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1 Biosphere Sci (2010) a chl. a 6-7 chl. a 8 chl. a 6-7 chl. a m 30m 1-3 chl. a chl. a a benthic nepheloid layer bottom turbid layer Kranck, 1980; Kawana and Tanimoto 1984; Iseki et al., 1987; ; Sanford, 1993; 2004; Uncloes, 2006 O Brien et al., ; Hoshika et al., 2003; Iseki et al., m 917 m ,400ha
2 chl. a Fig. 1 Compact CTD ASTD687 2 St.18 St L 0, 5, 10, 15, 20, 30, 40m 2m B-2m 0m 200 m chl. a a chl. a 25mm Whatman GF/F N, N- DMF -20 Turner Designs 10-AU Suzuki and Ishimaru, 1990 Fig. 1. Sampling stations in Suo-sound.
3 23 Fig. 2 St.8-St.20 10m m psu psu 6-7 St.20 St.18 St m 5psu St.8 0.2m 5psu mm d mm psu St.20 St mm chl. a Fig. 3 Fig St.20 chl. a 5m 25m 8 chl. a 6-7 chl. a St.20 6 g l -1 Fig. 2. Temperature and salinity distributions in Suo-sound, summer in 2009.
4 24 Fig. 3. Vertical profiles of chlorophyll a and turbidity in Suo-sound on June 29 - July 2 and August 22-23, Fig. 4. Chlorophyll a and turbidity distributions in Suo-sound, summer in 2009.
5 St.20 St.20 2m St.18, St.14 St.8 St.5 30m St.18 Fig cm cm cm cm 0.5m 10psu chl. a St.20 Fig cm cm cm cm m psu chl. a Fig. 5. Temporal variations of temperature, salinity, chl. a, and turbidity at St.18 observed at 1-hour intervals during June 29-30, 2009.
6 26 Fig. 6. Temporal variations of temperature, salinity, chl. a, and turbidity at St.20 observed at 1-hour intervals during July 1-2, m chl. a St.20 Fig. 7 chl. a cm cm cm cm chl. a Fig. 3, chl. a 6-7 St.18 St.20 chl. a Fig. 5, 6, 8 chl. a 8 chl. a Fig. 7, 8
7 27 Fig. 7. Temporal variations of temperature, salinity, chl. a, and turbidity at St.20 observed at 1-3 hours intervals during August 22-23, Solid triangles indicate the observation time m 10cm s -1 20cm s -1 St.18 St.20 chl. a Fig. 5-7, 8 1 St.20 8 chl. a chl. a chl. a Fig St.20 TP chl. a SCM BTL DWM chl. a
8 28 中西哲也 井関和夫 宮下幸久 小池一彦 浜口昌巳 手塚尚明 Fig. 8. Relationships between chl. a and salinity, turbidity and salinity, and turbidity and chl. a at St.20 observed during July 1-2 and August 22-23, TP: Terrigeous Particles; BTL: Bottom Turbid Layer; SCM: Subsurface Chl. a Maxima; DWM: Different Water Mass 程度の連続観測が望まれる 田中ら 2004 の有明海の連続観測結果によると 大潮時前後には干潮時に 高濁度 満潮時に低濁度となる周期を持つが 小潮時には濁度は大きく低下し 大潮時前後のような濁度の 変動は明瞭でないことを報告している また 川名 1982 は 燧灘で濁度と流速の連続測定を行い 干 潮と満潮時にはほとんど流速はなく 干潮 満潮時の約3時間後に流速が大きくなり 海底付近の濁度は流 速変動と良く対応していることを述べている 周防灘 特に浅海域では 海底高濁度層の分布 変動は 河川水や潮汐周期 海底流速 異水塊の流入 生物生産などに大きく影響されるため 海底高濁度層の形成機構や物質循環機構 機能の解明にとって 河 川や 河口域から沖合域までの総合研究と連続観測の実施が不可欠と考えられる 謝 辞 本研究の実施にあたり 観測時にご協力いただいた広島大学練習船 豊潮丸 および瀬戸内海区水産研究 所調査船 しらふじ丸 の船長をはじめ乗組員の皆様に感謝の意を表します なお 本研究は 広島大学と 独 水産総合研究センター瀬戸内海区水産研究所との共同研究 瀬戸内海におけるベントスの生産性評価手 法の開発 の一環として行われ 平成21年度連携機関との共同研究 大学院生物圏科学研究科 の予算 支援を受けたことに謝意を表する
9 : Hoshika, A., Tanimoto, T., Mishima, Y., Iseki, K., Okamura, K., Variation of turbidity and particle transport in the bottom layer of the East China Sea. Deep-Sea Research II. 50: Iseki, K., Macdonald, R. W., Carmack, E., Distribution of particulate matter in the southeastern Beaufort Sea in late summer. Proc. NIPR symp. Polar Biol. 1: Iseki, K., Okamura, K., Kiyomoto, Y., Seasonality and composition of downward particulate fluxes at the continental shelf and Okinawa Trough in the East China Sea. Deep-Sea Research II. 50: : Kawana, K., Tanimoto, T., Turbid bottom water layer and bottom sediment in the Seto Inland Sea. J. Oceanogr. Soc. Japan. 40: Krank, K Variability of particulate matter in a small coastal Inlet. Can. J. Fish. Aquatic Sci. 8: a 47: B2 66: O Brien, M. C., Macdonald, R. W., Melling, H., Iseki, K., Particle fluxes and geochemistry on the Canadian Beaufort Shelf: Implications for sediment transport and deposition. Conti. Shelf Res. 26: : Roland, S.B., Isobe, A., Shimizu, M., Kabeda, A., Takeuchi, T., Takeoka, H., Circulation and material transport in Suo-Nada during spring and summer. J. Oceanogr. 58: Sanford, L.P New sedimentation, resuspension, and burial. Limnol. and Oceanogr. 3: : pp Suzuki, R., Ishimaru, T., An improved method for determination of phytoplankton chlorophyll using N, N-dimethylformamide. J. Oceanogr. Soc. Japan. 46: : J. Oceanogr. Soc. Japan. 47: Uncloes, R. J., Stephens, J. A., Law, D. J., Turbidity maximum in the macrotidal, highly turbid Humber Estuary, UK: Flocs, fluid mud, stationary suspensions and tidal bores. Estuar. Coast. Shelf Sci. 67:
10 30 Summer distribution and short-term variation of the bottom turbid layer in Suo-sound in the Western Seto Inland Sea, Japan Tetuya NAKANISHI 1), Kazuo ISEKI 2), Yukihisa MIYASHITA 2), Kazuhiko KOIKE 2), Masami HAMAGUCHI 2),3) and Naoaki TEZUKA 3) 1) Faculty of Applied Biological Science, Hiroshima University, Kagamiyama, Higashi-hiroshima, Hiroshima Japan 2) Graduate School of Biosphere Science, Hiroshima University, Kagamiyama, Higashi-hiroshima, Hiroshima Japan 3) National Fisheries Research Institute of Seto Inland Sea, Maruishi, Hatsukaichi, Hiroshima Japan Abstract During June 28 to July 2 and August 22 to 23 in 2009, we investigated the distributiosn and diurnal variations of temperature, salinity, chlorophyll a (chl.a) and turbidity in Suo-sound, Seto Inland Sea. In June to July observation, the subsurface chl.a maximum layer (SCM) and the bottom turbid layer (BTL) were found throughout the Suo-sound. In August, the SCM almost diminished but the BTL significantly developed compared to June to July observations and chl.a also showed a noticeable increase in the bottom layer. June to July and August observations corresponded with a neap and spring tides, suggesting a close relation between the development of the BTL and the tidal cycle. The turbidity values of BTL showed a maximum when temperature and salinity changed rapidly, and the distribution pattern of the BTL well-corresponded to those of temperature and salinity, particularly in spring tide in August. Particulate matter was classified into four groups such as terrigeous matter, BTL, SCM, and different water mass according to salinity-chl.a, salinity-turbidity, and chl.a-turbidity relationships. Keywords: bottom turbid water, Suo-sound, chlorophyll a, short-term variations, tidal cycle
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