Characteristics of Nitrogen Outflow from Mountain Area in the Northwest of KantoPlain
| Project/Area Number |
15560439
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| Research Category |
Grant-in-Aid for Scientific Research (C)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
水工水理学
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| Research Institution | Gunma University |
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Principal Investigator |
KOBATAKE Shigeki Gunma University, Faculty of Engineering, Professor, 工学部, 教授 (00027260)
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| Co-Investigator(Kenkyū-buntansha) |
MATSUMOTO Kensaku Gunma University, Faculty of Engineering, Research Associate, 工学部, 助手 (90302455)
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| Project Period (FY) |
2003 – 2004
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| Project Status |
Completed (Fiscal Year 2004)
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| Budget Amount *help |
¥3,800,000 (Direct Cost: ¥3,800,000)
Fiscal Year 2004: ¥900,000 (Direct Cost: ¥900,000)
Fiscal Year 2003: ¥2,900,000 (Direct Cost: ¥2,900,000)
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| Keywords | Water quality of mountain stream / Nitrogen deposition / Nitrogen saturation / Transport of air pollutants / 環境汚染 |
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| Research Abstract |
The runoff characteristics of NO_3-N in forested mountain areas located in the northwest of Kanto Plain is investigated by field observation from 2001. The observation consists of two components, one is NO_3-N concentration in mountain stream water and the other is vertical profile of NO_3-N concentration in soil water. It is clarified that the large difference of NO_3-N concentration in mountain stream water exists between the west side and the east side of Tone River. Though NO_3-N concentration in soil water shows the almost similar tendency, vertical profile shows three types that do not exactly correspond to the areal distribution of concentration. By the correlation analysis, there is positive correlation between rainfall events and increase of NO_3-N concentration in mountain stream water in the east side of Tone River, where the concentration is low. On the contrary, no correlation is found out in the west side of Tone River, where the concentration is high. These phenomena correspond to the nitrogen saturation
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Report
(3 results)
Research Products
(5 results)
