Hydrogeochemical Modelling of Groundwater Chemical Evolution fromSouthern Margin to Hinterland of the Taklamakan Desert

Wei Yaping; Fan Jinglong; Xu Xinwen; Jin Xiaojun; Zhou Hongwei

doi:10.7522/j.issn.1000-694X.2015.00025

Journal of Desert Research >

2016 , Vol. 36 >Issue 3: 798 - 804

DOI: https://doi.org/10.7522/j.issn.1000-694X.2015.00025

Hydrogeochemical Modelling of Groundwater Chemical Evolution fromSouthern Margin to Hinterland of the Taklamakan Desert

Wei Yaping ,
Fan Jinglong ,
Xu Xinwen ,
Jin Xiaojun ,
Zhou Hongwei

Expand

1. Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;
2. University of Chinese Academy of Sciences, Beijing 100049, China;
3. PetroChina Tarim Oilfield Company, Korla 841000, Xinjiang, China

Received date: 2014-11-21

Revised date: 2015-02-06

Online published: 2016-05-20

Fold

Abstract

The oil and natural gas resources are rich in the hinterland of the Taklamakan desert, where weather is extremely dry, ecological environment is extremely frail. In this study,in order to provide dependable foundation for the reasonable exploitation of groundwater, the protection and improvement of water quality. A section crossing the from Kunlun piedmont to the hinterland of Taklimakan Desert is monitored,Piper diagram is utilized to analyze the hydrochemical type, and NETPATH Modeling is used to simulate the process of chemical evolution of groundwater. The results obtained are stated as follows: (1) The groundwater hydrochemical types are comparatively single in the area, the main types are Na-Mg-Cl-SO₄ and Na-Cl-SO₄; (2) The main representation properties of the water chemical evolution model are the strong evaporation and concentration, the dissolution of mirabilite, rock salt and pyroxene, and the more prominent Ca²⁺/Na⁺ ion exchange.

Key words： groundwater; chemical evolution; NETPATH model; Taklimakan Desert

Cite this article

Wei Yaping , Fan Jinglong , Xu Xinwen , Jin Xiaojun , Zhou Hongwei . Hydrogeochemical Modelling of Groundwater Chemical Evolution fromSouthern Margin to Hinterland of the Taklamakan Desert[J]. Journal of Desert Research, 2016 , 36(3) : 798 -804 . DOI: 10.7522/j.issn.1000-694X.2015.00025

References

[1] Zhao W Z,Cheng G D.Review of several problems on the study of eco-hydrological processes in arid zones[J].Chinese Science Bulletin,2002,47(5):353-360.
[2] Huang T M,Pang Z H.Changes in groundwater induced by water diversion in the Lower Tarim River,Xinjiang Uygur,NW China: Evidence from environmental isotopes and water chemistry[J].Journal of Hydrology,2010,387(3/4):188-201.
[3] 楼章华,金爱民,朱蓉,等.松辽盆地油田地下水化学场的垂直分带性与平面分区性[J].地质科学,2006,41(3):392-403.
[4] 安帅,王乃昂,陈会丽,等.基于SOFM网络的巴丹吉林沙漠湖泊聚类及其地下水补给来源推断[J].中国沙漠,2014,34(2):574-581.
[5] 张竞,王旭升,胡晓农,等.巴丹吉林沙漠地下水流场的宏观特征[J].中国沙漠,2015,35(3):774-782.
[6] çAfçin M.Hydrochemical evolution and water quality along the groundwater flow path in the Sandıklı plain,Afyon,Turkey[J].Environmental Geology,1997,31(16):221-230.
[7] Parnachev V P,Banks D,Berezovsky A Y,et al.Hydrochemical evolution of Na-SO₄-Cl groundwaters in a cold,semi-arid region of southern Siberia[J].Hydrogeology Journal,1999,7(10):546-560.
[8] Favara R,Grassa F,Valenza M.Hydrochemical evolution and environmental features of Salso River catchment,central Sicily (Italy)[J].Environmental Geology,2000,39(13):1205-1215.
[9] 郭永梅,沈照理,钟佐燊.河北平原地下水化学环境演化的地球化学模拟[J].中国科学(D辑),1997,27(4):360-365.
[10] 宋保平,张先林,方正.等.长江河口地区第四系地下水化学演化机制[J].地理学报,2000,55(2):208-218.
[11] Lei J Q,Li S Y,Fan D D,et al.Classification and regionalization of the forming environment of windblown sand disasters along the Tarim Desert Highway[J].Chinese Science Bulletin,2008,53(2):1-7.
[12] Lei J Q,Li S Y,Jin Z Z,et al.Comprehensive eco-environmental effects of the shelter-forest ecological engineering along the Tarim Desert Highway[J].Chinese Science Bulletin,2008,53(S2):190-202.
[13] 牟世芬,刘克纳.离子色谱方法及应用[M].北京:化学工业出版社,2000:64-128.
[14] 国家技术监督局.饮用天然矿泉水检验方法(中华人民共和国国家标准)[S].北京:中国标准出版社,2008.
[15] Plummer L N,Back W.The mass balance approach:application to interpreting the chemical evolations of hydrologic systems[J].American Journal Science,1980,280:130-142.
[16] Plummer L N,Prestemon E C,Parkhurst D L,et al.An interactive code (NETPATH) for modeling net geochemical reactions along a flow path,version 2.0[M].Reston,Virginia,USA:Geological Survey,1994.
[17] El Kadi A I,Plummer L N,Aggarwal P.NETPATH-WIN: An Interactive User Version of the Mass-Balance Model,NETPATH[J].Ground Water,2011,49(4):593-599.
[18] 中国科学院塔克拉玛干沙漠综合科学考察队.塔克拉玛干沙漠地区水资源评价与利用[M].北京:科学出版社,1993:160-162.
[19] 冯起,陈广庭,董光荣,等.塔克拉玛干沙漠北部泛滥平原全新世沉积相矿物成份分布与环境意义[J].沉积学报,1995,13(3):66-75.
[20] 朱震达,陈治平,吴正,等.塔克拉玛干沙漠风沙地貌研究[M].北京:科学出版社,1981:8-26.
[21] Fan J L,Xu X W,Lei J Q,et al.The temporal and spatial fluctuation of the groundwater level along the Tarim desert highway[J].Chinese Science Bulletin,2008,(Supp.II):53-62.
[22] 潘宏雨,马锁柱,刘连成,等.水文地质学概论[M].北京:地质出版社,2009:58-59.
[23] Zhu B Q,Yang X P.The ion chemistry of surface and ground waters in the Taklimakan Desert of Tarim Basin,western China[J].Chinese Science Bulletin,2007,52(15):2123-2129.
[24] 马金珠,李相虎,黄天明.石羊河流域水化学演化与地下水补给特[J].资源科学,2005,27(3):117-122.
[25] 赵华,马金珠,朱高峰,等.甘肃省民勤县盆地地下水环境变化及原因探讨[J].干旱区研究,2004,21(3):210-214.
[26] 丁洪伟,张举.河西走廊地下水水化学特征及其演化规律[J].干旱区研究,2005,22(1):24-28.
[27] 叶浩,王贵玲,叶思源,等.宁夏南部月亮山西麓地下水化学特征研究[J].地球学报,2001,22(4):330-334.
[28] 石培泽,马金珠,赵华.民勤盆地地下水地球化学演化模拟[J].干旱区地理,2004,27(3):305-309.
[29] 史基安,赵兴东,王琪,等.石羊河流域地下水化学演化特征研究[J].沉积学报,1998,16(2):145- 148.
[30] 王琪,史基安,赵兴东,等.石羊河流域地下水地球化学特征演化的计算机模拟研究[J].中国沙漠,2003,23(2):160-164.

Options

Outlines

模态框（Modal）标题

Abstract

Cite this article

References