{"_buckets": {"deposit": "03ff5bdc-3bc0-4129-881f-61f68a4970b5"}, "_deposit": {"id": "33954", "owner": "1", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "33954"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00033954", "sets": []}, "author_link": ["132408", "132409", "132410", "132411", "132404", "132405", "132406", "132407"], "item_4_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "Studies on the Spring and Underground Waters in Volcano Asama and its Vicinity (1) : Chemical Compositions of the Spring and Underground Waters in the Zyabori River Valley and its Neighbourhood"}]}, "item_4_biblio_info_7": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1957-09-25", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "2", "bibliographicPageEnd": "414", "bibliographicPageStart": "395", "bibliographicVolumeNumber": "35", "bibliographic_titles": [{"bibliographic_title": "\u6771\u4eac\u5927\u5b78\u5730\u9707\u7814\u7a76\u6240\u5f59\u5831 = Bulletin of the Earthquake Research Institute, University of Tokyo"}]}]}, "item_4_description_13": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8", "attribute_value_mlt": [{"subitem_description": "application/pdf", "subitem_description_type": "Other"}]}, "item_4_description_5": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "We have carried out chemical analyses on springs and underground waters collected from 31 localities on and around the Volcano Asama. Their characteristic chemical features are as follows: (A) generally rich in \u03a3CO2; (B) mostly poor in Cl-; (C) generally poor in SO4-- with an exception of those from Zigokudani; (D) comparatively rich in H2SiO3; (E) a little rich in Ca++: (F) show a remarkable difference between RoH and pH; and (G) give the ratios K(K+Na)=5\uff5e15% and Ca(Ca+Mg)=60\uff5e70%. They are classified according to their chemical contents into three groups: type (1) containing SO4--, \u03a3CO2, Al+++ and Fe++; type (2) \u03a3CO2 and Fe++ and type (3) chiefly \u03a3CO2.", "subitem_description_type": "Abstract"}]}, "item_4_full_name_3": {"attribute_name": "\u8457\u8005\u5225\u540d", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "132408", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Ossaka, Joyo"}]}, {"nameIdentifiers": [{"nameIdentifier": "132409", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Murai, Isamu"}]}, {"nameIdentifiers": [{"nameIdentifier": "132410", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Minami, Eiiti"}]}, {"nameIdentifiers": [{"nameIdentifier": "132411", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Tsuya, Hiromichi"}]}]}, "item_4_identifier_registration": {"attribute_name": "ID\u767b\u9332", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15083/0000033954", 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