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- W2357360960 abstract "The Zhuozi Mountain area of Inner Mongolia is an arid region in the northwest of China.The average annual precipitation is less than 200 mm.The middle and lower Ordovician carbonate rock karst water-bearing stratum in the district is important resource of water supply.Oxyhydrogen isotope relationship curve in the region indicates that the samples basically distribute in the upper left of local rainwater line and an obvious phenomenon of reverse Oxygen driftingexists.This kind of isotope distribution is the only one in the most karst groundwater in northern karst spring area that the authors have ever studied. From the particular climate,hydrogeological and natural conditions in this district it can be concluded that there might be condensed water supply to karst groundwater in this area.This point of view was evidenced by analysis of dew isotope." @default.
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- W2357360960 date "2006-01-01" @default.
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- W2357360960 title "DISCUSSION ON CONDENSED WATER SUPPLY TO KARST GROUNDWATER IN ZHUOZI MOUNTAIN REGION,INNER MONGOLIA" @default.
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