Formative Proceesses and Geomorphological Characteristics of Coastal Sand Dunes from the view point of sediment material
Formative Proceesses and Geomorphological Characteristics of Coastal Sand Dunes from the view point of sediment material
批准号:
16500646
负责人:
KODAMA Yoshinori
金额:
$2.57万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (C)
财政年份:
2004
资助国家:
日本
项目状态:
已结题
起止时间:
2004 至 2007
中文摘要
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英文摘要
We conducted research on historical development, formation processes and characteristic of geomorphology of coastal sand dunes in Japan from the sediment material points of view. Three field sites were surveyed intensively: the Enshu-nada Sand Dune at Shizuoka Prefecture, the Katamachi Sand Dune at Niigata Prefecture and the Tottori Sand Dune at Tottori Prefecture. The width of the coastal dunes along the Enshu-nada increases from 100m to more than 1,200m towards the east from the mouth of the Tenryu River. In contrast, moving away from the mouth of the Tenryu River, the beach width decreases from 260m to 30m. We surveyed size distributions of beach sediments and beach profiles and concluded that grain size distribution of berm deposits had clue to development of coastal dunes. Interaction between wave processes and blown sand ones were discussed. On the other hand, the Katamachi Sand Dune similarly illustrates that moving away from the mouth of the Seki River; size of the coastal sand … More dune increases. Mineral compositional surveys over the drainage basin of the Seki River revealed that longitudinal dunes were developed at c.a. 80,000-50,000y.B.P., triggered by the volcanic activity of the Myoukou Volcano. Historical formative processes of the Katamachi Sand Dune explain dimensional variations of the dune. Formation processes of the Tottori Sand Dune were surveyed with boreholes (named as B5 and B6) and microtremor measurements. With facies, sequence stratigraphy, diatom, pollen, paleo magne and electorical conductivity analyses as well, we are still discussing paleo environmental changes before the formation of the sand dune. In addition, formation processes of the Oigo-Suribachi at the Tottori Sand Dune were surveyed by wind tunnel experiments and proposed its conservational provision. As for countermeasures for meadow overgrowth at the Tottori Sand Dune, we conducted field experiments for vegetation mapagement using sandblasting and seawater spraying and got some valuable results. Less
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Investigations of borehole sediments of the Tottori Coastal Sand Dune for discussing paleo environments of the initial stage of the sand dune
鸟取滨海沙丘钻孔沉积物调查探讨沙丘初期的古环境
DOI:
--
发表时间:
2004
期刊:
Bulletine of the Geological Society of Tottori No.8
影响因子:
--
作者:
[Shoumei, Okada, Yoshinori, Kodama, Shuji, Maeta, Hiroshi, Iriguchi, Sayoko, Nagahata]
通讯作者:
Nagahata
鳥取砂丘における植生被覆に伴う飛砂量の減少
鸟取沙丘植被覆盖导致风沙量减少
DOI:
--
发表时间:
2006
期刊:
鳥取大学地域学部紀要 地域学論集 3
影响因子:
--
作者:
[木村一郎, 千葉賢, 河合隆行, 森井 愛]
通讯作者:
森井 愛
Investigations for buried paleo channel of the Sendai River underneath the Tottori Sand Dune, Japan
日本鸟取沙丘下仙台河埋藏古河道的调查
DOI:
--
发表时间:
2005
期刊:
影响因子:
--
作者:
[Yoshinori, Kodama, Shoumei, Okada, Daisuke, Mori, Shinya, Nakatsukasa]
通讯作者:
Nakatsukasa
Sandblastingによる植生管理の試み-鳥取砂丘の草原化対策-
利用喷砂进行植被管理的尝试 -将鸟取沙丘变成草原的措施-
DOI:
--
发表时间:
2007
期刊:
影响因子:
--
作者:
[岡国昭明, 小玉芳敬, 前田修司, 入口大志, 長畑佐世子, 小玉芳敬]
通讯作者:
小玉芳敬
鳥取砂丘における火山灰層露出域の分布と古千代川の埋没谷〔続報〕
鸟取沙丘和古千代川埋藏河谷火山灰暴露层区域的分布[后续]
DOI:
--
发表时间:
2006
期刊:
影响因子:
--
作者:
[Yukiko, Nishita, Yoshinori, Kodama, 小玉芳敬, 小玉芳敬, 小玉芳敬]
通讯作者:
小玉芳敬
共 28 条
Elucidation of formation conditions and morphological and dynamic characteristics of meg-ripples by field measurements and wind tunnel experiments
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批准号:16K01219
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项目类别:Grant-in-Aid for Scientific Research (C)
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资助金额:$3.0万
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财政年份:2016
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负责人:KODAMA Yoshinori
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依托单位:
Preparation of Bis-GMA monomer which does not release bisphenol A
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批准号:15592045
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项目类别:Grant-in-Aid for Scientific Research (C)
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资助金额:$2.24万
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财政年份:2003
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负责人:KODAMA Yoshinori
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依托单位: