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- W2368007817 abstract "In humid,temperate or humid wet tropical environments,chemical water-rock interaction plays an important role in rocky slope hydrogeology evolution and landslide pregnancy.From the earth's surface to fresh bedrock the profile of slope may be divided into soil zone,saprolite zone and weathered rock zone.Soil is made of dry branches and fallen leares layer and earth layer,but sometimes contains residuum material.Saprolite is isovolumetrically weathered soft rock.Weathered rock is the predecessor of saprolite and is mainly made of corestones surrounded by saprolite crust.It is by chemical water-rock interactionthat slope zoning is caused and the zoning affects strongly the distribution of groundwater.Soil zone can keep perched water and phreatic water or confined water may occur in weathered rock zone.Perched water is the main controlling factor of shallow slope failures and the phreatic water or confined water in weathered rock zone can bring out deep-seated landslides after heavy rainfall." @default.
- W2368007817 created "2016-06-24" @default.
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- W2368007817 date "2007-01-01" @default.
- W2368007817 modified "2023-09-28" @default.
- W2368007817 title "Effect of chemical water-rock interaction on hydrogeology and landslide of slope" @default.
- W2368007817 hasPublicationYear "2007" @default.
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