地理学报 ›› 1989, Vol. 44 ›› Issue (2): 185-194.doi: 10.11821/xb198902007

• 论文 • 上一篇    下一篇

辽南石英岩板岩区基岩地下水富集规律及富水点位的研究

刘庆书   

  1. 辽宁师范大学地理系,大连
  • 收稿日期:1987-03-01 出版日期:1989-04-15 发布日期:1989-04-15

STUDY ON THE LAW OF ABUNDANT GROUNDWATER CATCHMENT AND THE LOCALITY OF GROUNDWATER ABUNDANCE IN THE QUARTZITE AND SLATE REGION OF SOUTHERN LIAONING PROVINCE

Liu Qingshu   

  1. Crography Dapartment of Liaoning Normal University, Dalian
  • Received:1987-03-01 Online:1989-04-15 Published:1989-04-15

摘要: 文章从辽东半岛南部石英岩板岩区地下水富水不均的特点出发,论述了基岩地下水富集规律:贮存在蓄水构造中,汇集在集水网络里,运移富集在充水脉络交接、结点处。进一步对水文物探各类富水曲线进行了分类,概括富水异常特征。结合多年实际勘测成果,论证了依据“结点异常”确定富水点位。

关键词: 辽南石英岩板岩地区, 地下水, 集水网络, 充水脉络, 富水曲线类型, 富水部位确定, 格局

Abstract: This paper mainly discusses the law of abundant groundwater catchment and studies thedetermination of the locality of water abundance in the Quartzite and Slate region of SounthernLiaoning Province.The Localities of groundwater abundance in this region is unevenly distributed. Groun-dwater is stored in water-collectiong structure, aggregated in catchment network and abundantlvcollected in water-filled veins. Water-filled wins mainly form a pattern of double cross trel-dis-work. The best abundance positions of water are found at the joints of several water-filledveins.From the viewpoint of hydrography, wlth reference to many years’ achievement of surveyby means of composite profiling, electrode 5, audio-frequency and electrical sounding in theQuartzite and Slate region the groundwater abundance curve of water-filled veins can be clas-sified into many types. By making analyses of the characteristics of every such type, and byindicating the marks of the water aggregation localoty, We can effectively prove the deman-ded outcome.

Key words: The Quartzite and Slate region in Southern Liaoning Province, Groundwa-ter, water-collecting network, Water-filled veins, The types of abundance water curves, Thelocality of groundwater abundance, Pattern