黄土高原水蚀风蚀交错带不同土地利用方式坡面土壤水分特性研究


Autoria(s): 白一茹; 邵明安
Data(s)

2009

Resumo

为分析不同土地利用方式下坡面土壤水分特性的差异和规律,对黄土高原水蚀风蚀交错带典型坡面上农地、林地和草地的土壤水分特性进行了分析。结果表明:(1)苜蓿地土壤的持水能力和供水能力最强,其次是杏树林和长芒草地,谷子地最差;(2)通过土壤水分有效性分析发现,水蚀风蚀交错带田间持水量相当于-0.2×105Pa土壤基质势时的土壤含水量,永久凋萎点则低于-2.0×106Pa土壤基质势对应的土壤含水量;(3)苜蓿地有效水含量最高,谷子地有效水含量最低,而且苜蓿地土壤有效水含量的提高主要是提高了迟效水部分;(4)对不同土地利用方式下的土壤比水容量变化曲线研究表明,土壤比水容量在田间持水量附近随土壤含水量的降低减小的很快,而当土壤水分降低到田间持水量的50%~60%以下时,土壤比水容量基本不变。

Different land use has an important effect on soil moisture and soil quality.In order to describe the differences and features of soil water characteristics on a slope-land under different land uses,a research on soil water characteristics of farmland,woodland and grassland was carried out in the Wind-water Erosion Crisscross region.The results showed that:(1) the capacity of soil water retention and supply of alfalfas was the best,then almonds,and then stipa bungeana,and the capacity of millets was the wor...

Identificador

http://ir.iswc.ac.cn/handle/361005/462

http://www.irgrid.ac.cn/handle/1471x/86082

Idioma(s)

中文

Fonte

白一茹, 邵明安.黄土高原水蚀风蚀交错带不同土地利用方式坡面土壤水分特性研究.干旱地区农业研究,2009,1:122-129

Tipo

期刊论文