Sedimentation mechanism of fine materials in Lake Biwa: With 7 figures in the text
Sedimentation mechanism of fine materials in Lake Biwa: With 7 figures in the text
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琵琶湖细粒物质的沉降机理：文中附7图
DOI：
10.1080/03680770.1987.11897981
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发表时间：
1988
期刊：
影响因子：
--
通讯作者：
S. Terashima
中科院分区：
文献类型：
--
作者：
Y. Inouchi;S. Terashima
琵琶湖位于日本中部以西，面积670平方公里，最大深度104米，平均深度40米。为了揭示”深湖”中的沉积机制，沿东西两条线沿着进行了声学（“UNIBOM”）调查，两条线之间的间隔为2公里，并对每4平方公里（164个地点）的表层沉积物样品进行了化学分析。我们提出了可能的沉积模式作为这项研究的结果。
Lake Biwa, which lies to the west of central J apan, has an area of 670 km2, maximum depth of 104 m, and mean depth of 40 m. An acoustic (" UNIBOOM") survey along the east-west lines which are arranged at 2 km interval each other and chemical analyses of surface sediment samples representing every 4 km2 (at 164 sites) were carried out in order to reveal the sedimentation mechanism in a" deep lake". W e propose possible sedimentation models as a result of this study.