Carbon and nitrogen relationship in soil N Transformation of a forest ecosystem
Project/Area Number |
08660188
|
Research Category |
Grant-in-Aid for Scientific Research (C)
|
Allocation Type | Single-year Grants |
Section | 一般 |
Research Field |
林学
|
Research Institution | KYOTO UNIVERSITY |
Principal Investigator |
TOKUCHI Naoko Kyoto University, Graduate School of Agriculture Instructer, 農学研究科, 助手 (60237071)
|
Co-Investigator(Kenkyū-buntansha) |
NAKANISHI Asami Kyoto University University Forest Instructer, 農学部・附属演習林, 助手 (60273497)
|
Project Period (FY) |
1996 – 1998
|
Project Status |
Completed (Fiscal Year 1998)
|
Budget Amount *help |
¥2,500,000 (Direct Cost: ¥2,500,000)
Fiscal Year 1998: ¥700,000 (Direct Cost: ¥700,000)
Fiscal Year 1997: ¥700,000 (Direct Cost: ¥700,000)
Fiscal Year 1996: ¥1,100,000 (Direct Cost: ¥1,100,000)
|
Keywords | forest ecosystem / forest soil / N cycling / N transformation / nilrification / energy source / 窒素無機化能 / 可水溶性有機物 / 腐植 / 窒素無機化過程 / 無機態窒素 / 可水溶性炭素 / 微生物 |
Research Abstract |
The objectives of this study are to describe the relationship between the form of inorganic N and C and to evaluate the importance of C as energy source for N cycling. We studied the transect along a slope under the same aged Cryptomeria plantation in Mt. Ryuoh, Shiga prefecture. 1. Topographical variation of soil N transformation ; Although there was no significant difference in N mineralization rate, nitrification rate was different between the positions of the slope. Nitrification ratio to mineralization was almost 100% at the lower slope, while no nitrification occurred at the upper part of the slope. At the middle part of the slope, patchy distribution of high nitrification and low nitrification was shown. 2. Controlling factor of net soil N transformation ; Soil moisture content, total C and N, water extractable organic C and N (ex. C and N) and pH were investigated along the transect. The principle analysis showed nitrification was the function of ex. C, ex. N and moisture content, while mineralization was the function of total C and N.it indicated that nitrification was controlled by available substrate, mineralization was regulated by total substrate. 3. Controlling factor of gross soil N transformation ; Gross soil N transformation was investigated by using 15N dilution method. The high gross N mineralization and nitrification were shown at the lower part of the slope, It was consistent with the low soil C/N.At the upper part of the slope, low mineralization, low nitrification and high soil C/N was shown, It suggests that C is limiting under low C/N at the lower part of the slope and autotrophic nitrification dominated.
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Report
(4 results)
Research Products
(11 results)