著者

飯田 汲事

出版者

愛知工業大学

雑誌

愛知工業大学研究報告. B, 専門関係論文集 (ISSN:03870812)

巻号頁・発行日

vol.15, pp.171-177, 1980-03-31

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The earthquake and tsunami damages caused by the Meio earthquake of 1498 are investigated from old documents collected to understand the damage locality and the occurrence characteristics of an earthquake in off Tokaido districts. The distribution of seismic intensity and tsunami inundation heights are also studied. About 500 kilometers along the Paciffic Coasts in Tokaido districts, Central Japan were hit by the tsunami of this earthquake. Most severe inundation heights in the range of 8 to 15 meters are estimated at the Shima Peninsula. Wave source is estimated to be located along the Nankai trough, extending up to the south of lzu Peninsula. The remarkable changes in topographical features were the appearance of the sinking of several large areas such as Hamana, Yaezu, and Tsu distridts and of the opening of the Hamana lake to the sea. It is estimated that about 8,500 houses were destroyed and about 51,000 peoples were drowned by the 1498 earthquake and tsunami. The magnitude of this earthquake is estimated at 8.3 and the epicenter at 138.1°E and 34.0°E.

著者

五島 邦治

出版者

園田学園女子大学

雑誌

史園 (ISSN:13458396)

巻号頁・発行日

vol.2, pp.1-33, 2000-09-30

著者

宮脇 真彦

出版者

早稲田大学図書館

雑誌

ふみくら : 早稲田大学図書館報 (ISSN:02898926)

巻号頁・発行日

vol.75, pp.6-7, 2007-04-25

著者

Takako Sugisawa Ichiro Kishimoto Yoshihiro Kokubo Hisashi Makino Yoshihiro Miyamoto Yasunao Yoshimasa

出版者

The Japan Endocrine Society

雑誌

Endocrine Journal (ISSN:09188959)

巻号頁・発行日

vol.57, no.8, pp.727-733, 2010 (Released:2010-09-02)

参考文献数

23

被引用文献数

23 33

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The inverse association between plasma B-type natriuretic peptide (BNP) levels and body mass index (BMI) has been reported in Western populations. Here we analyzed the relationship between plasma BNP and obesity in a general urban Japanese population. We recruited 1,759 subjects without atrial fibrillation or history of ischemic heart disease aged 38-95 years (mean age ± standard deviation 64.5 ± 10.9 years, 56.1% women, mean BMI 22.8 ± 3.1 kg/m2) from the participants in the Suita Study between August 2002 and December 2003. In multivariable regression analyses adjusted for age, systolic blood pressure, pulse rate, serum creatinine, left ventricular hypertrophy in ECG, the inverse relationships between BNP levels and BMI (kg/m2) was found in both sexes (both p<0.001). Multivariable-adjusted mean plasma BNP levels in the group of BMI<18.5, 18.5≤BMI< 22, 22≤BMI<25, and 25≤BMI were 23.4, 17.9, 14.0 and 13.0 pg/mL, respectively (trend p<0.001). The negative association of body fat (percentage and mass), skin fold thickness, or waist circumference with BNP levels was observed the negative associations in both sexes (p<0.01). Among the obesity indices, body fat mass is most tightly associated with BNP. In conclusion, plasma BNP was inversely associated with obesityrelated markers such as body fat mass, skinfold thickness and waist circumferences after adjusted for relevant covariates in a Japanese population.

著者

小林 利行

出版者

NHK放送文化研究所

雑誌

放送研究と調査

巻号頁・発行日

vol.68, no.4, pp.44-56, 2018

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本稿では、1930年前後に大人気となった松内則三アナウンサーの「講談調」の野球実況について、これまでにないアプローチでその人気の背景の再分析を試みた。本稿ではまず、「報道」「教養」「娯楽」などの放送番組の種目割合の時系列変化に注目した。そして、「娯楽」の割合が減少している時期とこの実況の全盛期が重なることを示したうえで、これをベースとして以下の3つの視点から人気の背景を探った。【①聴取者】聴取者は「娯楽」を求めていたが、実際の放送では十分に供給されておらず、「娯楽」の少なさに不満を持っていた。【②松内則三】アナウンスのあり方において常に聴取者の意向を重視していた松内が、野球実況を「講談調」にした理由の一つに①が関係した可能性が高い。【③日本放送協会】聴取者加入が外国に比べて進まない要因の一つは「娯楽」の少なさだと認識していたと思われるが、「社会の公器」という建前上、いたずらに「娯楽」を増やすわけにもいかなかった。そこに登場したのがこの実況であり、客観性に疑問符がつくアナウンスながらも容認する姿勢をとったと推察される。先行研究で指摘されているように、この実況の人気の背景には、「講談調」という日本人になじみのある口調が広く受け入れられたことがあるのは間違いない。これに上記の3つの視点を加えることで、この実況の誕生と継続の解釈に厚みが増し、従来の野球ファン以外を取り込んで大人気となった背景をより明確にできるのではないだろうか。

著者

鈴木 紀子

出版者

メヂカルフレンド社

雑誌

看護技術 (ISSN:0449752X)

巻号頁・発行日

vol.58, no.1, pp.79-81, 2012-01

著者

山口 潔子 布野 修司 安藤 正雄 脇田 祥尚 柳沢 究

出版者

日本建築学会

雑誌

日本建築学会計画系論文集 (ISSN:13404210)

巻号頁・発行日

vol.67, no.553, pp.209-215, 2002-03-30 (Released:2017-02-04)

参考文献数

16

被引用文献数

1 1

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Vigan is one of the most preserved Spanish colonial towns in the Philippines. With numerous historical buildings and houses, UNESCO registered Vigan as the World Heritage in December 1999. As an entrepot flourished by Chinese mestizo residents, Vigan forms an amalgam of native, Chinese and Spanish cultural landscape. The public spaces such as the poblacion (city center) strongly reflects Leyes de Indias (Laws of Indies): plaza surrounded by cathedral, convent, city hall, and relatively grid street pattern. Yet, deviation from the Spanish colonial city planning concept is visible, in comprising two main plazas, and in the indistinct racial residential separation. The paper is composed of : administration history of Vigan and the Philippines ;reference to the Leves de Indias colonial law and other Hispanized towns ; and considerations on block formation, road width, and lot division in Vigan. In conclusion, this paper proposes 3×3 block subdivision style and the modified use of Spanish module svstem in Vigan.

著者

森下 みさ子

出版者

日本幼稚園協会

雑誌

幼児の教育 (ISSN:02890836)

巻号頁・発行日

vol.108, no.8, pp.36-41, 2009-08-01

著者

江村, 復所

出版者

写

巻号頁・発行日

vol.[7],

著者

崎山 武志 石野 尚吾 渡辺 賢治 PLOTNIKOFF Gregory A. 許 鳳浩 FROEHLICH Claus PFLUEGER Kerstin 柳澤 紘

出版者

社団法人日本東洋医学会

雑誌

日本東洋醫學雜誌 (ISSN:02874857)

巻号頁・発行日

vol.60, no.1, pp.99-118, 2009-01-20

被引用文献数

3

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世界的に伝統医学が再認識される流れにある。東南アジアの伝統医学は古代中国に端を発し,各国独自の発展を遂げた。これら関係国間の情報交換と意思疎通の手段として,世界保健機構・西太平洋地区(WHO-WPRO)は国際標準用語集(IST)を発刊した。わが国でも,日本漢方の講義が全医学部で行われるようになった。このような流れの中で,世界の中での日本漢方の現状を把握し,どのように世界に発信していくかに関して会議を開く意義は大きいと考える。そこで日本漢方の現状と世界から見た日本漢方とその問題点,同じ古代中国医学を起源とする現代中国と韓国での現状,日本国内で漢方を専門とする医師は日本漢方をどう捉えているのか,について計3回に亘り漢方医学国際会議(仮称)を開催した。「なぜ,今,日本漢方か」の主題,世界各国の医師が日本漢方を選ぶ理由と自国の事情あるいは普及,自分にとって日本漢方はどういうものか;漢方の世界への発信ということを踏まえて,の副題のもと,在日外国医師・医学生と代表的漢方医に講師を依頼し,その後に参加者で総合討論を行った。

著者

平田 健治

出版者

大阪大学

雑誌

基盤研究(C)

巻号頁・発行日

2014-04-01

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指図による占有移転の方法による即時取得の要件は何か。この明瞭化が本研究の目的であった。その点については、ドイツ法、フランス法、英米法、さらにはローマ法の議論を参照することで、要件設定の際に考慮されるべき諸要素を析出したことが成果である。それを列挙すれば、日本の指図による占有移転の要件の沿革から見た欠陥の指摘、占有改定と指図による占有移転の方法が前提とする取引態様の定型的相違に着目すべきことの指摘、物権関係(所有権移転)と債権関係(賃貸借や寄託契約)の連携のあり方が絡むことの指摘、占有意思、とりわけ即時取得において占有意思変更を議論とすることの問題の指摘などである。

著者

中村 信隆

出版者

Japanese Association for the Contemporary and Applied Philosophy (JACAP)

雑誌

Contemporary and Applied Philosophy (ISSN:18834329)

巻号頁・発行日

vol.10, pp.1-22, 2018-07-23

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The purpose of this paper is to morally justify the death penalty according to the "expressive theory of retribution, " which has been developed by Jean Hampton. She tries to justify retributive punishment on the basis of the expressive or communicative role of punishment, arguing that retributive punishment can express and reaffirm victims' worth or dignity and their equality with offenders, which were negated by the offenders' actions. In this paper, I try to apply the expressive theory of retribution to the issue of death penalty. The problem is that it is unclear whether the death penalty is compatible with the human dignity of offenders. The first purpose of retributive punishment is to express victims' dignity, but retributive punishment must also not degrade offenders' dignity, because both victims and offenders equally have dignity. How then can imposing the death penalty on murderers be consistent with respect for their dignity? To consider this problem, I take up two questions. The first question is whether the death penalty shows implicit disregard for the human dignity of unrepentant offenders by precluding the possibility of their resipiscence as the development of their own moral character. On this question I advocate the death penalty by arguing that it does not degrade offenders' dignity as long as we provide them the opportunity of resipiscence by allowing them sufficient time between sentencing and execution. The second question is whether any method of execution is not intrinsically degrading to offenders' dignity. On this question, I argue that some methods of execution are not intrinsically degrading to offenders' dignity, and even if those methods are accused of cruelty, cruelty is in itself irrelevant for the justification of the death penalty in the expressive theory of retribution.

著者

三島由紀夫著

出版者

集英社

巻号頁・発行日

1968

著者

東京帝国大学文学部史料編纂所 編

出版者

朝陽会

巻号頁・発行日

vol.巻6, 1933

著者

山崎 きく子

出版者

一般社団法人 日本調理科学会

雑誌

調理科学 (ISSN:09105360)

巻号頁・発行日

vol.9, no.1, pp.19-24, 1976-04-10 (Released:2013-04-26)

参考文献数

3

著者

[W.H.Medhurst] [原著]

巻号頁・発行日

vol.[3], 1863

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

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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.

著者

前田 博司

出版者

The Japanese Society of Snow and Ice

雑誌

雪氷 (ISSN:03731006)

巻号頁・発行日

vol.69, no.3, pp.383-387, 2007-05-15

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2005年12月から2006年2月にかけての豪雪で,岐阜県において発生した被害について調査した.この地域では,人的被害は死者4人・重傷49人・軽傷36人,住家被害は全壊なし・半壊2棟・一部破損601棟・床上浸水なし・床下浸水7棟,非住家被害は451棟であった.被害状況は全国的な傾向とは異なり,高齢者の人的被害が特に多いとはいえず,建物の被害数も多かった.しかし,被害の程度は必ずしも甚大ではなかった.

著者

鈴木 一成 五十嵐 康人 土器屋 由紀子 赤木 右

出版者

一般社団法人日本地球化学会

雑誌

日本地球化学会年会要旨集

巻号頁・発行日

vol.55, pp.318, 2008

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東アジアのエアロゾルの水溶性成分は、Ca2+、SO42-、NH4+が主要成分となっているため、エアロゾルの化学の大部分をこの3成分で議論できる場合が多い。そこで、Ca2+, SO42-, NH4+の3成分による三角ダイアグラムを用いて大気エアロゾルの化学的特徴を考察した。三角ダイアグラムはH+を考慮する必要のある酸性領域とCO32-を考慮する必要のある炭酸領域に分けることができ、CaCO3とCaSO4、(NH4)2SO4の混合状態を簡単に知ることができる。2002年3月から9月までに富士山山頂の富士山測候所で1日ごとにサンプリングしたエアロゾル試料のデータ(Suzuki et al., in press)を用いた。富士山頂での観測結果から、春季の通常の黄砂時には、ほとんどのCa成分がCaSO4として存在することが特徴的に示された。気塊が汚染地域を通過する際に黄砂粒子と汚染大気由来のH2SO4が混合し反応したと考えられた。夏季には通常の黄砂期間と異なり、SO42-がNH4+と等量濃度でほぼ1:1であり、Ca成分がCaCO3として存在することが明らかとなった。

著者

野中 健一

出版者

日本熱帯農業学会

雑誌

熱帯農業研究 (ISSN:18828434)

巻号頁・発行日

vol.8, no.2, pp.67-70, 2015 (Released:2016-03-29)

参考文献数

7