环境中的砷

I. Jones
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引用次数: 0

摘要

长期以来,砷在人们的心目中一直是毒药的代名词,它展现出一种多样、迷人、动态的生物地球化学特征。具有化学和生物活性,其化学形态或形态随化学或生物条件的微小变化而变化。根据任何含砷系统受物理/化学或生物过程支配的程度,砷的形式可能在有机和甲基化物种的各种形式之间发生变化,并可能随着条件的变化而迅速变化。早期的研究围绕着色素的配方,后来是有效药物的开发。再后来,由于其作为一种毒药的历史悠久,砷被纳入许多农业实践,主要作为除草剂或杀虫剂。它也被用于相当专业的化学战领域,并且由于处置不当仍然构成威胁。最近的许多研究都集中在鉴定河口和海水中发现的以前未知的有机砷种类。这项工作正在建立对砷的生化循环所涉及的生物途径的理解。与海洋和河口水域的循环相比,在淡水中砷的循环方面进行的工作很少。同样,对淡水沉积物间隙水中砷形态的研究也少于对海洋沉积物或潮间带沉积物的研究。动态孔隙水中砷的表征提出了一系列不寻常和困难的问题,而不是最不重要的是代表性,离散样品的采购。对许多可能的取样方法进行了审查,薄膜凝胶取样技术的变化可能是最好的选择,尽管这将取决于所调查的潮间带沉积物的类型和所寻求的信息。无论在地方规模还是在全球水平上,都不可能提出砷循环的一般模型。这当然是由于生态系统的巨大多样性,每个生态系统对砷的种类形成有不同的控制,并包含不同的生物群落。一旦描述了一个给定的系统,砷的物种形成模式(空间上和时间上)是可以解释的,并且可以确定潜在的影响,但它们不能转移到另一个系统。关于不同系统中砷物种形成的信息的持续积累有助于解开更大的全球砷循环。这样的理解只会有利于为受污染的土壤和水生系统制定安全有效的补救方案。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Arsenic in the Environment
Arsenic, long synonymous in people's mind with poison exhibits a varied, fascinating and dynamic biogeochemistry. Chemically and biologically reactive, its chemical form, or speciation, changes with slight variations in chemical or biological conditions. Depending upon the extent to which any arsenic containing system is dominated by physical/chemical or biological process, the forms of arsenic may change between the various in organic and methylated species, and may alter rapidly with varying conditions. Early research revolved around the formulation of pigments, and later in the development of effective medicines. Later still, thanks due to its long history as a poison, arsenic was included in numerous agricultural practices, mainly as a herbicide or pesticide. It has also seen service in the rather more specialised field of chemical warfare, and still poses threats as a result of improper disposal. Much of the recent research has focused on the identification of previously unknown organoarsenic species found in estuarine and marine waters. This work is building up an understanding of the biological pathways involved in the biochemical cycling of arsenic. Little work has been carried out with respect to the cycling of arsenic in freshwaters in comparison to that in marine and estuarine waters. Similarly, there has been less work performed on the speciation of arsenic in freshwater sediment interstitial waters, than there has on marine sediments, or intertidal sediments. The characterisation of arsenic in dynamic porewater poses a set of unusual and difficult problems, not the least being the procurement of representative, discrete samples. A number of potential sampling methods are reviewed, and variations on the thin film gel sampling technique are drought to provide perhaps the best option, although this will depend upon the type of intertidal sediment being investigated, and the information sought. It may be impossible to propose a general model of arsenic cycling either at a local scale or at a global level. This is of course due to the great diversity in ecosystems, each having different controls over arsenic speciation, and containing different biological communities. Once a given system has been described, the patterns of arsenic speciation (both spatially and temporally) are explainable, and potential impacts can be identified, but (hey cannot be transferred to another system. The continuing accumulation of information regarding arsenic speciation in different systems is helping in the unravelling of the larger global arsenic cycle. Such an understanding can only be a benefit in the development of safe and efficient remediation schemes for contaminated soil and aquatic systems.
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