
06/12/07, 03:18 PM
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Fair to adequate Mod
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Join Date: May 2002
Location: Between Crosslake and Emily Minnesota
Posts: 13,724
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I think your article will, at a minimum, get people to think about pH. Most people focus on fertilizers and do not understand how soil pH can influence the availability of nutrients. Ken is correct in stating that soil pH should not be used as an index of soil fertility. For instance, a soil may have sufficient to excessive levels of iron, but at high pH the iron is immobile (“tied-up”) and the plant may be starving for this nutrient.
I would recommend that your article describe exactly what form of lime it is discussing. You use the generic term “lime.” Lime can be “quick lime,” “hydrated lime,” or “ag lime.” I assume your article is referring to ag lime....which can be crushed, pulverized or granulated (pelled) calcitic lime or dolomitic lime.
Secondly I would recommend a bit more discussion in taking a good sample for analysis. The article talks about mixing sub-samples from three locations into one composite sample for analysis....and then doing it over from different sites in the yard (ie, west yard, south garden, etc.) It would be better be take samples from more locations....maybe 10 or 12....and mix for each “site” sample.
Adding too much ag lime will not make the soil “toxic” as the article implies. The pH of 100% ag lime is only 8, consequently it will not increase the soil pH above 8 no matter how much ag lime is applied.
I realize that the article is written for the average homeowner, so simplicity of the application rate table is adequate. However, just so you know, the amount of ag lime to apply to a given soil is more related to the soils buffering capacity than to it’s actual pH value. In other words, two soils can have identical pH, one soil has a low buffering capacity and the other a high buffering capacity. The soil with the high buffering capacity would require more ag lime to raise the soil pH than the one with low buffering capacity. You touched on this concept when you contrasted a sandy soil to a clayey one. But buffering capacity is determine by other properties in addition to texture.
You might want to consider adding a bit more explanation to the Colorado State University table. I use this exact table in some of the teaching that I have done.
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