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不同补给水源条件下形成的西安护城河底泥氮磷释放特征。

Release characteristics of nitrogen and phosphorus from sediments formed under different supplemental water sources in Xi'an moat, China.

机构信息

School of Environmental and Municipal Engineering, Xi'an University of Architecture and Technology, No. 13 Yanta Road, Beilin District, Xi'an, Shaanxi, China.

College of Chemistry & Materials Science, Northwest University, Xi'an, 710069, China.

出版信息

Environ Sci Pollut Res Int. 2019 Apr;26(11):10746-10755. doi: 10.1007/s11356-019-04537-z. Epub 2019 Feb 18.

Abstract

The endogenous release of nutrients from sediments contributes to the eutrophication of landscape water to a certain degree, which depends on the characteristics of sediments. The study explored the characteristics of nitrogen (N) and phosphorus (P) released from two different sediments, which were deposited from reclaimed water (SRW) or surface water (SSW) respectively in Xi'an moat. This paper aimed to compare the effects of nutrient release from SRW and SSW on the water quality. Results showed that the maximum increase rates reached 1.21 mg TN/(L·day) and 0.11 mg TP/(L·day), respectively, in the overlying water of SRW, which were 1.6 and 2.8 times those of SSW. The released amounts of SRW were 0.192 mg TN/g and 0.038 mg TP/g, which were 4.1 and 12.7 times those of SSW. Meanwhile, the densities of benthic algae in SRW and SSW were 5.605 × 10 and 2.846 × 10 cells/L, respectively. Moreover, the species number and individual sizes of benthic algae in SRW were also larger than those in SSW, which played an important role in the nitrogen circulation. Unexpectedly, oxidation reduction potential (ORP) level of SRW was lower than that of SSW, although SRW has a higher dissolved oxygen level. Therefore, the N and P concentrations in the overlying water of SRW were considerably higher than those of SSW, which was mainly attributed to the higher nutrient contents and lower ORP in SRW.

摘要

底泥中营养物质的内源释放在一定程度上导致景观水富营养化,这取决于底泥的特性。本研究探讨了分别来自西安护城河再生水(SRW)和地表水(SSW)的两种不同沉积物中氮(N)和磷(P)释放的特征,旨在比较 SRW 和 SSW 营养物质释放对水质的影响。结果表明,SRW 上覆水中的最大氮增加率达到 1.21mg TN/(L·天),磷增加率达到 0.11mg TP/(L·天),分别是 SSW 的 1.6 倍和 2.8 倍。SRW 的释放量为 0.192mg TN/g 和 0.038mg TP/g,分别是 SSW 的 4.1 倍和 12.7 倍。同时,SRW 和 SSW 底栖藻类的密度分别为 5.605×10 和 2.846×10 个细胞/L。此外,SRW 底栖藻类的物种数量和个体大小也大于 SSW,在氮循环中起着重要作用。出乎意料的是,尽管 SRW 的溶解氧水平较高,但 SRW 的氧化还原电位(ORP)水平却低于 SSW。因此,SRW 上覆水中的 N 和 P 浓度明显高于 SSW,这主要归因于 SRW 中较高的营养物质含量和较低的 ORP。

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