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A 5-year study of the impact of peatland revegetation upon DOC concentrations

机译:泥炭地植被对DOC浓度影响的5年研究

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Peatlands are among the largest long-term soil carbon stores on the globe, but their degradation can lead to significant carbon losses. Therefore, restoration of peatlands has received considerable attention but the impact of revegetation upon critical water quality parameters has not been assessed. In this paper we consider a 5-year study of three restored sites in comparison to both an unrestored, bare peat control and to a vegetated control that did not require restoration. The soil porewater dissolved organic carbon concentration (DOC) was measured (6 replicates) for each restoration treatment and each control. The soil water measurements were made in the context of measuring the depth to water table; soil water pH and conductivity; and DOC concentration in surface runoff for the same restored and control treatment. The study showed that the average soil porewater DOC concentration on the restored sites rose significantly over the 5 year study representing a 34% increase relative to the vegetated control and an 11% increase relative to the unrestored, bare control. Soil pore water concentrations were not significantly different from surface runoff DOC concentrations, and therefore restoration as conducted by this study would have contributed to water quality deterioration in the catchment. However, had water table restoration been conducted alongside revegetation then a significant decline in DOC concentrations could have been realised. (C) 2014 Elsevier B.V. All rights reserved.
机译:泥炭地是全球最大的长期土壤碳储库之一,但是它们的退化会导致大量的碳损失。因此,泥炭地的恢复受到了相当大的关注,但是植被恢复对关键水质参数的影响尚未得到评估。在本文中,我们将对三个恢复地点进行为期5年的研究,并与未恢复的裸泥炭控制和不需要恢复的植被控制进行比较。对于每个修复处理和每个对照,测量土壤孔隙水中溶解的有机碳浓度(DOC)(一式六份)。土壤水的测量是在测量地下水位的深度的情况下进行的。土壤水的pH和电导率;对于恢复和控制相同的处理,地表径流中的DOC和DOC浓度。该研究表明,在为期5年的研究中,恢复地点的平均土壤孔隙水DOC浓度显着提高,相对于植被控制而言增加了34%,相对于未恢复的裸露控制而言增加了11%。土壤孔隙水浓度与地表径流DOC浓度无显着差异,因此,本研究进行的恢复将导致流域水质恶化。但是,如果在恢复植被的同时进行了地下水位恢复,则DOC浓度可能会显着下降。 (C)2014 Elsevier B.V.保留所有权利。

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