Premium
Long‐Term Stimulatory Warming Effect on Soil Heterotrophic Respiration in a Cool‐Temperate Broad‐Leaved Deciduous Forest in Northern Japan
Author(s) -
Teramoto Munemasa,
Liang Naishen,
Ishida Sachinobu,
Zeng Jiye
Publication year - 2018
Publication title -
journal of geophysical research: biogeosciences
Language(s) - English
Resource type - Journals
eISSN - 2169-8961
pISSN - 2169-8953
DOI - 10.1002/2018jg004432
Subject(s) - environmental science , soil respiration , deciduous , temperate climate , global warming , soil carbon , water content , temperate deciduous forest , temperate forest , carbon cycle , atmospheric sciences , zoology , soil water , ecology , climate change , soil science , ecosystem , biology , geotechnical engineering , engineering , geology
To evaluate the long‐term response of soil organic carbon decomposition to global warming in Asian monsoon forests, we established a multichannel automated chamber system combined with infrared carbon‐filament heat lamps in a 70‐year‐old cool‐temperate broad‐leaved deciduous forest in northern Japan in September 2011. We designed control plots to measure total soil respiration ( R s ), root exclusion (trenched) plots to measure heterotrophic respiration ( R h ), and warmed trenched plots to measure R h under warmed conditions (+2.5°C soil temperature at 5 cm depth, R hw ). Annual effluxes ranged from 12.02 to 14.15 tC ha −1 in R s , 7.78 to 11.49 tC ha −1 in R h , and 8.76 to 15.25 tC ha −1 in R hw over five years (2012–2016). During the summer season (between July and September), the daily warming effect was negatively related to soil temperature. In comparison, the relationship between soil moisture and the daily warming effect varied in each year depending on soil moisture levels. The annual warming effect exhibited large interannual variation, ranging from 6.2 to 17.7% °C −1 ; however, the five year average (10.9% °C −1 ) was close to the estimated value (10.2% °C −1 ) based on the annual Q 10 of R h (2.66). Interannual variation was positively related to the number of rainy days ( p = 0.013). Our results indicate that existing global terrestrial models underestimate the strength of the feedback of R h to global warming in Asian monsoon forests, because most global terrestrial models used relatively low Q 10 values (usually below 2.0).