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- W2390079427 abstract "This paper deals with 9 drip points monitored for a year in Qixing cave,Duyun county of Guizhou province,China.According to the research of element geochemistry,water transporting in the cave roof influenced the sources of the substances,and the substances in drip water mainly come from the soil and rock in the roof of Qixing cave and the fewer content of elements origins from the rainfall.Variation of drip water composition is mainly controlled by processes of rock dissolution and calcite precipitation while water transporting in soil and rock.Contribution of water-rock interaction to drip water chemical composition is a bit more because the water of QXD-1#,QXD-2#,QXD-6#,QXD-7#,QXD-8# passes through a thinner soil.Dilution only happens on QXD-2# in drought seasons,piston flow happens on QXD-7# and QXD-9# in rainy seasons,and jumped drip ratio happens on QXD-1#,QXD-3#,QXD-8# because of different water sources,but all of these processes have much weaker effects on drip chemical composition.Mg/Ca of drips implies change of rainfall,and Mg/Ca values are controlled by hydrogeochemical process of water-soil,water-rock interaction while water transports in cave roof,that is the processes of rock dissolution and calcite precipitation and of soil physics,soil chemistry,and soil biology etc." @default.
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- W2390079427 date "2006-01-01" @default.
- W2390079427 modified "2023-09-23" @default.
- W2390079427 title "Drips Hydrogeochemical Characteristics of Qixing cave and its' Implications" @default.
- W2390079427 hasPublicationYear "2006" @default.
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