Podgorski Joel E, Eqani Syed Ali Musstjab Akber Shah, Khanam Tasawar, Ullah Rizwan, Shen Heqing, Berg Michael
Eawag, Swiss Federal Institute of Aquatic Science and Technology, Department Water Resources and Drinking Water, 8600 Dübendorf, Switzerland.
Public Health and Environment Division, Department of Biosciences, COMSATS Institute of Information Technology, Islamabad, Pakistan.
Sci Adv. 2017 Aug 23;3(8):e1700935. doi: 10.1126/sciadv.1700935. eCollection 2017 Aug.
Arsenic-contaminated aquifers are currently estimated to affect ~150 million people around the world. However, the full extent of the problem remains elusive. This is also the case in Pakistan, where previous studies focused on isolated areas. Using a new data set of nearly 1200 groundwater quality samples throughout Pakistan, we have created state-of-the-art hazard and risk maps of arsenic-contaminated groundwater for thresholds of 10 and 50 μg/liter. Logistic regression analysis was used with 1000 iterations, where surface slope, geology, and soil parameters were major predictor variables. The hazard model indicates that much of the Indus Plain is likely to have elevated arsenic concentrations, although the rest of the country is mostly safe. Unlike other arsenic-contaminated areas of Asia, the arsenic release process in the arid Indus Plain appears to be dominated by elevated-pH dissolution, resulting from alkaline topsoil and extensive irrigation of unconfined aquifers, although pockets of reductive dissolution are also present. We estimate that approximately 50 million to 60 million people use groundwater within the area at risk, with hot spots around Lahore and Hyderabad. This number is alarmingly high and demonstrates the urgent need for verification and testing of all drinking water wells in the Indus Plain, followed by appropriate mitigation measures.
目前估计,受砷污染的含水层影响着全球约1.5亿人。然而,该问题的全貌仍不明朗。巴基斯坦的情况也是如此,此前的研究集中在孤立地区。利用巴基斯坦各地近1200个地下水质量样本的新数据集,我们绘制了砷污染地下水的最新危害和风险地图,阈值分别为10微克/升和50微克/升。使用逻辑回归分析进行了1000次迭代,其中地表坡度、地质和土壤参数是主要预测变量。危害模型表明,印度河平原的大部分地区可能砷浓度升高,不过该国其他地区大多是安全的。与亚洲其他砷污染地区不同,干旱的印度河平原的砷释放过程似乎主要由高pH值溶解主导,这是由碱性表土和无压含水层的广泛灌溉导致的,尽管也存在一些还原溶解的区域。我们估计,在风险区域内约有5000万至6000万人使用地下水,拉合尔和海得拉巴周围存在热点地区。这个数字高得惊人,表明迫切需要对印度河平原的所有饮用水井进行核查和检测,随后采取适当的缓解措施。