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Chapter 5 in Lecture Manual
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K fixation
the process of reducing plant available K by trapping soil K+ between 2 clay units
K form in nature and use by plants
Plant available = K+
K+ exists in plants as free K+ (not chemically bound in plant)
Used for the activation of 60 enzymes, cell energetic,metabolism, and water movement in cells
K movement in soil
Mainly diffusion, some root interception
K+ adsorbs onto clay and Organic matter surfaces and gets fixed between clay mineral units
What factors affect soil K availability to plants?
Clay Quantity: soil K retention increases as clay quantity increases, solution K (available to plants) increases as CEC increases
Clay minerals: Mica and feldspar weather and release K+, Illite and Vermiculite fix K and lower plant availability
Tillage influences: K diffusion is slow in cold, dry soils. Conventional tillage heats soil faster, strip till is a good balance between conventional and no-till
Minerals and their availability mechanisms that influence soil K availability
Mica and Feldspar chemically weather and release K+ and increase available K levels
Illite: 2:1 non-expanding clay
Vermiculite: 2:1 expanding clay
Both fix K and lower soil K availability. Expanding clay traps K ions as it shrinks and swells.
Issues regarding tillage practices which influence soil K availability
Conventional: heats topsoil faster, encourages higher K diffusion rates sooner, dries soil out a bit
No-till: keeps soil covered and cooler, much slower K diffusion rate
Strip-till: good balance between the two
Popular fertilizer K sources and forms
Soluble chemical form: K+, fertilizer analysis expressed as K2O
Potash (0-0-60) - most popular, chemical formula is KCl dry material, is made from processed rock KCl
KCl Solution (liquid, 0-0-15) -is potash dissolved in water
Effective practices that enhance K availability to crops
Always use soil test results to formulate recommendations
Most common is to broadcast apply and incorporate with tillage
Safer option is to apply 2×2 starter bands to prevent high salt concentrations damage
No-till fields apply in strip till bands for wide row grain crops
chemical changes that influence exchangeable K
Changes in CEC and soil pH affect how tightly K+ is held by clay and OM. Faster processes.
chemical changes that influence fixed K
Clay tightly holds K+ through shrinking/swelling cycles. K+ ions are released when primary minerals are weathered. Slow process.