Rewetting a pump-drained fen converts a nutrient hotspot into a sink and reduces organic carbon export

IF 4.3 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Biogeochemistry Pub Date : 2026-07-01 Epub Date: 2026-09-21 DOI:10.1007/s10533-026-01349-5
Rasmus Jes Petersen, Dominik Henrik Zak, Hans Estrup Andersen, Joachim Audet, Vilius Asbjørn Lyby Tolsgaard, Carl Christian Hoffmann
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引用次数: 0

Abstract

Peatland drainage for agricultural purposes has transformed wetlands into major nutrient sources, but rewetting offers potential for nutrient retention and climate mitigation. We quantified hydrological and nutrient fluxes in a 14.5 ha former pump-drained fen (Strande Enge, Denmark) across 1 year before and 2 years after rewetting. Restoration involved removing pumping infrastructure and reconnecting upstream catchments with the aim to restore natural flow paths. Prior to rewetting, the site exhibited high hydraulic loading (5904 mm yr−1) dominated by groundwater inputs and acted as a strong nutrient source, with net losses of total nitrogen (TN: 123 kg ha−1 yr−1), total phosphorus (TP: 23 kg ha−1 yr−1), and total organic carbon (TOC: 1336 kg ha−1 yr−1). Following rewetting, hydraulic loading increased more than fourfold (24,258–27,160 mm yr−1), and the system shifted to a flow-through wetland dominated by surface water inputs. Despite substantially higher nutrient loads after rewetting, the fen became a large sink for TN (209–242 kg ha−1 yr−1; 21% retention) and retained 44–72% of soluble reactive phosphorus. However, although their losses declined, particulate phosphorus and organic matter were still exported, particularly during high-flow events. At catchment scale, rewetting reduced the yearly TN export to the downstream lake by 27–38%, while the annual TP export varied strongly after rewetting (12% reduction in year 1 and 74% increase in year 2). These findings demonstrate that rewetting of pumped fens can rapidly transform nutrient source hotspots into effective nitrogen sinks, but additional measures may be needed to control particulate losses of nutrients and organic carbon, if these prove to persist over time. Overall, our results show that rewetting can reduce nutrient losses, including TOC losses, thereby contributing to mitigation of aquatic pollution and helping preserve peatland carbon stocks.

重新润湿抽干的沼泽可以将营养热点转化为汇,减少有机碳的输出
用于农业目的的泥炭地排水已将湿地转变为主要的营养来源,但再湿润提供了保持营养和减缓气候变化的潜力。我们量化了14.5 ha前泵排沼泽(丹麦Strande Enge)在重新湿润前1年和2年后的水文和养分通量。修复包括拆除抽水基础设施和重新连接上游集水区,目的是恢复自然流道。在再湿润之前,该站点表现出以地下水输入为主的高水力负荷(5904 mm yr−1),并作为强大的营养来源,总氮(TN: 123 kg ha−1年−1年−1)、总磷(TP: 23 kg ha−1年−1)和总有机碳(TOC: 1336 kg ha−1年−1)的净损失。再湿润后,水力负荷增加了四倍多(24,258-27,160毫米/年),系统转变为以地表水输入为主的流经湿地。尽管再湿润后的养分负荷显著增加,但沼泽仍成为TN的大汇(209-242 kg ha - 1 yr - 1,保留率21%),并保留了44-72%的可溶性活性磷。然而,尽管它们的损失有所下降,但颗粒磷和有机物仍在输出,特别是在高流量事件期间。在流域尺度上,再湿润使下游湖泊的总氮年出口量减少了27-38%,而总磷年出口量在再湿润后变化强烈(第1年减少12%,第2年增加74%)。这些发现表明,重新润湿抽水沼泽可以迅速将营养源热点转化为有效的氮汇,但如果这些被证明持续一段时间,可能需要采取额外的措施来控制营养物质和有机碳的颗粒损失。总体而言,我们的研究结果表明,再湿润可以减少包括TOC损失在内的养分损失,从而有助于缓解水生污染,并有助于保护泥炭地的碳储量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Biogeochemistry
Biogeochemistry 环境科学-地球科学综合
CiteScore
7.10
自引率
5.00%
发文量
112
审稿时长
3.2 months
期刊介绍: Biogeochemistry publishes original and synthetic papers dealing with biotic controls on the chemistry of the environment, or with the geochemical control of the structure and function of ecosystems. Cycles are considered, either of individual elements or of specific classes of natural or anthropogenic compounds in ecosystems. Particular emphasis is given to coupled interactions of element cycles. The journal spans from the molecular to global scales to elucidate the mechanisms driving patterns in biogeochemical cycles through space and time. Studies on both natural and artificial ecosystems are published when they contribute to a general understanding of biogeochemistry.
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