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长江中的营养物质。

Nutrients in the Changjiang River.

作者信息

Shen Zhi-Liang, Liu Qun

机构信息

Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China.

出版信息

Environ Monit Assess. 2009 Jun;153(1-4):27-44. doi: 10.1007/s10661-008-0334-2. Epub 2008 May 17.

Abstract

N, P and SiO3-Si in the Changjiang mainstream and its major tributaries and lakes were investigated in the dry season from November to December, 1997, and in the flood season in August and October, 1998. An even distribution of SiO3-Si was found along the Changjiang River. However, the concentrations of total nitrogen, total dissolved nitrogen, dissolved inorganic nitrogen, nitrate and total phosphorus, total particulate phosphorus increased notably in the upper reaches, which reflected an increasing impact from human activities. Those concentrations in the middle and lower reaches of the Changjiang River were relatively constant. Dissolved N was the major form of N and the particulate P was the major form of P in the Changjiang River. The molar ratio of dissolved N to dissolved P was extremely high (192.5-317.5), while that of the particulate form was low (5.6-37.7). High N/P ratio reflected a significant input of anthropogenic N such as N from precipitation and N lost from water and soil etc. Dissolved N and P was in a quasi-equilibrium state in the process from precipitate to the river. In the turbid river water, light limitation, rather than P limitation, seemed more likely to be a controlling factor for the growth of phytoplankton. A positive linear correlationship between the concentration of dissolved N and the river's runoff was found, mainly in the upper reaches, which was related to the non-point sources of N. Over the past decades, N concentration has greatly increased, but the change of P concentration was not as significant as N. The nutrient fluxes of the Changjiang mainstream and tributaries were estimated, and the result showed that the nutrient fluxes were mainly controlled by the runoff, of which more than a half came from the tributaries. These investigations carried out before water storage of the Three Gorges Dam will supply a scientific base for studying the influences of the Three Gorges Dam on the ecology and environment of the Changjiang River and its estuary.

摘要

1997年11月至12月的枯水期以及1998年8月和10月的汛期,对长江干流及其主要支流和湖泊中的氮、磷和硅酸硅进行了调查。研究发现长江沿线硅酸硅分布均匀。然而,上游的总氮、总溶解氮、溶解无机氮、硝酸盐以及总磷、总颗粒磷的浓度显著增加,这反映了人类活动影响的加剧。长江中下游这些物质的浓度相对稳定。溶解态氮是长江中氮的主要形态,颗粒态磷是磷的主要形态。溶解态氮与溶解态磷的摩尔比极高(192.5 - 317.5),而颗粒态的摩尔比则较低(5.6 - 37.7)。高氮磷比反映了人为氮的大量输入,如降水带来的氮以及水体和土壤中流失的氮等。溶解态氮和磷在从降水到河流的过程中处于准平衡状态。在浑浊的河水中,光限制而非磷限制似乎更有可能是浮游植物生长的控制因素。在上游地区发现溶解态氮浓度与河流径流量之间存在正线性相关,这与氮的非点源有关。在过去几十年中,氮浓度大幅增加,但磷浓度的变化不如氮显著。估算了长江干流和支流的营养盐通量,结果表明营养盐通量主要受径流量控制,其中一半以上来自支流。这些在三峡大坝蓄水前进行的调查将为研究三峡大坝对长江及其河口生态环境的影响提供科学依据。

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