Jones Huw, Visoottiviseth Pornsawan, Bux M Khoda, Födényi Rita, Kováts Nora, Borbély Gábor, Galbács Zoltán
Institute of Social and Health Research, School of Health and Social Sciences, Middlesex University, The Burroughs, London NW4 4BT, UK.
Rev Environ Contam Toxicol. 2008;197:163-87. doi: 10.1007/978-0-387-79284-2_6.
Although arsenic contamination in the three countries described herein differs, a number of common themes emerge. In each country, the presence of arsenic is both long term and of geological origin. Moreover, in each of these countries, arsenic was only recently discovered to be a potential public health problem, having been first formally recognized in the 1980s or 1990s. In Bangledesh, exposure of the public to arsenic arose as a result of the search for microbially safe drinking water; this search resulted in the sinking of tube wells into aquifers. In Hungary, the natural bedrock geology was responsible for contamination of aquifer water. The genesis of arsenic contamination in Thailand arose primarily from small-scale alluvial mining activities, which mobilized geologically bound arsenic. Because of the complex chemistry of arsenic, and variability in where it is found and how it is bound, multiple mitigation methods must be considered for mitigating episodes of environmental contamination. The Ron Phibun region of Thailand has a 100-yr history of tin mining. A geological survey of the region was conducted in the mid-1990s by the Department of Mineral Resources and Department of Industry of Thailand, and was supported by the British Geological Society. Skin cancer in Thailand was first reported in 1987, in the southern part of the country; among other symptoms observed, there was evidence of IQ diminutions among the population. Arsenic water levels to 9,000 pg/L were reported; such levels are substantially above any guideline levels. A long-term plan to mitigate arsenic contamination was devised in 1998-2000. The plan involved removal of arsenic-contaminated land and improved management of mining wastes. However, at $22 million, the cost was deemed prohibitive for the regional Thai economy. An alternative solution of providing pipeline drinking water to the exposed population was also unsuccessful, either because arsenic contamination levels did not fall sufficiently, or because the quantity of water delivered to the population was inadequate. Membrane technology treatment, using reverse osmosis, was successful during the summer months, but membrane filter replacement costs prevented wide implementation. Less expensive options, such as the use of rainwater jars, were feasible in areas with adequate rainfall. Algae and phytoremediation and wetland treatment of surface waters were useful, but the waste disposal necessitated by such treatments reduces acceptance. The development and population growth in Bangladesh from 1980 to 2000 resulted in improved water quality, primarily because of the drilling of about 10 million tube wells. The unintended consequence of this action resulted in exposure of about 40 million people to toxic levels of arsenic, which was a natural contaminant of the aquifers. Numerous remediation strategies have been implemented to deal with this problem, including the use of dug wells, pond sand filters, household filters, rainwater harvesting, deep tube wells, chemical-based options, and construction of village piped water supplies. Varying levels of success, which is largely dependent on local resources and conditions, have been reported for the different mitigation methodologies. Although Hungary has already invested huge sums of money to reduce arsenic levels in the most contaminated counties, further investments are needed to comply with the strict European threshold value. The fact that arsenic contamination is a natural ongoing process creates a barrier to long-term success. At present, the most appropriate option for securing safe water for drinking and cooking is treatment of water at the tap. Both adsorption and membrane filtration are efficient methods to remove arsenic from drinking water. The presence of contaminants other than arsenic may also require dual or multiple removal processes. Decision makers, as is common, must consider not only removal efficiency but also operating and investment costs of an operation.
尽管本文所述三个国家的砷污染情况各不相同,但仍出现了一些共同主题。在每个国家,砷的存在都是长期的且源于地质因素。此外,在这些国家中,砷直到最近才被发现是一个潜在的公共卫生问题,最早在20世纪80年代或90年代才得到正式确认。在孟加拉国,公众接触砷是由于寻找微生物安全的饮用水;这一寻找导致了管井打入含水层。在匈牙利,天然基岩地质导致了含水层水的污染。泰国砷污染的成因主要源于小规模的冲积采矿活动,这些活动使地质结合的砷得以释放。由于砷的化学性质复杂,以及其存在位置和结合方式的多变性,必须考虑多种缓解方法来减轻环境污染事件。泰国的攀牙府地区有100年的锡矿开采历史。20世纪90年代中期,泰国矿产资源部和工业部对该地区进行了地质调查,并得到了英国地质学会的支持。泰国于1987年首次在该国南部报告了皮肤癌;在观察到的其他症状中,有证据表明当地人群的智商有所下降。报告的砷含量高达9000皮克/升;这一水平大大高于任何指导标准。1998 - 2000年制定了一项减轻砷污染的长期计划。该计划包括清除受砷污染的土地以及改善采矿废物管理。然而,由于成本高达2200万美元,对于泰国地方经济来说被认为过高而无法承受。为受影响人群提供管道饮用水的替代解决方案也未成功,要么是因为砷污染水平没有充分降低,要么是因为供应给人群的水量不足。使用反渗透的膜技术处理在夏季取得了成功,但膜过滤器的更换成本阻碍了其广泛应用。在降雨量充足的地区,使用雨水罐等成本较低的选择是可行的。藻类和植物修复以及地表水的湿地处理很有用,但此类处理所需的废物处置降低了其可接受性。1980年至2000年期间,孟加拉国的发展和人口增长使水质得到改善,这主要归功于大约1000万口管井的钻探。这一行动的意外后果是约4000万人接触到有毒水平的砷,而砷是含水层的天然污染物。为应对这一问题已实施了多种修复策略,包括使用挖井、池塘砂滤器、家用过滤器、雨水收集、深管井、基于化学的方法以及建设村庄管道供水系统。不同缓解方法的成功程度各不相同,这在很大程度上取决于当地资源和条件。尽管匈牙利已经投入巨额资金来降低污染最严重县的砷含量,但仍需要进一步投资以符合严格的欧洲阈值。砷污染是一个持续的自然过程这一事实为长期成功设置了障碍。目前,确保安全饮用水和烹饪用水的最合适选择是对自来水进行处理。吸附和膜过滤都是从饮用水中去除砷的有效方法。除砷之外的其他污染物的存在可能还需要双重或多重去除过程。与通常情况一样,决策者不仅必须考虑去除效率,还必须考虑运营的运营成本和投资成本。