Evaluation of groundwater resource loss in middle regions of Huaying mountain
-
摘要: 四川华蓥山中段地区水流失比较严重,供需矛盾突出,水环境持续恶化,不但影响到居民正常的生产和生活,而且严重影响了该地区国民经济的建设和发展。通过野外调查和综合分析现场收集的资料,总结出华蓥山中段地区地下水资源量流失情况:该区每年流失的水资源量约为0.914 4亿m3,且华蓥山褶皱西翼水流失总量大于东翼,而西翼北端是区内水流失量最严重的区域,其水资源量流失的影响因素主要为气候、社会发展及人类活动等。Abstract: Huaying mountain, a karst mountain area, is located in the east part of Sichuan Province. The study area is about 1,500 km2, with its middle part bestriding the east and west wings of Huaying mountain anticline which presents a north-east trending silver shape. Over the anticlinal wings, karst strata and non-karst strata alternately distribute. Bounded by non-karst strata constituting the aquitard, groundwater in the area mainly occurs in strip-shaped carbonate rock formations. Restricted by the conditions of stratum exposure, the karst water migrates in the direction from the southwest to the northeast. Since the 1980s, groundwater resources in middle regions of Huaying mountain area have drastically declined. The loss of the karst water has heavily affected both water supply to the local communities and development of regional economy. This paper discusses the factors and the quantity of water resources loss in the area. Through integrating analytical results of field survey and desktop study, the factors that have impacted on the water resources reduction, including climate change, social economic growth and human engineering activity, were identified. Among them the decrease of rainfall and the steep topography in mountain region have resulted in the shrink of water replenishment. In addition, social economic growth and expansion of human engineering activities both have led to great water consumption. According to the division method of karst water system, the groundwater units for water resources assessment in the study area were divided. On this basis, the water balance method was used to calculate the amount of water resources loss each year which is about 91.44×106 m3. The volume of water loss in west wing of Huaying mountain is larger than that of the east wing. Moreover, the north part of the west wing has suffered from the most serious water loss in the area. By discussing the relationship between social, economic, environmental and water resources loss, this paper provides a certain basis for the comprehensive assessment and sustainable development of water resources in the study area.
-
Key words:
- groundwater resources /
- middle regions of Huaying mountain /
- karst area
-
[1] 冯尚友.水资源持续利用与管理导论[M].北京:科学出版社,2000. [2] Xiaobing Kang, Sheng Luo, Mo Xu. Research on the mechanism of water resource loss in east karst mountain area of Sichuan[J]. Desalination and Water Treatment,2015,53(2):557-566. [3] Marco Franchini, Alessandra Bonoli. A Procedure for Evaluating the Compatibility of Surface Water Resources with Environmental and Human Requirements[J]. Water Resources Management,2011,25(14):3613-3634. [4] 胡彩虹,吴泽宁,高军省,等.区域水资源可利用量研究[J].干旱区地理,2010,33(3):404-410. [5] 陈绍林,李茂竹,陈忠恕,等.四川广(安)—渝(重庆)高速公路华蓥山隧道岩溶突水的研究与整治[J].岩石力学与工程学报,2002,21(9):1344-1349. [6] 黄继.华蓥山褶皱山区岩溶水系统循环演化模式分析[D].成都:成都理工大学,2009. [7] 刘丹,杨立中,于苏俊.华蓥山隧道排水的生态环境问题及效应[J].西南交通大学学报,2001,36(3):308-313. [8] 左烽林,魏朝富.基于DEM和SCS模型的重庆岩溶槽谷区塘堰复蓄次数的计算[J].中国岩溶,2016,35(1):87-97. [9] 易连兴,夏日元,唐建生,等.西南岩溶地下河流量重复统计问题及对策探讨[J].中国岩溶,2015,34(1):72-78. [10] 罗明明,尹德超,张亮,等.南方岩溶含水系统结构识别方法初探[J].中国岩溶,2015,34(6):543-550. [11] 苏印,官冬杰,苏维词.基于SPA的喀斯特地区水安全评价:以贵州省为例[J].中国岩溶,2015,34(6):560-569. [12] E Mougin, P Hiernaux , L Kergoat, et al. The AMMA-CATCH Gourma observatory site in Mali: Relating climatic variations to changes in vegetation, surface hydrology, fluxes and natural resources[J]. Journal of Hydrology,2009,375(1-2):14-33. [13] 段秀举.基于生态理念的山地城市水资源规划研究:以重庆市水资源规划为例[D].重庆:重庆大学,2015. [14] 刘俊杰,陈雄.地下开采条件下水资源流失机理与环境影响研究[J].中国地质灾害与防治学报,2003,14(4):71-74. [15] 田卫堂,胡维银,李军,等.我国水土流失现状和防治对策分析[J].水土保持研究,2008,15(4):204-209. [16] 雷才国,曹善华,郭平.华蓥山矿区龙滩煤矿水害因素分析评价[J].现代矿业,2011(3):44-48,61. [17] 向虎,叶秀娟,袁森林,等.华蓥山矿区龙滩煤矿开采系统涌水量分析比较[J].中国煤炭地质,2012,24(1):26-28.
点击查看大图
计量
- 文章访问数: 2034
- HTML浏览量: 607
- PDF下载量: 593
- 被引次数: 0