Analysis on Soil Moisture Content in the Middle Reaches of the Yellow River

Q3 Environmental Science
Gao Yuan
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引用次数: 2

Abstract

In this paper,the data of soil moisture content in the middle reaches of the Yellow River during the period of 1981-2002 were analyzed to find the horizontal and vertical distribution laws. Characteristics of interannual and inter-decadal change of soil moisture content were also analyzed. The results reveal that,horizontally,soil moisture content was approximately higher in the central part than that in the southwestern and southeastern parts of the study area. Vertical distribution of soil moisture content changed seasonally. Soil moisture content was sharply decreased from early spring to May,especially in topsoil,the time when soil became the driest was earlier for 3 ten-day periods than that in soil layer of 50-100 cm,and the upper soil layer was drier than the lower one. Moisture content in topsoil was sharply increased in rainy season,and it was higher than that in lower layer. Holistically,soil moisture content was in a decrease trend,and there was a 5-6-year periodic change in the study area during the period of 1981-1996. There was an abrupt change of soil moisture content around 1991 in the central-southern part. Soil moisture content and its interannual change extent were high before 1991,and then soil became drier and the interannual change extent was lower. The change of soil moisture content was the most remarkable in the central-southern part of the study area.
黄河中游土壤水分含量分析
本文对1981—2002年黄河中游土壤含水量资料进行了分析,得出了黄河中游土壤含水量的水平和垂直分布规律。分析了土壤水分年际和年代际变化特征。结果表明,在水平方向上,研究区中部土壤含水量大致高于西南部和东南部。土壤水分垂直分布有季节变化。从早春到5月,土壤含水量急剧下降,特别是表层土壤,3个10 d期土壤最干燥时间早于50 ~ 100 cm土层,上层土壤比下层土壤更干燥。表层土壤水分含量在雨季急剧增加,且高于下层土壤。1981—1996年,研究区土壤含水量总体呈下降趋势,并存在5—6 a的周期变化。中南部土壤含水量在1991年前后发生突变。1991年以前土壤含水量高,年际变化幅度大,1991年以后土壤变干,年际变化幅度小。研究区中南部土壤含水量变化最为显著。
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来源期刊
干旱区研究
干旱区研究 Environmental Science-Water Science and Technology
CiteScore
2.50
自引率
0.00%
发文量
4294
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