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低丘红壤区植物生长季降雨对土壤水分动态的影响分析

he analysis on the influence of rainfall on soil moisture dynamic in Low hill red soil region at plant growing season

中文摘要英文摘要

低丘红壤区气候资源丰富,降雨充足但分布不均,容易导致季节性暴雨、伏旱、秋旱等。本文在实测田间数据基础上分析了降雨对低丘红壤区橘园和花生地土壤水分变化的影响。结果表明:橘园和花生地土壤含水量的变化趋势与降雨变化一致,降雨影响与土壤初始含水量、土壤深度和降雨强度有关;橘园和花生地土壤含水量随土壤深度变化的趋势相似,土壤含水量变异系数随深度逐渐减小,含水量趋于稳定;橘园地生长季总蒸散量略大于花生地,径流量小于花生地。

he climate resource in Low hill red soil region is rich, plentiful rainfall but uneven distribution, easily lead to seasonal storms, drought, etc. This paper analyzes the effects of rainfall on soil moisture characteristics under two kinds of land use types based on the measured field data. The results show that the two types of land use change trend of soil moisture content is in line with rainfall; Two kinds of land use types of soil moisture content change trend with soil depth is consistent, the variation coefficient decreases with depth, water content tends to be stable; The total evaporation of two land use types in the growing season are same.

金心怡、陈昆、景元书

农业科学研究环境科学理论

红壤土地利用类型土壤水分蒸散量

red soilland use typessoil waterevaporation

金心怡,陈昆,景元书.低丘红壤区植物生长季降雨对土壤水分动态的影响分析[EB/OL].(2014-05-23)[2025-08-19].http://www.paper.edu.cn/releasepaper/content/201405-418.点此复制

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