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Characteristics of soil moisture under different vegetation coverage in Horqin Sandy Land, northern China

机译:北方科尔沁沙地不同植被覆盖下土壤水分特征

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摘要

Vegetation restoration as an effective sand fixation measure has made great achievements in China. However, soil water conditions deteriorate with the development and maturity of sand-fixing vegetation. In this study, we investigated the relationship between soil water content (SWC) and vegetation coverage (VC) at different portion (top, middle and bottom) on ten sand dunes during the growing season (April to October) in Horqin Sandy Land, northern China. We analyzed the temporal and spatial variation characteristics of SWC under different VC. The results indicate that VC and soil water storage were negatively correlated. The effect of vegetation on soil water storage on the sand dunes was greater in the dry season than the wet season. The VC and coefficient of coefficient of SWC were positively correlated at the 20 to 140 cm soil depth. As VC increased, the effect of drought stress increased at the 20 to 200 cm soil depths. The VC and SWC were negatively correlated at all the three portions of the sand dunes. According to soil water conditions and the concept of wilting humidity at different VC, we found that the suitable VC values were less than 0.46, 0.52, and 0.71 at the top, middle and bottom of the sand dunes, respectively.
机译:植被恢复作为一种有效的固沙措施在中国取得了巨大的成就。然而,随着固沙植被的发展和成熟,土壤水分状况恶化。在这项研究中,我们调查了北部科尔沁沙地生长季节(4月至10月)的10个沙丘不同部位(顶部,中部和底部)土壤水分(SWC)与植被覆盖率(VC)之间的关系。中国。我们分析了不同VC下SWC的时空变化特征。结果表明,VC与土壤储水量呈负相关。在干旱季节,植被对沙丘上土壤水分存储的影响大于潮湿季节。 VC和SWC系数在20至140 cm土层深度呈正相关。随着VC的增加,干旱胁迫的影响在20至200 cm的土壤深度增加。 VC和SWC在沙丘的所有三个部分均呈负相关。根据不同水分条件下土壤水分条件和萎humidity湿度的概念,发现沙丘顶部,中部和底部的适宜VC值分别小于0.46、0.52和0.71。

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