RESISTIVITY AND HYDROGEN UPTAKE MEASUREMENTS IN EVAPORATED MG FILMS AT 350 K

Citation
P. Hjort et al., RESISTIVITY AND HYDROGEN UPTAKE MEASUREMENTS IN EVAPORATED MG FILMS AT 350 K, Journal of alloys and compounds, 234(2), 1996, pp. 11-15
Citations number
8
Categorie Soggetti
Chemistry Physical","Metallurgy & Metallurigical Engineering","Material Science
ISSN journal
09258388
Volume
234
Issue
2
Year of publication
1996
Pages
11 - 15
Database
ISI
SICI code
0925-8388(1996)234:2<11:RAHUMI>2.0.ZU;2-2
Abstract
Resistivity measurements were performed during hydriding-decomposition cycles of UHV-prepared Mg films. The hydrogen exposures were made in situ at p(H2) = 0.6 torr and 350 K. To obtain measurable uptake rates at these conditions a thin layer of Pd (approximate to 7 nm) was depos ited on top of the typically 380 nm thick Mg films. Mg and Pd film thi cknesses and hydrogen uptakes were determined by the frequency shift o f a quartz crystal microbalance (QCM). Both the QCM and the quartz sub strate onto which the Mg resistor film was deposited were mounted on t he same sample holder. The p, T conditions were chosen so that hydroge n was distributed nearly homogeneously through the sample. The total h ydrogen uptakes were in most cases kept small (<40 at.% H) to minimize the morphology changes. The resistivity vs. H concentration relation is, within experimental uncertainty, linear up to x = (H/Mg) approxima te to 0.4 according to the formula rho(x) = rho(0)(1 + c . x), c = 1.0 8 +/- 0.25. The relatively large uncertainty is caused by a spread in the uptake data and by the irreversible resistance changes during hydr iding-decomposition cycles. Both these uncertainties could be attribut ed to morphological changes induced by the volume expansion-contractio n accompanying the cycles. Exploratory measurements were also made at much larger H uptakes. These measurements reveal a rapid reversible re sistivity increase at (H/Mg) approximate to 1.2, which can be qualitat ively attributed to the metal-insulator transition expected for the Mg -H-x system when the hydride phase becomes continuous. The measurement s and their quantitative interpretation were complicated by the morpho logical changes of the sample(s) caused by volume expansion-contractio n.