Impact of Initial Planting Density on Soil Water Resource use Limit by Plants


Introduction:


Because the origin vegetation is changed into sparse vegetation or farmland, soil and water loss in Loess Plateau of China is serious and became one of the most serious regions in the world after human activity lasted for thousands of years. In order to conserve water and soil and improve ecological environment, since 1950, a largescale afforestation has been carried out on the Loess Plateau, and great progress has been made.
Rainfall is the main way to recharge soil moisture in perennial forest and grass in the most of the Loess Plateau because groundwater table is deep and water resources are scarcity and irrigation is limited. 
Soil drought is easy to appear in perennial forest and grass. Dried soil layer is the soil layer in which the soil water content is equal to or lowers than the distinguishing standard, wilt point With vegetation restoration, soil and water loss reduced but the dried soil layer (DSL) appeared and then the location DSL appeared becomes deep. The soil water environment in root zone soil is getting worse because plant consumes large amounts of water which destroy the relationship between soil water and plant growth and at the same time, the recharged soil water is limited in perennial forest and grass.
Long term cumulative desiccation of soil forms severe desiccation of soil and DSL occurs in deeper soil layer. 
The soil desiccation causes soil water mobility reduces and the soil water exchange depth weakens, which cut off soil moisture contact between the soil layers higher than the MID and that in the soil layer lower than the MID. The soil desiccation deteriorates soil water environment, slow down plant growth and speed up plant communities’ recession. The declined forest and grassland is difficult to be renewed.
Severe desiccation of soil causes soil degradation and vegetation decline, which influences the stability of forest vegetation ecosystem and national ecologic security system. Controlling soil drought is important for vegetation restoration and reconstruction of ecological environment.

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