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  • 愛媛県松山市興居島・釣島を対象として
    武山 絵美
    農村計画学会誌
    2018年 37 巻 Special_Issue 号 183-189
    発行日: 2018/11/20
    公開日: 2019/11/20
    ジャーナル フリー

    Damage expansion by wild boar (Sus scrafa) and local farmer's intension to counter measure in Gogo-shima and Tsuru-shima islands were studied based on hearing and questioner survey. In Gogo-shima, sporadic damage phase exists for about 6 years after confirming inhabitation. After damage increase phase of about 4 years, grate damage phase has not yet started in 2017. In Tsuru-shima, a very small island, wild boar has immigrated but not colonized. Local government and university worked together to make opportunity for local people getting information and learning about wild boar. As results, local people tend to understand wild boar expansion, but to depend just only capturing as well as local government and farmers' cooperative organization.

  • 愛媛県松山市興居島を事例として
    間々田 理彦, 石黒 聡士, 淡野 寧彦, 山本 和博
    農村計画学会論文集
    2021年 1 巻 1 号 106-112
    発行日: 2021年
    公開日: 2021/11/25
    ジャーナル オープンアクセス

    In this study, to describes about significance and process of creating “hazard map with agricultural information”. Recently, hazard maps are attracting attention due to it is increase natural disasters, however, it does not take into account information related to agriculture. Therefore, we tried to creating hazard map based on a new concept in case of Yura area, Gogoshima Island in Matsuyama City, Ehime Prefecture. We emphasized the famerʼs knowledge and experience in the presses. In this study, three surveys were conducted in relation to the development of the agricultural version of the hazard map at Yura area, Gogoshima Island. The purpose of the first survey was to gather information on map making. A pre-map was developed based on the results of the first survey. The second survey used the pre-map to confirm the first survey and to add new information. In the second survey, new information was added, such as the condition of the landslide farmland and place names. The first and second surveys were conducted in a workshop format. The third survey involved reviewing the “The hazard map with agricultural information version Mar. 2020”. We then discussed how to use the maps and where to store them, but this discussion was initiated voluntarily by the farmers. The creation of the map not only fosters residentsʼ awareness of future disaster prevention and mitigation, but also serves as a model for rural communities that are resilient to disasters and can be restored and reconstructed at an early stage, and the hazard maps we created will be used in the future for inheritance of knowledge and at new disasters.

  • 佐藤 剛, 木村 誇, 廣田 清治, 鄒 青穎, 八木 浩司
    日本地すべり学会誌
    2019年 56 巻 3 号 129-134
    発行日: 2019年
    公開日: 2019/06/07
    ジャーナル フリー

      A heavy rain event in July 2018 caused many natural disasters such as landslides and floods in western Japan. Many shallow landslides were induced by heavy rain between the night of July 6 and the morning of July 7 in Gogoshima Island, which is located offshore of Matsuyama City, Ehime Prefecture. The main industry of the island is the cultivation of oranges. However, the orange farming infrastructure was devastated by shallow landslides across a large portion of the island. We created a spatial distribution map of the shallow landslides, based on interpretation of the SPOT-7 satellite imagery, to understand their characteristics. Moreover, the mass movement processes were clarified using the results of geomorphological and geological field surveys. The analysis revealed the following : 1) The shallow landslides induced by the heavy rain event were distributed across the island, and the total number of landslides was 207. 2) Relatively elongate, shallow landslides are distributed on the slopes of Mt. Kofuji. The shallow landslide materials changed to debris flows. 3) The field survey revealed that the heads of shallow landslides are located on the geological boundary between granodiorite and andesite. The landslide material was formed of loose, highly weathered granodiorite, called “masa” in Japanese, and thermally metamorphosed granodiorite. 4) The previous debris flow deposits that filled the gullies were eroded by the new debris flows and flash floods.

  • 村上 節太郎
    地学雑誌
    1933年 45 巻 7 号 356-359
    発行日: 1933/07/15
    公開日: 2010/10/13
    ジャーナル フリー
  • 井内 国光, 柿沼 忠男, 沢 資浩
    陸水学雑誌
    1990年 51 巻 2 号 79-88
    発行日: 1990/04/28
    公開日: 2009/10/19
    ジャーナル フリー
    This paper deals with the phenomena of seawater intrusion into the phreatic aquifer with an impermeable layer, by using a hydrodynamic dispersion model in both saturated and unsaturated domains. The numerical solutions by the finite-element method are obtained for various locations of an impermeable layer.
    The main results are as follows : Salt water under an impermeable layer contacted with the sea intrudes further inland with the lengthening/lowering of the impermeable layer. In the case of the lower impermeable layer, salt water intrudes inland around the inner edge of the impermeable layer. The pattern of the concentration distribution becomes close to the one obtained in the case of nonimpermeable layer with separating from the sea and shortening of the impermeable layer.
  • -高Mg安山岩から珪長質岩まで-
    新正 裕尚, 齊藤 哲
    地質学雑誌
    2017年 123 巻 8 号 571-584
    発行日: 2017/08/15
    公開日: 2017/09/05
    ジャーナル フリー

    瀬戸内火山岩類は九州東部の大野地域から愛知県東部の設楽地域にかけて,中央構造線沿いにおよそ600 kmにわたり分布する.瀬戸内火山岩類を特徴付ける岩石種のひとつである高Mg安山岩は大野地域から紀伊半島中部の範囲で見られ,松山周辺では高縄半島から防予諸島にかけて広く分布する.本巡検対象の松山周辺では,安山岩類の多くは小規模な岩頸あるいは岩脈として産するため,貫入様式の観察には好適である.さらに瀬戸内火山岩類にはピッチストーンなどを含む珪長質火山岩類も広くみられる.この珪長質火山岩類は,松山周辺では砕屑岩および火砕岩からなる高浜層群,

    興居島
    層群中に含まれる.分布は極めて狭いが多様な岩相をもつこれらの地層群についても
    興居島
    南東海岸の露頭で観察を行う.

  • 八木 繁一
    植物分類,地理
    1939年 8 巻 4 号 241-254
    発行日: 1939/12/01
    公開日: 2017/09/25
    ジャーナル フリー
  • 冀 北平, 三野 徹, 赤江 剛夫, 長堀 金造
    農業土木学会論文集
    1996年 1996 巻 182 号 207-214,a1
    発行日: 1996/04/25
    公開日: 2011/08/11
    ジャーナル フリー
    周波数領域における土壌の誘電率測定による土壌水分測定法(FDR法)を現地に適用し,その有用性を検討した.調査地点に,クロボク土普通畑およびマサ土ミカン園圃場を選び,対象深さに直接電極を設置する方法,土壌表面から長さの異なる電極を挿入する方法で50cmまで深さごとの水分を測定し,サンプリング炉乾法,テンシオメータ法の結果と比較した.クロボク土については,他の砂質系土壌と異なるキャリブレーションカーブが必要であった.FDR法と炉乾法による体積含水率の差は最大5%以内で,互いによく一致した.テンシオメータ法は約7~15%高い値を与えた.また,同一深さの土壌水分の平面的分布が迅速に測定できた.以上から,FDR法によって十分な精度で土層中の水分計測が可能であり,また測定の迅速性から土壌水分の空間的分布の把握に有望であることが確かめられた.
  • 地学雑誌
    1911年 23 巻 3 号 221
    発行日: 1911/03/15
    公開日: 2010/12/22
    ジャーナル フリー
  • 保田 仁資
    日本農村医学会雑誌
    1988年 36 巻 5 号 1023-1029
    発行日: 1988/01/30
    公開日: 2011/08/11
    ジャーナル フリー
    瀬戸内海の離島はミカンの生産地が多く, 大量の肥料および農薬を施す。さらに, これらの島の土質は花崩岩の風化土壌よりなり透水性が高くて良質の飲料水を得ることは困難である。
    ここでは
    興居島
    北浦地区における8本の井戸水の調査を行ない内陸部の井戸水と比較した。調査した項目は亜硝酸態窒素, 硝酸態窒素, アンモニア態窒素, 硫酸イオン, 塩素イオンであり, これらの陰イオンは内陸部の肱川町の2.5~13倍の濃度でありメトヘモグロビン血症の発生も予想される。硝酸態窒素と硫酸イオンはともに施肥時期より約一か月遅れて井戸水中に検出される。塩分濃度とNa/Cl比を検討した結果, 海水の浸入は考えられない。濃度相関マトリックスおよび土質柱状図から5→1→2, 8→7→2と低い2号井の方向に水が移動していることが推察される。
  • 井内 国光, 中山 祐輔, 柿沼 忠男
    地下水学会誌
    1993年 35 巻 3 号 157-163
    発行日: 1993/10/18
    公開日: 2012/12/11
    ジャーナル フリー
    Various water qualities, especially stable isotope ratios, of groundwater in shallow wells were measured, together with groundwater levels, in Gogo Island, Ehime Prefecture.
    In a coastal region of the Yura district, chloride ion concentration far greater than 200mg·1-1 (the standard value of city water) was always found and the δD versus δ18O diagram suggests that the groundwater in this region is a mixture of seawater and upstream groundwater.
    Non-dimensional values of δD, δ18O and Cl- of groundwater near the bottom of a well in a coastal region of the Yura district indicate almost the same value, and it was estimated that groundwater contained approximately 20% seawater. The vertical distribution of non-dimensional Cl- is different from those of δD or δ18O. The former indicates higher concentration in the upper part of the well. The higher concentration may be caused by the Cl source except seawater, e. g. fertilizer.
  • -愛媛県松山市全有人島を対象とした聞き取り調査に基づく考察-
    武山 絵美
    農村計画学会誌
    2016年 35 巻 1 号 33-42
    発行日: 2016/06/30
    公開日: 2017/06/30
    ジャーナル フリー
    Habitat expansion of wild boar (Sus scrafa) cross the waters in Island See is studied based on interview research conducted in all residential islands in Matsuyama City, Ehime Pref., Japan. Wild boar has immigrated around 1999 from the direction of Kashima Island, Hiroshima Pref. in the north. In A group islands where far from original habitat, sporadic damage phase exists for 6-8 years. After damage increase phase of 3-4 years, grate damage phase starts from 2009. In B group islands where near from original habitat, sporadic damage phase relatively short. In other islands far from original habitat and with very small area, wild boar has immigrated but not colonized. Gogo Island is now in sporadic damage phase, but predicted to go into damage increase phase in the near future. It is effective solution of wildlife-human conflict to make opportunity for local people getting information and learning opportunity about wild boar, as well as to monitor wild boar habitat expansion on the edge of original habitat, resulting in effective control of wild boar habitat.
  • 地学雑誌
    1894年 6 巻 2 号 116b-119
    発行日: 1894/02/25
    公開日: 2010/12/22
    ジャーナル フリー
  • 興居島の自由地下水帯における塩水汚染と肥料汚染
    井内 国光, 柿沼 忠男, 沢 資浩
    陸水学雑誌
    1988年 49 巻 4 号 237-250
    発行日: 1988年
    公開日: 2009/11/13
    ジャーナル フリー
    This paper deals with the problem of groundwater pollution caused by seawater intrusion and fertilizer dissolution into phreatic aquifers in Gogo Island, Ehime Prefecture, where the mandarin orange is widely cultivated.
    Groundwater levels, chloride ion concentrations and electric conductivities in shallow wells were measured in five districts on this island. In the Kitaura district, sulfate ion, nitrate nitrogen, nitrite nitrogen and phosphorus concentrations were also measured. In the case of the fertilizer dissolution, we propose a tank model simulating the concentration variation with time in the phreatic aquifer.
    The main results are as follows : 1) High chloride ion concentrations of far greater than 200 mg·l-1, the standard of drinking water, were always found in coastal regions of the Yura district. 2) The concentration of total ion except chloride ion, T-Cl-, increases at one to four months after fertilization, and T-Cl- correlates well with SO42- and NO3N (the multiple correlation coefficient is 0.88). 3) The predicted temporal variations of concentration by the tank model agree well with the observed T-Cl-variations by adopting relevant initial conditions and an a value which controls the fertilizer dissolution rate on the ground surface.
  • 地学雑誌
    1911年 23 巻 3 号 221a-222
    発行日: 1911/03/15
    公開日: 2010/12/22
    ジャーナル フリー
  • 井内 国光, 柿沼 忠男, 沢 資浩
    陸水学雑誌
    1989年 50 巻 3 号 207-217
    発行日: 1989/07/28
    公開日: 2009/10/19
    ジャーナル フリー
    This paper deals with the phenomena of seawater intrusion into the phreatic aquifer, by using a hydrodynamic dispersion model in both saturated and unsaturated domains. The numerical solutions are obtained by the finite- element method for various dispersion coefficients/dispersivities and precipitation intensities.
    The main results are as follows : 1) In the steady state analysis, as the value of dispersion coefficient/dispersivity gets smaller, the pattern of concentration distribution in the saturated domain changes from the strong mixing type to the moderate mixing type and a circulating current develops near the outlet of the aquifer. For relatively small dispersion coefficients/dispersivities, the degree of seawater intrusion predicted by the dispersion model agrees well with that by the fresh- salt water interface model. 2) In the unsteady state analysis, the movement of isocontours of concentration induced by a sudden change in precipitation intensity is faster in retreating than in advancing, and the smaller the value of the isocontour is, the more slowly the isocoutour moves both in retreating and in advancing.
  • 柿沼 忠男, 井内 国光, 沢 資浩
    陸水学雑誌
    1987年 48 巻 4 号 275-285
    発行日: 1987/10/30
    公開日: 2009/11/13
    ジャーナル フリー
    This report deals with the problem of contaminant transport in the saturated and unsaturated domains of phreatic aquifer. Numerical solutions by the finite-element method are obtained for fertilizer dissolution and seawater intrusion.
    The main results are as follows : 1) In fertilizer dissolution from the center of the aquifer surface, since the dispersion coefficient becomes smaller, the pattern of the steady state concentration distribution becomes more eccentric towards the outlet of the aquifer. When the dispersion coefficient increases or the precipitation intensity decreases, the concentration distribution changes more slowly to the steady state distribution. 2) With seawater intrusion, since the dispersion coefficient becomes smaller, the pattern of the steady state concentration distribution in the saturated domain chages from strong to moderate mixing, and a circulating current develops near the outlet of the aquifer.
  • 地学雑誌
    1929年 41 巻 10 号 659-660
    発行日: 1929/10/15
    公開日: 2010/12/22
    ジャーナル フリー
  • 地学雑誌
    1929年 41 巻 10 号 658-659
    発行日: 1929/10/15
    公開日: 2010/12/22
    ジャーナル フリー
  • 柿沼 忠男, 井内 国光
    日本地下水学会会誌
    1985年 27 巻 4 号 115-127
    発行日: 1985年
    公開日: 2012/12/11
    ジャーナル フリー
    This paper deals with the problem of the groundwater pollution caused by both the seawater intrusion into phreatic and confined aquifers and the fertilizer dissolution into a phreatic aquifer in Gogo Island, Ehime Prefecture.
    Groundwater levels, chloride ion concentrations and electrical conductivities in shallow wells were measured at five districts in this island during a period from August 1983 to December 1984. At Yura district, groundwater levels and chloride ion concentrations in deep wells as well as tide levels were measured.
    The main results are as follows: 1) Chloride ion concentration profiles show the rapid increase of the concentration in the neighborhood of the deep well bottom.2) Using a modified Kishi & Inouchi's model, the variation of the groundwater level and fresh water-salt water interface in response to the tide was analysed, which is applicable to the confined aquifer with an exponentially oaring thickness. It was found that the thickness of the confined aquifer estimated from this analysis is in fairly good agreement with the one obtained by boring examination.3) Very high chloride ion concentrations far greater than 200 mg⋅ 1-1, the standard value of city water, were found in coastal regions at Yura district.4) The concentration of total ions estimated by the electrical conductivity of groundwater minus the chloride ion- concentration increases at one to two months after fertilization.
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