摘要
对黄土高原沟壑区不同种植年限果园土壤深层水分变化进行了研究。结果表明,受降水影响0-2m土层水分变化较大,且0-40 cm、40-80 cm、80-200 cm三个土层土壤含水量之间的差异达到极显著水平;2m以下由于没有水分的补给,土壤水分含量趋于稳定,出现了干燥现象。随着种植年限的增加,深层土壤的干燥化现象有增加趋势。
Change of soil moisture in deep layer was studied in different planting-life in gully region of loess plateau. The results showed that, affected by precipitation, the soil moisture had great change in 0-2 m soil layer, and there was a significant difference among 0-40 cm, 40-80 cm and 80-200 cm. Without water supply, soil moisture tended to be stable under 2 m soil layer which appeared desiccation. With the planting-life increasing, desiccation of deep soil layer tended to increase.
出处
《西北农业学报》
CSCD
北大核心
2008年第4期229-233,共5页
Acta Agriculturae Boreali-occidentalis Sinica
基金
中科院农业项目(kscx1-yw-N-15-04)
国家科技支撑计划(2006BAD09B10)
关键词
黄土高原
果园
水分变化
Loess plateau
Orchard
Moisture changes