Potassium in Plants
Potassium is essential in nearly all processes needed to sustain plant growth and reproduction. Plants deficient in potassium are less resistant to drought, excess water, and high and low temperatures. They are also less resistant to pests, diseases and nematode attacks. Because potassium improves the overall health of growing plants and helps them fight against disease, it is known as the “quality” nutrient. Potassium affects quality factors such as size, shape, color and vigor of the seed or grain, and improves the fiber quality of cotton.
Potassium increases crop yields because it:
Increases root growth and improves drought tolerance
Builds cellulose and reduces lodging
Activates at least 60 enzymes involved in growth
Aids in photosynthesis and food formation
Helps translocate sugars and starches
Produces grains rich in starch
Increases protein content of plants
Maintains turgor, reduces water loss and wilting
Helps retard the spread of crop diseases and nematodes.
Potassium Uptake by Crops
Time of potassium uptake varies with different plants. However, plants generally absorb the majority of their potassium at an earlier growth stage than they do nitrogen and phosphorus.
Experiments on potassium uptake by corn showed that 70 to 80 percent was absorbed by silking time, and 100 percent was absorbed three to four weeks after silking. Translocation of potassium from the leaves and stems to the grain was much less than for phosphorus and nitrogen. The period during grain formation is apparently not a critical one for supply of potassium.
Note: Potassium content of fertilizers is expressed as K₂O, although there is no such compound in fertilizers, nor is it absorbed by or found in the plant in that form. Soil and plant tissue analysis values are usually expressed in terms of percent potassium (K), but fertilizer recommendations are expressed as K₂O. To convert from K to K₂O, multiply K by 1.2. To convert from K₂O to K, multiply K₂O by a factor of 0.83.
Potassium Removal by Crops
Nutrient uptake or utilization is an important consideration, but crops take up far more potassium than they remove with the harvested portion. For example, a 200 bu/acre corn crop takes up or utilizes about 266 lb/acre of potash. But when the corn is harvested as grain, only 0.25 lb/bu is removed, or 50 lb/acre K₂O is harvested and removed from the field. However, if the crop were harvested as silage, then 7.3 lb/ton K₂O are vested and removed from the field. Therefore, a 32-ton/acre silage crop would remove 234 lb/acre K₂O. Harvest management is the major consideration in developing a potash fertilization program. Crops harvested in which the whole plant is removed from the field, like alfalfa hay, must have more potash applied than crops where only grain, lint or fruit are removed. Often with hay and silage crops, removal is an excellent guide for planning the potash fertilization program. With other crops, such as grain, soil tests offer the best guide.
Potassium Deficiency Symptoms
Potassium is a highly mobile element in the plant and is translocated from the older to younger tissue. Consequently, potassium deficiency symptoms usually occur first on the lower leaves of the plant, and progress toward the top as the severity of the deficiency increases. One of the most common signs of potassium deficiency is the yellow scorching, or firing (chlorosis), along the leaf margin. In severe cases, the fired margin of the leaf may fall out. However, with broadleaf crops, such as soybeans and cotton, the entire leaf may shed, resulting in premature defoliation of the crop.
Potassium-deficient crops grow slowly and have poorly developed root systems. Stalks are weak, and lodging of cereal crops such as corn and small grain is common. Legumes are not strong competitors for soil potassium and are often crowded out by grasses in a grass-legume pasture. When potassium is not sufficient, winter killing of perennial crops such as alfalfa and grasses can occur.
For more information on potassium deficiency, click here.
Symptoms in Corn
Firing or scorching appears on outer edge of leaf while midrib remains green. May be some yellow striping on lower leaves. (Sorghum and most grasses also react this way.) Poor root development, defective nodal tissues, unfilled, chaffy ears, and stalk lodging are other symptoms in corn.
Symptoms in Soybeans
Firing or scorching begins on outer edge of leaf. When leaf tissue dies, leaf edges become broken and ragged/delayed maturity and slow defoliation/shriveled and less uniform beans, many worthless.
Symptoms in Alfalfa
With classical symptoms (shown at top right), first signs of K deficiency are small white or yellowish dots around outer edges of leaves. Then edges turn yellow and tissue dies and becomes brown and dry. However, for alfalfa grown on soils high in sodium (Na), the K deficiency symptoms have a different appearance, as indicated in the photo at left.
Symptoms in Cotton
Cotton “rust” – first a yellowish or bronze mottling in the leaf. Leaf turns yellowish green, brown specks at tip around margin and between veins. As breakdown progresses, whole leaf becomes reddish brown, dies, sheds prematurely. Short plants with fewer, smaller bolls or short, weak fibers. In the past, K deficiency symptoms have been described as occurring on older, mature leaves at the bottom of the plant. In recent years, symptoms have been observed at the top on young leaves of some heavily fruited cotton varieties.
Symptoms in Wheat
Frequently, no outstanding hunger signs on leaf itself (no discoloration, scorching, or mottling), but sharp difference in plant size and number, length, and condition of roots. Lodging tendency. Smaller kernels. In advanced stages, withering or burn of leaf tips and margins, beginning with older leaves.
Symptoms in Potatoes
Upper leaves, usually smaller, crinkled and darker green than normal with small necrotic patches. Middle to lower leaves show marginal scorch and yellowing. Early indicator: dark green, crinkled leaves, though varieties differ in normal leaf color and texture.
Symptoms in Canola
Potassium deficiency reduces growth, resulting in smaller leaves and thinner stems. Plants are more easily lodged and may wilt. Under severe deficiency, the edges of older leaves become yellow, or scorched and may die completely, but remain attached to the stem.
Symptoms in Rice
Rice deficient in K may show symptoms as stunted plants, a slight reduction in tillering, and short, droopy, dark green upper leaves. Yellowing may appear in interveinal areas of lower leaves, starting from the top and eventually drying to a light brown. Long thin panicles and black, deteriorated roots may be related to K deficiency.
Symptoms in Apples
Yellowish green leaves curl upward along entire leaf…scorched areas develop along edges that become ragged. Undersized and poorly colored fruit may drop prematurely. Poor storage, shipping and canning qualities in fruit.
Symptoms in Sugarbeets
The first sign of K deficiency appears as tanning and leathering of the edges of recently matured leaves. When the soil solution is very low in Na, a severe interveinal leaf scorch and crinkling proceeds to the midrib. Under high Na conditions, tanning and leaf scorch lead to a smooth leaf surface.
All photos are provided courtesy of The Fertilizer Institute (TFI) and its TFI Crop Nutrient Deficiency Image Collection. The photos above are a sample of a greater collection, which provides a comprehensive sampling of hundreds of classic cases of crop deficiency from research plots and farm fields located around the world. For access to the full collection, you can visit TFI’s website.
Potassium in Soil
Relatively Unavailable Potassium
From 90 to 98 percent of the total potassium present in soils is found in insoluble primary minerals that are resistant to chemical breakdown. They release potassium slowly, but in small quantities compared to total needs of growing crops.
Slowly Available Potassium
This form makes up 1–10 percent of the total potassium supply, and may originate from dissolved primary minerals or from potassium fertilizers. This potassium is attracted to the surface of clay minerals, where it may be firmly bound or fixed between the clay layers in a form slowly available to plants. The actual amount available depends on the type and amount of clay present.
Readily Available Potassium
Readily available forms of potassium make up only 0.1 to 2 percent of the total potassium in the soil, and consist of potassium dissolved in the soil solution and held on the exchange positions of the clay and organic matter. This potassium is “exchangeable” because it can be replaced by other positively charged ions (cations) such as hydrogen, calcium and magnesium. This exchange happens rapidly and frequently. The potassium in the soil solution may be taken up by the plant or lost from the soil by leaching, especially on sandy, coarse-textured soils.
Potassium and Balanced Crop Nutrition
Adequate supplies of other plant nutrients are required to obtain maximum responses to potassium fertilizer; however, there are several unique relations between potassium and other nutrients.
High-potassium fertilization can decrease the availability of magnesium to the plant, and may result in magnesium deficiency of crops grown on soils that are already low in magnesium. This problem is often encountered with crops grown on sandy soils, particularly in the coastal plain soils of the southern United States. Conversely, crops grown on soils high in magnesium can suffer potassium deficiency, especially if the soils are high phosphorus and low in potassium. This problem is especially severe in the soils of the Mississippi River flood plain.
Leaching of potassium in acidic, sandy soils may be reduced by liming the soil to a pH of 6.2 to 6.5; however, applications of high rates of limestone to a soil low in potassium may induce potassium deficiency of crops growing on those soils. This problem occurs more on soils with predominantly 2:1 type clays (such as montmorillonite clays) rather than the 1:1 type (such as kaolinitic clays).
Percent of soil samples that tested below critical levels for K for major crops in 2010. Source: TFI
Elemental potassium (K) is not found in a pure state in nature because of its high reactivity. It can be purified, but must be kept in oil to retain its purity and prevent violent reactivity. Potash deposits occur as beds of solid salts beneath the earth’s surface and brines in dying lakes and seas.
Placement of Potassium Fertilizers
The common potassium fertilizers are completely water soluble and, in some cases, have a high salt index. Consequently, when placed too close to seed or transplants, they can decrease seed germination and plant survival. This fertilizer injury is most severe on sandy soils, under dry conditions and with high fertilizer rates — especially nitrogen and potassium. Some crops such as soybeans, cotton and peanuts are much more sensitive to fertilizer injury than corn. Placement of the fertilizer in a band approximately 3 inches to the side and 2 inches below the seed is an effective method of preventing fertilizer injury. Band placement of potassium fertilizer is generally more efficient than broadcast application when the rate of application is low or soil levels of potassium are low.
Broadcast application of potassium under minimum tillage results in much of the applied potassium remaining in the top 1 to 2 inches of the soil; whereas, with conventional tillage, it is distributed throughout the plow layer. Corn usually absorbs sufficient potassium under no-till due to its extensive root system in the surface layer of the soil. Leaf analysis of corn shows lower potassium content under minimum tillage than with conventional tillage due to either the location of the applied potassium or to poorer aeration. Sufficient potassium can be supplied by using a higher rate of potassium fertilization with no-till systems.
Adapted from “The Efficient Fertilizer Use Manual”,
Potassium chapter by Dr. Bob Thompson
Potassium is required for plant growth and reproduction. Potash is defined as K₂0 and is used to express the content of various fertilizer materials containing K.
Potassium for crop production
Potassium (K) is an essential nutrient for plant growth. It’s classified as a macronutrient because plants take up large quantities of K during their life cycle.
Minnesota soils can supply some K for crop production, but when the supply from the soil isn’t adequate, a fertilizer program must supply the K.
Here, we’ll give you a basic understanding of K, including plants’ K nutrition, how it reacts in soils, its function in plants and its role in efficient crop production. In addition, you’ll find information about soil tests, K sources, predicting potash needs and effectively applying K to your fields.
Role in plant growth
Potassium is associated with the movement of water, nutrients and carbohydrates in plant tissue. It’s involved with enzyme activation within the plant, which affects protein, starch and adenosine triphosphate (ATP) production. The production of ATP can regulate the rate of photosynthesis.
Potassium also helps regulate the opening and closing of the stomata, which regulates the exchange of water vapor, oxygen and carbon dioxide. If K is deficient or not supplied in adequate amounts, it stunts plant growth and reduces yield.
For perennial crops such as alfalfa, potassium plays a role in stand persistence through the winter. Other roles of K include:
Increases root growth and improves drought resistance.
Maintains turgor; reduces water loss and wilting.
Aids in photosynthesis and food formation.
Reduces respiration, preventing energy losses.
Enhances translocation of sugars and starch.
Produces grain rich in starch.
Increases plants’ protein content.
Builds cellulose and reduces lodging.
Helps retard crop diseases.
Potassium in soils
The total K content of soils frequently exceeds 20,000 ppm (parts per million). While the supply of total K in soils is quite large, relatively small amounts are available for plant growth at any one time. That’s because nearly all of this K is in the structural component of soil minerals and isn’t available for plant growth.
The amount of K supplied by soils varies due to large differences in soil parent materials and the effect weathering has on these materials. Therefore, the need for K in a fertilizer program varies across the United States.
Three forms of K – unavailable, slowly available or fixed and readily available or exchangeable – exist in an equilibrium in the soil system. Below, we describe these forms and their relationship to one another. Figure 1 also illustrates the general relationship among these forms.
Guide to potassium for Minnesota crops, including fruits and vegetables: Covers potassium basics, predicting potash needs, soil tests, K sources and fertilizer application recommendations.