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长期居住的村镇土壤中铅的污染及口腔生物可给性

Pollution and Oral Bioaccessibility of Pb in Soils of Villages and Cities with a Long Habitation History.

作者信息

Walraven Nikolaj, Bakker Martine, van Os Bertil, Klaver Gerard, Middelburg Jack Jacobus, Davies Gareth

机构信息

GeoConnect, Meester Dekkerstraat 4, Castricum 1901 PV, The Netherlands.

Rijksinstituut voor Volksgezondheid en Milieu (RIVM), P.O. Box 1, Bilthoven 3720 BA, The Netherlands.

出版信息

Int J Environ Res Public Health. 2016 Feb 17;13(2):221. doi: 10.3390/ijerph13020221.

Abstract

The Dutch cities Utrecht and Wijk bij Duurstede were founded by the Romans around 50 B.C. and the village Fijnaart and Graft-De Rijp around 1600 A.D. The soils of these villages are polluted with Pb (up to ~5000 mg/kg). Lead isotope ratios were used to trace the sources of Pb pollution in the urban soils. In ~75% of the urban soils the source of the Pb pollution was a mixture of glazed potsherd, sherds of glazed roof tiles, building remnants (Pb sheets), metal slag, Pb-based paint flakes and coal ashes. These anthropogenic Pb sources most likely entered the urban soils due to historical smelting activities, renovation and demolition of houses, disposal of coal ashes and raising and fertilization of land with city waste. Since many houses still contain Pb-based building materials, careless renovation or demolition can cause new or more extensive Pb pollution in urban soils. In ~25% of the studied urban topsoils, Pb isotope compositions suggest Pb pollution was caused by incinerator ash and/or gasoline Pb suggesting atmospheric deposition as the major source. The bioaccessible Pb fraction of 14 selected urban soils was determined with an in vitro test and varied from 16% to 82% of total Pb. The bioaccessibility appears related to the chemical composition and grain size of the primary Pb phases and pollution age. Risk assessment based on the in vitro test results imply that risk to children may be underestimated in ~90% of the studied sample sites (13 out of 14).

摘要

荷兰城市乌得勒支和杜尔斯泰德附近的维克于公元前50年左右由罗马人建立,而菲耶诺尔特村和格拉夫-德里普村则于公元1600年左右形成。这些村庄的土壤受到铅污染(含量高达约5000毫克/千克)。铅同位素比率被用于追踪城市土壤中铅污染的来源。在约75%的城市土壤中,铅污染的来源是釉面陶片、釉面屋顶瓦片碎片、建筑遗迹(铅板)、金属矿渣、铅基漆片和煤灰的混合物。这些人为铅源很可能由于历史上的冶炼活动、房屋翻新和拆除、煤灰处理以及用城市垃圾进行土地堆肥和施肥而进入城市土壤。由于许多房屋仍含有铅基建筑材料,粗心的翻新或拆除可能会在城市土壤中造成新的或更广泛的铅污染。在约25%的研究城市表层土壤中,铅同位素组成表明铅污染是由焚烧炉灰和/或汽油铅造成的,这表明大气沉降是主要来源。通过体外试验测定了14个选定城市土壤中生物可利用铅的含量,其占总铅量的比例从16%到82%不等。生物可及性似乎与主要铅相的化学成分和粒度以及污染年代有关。基于体外试验结果的风险评估表明,在约90%的研究样本地点(14个中的13个),对儿童的风险可能被低估。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4596/4772241/0b53f8ed0ca3/ijerph-13-00221-g001.jpg

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