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Effects of sediment dredging on nitrogen cycling in Lake Taihu, China: Insight from mass balance based on a 2-year field study

机译:太湖底泥疏on对氮循环的影响:基于两年实地研究的质量平衡见解

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摘要

Sediment dredging can permanently remove pollutants from an aquatic ecosystem, which is considered an effective approach to aquatic ecosystem restoration. In this work, a 2-year field simulation test was carried out to investigate the effect of dredging on nitrogen cycling across the sediment-water interface (SWI) in Lake Taihu, China. The results showed that simulated dredging applied to an area rich in total organic carbon (TOC) and total nitrogen (TN) slightly reduced the NH4 (+)-N release from sediments while temporarily enhanced the NH4 (+)-N release in an area with lower TOC and/or TN (in the first 180 days), although the application had a limited effect on the fluxes of NO2 (-)-N and NO3 (-)-N in both areas. Further analysis indicated that dredging induced decreases in nitrification, denitrification, and anaerobic ammonium oxidation (anammox) in sediments, notably by 76.9, 49.0, and 89.9 %, respectively, in the TOC and/or TN-rich area. Therefore, dredging slowed down nitrogen cycling rates in sediments but did not increase N loading to overlying water. The main reason for the above phenomenon could be attributed to the removal of the surface sediments enriched with more TOC and/or TN (compared with the bottom sediments). Overall, to minimize internal N pollution, dredging may be more applicable to nutrient-rich sediments.
机译:泥沙淤积可以从水生生态系统中永久去除污染物,这被认为是恢复水生生态系统的有效方法。在这项工作中,进行了为期两年的现场模拟测试,以研究疏on对中国太湖跨沉积物-水界面(SWI)的氮循环的影响。结果表明,模拟疏to应用于富含有机碳(TOC)和总氮(TN)的区域,可略微减少沉积物中NH4(+)-N的释放,而暂时增加该区域中NH4(+)-N的释放(在开始的180天内)具有较低的TOC和/或TN,尽管该应用对两个地区的NO2(-)-N和NO3(-)-N的通量影响有限。进一步的分析表明,疏TO导致沉积物的硝化,反硝化和厌氧铵氧化(厌氧氨)降低,在富含TOC和/或TN的地区分别降低76.9%,49.0%和89.9%。因此,疏ging减慢了沉积物中氮的循环速度,但并未增加上覆水中的氮负荷。造成上述现象的主要原因可能是由于去除了富含TOC和/或TN的表层沉积物(与底部沉积物相比)。总体而言,为了最大程度地减少内部氮污染,疏dr可能更适用于营养丰富的沉积物。

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