4 Oehama Yoshida R. Kanaura Katashima Sumida R. Kasaoka Sumiyoshicho Tomioka Yokoshima Irie Seto Tenjin Furue Kounoshima Suiraku Terama Kamono Misaki

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1 33, Geoscience Rept. Shimane Univ., 33, p * ** Examination of tidal flat environment from geochemical analysis of suspended solid in relation to tidal change and of Zostera marina in Kasaoka Bay, Seto Inland Sea, Southwest Japan Hiroaki Ishiga* Erika Sano** Abstract Examination of tidal flat environment of the Kasaoka Bay in Seto Inland Sea was carried out from geochemical analysis of suspended solid (SS) in relation to tidal variation. Geochemical compositions of Zostera marina (submerged plan) was also examined for evaluation of water environment. Material filtered on quartz filter was observed using SEM and further analyzed by XRF to evaluated geochemical compositions. This method is a new examination for the SS in view point of both constituent observation and geochemical compositions. SS value varies with tidal change, namely, it increases toward the ebb tide. This is suggestive of increasing of detritus of tidal flat environment. SEM observation demonstrates that the material of the spring tide was composed of diatom mainly of Skeletonema sp. and some Chaetoceros sp. and Asterionella sp. were observed. The SS of ebb tide was fine grained detritus including fragment of biogenic material. Geochemical compositions of the SS of spring is characterized by higher contents of P 2 O 5, while that of ebb tide is enriched in heavy metals such as Zn, Cu, Cr, Fe and Mn. Although Br, F and Cl were measured for SS, iodine was not detected for all SS samples. This is suggestive of lacking of intake of iodine for diatom of these samples. Geochemical composition of Z. marina showed higher concentration of Zn, Cu, TS (total sulfur), iodine, MnO and P 2 O 5. Comparative examination of Z. marina from other localities of Seto Inland Sea shows that the Kasaoka Bay samples show higher values in Zn, Cr, MnO and P 2 O 5, suggesting enriched water environment of antholopologenic inputs. The Kasaoka Bay samples, however, show similar values to those of the Ise-Matsusaka area of Pacific Sea, excluding Zn concentration. I- P 2 O 5 diagram is useful for evaluation of nutrient competition between Z. marina and marine plankton and eutrophication of marine condition. Key words: tidal flat, sediments, multi-element geochemistry, suspended solid, Zostera marina, Kasaoka Bay, Seto Inland Sea Zn Pb Fe 3 21 Zn-Fe Rahman and Ishiga, 212a, b * Department of Geoscience, Shimane University, Matsue , Japan ** Geotechnos Co. Ltd., TOKYO SKYTREE EAST TOWER 14F, Oshiage, Sumida-ku, Tokyo, , Japan SS

2 4 Oehama Yoshida R. Kanaura Katashima Sumida R. Kasaoka Sumiyoshicho Tomioka Yokoshima Irie Seto Tenjin Furue Kounoshima Suiraku Terama Kamono Misaki Mizushimanada E N Takashima km b Imadate R. Natsume Torinoe Nagahama Satosho Oshima R. Oshimanaka Shoto a, b, c 1 3 d cm cm WT ph EC DO SS mg / L 1 2 L 1 2 km N 1 ph, EC, DO, WT, SS : 2 採水時間 潮位 ph EC DO WT SS cm ms/cm mg/l mg/l 13: : : : : : : : : : 第 1 表 : m 3 m 3 b 4 m 2 3 cm 8 cm 2 km m 2 m 3 d 1 m SS 2 L 11 2 SS X

3 41 潮位 (cm) 4 コンクリート排水溝 : :2 潮位変化曲線 1. 15: ホトトギスガイマウンド アマモ 潮位 (cm) 16: :2 18:2 最干 a b c d a 1 b 2 c d 1 1 cm 1 m kn 1 X RIX As, Pb, Zn, Cu, Cr, Ni, V, Sr, Y, Zr, Nb, Th, Sc, TS, Br, I, Cl ppm TiO 2, Fe 2 O * 3, MnO, CaO, P 2 O 5 wt% 3 TS Fe 2 O * 3

4 42 2 SS X SS : 2 SS 微量元素 (ppm) 主元素 (wt%) time As Pb Zn Cu Ni Cr V Sr Y Nb Zr Th Sc TS F Br I Cl TiO 2 Fe 2 O 3 MnO CaO P 2 O 5 13: : : : : : : : : : X Ex Zm / sed Zm sed 微量元素 (ppm) 主元素 (wt%) sample As Pb Zn Cu Ni Cr V Sr Y Nb Zr Th Sc TS F Br I Cl TiO 2 Fe 2 O 3 MnO CaO P 2 O 5 夏目 211,5, ,6, ,7, 長浜 211,6, 平均値 Ex Zm/sed 堆積物 n= ph /6/17 tide (cm) ph EC(mS/cm) DO(mg/L) DO tide (cm) WT WT( ) 7.6 EC Time ph, EC, DO, WT Time ph ph : EC 16 : 15 2 : 2 EC 2 DO 5.7 mg / L 4.4 mg / L SS SS JEOL Neo Scope JCM-5 1 kv 5 13 : : 2 21 : 5 A Skeletonema sp. Chaetoceros

5 43 A: 満潮時 13 時 15 分 μm B: 下げ潮時 16 時 15 分 C: 干潮時 18 時 2 分 D: 上げ潮時 21 時 5 分 5 SS SEM A Skeletonema sp. B C B D A Skeletonema sp. sp. Asterionella sp. B; 16 : 15 C D 6 5 A Skeletonema sp. 5 1 μm B C D A Skeletonema sp. 5 μm SS SS 2 7 SS 28.2 mg / L mg / L 1 Zn, Cu, Ni, Cr, TiO 2, Fe 2 O 3 SS 7 P 2 O 5.13 wt%.27 wt% SS TS P 2 O Zn ppm Cu, Cr, V Pb 2 ppm TS 1 wt% F ppm Br ppm I ppm Cl.7 wt% Fe 2 O wt% MnO wt% CaO wt% P 2 O wt% SS SS SEM P 2 O 5 SS

6 44 A: 満潮時 13 時 15 分 B: 下げ潮時 16 時 15 分 C: 干潮時 18 時 2 分 D: 上げ潮時 21 時 5 分 6 5 SS A Skeletonema sp. B C B 5 μm D A Skeletonema sp. EC 2 SS Nb, Zr, Th, Sc SS Ni, Cr Ni ppm Ni = 29 ppm; 13 : ppm; 21 : 5 Ni F, Br, ClI SS I I IO 3 Muramatsu et al., 4 I I 4 Zn ppm Cu 21.2 ppm Ni 16.2 ppm Cr 19.8 ppm Fe 2 O wt% MnO.243 wt% P 2 O 5.99 wt% SS 2 Zn SS 12 ppm Cu 29 ppm Cr SS 45 ppm 37.9 ppm Ni SS 29 ppm; 13 : ppm Ni Ex Zm / sed Zm sed Ex Zm / sed 1 Zn, Cu, Ni, Sr, TSMnO, CaO, P 2 O 5 3 P 2 O 5 1 SS P 2 O 5.27 wt%; 13 :

7 SS 4 25 SS 3.25 SS (mg/l) 15 Zn Fe2O3 3 2 Fe2O3 (wt%) 8 6 Zn (ppm) SS (mg/l) 15 P2O5 Cu 25 Cu (ppm).2 P2O5 (wt%) Time 7 SS SS Fe2O3, Zn, Cu P2O5 SS Time X Cl 1 wt% 微量元素 (ppm) 主元素 (wt%) sample As Pb Zn Cu Ni Cr V Sr Y Nb Zr Th Sc TS F Br I Cl TiO 2 Fe 2 O 3 MnO CaO P 2 O 5 笠岡 211 (n=4) 龍岩 (n=3) 尾道 214 (n=11) ハチ岩 212 (n=3) 上蒲刈島 211 (n=1) 松阪 212, 213 (n=13) 伊勢 213 (n=4) Zn ppm Ni 16.3 ppm Cr 19.8 ppm I 47.8 ppm P 2 O 5.91 wt% P 2 O wt% SS I P 2 O 5 SS SS Zn, Cu, Ni, Cr, TiO 2, Fe 2 O 3 Zn, Cu, Ni, MnO, Fe 2 O 3, P 2 O 5 8 I I 22.8 ppm 21 I- P 2 O I- P 2 O 5 I P 2 O 5 I P 2 O 5 I P 2 O 5 214

8 46 PO4 3-, I - 8 Zn, Fe, Ca, Mn, TS, P, I, Cl P 4 3 I- P 2 O 5 I (ppm) P2O5 (wt%) 笠岡 福山 尾道 竹原 広島 9 I- P2O I- P2O5 I- P 2 O 5 I P 2 O 5 P 2 O 5 Neckles, I- P 2 O 5 P 2 O 5 Zn- Fe 2 O 3 SS SS XRF SEM XRF I- P 2 O 5 SS SEM XRF , Zn-Fe 2 O 3

9 47 22, , ,. Muramatsu, Y., Yoshida, S., Fehn, U., Amachi, S. and Ohmomo, Y., 4, Studies with natural and anthropogenic iodine isotopes: iodine distribution and cycling in the global environment. Jour. Env. Radioactivity, 74, Neckles, H., Koepfler, E. T., Haas, L. W., Wetzei, R. L. and Orth, R. J., 1994, Dynamics of epiphytic photoaoutotrophs and heterotrophs in Zostera marina (Eelgrass) microcosms: responses to nutrient enrichment and grazing. Estuaries, 17, ,. Rahman, M. A. and Ishiga, H., 212a, Geochemical investigation of selected elements in coastal and riverine sediments from Ube, Kasado, and Suo-Oshima Bays in the western Seto Inland Sea, Southwest Japan. J. Oceanogr., 68, Rahman, M. A. and Ishiga, H., 212b, Trace metal concentrations in tidal flat coastal sediments, Yamaguchi Prefecture, southwest Japan. Environ. Monit. Assess., 184, ,

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