Instituto de Oceanografia - FURG, Rio Grande, Av Italia km 8, RS 96201-900, Brazil.
Department of Earth and Ocean Sciences, University of South Carolina, Columbia, SC 29208, USA.
Mar Pollut Bull. 2014 Jan 15;78(1-2):209-12. doi: 10.1016/j.marpolbul.2013.10.042. Epub 2013 Nov 12.
This study reports results of analysis of sediment cores collected from the Patos Lagoon estuary. This estuary receives materials from land runoff into Patos and Mirim lagoons and from exchange with the adjacent South Atlantic Ocean through a narrow inlet. Sediment from these sources is mostly natural, but additional contributions associated with source/activities related to the port of Rio Grande. The aim of this study was to estimate rates of accumulation of the sediments and to assess the significance of metal inputs from these activities relative to natural inputs. Our results indicate an average sedimentation rate of 0.3 cm/yr and that the transport of suspended solids from offshore sources into the estuary was enhanced after the deepening of the channel and construction of the breakwaters (in the early 1900). Results for metal accumulation in these sediments suggest that there have been only minor enrichments which can be attributed to anthropogenic sources.
本研究报告了从帕托斯泻湖河口采集的沉积物岩芯分析的结果。这个河口接收了来自帕托斯和米拉马尔泻湖的陆地径流带来的物质,以及通过一个狭窄的入口与相邻的南大西洋进行的交换。这些物质主要来自自然,但也有一些与里奥格兰德港的相关活动有关的额外贡献。本研究的目的是估计沉积物的堆积速率,并评估这些活动对金属输入的重要性相对于自然输入的重要性。我们的研究结果表明,平均沉积速率为 0.3 厘米/年,并且自航道加深和防波堤建设以来(20 世纪初),从近海来源进入河口的悬浮物输送增加了。这些沉积物中金属积累的结果表明,只有很小的富集,这可以归因于人为来源。