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黄河下游鲁北平原地下水砷浓度空间变异特征与成因

刘春华 张光辉 杨丽芝 卫政润 刘中业 陈相霖 张卓

地球学报Issue(4):470-476,7.
地球学报Issue(4):470-476,7.DOI:10.3975/cagsb.2013.04.10

黄河下游鲁北平原地下水砷浓度空间变异特征与成因

Variation Characteristics and Causes of Arsenic Concentration in Shallow Groundwater of Northern Shandong Plain in the Lower Reaches of the Yellow River

刘春华 1张光辉 2杨丽芝 1卫政润 3刘中业 3陈相霖 3张卓4

作者信息

  • 1. 中国地质科学院水文地质环境地质研究所,河北石家庄 050061
  • 2. 山东省地质调查院,山东济南 250013
  • 3. 山东省地质调查院,山东济南 250013
  • 4. 中国地质大学 武汉地球科学学院,湖北武汉 430074
  • 折叠

摘要

Abstract

Based on the inorganic analysis of 1092 groundwater samples collected from 2006 to 2009 in Yellow River Plain and using the method of geo-statistics, this paper discussed the spatial variation and pollution of arsenic in shallow groundwater under the influence of human activities in this region. 26.65% of the samples exceeded the Drinking Water Standard in arsenic concentration, and the area surpassing the set standard accounted for 17.3% of the total area. The degree of dispersion of shallow groundwater was high and the coefficient of variation was over 100%. The spatial distribution of arsenic was anisotropic. The relationship between arsenic distribution and groundwater flow was not close, and the native condition and impact of pollution sources seem to be the main reasons. 7%of shallow groundwater samples suffered from arsenic pollution from human activity, and 18% of the arsenic polluted samples were caused by livestock breeding farms. The detection rate and exceeding rate of samples from livestock breeding farms was 2 times that of the whole study area. The arsenic pollution source included the animal waste from the scattered livestock breeding farms, the application of arsenic-bearing pesticides, and the discharge of industrial wastewater.

关键词

黄河下游/冲积平原/浅层地下水/砷污染/地统计学/空间变异/成因

Key words

Lower Reaches of Yellow River/alluvial plain/shallow groundwater/arsenic pollution/geostatistics/spatial variability/causes

分类

资源环境

引用本文复制引用

刘春华,张光辉,杨丽芝,卫政润,刘中业,陈相霖,张卓..黄河下游鲁北平原地下水砷浓度空间变异特征与成因[J].地球学报,2013,(4):470-476,7.

基金项目

本文由国家自然科学基金项目(编号:41172214)和中国地质调查局地质调查项目(编号:1212010634603)联合资助。 (编号:41172214)

地球学报

OA北大核心CSCDCSTPCD

1006-3021

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