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Study on Replenishment Runoff and Discharg of the Shallow Groundwater Based on the Isotope and Hydrochemishtry Analysis Methods——For Example the Shallow Groundwater in Su-Xi-Chang Area(PDF)

《南京师大学报（自然科学版）》[ISSN:1001-4616/CN:32-1239/N]

Issue:
2011年02期
Page:
107-112
Research Field:
地理学
Publishing date:

Info

Title:
Study on Replenishment Runoff and Discharg of the Shallow Groundwater Based on the Isotope and Hydrochemishtry Analysis Methods——For Example the Shallow Groundwater in Su-Xi-Chang Area
Author(s):
Zhang Liyuan1; Chen Suozhong2; Du Ee2
1.Water Resources Service Centre of Jiangsu Province,Nanjing 210029,China
Keywords:
env ironm enta l iso tope;  w ater chem istry;  recharg e;  runo ff and d ischarge cond itions;  shallow groundwa ter;  Su??X i??Chang area
PACS:
P641.8
DOI:
-
Abstract:
On the basis o f analysis and study of spatia l distr ibution character istics of sha llow groundwa ter, th is paper studys rep lenishm en t, runoff and discharg conditions o f the sha llow groundw ater us ing isotope and hydro chem ishtry ana l?? ys is m ethods in Su??X i??Chang area. The ??D - ??18O% curve is established for phrea tic andm icro??confined underg roundw a?? ter by the ana lysis resu lts of hydrogen and oxygen isotope. A ccording to the ??D- ??18O% curve, ana lyzing the re lations o f the phreatic aqu ifer w ith r ivers, lakes and other surface w ater, and the evaporation deg ree o f m icro??confined g roundw a?? ter. The rep lenishm en t relations of m icro??confined g rounderwa ter and modern w ater are studyed by radio iso tope tr itium and 14 C. The problem of the sha llow groundw ate r replen ishment sources change is study ed by the conventiona lm ethod o f chem ica .l That synthetica lly ana ly ze the cond itions o f sha llow groundwa ter replenishm ent runoff and discharge com bining w ith groundwa ter leve,l litho logy, topog raphy and other aspects, in o rder to guide the rational deve lopm ent and utiliza?? tion of sha llow groundwa ter in Su??X i??Chang.

References:

[ 1]  顾阿明, 王彩会, 朱锦旗. 苏锡常地区浅层地下水开发利用前景分析[ J] . 水文地质工程地质, 2003, 30( 4) : 90-92.
[ 2] 陆徐荣, 朱锦旗, 王彩会. 环境同位素技术释解苏锡常地区浅层地下水水循环机制[ J]. 水文地质工程地质, 2006, 33 ( 4): 52-55.
[ 3]  王杰, 王文科, 田华, 等. 环境同位素在三水转化研究中的应用[ J]. 工程勘查, 2007, 7( 3): 31-39.
[ 4]  侯新伟, 李向全, 陈浩. 汾河中游干流河水与大气降水和浅层地下水的转化关系[ J]. 水文地质工程地质, 2008, 12 ( 6): 38-49.
[ 5] 钱云平, 林学钰, 秦大军. 应用同位素研究黑河下游额济纳盆地地下水[ J]. 干旱区地理, 2005, 10( 5): 574-580.
[ 6]  于艳青, 余秋生, 薛忠歧, 等. 同位素技术判定银川平原地下水补给模式[ J]. 宁夏工程技术, 2005, 6( 3) : 208-212.
[ 7]  V andensehr iek G, V anW esem ael B. U sing stable iso tope analysis( D18 0) to character ize the reg iona l hydro logy o f the S ie rra de Gador, sou th east Spain[ J] . Joum a l ofH ydrology, 2002( 265): 43-55.
[ 8]  Aggarwa l P K, Froeh lich K, Gon fian tini R, et a .l Isotope hydro logy: a histor ica l perspective from the IAEA [M ] / /Agga rw al P K, Gatj R, Froehlichkfo. Isotopes in theW ater Cyc le: Past, Present and Future o f aDeve lop ing Sc ience. Berlin: Spr inger, 2005: 3-8.
[ 9]  M ookW G. Env ironm enta l Iso topes in theH ydro log ica l Cycle[M ] . Par is: UNESCO, 2000.

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Last Update: 2011-06-15