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Soil nitrogen accumulation, denitrification potential, and carbon source tracing in bioretention basins

机译:生物盆地土壤氮积累,脱氮电位和碳源描图

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Bioretention basins are one of the most commonly used green stormwater features, with the potential to accumulate significant levels of nitrogen (N) in their soil and to permanently remove it through denitrification. Many studies have investigated the N removal potential of bioretention basins through the assessment of inflow and outflow concentrations. However, their long-term N removal through soil accumulation and denitrification potential is less known. This study investigated the temporal variation of total N (TN) accumulation and denitrification potential in soils of 25 bioretention basins within a 13-year soil chronosequence, in a subtropical climate in Australia. The denitrification potential of a subset of seven bioretention basins was investigated in accompaniment with nutrient and soil characteristics. Additionally, stable isotopes (delta C-13 and delta N-15) were used to assess temporal changes in the soil composition as well as to identify the sources of carbon (C) into these basins. Over 13 years of operation, TN accumulated faster in the top 5 cm of soil than deeper soils. Soil TN density was highest in the top 5 cm with an average of 1.4 kg N m(-3), which was about two times higher than deeper soils. Site age and soil texture were the best predictors of soil TN density and denitrification (1 to 9.7 mg N m(-2) h(-1)). The isotope values were variable among basins. Low delta N-15 values in young basins (-1.02 parts per thousand) suggested fixation as the main source of N, while older basins had higher delta N-15, indicating higher denitrification. Bioretention plants were the primary source of soil C; although the occurrence of soil amendment also contributed to the C pool. To improve the performance of these bioretention basins, we recommend increasing vegetation at initial years after construction, and enhancing more frequent anaerobic conditions in the high soil profile. These two conditions can improve denitrification potential, and thus the performance of these basins for improving water quality. (C) 2020 Elsevier Ltd. All rights reserved.
机译:Bioretentent盆地是最常用的绿雨水特征之一,潜力在其土壤中积累显着水平的氮气(n),并永久地将其通过反硝化去除。许多研究通过对流入和流出浓度的评估研究了生物化盆地的N去除潜力。然而,它们通过土壤积累和反硝化潜力的长期去除较少。本研究调查了在澳大利亚的亚热带气候中,在13年的土壤成分中,在澳大利亚的亚热带气候中调查了25个生物循环土壤中总N(TN)积聚和脱氮潜力的时间变化。伴随着营养和土壤特性,研究了七个生物池余池子集的脱氮电位。另外,使用稳定同位素(Delta C-13和Delta N-15)来评估土壤组合物的时间变化,以及将碳(C)的碳源鉴定到这些盆中。超过13年的操作,TN在土壤中的前5厘米的堆积比深层的土壤更快。土壤TN密度在前5厘米中最高,平均为1.4kg n m(-3),比更深的土壤高出两倍。现场年龄和土壤质地是土壤TN密度的最佳预测因子和脱氮(1至9.7mg N(-2)H(-1))。同位素值在盆之间是可变的。幼小盆地(-1.02份)的低Δn-15值建议固定作为n的主要来源,而较旧的盆地具有较高的δn-15,表明较高的脱氮。生物植物是土壤C的主要来源;虽然土壤修正案的发生也有助于C游泳池。为了提高这些生物化盆地的表现,我们建议在施工后初期增加植被,并在高土壤剖面中增强更频繁的厌氧条件。这两个条件可以改善脱氮电位,从而改善这些盆地的性能,以改善水质。 (c)2020 elestvier有限公司保留所有权利。

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