[1]杨红,许模,张劲松.滇东南弥勒盆地蓄水构造特征分析及找水方向[J].水土保持研究,2012,19(06):254-258.
　YANG Hong,XU Mo,ZHANG Jin-song.Analysis of the Characteristics of Groundwater Storage Structure and Groundwater Exploration in Mile Basin, Southeast Yunnan Province[J].Research of Soil and Water Conservation,2012,19(06):254-258.
点击复制

滇东南弥勒盆地蓄水构造特征分析及找水方向

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 19 期数: 2012年06期 页码: 254-258 栏目: 出版日期: 2012-12-20
Title:
Analysis of the Characteristics of Groundwater Storage Structure and Groundwater Exploration in Mile Basin, Southeast Yunnan Province
作者:
杨红1, 许模1, 张劲松2
1. 成都理工大学 地质灾害防治与地质环境保护国家重点实验室, 成都 610059;
2. 云南省交通规划设计研究院, 昆明 650011
Author(s):
YANG Hong1, XU Mo1, ZHANG Jin-song2
1. State Key Laboratory of Geo-hazard Prevention and Geo-environment Protection, Chengdu University of Technology, Chengdu 610059, China;
2. Traffic Planning and Design Institute of Yunnan Province, Kunming 650011, China
关键词:
地下水; 弥勒盆地; 蓄水构造; 找水方向
Keywords:
groundwater; Mile basin; water storage structure; water exploration
分类号:
TV211.1
摘要:
蓄水构造是富集地下水的地质构造形式,它是地下水形成、运动和蓄存的场所.在干旱地区寻找地下水主要是寻找有利的蓄水构造.通过分析弥勒盆地及其周边蓄水构造的特征,能为今后弥勒地区干旱年份寻找地下水提供水文地质依据.该文在对区域地质条件、地下水系统资料进行详尽分析并结合野外现场调查的基础上,基于蓄水构造的三要素,对滇东南弥勒盆地蓄水构造类型及其特征进行了分析,认为区内主要有汇水型蓄水构造、阻水型蓄水构造和风化带型蓄水构造三类,在干旱年份岩性分界面阻水型蓄水构造、断裂型蓄水构造和风化带型蓄水构造中的地下水具有供水意义.
Abstract:
Geological structure is important for controlling the formation, movement and accumulation of groundwater. Analysis of water storage structure is an useful method for groundwater exploration in arid area. Analyzing characteristics of water storage structure in Mile basin and its peripheral area can provide hydrogeological basis for groundwater exploration of Mile in future drought year. Base on the regional geological conditions, groundwater system data were analyzed in detailed, and this paper analyzed the type and characteristics of water storage structure in Mile basin according to the field survey and the critically examination of the three elements of water storage structure. According to the geological analysis, the main water storage structure types were catchment, water resisting structure and weathered zone in Mile basin, suggesting that the main direction of groundwater exploration in drought year was to find the water in the lithologic boundary as water resisting structure, as well as in fault and weathered zone.

参考文献/References:

[1] 张之淦,陈伟海.岩溶蓄水构造与找水:以广西来宾小平阳为例[J].水文地质工程地质,2000(6):1-5.
[2] 刘光亚.基岩蓄水构造[M].北京:地质出版社,1979.
[3] 钱学溥.中国蓄水构造类型[M].北京:科学出版社,1990.
[4] 沈照理,刘光亚,杨成田,等.水文地质学[M].北京:科学出版社,1985.
[5] 李希文,刘广培.个旧矿区及其外围的几种蓄水构造[J].云南地质,1986,5(3):235-240.
[6] 宋照光.利用断层蓄水构造在山区找水定井的探讨[J].水利科技,2007(12):27-29.
[7] 刘新号.基于蓄水构造类型的山区综合找水技术[J].水文地质工程地质,2011,38(6):8-12.
[8] 邸志强,金洪涛,苗英,等.辽西蓄水构造及找水方向[J].地质与资源,2007,16(2):112-115.
[9] 胡海涛,许贵森.论构造体系与地下水网络[J].水文地质工程地质,1980,7(3):1-5.
[10] 毛相义.遵义地区地下水控制条件分析及找水方向[J].贵州地质,1995,12(1):78-83.

相似文献/References:

[1]刘东,张健,付强.三江平原井灌区地下水人工回灌量测算[J].水土保持研究,2012,19(02):240.
　LIU Dong,ZHANG Jian,FU Qiang.Estimation of Groundwater Artificial Recharge Quantity in Area of Well Irrigation in Sanjiang Plain[J].Research of Soil and Water Conservation,2012,19(06):240.
[2]金绍兴,秦启文,范致豪,等.屏东平原之地下水经理[J].水土保持研究,1999,6(03):9.
　Shao-Hsing King,Chi-Van Chin,Chih-Hao Fan,et al.Groundwater Management in Pingtung Plain[J].Research of Soil and Water Conservation,1999,6(06):9.
[3]许中立,李正义.边坡稳定逆算分析法之应用探讨[J].水土保持研究,1999,6(03):80.
　Chung-LiHsu,Cheng-Yi Lee.The Application of Back Stability Analysis on Landslide Slope[J].Research of Soil and Water Conservation,1999,6(06):80.
[4]毛学森,刘昌明.太行山山前平原地下水变化趋势与农业持续发展[J].水土保持研究,2001,8(01):147.
　MAO Xuesen,LIU Changming.Ground Water Changing Trends and Agriculture Sustainable Development in Taihang Mountain-foot Plain of North China[J].Research of Soil and Water Conservation,2001,8(06):147.
[5]王恩志,王慧明,李昂,等.石门子水库近坝区渗漏与防渗分析[J].水土保持研究,2001,8(04):79.
　WANG En-zhi,WANG Hui-ming,LI Ang,et al.Analysis on Seepage and Anti-seepage Method of the Areas Near Shimenzi Reservoir[J].Research of Soil and Water Conservation,2001,8(06):79.
[6]唐小娟,吴普特.杨陵区地表水及地下水环境质量评价[J].水土保持研究,2002,9(02):135.
　TANG Xiao-juan,WU Pu-te.Environmental Quality Evaluation of Surface and Groundwater in Yangling[J].Research of Soil and Water Conservation,2002,9(06):135.
[7]罗芳,肖洪浪,齐善忠,等.额济纳三角洲地下水现状分析[J].水土保持研究,2005,12(01):56.
　LUO Fang,XIAO Hong-lang,QI Shan-zhong,et al.Changeable Characteristics of Groundwater and Salt in Erjina Oasis, Arid Northwestern China[J].Research of Soil and Water Conservation,2005,12(06):56.
[8]李海涛,许学工,肖笃宁.武威绿洲水资源利用分析[J].水土保持研究,2005,12(04):128.
　LI Hai-tao,XU Xue-gong,XIAO Du-ning.Analysis of Water Resources Utilization in Wuwei Oasis[J].Research of Soil and Water Conservation,2005,12(06):128.
[9]盛海洋,孟秋立,朱殿华,等.我国地下水开发利用中的水环境问题及其对策[J].水土保持研究,2006,13(01):51.
　SHENG Hai-yang,MENG Qiou-li,ZHU Dian-hua,et al.Environmental Problems of Underground Water Resources Development Use and Prevention and Control[J].Research of Soil and Water Conservation,2006,13(06):51.
[10]简武,许模,康小兵.西藏阿里地区地下水资源的形成分布特征[J].水土保持研究,2007,14(01):123.
　JIAN Wu,XU Mo,KANG Xiao-Bin.The Forming and Distribution Characteristic of the Groundwater Resource in Ali Area of Tibet[J].Research of Soil and Water Conservation,2007,14(06):123.

备注/Memo

收稿日期:2012-5-25;改回日期:2012-7-19。
作者简介:杨红(1987- ),女,四川遂宁人,在读研究生,主要从事环境水文地质研究工作.E-mail:739966214@qq.com

更新日期/Last Update: 1900-01-01