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Temporal and spatial variation of perchlorate in streambed sediments: results from in-situ dialysis samplers
The fate of perchlorate (ClO 4 −) in streambed sediments is becoming a concern due to the increasing number of groundwater and surface water contamination sites in the United States. Dialysis samplers were deployed at three sites over a period of 1 year to determine the vertical distribution of ClO...
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Published in: | Environmental pollution (1987) 2005-07, Vol.136 (2), p.283-291 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | The fate of perchlorate (ClO
4
−) in streambed sediments is becoming a concern due to the increasing number of groundwater and surface water contamination sites in the United States. Dialysis samplers were deployed at three sites over a period of 1 year to determine the vertical distribution of ClO
4
− in sediment pore water. Results indicated that the spatial and temporal ClO
4
− penetration into sediments could be affected by numerous factors, such as temperature, microbial degradation, ClO
4
− surface water concentration, and sediment physico-geological properties. In general, maximum ClO
4
− penetration into sediments at the studied sites was 30 cm below the sediment-water surface. The vertical sequential depletion of electron acceptors in sediments suggested that microbial reduction was responsible for ClO
4
− depletion in stream sediments. Biodegradation of ClO
4
− occurred over a seasonally variable active depth zone of 1–10 cm. Results implied that there was a rapid natural attenuation potential of perchlorate in saturated near-surface sediments.
Perchlorate may be rapidly attenuated in saturated near-surface sediments. |
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ISSN: | 0269-7491 1873-6424 |
DOI: | 10.1016/j.envpol.2004.12.037 |