✍ Scribed by M. J. Sparnaaij
No coin nor oath required. For personal study only.
Measurements of the electro‐osmotic transport of liquid in the germanium (powder) electrolyte solution were carried out. The results can be explained by a theory, which is given by Verwey and Payens, which was originally proposed for surface layers consisting of weakly ionized fatty acids. In the case of germanium it should be assumed that a weakly ionized germanic acid is present at the surface, giving the surface a negative charge. The experiments almost break down when p‐type Ge is used. This can be explained by potential current characteristics using p‐type or n‐type Ge as the anode.
📜 SIMILAR VOLUMES
## Abstract The density of the charge in slow surface states (∼ 10^12^cm^−2^V^−1^) is estimated from the ratio of the potential drops in the space charge region and the Helmholtz layer. These potential drops are determined from measurements of the surface conductance and electrode capacity of the g
We report computer simulations of semi-permeable membranes used to study electrolyte solutions undergoing osmosis, reverse osmosis, and electro-osmosis. The semipermeable roembrane, which is atomistic in nature, has been modeled using a novel technique developed by us rec~tly. Our results show a rat