Spatial controls over decomposition of soil organic matterOn 2. March 2018 by Joerg
Soil microbes need to be in close proximity to their substrate to be able to efficiently decompose it. Soil organic carbon content could be a proxy for the average distance between microbes and their substrate in soil. Soil carbon content is thus an potentially important, but often overlooked control over soil organic matter decomposition. With decreasing organic matter content in soils, the probability that a microbe meets its substrate decreases which might have consequences for carbon loss dynamics and microbial strategies to decompose organic matter. In this laboratory incubation experiment at the Grandy lab at the University of New Hampshire, I investigated the effect of spatial separation of microbes and substrate, as a function of organic matter content on microbial strategy for decomposition and decomposition itself. The findings of this project have implications for our understanding of decomposition dynamics in different soil horizons, soil C modelling and management practices for C sequestration.
A. Stuart Grandy, University of New Hampshire
Department of Microbiology and Ecosystem Research
University of Vienna
Soil ecology and biogeochemistry, microbial C stabilization, climate change mitigation. Department for Microbiology and Ecosystem Science, @univienna
Link update: We are looking for 2 new PhD students for an exciting new project on permafrost soil-aquatic microbial ecology and biogeochemistry based at #McGill University and #INRS.
New link: https://d5118340-9f6d-4835-9b9a-926204256848.filesusr.com/ugd/daa7c8_3fd9bf6021fc4614b87bba3e2bff60f3.pdf
Quantifying microbial growth and carbon use efficiency in dry soil environments via 18O water vapor equilibration @AlbertoCanarini @TER_Vienna