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Solvation or dissolution is a kinetic process and is quantified by its rate. Solubility quantifies the dynamic equilibrium state achieved when the rate of dissolution equals the rate of precipitation. The consideration of the units makes the distinction clearer. The typical unit for dissolution rate is mol/s.
Dissociation in chemistry is a general process in which molecules (or ionic compounds such as salts, or complexes) separate or split into other things such as atoms, ions, or radicals, usually in a reversible manner.
In chemistry, solubility is the ... A stable state of the solubility equilibrium occurs when the rates of dissolution and re-joining are equal, meaning the relative ...
Dissolution (politics), when a state or institution ceases to exist Dissolution of parliament. Dissolution of the Parliament of the United Kingdom; Dissolution (law), any of several events that terminate a legal entity such as a marriage, adoption, corporation, or union; Dissolution of the Monasteries, in England, Wales and Ireland 1536–1541
A solubility equilibrium exists when a chemical compound in the solid state is in chemical equilibrium with a solution containing the compound. This type of equilibrium is an example of dynamic equilibrium in that some individual molecules migrate between the solid and solution phases such that the rates of dissolution and precipitation are equal to one another.
Also acid ionization constant or acidity constant. A quantitative measure of the strength of an acid in solution expressed as an equilibrium constant for a chemical dissociation reaction in the context of acid-base reactions. It is often given as its base-10 cologarithm, p K a. acid–base extraction A chemical reaction in which chemical species are separated from other acids and bases. acid ...
The integral heat of dissolution is defined as a process of obtaining a certain amount of solution with a final concentration. The enthalpy change in this process, normalized by the mole number of solute, is evaluated as the molar integral heat of dissolution. Mathematically, the molar integral heat of dissolution is denoted as:
The rate of dissolution will decrease substantially once it needs to penetrate through the pores of substance A in order to continue targeting substance B. [1] This penetration can often lead to dissolution of substance A, [1] or the product of more than one solute, [10] both unsatisfactory if specific leaching is desired.