对低山丘陵区基岩裂隙水富存部位的分析

摘要

低山丘陵区基岩裂隙水分布埋藏极不均一，含水层分布在水平和垂直方向上异差性大，涌水量大小相差悬殊。富存形式往往呈点状、线状、面状赋存于岩石的裂隙中。本文采用力学性质分析，构造形迹分析，物探方法测量，确定基岩裂隙水的富存部位，以北票地区作为研究区域，定量分析北票低山丘陵区基岩裂隙水富存的差异性。研究成果为低山丘陵区开发基岩裂隙水提供重要参考价值。%The hilly region buried bedrock fissure water extremely uneven distribution ,the distribution of the aquifer in the horizontal and vertical difference between different large size differences between water inflow. Rich deposit in the form of often spotty,linear,planar occur in rock fissures.In this paper,the analysis of me-chanical properties,structural features analysis,geophysical methods to measure to determine the bedrock fis-sure water-rich deposit area,north of the votes in the region as a study area,quantitative analysis Beipiao bedrock fissure water-rich hilly area differences exist.Research for the development of the hilly area of bedrock fissure water provide important reference value.