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The most common commercial form of potash is potassium chloride, also called muriate of potash or MOP. Other forms include potassium sulfate and potassium-magnesium sulfate. Fertilizer products are often labeled using the N-P-K system, in which potassium is represented by the letter K.
Most commercial potash comes from mineral deposits formed when ancient seas and saltwater basins evaporated. Today, it is obtained through conventional underground mining or solution mining. In solution mining, water is injected into underground deposits to dissolve potassium salts, and the resulting brine is pumped to the surface for processing.
Approximately 95 percent of potash consumption is associated with fertilizer production. By improving potassium availability, potash can help crops manage water, develop stronger structures, and tolerate drought or other stresses. However, fertilizer should be applied according to soil conditions and crop requirements, because excessive or poorly timed use can waste resources and increase environmental risks.
Potash is therefore an important mineral resource linking geology, agriculture, food production, and global trade.
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