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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Suitability of degraded peat for constructed wetlands - hydraulic properties and nutrient flushing. (Special Issue: Properties, processes and ecological functions of floodplain, peatland, and paddy soils.)
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Suitability of degraded peat for constructed wetlands - hydraulic properties and nutrient flushing. (Special Issue: Properties, processes and ecological functions of floodplain, peatland, and paddy soils.)

机译:退化泥炭对人工湿地的适应性-水力特性和养分冲洗。 (特刊:洪泛区,泥炭地和水稻土的特性,过程和生态功能。)

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摘要

Nitrate removal from runoff from agricultural land is in general required to reach a "good chemical status" of surface and groundwater bodies according to the European Water Framework Directive. Removing nitrates via heterotrophic denitrification is highly effective but requires stable anoxic environmental conditions as well as available organic carbon as electron donator. Constructed wetlands (CWs), established on peat soils, through which the nitrate-loaded water is routed, may provide denitrification favorable conditions. To study nitrate turnover, hydraulic properties and possible negative side effects of CWs on formerly drained fens, we developed a mesocosm experiment with vertical flow and an open water surface. The first flushing of nitrate during the exchange of the initial pore volume was quantified with 0.58 g NO3-N kg-1 organic substance. Both nitrate and sulfate were released faster and in higher concentrations than DOC and with a ratio corresponding to the composition of the peat. Redox potential measurements revealed that denitrifying conditions established in certain soil depths after roughly 40 days of continuous flux. Transport properties were obtained from analyzing tracer breakthrough curves. It could be demonstrated that the degraded peat had a dual porosity structure. Subjected to nitrate enriched water for two years, the immobile pore water fraction increased from 40 to 80% probably because of physical consolidation processes and microbial activity and subsequent clogging of pores. This was not considered as negative since denitrification processes are believed to preferably operate in immobile, oxygen depleted water regions. We concluded that the first flushing of mineralized nitrate upon rewetting after onset of flux may compromise any positive clean up and nitrate removal effects occurring during long-term operation of peat-wetlands. It is thus advisable to recycle the water during early stages of the establishment of constructed wetlands.
机译:根据欧洲水框架指令,通常需要从农田的径流中去除硝酸盐,以达到地表水和地下水体的“良好化学状态”。通过异养反硝化去除硝酸盐非常有效,但需要稳定的缺氧环境条件以及可用的有机碳作为电子给体。在泥炭土上建立的人工湿地(CW),通过其输送硝酸盐负荷的水,可以提供反硝化的有利条件。为了研究硝酸盐的转化,水力特性以及连续水对以前排水的的可能的负面影响,我们开发了垂直流动和开放水面的中观试验。用0.58 g NO 3 -N kg -1 有机物定量交换初始孔体积时硝酸盐的第一次冲洗。硝酸盐和硫酸盐均以比DOC更快的速度和更高的浓度释放,其比例对应于泥炭的组成。氧化还原电位测量表明,经过大约40天的连续通量后,反硝化条件在某些土壤深度中建立。通过分析示踪剂穿透曲线获得了运输性质。可以证明降解的泥炭具有双重孔隙结构。经过两年的硝酸盐浓缩水处理后,固定的孔隙水比例从40%增至80%,这可能是由于物理固结过程和微生物活性以及随后的孔隙堵塞所致。这被认为不是不利的,因为据信反硝化过程优选在不动的贫氧水区域中进行。我们得出的结论是,在助焊剂出现后,重新润湿后首次冲洗矿化的硝酸盐可能会损害泥炭湿地长期运行期间发生的任何积极清除和硝酸盐去除效果。因此,建议在建立人工湿地的早期阶段对水进行再循环。

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