Research Article

Particle-Size Distribution Models for the Conversion of Chinese Data to FAO/USDA System

Table 3

Number of cases as the best model with the smallest AIC value for each soil textural class in T1 schemes .

Texture ADF3PF4PMLONLORLSVGVGMWSELFSum

Sa643317903273 004547320
LoSa163 395346337153007854626
Lo799 163241703800136471377
SaLo979 5655362235589041893122277
SaClLo464 255623712229023197946
SiClLo244 221601419610270511
SiLo137 9040179500240286
ClLo1929 31062972102402801103319
SaCl108 416301360076181
SiCl23616155218264 30390634
LCl2086 3334138166134601971153917
HCl385 10213912333500477868

Sum7594 29425744546397472041070079515262

For example, if the best model according to AIC value of a soil sample is the AD model, the number of the AD model in the table will increase by one. If a model has a big number in a soil textural class, it has advantages in fitting the PSD curve compared to models with small number. The compared eleven models are AD = Anderson model, F3P = Fredlund3P model, F4P = Fredlund4P model, ML = modified logistic growth model, ONL = offset-nonrenormalized lognormal model, ORL = offset-renormalized lognormal model, S = Skaggs model, VG = van Genuchten type model, VGM = van Genuchten type modified model, W = Weibull model, and SELF = self-similar model.
Textural classes of ISSS system: Sa = sand, LoSa = loamy sand, Lo = loam, SaLo = sandy loam, SaClLo = sandy clay loam, SiClLo = silty clay loam, SiLo = silt loam, ClLo = clay loam, SaCl = sandy clay, SiCl = silty clay, LCl = light clay, and HCl = heavy clay.
The biggest number of cases as the best model for the specific soil texture class.