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强制曝气对营养物质和金属(类)物生物地球化学循环的影响,作为永久性分层河口(的里雅斯特湾,亚得里亚海北部)缺氧的补救措施。

Effect of forced aeration on the biogeochemical cycle of nutrients and metal(loid)s as a remedy for hypoxia in a permanently stratified estuary (Gulf of Trieste, northern Adriatic Sea).

机构信息

Department of Mathematics, Informatics and Geosciences, University of Trieste, Via E. Weiss 2, 34128 Trieste, Italy.

Department of Mathematics, Informatics and Geosciences, University of Trieste, Via E. Weiss 2, 34128 Trieste, Italy.

出版信息

Mar Pollut Bull. 2024 Aug;205:116632. doi: 10.1016/j.marpolbul.2024.116632. Epub 2024 Jun 28.

Abstract

The Timavo River estuary (northern Adriatic Sea) is characterised by strong thermohaline stratification that keeps the deep waters hypoxic. The consequence is an harmful algal bloom at the surface in summer that can be mitigated with a forced aeration system installed at the bottom to improve water oxygenation. The nutrient and metal(loid) cycle was investigated, before and during reoxygenation, using an in situ benthic chamber coupled with sampling and analyses of the water column, sediments and porewater. Dissolved oxygen (DO) decreased along the water column and quickly within the benthic chamber when aeration was not in operation, resulting in hypoxia (2.29 mg L) at the bottom and consequent increase in nutrient and metal(loid) concentrations. In contrast, DO levels increased during the activation of the forced aeration system, which proved effective in mitigating oxygen depletion and the efflux of metal(loid)s and nutrients into the overlying water.

摘要

蒂马沃罗河河口(亚得里亚海北部)的特点是强烈的温盐分层,这使得深层水处于缺氧状态。其结果是夏季表层出现有害藻类水华,可以通过在底部安装强制曝气系统来减轻这种情况,从而改善水的充氧。在重新充氧之前和期间,使用原位底栖室结合对水柱、沉积物和孔隙水的采样和分析,研究了营养物和金属(类)循环。当不进行曝气时,溶解氧 (DO) 沿水柱下降,在底栖室中迅速下降,导致底部缺氧(2.29 mg/L),并导致营养物和金属(类)浓度增加。相比之下,在强制曝气系统启动期间,DO 水平增加,该系统有效地缓解了缺氧和金属(类)和营养物向表层水的外溢。

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