BioRT-HBV is a catchment scale reactive transport model that can simulate a variety of biogeochemical processes using hydrology as simulated by HBV-light model.
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Stream Chemistry Calculation for Speciation Reactions #34
I am able to run the calcite weathering reaction with just the primary species (Ca2+ and CO32-), but the stream chemistry for DIC does not look correct when I add in secondary species (HCO3- and CO2(aq)).
I have a base case with just the primary species, and a speciation case with the secondary species included. The inclusion of secondary species should allow more calcite to dissolve as CO32- can change species depending on pH conditions, meaning that the [DIC] and [Ca2+] should increase. However, the results of the case with speciation have lower [DIC] in the stream than the base case, but higher [Ca2+] in the stream. This seems to only be an issue with the stream chemistry, as the [DIC] in the UZ and LZ behaves as expected.
Model version: HBV-BioRT - Numexp branch (no surface reactions, last updated 10/17/2021)
I am able to run the calcite weathering reaction with just the primary species (Ca2+ and CO32-), but the stream chemistry for DIC does not look correct when I add in secondary species (HCO3- and CO2(aq)).
I have a base case with just the primary species, and a speciation case with the secondary species included. The inclusion of secondary species should allow more calcite to dissolve as CO32- can change species depending on pH conditions, meaning that the [DIC] and [Ca2+] should increase. However, the results of the case with speciation have lower [DIC] in the stream than the base case, but higher [Ca2+] in the stream. This seems to only be an issue with the stream chemistry, as the [DIC] in the UZ and LZ behaves as expected.
Model version: HBV-BioRT - Numexp branch (no surface reactions, last updated 10/17/2021)
To reproduce: Calcite_Speciation.zip