文献一覧: 白 (著者) - Ceek.jp Altmetrics

The purpose of this paper is to shed light on the significance of education research by elementary school teachers in Japan from 1901 to 1903, through an analysis of Ōse Jintarō's theory of pedagogy as a science and through activities of the Society for Pedagogy and Educational Methods.In Japan after 1897, why did action-training-research come to be emphasized in education research? Why was school teacher's education research considered to be linked to pedagogy study? This paper focuses on Ōse's theory and activities to answer these questions. The Society for Pedagogy and Educational Methods, formed in 1901, is an important resource that provides an understanding of the history and origins of school teacher's education research. It is necessary to research Ōse's theory as the basis for this research. How was Ōse's theory related to the activities of school teachers' education research and the Society of Pedagogy and Educational Methods?This paper reveals three facts. First, in order to establish pedagogy study as an independent science, Ōse separated research on educational methods from research on the purpose of education, defining teacher education research as educational methods research. Second, influenced by Ernst Meumann's experimental pedogogy study, Ōse attempted to transform teachers into educational methods researchers. Ōse abandoned experimental psychological research methods. Third, Ōse established the Society for Pedagogy and Educational Methods in order to organize education scholars involved in Higher Normal School, Imperial University, and private schools for education research of pedagogy and educational methods.

2018-08-16 23:15:03
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1 0 0 0 空間的セリエーションの実践 : 北白川C式を素材として

著者: 白川綾
出版者: 日本考古学協会 ; 1994-
雑誌: 日本考古学 (ISSN:13408488)
巻号頁・発行日: no.43, pp.1-20, 2017-05

2018-08-16 11:14:21
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https://ci.nii.ac.jp/naid/40021237015

1 0 0 0 OA 二重奏音からの基本周波数分離抽出

著者: 白土保
出版者: 一般社団法人日本音響学会
雑誌: 日本音響学会誌 (ISSN:03694232)
巻号頁・発行日: vol.54, no.10, pp.715-719, 1998-10-01 (Released:2017-06-02)

二重奏音から, 個々の単音の基本周波数を分離抽出する手法と提案した。本手法は, 対象音の音響的性質に関して二つの穏やかな制約:(1)単音や調波複合音に類似しており, 低次の調波成分のパワーは他の部分音のパワーに比べ概して大きい, (2)二重奏音のパワースペクトルはそれぞれの単音のパワースペクトルの和として近似できる, ものを仮定している。このため本手法は, 対象とする楽器固有の音響特性やad hocなシステムパラメータを用いることなく幅広い範囲の二重奏音に対して適用することができる。また, 本手法では統計的検定手法を導入することにより, 基本周波数比が1:n(ただしnは2以上の整数)の関係, すなわち調波的関係の単音からなる二重奏音からの基本周波数の分離抽出を可能にしている。ヴァイオリン二重奏音, フルート二重奏音, 及び1台のピアノによるピアノ二重音に対し基本周波数分離抽出実験を行った。その結果, 調波的関係の単音からなる二重奏音に対し60〜90%程度, それ以外の二重奏音に対し90%程度の正解率で演奏された音名を同定でき, 本手法の有効性が確認された。

2018-08-15 19:32:00
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1 0 0 0 Violin 二重奏音からの基本周波数の分離抽出

著者: 白土保
雑誌: 日本音響学会音楽音響研究会資料
巻号頁・発行日: vol.14, no.4, pp.1-8, 1995
被引用文献数: 1

2018-08-15 19:30:58
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https://ci.nii.ac.jp/naid/10022356332

1 0 0 0 OA 牡丹

著者: 北原白秋[作詞]
出版者: ビクター
巻号頁・発行日: 1931-09

2018-08-15 02:44:24
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http://dl.ndl.go.jp/info:ndljp/pid/1320608

1 0 0 0 OA 城ケ島の雨

著者: 北原白秋[作詞]
出版者: ビクター
巻号頁・発行日: 1935-12

2018-08-15 02:44:24
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http://dl.ndl.go.jp/info:ndljp/pid/1328792

1 0 0 0 訪問看護師のとらえる臨死期における在宅終末期がん療養者の家族介護者の体験と支援に関する質的研究

著者: 齋木千尋伊藤絵梨子田髙悦子有本梓大河内彩子白谷佳恵臺有桂
出版者: 一般社団法人日本地域看護学会
雑誌: 日本地域看護学会誌 (ISSN:13469657)
巻号頁・発行日: vol.18, no.1, pp.56-64, 2015

目的:本研究では,訪問看護師のとらえる臨死期にある在宅終末期がん療養者の家族介護者の体験と支援を明らかにすることを目的とした.方法:対象は,関東圏A市内に所在する2か所の訪問看護ステーションに勤務する訪問看護師である.管理者より熟練訪問看護師として推薦され,かつ在宅終末期がん療養者と家族介護者に対する支援の実務経験が3年以上,おおむね10事例を有する者5人である.臨死期にある在宅終末期がん療養者の家族介護者の体験と支援について半構成的面接を行い,質的帰納的に分析した.結果:臨死期の家族介護者の体験について分析した結果,【在宅での看取りの決意とジレンマ】【家族の死の接近に対する知覚と混乱】【家族間の意思や感情の衝突と再結集】【家族の最期の瞬間の立ち会いと看取り】【家族の死の体験の振り返りと意味づけ】の5つのカテゴリーが抽出された.また支援については【臨死に揺れ動く家族の繊細な思いに対する見守りと対処】【在宅での看取りに必要な家族の資源力の引き出し】【看取りに求められる家族の心身の健康と日常生活の保障】の3つのカテゴリーが抽出された.考察:臨死期における在宅終末期がん療養者の家族介護者への支援においては,臨死期の家族が看取りの過程におけるさまざまな体験を乗り越えるとともに,家族がその後の人生も主体的に生きていけるよう,成長のプロセスを支えることが重要である.

2018-08-14 17:46:35
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1 0 0 0 近世イタリア君主国の行政機構による軍隊の管理・統制について : イタリア戦争末期のフェッラーラ砲兵隊『戦争器材に対する支出簿』の分析から

著者: 白幡俊輔
出版者: 世界史研究会
雑誌: 世界史研究論叢 = The journal of world history research (ISSN:2186442X)
巻号頁・発行日: vol.7, pp.1-22, 2017-10

2018-08-14 15:06:26
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https://ci.nii.ac.jp/naid/40021408212

1 0 0 0 IR 八重山群島石垣島・西表島の地質

著者: 中川久夫土井宣夫白尾元理荒木裕 Hisao Nakagawa Nobuo Doi Motomaro Shirao Yu Araki 東北大学理学部地質学古生物学教室日本重化学工業株式会社盛岡工業所 (盛岡市) 徳本寺 (東京都台東区西浅草) 長谷地質調査事務所 (仙台市)
出版者: 東北大學
雑誌: 東北大學理學部地質學古生物學教室研究邦文報告 = Contributions from the Institute of Geology and Paleontology Tohoku University (ISSN:00824658)
巻号頁・発行日: vol.84, pp.1-22, 1982-03-29
被引用文献数: 2

Ishigaki-jima and Iriomote-jima are the largest two islands of Yaeyama Gunto in the westernmost part of the Ryukyu Islands. Major startigraphic units on them are pre-Eocene Ishigaki Group, Upper Eocene Miyara Group, Lower Miocene Yaeyama Group, Sonai Conglomerate of unknown age, Pleistocene Ryukyu Group and the recent coastal and fluvial deposits. The Ishigaki Group comprises the Tomuru and Fusaki Formations. The Tomuru Formation occurs in the northeastern, east central and northwestern parts of Ishigaki-jima and in the eastern part of Iriomote-jima. Rocks are glaucophane schist, graphite schist, quartz-mica schist, phyllite, green and black schists and basalt. Maximum thickness is 2100 m. The Fusaki Formation crops out in the west central to southwestern part of Ishigaki-jima and on Taketomi-Jima, a small island to the southwest of Ishigaki-jima. It consists of sandstone, shale, phyllite, chert and limestone. The measured section in the southwestern part of the island is about 400 m. No fossils have been found in the Ishigaki Group. The sedimentary rocks of the Fusaki Formation are bounded on the east and northwest by the metamorphic rocks of the Tomuru Formation, but the relation between them remains uncertain because of poor exposure along the boundary. The estimated boundaries pass through the central part of Ishigaki-jima in north direction and the northwestern part in northeast direction. In the central part of the island, the boundary extends northward to the eastern margin of the granitic intrusion, along which dunite crops out in a few places. The Miyara Group comprises the Miyaragawa and Nosoko Formations. The Miyaragawa Formation unconformably overlies the Ishigaki Group in many places of Ishigaki-jima and in a small area in the eastern part of Iriomote-jima. It consists of conglomerate, an alternation of sandstone and siltstone and limestone. The limestone is biogenic and cotains well preserved fossils of the Late Eocene age. Fossils occur also in the conglomerate, sandstone and siltstone. Thickness of the Miyaragawa Formation is about 80 m. The Nosoko Formation overlies conformably the Miyaragawa Formation and unconformably the Ishigaki Group. The Nosoko Formation is distributed mainly in the northeastern and northwestern parts of Ishigaki-jima and in the eastern part of Iriomote-jima. It consists largely of andesite, dacite and tuff breccia, but includes conglomerate and sandstone, which yielded fossils. The pyroclastic rocks of the Nosoko Formation are altered and colored green ; they closely resemble the so-called green-tuff of the Early to Middle Miocene in the mainland of Japan. However, the fossils from the interbedded conglomerate and sandstone indicate the Late Eocene age. Total thickness of the Nosoko Formation is about 400 m. Granitic rocks intrude the Ishigaki and Miyara Groups in the northwestern part of Ishigaki-jima. The rocks are biotite adamellite and biotite granite which are accompanied by biotite-hornblende-augite quartzdiorite, granodiorite, dacite and rhyolite. In contact with the intrusions, the rocks of the Ishigaki and Miyara Groups are metamorphosed into hornfels. K-Ar age of the biotite adamellite is 21 Ma. The Yaeyama Group includes the Iriomote Formation, which occupies most part of Iriomote-jima. The Iriomote Formation consists of conglomerate, sandstone and siltstone. By the predominant lithofacies, the Iriomote Formation is subdivided into seven beds ; they are called with the letters A to G, in ascending order. Among them, the bed F is characterized by coal layers interbedded with an alternation of siltstone and silty sandstone, and is named the Uchiba-narejima Coal-bearing Member. The conglomerate and sandstone yielded molluscan and other fossils. The sandstone of the bed C and G are partly fossiliferous, and in places they grade into calcarenite and shell-limestone which form small lenses. Total thickness of the Iriomote Formation amounts to 700 m. The Sonai Conglomerate is distributed in several places in the north central to western part of Iriomote-jima. It unconformably overlies the Iriomote Formation. The conglomerate consists mostly of rounded cobbles, but includes pebbles and boulders in palces. Predominant rocks of cobbles are sandstone in the northern part and limestone and sandstone in the western part of the island, most of which are derived from the Iriomote Formation. The limestone cobbles contain larger foraminifera of the Early Miocene age. Maximum thickness of the conglomerate is 80 m. The Ryukyu Group includes the Ohama Formation on Ishigaki-jima and the Sumiyoshi Formation on Iriomote-jima. The Ohama Formation overlies the Nosoko and older formations with unconformity, and the Sumiyoshi Formation overlies the Sonai Conglomerate and older formations with unconformity. Distribution of the Ryukyu Group is limited to the area less than 70 m above sea level. In the inland area of Ishigaki-jima, the Ohama Formation consists of gravel, sand and clayey silt. The main part of the formation in the coastal area consists of detrital, foraminiferal, algal and coral limestones. The Ohama Formation occupies large area on Ishigaki-jima. Depositional surface is preserved between 20 and 70 m above sea level. The Sumiyoshi Formation is distributed in small areas along the coast of Iriomote-jima except the south coast. It consists of detrital, algal and coral limestones. Depositional surface is between 20 and 40 m above sea level. The Ryukyu Group on Ishigaki-jima and Iriomote-jima is correlated with the younger part of the Ryukyu Group in Amami-Okinawa Gunto. The recent deposits include coral reefs, beach sand and gravel, dune sand, fluvial clay, sand and gravel and residual soils. Deposits of cave and fissure in the limestone of the Ohama Formation yielded various remains of land animals.