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Old 11-21-2013, 10:53 AM
Kiril Kiril is offline
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Join Date: Jun 2007
Location: District 9 CA
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From your link.

http://www.soil.ncsu.edu/about/century/soilacidity.html
The procedure for measuring exchangeable Al+3 is not well suited for routine soil testing procedure. For this reason a buffer solution pH 6.6 is used to measure extractable acidity (Ac) in North Carolina soils. The buffered solution extracts both exchangeable Al3+ and the pH dependent acidity (H+) which becomes ionized up to pH 6.6. The lime rate to apply is calculated with the following equation.

tons CaCO3 / acre = Ac [(desired pH - soil pH) / (6.6 - soil pH)]

The desired pH for a soil is the pH at which the activity of Al+3 is neutralized. The effect of soil organic matter in decreasing the activity of Al+3 has been taken into account by establishing desired pH for each of three classes of soils (mineral, mineral-organic and organic) based on their organic matter content. The desired pH at which exchangeable Al+3 is essentially neutralized is 6 for mineral soils, 5.5 for mineral-organic soils, and 5 for organic soils.
Furthermore, without a value for Ac the formula is worthless.
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