Another word for saturation

If, however, a solution be cooled slowly past its saturation point with no solid present, crystallization does not occur till some lower temperature is reached.

These saturation capacities were assidu- valency.

The positions of springs are determined by permeable depressions in the surface of the ground below the general level of saturation, and frequently also by the holding up of that level locally by comparatively impermeable strata, sometimes combined with a fault or a synclinal fold of the strata, forming the more permeable portion into an underground basin or channel lying within comparatively impermeable boundaries.

The decrease is most marked as saturation approaches.

If the solution of a solid more soluble when hot be cooled below the saturation point, the whole of the solid sometimes remains in solution.