Cation Exchange Capacity in Sand Rootzones
07 November 2009
Cation exchange capacity (CEC) is important because it is a measure of the nutrient holding capacity of a soil. I was reminded this week of something that turfgrass managers should know about CEC in sand rootzones. The 2009 International Annual Meetings of the Agronomy, Crops, and Soil Science Societies of America were held this week at Pittsburgh. I was co-author on a paper presented there by Dr. Quirine Ketterings of Cornell University. The paper, entitled A Simple Method for Estimating Cation Exchange Capacity Across a Wide Range of Soils, showed the results of experiments on estimating CEC on a range of fifty different soils from around New York state.
What is important to know?
- Normal soil test procedures and the CEC values that you see on your soil reports are overestimated, especially for sand rootzones
- Cation ratios or percentages based on these erroneous CEC values are meaningless
- Addition of calcium, magnesium, and potassium fertilizers should be based on the amount of that element in the soil, and not on the percentage of that element
- A nearly foolproof method of applying the right amount of nutrients to turfgrass, even without having any idea of the soil CEC, is to base the nitrogen application rate on the turfgrass growth potential (varies with turf species and temperature) and then to apply an 8:1:4 ratio of nitrogen, phosphorus, and potassium
In my research (you can download the chapter about CEC from my dissertation here) I looked at 54 sand and soil samples from around the world. Many samples were collected from golf course sites in Asia. We found that the best way to estimate CEC in sand rootzones is to use a 0.01 M solution of SrCl2 in a rapid five minute extraction. The standard soil tests such as Mehlich 3 produced an inflated value of the CEC. Because commercial soil testing laboratories do not use the SrCl2 method, the best way to estimate CEC for the average turfgrass manager is to use an equation with only two variables (soil pH and soil organic matter) to predict the CEC. Surprising, for sand rootzones, this equation predicts CEC more accurately than does a conventional soil test.
CEC (mmolc kg-1) = soil organic matter/100 * (-311 + (268 * soil pH))
If you are more comfortable in CEC units of cmolc kg-1 (or meq/100 g), then divide the soil organic matter by 1000 rather than 100 as is shown in the equation above.
Sorry I missed this paper. It looks very interesting.
Posted by: Rodney | 15 April 2010 at 22:53