Department of Soil and Environment, Swedish University of Agricultural Sciences, Uppsala, Sweden.
Department of Forest Mycology and Plant Pathology, Swedish University of Agricultural Sciences, Uppsala, Sweden.
Water Res. 2024 Jul 1;258:121770. doi: 10.1016/j.watres.2024.121770. Epub 2024 May 11.
To improve water quality and reduce instream erosion, floodplain remediation along agricultural streams can provide multiple ecosystem services through biogeochemical and fluvial processes. During floodplain inundation, longer water residence time and periodic anoxic conditions can lead to increased nitrogen (N) removal through denitrification but also mobilization of phosphorus (P), impeding overall water quality improvements. To investigate the capacity for N and P processing in remediated streams, we measured potential denitrification and nitrous oxide production and yields together with potential P desorption and P fractions in floodplain and stream sediments in ten catchments in Sweden. Sediment P desorption was measured as equilibrium P concentration, using P isotherm incubations. Denitrification rates were measured with the acetylene inhibition method. Sediment nutrient process rates were combined with hydrochemical monitoring along remediated streams and their paired upstream control reaches of trapezoidal shape to determine the impact of floodplains on water quality. The correlation between floodplain denitrification rates and P desorption (r = 0.53, p = 0.02) revealed a trade-off between soluble reactive P (SRP) and nitrate removal, driven by stream water connectivity to floodplains. Nitrous oxide production was not affected by differences in P processing, but nitrous oxide yields decreased with higher denitrification and P desorption. The release of SRP from floodplains (0.03 ± 0.41 mg P kg1 day1) was significantly lower than from trapezoidal stream banks (0.38 ± 0.37 mg P kg1 day1), predicted by long-term SRP concentrations in stream water and floodplain inundation frequency. The overall impact of SRP release from floodplains on stream SRP concentrations in remediated reaches was limited. However, the remediated reaches showing increased stream SRP concentrations were also frequently inundated and had higher labile P content and coarse soil texture in floodplain sediments. To fully realize the potential for water quality improvements with constructed floodplains in agricultural streams, the promotion of denitrification through increased inundation should be balanced against the risk of P release from sediments, particularly in streams with high SRP inputs.
为了改善水质和减少河流侵蚀,对农业流域的洪泛区进行修复,可以通过生物地球化学和河流过程提供多种生态系统服务。在洪泛区淹没期间,较长的水停留时间和周期性的缺氧条件可以通过反硝化作用增加氮(N)去除,但也会使磷(P)移动,从而阻碍整体水质改善。为了研究修复河流中 N 和 P 的处理能力,我们测量了十个瑞典流域中十个流域的洪泛区和溪流沉积物中的潜在反硝化作用和一氧化二氮的产生和产量以及潜在的 P 解吸和 P 分数。使用 P 等温孵育法测量沉积物 P 解吸作为平衡 P 浓度。通过乙炔抑制法测量反硝化速率。将沉积物养分过程速率与沿修复河流及其配对上游梯形控制流域的水文化学监测相结合,以确定洪泛区对水质的影响。洪泛区反硝化速率与 P 解吸之间的相关性(r = 0.53,p = 0.02)表明,可溶性反应性磷(SRP)和硝酸盐去除之间存在权衡,这是由溪流与洪泛区的连通性驱动的。一氧化二氮的产生不受 P 处理差异的影响,但随着反硝化和 P 解吸的增加,一氧化二氮的产量会降低。从洪泛区释放的 SRP(0.03 ± 0.41 mg P kg1 day1)明显低于从梯形溪岸释放的 SRP(0.38 ± 0.37 mg P kg1 day1),这是由溪流水中长期的 SRP 浓度和洪泛区淹没频率预测的。从洪泛区释放的 SRP 对修复河段中溪流 SRP 浓度的总体影响是有限的。然而,显示出增加的溪流 SRP 浓度的修复河段也经常被淹没,并且洪泛区沉积物中具有更高的活性 P 含量和粗土壤质地。为了充分实现通过构建农业流域的洪泛区改善水质的潜力,应通过增加淹没来促进反硝化作用,同时要平衡沉积物中 P 释放的风险,特别是在具有高 SRP 输入的溪流中。