Division of karst water protection areas based on analysis of hydrogeologic conditions
-
摘要: 以邢台百泉岩溶水系统为例,分析了邢台百泉岩溶水系统的地下水流场受人类活动影响的演变特征,并采用数值模拟法预测了超采条件下水源地未来十年流场的变化。首次发现了泉域矿山疏排水形成了“沙河人工分水岭”并迅速北移的现象,标志百泉泉域地下水资源恶化严重,提出了在复杂岩溶水文地质条件下,采用以计算流程的方法划分保护区造成保护区浪费和碳酸盐岩裸露补给区没有保护的问题。在兼顾水质保护和水资源量可持续利用的前提下,分析了水源地上覆地层的防护能力和碳酸盐岩裸露补给区矿山疏排水对水源地的影响,将碳酸盐岩裸露补给区划分为二级保护区,突破了传统的“二级保护区包裹一级保护区”的模式,以较小的保护区面积有效地保证水源地的水质安全和可持续利用。Abstract: This paper discussed the division of water source protection zones in karst areas with complex hydro-geological conditions. Taking the Baiquan karst water system of Xingtai City, Hebei Province as an example, we analyzed the historical evolution characters of the groundwater flow field of the karst system influenced by human activities, and forecasted the variation of this field in ten years under the conditions of over exploitation by the numerical modeling method. It is found that "the artificial watershed of the Shahe River" has formed due to water drainage from mines in the spring areas, which is moving north rapidly, indicative of the seriousness of water resource shortage in the Baiquan karst area. We suggested that under complex karst hydro-geological conditions, if the protection zone is divided using the calculation flow method, it can result in waste of the protected area and the non-protection of the recharge area with carbonate exposure. On the premise of water quality protection and sustainability of water resources, we analyzed the protective capability of overlying strata of the water source and the influence on the water source of drainage from mines in the recharge area with carbonate exposure. Such recharge area should be attributed to a secondary protection zone, which breaks the traditional pattern of "the primary protection zone enclosed by the second protection zone". The overall water level of the Baiquan karst water system has increased for nearly 30 m in two years since the adjustment of the protection area, which proves that the quality and sustainability of the water source with a relatively small protection zone is guaranteed by the new division method and that the hydrogeological condition analysis is important for the division of water source protection zones in complicated areas.
-
[1] 国家环境保护总局.饮用水水源保护区划分技术规范(HJ/T3382007)[S]. 2007. [2] 李星宇.数值模拟方法在隐伏岩溶水源地保护区划分及污染治理中的应用[J].中国岩溶,2014,33(3):281-286. [3] Panagopoulos G. Application of MODFLOW for simulating groundwater flow in the Trifilia karst aquifer, Greece [J].Environmental Earth Sciences,2012,67(7):1877-1889. [4] Giudici M,Margiotta S,Mazzone F,et al.Modelling hydrostratigraphy and groundwater flow of a fractured and karst aquifer in a Mediterranean basin (Salento peninsula, southeastern Italy) [J]. Environmental Earth Sciences, 2012, 67 (7): 1891 - 1907. [5] 翟立娟.岩溶水饮用水水源保护区划分技术方法:以邯郸市羊角铺水源地为例[J].中国岩溶,2011,30(1):47-52. [6] 侯燕军.临汾市土门水源地保护区划分的数值模拟方法研究[D].太原:太原理工大学,2006. [7] 杨炳超.地下水质量综合评价方法的研究[D].西安:长安大学,2004. [8] 张丽君,曹红,马颖.地下水源保护区划分方法的探讨[J].辽宁城乡环境科技,2006,26(2):910,13. [9] 王建国.河北省邯邢铁矿田岩溶充水铁矿开采与地下水环境保护[R].石家庄:华北有色工程勘察院,2007. [10] 付延玲.邯邢水文地质南单元岩溶地下水系统数值预报[J].中国岩溶, 2002, 21 (4):269275. [11] 南天,李鹏,李星宇,等.大兴迭隆起隐伏岩溶水资源评价及开采方案预测[J].中国岩溶, 2014, 33 (2):156166. [12] 李国敏,徐海珍.地下水源地保护区划分方法与应用[M].北京:中国环境科学出版社,2011.
点击查看大图
计量
- 文章访问数: 1450
- HTML浏览量: 281
- PDF下载量: 689
- 被引次数: 0