作者: A. Alaoui , J. Lipiec , H.H. Gerke
DOI: 10.1016/J.STILL.2011.06.002
关键词:
摘要: Compaction and shearing, as well as the rearrangement of soil aggregates and clods due to shrinkage, among other processes, can strongly affect the pore geometry of agricultural soils. These soil structural changes directly affect soil water movement by altering the hydraulic properties that are commonly described by the soil water retention curve (WRC) and the unsaturated hydraulic conductivity function (HCF). This review focuses on recent advances in the understanding and evaluation of changes in hydraulic functions in relation …