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首页> 外文期刊>Journal of marine systems: journal of the European Association of Marine Sciences and Techniques >Response of benthic infauna and epifauna to ocean disposal of red clay dredged material in the New York Bight: A study using sediment-profile imaging, surface imaging and traditional methods
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Response of benthic infauna and epifauna to ocean disposal of red clay dredged material in the New York Bight: A study using sediment-profile imaging, surface imaging and traditional methods

机译:纽约湾底栖动物和表生动物对红黏土疏material材料的海洋处置的响应:使用沉积物剖面成像,表面成像和传统方法的研究

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摘要

In 1997, approximately I million cubic yards of consolidated red clay was dredged from Newark Bay in New Jersey and deposited on the seafloor at an open-water dredged material disposal site located on the inner continental shelf of the New York Bight. To address concerns about the ability of benthic organisms to colonize the seafloor deposits of this compact, organic-poor red clay, monitoring surveys were conducted in 1998 (1 year after disposal) and 2002 (5 years after disposal). The surveys used a combination of sediment imaging and traditional grab sampling methods to characterize physical and biological conditions over the surface of the red clay deposits in comparison to nearby reference areas consisting of either naturally-occurring, sandy surface sediments or deposits of unconsolidated, muddy dredged material. Sediment-surface and sediment-profile images (SPI) collected in summer 2002 indicated that the surface of the red clay deposits had become much smoother and more heterogeneous in texture compared to images collected in 1998. The images also indicated that these deposits had become colonized to a much greater degree by relatively abundant and diverse infaunal and epifaunal communities compared to 1998. Taxonomic analysis of benthic grab samples confirmed the imaging results and indicated relatively high infaunal organism abundance and diversity over the red clay deposits in 2002 compared to the reference areas. However, the structure of the benthic community inhabiting the red clay was fundamentally different from the communities in the reference areas, due to the differences in sediment texture and composition. The combination of imaging and traditional taxonomic approaches used in this study provided much greater insight on the red clay colonization process than either approach by itself. (c) 2006 Elsevier B.V. All rights reserved.
机译:1997年,从新泽西州的纽瓦克湾疏approximately了大约一百万立方码的固结红粘土,并将其沉积在位于纽约湾内陆架上的一个露天疏dr物料处置场的海底。为了解决有关底栖生物在这种致密的,有机贫瘠的致密红粘土的海底沉积物中定殖的能力的担忧,分别于1998年(处置后1年)和2002年(处置后5年)进行了监测调查。这些调查结合了沉积物成像和传统抓斗采样方法,与附近的参考区域(包括天然存在的沙质表面沉积物或未固结,泥泞疏ged的沉积物)相比,来表征红粘土沉积物表面的物理和生物学条件。材料。 2002年夏季收集的沉积物表面和沉积物剖面图像(SPI)表明,与1998年收集的图像相比,红粘土沉积物的表面变得更加光滑,质地更加不均一。图像还表明,这些沉积物已被定殖。与1998年相比,相对丰富和多样的非生物和表生动物群落在很大程度上得到了改善。对底栖生物样品的分类学分析证实了成像结果,并表明与参考地区相比,2002年红黏土沉积物的非生物有机物丰度和多样性相对较高。但是,由于沉积物质地和组成的差异,居住在红粘土中的底栖生物群落的结构与参考地区的群落根本不同。这项研究中使用的成像方法和传统分类方法相结合,比任何一种方法本身对红粘土定殖过程的了解要大得多。 (c)2006 Elsevier B.V.保留所有权利。

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