纸质出版:2005
移动端阅览
傅伟 王克林 陈洪松 苏以荣. 典型峰丛洼地坡面土壤水分动态变化的时序分析[J]. 水土保持学报, 2005,19(4):111-114.
Time Series Analysis of Soil Moisture Dynamic Change on Hillslope in Typical Karst Peak-Cluster Depression Area[J]. 2005, 19(4): 111-114.
采用时间序列分析方法,分析了2004年5~9月广西环江典型峰丛洼地坡面上6种土地覆被类型10,20cm土壤水势与降水动态变化的相关关系。结果表明:(1)灌丛与板栗覆草土壤中的水分较充裕,其含量受天气的波动变化较小,对降水的影响具有缓效性、长期性的特点;(2)坡耕地中水分含量较低,随降雨的波动变化剧烈,但南瓜的地上植株部分对土壤水分的调节保持有积极作用;(3)撂荒草地与木豆土壤水分含量的层间差异都较显著,对降水响应的即时性也强,但撂荒地20cm土层对降水的响应期长些,能保证短时间内向10cm土层的水分补给;(4)处于幼龄期的板栗,土壤水分变化反映的是仅受天气影响下的自然裸露坡地的状况,变化介于灌丛、板栗覆草和撂荒草地、木豆之间。
By time series analysis
the relationships between soil water potential and precipitation dynamic change on hillslope in the typical peak-cluster depression area of Huanjiang county in Guangxi Autonomous region have been analyzedfrom May to September in 2004
and the soil water potential was collected from 10 and 20 cm depths of the six kinds of land covers. The results show as follows:(1) with the soil character of hysteresis and retentivity with precipitation
shrubbery and hay-covered chesnut were both abundant in soil moisture storage
which of the two kinds were slightly influenced by the weather fluctuation; (2) the soil moisture content kept lower on the slope land cultivated
obviously changing with the precipitation fluctuation
yet has been adjusted to detain for long period with the help of cushaw of creeping vegetation;(3) grassland and cajanus both had great difference in depths with soil moisture content which instantaneously responded to precipitation
but the 20cm depth of the first land cover had a better moisture retention
so as to be good for the moisture compensation for the 10 cm; (4) at the age of sapling
chesnut field was nearly bare ground
its soil moisture dynamic change had little connection with vegetation
but mostly with meteorological factors
which induced the change between that of the kinds of shrubbery
hay-covered chesnut and that of the kinds of grassland
cajanus.
0
浏览量
10
下载量
18
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621