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Concept of Soil Water Movement in Relation to Variable Water Potential

机译:与水势变化有关的土壤水分运动概念

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Soil water potential is the main driving force which causes the soil water to move from one point to other point in the soil depending upon it’s energy state. The total energy state of soil water is defined by its equivalent potential energy, as determined by the various forces acting on the water per unit quantity. In general, flow rates of water in soils is too small to consider kinetic energy. Therefore, the energy state of soil water is defined by its equivalent potential energy, that is by virtue of its position in a force field and which further has a scope to manage irrigation. Usually, farmers mostly apply flood irrigation but after properly monitoring soil water potential with the help of tensiometer helps us to save a significant amount of water. Thus, a proper understanding of soil water potential, it’s components and their relation with the soil water movement is a must for every soil scientist, agronomist and hydrologist for implementing effective plans towards the judicious use of water.
机译:土壤水势是导致土壤水根据其能量状态从一个点移动到另一点的主要驱动力。土壤水的总能量状态由其等效势能定义,等效势能由单位量作用于水的各种力确定。通常,土壤中水的流速太小,无法考虑动能。因此,土壤水的能量状态由其等效势能定义,即通过其在力场中的位置来定义,并且还具有管理灌溉的范围。通常,农民大多进行洪水灌溉,但在使用张力计适当监测土壤水势后,可以帮助我们节省大量水。因此,对土壤水势,水的组成及其与土壤水运动的关系的正确理解是每位土壤科学家,农艺师和水文学家都必须执行明智计划的明智计划。

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