摘要
依据大量地下水化学分析资料 ,揭示了咸阳城区高氟地下水呈带状分布的规律和水化学特征 ,并从岩土条件、地貌、水文地球化学、气候及地质构造等方面分析了高氟地下水的形成因素。认为本区高氟地下水的形成是多种因素共同作用的结果 ,其中岩土、气候、地貌条件及水文地球化学环境是咸阳城区地下水中氟离子背景含量的主要影响因素 ,而隐伏断裂构造形成的深层高氟地下温水运移通道 。
The hydrochemical characteristics and zonal distribution of groundwater with high fluorine in Xianyang city are revealed according to the data from the chemical analysis of the groundwater,and the formation of the groundwater is discussed through the conditions of rock and soil,geomorphy,hydrogeochemistry,weather and geological structure.Among them,the conditions of rock,soil and weather,geography and hydrogeochemistry environment are the main influencing factors to decide the background contain of the fluorine of the groundwater in Xianyang area,but the geological structure is the decision factor that affects the zonal distribution of the groundwater with high fluorine in the area.
出处
《工程勘察》
CSCD
北大核心
2004年第4期31-34,共4页
Geotechnical Investigation & Surveying
基金
陕西省教育厅专项科研基金资助项目 (0 2JK2 0 0 )
关键词
高氟地下水
分布成因
咸阳城区
bearing groundwater with high fluorine
distribution and formation
Xianyang area
