| Project/Area Number |
17380146
|
|---|
| Research Category |
Grant-in-Aid for Scientific Research (B)
|
| Allocation Type | Single-year Grants |
|---|
| Section | 一般 |
|---|
| Research Field |
Irrigation, drainage and rural engineering/Rural planning
|
|---|
| Research Institution | Saga University |
|---|
Principal Investigator |
SEGUCHI Masahiro Saga University, Faculty of Agriculture, Professor (20093974)
|
|---|
| Co-Investigator(Kenkyū-buntansha) |
KATO Fumio Saga University, Faculty of Agriculture, Professor (90109223)
KANDA Kohzo Saga University, Faculty of Agriculture, Professor (00117095)
TABATA Masaaki Saga University, Faculty of Science and Engineering, Professor (40039285)
加藤 治 佐賀大学, 農学部, 教授 (40038295)
|
|---|
| Project Period (FY) |
2005 – 2007
|
| Project Status |
Completed (Fiscal Year 2007)
|
| Budget Amount *help |
¥13,920,000 (Direct Cost: ¥13,200,000、Indirect Cost: ¥720,000)
Fiscal Year 2007: ¥3,120,000 (Direct Cost: ¥2,400,000、Indirect Cost: ¥720,000)
Fiscal Year 2006: ¥5,300,000 (Direct Cost: ¥5,300,000)
Fiscal Year 2005: ¥5,500,000 (Direct Cost: ¥5,500,000)
|
|---|
| Keywords | Ariake Sea / hypoxic water / dissolved oxygen / pycnocline / vertical diffusion coefficient / inorganic nitrogen / prevention block / upwelling current / アンモニア態窒素 / イトゴカイ / 塩分 / 酸素消費速度 / DO / 密度 / 成層 / 躍層 |
|---|
| Research Abstract |
The actual conditions of hypoxic water which occurred in the western interior parts of the Ariake Sea were clarified based on the data of dissolved oxygen concentration (DO), velocity (V), salinity (S) and water temperature (T) at the 30 cm height from the sea-bottom measured hourly in summer of 2005-2007 using two multi-items measures with DoPa communication system. The relationships between the occurrence of hypoxic water and vertical structure of density calculated from Sand Talong the measurement lines in longitudinal and lateral directions set in this sea area were also grasped, and it was shown that the density pycnocline were always formed at the time of the outbreaks of hypoxic water and the vertical diffusion coefficient decreased rapidly near the density pycnocline. Moreover the consumption rates of DO in the bottom layer depended largely on the amount of suspended organic mutter there. On the other hand, the analysis results of DO data during 34 years by a two-layer box model indicated that the vertical diffusion coefficients decreased rapidly, and on the contrary, the consumption rate increased largely as the density stratification parameter rose greatly in summer. The occurrence of hypoxic water in summer was due to the fact that with the formation of the density pycnocline, the vertical diffusion flux of DO from the surface layer to the bottom one in the sea-water column became more than the consumption of DO in the bottom layer. It was also presented experimentally that the installation of a triangle block with special shape on the sea-bottom was effective for prevention of the occurrence of hypoxic water in the study sea area
|
