Skip to main content
. 2019 Jun 24;38(7):1386–1399. doi: 10.1002/etc.4440

Figure 5.

Figure 5

Mass balance results for tableau input coupled kinetic equilibrium transport–unit world model (TICKET–UWM) sediment simulations with an (a) anoxic sediment and (b) oxic sediment. Mass values from the model have been normalized to an input mass of 100 kg. Simulations for both sediment types had an initial total water column copper concentration of 35 μg/L. The anoxic sediment simulation had an acid‐volatile sulfide = 9.1 μmol/g. The oxic sediment simulation had sediment hydrous ferric oxide (HFO) = 18 600 mg HFO/kg and sediment hydrous manganese oxide (HMO) = 154 mg HMO/kg.