引田湾に隣接する森林流域からの物質流出機構と流出負荷量 SOLUTE RUNOFF SYSTEM AND RUNOFF LOAD FROM THE FORESTED BASIN ADJACENT TO HIKETA BAY

Access this Article

Author(s)

Abstract

Hiketa bay is located in southwest of Harima-Nada where the red tide happens frequently. For estimating the solute runoff system to Hiketa bay from a surrounding forested basin, water quality observation was executed in Umayado river basin adjacent to the bay. The following findings were obtained. (1) The seasonal change of the stream water quality was not seen, as for the solute like NO<SUB>3</SUB><SUP>-</SUP>. It is thought that the paucity of precipitation caused it. (2) Rain that exceeds 100mm influences the stream water quality system of about one month after the rainfall event. (3) The dam in the upstream decreases the concentration of NO<SUB>3</SUB><SUP>-</SUP> and SO<SUB>4</SUB><SUP>2</SUP><SUP>-</SUP>. However the concentration of SiO<SUB>2</SUB> and T-Fe were not influenced. (4) The amount of SiO<SUB>2</SUB> supplied from the forested basin in a year equals the amount of SiO<SUB>2</SUB> that always exits in Hiketa Bay. (5) The heavy rain caused by the seasonal rain front and the typhoon is the key role of SiO<SUB>2</SUB> and T-Fe runoff system in the basin.

Journal

  • PROCEEDINGS OF HYDRAULIC ENGINEERING

    PROCEEDINGS OF HYDRAULIC ENGINEERING (51), 1165-1170, 2007

    Japan Society of Civil Engineers

Codes

  • NII Article ID (NAID)
    130003842379
  • Text Lang
    UNK
  • ISSN
    0916-7374
  • Data Source
    J-STAGE 
Page Top