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湿地缓冲区对氮磷的截留:土壤类型、水文学和植被的影响。

Wetland buffer zones for nitrogen and phosphorus retention: Impacts of soil type, hydrology and vegetation.

机构信息

Chemical Analytics and Biogeochemistry, Leibniz-Institute of Freshwater Ecology and Inland Fisheries Berlin (IGB), Berlin, Germany.

Chemical Analytics and Biogeochemistry, Leibniz-Institute of Freshwater Ecology and Inland Fisheries Berlin (IGB), Berlin, Germany; Department of Bioscience, Aarhus University, 8600 Silkeborg, Denmark.

出版信息

Sci Total Environ. 2020 Jul 20;727:138709. doi: 10.1016/j.scitotenv.2020.138709. Epub 2020 Apr 16.

Abstract

Wetland buffer zones (WBZs) are riparian areas that form a transition between terrestrial and aquatic environments and are well-known to remove agricultural water pollutants such as nitrogen (N) and phosphorus (P). This review attempts to merge and compare data on the nutrient load, nutrient loss and nutrient removal and/or retention from multiple studies of various WBZs termed as riparian mineral soil wetlands, groundwater-charged peatlands (i.e. fens) and floodplains. Two different soil types ('organic' and 'mineral'), four different main water sources ('groundwater', 'precipitation', 'surface runoff/drain discharge', and 'river inundation') and three different vegetation classes ('arboraceous', 'herbaceous' and 'aerenchymous') were considered separately for data analysis. The studied WBZs are situated within the temperate and continental climatic regions that are commonly found in northern-central Europe, northern USA and Canada. Surprisingly, only weak differences for the nutrient removal/retention capability were found if the three WBZ types were directly compared. The results of our study reveal that for example the nitrate retention efficiency of organic soils (53 ± 28%; mean ± sd) is only slightly higher than that of mineral soils (50 ± 32%). Variance in load had a stronger influence than soil type on the N retention in WBZs. However, organic soils in fens tend to be sources of dissolved organic N and soluble reactive P, particularly when the fens have become degraded due to drainage and past agricultural usage. The detailed consideration of water sources indicated that average nitrate removal efficiencies were highest for ground water (76 ± 25%) and lowest for river water (35 ± 24%). No significant pattern for P retention emerged; however, the highest absolute removal appeared if the P source was river water. The harvesting of vegetation will minimise potential P loss from rewetted WBZs and plant biomass yield may promote circular economy value chains and provide compensation to land owners for restored land now unsuitable for conventional farming.

摘要

湿地缓冲带 (WBZ) 是陆地和水生环境之间的过渡区域,众所周知,它们可以去除农业水中的污染物,如氮 (N) 和磷 (P)。本综述试图合并和比较来自不同 WBZ 的多项研究的数据,这些 WBZ 被称为河岸矿质土壤湿地、充水泥炭地 (即沼泽地) 和洪泛平原。分别考虑了两种不同的土壤类型(“有机”和“矿质”)、四种不同的主要水源(“地下水”、“降水”、“地表径流/排水”和“河流泛滥”)和三种不同的植被类型(“乔木”、“草本”和“通气组织”)进行数据分析。所研究的 WBZ 位于温带和大陆性气候区,常见于北欧、北美和加拿大。令人惊讶的是,如果直接比较这三种 WBZ 类型,发现它们的养分去除/保留能力差异很小。我们的研究结果表明,例如,有机土壤的硝酸盐保留效率(53±28%;平均值±标准差)仅略高于矿质土壤(50±32%)。负荷的变异性比土壤类型对 WBZ 中 N 的保留有更强的影响。然而,由于排水和过去的农业使用,沼泽地的有机土壤往往是溶解有机氮和可溶性活性磷的来源。对水源的详细考虑表明,地下水的硝酸盐去除效率最高(76±25%),河水的最低(35±24%)。P 保留没有出现明显的模式;然而,如果 P 源是河水,则会出现最高的绝对去除。植被的收割将最大限度地减少重新湿地化的 WBZ 中潜在的 P 损失,植物生物量的产量可能会促进循环经济价值链,并为恢复的土地提供补偿,这些土地现在不适用于传统农业。

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