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山东沾化滨海地区浅层地下卤水矿层特征及形成条件
引用本文:张新文,胡松涛,胡彩萍,张学斌.山东沾化滨海地区浅层地下卤水矿层特征及形成条件[J].山东国土资源,2009,25(10):28-31.
作者姓名:张新文  胡松涛  胡彩萍  张学斌
作者单位:1. 山东省第一地质矿产勘查院,山东,济南,250014
2. 山东省地矿工程勘察院,山东,济南,250014
摘    要:山东沾化滨海地区地下卤水为古浓缩海水封存而成。浅层地下卤水主要赋存在40 m深度以上的粉砂和粉土层中,垂向上分为2个矿层,总厚度9.9-33.7 m,矿化度50.0-99.7 g/L,水位埋深1.2-4.3 m,单位出水量10.42-58.94 m3/(d.m),富水性中等,动态较为稳定。卤水开发利用应合理规划,避免资源浪费,注重综合利用和环境保护。

关 键 词:卤水  浅层地下水  形成条件  山东沾化

Strata Characteristics and Forming Condition of Shallow Underground Brine in Coastal Areas of Zhanhua County in Shandong Province
Zhang Xinwen,Hu Songtao,Hu Caiping and Zhang Xuebin.Strata Characteristics and Forming Condition of Shallow Underground Brine in Coastal Areas of Zhanhua County in Shandong Province[J].Land and Resources in SHANDONG Province,2009,25(10):28-31.
Authors:Zhang Xinwen  Hu Songtao  Hu Caiping and Zhang Xuebin
Abstract:Underground brine in coastal areas of Zhanhua county is formed by sealing ancient concentrated sea water. Shallow underground brine is mainly existed in silt and powder layers with the depth of 40m. It is divided into two strata in the vertical direction.
Keywords:Brine  underground water in shallow part  forming condition  Zhanhua in Shandong province
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