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Study of elementary mechanisms of creep in uranium as a function of temperature (150 deg. to 760 deg. C) by activation energy measurements; Etude des mecanismes elementaires de deformation par fluage de l'uranium en fonction de la temperature (de 150 deg. a 760 deg. C) par la mesure des energies d'activation

Abstract

Creep tests were carried out on single crystals and polycrystalline specimens of uranium in both the {alpha} and {beta} phases over the temperature range 150 - 760 deg. C. The determination of the activation energy for creep and the study of its variation with temperature made it possible to distinguish various temperature ranges in which one or more elementary mechanisms govern deformation. Micrographic observations after creep and the study of the variation of creep-rate with load support the conclusions. The creep behavior of single crystals is identical with that of polycrystalline material below 325 deg. C. From 325 deg. C to one upper limiting temperature whose value depends on the purity and previous history of the metal, the creep deformation of uranium is controlled by cross-slip. From this limiting temperature up to 520 deg. C, the creep of uranium involves two independent mechanisms operating simultaneously, the movement of screw dislocation by cross-slip and the climbing of edge dislocations out of their slip plane. Between 520 deg. C and the {alpha} - {beta} transformation temperature creep in polycrystals is governed by the climb of edge dislocations out of their slip planes, by a pile up mechanism in the case of primary  More>>
Authors:
Grenier, P [1] 
  1. Commissariat a l'Energie Atomique, Saclay (France). Centre d'Etudes Nucleaires
Publication Date:
Jul 01, 1967
Product Type:
Thesis/Dissertation
Report Number:
CEA-R-3187
Resource Relation:
Other Information: TH: These docteur es-sciences physiques; 58 refs; PBD: 1967
Subject:
36 MATERIALS SCIENCE; ACTIVATION ENERGY; CLEAVAGE; CREEP; DEFORMATION; DIFFUSION; EDGE DISLOCATIONS; GRAIN BOUNDARIES; GRAIN SIZE; MOLYBDENUM ADDITIONS; MONOCRYSTALS; POLYCRYSTALS; SCREW DISLOCATIONS; SLIP; STRESSES; TEMPERATURE DEPENDENCE; URANIUM
OSTI ID:
20626235
Research Organizations:
Commissariat a l'Energie Atomique, Saclay (France). Centre d'Etudes Nucleaires; Faculte des Sciences de l'Universite de Paris - 75 (France)
Country of Origin:
France
Language:
French
Other Identifying Numbers:
TRN: FR05R3187069348
Availability:
Available from INIS in electronic form
Submitting Site:
FRN
Size:
44 pages
Announcement Date:

Citation Formats

Grenier, P. Study of elementary mechanisms of creep in uranium as a function of temperature (150 deg. to 760 deg. C) by activation energy measurements; Etude des mecanismes elementaires de deformation par fluage de l'uranium en fonction de la temperature (de 150 deg. a 760 deg. C) par la mesure des energies d'activation. France: N. p., 1967. Web.
Grenier, P. Study of elementary mechanisms of creep in uranium as a function of temperature (150 deg. to 760 deg. C) by activation energy measurements; Etude des mecanismes elementaires de deformation par fluage de l'uranium en fonction de la temperature (de 150 deg. a 760 deg. C) par la mesure des energies d'activation. France.
Grenier, P. 1967. "Study of elementary mechanisms of creep in uranium as a function of temperature (150 deg. to 760 deg. C) by activation energy measurements; Etude des mecanismes elementaires de deformation par fluage de l'uranium en fonction de la temperature (de 150 deg. a 760 deg. C) par la mesure des energies d'activation." France.
@misc{etde_20626235,
title = {Study of elementary mechanisms of creep in uranium as a function of temperature (150 deg. to 760 deg. C) by activation energy measurements; Etude des mecanismes elementaires de deformation par fluage de l'uranium en fonction de la temperature (de 150 deg. a 760 deg. C) par la mesure des energies d'activation}
author = {Grenier, P}
abstractNote = {Creep tests were carried out on single crystals and polycrystalline specimens of uranium in both the {alpha} and {beta} phases over the temperature range 150 - 760 deg. C. The determination of the activation energy for creep and the study of its variation with temperature made it possible to distinguish various temperature ranges in which one or more elementary mechanisms govern deformation. Micrographic observations after creep and the study of the variation of creep-rate with load support the conclusions. The creep behavior of single crystals is identical with that of polycrystalline material below 325 deg. C. From 325 deg. C to one upper limiting temperature whose value depends on the purity and previous history of the metal, the creep deformation of uranium is controlled by cross-slip. From this limiting temperature up to 520 deg. C, the creep of uranium involves two independent mechanisms operating simultaneously, the movement of screw dislocation by cross-slip and the climbing of edge dislocations out of their slip plane. Between 520 deg. C and the {alpha} - {beta} transformation temperature creep in polycrystals is governed by the climb of edge dislocations out of their slip planes, by a pile up mechanism in the case of primary creep and by dipole annihilation in the case of secondary creep. In single crystals creep is dependent on the climb of edge dislocations into pre-existent sub-boundaries and their subsequent rearrangement within these boundaries. In the {beta} phase the creep of polycrystals is governed by the diffusional climb of edge dislocations. Between 450 and 630 deg. C small alloy additions of molybdenum modify the creep characteristics of uranium although the deformation mechanisms involved are analogous to those in the pure metal. (author) [French] Des essais de fluage a diverses temperatures comprises entre 150 et 760 deg. C ont ete effectues sur des polycristaux et des monocristaux d'uranium, en phase {alpha} et en phase {beta}. La determination de l'energie d'activation pour le fluage et l'etude de ses variations en fonction de la temperature ont permis de definir differents domaines de temperature pour lesquels un ou plusieurs mecanismes elementaires controlent la deformation. Les observations micrographiques effectuees directement apres fluage et l'etude des variations de la vitesse de fluage en fonction de la charge appliquee confirment les hypotheses prononcees. Au-dessous de 325 deg. C, le comportement au fluage des monocristaux et des polycristaux est identique. De 325 deg. C a une limite superieure de temperature dependant de l'etat structural du metal et de son degre de purete, la deformation par fluage de l'uranium est controlee par un glissement devie. De ces limites de temperature a 520 deg. C, le fluage de l'uranium fait intervenir deux mecanismes simultanes et independants, le deplacement des dislocations-vis par un systeme de glissement devie et la montee d'une partie des dislocations-coins hors de leur plan de glissement. Au-dessus de 520 deg. C jusqu'au haut de la phase {alpha}, le fluage des polycristaux est controle par la montee des dislocations-coins hors de leur plan de glissement, suivant un mecanisme d'empilement dans le cas du fluage primaire et d'annihilation de dipoles dans le cas du fluage secondaire. Pour les monocristaux, le fluage depend de la montee des dislocations-coins dans les sous-joints preexistant au fluage et de leur rearrangement ulterieur au sein de ces sous-joints. En phase {beta}, le fluage des polycristaux est controle par la montee des dislocations-coins par diffusion. Entre 450 et 630 deg. C, l'addition de faibles teneurs de molybdene a l'uranium modifie les caracteristiques du fluage, tout en conservant des mecanismes de deformation analogue a ceux de l'uranium non allie. (auteur)}
place = {France}
year = {1967}
month = {Jul}
}