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A ternary flammability diagram, showing which mixtures of methane, oxygen gas, and inert nitrogen gas will burn. A ternary plot, ternary graph, triangle plot, simplex plot, or Gibbs triangle is a barycentric plot on three variables which sum to a constant. [1] It graphically depicts the ratios of the three variables as positions in an ...
Piper diagram of water samples from the Mtshabezi River, Zimbabwe. Data source: [2] A Piper diagram is a graphical representation of the chemistry of a water sample or samples. The cations and anions are shown by separate ternary plots. The apexes of the cation plot are calcium, magnesium and sodium plus potassium cations.
Dmitri Petrovich Konovalov (22 March 1856 – 6 January 1929) was a Russian-Soviet physical chemist who worked on gas-liquid phases of solutions in equilibrium and came up with several rules that were also independently worked on by J. Willard Gibbs and the rules are often called Gibbs-Konovalov rules.
Thermodynamic data is usually presented as a table or chart of function values for one mole of a substance (or in the case of the steam tables, one kg). A thermodynamic datafile is a set of equation parameters from which the numerical data values can be calculated. Tables and datafiles are usually presented at a standard pressure of 1 bar or 1 ...
Pitzer equations [1] are important for the understanding of the behaviour of ions dissolved in natural waters such as rivers, lakes and sea-water. [2] [3] [4] They were first described by physical chemist Kenneth Pitzer. [5]
A miscibility gap between isostructural phases may be described as the solvus, a term also used to describe the boundary on a phase diagram between a miscibility gap and other phases. [2] Thermodynamically, miscibility gaps indicate a maximum (e.g. of Gibbs energy) in the composition range. [3] [4]
(based nn raster werion Gibbs-plot.jpg}. The original image appeared in Gibbs, J.W. (1873). "A method of geometrical representation of the thermodynamic properties of substances by means of surfaces". Transactions of the Connecticut Academy of Arts and Sciences 2: 382-404. Author: Diagram by J. Willard Gibbs (1839 – 1903), digitalized by Fraximus
The groundwater flow between neighboring prisms is calculated using 2-dimensional horizontal groundwater flow equations. Vertical flows are found by applying one-dimensional flow equations in a vertical sense, or they can be derived from the water balance: excess of horizontal inflow over horizontal outflow (or vice versa) is translated into ...