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南阳盆地浅层地下水中氟的分带性分布特点及其成因

宁立波 卜新峰 莫春雷

水资源保护2012,Vol.28Issue(6):66-69,4.
水资源保护2012,Vol.28Issue(6):66-69,4.DOI:10.3969/j.issn.1004-6933.2012.06.015

南阳盆地浅层地下水中氟的分带性分布特点及其成因

Zonation characteristics of fluorine and its causes in shallow groundwater in Nanyang Basin

宁立波 1卜新峰 1莫春雷1

作者信息

  • 1. 中国地质大学(武汉)环境学院,湖北武汉430074
  • 折叠

摘要

Abstract

The characteristics of fluorine distribution in shallow groundwater in the Nanyang Basin were analyzed. The results show that the fluorine concentration increases gradually from mountainous areas to plain areas, and increases initially and then decreases from the upper reaches to the lower reaches of the river. Based on the hydrogeological conditions of the study area, the groundwater flow system theory was used to analyze the causes of the zonation. The conclusion is that the spatial heterogeneity of the groundwater flow system from the recharge area to the discharge area is the main cause of the zonation.

关键词

地下水//分带性分布/地下水流动系统/南阳盆地

Key words

groundwater/ fluorine/ zonation/ groundwater flow system/ Nanyang Basin

分类

天文与地球科学

引用本文复制引用

宁立波,卜新峰,莫春雷..南阳盆地浅层地下水中氟的分带性分布特点及其成因[J].水资源保护,2012,28(6):66-69,4.

基金项目

国家自然科学基金(40802057) (40802057)

水资源保护

OACSTPCD

1004-6933

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