Y. Sakamoto et al., SELF STRAIN GRADIENT INDUCED DIFFUSION OF HYDROGEN IN PD-AG ALLOY MEMBRANES, International journal of hydrogen energy, 20(1), 1995, pp. 35-41
Citations number
36
Categorie Soggetti
Energy & Fuels","Environmental Sciences","Physics, Atomic, Molecular & Chemical
Self strain gradient induced uphill diffusion effects of hydrogen in a
series of Pd-Ag alloys with up to 39.9at% Ag have been investigated b
y an electrochemical permeation method. The uphill diffusion effects d
uring hydrogen absorption into and desorption from the alloys have bee
n observed over a range of initial hydrogen content from about H/M = 0
.01 to H/M = 0.25. In higher Ag content alloys of Pd-30.0 and 39.9at%
Ag, the effects have been observed even to occur at initial hydrogen c
ontent of more than H/M = 0.3. The uphill diffusion effects in relativ
ely low Ag content alloys have been primarily associated with lattice
strain gradients corresponding to the temporary formation of quite wel
l differentiated lattice volume differences across (alpha + beta)/beta
and (alpha + beta)/alpha interfaces during absorption and desorption
processes, respectively. In higher Ag content alloys, the non-Fickian
diffusion effects seem better to be associated with the more usual lat
tice strain gradients corresponding to sequences of more uniform conce
ntration gradients of the permeating hydrogen. The magnitude of these
uphill effects, compared at almost the same initial hydrogen content,
have a tendency to increase with an increase of the Ag content of the
alloys. This may be related to a decrease of hydrogen diffusivity in P
d-Ag alloys with increasing Ag content and also may be related to a de
crease in the bulk modulus of the alloys with Ag content.