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Biological product system around the halocline in the brackish water environment and the geological record.

Biological product system around the halocline in the brackish water environment and the geological record.
咸水环境盐跃层生物产物系统及地质记录.
批准号:
15540436
负责人:
SETO Koji
金额:
$2.3万
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:
2003
资助国家:
日本
项目状态:
已结题
起止时间:
2003 至 2005

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中文摘要
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英文摘要
Water quality and bottom sediment survey were carried out on Abashiri Lake, Aso sea, Uranouchi Bay, Notoro Lake and Nakaumi Lake and Shinji Lake in order to do this study problem. Features of the brackish environment are to be the environment where the top and bottom mixing is difficult to happen by the halocline. Therefore, the advection of water mass of bottom is mainly horizontally generated of the fresh water of the inflow side from the seaward. The bottom water mixes with the surface water, and it is discharged by the flow of the surface water. Inflow direction of surface water and bottom layer water is reverse-directional. Therefore, the weak mixing happens in the boundary of two flow. In addition, in the end of the water mass, the upwelling is generated by the river direction pushing in the tide, and the mixing becomes frequent. Therefore, the high production is maintained with the surface water by the mixture of bottom water of rich nutrient in Nakaumi Lake and Abashiri Lake, e … More tc.. Driving force of this bottom layer water circulation is water current from the river, mixed action by the wind, tide actions and so on. It continuously changes to the sediment of which only the reduced layer is seen from the sediment with thick oxidized layer in order to almost continuously shift to the end which shows absence of oxygen from entrance side which shows the environment where the bottom water is oxidative for such bottom water circulation for surface sediments. When it is considered at organic composition of the surface sediments, in entrance side which piles up in the environment where the organic substance is easy to be decomposed, the TOC contents is low. On the other hand, in end side which piles up in the environment where the organic substance is difficult to be decomposed, the TOC contents is high. In addition, the difference will be extremely possible for the TOC contents in entrance and end side of bottom water mass, since there is some the enhanced production layer near the halocline. Less
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野中崇春, 松永恒雄, 梅干野晃, 中山大介, 瀬戸浩二: "中海・宍道湖における国土交通省自動観測水質データの検証"Laguna. no.10. 101-107 (2003)
Takaharu Nonaka、Tsuneo Matsunaga、Akira Umeboshino、Daisuke Nakayama、Koji Seto:“国土交通省中海湖和宍道湖自动观测水质数据的验证”Laguna 101-107。 (2003)
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作者: []
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入月俊明, 中村雄三, 高安克己, 坂井三郎: "中海における過去約40年間の貝形虫(甲殻類)の群集変化"島根大学地球資源環境学研究報告. no.22. 149-160 (2003)
Toshiaki Iriduki、Yuzo Nakamura、Katsumi Takayasu、Saburo Sakai:“过去 40 年来中海介形类(甲壳类)群落的变化”岛根大学地球资源和环境研究报告第 22. 149-160 期。 )
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发表时间: 2005
期刊: Journal of Micropalaeontology 24・2
影响因子: --
作者: [Takata, H., Seto, K., Sakai, S., Tanaka, S., Takayasu,K]
通讯作者: Takayasu,K
DOI: --
发表时间: 2005
期刊: Journal of Micropalaeontology 24.2
影响因子: --
作者: [Takata, H., Seto, K., Sakai, S., Tanaka, S., Takayasu, K.]
通讯作者: K.
20
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    • 批准号:
      21651009
    • 项目类别:
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    • 资助金额:
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    • 财政年份:
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    • 依托单位:
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    • 批准号:
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    • 项目类别:
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    • 资助金额:
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    • 财政年份:
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    • 负责人:
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    • 依托单位:
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