#AGU23 Tang (LBNL): Carbon use efficiency of microbes through the lense of thermal efficiency. There is a relationship between cue and uptake rate that is often not represented but thermodynamically required. We need to be more careful as a community to preserve these trade-offs.
#AGU23 Bloom (UFlorida): NWT Canada moving from Black Spruce to Jack Pine due to fire frequency. Pyrogenic carbon less susceptible to decay => model this! Was expecting pyrogenic carbon to compensate for fire driven losses. We saw losses in total carbon stocks across the board instead.
https://agu.confex.com/agu/fm23/meetingapp.cgi/Paper/1288742
Zhu (Iowa State U): Drainage of wetland prairie in Iowa led to ag land. How does drainage system (intensity & spacing) affect N2O in context of ag systems. Field flux measurements and depth flux measurements => fertilizer pulses N2O flux MUCH (x10+) bigger then freeze/thaw pulse + no drain increases N2O emissions. N2O in subsoil is inverse from surface emissions ? possibly due to microbial community anoxic conditions. Drainage reduces N2O emissions by 8 kg ha-1 yr-1.
#AGU23 Torn (Berkley Lab): Soil temperature response persist over ~10yr of field warming. Whole soil 4C to 1m deep, working on year 10; does not warm plants. Monthly collar respiration. Seeing a 30% increase in warmed vs control plots w/ annual variation; hard to see trend. Expanded sites and saw similar trends => unlikely to be a legacy site effect.
#SoilBGC https://agu.confex.com/agu/fm23/meetingapp.cgi/Paper/1265739
#AGU23 Wood (USDA-FS): Field warming in tropical forest TRACE in Puerto Rico, (+4C, soil respiration auto-chambers). Slope significantly mattered (!!! 1 order of magnitude). First, convince ourselves high flux was real => Lots of work for a "Yep". Root biomass and respiration declined but biomass and heterotrophic respiration did increase even with declining Q10 in warmed plots. Need to move beyond Q10 for tropical warming.
#SoilBGC https://agu.confex.com/agu/fm23/meetingapp.cgi/Paper/1342422
#AGU23 McMillian (UToledo): All frozen soils are not equal. 3mth -2C and -6C incubation with respiration tracked followed by a 1wk incubation gradient 2C to 10C. Colder pre-incubation temperatures respired more carbon during 1wk thaw and effect stronger with higher temperatures. Did chemistry OM changes (more simple carbon forms).
#SoilBGC https://agu.confex.com/agu/fm23/meetingapp.cgi/Paper/1403371