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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Geochemistry and particle size of surface sediments of Exmouth Gulf, northwest shelf, Australia
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Geochemistry and particle size of surface sediments of Exmouth Gulf, northwest shelf, Australia

机译:澳大利亚西北大陆架埃克斯茅斯海湾的地球化学和表层沉积物的粒径

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Exmouth Gulf is a shallow (mean depth 11.9 m, 2600 km(2) area) inverse estuarine embayment on the northwest shelf of Australia, with a catchment area of 6400 km(2) with low human and livestock populations in an arid climate. The Gulf is an extreme example of a tide and wave dominated estuary, with very small river inputs. Freshwater supply from the land is very small, and terrestrial run-off nutrient supply is estimated to be 0.8 mmol TN and 0.4 mmol TP per square metre Gulf area per year (TN = total dissolved and particulate nitrogen, TP=total dissolved and particulate phosphorus). Holocene deposits in the mangrove margins are less than Im thick, and are relict and partly aeolian in origin. Surficial sediments are largely quartz and calcite sand, and fine-grained recent sediments are probably removed by energetic Indian Ocean tide and wave mixing and circulation. Geochemical variations in sediment composition across the Gulf are small, and appear to be little affected by redox cycles. Marine organic matter is efficiently decomposed, leaving behind excess phosphorus associated with carbonate and iron-rich sediments. The thin ribbon of stunted mangroves along the eastern margin of the Gulf has little influence on the composition of sedimentary organic matter in the Gulf, and the mangrove sediments are not a trap for trace elements as has been found in other parts of the tropical world. Ba, Li, Pb, and Cu vary in direct proportion to the abundance of the bulk sediment aluminosilicate fraction, boron is enriched by evaporation in the supratidal saltflat regions, and cadmium has large variations perhaps related to the carbonate fraction of the sediments. There is little evidence for coastal trapping of sediment and oceanic elements in Exmouth Gulf, and some regions of the intertidal mangrove and saltflat zones are being eroded into the Gulf and adjacent shelf. (C) 2001 Elsevier Science Ltd. All rights reserved. [References: 98]
机译:埃克斯茅斯海湾是澳大利亚西北陆架上的浅河口(平均深度11.9 m,2600 km(2)),河口反向集水区,集水区6400 km(2),干旱气候下人畜稀少。海湾是潮汐和海浪主导的河口的一个极端例子,河流输入量很小。土地上的淡水供应非常少,据估计,陆地径流养分的供应量为每年每平方米海湾地区0.8 mmol TN和0.4 mmol TP(TN =溶解的总氮和颗粒氮,TP =溶解的总磷和颗粒磷) )。红树林边缘的全新世沉积物小于1m厚,起源为遗迹,部分为风成。表层沉积物主要是石英和方解石砂,最近的细颗粒沉积物可能会因印度洋高潮和波浪混合和环流而被清除。整个海湾地区沉积物组成的地球化学变化很小,并且受氧化还原循环的影响似乎很小。海洋有机物被有效分解,留下了与碳酸盐和富含铁的沉积物相关的过量磷。海湾东部边缘的发育不良的红树林带状薄带对海湾地区沉积有机物的组成影响很小,而且红树林沉积物也不是热带世界其他地区发现的微量元素的陷阱。 Ba,Li,Pb和Cu与大量沉积物铝硅酸盐组分的丰度成正比,硼在上部盐滩地区通过蒸发而富集,镉的变化很大,可能与沉积物中碳酸盐含量有关。几乎没有证据表明埃克斯茅斯海湾沿岸有沉积物和海洋元素的圈闭,潮间带红树林和盐滩带的某些地区正被侵蚀到海湾和邻近的陆架中。 (C)2001 Elsevier ScienceLtd。保留所有权利。 [参考:98]

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