Parole in English per 'Alternative form of solvsbergite.'
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- (not comparable, chemistry, of a solution) Containing all the solute that can normally be dissolved at a given temperature.
- (chemistry) Having all available valence bonds filled; especially of any organic compound containing only single bonds between carbon atoms.
- (mathematics, especially topology, with respect to a function f) Saturated with respect to the equivalence relation x≡y⟺f(x)=f(y) (the kernel, noun sense 10, of f).
- (mathematics, set theory, of a set S, with respect to an equivalence relation ≡) Equal to a union of equivalence classes of ≡; such that if x∈S and x≡y then y∈S.
- (not comparable) Full; unable to hold or contain any more.
- (comparable) Soaked or drenched with moisture.
- Having a high level of saturation (in various senses).
- (computing) Conforming to saturation arithmetic.
- used especially of organic compounds; having all available valence bonds filled
- (of color) being chromatically pure; not diluted with white or grey or black
- being the most concentrated solution possible at a given temperature; unable to dissolve still more of a substance
- (chemistry, of a solution) Not saturated; capable of dissolving more of a solute at the same temperature.
- (of a colour) Not chromatically pure; diluted.
- (chemistry) Of a compound containing atoms sharing more than one valence bond, especially of an organic compound having one or more double bonds or triple bonds between carbon atoms.
- not saturated; capable of dissolving more of a substance at a given temperature
- used of a compound (especially of carbon) containing atoms sharing more than one valence bond
- (of color) not chromatically pure; diluted
- (mineralogy) A plagioclase feldspar, the second member of the Albite-Anorthite solid solution series. Primarily found as small crystals in impure marble. Oligoclase contains a small amount of calcium substituting for some of the sodium in its formula. Oligoclase with reddish-golden inclusions found in Norway and Canada is called sunstone.
- any of a series of triclinic feldspars that form rocks
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noun
adj
verb
adj
noun
- (mineralogy) A plagioclase feldspar, the second member of the Albite-Anorthite solid solution series. Primarily found as small crystals in impure marble. Oligoclase contains a small amount of calcium substituting for some of the sodium in its formula. Oligoclase with reddish-golden inclusions found in Norway and Canada is called sunstone.
- any of a series of triclinic feldspars that form rocks
verb
noun
noun
verb
noun
- (not comparable, chemistry, of a solution) Containing all the solute that can normally be dissolved at a given temperature.
- (chemistry) Having all available valence bonds filled; especially of any organic compound containing only single bonds between carbon atoms.
- (mathematics, especially topology, with respect to a function f) Saturated with respect to the equivalence relation x≡y⟺f(x)=f(y) (the kernel, noun sense 10, of f).
- (mathematics, set theory, of a set S, with respect to an equivalence relation ≡) Equal to a union of equivalence classes of ≡; such that if x∈S and x≡y then y∈S.
- (not comparable) Full; unable to hold or contain any more.
- (comparable) Soaked or drenched with moisture.
- Having a high level of saturation (in various senses).
- (computing) Conforming to saturation arithmetic.
- used especially of organic compounds; having all available valence bonds filled
- (of color) being chromatically pure; not diluted with white or grey or black
- being the most concentrated solution possible at a given temperature; unable to dissolve still more of a substance
- (chemistry, of a solution) Not saturated; capable of dissolving more of a solute at the same temperature.
- (of a colour) Not chromatically pure; diluted.
- (chemistry) Of a compound containing atoms sharing more than one valence bond, especially of an organic compound having one or more double bonds or triple bonds between carbon atoms.
- not saturated; capable of dissolving more of a substance at a given temperature
- used of a compound (especially of carbon) containing atoms sharing more than one valence bond
- (of color) not chromatically pure; diluted