巻号一覧
1 巻, 3 号
選択された号の論文の7件中1～7を表示しています
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渡辺 和衛1960 年 1 巻 3 号 p. 1-6
発行日: 1960/07/31
公開日: 2010/06/04
ジャーナル フリーPDF形式でダウンロード (750K) -
尾原 信彦1960 年 1 巻 3 号 p. 6-12
発行日: 1960/07/31
公開日: 2010/06/04
ジャーナル フリーThe author has found such an interesting fact that the concentration of saline pore water influences the bearing power of earth foundation, i. e. the more saline the concentration of pore water becomes, the more decreases the value of compression test (qu). He has attributed the cause to dispersion owing to: base, exchange activity of Na-ions. Moreover he discusses possibility of katagenesis around clay particles in an alkaline, environment under reduction potential.抄録全体を表示PDF形式でダウンロード (686K) -
土木工事における岩石風化の度合測定渋谷 長美1960 年 1 巻 3 号 p. 12-18
発行日: 1960/07/31
公開日: 2010/06/04
ジャーナル フリーThe weathering of rock loosens the combination of rock forming minerals and increases the porosity of rock, It decreases the strength of rock and forms the weakpart.
The porosity changes with degree of weathering. Therefore by measuring of the porosity we can express quantitatively on the state of the weathering of rock.
Accordingly the measurement of porosity is useful to judge the degree of the weathering of rock.抄録全体を表示PDF形式でダウンロード (928K) -
伊崎 晃1960 年 1 巻 3 号 p. 19-29
発行日: 1960/07/31
公開日: 2010/06/04
ジャーナル フリーJapanese National Railways, famous for its Kammon undersea tunnel, is now carrying out his next marine geological survey in three localities, i. e. Tsugaru, Akashi and Naruto Straits. We can have much more useful methods than in Kammon days, and so the secret of deeper, wider, and rapidswifting sea bottom is revealed step by step by tight combination of all possible survey works.抄録全体を表示PDF形式でダウンロード (1195K) -
山崎 寿雄1960 年 1 巻 3 号 p. 30-48
発行日: 1960/07/31
公開日: 2010/06/04
ジャーナル フリー1. The Northern Joso upland is a diluvial terrace consisting of two surfaces nominated Juri-face and Genpoji-face, the specific height of which in comparison with the alluvial plain are more or less 10 meters and 15-20 meters, respectively.
2. Paleozoic and Granitic rocks found in the eastern margin of this area compose the base rock under the terrace gravels. This forms a foundation of the Kanto Tectonic Basin, inclining to the south-east with considerable undulations. Between these terrace gravels and the base rocks intervene the sediments covering the whole base made up of a large scale of alternation, gravelly and muddy layers which is liore than 100 meters thick, and considered to be identified with the Narita group. Furthermore, the fine grained rocks thought to be formed in pliocene or miocene epoch is formed under the afore mentioned sediments covering a part of the northern margin of this area.
3. Due mainly to these geological environments, the deep ground-water is for more dominant in the west and southwest than any other directions, supplying groundwater to the law land of the eastern district of Kinu giver around Simodate City, thus forms an eminant flowing well zone there.
As for the groundwater of terraces themselves, the lower Jari face is superior to the Genpoji face, concerning the shallow one, while deep ground water isn't dependent on such a terrace configuration but dominated by the geological structure of the Kanto basin. In this respect, it is thought to be able to expect a considerable amount of artesian groundwater in the gravelly layers (Yamato, Shimozuma and Kyowa formations) belonging so-called “the Narita group”, although slightly inferior to thoso around Shimodate City.抄録全体を表示PDF形式でダウンロード (1967K) -
広田 孝一1960 年 1 巻 3 号 p. 49-56
発行日: 1960/07/31
公開日: 2010/06/04
ジャーナル フリーPDF形式でダウンロード (1658K) -
竹山 一郎1960 年 1 巻 3 号 p. 57-70
発行日: 1960/07/31
公開日: 2010/06/04
ジャーナル フリー南米のチリ沖に起った大地震のため、5月24日未明 (1960年) 日本の太平洋沿岸は大津波の来襲を受けた。その被害の大きかったこと、被害地域が全国的であったことは、地震国とは言いながら、日本では近年まれなことであった。詳細の調査には、まだ相当の日時を要するので、ここには、現在までの資料に基いて、その概要をお伝えしよう。抄録全体を表示PDF形式でダウンロード (1207K)
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