the walls. Once the compounds have dissolved, submersible pumps transport the solution to an evaporation pond, where the liquid cools and potash and salt crystals consequently settle to the bottom.

This potash is eventually collected with floating dredges and then pumped to a mill for further processing.

Worldwide Potash Production

Worldwide Production
(click to enlarge)

Currently, potash is produced in only 12 countries, while more than 150 countries utilising it. According to the International Fertilizer Industry Association, or IFA, six countries accounted for approximately 87% of the world’s aggregate potash production in 2007. During this time period, the top seven potash producers controlled approximately 83% of world production. Five of the top ten producers are further concentrated into two marketing groups, which together controlled approximately 57% of global potash production in 2007. The main producing countries include Canada, Belarus, Russia and Israel. At this time Saskatchewan, Canada, is the largest potash producing region in the world, accounting for almost a quarter of world production.  The Untied States also produces potash, about 1,200,000 tonnes a year, but consumes 5,200,000 tonnes, to make it one of the largest net importers of potash in the world.

Potash Demand

Worldwide Demand
(click to enlarge)
Worldwide, the increasing demand for potash is expected to exceed the current supply. Over the last decade, the potash industry has experienced rapid growth mostly as a result of higher demands for food, feed and fuel.

With an ever increasing world’s population, farmers are relying more than ever on potash fertilizer to maximize their yields to satisfy the associated increase in the consumption of food. This soaring global population is resulting in less and less arable land available. This means that the dwindling farm land that is available needs to be as productive as possible, and one of the only ways to achieve this is through fertilization, namely with potash. From 1962 to 2007, global consumption of potash as a fertilizer grew from approximately 10 million nutrient tons to approximately 30 million nutrient tons, according to the IFA. World consumption of potash grew at an annual rate of 2.5% since 1962, 2.7% since 1993 and 3.5% since 2000. If global potash consumption grows at an average rate of 3.5% per year from 2007 to 2011, as estimated by Fertecon, an average of 1.3 million additional tons of K2O will be required every year by potash consumers and capacity additions will be needed to meet this future demand.

In addition, rapidly expanding economies in developing nations, particularly in large countries like India and China, with growth rates of approximately 10% annually, are resulting in increased global wealth.  As a result of increased income, larger numbers of people are changing their diets to include more protein. Meat is one of the main sources of this protein which necessitates the use of potash to increase the quality and quantity of feed for livestock. While developed countries have traditionally been the largest consumers of potash, developing countries are the fastest growing markets for potash. Over the next five years, Fertecon estimates that potash fertilizer consumption will grow at an average rate of 6.0%, 4.5% and 4.5% per year in India, Brazil and China, respectively.

Lastly, the increasing demand for bio-fuels in the face of higher oil prices and carbon emissions concerns creates pressure to increase the yield of crops such as corn or sugar cane on ever decreasing agricultural lands. This requires an increased use of fertilizers which often include potash.

The current potash market is estimated at 50 million tons annually, and is projected to grow at 3-4% rate. However with the potash industry struggling to meet new demands, and with no new major projects yet announced, it seems that the gap between the demand for potash and the available supply may continue to widen.

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