收藏 ｜ 设为首页 广告服务 ｜ 联系我们 ｜ 在线留言
高级检索

干旱区地理 >

2019 , Vol. 42 >Issue 1: 85 - 93

DOI: https://doi.org/10.12118/j.issn.1000-6060.2019.01.10

气候与水文

克鲁伦河流域下游水体氢氧同位素与水化学特征

展开
  • 内蒙古农业大学，水利与土木建筑工程学院，呼和浩特 010018
韩知明(1992-)，男，硕士研究生：E-mail: m15029258074@163.com

网络出版日期: 2019-01-16

基金资助

国家自然科学基金项目：(51339002，51509133，51569019，51669022)；内蒙古农业大学优秀青年科学基金：(2014XYQ-10)

收起

The hydrochemical and hydrogen and oxygen isotopic characteristics of water in the low reach of Kherlen River

Expand
  • College of Water Conservancy and Civil Engineering, Inner Mongolia Agricultural University, Hohhot 010018, China

Online published: 2019-01-16

Fold

摘要

通过对克鲁伦河流域下游河水与地下水的主要离子水化学与氢氧同位素进行分析，结合区域水文地质资料，利用Durov图、空间插值、统计分析等方法分析了河水与地下水水化学与氢氧同位素特征。结果表明，河水的水化学类型主要为Na-Ca-HCO3型，地下水水化学类型为Na-Cl和Ca-Na-HCO型。克鲁伦河水主要离子浓度与氢氧同位素空间分布特征显著较地下水稳定、空间差异小。流域内地下水与地表水主要来自降水补给，地下水也是克鲁伦河的主要补给源。氘盈余变化揭示出克鲁伦河水的蒸发分馏程度强于地下水，除流域内水体蒸发主要受地质地貌影响外，人类活动对河水的影响显著于周边地下水。G3点所在的西庙为一个完整独立的水文地质单元，其表现出的水化学与氢氧同位素特征均异于其他地下水。流域内部分地下水F-含量超标，虽然一定程度是受人类活动影响，但更多的是基于综合水文地质条件基础上的自然现象，已严重威胁人类生存，应引起当地有关部门的高度重视，避免氟中毒事件重现。

关键词： 克鲁伦河水; 地下水; 水化学; 氢氧同位素; 氘盈余

本文引用格式

韩知明, 贾克力?, 史小红, 孙标, 杨芳, 吴其慧 . 克鲁伦河流域下游水体氢氧同位素与水化学特征[J]. 干旱区地理, 2019 , 42(1) : 85 -93 . DOI: 10.12118/j.issn.1000-6060.2019.01.10

Abstract

The Kherlen River is the largest lake in the north of China - the main river flowing into Hulun Lake, and it is located in Hulunbeier grassland as a typical grassland river. The Kherlen River originates from the south of Kent Mountain in Mongolia and flows from west to east. The Kherlen River has a total length of 1264 km, with 206.44km in China, and it has a total drainage area of 7153 km2. Combining with the regional hydrogeological data, the characteristics of the hydrochemistry and hydrogen and oxygen isotopes of the main ions in the river water and underground water in the low reach of Kherlen River were analyzed using the Durov diagram, spatial interpolation and statistical analysis method. The results show that the hydrochemical types of the river water are mainly Na-Ca-HCO3 type, and the hydrochemical types of underground water are Na-Cl and Ca-Na-HCO. The spatial distribution characteristics of the main ion concentration and hydrogen and oxygen isotope in the Kherlen river water are more stable than the groundwater, and the spatial difference is small. Hydrogen and oxygen isotope relationship indicates the groundwater and surface water were mainly supplied by the precipitation, while the groundwater is the main supply source of Kherlen River. The variation of deuterium surplus reveals that the evaporation and fractionation degree of the Kherlen River is stronger than that of the groundwater. Besides the water evaporation of the basin is mainly influenced by the geology and geomorphology of the region, the influence by the human activities on the river water is much stronger than that on the underground water. The West Temple at the G3 point is a complete and independent hydrogeological unit, where the characteristics of hydrochemistry and hydrogen and oxygen isotopes are different from other groundwater. The Fl- content of some groundwater in the basin exceeds certain limits, which is caused partially by the human activities to a certain degree but is mainly a naturel result of the comprehensive hydrogeological conditions. This becomes a serious threat to human survival, and the local authorities should pay more attention to this issue and take action to avoid the recurrence of fluorosis.

Key words： Kherlen River; Groundwater; Hydrochemistry; Hydrogen and oxygen isotopes; Deuterium excess

参考文献

[1] 叶宏萌, 袁旭音, 葛敏霞, 李继洲, 孙慧. 太湖北部流域水化学特征及其控制因素[J]. 生态环境学报, 2010, 19(1):23-27.[YE Hongmeng, YUAN Xuyin, GE Minxia, LI Jizhou, SUN Hui. Water chemistry characteristics and controlling factors in the northern rivers in the Taihu Basin [J]. Ecology and Environmental Sciences, 2010, 19(1):23-27.]
[2] Meredith K T, Hollins S E, Hughes C E, Cendón D I, Hankin S, Stone D J M. Temporal variation in stable isotopes (18O and 2H) and major ion concentrations within the Darling River between Bourke and Wilcannia due to variable flows, saline groundwater influx and evaporation.[J]. Journal of Hydrology, 2009, 378(3):313-324.
[3] Tsung-Ren Peng, Chi-Chao Huang, Chung-Ho Wang, Tsung-Kwei Liu, Wan-Chung Lu, Kuan-Yu Chen. Using oxygen, hydrogen, and tritium isotopes to assess pond water’s contribution to groundwater and local precipitation in the pediment tableland areas of northwestern Taiwan[J]. Journal of Hydrology, 2012, s 450–451:105-116.
[4] 王仕琴, 宋献方, 肖国强, 王志民, 刘鑫, 王鹏. 基于氢氧同位素的华北平原降水入渗过程[J]. 水科学进展, 2009, 20(4):495-501.[WANG Shiqin, SONG Xianfang, XIAO Guoqiang, WANG Zhimin, LIU Xin, WANG Peng. Appliance of oxygen and hydrogen isotope in the process of precipitation infiltration in the shallow groundwater areas of North China Plain [J]. Advance in Water Sciences, 2009, 20(4):495-501.]
[5] 徐学选, 张北赢, 田均良. 黄土丘陵区降水-土壤水-地下水转化实验研究[J]. 水科学进展, 2010, 21(1):16-22. [XU Xuexuan, ZHANG Beiying, TIAN Junliang. Experimental study on the precipitation-soil water-groundwater transformation in loese hilly region [J].  Advance in Water Sciences, 2010, 21(1):16-22.]
[6] 蒲焘, 何元庆, 朱国锋, 张蔚, 曹伟宏, 常丽, 王春凤. 丽江盆地地表-地下水的水化学特征及其控制因素[J]. 环境科学, 2012, 33(1):48-54.[PU Tao, HE Yuanqin, ZHU Guofeng, ZHANG Wei, CAO Weihong, CHANG Li, WANG Chunfeng. Hydrochemical characteristics of surface ground water in Lijiang basin and its controlling factors[J]. Environmental science, 2012, 33(1):48-54.]
[7] 巴图. 中蒙克鲁伦河流域草地植被退化及土壤特性比较研究[D]. 内蒙古农业大学, 2013.[Batu. A comparative study on degradation and soil characteristics of grassland vegetation in Mongolia Kherlen Basin
[8] 杨培峰, 李卫平, 于玲红, 陈阿辉, 杨文焕, 韩佩江, 任娟慧, 焦丽燕. 克鲁伦河滨岸带土壤重金属污染风险评估[J]. 农业环境科学学报, 2015, 34(11):2126-2132.[YANG Peifeng, LI Weiping, YU Linghong, CHEN Ahui, YANG Wenhuan, HAN Peijiang, REN Juanhui, JIAO Liyan. Ecological Risk Assessment of Soil Heavy Metals in Riparian Zone of Kerulen River[J]. Journal of Agro-Environment Science, 2015, 34(11):2126-2132.]
[9] 上官存民, 文潮. 地方性氟中毒概述[J]. 陕西医学杂志, 1980(12).[SHANGGUAN Cunmin, WEN chao. An overview of endemic fluorosis[J]. Shaanxi Medical Journal, 1980(12).]
[10] 刘学慧, 胡日查, 郑长顺, 周明仁, 姜志立, 田淑彩, 盖长城, 璋显坤. 2000-2009年内蒙古呼伦贝尔市新巴尔虎右旗地方性氟中毒监测结果分析[J]. 中华地方病学杂志, 2011, 30(5):546-548.[LIU Xuehui, HU Richa, ZHENG Changshun, ZHOU Mingren, JIANG Zhili, TIAN Shucai, GAO Changcheng, ZHANG Xiankun. Analysis of endemic flourosis of Xinbaerhuyouqi in Hulunbeier city of Inner Mongolia in 2000-2009[J]. Chinese Journal of Endemiology, 2011, 30(5):546-548.]
[11] 刘学慧, 李树海. 呼伦贝尔市新巴尔虎右旗改水降氟5年监测结果分析[C]. 中华地方病学杂志. 2005.[LIU Xuehui, LI Shuhai. Analysis of the monitoring results of 5 years of defluoridation in Hulunbeier city in Xinbaerhuyouqi[C]. Chinese Journal of Endemiology, 2005.]
[12] 陈静生. 水环境化学[M]. 高等教育出版社, 1987.45-66. [CHEN Jingsheng. Water environmental chemistry[M]. Higher Education Press, 1987.45-66]
[13] 王苏民. 窦鸿身. 中国湖泊志[M]. 北京: 科学出版社, 1998. [WANG Sumin, DOU Hongshen. Lake of China[M]. Beijing: Science press, 1998.]
[14] 张艳, 吴勇, 杨军, 孙厚云. 阆中市思依镇水化学特征及其成因分析[J]. 环境科学, 2015(9):3230-3237.[ZHANG Y, WU Yong, YANG Jun, SUN Houyun. Hydrochemical characteristic and reasoning analysis in Siyi Town, Langzhong City[J]. Environmental Science, 2015(9):3230-3237.]
[15] 郭巧玲, 熊新芝, 姜景瑞. 窟野河流域不同水体同位素及水化学特征分析[J]. 水土保持学报, 2016, 30(2):237-242.[GUO Qiaoling, XIONG Xinzhi, JIANG Jingrui. Analysis of Isotopic and Hydrochemical Chaiicteristics of Different Waters in Kuye River Basin[J]. Journal of Soil and Water Conservation, 2016, 30(2):237-242.]
[16] 李培月, 钱会. 彭阳县饮用地下水氟离子含量空间变异性及其与地质环境的关系[J]. 水资源与水工程学报, 2010, 21(2):33-38.[LI Peiyue, QIAN Hui. Spatial variability of flourion in drinking groundwater and Its relationship with Geologic Environment in Pengyang Count [J]. Journal of Water Resources & Water Engineering, 2010, 21(2):33-38.]
[17] 韩向红, 杨持. 呼伦湖自净功能及其在区域环境保护中的作用分析[J]. 自然资源学报, 2002, 17(6):684-690.[HAN Xianghong, YANG Chi. An analysis of the self-purification function of Hulun Lake and its effect on regional environmental conservation[J]. Journal of Natural Resources, 2002, 17(6):684-690.]
[18] 牛磊. 基于亚洲地下水资源与环境地质图的跨界含水层研究[D]. 中国地质大学(北京), 2011.[NIU Lei. Research on Transboundary Aquifers Bases on Map of Groundwater Resources and Environment in Asia [D]. China University of Geosciences (Beijing), 2011]
[19] 胡春华, 周文斌. 鄱阳湖流域水化学环境参数的变化特征[J]. 长江流域资源与环境, 2014, 23(3).[HU Chunhua, ZHOU Wenbin. Spatiotemporal variations of hydrochemistry parameters in the Poyang Lake catchment[J]. Yangtze River Basin Resources and Environment, 2014, 23(3).]
[20] Tsujimura M, Abe Y, Tanaka T, Shimade J, Higuchi S, Yamanaka T, Davaa G, Oyunbaatar D. Stable isotopic and geochemical characteristics of groundwater in Kherlen River basin, a semi-arid region in eastern Mongolia[J]. Journal of Hydrology, 2007, 333(1):47-57.
[21] Craig H. Isotopic Variations in Meteoric Waters [J]. Science, 1961, 133(3465):1702.
[22] IanD.Clark, PeterFritz. Environmental isotopes in hydrogeology [M]. The Yellow River Water Conservancy Press, 2006.
[23] 顾慰祖, 刘涌, 贺祥, 邓吉友, 乔茂云. 阿拉善高原地下水的稳定同位素异常[J]. 水科学进展, 1998, 9(4):333-337.[GUI Weizu, LIU Yong, HE Xiang, DENG Jiyou, QIAO Maoyun. Isotopically Anomalous Groundwater of Alxa Plateau, Inner Mongolia[J]. Advance in Water Sciences, 1998, 9(4):333-337.]
[24] 张华安, 王乃昂, 李卓仑, 董春雨, 陆莹, 李贵鹏. 巴丹吉林沙漠东南部湖泊和地下水的氢氧同位素特征[J]. 中国沙漠, 2011, 31(6):1623-1629.[ZHANG Huaan, WANG Naiang, LI Zhuolun, DONG Chunyu, LU Ying, LI Guipeng. Features of Hydrogen and Oxygen Isotopes in Lakes and Groundwater in Southeast Badain Jaran Desert[J]. Journal of Desert Research, 2011, 31(6):1623-1629.]
Options
文章导航

/

〈 〉