摘 要：
玛曲位于青藏高原东缘,是黄河重要的水源涵养区,也是生态脆弱地区,研究土壤湿度动态变化及其影响因素,对青藏高原区水资源、生态安全保障具有重要的现实意义。利用温度植被干旱指数法(TVDI)反演玛曲2000—2015年土壤湿度,分析土壤湿度空间分布和时间变化特征,并采用多元线性回归模型探讨了影响土壤湿度的关键要素。研究表明:1) 2000—2015年玛曲地区土壤湿度整体呈现下降趋势,呈旱化的现象,土壤湿度的空间分异特征和季节变化规律显著。其中:土壤湿度空间分布格局为从西北向东南逐渐减少,总体干湿等级以正常为主(0. 5
译 名：
Spatio-temporal variation of soil moisture and analysis on its influencing factors in Maqu county based on TVDI
作 者：
WANG Meilin;JIANG Qun'ou;SHAO Yaqi;SUN Siyang;School of Soil and Water Conservation,Beijing Forestry University;State Key Laboratory of Soil and Water Conservation and Desertification Combating,Ministry of Education,Beijing Forestry University;Research Center of Agricultural Policy,Institute of Geographic Sciences and Natural Resources Research,Chinese Academy of Sciences;
关键词：
soil moisture;;temperature vegetation drought index(TVDI);;influencing factors;;Maqu county
摘 要：
[Background] Maqu is a significant water conservation area of the Yellow River and an ecologically fragile area,which is located on the eastern edge of the Qinghai-Tibet Plateau. Studying the dynamic changes of soil moisture and its influencing factors have important practical significance for water resources and ecological security in the Qinghai-Tibet Plateau. [Methods] In this study, the temperature vegetation drought index(TVDI) method was used to invert the soil moisture of Maqu county from 2000 to 2015,then the spatial distribution and temporal variation characteristics of soil moisture were analyzed,and finally the correlation analysis and multiple linear regression models were applied to explore the key factors affecting soil moisture. [Results] 1) The soil moisture in the Maqu area from2000 to 2015 showed a downward trend as a whole,with signs of drought,and the spatial differentiation characteristics and seasonal variation of soil moisture were significant. Among them, the spatial distribution pattern of soil moisture gradually decreased from northwest to southeast,and the overall dry and wet grade was dominated by normal(0. 5 < TVDI≤0. 6). On the seasonal scale,the surface soil moisture in the spring gradually decreased with the passage of time,tending to become dry. In summer,the soil moisture in the surface layer was large and stable,which was directly related to the recharge of summer precipitation. Due to the decrease of winter precipitation,the overall soil moisture in winter was the lowest and continued to decline,and further led to the reduction of spring ice and snow melt water. 2)The spatial pattern and change of soil moisture were formed by a combination of several influencing factors. Among them, net primary productivity, annual precipitation, elevation, slope and GDP demonstrated significant positive effects on soil moisture, while annual average temperature and population presented significant negative effects on soil moisture. [Conclusions] Therefore, it is necessary to control the population growth,increase vegetation coverage,actively respond to climate changes to reduce the adverse effects of temperature on soil moisture and so on,so that the soil moisture of the surface of Maqu is maintained in a fine condition,providing a certain guarantee for the runoff of the Yellow River. These research results will provide important reference information for water resources and ecological environment research in the Yellow River source area.
