Aggregate Stability and Size Distribution

W. D. Kemper, R. Rosenau
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引用次数: 1809

Abstract

An aggregate is a group of primary particles that cohere to each other more strongly than to other surrounding soil particles. Most adjacent particles adhere to some degree. Therefore, disintegration of the soil mass into aggregates requires imposition of a disrupting force. Stability of aggregates is a function of whether the cohesive forces between particles withstand the applied disruptive force.
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骨料稳定性和粒度分布
团聚体是一组基本颗粒,它们之间的结合力比与周围土壤颗粒之间的结合力更强。大多数相邻的粒子都有一定程度的粘附。因此,土质分解成团聚体需要施加破坏力。聚集体的稳定性是粒子之间的凝聚力能否承受施加的破坏力的函数。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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Nitrogen-Inorganic Forms Kaolin and Serpentine Group Minerals Chemistry of Redox Processes in Soils Intake Rate: Sprinkler Infiltrometer 3.6.1.1 Laboratory
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