乌蒙山区革香河流域干旱成因及打井找水模式
Causes of drought and models of drilling wells for water exploration in the Gexiang river basin of the Wumeng mountains
-
摘要: 地下水是乌蒙山区革香河流域重要的饮用水源,由于地下水发育规律复杂,地形起伏巨大,给地下水的有效开发利用带来了诸多困难,广大地区存在干旱缺水问题。文章利用岩溶地下水综合调查—探测—评价方法,查明革香河流域地下水赋存发育规律,揭示流域内干旱频发的成因机理,归纳总结出向斜蓄水构造、背斜蓄水构造、断层蓄水带和断陷盆地蓄水构造四类典型蓄水构造模式,优选了断层阻水、向斜蓄水、岩性界线阻水、上下阻水和地下河径流带五种富水成井区位,并有效应用于严重干旱缺水区的打井找水工作,定井成功率达到70%以上,解决了流域内2万多人的饮水困难问题,有效服务脱贫攻坚。Abstract: Groundwater is an important drinking water source in the Gexiang river basin of the Wumeng mountains area. Because of the complex development law of groundwater and the huge topographic relief, the development and utilization of groundwater are facing big difficulties, resulting in water shortage in the vast area. To solve this problem, the hydrogeological investigation team of Institute of Karst Geology used the comprehensive investigation, exploration and the evaluation method of karst groundwater and the combination method of effective geophysical exploration of "three determinations" to clarify the occurrence and development law of groundwater in the study area, reveal the genetic mechanism of frequent droughts in the basin, establish four types of water storage structure models, summarize five types of locations with rich water, and effectively apply them to severe droughts in the water shortage area. The success rate of well location increased more than 70%, which has solved the problem of drinking water for more than 20,000 people in the basin, and effectively aided in the effort of poverty alleviation.
-
Key words:
- Gexiang river basin /
- drought and water shortage /
- groundwater /
- drilling wells for water
-
[1] 唐佐其,李瑞敏,谯文浪,等. 西南岩溶山区地下水资源承载能力评价:以贵州省七星关区为例[J].地质通报,2020,39(1):124-130. [2] 樊云龙,潘保田,胡振波,等.云贵高原北盘江流域构造地貌特征分析[J].地球科学进展,2018,33(7):751-761. [3] 望建成.北盘江流域水文特性分析[J].人民珠江,2014,35(6):55-58. [4] 陈远荣,徐庆鸿,张俊鹏,等.岩溶区生态恢复与重建的初步效果及意义[J].地质通报,2005,24(10-11):1002-1006. [5] 王宇.岩溶高原地下水径流系统垂向分带[J].中国岩溶,2018,37(1):1-8. [6] 余航,王龙,文俊,等.云南省500年干旱灾害时空分布研究[J].干旱区资源与环境,2014,28(12):38-44. [7] 范晓红,沈才明,任宾宾,等.近半个世纪云南持续数年干旱事件时空分布[J].云南师范大学学报(自然科学版),2016,36(1):71-78. [8] 沈祥斌,何丽华,郭赟. 宣威市水土保持工程抗旱减灾效益分析[J].中国水土保持,2011(2):22-24. [9] 王文道,叶文辉.煤炭资源型城市经济转型研究:以云南省宣威市为例[J].时代金融,2010(3):58-60. [10] 南竣祥,赵志芳,洪友堂,等.云南宣威煤矿开发遥感调查研究[J].国土资源遥感,2012(2):121-124. [11] 王宇,王梓溦.岩溶地下水富集的地貌组合形态[J].中国岩溶,2015,34(4):314-324. [12] 李云,姜月华,叶念军,等.基岩山区找水与蓄水条件分析:以单斜和接触型蓄水构造为例[J].地下水,2015,37(1):106-108. [13] 刘光亚.基岩蓄水构造的理论与实践[J].河北地质学院学报,1981(4):50-56,28. [14] 陈萍,王明章.基于地下水开发的岩溶地下水系统类型划分方案探讨[J].中国岩溶,2015,34(3):234-237.
点击查看大图
计量
- 文章访问数: 1487
- HTML浏览量: 615
- PDF下载量: 158
- 被引次数: 0