Research on geoenvironmental dynamics of coastal and alluvial lowlands
沿海和冲积低地地质环境动力学研究
基本信息
- 批准号:19300308
- 负责人:
- 金额:$ 12.48万
- 依托单位:
- 依托单位国家:日本
- 项目类别:Grant-in-Aid for Scientific Research (B)
- 财政年份:2007
- 资助国家:日本
- 起止时间:2007 至 2010
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
In this study, we discussed on the evolution and geo-environment of alluvial and coastal lowlands in relation to natural disasters and environmental change. The landforms of the alluvial lowlands have developed in response to sealevel and climate changes during the postglacial age.The Tsugaru, Noubi and Echigo plains were the target plains, and the sedimentation rate and the evolution process of the alluvial lowlands were discussed by 10^3 or 10^2 years.As a result, it was found that the eruption of Towada had a great influence on the geo-environmental change in the flood plain formed by the Iwaki river and its tributaties. The aggradation of flood plain sediments in the Nobi and Tenryu plains progressed after the culmination of the Holocene transgression. In the Echigo plain, the rate of the sedimentation is almost equivalent to the Holocene sealevel rise. The sedimentation rate of natural levees in the Nobi plain is about 10 times larger than that of the flood basin.Flood condition a … More nd micro-landforms of the flood plain were studied about in the plains of Thailand and Java. Flood level based on the images of RADARSAT was analyzed in relation to the topography. Based on the analysis, good relationship between flood condition and the seasonal variation of the paddy-rice planting pattern were clarified in the flood plain of central Thailand.Landform classification based on SRTM-DEM data and satellite images were done in the Thu Bon alluvial plain, central Vietnam. Good relationship between the flood condition and the topography of the plain were clarified and shown with GIS. Furthermore, formation of the acid sulfate acid soil in the Lower Central Plain, Thailand was discussed. And it was made clear that the distribution of acid sulfate soils is related to the distribution of mangrove forest which developed along the extended coastline during the middle Holocene embayment.As mentioned above, time and spatial dynamics in relation to the formation of alluvial lowland were clarified, and the relationship between the geo-environmental dynamics in alluvial and coastal plains and various issues as to natural disasters and human habitation in the lowlands were shown in this study. In addition, several researches for this study were done particularly in Southeastern Asian areas and the result may be able to contribute to the local people. Less
在这项研究中,我们讨论了与自然灾害和环境变化有关的冲积和沿海低地的进化和地理环境。冲积低地的地面是为了响应冰期冰期时代的海升和气候变化而发展起来。Tsugaru,noubi和echigo飞机是目标计划,而沉积速率和沉积率和相似低地的进化过程在10^3或10^2年之间进行了批评。伊瓦基河及其支流形成的洪水平原。在全新世犯的高潮之后,NOBI和Tenryu布局中洪水平原沉积物的聚集进展。在Echigo平原上,沉积物的速度几乎等同于全新世海平面上升。 NOBI平原上自然水平的沉积速率大约是洪水盆地的10倍。根据地形分析了基于Radarsat的图像的洪水水平。基于分析,在泰国中部的洪水平原上阐明了洪水状况与帕迪雷斯种植模式的季节性变化之间的良好关系。基于SRTM-DEM数据和卫星图像的地面分类是在越南中部的Thu Bon Bolluvial Plain中进行的。洪水状况与平原地形之间的良好关系被阐明并用GIS显示。此外,讨论了泰国下部平原下酸硫酸盐酸土的形成。而且清楚地表明,硫酸盐土壤的分布与在全新世胚胎期间沿着延伸的海岸线发展的红树林的分布有关。如上所述,与冲积低地形成有关的时间和空间动力学澄清了,以及在各种沿海地区和人类计划中的地理环境动力学之间的关系和各种问题与人类的习惯和人类之间的习惯和人类之间的习惯与自然和人类的研究之间的关系。此外,这项研究的几项研究尤其是在东南亚地区进行的,结果可能能够为当地人民做出贡献。较少的
项目成果
期刊论文数量(0)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Paleoenvironment of Acid Sulfate Soil Formation in the Lower Central Plain of Thailand
泰国中下部平原酸性硫酸盐土壤形成的古环境
- DOI:
- 发表时间:2010
- 期刊:
- 影响因子:0
- 作者:Janjirawuttikul;N.;Umitsu;M.;Vijarnsorn;P.
- 通讯作者:P.
Late Holocene evolution of the Songkhla Coastal Plain in Southern Thailand.
泰国南部宋卡沿海平原的全新世晚期演化。
- DOI:
- 发表时间:2007
- 期刊:
- 影响因子:0
- 作者:Umitsu;M.;Janjrawuttikul;N.;Tanavud;C. and Kawase;K
- 通讯作者:K
完新世後半における津軽平野の地形環境変遷
全新世后半期津轻平原地形环境的变化
- DOI:
- 发表时间:2009
- 期刊:
- 影响因子:0
- 作者:藤原治;小野映介;矢田俊文;海津正倫;佐藤善輝;Vanessa Heyvaert;小野映介;河角龍典・小野映介;佐藤善輝・小野映介;小野映介・片岡香子;佐藤善輝・藤原治・小野映介・海津正倫・鹿島薫;佐藤善輝・小野映介;佐藤善輝・藤原治・小野映介・海津正倫;藤原治・佐藤善輝・小野映介・海津正倫;堀和明・廣内大助;小野映介;堤浩之・杉戸信彦・越谷信・石山達也・今泉俊文・丸島直史・廣内大助;小野映介・宮本真二・海津正倫・上中央子
- 通讯作者:小野映介・宮本真二・海津正倫・上中央子
バンダアチェにおけるインド洋大津波の被害の地域的特徴.
印度洋海啸对班达亚齐造成的损害的区域特征。
- DOI:
- 发表时间:2007
- 期刊:
- 影响因子:0
- 作者:Umitsu;M.;Tanavud;C.;Patanakanog;B.;海津正倫・高橋 誠
- 通讯作者:海津正倫・高橋 誠
Paleoenvironment of Acid Sulfate Soil Formation in the Lower Central Plain of Thailand. Research Journal of Environmental Sciences, Academic Journals Inc.
泰国中下部平原酸性硫酸盐土壤形成的古环境。
- DOI:
- 发表时间:2010
- 期刊:
- 影响因子:0
- 作者:Janjirawuttikul;N.;Umitsu;M.;Vijarnsorn;P.
- 通讯作者:P.
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UMITSU Masatomo其他文献
The impact of the 1498 Meio earthquake on the river Hamana, Enshunada coastline, Central Japan : evidence from the sedimentary record
1498 年名王地震对日本中部远州滩海岸线滨名河的影响:来自沉积记录的证据
- DOI:
- 发表时间:
2011 - 期刊:
- 影响因子:0
- 作者:
FUJIWARA Osamu;HEYVAERT Vanessa;UMITSU Masatomo;SATO Yoshiki;ONO Eisuke;YATA Toshifumi - 通讯作者:
YATA Toshifumi
天然物合成で活躍した反応:実験のコツとポイント(有機合成化学協会編)
天然产物合成中使用的反应:实验技巧和要点(有机合成化学协会编辑)
- DOI:
- 发表时间:
2011 - 期刊:
- 影响因子:0
- 作者:
FUJIWARA Osamu;HEYVAERT Vanessa;UMITSU Masatomo;SATO Yoshiki;ONO Eisuke;YATA Toshifumi;有本博一分担執筆 - 通讯作者:
有本博一分担執筆
UMITSU Masatomo的其他文献
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{{ truncateString('UMITSU Masatomo', 18)}}的其他基金
Research on vulnerability of the coastal lowland against tsunami in relation to the coastal landform environment
滨海低地海啸脆弱性与滨海地貌环境的关系研究
- 批准号:
26350409 - 财政年份:2014
- 资助金额:
$ 12.48万 - 项目类别:
Grant-in-Aid for Scientific Research (C)
Research on the micro landforms of the coastal and alluvial lowlands in relation to the Holocene geo-environment.
全新世地质环境与滨海冲积低地微地貌的关系研究。
- 批准号:
15300302 - 财政年份:2003
- 资助金额:
$ 12.48万 - 项目类别:
Grant-in-Aid for Scientific Research (B)
Coastal Landform Evolution and Environmental Changein the Late Holocene
全新世晚期滨海地貌演化与环境变化
- 批准号:
11480020 - 财政年份:1999
- 资助金额:
$ 12.48万 - 项目类别:
Grant-in-Aid for Scientific Research (B)
Landform evolution and sedimentary environment of the riverine coastal plain around the Holocene/Pleistocene boundary.
全新世/更新世边界沿河滨海平原地貌演化与沉积环境.
- 批准号:
07680185 - 财政年份:1995
- 资助金额:
$ 12.48万 - 项目类别:
Grant-in-Aid for Scientific Research (C)
Study of the Upper Sand Layer in the Late Quaternary Sediments of Japanese Alluvial Lowlands.
日本冲积低地晚第四纪沉积物上沙层的研究。
- 批准号:
63580196 - 财政年份:1988
- 资助金额:
$ 12.48万 - 项目类别:
Grant-in-Aid for General Scientific Research (C)
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