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。
:
This paper mainly discusses the law of abundant groundwater catchment and studies the
determination of the locality of water abundance in the Quartzite and Slate region of Sounthern
Liaoning 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 abundantlv
collected 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-filled
veins.
From the viewpoint of hydrography, wlth reference to many years' achievement of survey
by means of composite profiling, electrode 5, audio-frequency and electrical sounding in the
Quartzite 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 by
indicating the marks of the water aggregation localoty, We can effectively prove the deman-
ded outcome.
出处
《地理学报》
EI
CSSCI
CSCD
北大核心
1989年第2期185-194,共10页
Acta Geographica Sinica
关键词
基岩
地下水
富集
石类岩
板岩
: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
