TY - JOUR
T1 - On simulating reactive chemical transport with dominating precipitated species controlling chemical equilibrium
AU - Cheng, Hwai Ping
AU - Yeh, Gour Tsyh
N1 - Funding Information:
This research was supported by the Office of Health and Environmental Research, Department of Energy, Grant No. DE-FG02-91ER61197.
PY - 1998
Y1 - 1998
N2 - We present an approach developed to compute chemical equilibrium and its corresponding reactive chemical transport when dominating precipitated species (DPS) exist. In computing chemical equilibrium, most models take the concentrations or activities of component species and precipitated species as the master variables. However, when the amount of a precipitated species is much larger than those of other species, small computational errors on this DPS concentration might introduce large errors on the concentrations of other species and would cause non-mass-conserved numerical results. To deal with the existence of DPS, we pick as master variables the concentration change, rather than the concentration, of DPS to compute chemical equilibrium. Since the concentration changes of DPS will no longer be much larger than the concentrations of other species in determining equilibrium, our approach is able to provide correct numerical results. We also employ the modified total analytical concentrations, rather than the total analytical concentrations, of aqueous components as the dependent variables in presenting and solving corresponding transport equations. Several examples are given to reveal the numerical problems associated with DPS and to demonstrate the success of our approach.
AB - We present an approach developed to compute chemical equilibrium and its corresponding reactive chemical transport when dominating precipitated species (DPS) exist. In computing chemical equilibrium, most models take the concentrations or activities of component species and precipitated species as the master variables. However, when the amount of a precipitated species is much larger than those of other species, small computational errors on this DPS concentration might introduce large errors on the concentrations of other species and would cause non-mass-conserved numerical results. To deal with the existence of DPS, we pick as master variables the concentration change, rather than the concentration, of DPS to compute chemical equilibrium. Since the concentration changes of DPS will no longer be much larger than the concentrations of other species in determining equilibrium, our approach is able to provide correct numerical results. We also employ the modified total analytical concentrations, rather than the total analytical concentrations, of aqueous components as the dependent variables in presenting and solving corresponding transport equations. Several examples are given to reveal the numerical problems associated with DPS and to demonstrate the success of our approach.
UR - http://www.scopus.com/inward/record.url?scp=6544276455&partnerID=8YFLogxK
U2 - 10.1023/A:1011546118610
DO - 10.1023/A:1011546118610
M3 - 期刊論文
AN - SCOPUS:6544276455
SN - 1420-0597
VL - 2
SP - 151
EP - 170
JO - Computational Geosciences
JF - Computational Geosciences
IS - 2
ER -