Response of soil respiration to climate across biofuel crops and land use histories

Land use change (LUC) due to the worldwide increasing production of biofuel crops creates carbon debt that would require decades to repay. The payback time depends on the net ecosystem exchange (NEE) of CO2 and more determined by the carbon loss, such as soil respiration, than photosynthesis offset. Soil respiration is not only an important part of ecosystem respiration, but is also highly correlated with ecosystem production, via substrate subsidies from plants. Both autotrophic and heterotrophic soil respiration were regulated by climated-induced factors (e.g. soil temperature and soil water content) and also affected by substrate supply. In 2009, three sites in conservation reserve program (CRP) and conventional corn-soybean rotation agricultural lands (AG), were converted to soybean production, in experimental sites at Kellogg Biological Station, MI. In 2010, the three sites of differential previous land uses were then converted to corn (Cr), switchgrass (Sw) and prairie mixture (Pr) production. A reference site has been maintained CRP status since then. We used chamber-based method to assess total and heterotrophic soil respirations rate (SRRt and SRRh) from control treatment (C) and root exclusion treatment (E) at all sites, in 2011 and 2012, to explore how soil respiration rate (SRR) respond to the change of abiotic and biotic factors. Our results show that soil temperature (Ts) are important factors that affect SRR patterns. At the beginning of growing season, SRRs are low (average SRRt and SRRh are 3.19 and 3.11 umol CO2/m2s, respectively, on April 10th, 2011) when soil temperature is low. SRRs in general increased over time in a year, peaked in late July- early August, 1-2 weeks after soil temperature arrive its peak (maximum average SRRt and SRRh are 8.64 and 5.68, respectively, on August 3rd/4th, 2011). Soil water content (VWC) did not affect the time of SRR peak but limited its amount; when VWCs were extremely low in 2012 (average VWC at C and E treatment decreased 2.25% and 8.55%, respectively, in mid-summer between 2011 and 2012), SRRs were also comparatively low (average SRRt and SRRh decreased 5.57 and 3.12 umol CO2/m2s, respectively, in 2012). Besides, substrate supply importantly regulates SRRs; the patterns of SRR coincide that of crop growth through a growing season. SRRs of annual plan (corn) sites have very narrow peaks while SRRs of perennial crops (all of the rest crops in the experiment) have extended periods of highest SRRs. This may be a consequence of the difference between the phenology of annual and perennial crops. Generally, SRRh are lower than SRRt at all AG and reference sites (the difference between SRRh and SRRt are 5.23, 2.32, 3.87 and 6.03 at AG-Cr, AG-Sw, AG-Pr and reference site, respectively) in mid-summer in 2011, however, the difference between SRRh and SRRt are close at CRP sites (the difference are 1.42, 1.87 and -0.07 at CRP-Cr, CRP-Sw and CRP-Pr site). Large amount of carbon released into soil due to land use change at CRP sites would lead to high SRRh.