塔里木河流域中游绿洲地下水资源评价——以沙雅县为例
|
摘要
地下水资源是我国西部地区水资源的主要组成部分,对地下水资源全面科学的调查和评价,是解决水资源问题的基础性工作。本文尝试采用水均衡方法的同时进行数值模拟的方法对塔里木河流域中游绿洲沙雅县地下水水资源进行评价。结果表明:通过地下水资源均衡计算,绿洲地下水处于正均衡状态,通过数值模拟法计算,绿洲地下水处于负均衡状态。水均衡方法对较大区域地下水资源评价方便易行,但是局部地区精细化计算能力不足,由于多数补给项采用补给系数法计算,结果误差偏大;数值模拟方法对各种尺度研究区均可以进行模拟计算,但是对已有基础资料要求较高,模拟过程充分考虑实际水文地质条件及地下水位动态拟合精度,各源汇项计算精度优于水均衡评价方法结果。两种方法结合应用可更好地用于地下水资源评价。对沙雅县的地下水资源进行评价和分析,目的是科学合理开发利用地下水,保持水土平衡,促进沙雅县经济可持续发展。
Groundwater resources is an important part of whole water resources in the west of China.Scientific investigation and evaluation for underground water is the basic work to resolve water resources problem.The water balance method is often used in groundwater resources evaluation.In this paper,the numerical simulation method was used to evaluate groundwater resources of Tarim Basin after the water balance method.Through the balance of groundwater resources method,groundwater was a positive equilibrium,and through the numerical simulation method,groundwater was a negative equilibrium.By comparing and analyzing,the water balance method can be evaluated facilities in large areas.But it can not be evaluated local area easily.Because there were many recharge items due from supply coefficient.The numerical simulation method can be evaluated all kinds of region,big or small.But,it needed more particular data.The numerical simulation process depended on exact hydrogeological conditions.The results were close to the realty than the water balance method.The two methods combined use for groundwater resources evaluation was better than one.It evaluated and analyzed the groundwater resource in Shaya County which purpose was scientific and reasonable exploitation and utilization of groundwater kept soil and water balance and promoted sustainable development of economy in Shaya County.
Groundwater resources is an important part of whole water resources in the west of China.Scientific investigation and evaluation for underground water is the basic work to resolve water resources problem.The water balance method is often used in groundwater resources evaluation.In this paper,the numerical simulation method was used to evaluate groundwater resources of Tarim Basin after the water balance method.Through the balance of groundwater resources method,groundwater was a positive equilibrium,and through the numerical simulation method,groundwater was a negative equilibrium.By comparing and analyzing,the water balance method can be evaluated facilities in large areas.But it can not be evaluated local area easily.Because there were many recharge items due from supply coefficient.The numerical simulation method can be evaluated all kinds of region,big or small.But,it needed more particular data.The numerical simulation process depended on exact hydrogeological conditions.The results were close to the realty than the water balance method.The two methods combined use for groundwater resources evaluation was better than one.It evaluated and analyzed the groundwater resource in Shaya County which purpose was scientific and reasonable exploitation and utilization of groundwater kept soil and water balance and promoted sustainable development of economy in Shaya County.
引文
[1]曲焕林.中国干旱半干旱地区水资源评价[M].北京:科学出版社,1991.
[2]王浩,陈敏建,秦大庸,等.西北地区水资源合理配置和承载力研究[M].郑州:黄河水利出版社,2003.
[3]胡汝骥,樊自立,王亚俊,等.中国西北干旱区的地下水资源及其特征[J].自然资源学报,2002,17(3):321-326.
[4]Maciek W L.Groundwater fluxes in arid and semi-arid envi-ronments[J].Groundwater and Ecosystem,2006:225-236.
[5]赵成义,王玉朝,李保国.内陆河流域植被变化与地下水运动的耦合关系[J].水利学报,2003,34(12):59-65.
[6]肖笃宁,李小玉,宋冬梅,等.民勤绿洲地下水开采时空动态模拟[J].中国科学(D辑:地球科学),2006,36(6):567-578.
[7]鲍超,方创琳.干旱区水资源开发利用对生态环境影响的研究进展与展望[J].地理科学进展,2008,27(3):38-46.
[8]孙栋元,伊力哈木,冯省利,等.干旱内陆河流域地表水地下水联合调度研究进展[J].地理科学进展,2009,28(2):167-173.
[9]刘予伟,金栋梁.平原区地下水资源评价[J].水利水电快报,2004(12):5-8.
[10]任洪雨,冯斌,郭新体.数值法在地下水资源评价中的应用[J].西部探矿工程,2003(3):27-29.
[11]李宏卿,吴琼,李宏罡,等.Visual Modflow在地下水资源评价中的应用[J].工程勘察,2005(3):27-28.
[12]吴文强,李文文,刘君利.水均衡与数值模拟法在地下水资源评价中对比应用[J].中国农村水利水电,2009(6):45-48.
[13]王金生,王长申,滕彦国.地下水可持续开采量评价方法综述[J].水利学报,2006,37(5):525-533.
[14]张飞,塔西甫拉提.特依拜,丁建丽,等.干旱区土壤盐渍化及其对生态环境的损害评估——以新疆沙雅县为例[J].自然灾害学报,2009,18(4):55-62.
[15]Bridget R Scanlon,Healy R W,Cook P G.Choosing ap-propriate techniques for quantifying groundwater recharge[J].Hydrogeology Journal,2002,10(1):18-39.
[16]Glenn A Harrington,Glen R Walker,Andrew J Love,etal.A compartmental mixing cell approach for the quantita-tive assessment of groundwater dynamics in the Otway Ba-sin,South Australia[J].Journal of Hydrology,1999:214:49-63.
[17]Frans R P,Kalf D R,Woolley.Applicability and meth-odology of determining sustainable yield in groundwater sys-tems[J].Hydrogeology Journal,2005,13(2):295-312.
[18]孟涛,王东.塔里木河南岸14团灌区地下水资源评价与分析[J].地下水,2006,28(6):72-75.
[19]董新光,邓铭江.新疆地下水资源[M].乌鲁木齐:新疆科学技术出版社,2005.
[20]陈梦熊.中国水文地质工程地质事业的发展与成就[M].北京:地震出版社,2003.
[21]孙承志.干旱山区地下水资源开发应用研究[D].中国地质大学博士学位论文,2007.5
[22]陈红媛.新疆玛纳斯县平原区地下水资源量及可开采量计算[J].水利科技与经济,2010,16(8):905-907.
[2]王浩,陈敏建,秦大庸,等.西北地区水资源合理配置和承载力研究[M].郑州:黄河水利出版社,2003.
[3]胡汝骥,樊自立,王亚俊,等.中国西北干旱区的地下水资源及其特征[J].自然资源学报,2002,17(3):321-326.
[4]Maciek W L.Groundwater fluxes in arid and semi-arid envi-ronments[J].Groundwater and Ecosystem,2006:225-236.
[5]赵成义,王玉朝,李保国.内陆河流域植被变化与地下水运动的耦合关系[J].水利学报,2003,34(12):59-65.
[6]肖笃宁,李小玉,宋冬梅,等.民勤绿洲地下水开采时空动态模拟[J].中国科学(D辑:地球科学),2006,36(6):567-578.
[7]鲍超,方创琳.干旱区水资源开发利用对生态环境影响的研究进展与展望[J].地理科学进展,2008,27(3):38-46.
[8]孙栋元,伊力哈木,冯省利,等.干旱内陆河流域地表水地下水联合调度研究进展[J].地理科学进展,2009,28(2):167-173.
[9]刘予伟,金栋梁.平原区地下水资源评价[J].水利水电快报,2004(12):5-8.
[10]任洪雨,冯斌,郭新体.数值法在地下水资源评价中的应用[J].西部探矿工程,2003(3):27-29.
[11]李宏卿,吴琼,李宏罡,等.Visual Modflow在地下水资源评价中的应用[J].工程勘察,2005(3):27-28.
[12]吴文强,李文文,刘君利.水均衡与数值模拟法在地下水资源评价中对比应用[J].中国农村水利水电,2009(6):45-48.
[13]王金生,王长申,滕彦国.地下水可持续开采量评价方法综述[J].水利学报,2006,37(5):525-533.
[14]张飞,塔西甫拉提.特依拜,丁建丽,等.干旱区土壤盐渍化及其对生态环境的损害评估——以新疆沙雅县为例[J].自然灾害学报,2009,18(4):55-62.
[15]Bridget R Scanlon,Healy R W,Cook P G.Choosing ap-propriate techniques for quantifying groundwater recharge[J].Hydrogeology Journal,2002,10(1):18-39.
[16]Glenn A Harrington,Glen R Walker,Andrew J Love,etal.A compartmental mixing cell approach for the quantita-tive assessment of groundwater dynamics in the Otway Ba-sin,South Australia[J].Journal of Hydrology,1999:214:49-63.
[17]Frans R P,Kalf D R,Woolley.Applicability and meth-odology of determining sustainable yield in groundwater sys-tems[J].Hydrogeology Journal,2005,13(2):295-312.
[18]孟涛,王东.塔里木河南岸14团灌区地下水资源评价与分析[J].地下水,2006,28(6):72-75.
[19]董新光,邓铭江.新疆地下水资源[M].乌鲁木齐:新疆科学技术出版社,2005.
[20]陈梦熊.中国水文地质工程地质事业的发展与成就[M].北京:地震出版社,2003.
[21]孙承志.干旱山区地下水资源开发应用研究[D].中国地质大学博士学位论文,2007.5
[22]陈红媛.新疆玛纳斯县平原区地下水资源量及可开采量计算[J].水利科技与经济,2010,16(8):905-907.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心