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东江流域河水电导率形成机制

李姗迟 郑雄波 高全洲 陶贞 解晨骥 刘龙海

中山大学学报(自然科学版)2013,Vol.52Issue(1):142-146,5.
中山大学学报(自然科学版)2013,Vol.52Issue(1):142-146,5.

东江流域河水电导率形成机制

Mechanism of River Electrical Conductivity in the Dongjiang River Basin

李姗迟 1郑雄波 1高全洲 1陶贞 2解晨骥 1刘龙海1

作者信息

  • 1. 中山大学地理科学与规划学院∥广东省城市化与地理环境空间模拟重点实验室,广东广州 510275
  • 2. 广东省地质过程与矿产资源探查重点实验室,广东广州 510275
  • 折叠

摘要

Abstract

Based on the hydrochemical data of water samples from the Dongjiang River Basin in dry and wet seasons, the mechanism of river electrical conductivity ( EC ) is considered. The results show that EC in the Dongjiang River Basin is 85. 3μS/cm in January and 87. 7μS/cm in July. The share of weathering conductivity ( Cw ) , seasalt conductivity ( Cs) and anthropogenic conductivity ( Ch ) is 46. 4% , 19. 6% and 33. 9% respectively. It indicates that chemical weathering is the main contributing factor for EC in the Dongjiang River Basin. The humanity interference cannot be neglected, while the seasalt settlement has certain effects on the hydrochemistry. Furthermore, the nonparametric statistics methods and spatial analysis are used to prove that the geographic features (lithology, landform, soil, vegetation and human activities) have played an important role in the EC mechanism.

关键词

河流水化学/电导率/化学风化/人类活动/东江流域

Key words

hydrochemistry/ electrical conductivity/ chemical weathering/ human activities/ the Dongjiang River Basin

分类

天文与地球科学

引用本文复制引用

李姗迟,郑雄波,高全洲,陶贞,解晨骥,刘龙海..东江流域河水电导率形成机制[J].中山大学学报(自然科学版),2013,52(1):142-146,5.

基金项目

国家自然科学基金资助项目(41071054 ()

40871143) ()

中央高校基本科研业务费专项基金资助项目(11lgjc13,11lgjc10) (11lgjc13,11lgjc10)

中山大学学报(自然科学版)

OA北大核心CSCDCSTPCD

0529-6579

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