IQAC Image
IQAC Image
DIU Logo
QS Ranking


Our Feauture
  • Free of Cost Publishing
  • Global Exposer
  • Rigorous Peer Review
  • Prompt Publishing
  • Open Access

Paper Title


Moqsud, M. Azizul; Hayashi, Shigenori


The Ariake Sea having a unique feature is one of the best-known semi-closed shallow seas in Japan. The total area of this sea is 1700 km2 with an extended 96 km of the bay axis and an average width of 18 km. The vast tidal flat mud of the Ariake Sea, which is almost 40% of the total tidal flat area of Japan, is famous for its rich fishery products and Porphyra sp. cultivation. The tidal height at the flood tide is about 3 m in the bay mouth area, and it becomes bigger in the bay head area with the tidal height of 4.5-5.0 m. Azad et al., (2005) mentioned that many rivers flow into the eastern coast area of the Ariake Sea and carry 4.4 x 108 kg of sediments per year. Kato and Seguchi (2001) conducted tests and showed that coarse sediments accumulate in the eastern coast, and fine grains brought by the residual current accumulate in the bay head to form vast tidal flats with fine sediments. Cyranoski, 2001; Zhang et al., (2004), mentioned that environmental issues related to the Ariake Sea have been a topic of increasing interest recently and analysis of characteristics of tidal flats is of great interest to the regional population. Ariake sea is situated in the north-western part of Kyushu island in Japan. Figure 1 shows the locations of the study area along with the different types of Porphyra spp. cultivation areas. The tidal currents sweep into the sea and move northwards along the eastern shoreline and create a counterclockwise water movement [1, 3]. This would sweep the finer suspended particles delivered by rivers on the east side towards the inland end, where sedimentation would occur which was discussed by Ohtsubo et al., (1995).Azad et al., (2005) showed that sediments in the Ariake Sea tidal flats are medium sand to silty mud. Medium sand, which accounts for 71% of the total tidal flats, is located mainly in the east and south coast areas which is discussed by Azad et al., (2005). The study area Iida (33.57º N, 130.40º E), is the most affected by the acid treatment practice. The mud samples at the Iida site gave out a strong unpleasant odor due to the gas-phased hydrogen-sulphide (H2S). In the Iida tidal area, an artificial fishing land (40 x 25 m) was created to improve the tidal mud. The mixing of sand and the foamed waste glass with tidal mud was done thoroughly upto 1 meter depth. The quantity of materials in the improvement area was; clay 80% foamed waste glass 15 % and sand 5 %. Figure 2 shows the cross-section of the improvement area by using sand and the foamed waste glass in the contaminated Iida tidal flat mud. After preparing the improvement area, the baby Sinonovacula constricta shells were discharged into the improvement area. The regular monitoring of the geoenvironmental condition of this improvement area was carried out once in every month. A 90 cm long and 7 cm diameter steel tube sampler was used to collect the samples by inserting the tube sampler vertically. The most important geoenvironmental parameter for the benthos life is sulphide content. The sulphide content along with the other geoenvironmental parameters are measured in the pre specified layers. The sulphide content was measured by using the GASTEK 201 H/L methods.


Manuscript Submission
Click Here to Submit Manuscript