大庆市地下水化学特征  

Chemical Characteristics of Groundwater in Daqing

作　　者：刘文忠[1] 王立勇[1] 陈兴国[1] 张旭临[1] 李楠[1] 

机构地区：[1]黑龙江省904水文地质工程地质勘察院,黑龙江双城150100

出　　处：《黑龙江水专学报》2009年第1期113-115,共3页Journal of Heilongjiang Hydraulic Engineering College

基　　金：黑龙江省水利厅项目(HSKY2005-16);黑龙江省教育厅科技项目(11511298)

摘　　要：大庆市地下水由于受地形地貌、水文气象和水文地质条件的影响,属于高铁锰、高溶解性固体、低氟的地下水。东部地区的水好于西部,榆树林油田和八厂靠近榆树林油田地区的地下水属于较好的水,其它地区均属于较差或极差的水,工业锅炉用水大多数为锅垢或很多、具有软沉淀物的、起泡或半起泡的、非腐蚀性的水。Groundwater of Daqing has the landform, hydrological and meteorological and hydrological geology condition. The high Fe and Mn, solid solubility, low fluorous features the groundwater of this regional. The quality of water in the eastern region is better than the western part. The groundwater of Yushulin oil field and eight factory area near Yushulin oil field is the better water, other areas are poor or extremely poor one, most of water for industrial boiler is the soft sediments, and bubbles or half bubbles, corrosive water.

关 键 词：地下水 化学特征 大庆市 

分 类 号：P541.12[天文地球—构造地质学]