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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Sediment and trace element depositional history from the Ajkwa River estuarine mangroves of Irian Jaya (West Papua), Indonesia
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Sediment and trace element depositional history from the Ajkwa River estuarine mangroves of Irian Jaya (West Papua), Indonesia

机译:印度尼西亚伊里安加亚(西巴布亚)阿克夸河河口红树林的沉积物和微量元素沉积历史

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摘要

Radiotracer Pb-210 and contaminant copper were used to estimate sediment accumulation rates in 4 cores from the Ajkwa River estuary and mangrove tidal channels in western Irian Jaya. Mass accumulation rates (4.5-13 kg dry wt m(-2) yr(-1)) were within the envelope of expectations for a region of high rainfall, great river catchment relief, and rapid tectonic uplift of mountains. Copper accumulation rates were enhanced 40 fold in surface sediments, compared to pre-1950 sections of the sediment cores. These recent sediments with enhanced copper concentrations come from Freeport Indonesia mine tailings over the last 27 years. Variations in sediment core profiles of Al, Fe, and organic carbon were small, indicating no great change in bulk sediment composition. Sulfur concentrations decline toward the sediment surface, suggesting a decline in rates of microbial sulfate reduction. Enhanced sediment copper concentrations will be a useful tracer of sediment dispersal from the Ajkwa River estuary along this coast. (C) 2004 Elsevier Ltd. All rights reserved.
机译:放射性示踪剂Pb-210和污染铜用于估算Irian Jaya西部Ajkwa河口和红树林潮汐通道4个岩心中的沉积物积累速率。质量积累率(4.5-13 kg干重m·m·(-2)·yr·-1)处于降雨范围大,集水量大和山区快速构造抬升的预期范围之内。与1950年前的沉积物芯剖面相比,表层沉积物中的铜累积速率提高了40倍。这些最近的含铜量增加的沉积物来自过去27年中来自印度尼西亚Freeport矿山的尾矿。铝,铁和有机碳的沉积物芯剖面变化很小,表明总体沉积物组成没有很大变化。硫的浓度向沉积物表面下降,表明微生物硫酸盐还原速率下降。沉积物铜浓度的增加将是沿该海岸Ajkwa河口的沉积物扩散的有用示踪剂。 (C)2004 Elsevier Ltd.保留所有权利。

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