铝对人体的一般影响

A. Ergashov
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引用次数: 0

摘要

铝无处不在;地壳中第三常见的元素。它是由岩石风化和火山活动自然释放到环境中的。采矿等人类活动也导致铝释放到环境中。环境介质中的铝含量因地点和采样地点的不同而有很大差异。一般来说,大气中铝的本底含量很低,通常在0.005至0.18 μg/m3之间。在城市和工业场所通常观察到的水平要高得多。地表水中的铝含量通常很低(<0.1毫克/升);然而,在酸性水域或腐殖酸或黄腐酸含量高的水中,由于氧化铝和铝盐的溶解度增加,可溶性铝的浓度增加。它在土壤中的浓度变化很大,从7克到100克以上不等。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
THE GENERAL EFFECT OF ALUMINUM ON THE BODY
Aluminum is ubiquitous; the third most common element of the earth's crust. It is naturally released to the environment from the weathering of rocks and volcanic activity. Human activities such as mining also result in the release of aluminum to the environment. Aluminum levels in environmental media vary widely depending upon the location and sampling site. In general, background levels of aluminum in the atmosphere are low, typically ranging from about 0.005 to 0.18 μg/m3. Much higher levels are routinely observed in urban and industrial locations. Aluminum levels in surface water is usually very low (<0.1 mg/L); however, in acidic waters or water high in humic or fulvic acid content, the concentration of soluble aluminum increases due to the increased solubility of aluminum oxide and aluminum salts. Its concentration in soils varies widely, ranging from about 7 to over 100 g/kg.
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