Research Article

Spatial Distribution and Evolution of pH as a Function of Cation Exchange Capacity, Sum of Exchangeable Bases, and Organic Matter and Aluminum in the Soils of Foumban

Table 1

Summary statistics of the original Foumban soil variables.

StatsNumber of valuesMinimumMaximumRangeMeanStandard deviationCoefficient of variationSkewKurtosis

%S9023.5075.0051.5052.9911.830.22−0.32−0.43
%L905.5037.5732.0718.506.380.341.020.57
%A909.5061.5052.0028.6411.050.390.660.40
pH903.806.402.605.010.580.120.14−0.51
OM (%)900.6211.0910.465.212.170.420.220.11
SBE (méq/100 g)900.5731.8731.3010.655.890.551.281.86
CEC (méq/100 g)902.4639.6837.2220.456.840.330.281.16
(Ca + Mg)/K900.371079.391079.0257.91159.512.755.3629.31

%S: percentage of sands; %A: percentage of clays; %L: percentage of silts; SBE: sum of exchangeable bases. CEC: cation exchange capacity; Ca: calcium; Mg: magnesium; K: potassium; OM: organic matter.