Sediment 1D reaction-transport configuration with C, O, N, P, S, Fe, Mn

Dale (2015) configuration

julia> include("PALEO_examples_sediment_NNFeMn.jl")

Configuration is similar to shelf and slope test cases in Dale (2015) GBC https://dx.doi.org/10.1002/2014GB005017, with:

• a discrete (multi-G) approximation to POC reactive-continuum distribution
• NO2 and NO3 oxidants
• Mn oxides with two reactivity fractions
• Fe oxides with three reactivity fractions

There are four sediment columns: oxic and anoxic 'shelf', oxic and anoxic 'slope'

Minimal model for P diagenesis

julia> include("PALEO_examples_sediment_NNFeMnP.jl")

Includes a minimal model for P diagenesis including:

• P coprecipitation on FeHR, FeMR iron oxides
• CFA formation

See:

• Slomp (1996) https://dx.doi.org/10.1357/0022240963213745
• Reed (2011) https://dx.doi.org/10.4319/lo.2011.56.3.1075
• Dale (2016) https://dx.doi.org/10.1016/j.gca.2016.05.046