Advanced Search
  • Included in CSCD
  • Chinese Core Journals
  • Included in WJCI Report
  • Included in Scopus, CA, DOAJ, EBSCO, JST
  • The Key Magazine of China Technology
Volume 42 Issue 6
Dec.  2023
Turn off MathJax
Article Contents
Article Navigation >  CARSOLOGICA SINICA  > 2023  >  42(6): 1183-1192
REN Shichuan, YANG Xiaoyan, YANG Yingbin, LIU Haifeng, YANG Fan. Equilibrium analysis and prediction evaluation of the Heilongtan groundwater system in Lijiang of northwestern Yunnan Province[J]. CARSOLOGICA SINICA, 2023, 42(6): 1183-1192. doi: 10.11932/karst20230604
Citation: REN Shichuan, YANG Xiaoyan, YANG Yingbin, LIU Haifeng, YANG Fan. Equilibrium analysis and prediction evaluation of the Heilongtan groundwater system in Lijiang of northwestern Yunnan Province[J]. CARSOLOGICA SINICA, 2023, 42(6): 1183-1192. doi: 10.11932/karst20230604
shu

Equilibrium analysis and prediction evaluation of the Heilongtan groundwater system in Lijiang of northwestern Yunnan Province

doi: 10.11932/karst20230604
  • 1.

    Key Laboratory of Geohazard Forecast and Geoecological Restoration in Plateau Mountainous Area, MNR, Kunming, Yunnan 650216, China

  • 2.

    Yunnan Key Laboratory of Geohazard Forecast and Geoecological Restoration in Plateau Mountainous Area, Kunming, Yunnan 650216, China

  • 3.

    Yunnan Institute of Geo-Environment Monitoring, Kunming, Yunnan 650216, China

  • Received Date: 2023-01-01
    Available Online: 2023-12-28
    Abstract
  • The karst water system is a dynamic system controlled by the degree of karst development and the underlying geological conditions. It constantly evolves with changes in climate, human activities, and many other factors. As one of the main driving forces of environmental change, human activities have caused the change at the rate and intensity far exceeding that of natural succession in a short period of time. The environmental effects and induced hydrogeological problems resulting from human activities are extremely difficult to distinguish and quantify, and hence have been the working focus of local governments and scholars at home and abroad. The Lijiang basin is a typical covered and semi-covered karst water system developed in the strong uplift zone of the late Cenozoic crust, which has given birth to the Heilongtan spring, the Xiguanlongtan spring, the Jiudinglongtan spring and other karst springs (spring groups). These springs are not only important water sources for Lijiang City, but also the city's highlights of tourism resources. Among them, the Heilongtan groundwater system is the most important karst water subsystem in the groundwater system of the Lijiang basin. However, the primary discharge point of this system, the Heilongtan spring, has currently experienced a significant reduction in flow and increasing intermittent drying up, which have become important factors restricting local economic and social development. Based on the comprehensive analysis of data over the past 70 years, the investigation of hydrogeological conditions in the Lijiang basin area, and the dynamic monitoring of the Heilongtan groundwater system, we quantitatively evaluated the dynamic flow change of and its influencing factors on the Heilongtan groundwater system with the method of water equilibrium. Fully considering the impact of human engineering activities in socioeconomic development, we summarized factors for the drying-up of the Heilongtan groundwater system as follows. (1) From 1951 to 1990, human engineering activities that replaced and reduced regional vegetation increased natural evaporation capacity and continuously increased evaporative discharge by 10,827,400 m3, accounting for 87.00% of the total decrease in the resources of the Heilongtan groundwater system (12,445,400 m3). This is the main reason for the drying-up probability and the increasing span of Heilongtan spring. (2) From 1991 to 2018, with the recovery of vegetation, the evaporative discharge continuously decreased by 18,303,400 m3, compared with that in the 1980s, which was beneficial to the recovery of Heilongtan spring. However, the factors such as human mining, leakage from the surface river system, and urban development and rereconstruction have caused a total decrease of groundwater resources by 50,586,900 m3, which is unfavorable to the recovery of the Heilongtan spring and is also the cause for its drying up. Among these causes, urbanization and human groundwater extraction reduced groundwater resources by 45,805,200 m3, which accounted for 90.54% of the overall decrease and was another primary cause of the drying-up. According to the change of influencing factors of the Heilongtan spring in recent years, the future changes of its flow predicted by the method of water equilibrium shows that: (1) From 2021 to 2030, the Heilongtan spring will change into a seasonal spring and become drying up during median water year and low flow year. (2) After 2030, the Heilongtan spring groups will remain drying up for a considerable amount of time with a very slim chance of reproduction. This study research can serve as a foundation for the dynamic recovery of Heilongtan groundwater, and the development and environmental protection of the groundwater resources in the urban area of Lijiang.

     

    • FullText(HTML)
  • loading
    • References(26)
  • [1]
    Xing Liting, Huang Linxian, Chi Guangyao, Yang Lizhi, Li Changsuo, Hou Xinyu. A dynamic study of a karst spring based on wavelet analysis and the mann-kendall trend test[J]. Water, 2018, 10(6):698. doi: 10.3390/w10060698
    [2]
    王宇, 何绕生, 刘海峰, 王梓溦, 晏祥省, 双灵, 彭淑惠. 昆明翠湖九龙池泉群断流原因及恢复措施[J]. 中国岩溶, 2014, 33(3):263-271. doi: 10.11932/zgyr20140301

    WANG Yu, HE Raosheng, LIU Haifeng, WANG Ziwei, YAN Xiangsheng, SHUANG Ling, PENG Shuhui. Drought causes and restoration measures for Jiulongchi spring group within Cuihu lake[J]. Carsologica Sinica, 2014, 33(3):263-271. doi: 10.11932/zgyr20140301
    [3]
    梁永平, 王维泰, 赵春红, 王玮, 唐春雷. 中国北方岩溶水变化特征及其环境问题[J]. 中国岩溶, 2013, 32(1):34-42.

    LIANG Yongping, WANG Weitai, ZHAO Chunhong, WANG Wei, TANG Chunlei. Variations of karst water and environmental problems in North China[J]. Carsologica Sinica, 2013, 32(1):34-42.
    [4]
    于苗, 邢立亭, 吴吉春, 侯玉松, 朱恒华, 彭玉明, 李罡. 基于时间序列分形的济南岩溶大泉动态研究[J]. 地质学报, 2020, 94(8):2509-2519. doi: 10.3969/j.issn.0001-5717.2020.08.025

    YU Miao, XING Liting, WU Jichun, HOU Yusong, ZHU Henghua, PENG Yuming, LI Gang. Study of large karst springs using the time series fractal method in Jinan[J]. Acta Geologica Sinica, 2020, 94(8):2509-2519. doi: 10.3969/j.issn.0001-5717.2020.08.025
    [5]
    韩宝平. 国外岩溶水文地质学进展[J]. 中国岩溶, 1993, 12(4):400-406.

    HAN Baoping. Advances in foreign karst hydrogeology[J]. Carsologica Sinica, 1993, 12(4):400-406.
    [6]
    张军以, 王腊春, 苏维词, 曾春芬. 岩溶地区人类活动的水文效应研究现状及展望[J]. 地理科学进展, 2014, 33(8):1125-1135.

    ZHANG Junyi, WANG Lachun, SU Weici, ZENG Chunfen. Status and prospect of the hydrological effects of human activities in the karst area[J]. Progress in Geography, 2014, 33(8):1125-1135.
    [7]
    曾成, 杨睿, 杨明明, 胡君春, 武贵华, 樊宇红. 丽江市黑龙潭泉群断流的人工神经网络模拟[J]. 中国岩溶, 2013, 32(4):391-397.

    ZENG Cheng, YANG Rui, YANG Mingming, HU Junchun, WU Guihua, FAN Yuhong. Artificial neural network simulation to zero flow of the Heilongtan spring groups in Lijiang[J]. Carsologica Sinica, 2013, 32(4):391-397.
    [8]
    康晓波, 王宇, 张华, 曹瑾. 丽江黑龙潭泉群水文地质特征及断流的影响因素分析[J]. 中国岩溶, 2013, 32(4):398-403.

    KANG Xiaobo, WANG Yu, ZHANG Hua, CAO Jin. Hydrogeologic features and influence factors of zero flow of the Heilongtan spring group in Lijiang[J]. Carsologica Sinica, 2013, 32(4):398-403.
    [9]
    周友妹. 丽江古城黑龙潭泉水断流原因分析[J]. 人民珠江, 2015, 36(1):54-58.
    [10]
    和菊芳, 方金鑫. 丽江黑龙潭泉水动态变化与降水关系初探[J]. 中国农村水利水电, 2019(8):26-27, 35.
    [11]
    李豫馨. 基于时间序列分析的丽江黑龙潭泉域动态研究[D]. 成都: 成都理工大学, 2016

    LI Yuxin. Dynamic research of the Lijiang Heilongtan spring system based on the time series analysis[D]. Chengdu: Chengdu University of Technology, 2016.
    [12]
    高伟. 云南省丽江市黑龙潭泉域地下水系统分析[D]. 成都: 成都理工大学, 2016

    GAO Wei. The systematic analysis of Heilongtan spring area karst-water system in Lijiang City of Yunnan Province[D]. Chengdu: Chengdu University of Technology, 2016.
    [13]
    唐克旺, 谭乃元, 谭大书. 丽江黑龙潭泉群保护理论与实践[M]. 北京: 中国水利水电出版社, 2015
    [14]
    中国人民解放军00931部队. 区域水文地质普查报告(丽江幅)[R]. 1979
    [15]
    四川省地质调查院. 石鼓、丽江县等5幅区域地质调查报告[R]. 2016
    [16]
    丽江纳西族自治县县志编纂委员会. 丽江纳西族自治县志[M]. 昆明: 云南人民出版社, 2001
    [17]
    王瑞雪, 史茂, 余其芬. 基于遥感影像解读丽江古城的历史变迁[J]. 昆明理工大学学报, 2000, 35(3):6-11.

    WANG Ruixue, SHI Mao, YU Qifen. Historical changes of ancient Lijiang town based on remote sensing images[J]. Journal of Kunming University of Science and Technology, 2000, 35(3):6-11.
    [18]
    方宝初. 丽江地区森林历史变迁及其对环境的影响[J]. 林业调查规划, 2002, 27(4):42-45. doi: 10.3969/j.issn.1671-3168.2002.04.011

    FANG Baochu. Historical transition of the forests of Lijiang prefecture and its effect on environment[J]. Forest Inventory and Planning, 2002, 27(4):42-45. doi: 10.3969/j.issn.1671-3168.2002.04.011
    [19]
    蒋雪中. 滇西北漾弓江流域近期景观格局演变分析[J]. 华东师范大学学报(自然科学版), 2005(3):84-91.

    JIANG Xuezhong. The evolution analysis of the spatial landscape pattern in the Yanggong river watershed, northwest Yunnan Province during last 15 years[J]. Journal of East China Normal University (Natural Sciences), 2005(3):84-91.
    [20]
    杨海潮. 丽江古城及形象的形成与变迁[J]. 西南民族大学学报(人文社会科学版), 2009, 219(11):44-51.

    YANG Haichao. Formation and transformation of the Lijiang old town and its images[J]. Journal of Southwest Minzu University (Humanities and Social Science), 2009, 219(11):44-51.
    [21]
    杜建括. 基于遥感与实测的玉龙雪山冰川变化[D]. 兰州: 兰州大学, 2008

    DU Jiankuo. The research of glacier change in the Yulong Snow Mountains based on remote sensing and observation data[D]. Lanzhou: Lanzhou University, 2008.
    [22]
    董智杰, 施昆, 王瑞雪, 隋玉成. 基于遥感影像解读玉龙雪山的冰雪动态变化[J]. 科学技术与工程, 2009, 11(9):2075-2093.

    DONG Zhijie, SHI Kun, WANG Ruixue, SUI Yucheng. Interpreted the dynamic changes of the ice on Yulong Jokul based on remote sensing images[J]. Science Technology and Engineering, 2009, 11(9):2075-2093.
    [23]
    李敏敏, 张增祥, 赵晓丽, 汪潇, 刘芳. 丽江市空间扩展与外部形态演变[J]. 遥感信息, 2015, 30(6):102-110. doi: 10.3969/j.issn.1000-3177.2015.06.019

    LI Minmin, ZHANG Zengxiang, ZHAO Xiaoli, WANG Xiao, LIU Fang. Urban spatial expansion and external morphology evolution of Lijiang City[J]. Remote Sensing Information, 2015, 30(6):102-110. doi: 10.3969/j.issn.1000-3177.2015.06.019
    [24]
    郑香. 玉龙雪山冰川变化研究[J]. 社会研究, 2018:279-281.

    ZHENG Xiang. A study of glacier changes in Yulong Snow Mountain[J]. Social Research, 2018:279-281.
    [25]
    李芸. 浅析丽江盆地地下水开发利用现状与保护对策[J]. 水土保持, 2016, 4(1):7-11. doi: 10.12677/OJSWC.2016.41002

    LI Yun. Brief analysis of development and utilization status and protection strategies of Lijiang basin groundwater[J]. Open Journal of Soil and Water Conservation, 2016, 4(1):7-11. doi: 10.12677/OJSWC.2016.41002
    [26]
    高久富, 王庆堂, 王丽荣. 森林覆盖对水面蒸发的影响分析[J]. 黑龙江水专学报, 2001, 28(2):27-28.

    GAO Jiufu, WANG Qingtang, WANG Lirong. Effect analysis of plant-covering to evaporating of water surface[J]. Journal of Heilongjiang Hydraulic Engineering College, 2001, 28(2):27-28.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Get Citation
    PDF(2220.0KB)
    XML

    Article Metrics

    Article views (115) PDF downloads(43) Cited by()
    Proportional views
    Related

    Website Copyright © CARSOLOGICA SINICA 桂ICP备05009877号-1

    Sponsor: Chinese Academy of Geological Sciences Sponsored by: Institute of Karst Geology, Chinese Academy of Geological Sciences Address: No.50, Qixing Road, Guilin, Guangxi

    Post Code: 541004 Tel: 0773-5812949 7796657 Email: zgyr@mail.cgs.gov.cn; zgyrbjb@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd.    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return