I am growing H. psuedoflava DSM 1084 autotrophically. When I compare cell dry weight produced to CO2 consumed, I find that more CO2 is consumed than expected.

I wonder if this is because my bacteria is accumulating an intracellular storage compound like PHA. It's been suggested to me, though, that such intracellular compounds would not necessarily affect CDW that much if PHA and biomass had similar carbon oxidation states. Therefore, I would like to know:

  • What is the oxidation state of carbon in PHA and in bacterial biomass? Are they far off from each other?
  • Could the formation of intracellular storage compounds (PHA) affect the OD-CDW correlation factor for my bacteria?
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