𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Mössbauer effect on ferrous ions in cubic ice

✍ Scribed by J.A. Cameron; L. Keszthelyi; G. Nagy; L. Kacsóh


Publisher
Elsevier Science
Year
1971
Tongue
English
Weight
258 KB
Volume
8
Category
Article
ISSN
0009-2614

No coin nor oath required. For personal study only.

✦ Synopsis


Ii has been demonstrated by combining M'dssbauer absorption and differential thermal analysis. that Fez1 ions in frozen ferrous perchlorate solution are cnaffected by the presence of the cubic phase of the ice. In early investigations of frozen aqueous solu-'.


📜 SIMILAR VOLUMES


Kinetics of the cubic-to-hexagonal phase
✍ A.J. Nozik; M. Kaplan 📂 Article 📅 1967 🏛 Elsevier Science 🌐 English ⚖ 412 KB

The transformation of cubic to hexagonal ice has been studied by measuring the time dependence of the dependence of the disappearance and reappearance of the MSssbauer effect in frozen aqueous solutions containing ferrous, ferric and europic ions. The rate of transformation is significantly decrease

Mössbauer study of deuteration effects o
✍ Bernard Brunot 📂 Article 📅 1975 🏛 Elsevier Science 🌐 English ⚖ 338 KB

The quadrupole splitting E was measured between 90 and 350 K for the compounds Fe(NHj;hX2 and Fe(NDs)& where X = (11, BF4 and SiF6. At 100 K the tetrafluoroborate.shows a relative isotope effect {E(deuterated} -E(hydrogenated)}/c(hydrogenated) of about 10%. In the case of the tetiafluoroborate, too,

The effect of flake size on the Mössbaue
✍ J.G. Hooley; J.R. Sams; B.V. Liengme 📂 Article 📅 1970 🏛 Elsevier Science 🌐 English ⚖ 458 KB

The thermal decomposition of graphite ferric chloride produces graphite ferrous chloride with two quadrupole splittings for iron. One of these is the same as the single splitting in bulk FeCl,. The other is larger and has an intensity, relative to the normal splitting, which increases with flake thi

Mössbauer investigation on the crystal f
✍ F. Varret; J. Danon 📂 Article 📅 1973 🏛 Elsevier Science 🌐 English ⚖ 213 KB

The hfdssbauer quodrupoie interaction Q'o of the Fe '+ ion has been measured with 2% 3i. 57Fe in ZnSiF, \* 6H,O, betwve-n 1.3 and 20°K. The sign of tiQ f< O\_) .has been determined by using a single crystal absorber. These results are interpreted in terms of a triponal crystal txld potential that sp