Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1029/2017WR022362 |
Effects of Drainage and Subsequent Restoration on Peatland Hydrological Processes at Catchment Scale | |
Menberu, Meseret Walle; Haghighi, Ali Torabi; Ronkanen, Anna-Kaisa; Marttila, Hannu; Klove, Bjorn | |
2018-07-01 | |
发表期刊 | WATER RESOURCES RESEARCH |
ISSN | 0043-1397 |
EISSN | 1944-7973 |
出版年 | 2018 |
卷号 | 54期号:7页码:4479-4497 |
文章类型 | Article |
语种 | 英语 |
国家 | Finland |
英文摘要 | Potential benefits of peatland restoration by rewetting include carbon sequestration, restored biodiversity, and improved hydrological functions. There is great uncertainty about how catchment hydrological processes change after restoration, with a particular lack of well-documented catchment runoff data. This study compared five formerly Disturbed (now Restored) and two undisturbed peatlands. In total, 455 and 728 hydrological events were selected for the analysis, using a three-event selection technique. Mean event runoff coefficient (RC) values varied greatly between conditions and hydrological events. RC in Disturbed conditions was slightly higher than in undisturbed conditions, but RC in Restored conditions was higher than under other conditions. Mean transit time revealed that event rainfall water reached the outlet faster in Disturbed conditions. Mean event peak flow in Disturbed conditions was higher and peaked faster than under other conditions. However, the base flow showed no noticeable difference between treatments. Significantly higher watertable (WT) rise per rainfall input (0.36-0.85 cm/mm) was observed in Disturbed conditions, due to lower specific yield (Sy) values (0.13-0.24) than under Restored and undisturbed conditions (Sy 0.25-0.50). Shallow WT showed significant positive correlations with runoff and storage properties and was a key component of the runoff generation mechanisms in peatlands. Storage-related parameters (Sy, WT rise per rainfall input) and catchment response time parameters revealed disturbance-related hydrological changes in peatlands more clearly than other runoff parameters tested (e.g., RC). Overall, with restoration, WT and storage properties recovered to the levels at undisturbed sites but increased runoff was observed occasionally due to wetter antecedent moisture conditions. |
英文关键词 | hydrology drainage runoff forestry restoration watertable |
领域 | 资源环境 |
收录类别 | SCI-E |
WOS记录号 | WOS:000442502100018 |
WOS关键词 | RUNOFF GENERATION ; HYDRAULIC CONDUCTIVITY ; POST-RESTORATION ; ORGANIC-CARBON ; BLANKET PEAT ; WATER ; BOG ; RAINFALL ; QUEBEC ; IMPACT |
WOS类目 | Environmental Sciences ; Limnology ; Water Resources |
WOS研究方向 | Environmental Sciences & Ecology ; Marine & Freshwater Biology ; Water Resources |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/21759 |
专题 | 资源环境科学 |
作者单位 | Univ Oulu, Water Resources & Environm Engn, Oulu, Finland |
推荐引用方式 GB/T 7714 | Menberu, Meseret Walle,Haghighi, Ali Torabi,Ronkanen, Anna-Kaisa,et al. Effects of Drainage and Subsequent Restoration on Peatland Hydrological Processes at Catchment Scale[J]. WATER RESOURCES RESEARCH,2018,54(7):4479-4497. |
APA | Menberu, Meseret Walle,Haghighi, Ali Torabi,Ronkanen, Anna-Kaisa,Marttila, Hannu,&Klove, Bjorn.(2018).Effects of Drainage and Subsequent Restoration on Peatland Hydrological Processes at Catchment Scale.WATER RESOURCES RESEARCH,54(7),4479-4497. |
MLA | Menberu, Meseret Walle,et al."Effects of Drainage and Subsequent Restoration on Peatland Hydrological Processes at Catchment Scale".WATER RESOURCES RESEARCH 54.7(2018):4479-4497. |
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