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衰老对中国一些典型土壤中镉的生物可及性和形态分布的影响。

The effect of ageing on the bioaccessibility and fractionation of cadmium in some typical soils of China.

作者信息

Tang Xiang-Yu, Zhu Yong-Guan, Cui Yan-Shan, Duan Jing, Tang Lily

机构信息

Department of Soil Environmental Sciences, Research Center for Eco-Environmental Sciences, the Chinese Academy of Sciences, Beijing 100085, PR China.

出版信息

Environ Int. 2006 Jul;32(5):682-9. doi: 10.1016/j.envint.2006.03.003. Epub 2006 Apr 17.

Abstract

Ingestion of contaminated soil has been recognized as an important exposure pathway of cadmium (Cd) for humans, especially for children through outdoor hand-to-mouth activities. The effect of ageing process following the input of Cd into soil on the bioaccessibility of Cd in five typical soils of China was investigated using physiologically based in vitro test in this study. A sequential extraction procedure was employed with attempt to identify the bioaccessible fraction(s) of Cd in soils. The bioaccessibility of Cd in strongly acidic (approximately pH 4.5) soils reached nearly steady levels (76.5-76.9% and 52.0-52.6% in the gastric and small intestinal phases, respectively) after a sharp decline in the first week of ageing. In contrast, the bioaccessibility of Cd in higher pH (>6.0) soils was found to be much lower (53.3-72.7% and 29.9-43.4% in gastric and small intestinal phases, respectively) and took 2 weeks of ageing to reach steady levels. The freshly spiked Cd was more labile than native Cd. The main proportion of spiked Cd was found in exchangeable Cd which was higher in strongly acidic soils (68.6-71.8%) than in higher pH soils (53.4-61.4%) at day 120 after a sharp decline to the nearly steady state in the first 1 and 2 weeks, respectively. Significant correlations between Cd bioaccessibility and either water soluble and exchangeable Cd individually, or the sum of water soluble and exchangeable Cd throughout the incubation period for all soils, indicate that these forms of Cd are likely to constitute the main proportion of bioaccessible Cd in soils.

摘要

摄入受污染土壤已被公认为是人类镉(Cd)暴露的重要途径,尤其是儿童通过户外手口活动接触镉。本研究采用基于生理学的体外试验,研究了镉输入土壤后的老化过程对中国五种典型土壤中镉生物可及性的影响。采用连续提取程序试图确定土壤中镉的生物可及部分。在老化的第一周急剧下降后,强酸性(约pH 4.5)土壤中镉的生物可及性达到了近乎稳定的水平(胃相和小肠相中分别为76.5 - 76.9%和52.0 - 52.6%)。相比之下,发现较高pH值(>6.0)土壤中镉的生物可及性要低得多(胃相和小肠相中分别为53.3 - 72.7%和29.9 - 43.4%),并且需要2周的老化时间才能达到稳定水平。新添加的镉比天然镉更不稳定。在第120天,添加镉的主要部分存在于可交换镉中,在最初的1周和2周分别急剧下降到近乎稳定状态后,强酸性土壤中的可交换镉(68.6 - 71.8%)高于较高pH值土壤(53.4 - 61.4%)。所有土壤在整个培养期内,镉生物可及性与水溶性镉和可交换镉单独或两者之和之间均存在显著相关性,这表明这些镉形态可能构成土壤中生物可及镉的主要部分。

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