Assessment of density variations of marine sediments with ocean and sediment depths.

Q2 Environmental Science
The Scientific World Journal Pub Date : 2014-03-06 eCollection Date: 2014-01-01 DOI:10.1155/2014/823296
R Tenzer, V Gladkikh
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引用次数: 77

Abstract

We analyze the density distribution of marine sediments using density samples taken from 716 drill sites of the Deep Sea Drilling Project (DSDP). The samples taken within the upper stratigraphic layer exhibit a prevailing trend of the decreasing density with the increasing ocean depth (at a rate of -0.05 g/cm(3) per 1 km). Our results confirm findings of published studies that the density nonlinearly increases with the increasing sediment depth due to compaction. We further establish a 3D density model of marine sediments and propose theoretical models of the ocean-sediment and sediment-bedrock density contrasts. The sediment density-depth equation approximates density samples with an average uncertainty of about 10% and better represents the density distribution especially at deeper sections of basin sediments than a uniform density model. The analysis of DSDP density data also reveals that the average density of marine sediments is 1.70 g/cm(3) and the average density of the ocean bedrock is 2.9 g/cm(3).

Abstract Image

Abstract Image

Abstract Image

海洋沉积物密度随海洋和沉积物深度变化的评估。
我们利用深海钻探项目(DSDP) 716个钻探点的密度样本分析了海洋沉积物的密度分布。上层地层样品的密度随海洋深度的增加呈下降趋势(-0.05 g/cm(3) / 1 km)。我们的研究结果证实了已发表的研究结果,即由于压实作用,密度随沉积物深度的增加而非线性增加。我们进一步建立了海洋沉积物的三维密度模型,并提出了海洋-沉积物和沉积物-基岩密度对比的理论模型。泥沙密度-深度方程近似于密度样本,平均不确定度约为10%,比均匀密度模型更能代表盆地沉积物的密度分布,特别是在较深的剖面上。DSDP密度数据分析也表明,海洋沉积物的平均密度为1.70 g/cm(3),海洋基岩的平均密度为2.9 g/cm(3)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
The Scientific World Journal
The Scientific World Journal 综合性期刊-综合性期刊
CiteScore
5.60
自引率
0.00%
发文量
170
审稿时长
3.7 months
期刊介绍: The Scientific World Journal is a peer-reviewed, Open Access journal that publishes original research, reviews, and clinical studies covering a wide range of subjects in science, technology, and medicine. The journal is divided into 81 subject areas.
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