«SUBFLUID» 관련 영어 책
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1
The Non-Linear Field Theories of Mechanics
If a subfluid is also a hyperelastic material, it is called a hyperelastic subfluid. In
the previous section, after seeing that p and ga need not be the same in general,
we have proved that for hyperelastic fluids and solids they are. The first example
...
C. Truesdell, Walter Noll, Stuart Antman, 2004
2
Non-linear Continuum Theories: Lectures given at a Summer ...
Consequently, the constituitive equation reduces to the form (5) T (t) = ^ (Cjjj , j> (t
) ) From the table above we see that the local configuration of a subfluid is
characterized by the density and the orientation of certain material linear
manifolds.
Giuseppe Grioli, C. Truesdell, 2011
3
Encyclopedia of physics
If a subfluid is also a hyperelastic material, it is called a hyperelastic subfluid. In
the previous section, after seeing that p and ga need not be the same in general,
we have proved that for hyperelastic fluids and solids they are. The first example
...
4
Bull. Math. de la Soc. Sci. Math. de Roumanie
The configurations of a subfluid can be characterized by a preferential basis [
which defines the privilged elements (lines or planes) of the subfluid. The
privileged vector e is transformed by the deformation gradient F, becoming F e,
where the ...
Societatea de Ştiinţe Matematice, 1989
5
The rural economy of Gloucestershire: including its dairy : ...
Thus the pomage(a subfluid) is forced toward the outer edges of the cloths ;
which, in this form of the pile, bane no immediate pressure:-an indirect horizontal
pressure, arising from the natural law of fluids, being all the compression which
the ...
Mr. Marshall (William), 1796
6
The Rural Economy of Glocestershire; Including Its Dairy: ...
T hus' the pomage (a subfluid) is forced toward the outer edges of the cloths;
which, in this form of the pile, have no immediate prefftrez-an indirect horizontal
pressure, arising from the natural law of fiuids, being all the compression which
the ...
Mr. Marshall (William), 1789
7
An Introduction to Fossils and Minerals: Seeking Clues to ...
Aa, or blocky lava, forms when viscous, subfluid lava presses forward, carrying a
thick, brittle crust along with it. As the lava flows, it stresses the overriding crust,
breaking it into rough, jagged blocks, which are pushed ahead of or dragged ...
8
Making of the Earth: Geologic Forces That Shape Our Planet
Aa or blocky lava forms when viscous, subfluid lavas press forward, car- rying
along a thick and brittle crust.As the lava flows, it stresses the overriding crust,
breaking it into rough, jagged blocks.These are pushed ahead of or dragged
along ...
9
Alternative Mathematical Theory of Non-equilibrium Phenomena
Here |.t*J-k is the chemical potential (or specific Gibbs function) for the kth
subfluid within the jth component; for the mass fraction col-k of this component
the closure rule (5.24) must be observed. If equilibrium prevails between the
constituents ...
10
Introduction to Rational Elasticity
Thus in order to effect a simple shear of this kind of subfluid in this particular
configuration, it is always necessary to apply a suitable non-zero shear stress.
Substituting (3.47) into (3.45), we find for the components of T the formulae rn =
— p + t ...
Chao-cheng Wang, C. Truesdell, 1973
