(b).
Texture‡ | AD | F3P | F4P | ML | ONL | ORL | S | VG | VGM | W | SELF | Sum |
---|---|---|---|---|---|---|---|---|---|---|---|---|
TS | 2§ | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 |
LS | 0 | 1 | 2§ | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 |
SL | 9§ | 2 | 1 | 0 | 1 | 2 | 5 | 0 | 0 | 0 | 0 | 20 |
HL | 74§ | 1 | 16 | 10 | 22 | 7 | 45 | 0 | 3 | 23 | 6 | 207 |
ML | 53§ | 7 | 9 | 4 | 6 | 15 | 14 | 0 | 1 | 13 | 1 | 123 |
LL | 21§ | 4 | 7 | 1 | 0 | 5 | 4 | 1 | 0 | 4 | 0 | 47 |
HC | 40§ | 7 | 14 | 0 | 0 | 0 | 12 | 0 | 0 | 7 | 11 | 91 |
MC | 90§ | 1 | 37 | 2 | 9 | 7 | 44 | 0 | 0 | 30 | 9 | 229 |
LC | 143§ | 5 | 39 | 0 | 39 | 3 | 85 | 1 | 4 | 39 | 8 | 366 |
| ||||||||||||
Sum | 432§ | 29 | 126 | 17 | 77 | 39 | 209 | 2 | 8 | 116 | 35 | 1090 |
†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.
‡Textural classes of Katschinski system: TS = tight sand, LS = loose sand, SL = sandy loam, HL = heavy loam, ML = moderate loam, LL = light loam, HC = heavy clay, MC = moderate clay, and LC = light clay.
§The biggest number of cases as the best model for the specific soil texture class.