clay loam

基本解释

The two-dimensional space variability of some physical properties of sandy loam and sandy clay loam in the Yellow River Delta was investigated.
本文对黄河三角洲的砂质壤土及砂质粘壤土的部分物理特性，在二维空间平面上的空间变异结构做了初步探讨。
With the temperature rising from 5℃ to 45℃ , the soil water content detected by TDR will decline in sandy loam soil, and rise in clay loam and organic soil.
当温度在5～45℃之间变化时随着温度的升高，TDR在沙壤土中测定的土壤含水量降低，而在粘壤土和有机质含量高的土壤测定的土壤含水量值升高。
Forensic analysis of the site explained significant canopy loss. Poorly drained areas with silty clay loam soils – conditions more representative of prairie environments – were widespread on the site.
对现场的取样分析解释了显著的树冠损失的原因。排水不良地区的粉质粘土壤土和具有代表性的草原环境条件都在现场广为散播。

The soil should be full of loam, a mixture of sand, silt,clay and organic material.