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Friedrich Möglich 《Die Naturwissenschaften》1938,26(24-25):409-410
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Laturnus F Fahimi I Gryndler M Hartmann A Heal MR Matucha M Schöler HF Schroll R Svensson T 《Environmental science and pollution research international》2005,12(4):233-244
- DOI: http:/dx.doi.org/10.1065/espr2005.06.262
Goal, Scope and Background The anthropogenic environmental emissions of chloroacetic acids and volatile organochlorines have been under scrutiny in
recent years because the two compound groups are suspected to contribute to forest dieback and stratospheric ozone destruction,
respectively. The two organochlorine groups are linked because the atmospheric photochemical oxidation of some volatile organochlorine
compounds is one source of phytotoxic chloroacetic acids in the environment. Moreover, both groups are produced in higher
amounts by natural chlorination of organic matter, e.g. by soil microorganisms, marine macroalgae and salt lake bacteria,
and show similar metabolism pathways. Elucidating the origin and fate of these organohalogens is necessary to implement actions
to counteract environmental problems caused by these compounds.
Main Features While the anthropogenic sources of chloroacetic acids and volatile organochlorines are relatively well-known and within human
control, knowledge of relevant natural processes is scarce and fragmented. This article reviews current knowledge on natural
formation and degradation processes of chloroacetic acids and volatile organochlorines in forest soils, with particular emphasis
on processes in the rhizosphere, and discusses future studies necessary to understand the role of forest soils in the formation
and degradation of these compounds.
Results and Discussion Reviewing the present knowledge of the natural formation and degradation processes of chloroacetic acids and volatile organochlorines
in forest soil has revealed gaps in knowledge regarding the actual mechanisms behind these processes. In particular, there
remains insufficient quantification of reliable budgets and rates of formation and degradation of chloroacetic acids and volatile
organochlorines in forest soil (both biotic and abiotic processes) to evaluate the strength of forest ecosystems regarding
the emission and uptake of chloroacetic acids and volatile organochlorines, both on a regional scale and on a global scale.
Conclusion It is concluded that the overall role of forest soil as a source and/or sink for chloroacetic acids and volatile organochlorines
is still unclear; the available laboratory and field data reveal only bits of the puzzle. Detailed knowledge of the natural
degradation and formation processes in forest soil is important to evaluate the strength of forest ecosystems for the emission
and uptake of chloroacetic acids and volatile organochlorines, both on a regional scale and on a global scale.
Recommendation and Perspective As the natural formation and degradation processes of chloroacetic acids and volatile organochlorines in forest soil can
be influenced by human activities, evaluation of the extent of this influence will help to identify what future actions are
needed to reduce human influences and thus prevent further damage to the environment and to human health caused by these compounds. 相似文献