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水对土壤结构的稳定性是指通过比较在空气中风干的1—2毫米土壤团粒,在缓慢湿润与快速湿润后,由于土壤崩解程度不一而导致释水量多少不等所表现
The stability of water to the soil structure means that by comparing the dried 1-2 mm soil aggregates in the air, the amount of water released due to the different degrees of soil disintegration after being slowly wetted and quickly wetted