Farooqi Abida, Masuda Harue, Firdous Nousheen
Department of Geosciences, Osaka City University, 3-3-138, Sugimoto, Osaka 558-8585, Japan.
Environ Pollut. 2007 Feb;145(3):839-49. doi: 10.1016/j.envpol.2006.05.007. Epub 2006 Jun 13.
The present study is the first attempt to put forward possible sources of As, F- and SO4(2-) contaminated groundwater in the Kalalanwala area, Punjab, Pakistan. Five rainwater and 24 groundwater samples from three different depths were analyzed. Shallow groundwater from 24 to 27 m depth contained high F- (2.47-21.1mg/L), while the groundwater samples from the deeper depth were free from fluoride contamination. All groundwater samples contained high As (32-1900 microg/L), in excess of WHO drinking water standards. The SO4(2-) ranges from 110 to 1550 mg/L. Delta34S data indicate three sources for SO4(2-) air pollutants (5.5-5.7 per thousand), fertilizers (4.8 per thousand), and household waste (7.0 per thousand). Our important finding is the presence of SO4(2-), As and F- in rainwater, indicating the contribution of these elements from air pollution. We propose that pollutants originate, in part, from coal combusted at brick factories and were mobilized promotionally by the alkaline nature of the local groundwater.
本研究首次尝试提出巴基斯坦旁遮普省卡拉兰瓦拉地区砷、氟化物和硫酸根离子污染地下水的可能来源。分析了来自三个不同深度的5个雨水样本和24个地下水样本。深度在24至27米的浅层地下水中氟化物含量较高(2.47 - 21.1毫克/升),而深层地下水样本未受氟化物污染。所有地下水样本中的砷含量都很高(32 - 1900微克/升),超过了世界卫生组织的饮用水标准。硫酸根离子含量在110至1550毫克/升之间。δ34S数据表明硫酸根离子有三个来源:空气污染物(5.5 - 5.7‰)、化肥(4.8‰)和生活垃圾(7.0‰)。我们的重要发现是雨水中存在硫酸根离子、砷和氟化物,表明这些元素来自空气污染。我们认为污染物部分源自砖厂燃烧的煤炭,并因当地地下水的碱性而被促进迁移。