1958年8月,我队在黄骅盐埸供水勘测中,采用了泥浆鑽探和分层观测各含水层的静止水位、水温及水质的方法,并获得初步成功。该区高矿化水分界据几个深孔资料均住200来深左右,因此,决定在200米以上采用分层观测方法,确定地下水矿化度垂直变化规律和取水深度及隔离上部高矿化水的方法。 In August 1958, our team employed mud drilling and stratified observation of the still water level, water temperature and water quality of aquifers in the investigation of the salt water supply in Huanghua, and achieved initial success. According to the data of several deep-hole pores in the area with high mineralization, the area of ​​high mineralization has lived at a depth of about 200. Therefore, it is decided to adopt a stratified observation method above 200 meters to determine the vertical variation of groundwater salinity and the depth of water intake and to isolate the upper mineralization Water method.