1948
DOI: 10.1002/hlca.19480310610
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Variation de la chaleur spécifique du caoutchouc en fonction de l'allongement

Abstract: B condition que la tension a longueur constante varie lineairement avec l) Voir communication provisoire, Exper. 3, 26 (1947). Fil du pont de Wheatstone: constantan 0 1 mm., 1 m., 0,62 9. RBsistances: constantan $3 0,2 mm., 109 Q. RBsistance d'itquilibre: manganine 0 0.5 mm., 7 Sa env. Resistance variable: 54 9 max. RBsistance variable : 30 9 max. RBsistance constantan: 27 Q env. Ritsistance thermom6trique: platine 0 0,15 mm., 7 52. RBsistance chauffage: constantan 0 0,15 mm., 26,65 Q. Amperemetre MULTAVI I1 (… Show more

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Cited by 8 publications
(5 citation statements)
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“…It is defined by C=T()2normalΨTTboldF,ξα>0 where Ψ is the free energy function. In unfilled natural rubber, volume changes are small[] and the specific heat does not vary significantly, even when crystallization occurs[]; therefore, the product ρ C can be assumed to be constant. The local form of the heat diffusion equation writes as follows: ρCtrueT˙Divfalse(κ00.3emGrad0.3emTfalse)=Dint+TboldPT:trueF˙+Ttrueβ=1mAβT:trueξβ˙s+R where κ 0 is a positive semidefinite tensor characterizing the thermal conductivity of the material and s denotes the overall heat power density induced by the deformation process.…”
Section: Methodology For Crystallinity Measurementmentioning
confidence: 99%
See 1 more Smart Citation
“…It is defined by C=T()2normalΨTTboldF,ξα>0 where Ψ is the free energy function. In unfilled natural rubber, volume changes are small[] and the specific heat does not vary significantly, even when crystallization occurs[]; therefore, the product ρ C can be assumed to be constant. The local form of the heat diffusion equation writes as follows: ρCtrueT˙Divfalse(κ00.3emGrad0.3emTfalse)=Dint+TboldPT:trueF˙+Ttrueβ=1mAβT:trueξβ˙s+R where κ 0 is a positive semidefinite tensor characterizing the thermal conductivity of the material and s denotes the overall heat power density induced by the deformation process.…”
Section: Methodology For Crystallinity Measurementmentioning
confidence: 99%
“…where Ψ is the free energy function. In unfilled natural rubber, volume changes are small [23,24] and the specific heat does not vary significantly, even when crystallization occurs [25][26][27] ; therefore, the product C can be assumed to be constant. The local form of the heat diffusion equation writes as follows:…”
Section: Calorimetry Under Stretching: Thermodynamical Frameworkmentioning
confidence: 99%
“…In unfilled natural rubber, volume changes are small (Le Cam and Toussaint, 2008;Chenal et al, 2007) and the specific heat does not vary significantly, even when crystallization occurs (Vogt, 1937;Boissonnas, 1939;Mayor and Boissonnas, 1948), therefore the product ρC can be assumed to be constant. As the heat produced and absorbed due to thermomechanical s tmc couplings is the same, the temporal integration of Equation 5 over one mechanical cycle provides the energy due to intrinsic dissipation W intrinsic :…”
Section: Heat Power Densitymentioning
confidence: 99%
“…In unfilled natural rubber, volume changes are small, i.e. ρ ¼ ρ 0 Toussaint 2008, Chenal, Gauthier, Chazeau, Guy, andBomal 2007), and the specific heat is assumed to not vary significantly, even when crystallization occurs (Vogt 1937, Boissonnas 1939, Mayor and Boissonnas 1948, therefore the product ρC can be assumed to be constant. τ is a parameter characterizing the heat exchanges between the specimen and its surroundings.…”
Section: Heat Source Reconstructionmentioning
confidence: 99%