Fluxes of Suspended Sediment and Dissolved Inorganic Nutrients at the Welu River Mouth in Dry and Wet Seasons in 2014

Authors

  • Anukul Buranapratheprat ภาควิชาวาริชศาสตร์ คณะวิทยาศาสตร์ มหาวิทยาลัยบูรพา
  • Suthida Kan-atireklarp
  • Suphachai Yuenyong
  • Supawat Kan-atireklap

Abstract

The researchers studied the fluxes of water, suspended sediment and dissolved inorganic nutrients in a tidal cycle at the Welu River mouth during the periods from 13 to 14 February (dry season) and from 13 to 14 August (wet season). The net fluxes of water were directed to the sea in both seasons in the amount of 14.71 million m3/day in dry season and 17.36 million m3/day in wet season. Fluxes of suspended sediment was directed seaward in dry season in the amount of 2,214.45 ton/day, and landward in wet season in the amount of 3,546.73 ton/day, opposed to the flux of water. This may be due to the resuspension of sediment on the sea floor or the coastal erosion of the outer area during the strong southwest monsoon. Fluxes of ammonia were directed seaward in wet season (3.31 kg N/day) and landward in dry season (771.13 kg N/day). There may be sources of ammonia from coastal aquaculture activities outside of the river mouth in dry season. The effect of leaching from the soil resulted in a very high silicate flux in both dry (19,946.24 kg Si/day) and wet seasons (17,882.28 kg Si/day). Fluxes of nitrate with nitrite (130.68 kg N/day) and phosphate (8.59 kg P/day) in dry season were directed landward whereas in wet season were directed seaward (1,346.07 kg N/day and 4.77 kg P/day, respectively) indicating sources from both the land and the sea. The study showed that the Welu River water was affected by dissolved inorganic nutrients from sources within the watershed and offshore. Key words: fluxes of suspended sediment, fluxes of dissolved inorganic nutrients, Welu River, Gulf of Thailand

Author Biography

Anukul Buranapratheprat, ภาควิชาวาริชศาสตร์ คณะวิทยาศาสตร์ มหาวิทยาลัยบูรพา

     

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Published

2018-03-27