{"_buckets": {"deposit": "cc4e25ec-d088-45c8-b401-5d0f89c2bccd"}, "_deposit": {"id": "12120", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "12120"}, "status": "published"}, "_oai": {"id": "oai:soar-ir.repo.nii.ac.jp:00012120"}, "item_10_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\uff08\u5225\u8a00\u8a9e\u7b49\uff09\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "Preliminary report on the grain-size distribution of the surface sediments in Lake Nojiri, Central Japan"}]}, "item_10_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1987-11-30", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "1", "bibliographicPageEnd": "48", "bibliographicPageStart": "39", "bibliographicVolumeNumber": "22", "bibliographic_titles": [{"bibliographic_title": "\u4fe1\u5dde\u5927\u5b66\u7406\u5b66\u90e8\u7d00\u8981"}]}]}, "item_10_description_20": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "Grain-size analysis of muddy sediments taken from the bottom surface of Lake Nojiri was carried out by the method of JIS A 1204, so called hydrometer analysis. Most sediments are clayey silt, and six samples are silty clay. C-M pattern diagram of these sediments indicates that the most sediments are pelagic or hemipelagic, transported by suspension. Silty clay sediments whose median grain-size are larger than 8.0 phi, are distributed in a small elongated area off the Momigasaki. The locality is not the center of the lake but also not the deepest part of the lake. Such a distribution pattern seems to be related to some flow mechanisms such as a circulation current. Sediment of ST-3 off the mouth of the River Sugakawa is sandy silt. It probably results from the pour of the river. Sample of ST-31 taken from the subsurface terrace at 20 meters deep is ill-sorted gravelly sand. It seems to be relict sediment or old debris flow deposit. Sediment of ST-35 is muddy sand. It is near the southern margin of the basin plain of 36 to 38 meters in depth. 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