塔里木河下游土壤水分与植被时空变化特征
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新疆科技重大专项资助项目(200733144-4); 国家科技支撑课题资助项目(2006BAC01A03)


Spatio-temporal variation in soil moisture and vegetation along the lower reaches of Tarim River, China
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    摘要:

    运用变异系数、Pearson相关和回归的方法,分析了塔里木河下游2002-2006年土壤水分的时空变化和植被的分布,以及二者之间的相互关系。结果表明:土壤含水率水平空间分布随离水源地距离增加而降低,垂直分布随土层深度的增加而增加;0-60cm土壤含水率变异性最小,属中等变异性;60cm以下土壤含水量变异性增大,属强变异性;土壤含水率的时间变化受生态输水量和持续时间的制约。土壤含水率与植被的时空分布具有同步性;植被特征指数与80-280cm土壤含水率显著相关,且二者与地下水埋深均呈现极显著负相关,说明60cm以下的土壤含水率显著影响植被的生长和分布,而且地下水位是影响土壤水分和植被时空变异的主要因素。

    Abstract:

    Using the methods of coefficient of variation (CV), Pearson correlation and regression analysis, the paper analyzed the spatio-temporal variation of soil moisture, the distribution of vegetation and the relationship between them for the period 2002-2006 in the lower reaches of Tarim River. Results showed that in spatial the soil moisture of horizontal direction decreased with the distance away from water source, and that of vertical direction increased with the soil depth increasing. The soil moisture in the 0-60 cm layer had the least CV belonging to moderate variability, and that below 60 cm had the larger CV belonging to strong variability. In temporal the variability of soil moisture was restricted by both the amount and the duration of ecological water delivery. The spatio-temporal distribution of soil moisture was synchronized with that of vegetation in this area. The characteristic index of vegetation was significantly correlated to the soil moisture in the layer 80-280 cm; Meanwhile both of them had the negative correlation with (the groundwater depth significantly. It indicated that the soil moisture in the soil layer blow 60cm (affected the growth and distribution of vegetation significantly, and that groundwater table was the leading factor that determined the spatio-temporal variability of soil moisture and vegetation.

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马晓东,李卫红,朱成刚,陈亚宁*.塔里木河下游土壤水分与植被时空变化特征.生态学报,2010,30(15):4035~4045

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