Sustained large stimulation of soil heterotrophic respiration rate and its temperature sensitivity by soil warming in a cool-temperate forested peatland

التفاصيل البيبلوغرافية
العنوان: Sustained large stimulation of soil heterotrophic respiration rate and its temperature sensitivity by soil warming in a cool-temperate forested peatland
المؤلفون: Kentaro Takagi, Seijiro Goto, Maricar Aguilos, Munemasa Teramoto, Hitoshi Mukai, Kaichiro Sasa, Naishen Liang, Yoshiyuki Takahashi, Yoko Watanabe
المساهمون: Ministry of the Environment, Japanese Ministry of Education, Culture, Sports, Science and Technology, Japan Society for the Promotion of Sciences
المصدر: Tellus B; Vol 65 (2013)
Tellus: Series B, Chemical and Physical Meteorology, Vol 65, Iss 0, Pp 1-13 (2013)
بيانات النشر: Stockholm University Press, 2013.
سنة النشر: 2013
مصطلحات موضوعية: Hydrology, Atmospheric Science, Peat, Q10, automated-chamber, Global warming, infrared heater, Soil carbon, lcsh:QC851-999, micrometeorology, soil science, carbon balance, Agronomy, basal respiration, soil CO2 efflux, soil carbon, global warming, heterotrophic respiration, Soil water, Respiration, Temperate climate, Environmental science, lcsh:Meteorology. Climatology, Ecosystem, Q(10), Respiration rate, soil carbon stock
الوصف: We conducted a soil warming experiment in a cool-temperate forested peatland in northern Japan during the snow-free seasons of 2007–2011, to determine whether the soil warming would change the heterotrophic respiration rate and its temperature sensitivity. We elevated the soil temperature by 3°C at 5-cm depth by using overhead infrared heaters and continuously measured hourly soil CO 2 fluxes with a 15-channel automated chamber system. The 15 chambers were divided into three groups each with five replications for the control, unwarmed-trenched and warmed-trenched treatments. Soil warming enhanced heterotrophic respiration by 82% (mean of four seasons (2008–2011) observation± SD , 6.84±2.22 µmol C m −2 s −1 ) as compared to the unwarmed-trenched treatment (3.76±0.98 µmol C m −2 s −1 ). The sustained enhancement of heterotrophic respiration with soil warming suggests that global warming will accelerate the loss of carbon substantially more from forested peatlands than from other upland forest soils. Soil warming likewise enhanced temperature sensitivity slightly ( Q 10 , 3.1±0.08 and 3.3±0.06 in the four-season average in unwarmed- and warmed-trenched treatments, respectively), and significant effect was observed in 2009 ( p< 0.001) and 2010 ( p< 0.01). However, there was no significant difference in the basal respiration rate at 10°C ( R 10 , 2.2±0.52 and 2.8±1.2 µmol C m −2 s −1 ) between treatments, although the values tended to be high by warming throughout the study period. These results suggest that global warming will enhance not only the heterotrophic respiration rate itself but also its Q 10 in forests with high substrate availability and without severe water stress, and predictions for such ecosystems obtained by using models assuming no change in Q 10 are likely to underestimate the carbon release from the soil to the atmosphere in a future warmer environment. Keywords: automated-chamber, basal respiration, infrared heater, Q 10 , soil carbon stock (Published: 30 July 2013) Citation: Tellus B 2013, 65 , 20792, http://dx.doi.org/10.3402/tellusb.v65i0.20792Test
وصف الملف: application/pdf; text/html; application/epub+zip; text/plain
تدمد: 1600-0889
0280-6509
الوصول الحر: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::20e70c013436a841bc7fe905a5b2f91cTest
https://doi.org/10.3402/tellusb.v65i0.20792Test
حقوق: OPEN
رقم الانضمام: edsair.doi.dedup.....20e70c013436a841bc7fe905a5b2f91c
قاعدة البيانات: OpenAIRE