Modelling detritus mineralization by bacteria

Detritus in the marine system is degraded by the action of heterotrophic bacteria. This is not a one-step process: bacteria cannot 'eat' detritus! A model that is closer to the reality of the process considers that particulate detritus (POC) is first hydrolysed by the action of bacterial exoenzymes to high-molecular-weight dissolved organic carbon (HMWC). This carbon pool is, in turn, attacked by bacterial enzymes to yield low-molecular-weight dissolved organic carbon (LMWC), which can then be taken up by the bacteria (BACT) to grow on it. The conceptual diagram of this model is shown in the figure below.

knitr::include_graphics("Detritus.jpg")

Problem formulation

In class you have seen how to write rate expressions for ecological interactions: you need to distinguish between compartments that are actively performing the task (the "worker"), and compartments that are taken up as a result (the "resource"). This exercise is meant to make you think about these different roles that compartments may play in the model.

Tasks

Model parameters:

| parameter | value | description | units | |:-----------|:-------|:----------------------------------------|:-------| | rPOC | 0.75 | rate constant of hydrolysis of POC | $d^{-1}$ | | rHMWC | 0.5 | rate constant of hydrolysis of HMWC | $d^{-1}$ | | rUptake | 2 | uptake rate constant of LMWC by bacteria | $d^{-1}$ | | ksPOC | 0.10 | Monod constant for POC hydrolysis | $mol~C~m^{-3}$ | | ksHMWC | 0.005 | Monod constant for HMWC hydrolysis | $mol~C~m^{-3}$ | | ksLMWC | 0.0005 | Monod constant for LMWC uptake by bacteria | $mol~C~m^{-3}$ | | rBasal | 0.1 | basal respiration rate constant | $d^{-1}$ | | fLoss | 0.5 | fraction of LMWC uptake respired | - | | rMort | 50 | quadratic mortality rate constant for bacteria | $(mol~C~m^{-3})^{-1}~d^{-1}$ | | fluxPOC | 0.0005 | constant influx of POC | $mol~C~m^{-3}~d^{-1}$ |

If you have time



dynamic-R/RTM documentation built on Feb. 28, 2025, 1:23 p.m.