Tenzer R, Gladkikh V
Institute of Geodesy and Geophysics, School of Geodesy and Geomatics, Wuhan University, 129 Luoyu Road, Wuhan 430079, China.
International IT University, 34A/8A Manas/Zhandosov Street (Intersection), Almaty 050040, Kazakhstan.
ScientificWorldJournal. 2014 Mar 6;2014:823296. doi: 10.1155/2014/823296. eCollection 2014.
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).
我们利用从深海钻探计划(DSDP)的716个钻探地点采集的密度样本,分析了海洋沉积物的密度分布。在上部地层内采集的样本呈现出随着海洋深度增加密度普遍降低的趋势(每1千米降低0.05克/立方厘米)。我们的结果证实了已发表研究的发现,即由于压实作用,密度随沉积物深度增加而非线性增加。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。沉积物密度 - 深度方程以约10%的平均不确定性逼近密度样本,并且比均匀密度模型能更好地表示密度分布,尤其是在盆地沉积物的较深部分。对DSDP密度数据的分析还表明,海洋沉积物的平均密度为1.70克/立方厘米,海洋基岩的平均密度为2.9克/立方厘米。