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Physical, Chemical, and Geological Changes of Marine Environment Caused by the Benthic Impact Experiment at the IOM BIE Site

机译:IOM BIE网站底栖影响实验引起的海洋环境的物理,化学和地质变化

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In order to predict potential effects of mining of polymetallic nodules, Interoceanmetal Joint Organization (IOM) carried out, in 1995, a Benthic Impact Experiment (IOM BIE) in its pioneer area within the Clarion-Clipperton Fracture Zone. The IOM BIE study involved pre-disturbance (baseline), disturbance and post-disturbance stages as well as subsequent monitoring sampling in 1997. Comparison of data on physical and chemical characteristics of bottom sediment, near-bottom and pore water collected before and after experiment showed alterations in those characteristics. Contents of nutrients (silicates, nitrates, nitrites, and phosphates) and heavy metals (Cu, Zn, Pb, Cd) as well as the mineralogicai and grain size composition of the discharged sediments were determined on material collected by sediment traps, water bottles, and a multiple corer. Preliminary data on characteristics of the disturbed and resettled sediment layer obtained during the 1997 monitoring cruise are presented and discussed.
机译:为了预测挖掘多金属结节的潜在影响,1995年进行的互相联合组织(IOM)在Clarion-Ccripperton骨折区内的先驱地区的底晶冲击实验(IOM BIE)。 IOM BIE学习涉及1997年的扰动(基线),干扰和后扰动阶段以及随后的监测采样。数据和实验前后收集的底部沉积物的物理和化学特性的数据比较在这些特征中显示了改变。在由沉积物陷阱,水瓶收集的材料上确定营养素(硅酸盐,硝酸盐,亚硝酸盐和磷酸盐)和重金属(Cu,Zn,Pb,Cd)以及矿物学的矿物学和晶粒尺寸组成,和一个多念头。提出并讨论了在1997年监测巡航期间获得的受扰动沉积层特性的初步数据。

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