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江南红黄壤丘陵区土壤湿度模拟和季节性干旱的研究 被引量:5

SIMULATION OF SOIL MOISTURE AND STUDY ON SEASONAL SOIL SOIL DROUGHT IN THE RED-YELLOW SOIL ZONE SOUTH OF YANGTZE RIVER
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摘要 根据江南红黄壤丘陵区17个站点1951~1988年逐旬气象资料以及相应地区的土壤物理参数,模拟出各站点土壤层的土壤湿度数据库,并分析土壤季节性干旱规律。其中衡阳、邵阳地区是江南红黄壤丘陵区土壤季节性干旱最严重的地区,其次是南昌、贵溪市一带。通常年份,2月中旬~6月下旬,全区几乎不出现土壤季节性干旱。土壤季节性干旱主要出现在7月下旬到10月下旬,其机率在50%以上,8月上、中旬,9月中~10月中旬出现的机率为60%。江南红黄壤丘陵区夏季干旱往往连着秋季干旱。这种连旱的机率衡阳地区在60%以上。冬季1~2月的土壤季节性干旱应是第一年秋旱的延续。文中也提出江南红黄壤丘陵区土壤季节性干旱的防御措施。 According to the every 10-day routine meteorological data and the related physical parametersof soil from 17 stations in the red-yellow soil zone south of Yangtze River in period from 1051 to1988, we simulated a data base,calculated the soil moisture and analysed the characteristics of theseasonal soil drought about these stntions.The most serious seasonal soil drought occurs in theregions Hengyang and Shaoyang.The second serious drought is in the Nanchng and GuixiRegions.In normal years,the seasonal soil drotight seldom occurs in the zone from the middle ofFebruary to middle of June. Drought occurs mainly in the period from middle of July to lateOctober;the probability is higher than 50%. In the early and middle of August and from middleof September to middle of October, such a probability is more the 60%.The autumn soildrought frequently succeeded the summer soil drought in the zone; the probability of suchsuccessive drought is higher than 60% in Hengyang region. Winter soil drought should be theprolongation of autumn soil drought.Countermeasures against the seasonal soil drought are alsoput forwnrd in this paper.
出处 《长江流域资源与环境》 CAS CSCD 1995年第3期251-256,共6页 Resources and Environment in the Yangtze Basin
关键词 江南红黄壤 土壤 湿度 模拟 季节性干旱 ed-yellow soil zone south of Yangtze River, soil moisture, simulation, seasonal soil drought
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