首页> 外文会议>International Soil Conservation Organization Conference vol.2; 20020526-31; Beijing(CN) >Benefits of Soil and Water Conservation and Soil Moisture of Seabuckthorn Stands in Semi-Arid Hilly Region of Loess Plateau
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Benefits of Soil and Water Conservation and Soil Moisture of Seabuckthorn Stands in Semi-Arid Hilly Region of Loess Plateau

机译:黄土高原半干旱丘陵区沙棘林分水土保持效益的研究。

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摘要

There is a remarkable function on decreasing runoff and sediment in seabuckthorn and its mixed stands. Meanwhile, the effect of seabuckthorn and its mixed stands on soil and water conservation is different with change of their structure and patterns. The utilization of seabckthorn forest to soil water is more less in spring than that in rainy season as well as there is a definite recovery of soil water in the whole soil layer in the end of growing season. The age of seabuckthorn plantation has an influence on the using intensity of soil water and the 8 years old seabuckthorn plantation should be cut because of a soil dry-layer in the stand. Location of slope has remarkable effect on soil water of seabuckthorn woodlands. Average soil moisture of 500cm depth on the down slope is higher of 1.16% than that on the upper slope. Soil water status on northern slope is better than that on eastern slope. The utilization of Seabuckthorn plantation on soil water is more than the mixed stands of seabuckthorn with other tree species. Soil moisture of seabuckthorn woodland changes largely with the zones, soil moisture of seabuckthorn woodland in the depth of 350cm is low and the growth of seabuckthorn depends on the same year's rainfall in semi-arid region. Soil water of seabuckthorn woodland maintains perennial basic balance in semi-humid region.
机译:在减少沙棘及其混交林中的径流和沉积物方面,具有显着的作用。同时,沙棘及其混交林对水土保持的影响随其结构和样式的变化而不同。春季沙棘森林对土壤水的利用比雨季少,而且在生长季节结束时,整个土壤层都有一定的土壤水回收。沙棘人工林的年龄对土壤水的利用强度有影响,由于林分中的土壤是干层,因此应砍伐8岁的沙棘人工林。坡地位置对沙棘林地土壤水分有显着影响。下坡500cm深度的平均土壤水分比上坡高1.16%。北坡土壤水分状况好于东坡。沙棘人工林在土壤水上的利用比沙棘与其他树木的混合林还多。沙棘林地土壤水分随区域变化很大,在350cm深度沙棘林地土壤水分较低,沙棘的生长取决于同年半干旱地区的降雨。沙棘林地土壤水在半湿润地区保持常年基本平衡。

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