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Adding ice flow composite rheology requires to incorporate following diffusion creep law from Goldsby and Kohlstedt (2001), eq.4 + Table 6:
# Diffusion creep rheology (Goldsby and Kohlstedt 2001, eq.4 + Table 6)
m_diff = 2
n_diff = 1
F_diff = (2^((2*n_diff-1)/n_diff))^-1 # simple shear epxeriments (not sure 100%)
Dv = 9.1e-4 # Dv: exponential prefactor[m^2/s]
Vm = 1.97e-5 # Vm: molar volume
A_diff = 42.0*Vm./(R.*T_h).*Dv
Q_diff = 59.4e3 # Q1: diffusional activation energy[J/mol]
# Pre-computations
B_diff = F_diff .* A_diff .^(-1.0) .* exp.( Q_diff ./(R.*T_h))
# Isolated viscosities
Eta_diff .= fact^(n_diff-1) .* B_diff .* Tii.^(1.0-n_diff ).*d.^m_diff
The "problem" is that the factor A_diff depends on temperature (and R*T). It is unclear how to implement this flow law. Can we readily use abstract flow laws to account for this or is more engineering needed?
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