With regard to solution, I have met with some reasons for supposing that it will probably disappear as a cause of transference, and intend resuming the consideration at a convenient opportunity.
See now, 1340, 1341.—Dec. 1838.
De la Rive.
With regard to perchloride and periodide of mercury, see now 1340, 1341.—Dec. 1838.
In relation to this and the three preceding paragraphs, and also 801, see Berzelius's correction of the nature of the supposed now sulphuret and oxide, Phil. Mag. 1836, vol. viii. 476: and for the probable explanation of the effects obtained with the protoxide, refer to 1340, 1341.—Dec. 1838.
Philosophical Transactions, 1807, pp. 32, 39; also 1826, pp. 387, 389.
For a simple table of correction for moisture, I may take the liberty of referring to my Chemical Manipulation, edition of 1830, p. 376.
As early us the year 1811, Messrs. Gay-Lussac and Thénard employed chemical decomposition as a measure of the electricity of the voltaic pile. See Recherches Physico-chymiques, p. 12. The principles and precautions by which it becomes an exact measure were of course not then known.—Dec. 1838.
Annales de Chimie, 1801, tom. li. p. 167.
Annales de Chimie, 1804, tom. li. p. 172.