| | 27 | |
| | 28 | * '''Calculation of the oxygen partial pressure'''. For both the calculation of the gradient of oxygen partial pressure (d(pO2)/dz) and the change in oxygen partial pressure (d(pO2)/dt), we need dz, the depth over which one makes the calculation. It is not clear to me which depth one should use. For information, OCN used z_decomp ([[source:branches/orchidee-N/ORCHIDEE/src_stomate/stomate_soilcarbon.f90@19#L705, here], see here]) |
| | 29 | |
| | 30 | * '''Calculation of the oxygen partial pressure'''. Still in the calculation of the change in oxygen partial pressure (d(pO2)/dt) in OCN, it seems that "dz" term (z_decomp) is missing in the following equation ([[source:branches/orchidee-N/ORCHIDEE/src_stomate/stomate_soilcarbon.f90@19#L705, here], see here]) when we compare with the reference formulation (Li et al., 2000, Eq. 4 of Table 2) |
| | 31 | |
| | 32 | * '''Calculation of the oxygen partial pressure'''. Still in the calculatin of the change in oxygen partial pressure ([[source:branches/orchidee-N/ORCHIDEE/src_stomate/stomate_soilcarbon.f90@19#L705, here], see here]), in OCN it is written as : pO2(t+dt)=pO2(t)+d(pO2)/dt |
