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The lipid extraction from the microbial biomass is a tedious and high cost dependent process.
Selective plugging by microbial biomass is one of the proposed mechanisms for improving reservoir sweep efficiency in fractured reservoirs.
This heat map shows the areas of the United States where the soil microbial biomass is susceptible to changes in vegetation cover.
The chloroform fumigation-extraction method for determining soil microbial biomass is commonly applied at soil moisture (SM) levels of 40 50% water-holding capacity (WHC).
Our work demonstrates that abundant microbial biomass is supported in C-rich buried soils while SOC is largely preserved for decades.
The soil microbial biomass is surrounded by about 50 times its mass of soil organic matter, but can only metabolize it very slowly.
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Microbial biomass was observed in all of the soils.
Nevertheless, increases in soil functionality and microbial biomass were not related to changes in microbial diversity.
Microbial biomass was inferred from the C content in the soil microbiota.
Microbial biomass was significantly (p < 0.05) higher under dry conditions compared to more mesic conditions.
The metabolic profile of the microbial biomass was accessed using substrate-induced respiration.
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