Development of an automatic chamber system for long-term measurements of CO2 flux from roots

被引:24
作者
Dannoura, Masako
Kominami, Yuji
Tamai, Koji
Jomura, Mayuko
Miyama, Takafumi
Goto, Yoshiaki
Kanazawa, Yoichi
机构
[1] Kobe Univ, Grad Sch Sci & Technol, Nada Ku, Kobe, Hyogo 6578501, Japan
[2] Forestry & Forest Prod Res Inst, Dept Meteorol Environm, Tsukuba, Ibaraki 3058687, Japan
[3] Forestry & Forest Prod Res Inst, Kyushu Res Ctr, Kumamoto 8600862, Japan
[4] Forestry & Forest Prod Res Inst, Kansai Res Ctr, Kyoto 6120855, Japan
关键词
D O I
10.1111/j.1600-0889.2006.00216.x
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
To separate CO2 efflux from roots (R-r) and soil (R-s), we developed a system to measure R-r continuously. Using this system, seasonal variation in R-r was obtained in a temperate forest in Japan. We measured R-s, CO2 efflux from mineral soil (R-m) and environmental factors simultaneously, and the characteristic and seasonality of R-r were analysed in comparison with R-s. R-r and R-s showed different responses to soil water content: R-s decreased with decreasing soil water content, whereas R-r peaked at relatively low soil water content. R-r/R-s decreased from 64.8% to 27.3% as soil water content increased from 0.075 to 0.225 cm cm(-3). The relationship between respiration and temperature appears to change seasonally in response to phenological and biological factors. R-r showed clear seasonal variation as a function of soil temperature. During the growing period, R-r exhibited a higher rate at the same soil temperature than during other periods, which may be due to phenological influences such as fine root dynamics. R-s decreased during the summer despite high soil temperatures. The seasonal peak for R-s occurred earlier than that for soil temperature. R-r/R-s ranged between 25% and 60% over the course of the year.
引用
收藏
页码:502 / 512
页数:11
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