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- W2393313683 abstract "Soil moisture is the lifeblood of karst vegetation,the driving force of karstification and important factors of soil erosion.It not only affect ecological and geological security of karst region,but also concern the social and economic development.The existing research shows that: a) the difference of karst soil moisture in southwest China is great,the sequence of soil moisture content is as follows,forest shrub grass,broadleaf forests coniferous forests,and natural forests plantations;b) the spatial distribution of soil moisture content is in the form of patchy,having variability and relativity and complicated distribution on slope;c) the moisture content increases along with the increase of soil depth,changing as low-up-high-down with seasonal succession.The moisture content is difference between wet and dry season and the daily change is down in the morning and up at night and;d) the difference of sub-environment of soil alternates with rock and the fracture extension under soil are the important reasons for great spatial differences of karst soil moisture and abnormal changes of slope.The main research in the future is on the studies of the physical and chemical properties of karst soil moisture,dynamic characteristic of soil water storage reservoir,moderate moisture,engineering techniques of replenishment water in dry season and drainage in wet season with no soil loss,respond to global climate change and soil moisture of karst area in eastern of Yunnan plateau." @default.
- W2393313683 created "2016-06-24" @default.
- W2393313683 creator A5054876323 @default.
- W2393313683 date "2013-01-01" @default.
- W2393313683 modified "2023-09-23" @default.
- W2393313683 title "Progress of Study on Karst Soil Moisture Characteristics of Southwest China" @default.
- W2393313683 hasPublicationYear "2013" @default.
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