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陕西秦岭以北地区高氟地下水的成因与防治研究
引用本文:王德耀. 陕西秦岭以北地区高氟地下水的成因与防治研究[J]. 陕西师范大学学报(自然科学版), 2004, 32(3): 112-115
作者姓名:王德耀
作者单位:陕西省地质矿产局区域地质矿产研究院,陕西咸阳712000
基金项目:国家自然科学基金资助项目(40271052)
摘    要:根据陕西秦岭以北地区高氟地下水分布状况,分析了该地区高氟地下水的分布规律.结果表明,高氟地下水的形成原因主要是受地层岩土、地貌、气候、水文地球化学和地质构造等条件的制约.提出了防氟改水措施是以在陕北打窖、关中打井为主,其次伴以理化除氟等方法.

关 键 词:高氟  改水  防治研究  理化  地区  状况  打井  西秦岭  地下水  水文地球化学
文章编号:1672-4291(2004)03-0112-04
修稿时间:2003-04-16

Formation and control of high-fluoride underground water in northern area of Qinling Mountains of Shaanxi
WANG De-yao. Formation and control of high-fluoride underground water in northern area of Qinling Mountains of Shaanxi[J]. Journal of Shaanxi Normal University: Nat Sci Ed, 2004, 32(3): 112-115
Authors:WANG De-yao
Abstract:Based on the analysis of distributing rules of the water, conclusion is drawn that the formation of the high-fluorine underground water in the northern area of Qinling Mountains of Shaanxi mainly depends on conditions of the strata, rock and soil, geomorphic, climate and hydro-geochemistry, geological structural etc. furthermore, digging water-storing cellar in northern Shaanxi and digging wells in Guanzhong area are put forward as major measures to purify fluoride water, which can be accompanied by physical-chemical methods as well.
Keywords:high-fluoride underground water  distributing  formation
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