Adapting molar data (without density) for molal models
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Summary
An algorithm that can accurately calculate the density of molar-based solutions, and, as a consequence, molality is presented, which opens a large literature based on molar concentrations to exploration with theoretical models based on molal concentrations and classical thermodynamic principles.
- Type
- article
- Published
- 2007-06-01
- Cited by
- 11
- References
- 19
- OpenAlex
- https://openalex.org/W2070806756
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:1872761
Keywords
Molality, Molar concentration, Molar, Electrolyte, Thermodynamics
References
- Properties and Classification of Cold Desert Soils from Antarctica
- Modeling gas hydrate equilibria in electrolyte solutions
- A molal-based model for strong acid chemistry at low temperatures (<200 to 298 K)
- Halogen geochemistry of the McMurdo dry valleys lakes, Antarctica: Clues to the origin of solutes and lake evolution
- Mineral solubilities in the Na-K-Mg-Ca-Cl-SO4-H2O system: a re-evaluation of the sulfate chemistry in the Spencer-Møller-Weare model
- Effects of pressure on aqueous chemical equilibria at subzero temperatures with applications to Europa
- A new extended Gibbs thermodynamic potential of seawater
- Comparison of immiscibly displaced soil solutions and saturated paste extracts from saline soils
- Density calculation and concentration scale conversions for natural waters
- Carbonate mineral solubility at low temperatures in the Na-K-Mg-Ca-H-Cl-SO
- Modeling aqueous ferrous iron chemistry at low temperatures with application to Mars
- Evaporite Mineralogy and Groundwater Chemistry Associated with Saline Soils in Eastern North Dakota
- The physical chemistry of natural waters
- Chemical Oceanography
- Physico-chemical characteristics and origin of hypersaline meromictic Lake Garrow in the Canadian high Arctic
Cited by
- Validity and slopes of the linear equation of state for natural brines in salt lake systems
- Sulfite–sulfide–sulfate–carbonate equilibria with applications to Mars
- The formation of Ca-Cl-rich groundwaters in the Dry Valleys of Antarctica: Field measurements and modeling of reactive transport
- FREZCHEM: A geochemical model for cold aqueous solutions
- Modeling ferrous–ferric iron chemistry with application to martian surface geochemistry
- Modeling hot spring chemistries with applications to martian silica formation
- Carbon Sequestration and Release from Antarctic Lakes: Lake Vida and West Lake Bonney (McMurdo Dry Valleys)
- Modeling aqueous perchlorate chemistries with applications to Mars
- Modeling Low-Temperature Geochemical Processes
- Chemical equilibrium between aqueous fluids and minerals in the marine environment
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