茅草铺灰岩富水规律分析
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摘要
以黔北安场复向斜中茅草铺组灰岩分布区的地形地貌、地层岩性、地质构造、岩溶发育等阐述地下水的赋存和运移规律,以及地下水资源的合理开发利用。通过此含水岩组中钻井取水的实践,发现同一含水岩组地层因地貌单元、构造部位、岩溶发育程度不一致时,其富水程度也有差异。不论在何种类型构造带中定井,均应以地质分析与物探方法来综合确定,从而提高钻井取水的可靠性。
In light of the research on topography,lithological characters,geological structure and karst development in the Maocao Group limestone area,Anchang multiple trough bend,north Guizhou,occurrence and movement and reasonable development and utilization of the groundwater are discussed.By hole-drilling and water pumping,it is found that the water abundance differs at the same water bearing group due to the differences of topographical units,geological structure position and karst development.No matter in what kind of geological structure a well is drilled,it is determined by comprehensive geological analysis and geophysical exploration so as to heighten the reliability of drilling and water pumping.
In light of the research on topography,lithological characters,geological structure and karst development in the Maocao Group limestone area,Anchang multiple trough bend,north Guizhou,occurrence and movement and reasonable development and utilization of the groundwater are discussed.By hole-drilling and water pumping,it is found that the water abundance differs at the same water bearing group due to the differences of topographical units,geological structure position and karst development.No matter in what kind of geological structure a well is drilled,it is determined by comprehensive geological analysis and geophysical exploration so as to heighten the reliability of drilling and water pumping.
引文
[1]熊剑飞.贵州遵义三迭纪茅草铺灰岩Tiroliotes的发现[J].地质沦评,1964(04):321.
[2]尹赞勋,秦鼎,谌义睿.贵州遵义县东乡之三叠纪地层[J].地质评论,1944(03):313-338.
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[5]卢耀如,张凤娥,刘长礼,童国榜,张云.中国典型地区岩溶水资源及其生态水文特性[J].地球学报,2006,27(05):393-402.
[6]杨明德.论贵州岩溶水赋存的地貌规律性[J].中国岩溶,1982,1(02):81-91.
[7]杨明德.岩溶地貌环境评价(以贵州岩溶地区为例)[J].环保科技,1983(Z1):22-28.
[8]王宇.西南岩溶地区岩溶水系统分类、特征及勘查评价要点[J].中国岩溶,2002,21(02):114-119.
[9]单海平,邓军.我国西南地区岩溶水资源的基本特征及其和谐利用对策[J].中国岩溶,2006,25(04):324-329.
[10]路洪海,章程.中国西南地区岩溶水资源的特点及可持续利用对策[J].西华师范大学学报:自然科学版,2006,27(02):139-142.
[11]熊道锟,傅荣华.岩溶发育强度垂直分带方法[J].岩土工程技术,2005,19(03):113-117.
[2]尹赞勋,秦鼎,谌义睿.贵州遵义县东乡之三叠纪地层[J].地质评论,1944(03):313-338.
[3]B.K.沃洛布耶夫,周叔良.露天矿含水岩层的爆破工艺[J].国外金属矿采矿,1987(03):40-49.
[4]张钦朋.张夏灰岩富水规律的探讨[J].水利水电技术,1994(08):34-39.
[5]卢耀如,张凤娥,刘长礼,童国榜,张云.中国典型地区岩溶水资源及其生态水文特性[J].地球学报,2006,27(05):393-402.
[6]杨明德.论贵州岩溶水赋存的地貌规律性[J].中国岩溶,1982,1(02):81-91.
[7]杨明德.岩溶地貌环境评价(以贵州岩溶地区为例)[J].环保科技,1983(Z1):22-28.
[8]王宇.西南岩溶地区岩溶水系统分类、特征及勘查评价要点[J].中国岩溶,2002,21(02):114-119.
[9]单海平,邓军.我国西南地区岩溶水资源的基本特征及其和谐利用对策[J].中国岩溶,2006,25(04):324-329.
[10]路洪海,章程.中国西南地区岩溶水资源的特点及可持续利用对策[J].西华师范大学学报:自然科学版,2006,27(02):139-142.
[11]熊道锟,傅荣华.岩溶发育强度垂直分带方法[J].岩土工程技术,2005,19(03):113-117.