[1]穆兴民,陈国良,郭宝安,等.宁南黄土丘陵区荒坡地土壤水分分布与运行特征[J].水土保持研究,1992,(02):72-79.
　Mu Xingmin,Chen Guoliang,Guo Baoan,et al.ANALYSIS OF THE SOIL WATER DISTRIBUTION AND MOVING CHARACTERISTICS ON THE PASTURING SLOPE LAND IN SOUTHERN NINGXIA LOESS HILLY REGION[J].Research of Soil and Water Conservation,1992,(02):72-79.
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宁南黄土丘陵区荒坡地土壤水分分布与运行特征

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 期数: 1992年02期 页码: 72-79 栏目: 出版日期: 1900-01-01
Title:
ANALYSIS OF THE SOIL WATER DISTRIBUTION AND MOVING CHARACTERISTICS ON THE PASTURING SLOPE LAND IN SOUTHERN NINGXIA LOESS HILLY REGION
作者:
穆兴民1, 陈国良1, 郭宝安1, 赵克学2
1. 中国科学院水利部西北水土保持研究所 陕西杨陵 712100;
2. 宁夏回族自治区固原县科委
Author(s):
Mu Xingmin1, Chen Guoliang1, Guo Baoan1, Zhao Kexue2
Northwestern Institute of Soil and Water Conservation, Academia Sinica and Minstry of Water Resources, Yangling, Shaanxi, 712100
关键词:
宁南黄土丘陵区; 土壤水分分布; 运行特征
Keywords:
southern Ningxia Loess Hilly Region; soil water distribution; moving characteristics
摘要:
用土钻法连续5年对荒坡地不同坡向、坡位的土壤水分进行了定位测定，表明不同坡向土壤水分差异显著，南坡和北坡相比，0～2m土层北坡含水量高，但1～2m土层南坡比北坡土壤含水量高。荒坡地耗水深度南坡2.3m，北坡1.3m。坡地蒸散平均305～335mm，其中90%来自大气降水。
Abstract:
This paper has studied the soil moisture content of the slope land (for the different direction slopes, the different site of the slope).The data has been gotten by the soil auger method at the same pinpoint for 5 years (1985-1989).The soil moisture content of the different slopes are obvious difference.The soil moisture content of northern slope is more than the southern slope’s in the 0-20cm soil layer.but the northern slope’s is less than the southern slope’s in the 100-200cm layer.The main depth of the consumed soil water is 2.3m at the southern slope and about 1.7m at the northern slope.The mean evaporation in the slope land are about 305-335mm, the ninety percent of the sum evaporation comes from rainfall.

参考文献/References:

1 E H 罗曼诺娃[苏].基本气候要素的小气候变化.北京:科学出版社,1981
2 么枕生主编.黄土高原小气候.北京:科学出版社,1959
3 傅抱璞著.山地气候.北京:科学出版社,1983

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备注/Memo

收稿日期:1992-5-30

更新日期/Last Update: 1900-01-01