MANGROVE FORMEMATION PROCESS BEHIND THE PEAT BAR AND THE AMOUNT OF THE CARBON STORAGE IN THE TIDAL FLAT
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- YAMAMOTO Koichi
- 山口大学 大学院創成科学研究科
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- MIYARA Kou
- 沖縄環境地域コンサルタント
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- KOBAYASHI Taishin
- 国土交通省中国地方整備局 松江国道事務所
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- AKAMATSU Yoshihisa
- 山口大学 大学院創成科学研究科
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- KANNO Ariyo
- 山口大学 大学院創成科学研究科
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- BASIR Noerdin
- 京都大学 防災研究所
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- KAGAWA Hiroki
- 山口大学大学院創成科学研究科
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- SUTIKNO Sigit
- Civil engineering departmet of Riau University
Bibliographic Information
- Other Title
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- 泥炭砂州の背後に形成されたマングローブの形成過程と有機炭素現存量
- デイタン サス ノ ハイゴ ニ ケイセイ サレタ マングローブ ノ ケイセイ カテイ ト ユウキ タンソ ゲンソンリョウ
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Description
For the newly formed tidal flats on Benkalis Island in Riau Province, Republic of Indonesia, its formation history and the amount of carbon deposited there were estimated from the field survey. The elevation of the coastal seafloor was initially about -1 m from MSL when tidelands began to be formed. Judging from the satellite image and the result of the field observation, the sandspits which consisted of peat particles deposited first, then the lagoon was formed behind the sandspit. After that, clay particles accumulated in the lagoon. Finally, a tidal flat with mangroves was formed at lagoon. It was found that the secondary sediments derived from the peat that had collapsed on another coast were accumulated in the tidal flat with less decomoposed.
Journal
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- Journal of Japan Society of Civil Engineers, Ser. B2 (Coastal Engineering)
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Journal of Japan Society of Civil Engineers, Ser. B2 (Coastal Engineering) 73 (2), I_1573-I_1578, 2017
Japan Society of Civil Engineers
