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Soil properties of the shallow type methane hydrate-bearing sediments in the Lake Baikal

机译:贝加尔湖浅层含甲烷水合物的沉积物的土壤特性

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The purpose of this study is to understand the soil properties of grounds contained shallow type methane hydrates. For this study, the surveys were conducted in the Lake Baikal, Russia in 2005-2007, existed shallow type methane hydrates, and the several kinds of tests (physical and mechanical tests) were preformed for the lake-bottom sediments. The tested samples were collected from the mud volcano ground contained shallow type methane hydrates and the reference ground at same area. From the results, it was found that the reference samples in the Lake Baikal have no marked differences in the soil properties of the sediment obtained from other sea-bottom areas. On the other hand, the strengths and shear modulus of the mud volcano samples obtained from the on-board tests were lower than those of the reference samples.
机译:这项研究的目的是了解含有浅型甲烷水合物的土壤的土壤特性。为了进行这项研究,调查于2005年至2007年在俄罗斯贝加尔湖进行,其中存在浅型甲烷水合物,并对湖底沉积物进行了多种测试(物理和机械测试)。测试样品是从含有浅层甲烷水合物的泥火山地面和相同区域的参考地面收集的。从结果中发现,贝加尔湖的参考样品在从其他海底地区获得的沉积物的土壤特性方面没有明显差异。另一方面,从机载测试获得的泥火山样品的强度和剪切模量低于参考样品。

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