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  • 山口 彌一郎
    地理学評論
    1958年 31 巻 11 号 685-689
    発行日: 1958/11/01
    公開日: 2008/12/24
    ジャーナル フリー
  • 岩塚 守公
    地理学評論
    1960年 33 巻 3 号 97-104
    発行日: 1960/03/01
    公開日: 2008/12/24
    ジャーナル フリー
    Flood damages are brought frequently on the land of Japan by heavy rainfall in typhnon season (from middle August to late September) and the rainy season (from early June to middle July), and her communities suffer a large amount of loss by those damages.
    In 1958, from Sept. 26 to 27, a large scale typhoon (So called the Kanogawa Typhoon) attacked the eastern Japan (Fig, 1), and the followed heavy rainfall caused violent flood damages on several parts in these regions. The distribution of rainfall at that time was very complicateb (Fig. 2), and an extremely heavy rainfall were concentrated on the middle part of Izu Peninsula, Tokyo metropolitan area and another several regions. The characteristics of disasters, however, much differed in each regions, in accordance with their physio-and socio-characters.
    In Tokyo metropolitan area, the extensive alluvial plain develops to the east, and flood damages happened often there by overflowing from large rivers (the Arakawa, the Edogawa and Tamagawa etc.). But rainfall distribution brought by that typhoon was somewhat un usual and the rain did not concentrate on the upper part of these large river area but on the place near Tokyo Bay. So, by overflowing rlom small rivers, flood damages were more severe in and around the low upland and the hill to the west of city than on the extensive alluvial lowland along to these large rivers. The total amount of flooded houses reached to about 460 thousands at that time.
    Kanogawa is a small stream which runs in the nouthern part of Izu Paninsula. The disaster occured in the Kanogawa river basin was characterized by the violent inundation, covered almost whole lowland in this river basin, and the severe damage, caused by this inundation: for example, 1, 273 of people were killed and injured, the amount of flowed and destroyed houses exceeded the number of flooded houses and the amount of flowed and buried arable lands are much more than the quantity of flooded (Table 1).
    Chiefly from the physical points of view, we tried to make clear the causes which brought the disasters in this river basin. These causes may be briefly summarized as follows;
    1) The extremely heavy rainfall concentrated on the upper part of this river basin, and theextremely volumenous runoff took place very rapidly, because of the full saturation of the land surface by foregoing much rainfall and the steep gradient of the river and its branches.
    2) Moreover, bridges obstructed the flowing of runoff and temporarily reserved more volumenous water behind them. So, when these bridges were destroyed, the extremely volumenous runoff flowed suddenly downwards.
    3) Consequently, the volume of maximum discharge far exceeded the estimated hiqh waten dis charge flood and the bank was broken at everywhere. The bank on undercut slopes of meander course were especially destroyed than others.
    4) At the mountain region, many landslides and debris flows occurred, and the debris flows caused some damages on roads and horseradish (Wasabi) fields which are the important fields for the cash products in this region.
  • 市川 正己
    応用地質
    1960年 1 巻 2 号 30-31
    発行日: 1960/06/06
    公開日: 2010/06/04
    ジャーナル フリー
  • 高山 茂美
    地理学評論
    1958年 31 巻 8 号 486-495
    発行日: 1958/08/01
    公開日: 2008/12/24
    ジャーナル フリー
    以上のような資料処理を行つた結果知り得た若干のことがらを要約すると次のようである.
    (i) 利根川本川中流部において,河床の堆積および洗掘傾向は交互に出現し,調査期間中堆積あるいは洗掘のみが行われた時期および区間はともに存在しない.堆積および洗掘区間は時間の経過とともに下流に移行するもののようである.
    (ii) 第4図からこの区間は大略3つの部分に分けられる.すなわち,河床変動の比較的激しい区間 (A), 比較的河床変動の少い区間 (B), 河積の変動が河床高度の変動に較べて激しい区間 (C) である.
    (iii) 平均河床高変動量ど河積変動量によつて示される堆積 (+), 洗掘 (-) の傾向は同一測点において一致しない場合があつた.これは洗掘および堆積の様相が複雑なために,河床の横断面形状が極めて不規則になるからであろう.
    この稿を終えるにあたり,終始御指導を賜わつた東京教育大学の石川教授,町田助教授,市川・荒巻両理学士,その他御助言をいただいた教室関係の各位に厚く御礼申し上げる.
  • 藤井 素介
    水利科学
    1958年 1 巻 4 号 132-134
    発行日: 1958/03/01
    公開日: 2023/09/18
    ジャーナル フリー
  • 田中 正央, 森 正樹
    地理学評論
    1976年 49 巻 4 号 236-248
    発行日: 1976/04/01
    公開日: 2008/12/24
    ジャーナル フリー
    丹沢山地東北部の2地区,それぞれ3km2と4km2について,精確な崩壊地分布図(縮尺5千分の1)を1946年および1971年撮影の空中写真から作成した.
    既往の資料に基づき, 1つの中小規模の山崩れによる崩壊量を2m3/m2, 山崩れ後の崩壊裸地での岩屑生産速度を3×10-2m3/m2・year, 植被におおわれた崩壊地での岩屑生産速度を10-3m3/m2・year, 山崩れを生じたことのない植被地の土壌浸食速度を10-4m3/m2・yearと想定し, 1946年以後生じた山崩れの発生と崩壊地のその後の変遷を考慮して,最近25年間の調査地における浸食量を求めた.
    この山崩れは5年に1回発生しているとすれぽ,この25年間の年平均単位面積当りの浸食速度は, 103m3/km2・yearのオーダーである.こ一の値は,ダムの堆砂量から求められた日本各地の山地の浸食速度の比較的大きな値と等しい.
    調査地域の山崩れは小規模なものであるが,数年間隔で発生しているとみられる.こうした山崩れや土壌浸食等は,いわば定常的な浸食作用であり,それが累積すると量的には発生間隔の長い大規模山崩れに匹敵する効果を持つと考えられる.
  • 川崎市の例
    村山 良之
    東北地理
    1987年 39 巻 3 号 147-160
    発行日: 1987/08/10
    公開日: 2010/04/30
    ジャーナル フリー
    本論は, 川崎市を事例としてとりあげ, 都市水害の常襲地域の形成過程を明らかにしようとしたものである。まず常襲地域を選択し, 水害の特徴について調べ, 典型的な都市水害の常襲地域であることを明らかにした。そして, 土地条件の悪い地域の都市化が, (1) 戦中期の軍需工場進出期と, (2) 戦後の高度経済成長期 (とくに1950年代中頃~60年代初め) に, 集中的に進行したことが判明した。このうちとくに (2) の時期について, アンケート調査の結果によって居住地選択の特徴が明らかにされた。これらの地域には, 戦後をとおして“若夫婦のみ”ないし“第1子が小学生”程度の特定のライフ・ステージの家族が居住地として選択してきており, 選択の際には通勤・通学や地価・家賃といった条件が主として考慮されて, 水害のことはほとんど無視されていたのである。このような居住地選択がなされることを前提として宅地化がなされ, 結果として, 都市水害の常襲地域が形成されるに至ったと考えられる。
  • 地理学評論
    1956年 29 巻 10 号 636-686
    発行日: 1956/10/01
    公開日: 2008/12/24
    ジャーナル フリー
  • 南山城について
    小池 洋一
    人文地理
    1954年 6 巻 4 号 264-278,321
    発行日: 1954/10/30
    公開日: 2009/04/28
    ジャーナル フリー
    A flood-disaster is not a mere natural phenomenon but a regional one which figures as synthesis of natural conditions and social conditions the latter of which have influence upon the former. Starting from this point of view, I chose as the object of investigation the flood-disaster on August 15th, 1953, in the southern part of Kyoto Prefecture (Minamiyamashiro).
    The distinctive feature of the damage by the flood in Minamiyamashiro was destruction of houses and casualities done to men. Although it was partly due to the torrential rain limited to one particular locality, the immediate cause was that the dykes of the up-floored rivers, many of which are seen in this district, were broken. The flood-disaster at Ide-cho serves as an example of the damage done by the above-mentioned cause. And, the up-floored rivers in the district were made by human agency, not by nature at all. Namely, grit and sand were carried down the lower reaches of a river owing to reckless deforestation at the basin of the uppor stream; and people at the basin of the downstream made an embankment higher and higher lest the grit and sand should not flow into the ploughed land. Why, then, such land utilization as this is still conducted which is easy to cause a flood-disaster? The answer to this was worked out by analysis as to how infinitesimal peasantry who owed woodlands in the district ran their works. By the analysis were known the actual circumstances of the infinitesiman farmers who are unable to maintain themselves by any other means but reckless deforestation and cultivation of tea garden; and that woodlands denudation is made worse by the fact that there are ample funds for facilities of forest roads which promote deforestation, while there is deficiency in circulating capital for expenses of afforestation which such farmers as aforementioned can not afford. In short, what brings a flood-disaster is a contradiction between the public good (conserving water power) and the economic phase (profit made by deforestation) of woodlands.
  • 白井 義彦
    人文地理
    1962年 14 巻 2 号 146-170
    発行日: 1962/04/28
    公開日: 2009/04/28
    ジャーナル フリー
    The lower Shinano basin in Niigata prefecture is one of the main rice-producing regions in Japan, with the highest rice productivity, which results mostly from the remarkable development of water control and farm improvement. The present writer aims at the geographical study of farm improvement, mainly on the western Kanbara plain in this basin.
    Before the development of water control and farm improvement, rice production was unstable in wet paddy field under the frequent flood damages and the incomplete drainage conditions (Fig. 1). This plain was newly reclaimed from the alluvial plain with many lagoons and paddy-fields had been only partly developed till modern times. As a new region for the arable land, there was the characteristic social relationship between landowners and tenants; the rich owned high, good-conditioned paddy fields and the poor possessed remote, bad-conditioned paddy field (Table 2, Fig. 2). Land-allotment was carried out for the constant farm rent and for the equal share of the flood damage. After the allotment system disappeared in Meji Era, dispersed fields were rarely re-adjusted, as the case in Europe after the disolution of open field system (Fig. 3). The final aim of the farm improvement began since 1900's in this region is to stabilze such unstable land condition and to consolidate holdings towards rationalization in agriculture.
    The improvement process is seen geographically and historically as follow; along the Nishi river in Meiji and Taisho Eras, and a long the Shin river (in Shimogo section) and the Odori river (in Kamigo section) in Showa Era especially after the agricultural reformation, with the financial aid from the government in parallel with drainage and irrigation projects. Some areas remains unimproved in Kamigo section because of the sectional struggle for the water interest between Kamigo and Shimogo sections and because of the delay in the drainage and irrigation projects. The farm improvement in this region depends upon the condition of irrigation and drainage, and the investment from the government, owners and/or cultivators (Fig. 4, 5).
    From the point of farm improvement, the following four types of areas are pointed out; (a) Unimproved area, with horiage-den fields, remarkably dispersed, inconveniently irrigated and drained (Fig. 6, Photo. 1). (b) Improved area in Meiji Era, re-arranged rhombic-shaped, with the result of inconvenient agricultural working (Fig. 7). (c) Re-improved area for the modernization of agriculture, such as the rationalization of water use and the improvement of farm road (Fig. 8, 9). (d) Rationally improved area, upon the basis of 20a division adjustment, for the consolidation of holding, with the introduction of tractors (i.e. Lanz) (Fig. 10, Photo. 2). The future farm improvement will be developed into two directions from (a) to (d), and from (b) to (c).
  • 東京都下鶴川村における調査を例として
    西川 治
    地理学評論
    1952年 25 巻 3 号 85-99
    発行日: 1952/03/01
    公開日: 2008/12/24
    ジャーナル フリー
    The one-six hundredth cadastral maps of Japanese villages were prepared in or a little before 1873, but they are too incorrect to measure the area on them. Therefore it is now urgently necessary for our own country to make a modern correct maps of large scale and to survey land capability rind utilization in every acre by it. Such a map and the results of survey should be the most fundamental material to the improvement of landuse, and to synthetic land plannings.
    In the Land Division of the Japanese Resources Committee established in 1947 a Subcommittee was organized to research how the aerophotographs of one to 40, 000 are valuable for the understanding of real landuse, and to determine the method for the detailed land utilization survey in every piece of cultivated land to which the large scale map made from the developed aerophotograph should be adopted. This base map of one to 2, 500 in scale is to be made from the one thousandth aerophotograph by the development and amendment of distortion in aerophoto.
    The staffs of the Geographical Institute of Tokyo University and Tokyo Bunrika University were entrusted with the task to determine the method for the fine land utilization survey and to investigate land use in field under the method on that base map. They arranged to adopt the long fractional code method for the survey and its descriptions which Prof. V. Finch and D. Hudson practised and developed.
    Our survey items consist mainly of the observable phenomena in field; but they partly include the questionings to the farmer. The items are as follows: I natural elements- 1. the topographical location of each cultivated land. 2. the direction and degree of slope. 3. the duaration of sunshine. 4. the humidity of soils. 5. the color of soils. 6. soil texture. 7. the amount of gravel contained. 8. the depth of top soil. 9, the acidity of soil. 10. soil type. 11. the efficiency of irrigationa and drainage. 12. disasters (soil erosion, soil accumulation, and etc.) II human elements- 1. main sort of landuse 2. the sort of crop (intercrop, crop rotation, endicsing crop, etc.) 3. the ..width and direction of ridge, and the height of terrace. 4, tillage method. 5. weeding rnethod. 6. length of fallows. 7. the distance to the farmer's house. 8. the quantity and kind of manure given a year, 9. farmer's own land or not. 10. the age of land cleared or of land improved. 11. labor days a year. 12. the present degree of arable land.
    These items were checked to select the necessary elements in every piece of cultivated land in a section of Tsurukawa-mura of Tokyo Prefecture, included in Tama Hills, The fractional code was described in note-book. The results of the land utilization survey in Tsurukawa-mura may be described in another paper.
    The survey like this may be allowed only in sampling, for it consumes too much expenses, labor, and time. Then it is necessary to survey landuse in the smallest homogeneous unit area. For the demarcation of this unit area the thoughts of “Ökotop or natlürliche Standortseinheit” are very sugestive. The survey items on this unit area were also devised by us but were not yet checked in field.
  • 方法論的展望
    浅井 辰郎
    人文地理
    1962年 14 巻 1 号 59-72
    発行日: 1962/02/28
    公開日: 2009/04/28
    ジャーナル フリー
  • 宮越 博輔
    人文地理
    1968年 20 巻 2 号 232-248
    発行日: 1968/04/28
    公開日: 2009/04/28
    ジャーナル フリー
  • 赤峰 倫介
    人文地理
    1960年 12 巻 1 号 77-89
    発行日: 1960/02/28
    公開日: 2009/04/28
    ジャーナル フリー
  • 中野 秀治
    人文地理
    1973年 25 巻 1 号 95-113
    発行日: 1973/02/28
    公開日: 2009/04/28
    ジャーナル フリー
  • 武永 健一郎
    地学雑誌
    1968年 77 巻 1 号 37-55
    発行日: 1968/02/25
    公開日: 2009/11/12
    ジャーナル フリー
    The purpose of this paper is to classify low-altitude erosional surfaces in Japan and also to investigate the characteristic features of the granite mountains.
    Mt. Suzugamine at the western part of Hiroshima city is consisting only of granite. The geomorphic surfaces of Mt. Suzugamine are classified roughly into two, Higher-Setouchi surfaces and Lower-Setouchi surfaces. Yamada surface of the Plio-Pleistocene in origin and Piedmonttreppen belong to the former and gentle slope remnants of early-middle Pleistocene and “Kannon surface” of middle-late Pleistocene belong to the latter. Neither marine terraces nor tephra are found in this area. As a result, it is difficult to correlate these with the geomorphological surfaces elsewhere which have already been well examined.
    The gentle slopes were formed by the removal of deeply weathered granitic top soils about 50 m in thickness and the climatic change seemed to be less active.
    Landforms were modified even in Würm glacial period as was seen in the “Kannon surface”. The agencies which formed the initial gentle slope is similar to one which formed “Kannon surface”.
    Suzugamine mountains, which consists of granite, is characterized by gentle slope, box valley, earth fall, block stream, wide-opening valley and inward-opening valley. I should like to propose to term such geomorphology “granite topography”. It may be seemed that downwarping movement toward the Inland Sea (Setonaikai) has lasted down to the Pleistocene period, on the ground that the upper streams running down northward were captured by the ones running down southward.
  • 地理学評論
    1958年 31 巻 11 号 690-701_1
    発行日: 1958/11/01
    公開日: 2008/12/24
    ジャーナル フリー
  • 長谷坂 大樹
    大学経営政策研究
    2024年 14 巻 109-125
    発行日: 2024年
    公開日: 2024/06/11
    ジャーナル フリー

     This study aims to clarify the development of a student community during the late Taisho and early Showa periods. It examines the establishment of “Yokakai,” a student organization at Keio University, and the creation of the college song “Wakakichi,” to analyze the aspirations and actions of the students involved.

     The three main conclusions are as follows:

    (1) To develop a community, the students aimed to establish “Yokakai” as the executing body and “Wakakichi” as the means of realization.

    (2) The formation of “Yokakai” encountered challenges, particularly the clash between the concepts of the cross-grade “Sanshikai” and the cross-faculty “Yokakai.”

    (3) Community formation took place in cooperation with faculty members.

     During the late Taisho and early Showa periods, higher education in Japan expanded significantly. The number of students at Keio University tripled, leading to concerns about the weakening of interpersonal relationships. However, the students voluntarily sought to develop a community and navigate through this crisis.

  • 地理学評論
    1954年 27 巻 7-8 号 314-354_1
    発行日: 1954/08/01
    公開日: 2008/12/24
    ジャーナル フリー
  • 経済地理学年報
    1961年 7 巻 56-71
    発行日: 1961/05/25
    公開日: 2017/05/19
    ジャーナル フリー
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