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《ACTA GEOSICIENTIA SINICA》 1994-Z1
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A STUDY ON THE DISTRIBUTION AND ENVIROUNMENT ISOTOPEOF UNDERGROUND WATER IN THE WEIHE PLAIN ENVIDENCE FROM BAIYANG SOURCE REGION OF WATER

Li Xingsuo Chang Pixing Gao Wenyi He Juanhua(Xi'an College of Geology)Zhang Maosheng Qi Jialin Xu Renchao Xu Qingzhou(Hydrogeology and Engineering Geology Brigade No:2.BGMR of Shaanxi Province)  
Weihe river,the largest tributary of Yellow river,is the main trunk river of river system in thecentral Shaanxi Plain.Weihe river plain is situated in the middle sector , Shaanxi province.It was resulting from longevolution of Weihe river system. It is a Cenozoic graben basic with considerable thich Cenozoicdeposits. The south and north borders are respectively bounded by Qinling Mountains and NorthMountains,Which extends about 300km in length from Baoji on the west to Tongguan on east,Shaanxi province where it meet Yellow river.Weihe river has an asymmetric drainage.Its north bank tributaries present a dendritic drainage,whereas south tributaries a featherllke drainage.Baiyang source region of water is located at the flood plain-terrace I on the south bank of Weiheriver, near the Linghe- Weihe rivers junction at Baiyang country in Weinan county , covering an areaabout 10km ̄2. It is a source region of water of polylaminate texture consisting of quaternary alluvionsand lake deposits, containg a phreatic water,a shallow,a middle and a deep confined water four aquifers。Phreatic water is maily supplied by lateral influent seepage of river,and infiltration ofprecipitated water.Being exploited,it is mainly supplied by lateral influent seepage of river and run-off.Confined water is mainly supplied by underground water flow from west side of explorationregion,As phreatic table is a little higher than shallow confined water, and middle confined waterhigner than deep confined water, there is an overwash relationship between them,Shallow confinedwater and phreatic water in some section of seurce region of water turn into saline water.It resultfrom gelolgical environment and hydrogeochemical environment characters of the storage andmigration of underground water at the source region of water。Feeding water from Weihe river makes up abeut 1/2 of feeding phreatic water at the Baiyangseurce region of water,Water-bearing strata have a better pormeabiling,and water exchange is bettertoo,The water preduction of a single well is more than 5 0 00m ̄3/d.Middle and deep confined waterwas buried at a deeper depth,with feeder channel being longer,and the age of underground waterbeing more than 4 000-8000 years.B.P.
【Fund】: 地矿部同位素地质开放研究实验室资助课题
【CateGory Index】: P641.7
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