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[与地质成因性砷污染相关的饮用水供应]

[Drinking water supply with reference to geogenic arsenic contamination].

作者信息

Kevekordes S, Suchenwirth R, Gebel T, Demuth J, Dunkelberg H, Küntzel H

机构信息

Abteilung Allgemeine Hygiene und Umweltmedizin, Zentrum Umwelt- und Arbeitsmedizin, Universität Göttingen.

出版信息

Gesundheitswesen. 1998 Oct;60(10):576-9.

PMID:9844293
Abstract

Geogenic Arsenic in Drinking Water. Drinking water production of surface spring water in southern Lower Saxony (Niedersachsen, Germany) was reduced because of microbiological contaminations and unreliably variable water reserves. Surface spring water in general has a low arsenic content. As a consequence ground water has been increasingly used for drinking water. Thus, high geogenic concentrations of arsenic in the central "Buntsandstein" in southern Lower Saxony caused high arsenic contents in the groundwater. Under the regulation of the German Drinking Water Ordinance (1986) the limit for total arsenic (40 micrograms/l) was exceeded in 2% of 150 fountains, wells and sources in southern Lower Saxony. Because of the well-known cancerogenic potential of arsenic the limit for total arsenic in drinking water was reduced from 40 micrograms/l to 10 micrograms/l suspending the new standard value until January 1996. This regulation based on new calculations revealing a skin cancer risk of roughly 6:10,000 and a mortality risk of roughly 1:10(6) in respect of lifetime in case of arsenic concentrations of 10 micrograms As/l drinking water. After that limit change 40% of 150 wells and sources in southern Lower Saxony exceeded the arsenic limit of 10 micrograms/l drinking water. As a matter of fact, it became necessary for a large number of water supply works to eliminate arsenic from the drinking water by technical means or to dilute drinking water with high concentrations of arsenic.

摘要

饮用水中的地质源砷。德国下萨克森州南部的地表泉水因微生物污染和不稳定的水量储备而导致饮用水产量减少。一般来说,地表泉水的砷含量较低。因此,越来越多地使用地下水作为饮用水。这样一来,下萨克森州南部中部“斑砂岩”中高含量的地质源砷导致地下水中的砷含量升高。根据德国《饮用水条例》(1986年)的规定,在下萨克森州南部的150个喷泉、水井和水源中,有2%的总砷含量(40微克/升)超过了标准。由于砷具有众所周知的致癌潜力,饮用水中的总砷含量限制从40微克/升降至10微克/升,并将新标准值推迟到1996年1月实施。这一规定是基于新的计算结果,即当饮用水中砷浓度为10微克砷/升时,终生患皮肤癌的风险约为6:10000,死亡风险约为1:10(6)。在限值改变后,下萨克森州南部150口水井和水源中有40%的饮用水砷含量超过了10微克/升的限值。事实上,大量供水工程有必要通过技术手段去除饮用水中的砷,或者稀释高砷含量的饮用水。

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