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#31
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1) P has always been regarded as relatively immobile in the soil. Leaching has never been a worry for water contamination with P. 2) The environmental worry about P applications are off-target apps that put P fertilizers directly in surface water (like getting fert on driveways, sidewalks, roads, and misapplications). Because P is tightly bound to the soil, the only way it can get into water after a proper application is if the soil ends up in the water. 3) K isn't volatile. Urea is volatile. Ester formulations of herbicides are volatile. Gasoline is volatile. K is not. "Volatile" simply means that a compound's vapor pressure is low and it evaporates quickly. |
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#32
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Here is a link on K that may be of some help. http://www.ianrpubs.unl.edu/epublic/...ld/ec155-3.pdf
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Barry Draycott The nation that destroys its soil destroys itself. Franklin D. Roosevelt |
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#33
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The question was whether K leaches from the soil... volatility is not the question...
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* Water/air ratio in relation to water flow to/from any plantlife is a Basic Fundamental Concept in understanding seed germination as much as transplanting a 20' Maple tree in 90 degree weather... * |
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#34
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Losses of potassium from soils are caused primarily by crop removal, fixation by clay minerals and leaching. ...leaching may be a minor factor in very sandy soils. Yes, it's an agricultural article.
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Barry Draycott The nation that destroys its soil destroys itself. Franklin D. Roosevelt |
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#35
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You are right to recognize that K is not as tightly held on cation exchange sites as P. But, soil K is a different animal. K usually hangs out in four places in soils.: 1) Unexchangeable K is held in K-bearing minerals, like micas and feldspars (90-98% of soil K). This is NOT leachable and NOT plant available. 2) Unexchangeable K can be held inisde layers of 2:1 clays (1-10% of soil K). This is NOT leachable and NOT plant available. 3) Exchangeable K can be adsorbed to soil particles on CE sites and in soil solution (1-2% of soil K). This is somewhat leachable and is totally plant available. 4) Exchangeable K can be bound in OM (<1% of soil K). A study by Jerry Sartain on sandy soils at University of FL in 1998 showed K source to be an important factor in leaching loss from turf. K2SO4 required 50 inches of water to move any K below the rootzone, while K3PO4 required 100 inches of water to move any K below the rootzone. Maximum leaching depth was 10 inches. So, K can be leached, but it doesn't move far. |
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#36
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Sorry. I used volatile meaning easily depleted. The last 13 years I read about 120 customer soil samples per year. They were from all over central Fl. These were 90% serviced lawns & 10% customers who were just starting applications. Round about average yearly. I promise less than 5 ever showed sufficient K. These customers admitted a recently applied application. Everyone else's showed almost no K available... even after 16 days testing after app of K. Just my experience. Alot of these customers used 9-2-24 religioy.
All samples were done at CLC LABS in Ohio. Posted via Mobile Device Last edited by turfmd101; 09-13-2012 at 11:55 AM. |
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#37
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To add. I'm not sure If any of these customers took samples deeper than 4" or what the root systems depths were at time of sample.
Posted via Mobile Device |
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#38
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Solution P is an anion. It is incorrect to speak of P being bound by the CEC.
Further, P can and does leach. A review of available published literature on P mobility in soils will reveal this. |
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#39
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1) In acidic soils, mineral surfaces have a net positive charge (both + and - exist, but the +s outnumber the -s), so some phosphate ions are adsorbed electrochemically. 2) Phosphate ions don't exist as free H2PO4- and HPO4-- very long. They react very quickly and readily with Fe, Al, Mn, and Ca ions on CE sites and in solution. In acidic soils, Fe and Al are the main bonds. B/c the Al-O-P and Fe-O-P bonds are very strong, desorption is very difficult. 3) In alkaline soils, Ca and Mn bond more readily than Fe or Al and sequester phosphates on cations attached to CE sites. So, while phosphates don't directly adsorb to CE sites, they bond with cations that are directly adsorb to CE sites and they adsorb to AE sites. |
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#40
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CEC = cation exchange complex ... not anion exchange complex. Errr Skip, when P become fixed to select cations it precipitates out of solution as a compound with variable solubility ... some of which may become part of the active pool, some part of the fixed pool. This has nothing to do with the CEC. |
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