In der Kontinuumsmechanik wurde die Finite-Stamm-Theorie - auch als große Dehnungstheorie bezeichnet, oder große Deformationstheorie genannt - wobei bei Deformationen Dehnungen und / oder Rotationen sind groß genug, um Annahmen der Infinitesimaltheorie zu entkräften. In diesem Fall unterscheiden sich die unverformten und verformten Konfigurationen des Kontinuums erheblich, was eine klare Unterscheidung zwischen ihnen erfordert. Dies ist im Allgemeinen bei Elastomeren, plastisch verformenden Materialien und anderen Flüssigkeiten und biologischem Weichgewebe der Fall.
Verschiebung [ edit ]
Abbildung 1. Bewegung eines Kontinuumskörpers.
Die Verschiebung eines Körpers besteht aus zwei Komponenten: einer Verschiebung eines starren Körpers und einer Verformung.
Eine Verschiebung eines starren Körpers besteht aus einer simultanen Translation (Physik) und einer Rotation des Körpers, ohne seine Form oder Größe zu verändern.
Unter Verformung versteht man die Änderung der Form und / oder Größe des Körpers von einer anfänglichen oder unverformten Konfiguration in eine aktuelle oder verformte Konfiguration (Abbildung 1
In der Euler-Beschreibung wird der Vektor, der sich von einem Partikel aus erstreckt, in der unverformten Konfiguration wird der Ort in der deformierten Konfiguration als Verschiebungsvektor bezeichnet:
wobei sind die Einheitsvektoren, die die Basis des Materials definieren ( Koordinatensystem (Körper-Rahmen).
In räumlichen Koordinaten ausgedrückt, lautet das Verschiebungsfeld:
Die partielle Ableitung der Verschiebung Vektor in Bezug auf die Ortskoordinaten ergibt den räumlichen Verschiebungsgradienten-Tensor . So haben wir
Beziehung zwischen den materiellen und räumlichen Koordinatensystemen edit
Betrachten Sie einen Partikel- oder Materialpunkt P P { displaystyle P , !} mit Positionsvektor X = X I I I 19659030] { displaystyle mathbf {X} = X_ {I} mathbf {I} _ {I} , !} in der nicht deformierten Konfiguration (Abbildung 2). Nach einer Verschiebung des Körpers wird die neue Position des Partikels durch
{ displaystyle p , !} in der neuen Konfiguration angezeigt gegeben durch die Vektorposition x = x i e i { displaystyle mathbf {x} = x_ {i} mathbf {e} _ {i} , !} . Die Koordinatensysteme für die unverformte und verformte Konfiguration können der Einfachheit halber überlagert werden.
Betrachten wir nun einen materiellen Punkt Q { displaystyle Q , !} benachbart P { displaystyle P , !} mit Positionsvektor X + Δ X = X I + Δ X I ) I I I (19659030) (19459044) (19659030) (19459044) {X} + Delta mathbf {X} = (X_ {I} + Delta X_ {I}) mathbf {I} _ {I} , !} . In der deformierten Konfiguration hat dieses Teilchen eine neue Position q { displaystyle q , !} gegeben durch den Positionsvektor x [19659059] + Δ x { displaystyle mathbf {x} + Delta mathbf {x} , !} . Angenommen, die Liniensegmente Δ X { displaystyle Delta X , !} und Δ x { displaystyle Delta mathbf {x} , !} das die Teilchen verbindet "/> . 19659181] P { displaystyle P , !} und Q { displaystyle Q , !} [19659716] Q , ! "/> sowohl in der unverformten als auch in der deformierten Konfiguration sehr klein, dann können wir sie als d X { displaystyle d ausdrücken. mathbf {X} , !} und d x { displaystyle d mathbf {x} , !} . So aus Abbildung 2 haben wir
x + d x = X + d X + u ] X + d X ) d x = X - x + 19659060] d X + u X + d X d d [196596] X + u ( X + d X ) - u ] X ) = d X + d u { displaystyle { begin {align} mathbf {x} + d mathbf {x} & = mathbf {X} + d mathbf {X} + mathbf {u} ( mathbf {X} + d mathbf {X}) \ d mathbf {x} & = mathbf {X} - mathbf {x} + d mathbf {X} + mathbf {u} ( mathbf {X} + d mathbf {X}) \ & = d mathbf {X} + mathbf { u} ( mathbf {X} + d mathbf {X}) - mathbf {u} ( mathbf {X}) \ & = d mathbf {X} + d mathbf {u} \ Ende {alig ned}} , !}
wobei d u u ] { displaystyle mathbf {du} , !} ist der relative Verschiebungsvektor der den Verwandten darstellt Verschiebung von Q { displaystyle Q , !} in Bezug auf P { displaystyle P , !} in der verformten Konfiguration.
Für ein infinitesimales Element d X { displaystyle d mathbf {X} , !} und unter der Annahme einer Kontinuität auf dem Verschiebungsfeld ist es möglich, eine Taylorreihen-Erweiterung um den Punkt P zu verwenden ] { displaystyle P , !} wobei Ausdrücke höherer Ordnung vernachlässigt werden, um die Komponenten des relativen Verschiebungsvektors für das benachbarte Teilchen zu approximieren Q ] { displaystyle Q , !} as
u ( X + d X ) = 19659058] u ( X ) ] + d u oder u i 19 = 19659063] u i + d d d d i [1945 u ( X ) + X u [1945[1945 d X oder u i 19 90 u i + u i 19 X J d X J [19589681] { displaystyle { begin {align} {u} ( mathbf {X} + d mathbf {X}) & = mathbf {u} ( mathbf {X}) + d mathbf {u} quad & { text {oder}} & quad u_ {i} ^ {*} = u_ {i} + du_ {i} \ & approx mathbf {u} ( mathbf {X}) + nabla _ { mathbf {X}} mathbf { u} cdot d mathbf {X} quad & { text {oder}} & quad u_ {i} ^ {*} ungefähr u_ {i} + { frac { partial u_ {i}} { partial X_ {J}}} dX_ {J} ,. end {Ausrichten}} , !}
die vorhergehende Gleichung d x = d X + d u {1945Start d mathbf {x} = d mathbf {X} + d mathbf {u} , !} kann als geschrieben werden
d x = d X + d u = d X + X u [1945 d X = (19659959) I + X X 19659127] u ) d X = F d X { displaystyle { begin {align} d mathbf {x} & = d mathbf {X} + d mathbf {u} \ & = d mathbf {X} + nabla _ { mathbf {X}} mathbf {u} cdot d mathbf {X} \ & = left ( mathbf {I} + nabla _ { mathbf {X}} mathbf {u} right) d mathbf {X} \ & = mathbf {F} d mathbf {X} end {align}} , !}
Berechnungen, bei denen die zeitabhängige Verformung eines Körpers eine Rolle spielt, erfordern oft eine zeitliche Ableitung des Verformungsgradienten. Eine geometrisch konsistente Definition einer solchen Ableitung erfordert eine Exkursion in die -Differentialgeometrie [2] aber wir vermeiden diese Probleme in diesem Artikel.
Die zeitliche Ableitung von F { displaystyle mathbf {F}} ist
F = F t = 19659102] t [[1945 x ( X t [196500061] ∂ 19 [19650008] X 19660006]] = 19 [1945 X x X X [19659060] t ) [1945 t = 19659993] [1945 X V 19659057] ( X t ) { displaystyle { dot { mathbf {F}}} = { frac { partial mathbf { F}} { partial t}} = { frac { partial} { partial t}} left [{frac {partial mathbf {x} (mathbf {X} ,t)}{partial mathbf {X} }}right] = { frac { partial} { partial mathbf {X}}} left [{frac {partial mathbf {x} (mathbf {X} ,t)}{partial t}}right] = { frac { partial} { partial mathbf {X}}} left [mathbf {V} (mathbf {X} ,t)right]}
wobei V { displaystyle mathbf {V}} ist die Geschwindigkeit. Die Ableitung auf der rechten Seite repräsentiert einen Materialgeschwindigkeitsgradienten . Es ist üblich, das in einen räumlichen Gradienten umzuwandeln, d. H.
F 19 = 19 [1945 X V X t ) ] = 65 [1945 x V X X ]t)]⋅∂x(X,t)[19660004]∂X=l⋅F{displaystyle {dot {mathbf {F} }}={frac { partial }{partial mathbf {X} }}left[mathbf {V} (mathbf {X} ,t)right]={frac {partial }{partial mathbf {x} }}left[mathbf {V} (mathbf {X} ,t)right]cdot {frac {partial mathbf {x} (mathbf {X} ,t)}{partial mathbf {X} }}={boldsymbol {l}}cdot mathbf {F} }
where l{displaystyle {boldsymbol {l}}} is the spatial velocity gradient. If the spatial velocity gradient is constant, the above equation can be solved exactly to give
The rate of deformation tensor gives the rate of stretching of line elements while the spin tensor indicates the rate of rotation or vorticity of the motion.
Transformation of a surface and volume element[edit]
To transform quantities that are defined with respect to areas in a deformed configuration to those relative to areas in a reference configuration, and vice versa, we use Nanson's relation, expressed as
where da{displaystyle da,!} is an area of a region in the deformed configuration, dA{displaystyle dA,!} is the same area in the reference configuration, and n{displaystyle mathbf {n} ,!} is the outward normal to the area element in the current configuration while N{displaystyle mathbf {N} ,!} is the outward normal in the reference configuration, F{displaystyle mathbf {F} ,!} is the deformation gradientand J=detF{displaystyle J=det mathbf {F} ,!}.
The corresponding formula for the transformation of the volume element is
Polar decomposition of the deformation gradient tensor[edit]
Figure 3. Representation of the polar decomposition of the deformation gradient
The deformation gradient F{displaystyle mathbf {F} ,!}like any invertible second-order tensor, can be decomposed, using the polar decomposition theorem, into a product of two second-order tensors (Truesdell and Noll, 1965): an orthogonal tensor and a positive definite symmetric tensor, i.e.
where the tensor R{displaystyle mathbf {R} ,!} is a proper orthogonal tensori.e. R−1=RT{displaystyle mathbf {R} ^{-1}=mathbf {R} ^{T},!} and detR=+1{displaystyle det mathbf {R} =+1,!}representing a rotation; the tensor U{displaystyle mathbf {U} ,!} is the right stretch tensor; and V{displaystyle mathbf {V} ,!} the left stretch tensor. The terms right and left means that they are to the right and left of the rotation tensor R{displaystyle mathbf {R} ,!}respectively. U{displaystyle mathbf {U} ,!} and V{displaystyle mathbf {V} ,!} are both positive definitei.e. x⋅U⋅x≥0{displaystyle mathbf {x} cdot mathbf {U} cdot mathbf {x} geq 0,!} and x⋅V⋅x≥0{displaystyle mathbf {x} cdot mathbf {V} cdot mathbf {x} geq 0,!} for all x∈R3{displaystyle mathbf {x} in mathbb {R} ^{3}}and symmetric tensorsi.e. U=UT{displaystyle mathbf {U} =mathbf {U} ^{T},!} and V=VT{displaystyle mathbf {V} =mathbf {V} ^{T},!}of second order.
This decomposition implies that the deformation of a line element dX{displaystyle dmathbf {X} ,!} in the undeformed configuration onto dx{displaystyle dmathbf {x} ,!} in the deformed configuration, i.e. dx=FdX{displaystyle dmathbf {x} =mathbf {F} ,dmathbf {X} ,!}may be obtained either by first stretching the element by U{displaystyle mathbf {U} ,!}i.e. dx′=UdX{displaystyle dmathbf {x} '=mathbf {U} ,dmathbf {X} ,!}followed by a rotation R{displaystyle mathbf {R} ,!}i.e. dx=Rdx′{displaystyle dmathbf {x} =mathbf {R} ,dmathbf {x} ',!}; or equivalently, by applying a rigid rotation R{displaystyle mathbf {R} ,!} first, i.e. dx′=RdX{displaystyle dmathbf {x} '=mathbf {R} ,dmathbf {X} ,!}followed later by a stretching V{displaystyle mathbf {V} ,!}i.e. dx=Vdx′{displaystyle dmathbf {x} =mathbf {V} ,dmathbf {x} ',!} (See Figure 3).
Due to the orthogonality of R{displaystyle mathbf {R} }
so that U{displaystyle mathbf {U} ,!} and V{displaystyle mathbf {V} ,!} have the same eigenvalues or principal stretchesbut different eigenvectors or principal directionsNi{displaystyle mathbf {N} _{i},!} and ni{displaystyle mathbf {n} _{i},!}respectively. The principal directions are related by
This polar decomposition, which is unique as F{displaystyle mathbf {F} ,!} is invertible with a positive determinant, is a corrolary of the singular-value decomposition.
Several rotation-independent deformation tensors are used in mechanics. In solid mechanics, the most popular of these are the right and left Cauchy–Green deformation tensors.
Since a pure rotation should not induce any strains in a deformable body, it is often convenient to use rotation-independent measures of deformation in continuum mechanics. As a rotation followed by its inverse rotation leads to no change (RRT=RTR=I{displaystyle mathbf {R} mathbf {R} ^{T}=mathbf {R} ^{T}mathbf {R} =mathbf {I} ,!}) we can exclude the rotation by multiplying F{displaystyle mathbf {F} ,!} by its transpose.
In 1839, George Green introduced a deformation tensor known as the right Cauchy–Green deformation tensor or Green's deformation tensor defined as:[4][5]
Physically, the Cauchy–Green tensor gives us the square of local change in distances due to deformation, i.e. dx2=dX⋅C⋅dX{displaystyle dmathbf {x} ^{2}=dmathbf {X} cdot mathbf {C} cdot dmathbf {X} ,!}
where λi{displaystyle lambda _{i},!} are stretch ratios for the unit fibers that are initially oriented along the eigenvector directions of the right (reference) stretch tensor (these are not generally aligned with the three axis of the coordinate systems).
The IUPAC recommends[5] that the inverse of the right Cauchy–Green deformation tensor (called the Cauchy tensor in that document), i. e., C−1{displaystyle mathbf {C} ^{-1}}be called the Finger tensor. However, that nomenclature is not universally accepted in applied mechanics.
The left Cauchy–Green or Finger deformation tensor[edit]
Reversing the order of multiplication in the formula for the right Green–Cauchy deformation tensor leads to the left Cauchy–Green deformation tensor which is defined as:
The left Cauchy–Green deformation tensor is often called the Finger deformation tensornamed after Josef Finger (1894).[5][6][7]
Invariants of B{displaystyle mathbf {B} ,!} are also used in the expressions for strain energy density functions. The conventional invariants are defined as
Earlier in 1828,[8]Augustin Louis Cauchy introduced a deformation tensor defined as the inverse of the left Cauchy–Green deformation tensor, B−1{displaystyle mathbf {B} ^{-1},!}. This tensor has also been called the Piola tensor[5] and the Finger tensor[9] in the rheology and fluid dynamics literature.
If there are three distinct principal stretches λi{displaystyle lambda _{i},!}the spectral decompositions of C{displaystyle mathbf {C} ,!} and B{displaystyle mathbf {B} ,!} is given by
Therefore, the uniqueness of the spectral decomposition also implies that ni=RNi{displaystyle mathbf {n} _{i}=mathbf {R} ~mathbf {N} _{i},!}. The left stretch (V{displaystyle mathbf {V} ,!}) is also called the spatial stretch tensor while the right stretch (U{displaystyle mathbf {U} ,!}) is called the material stretch tensor.
The effect of F{displaystyle mathbf {F} ,!} acting on Ni{displaystyle mathbf {N} _{i},!} is to stretch the vector by λi{displaystyle lambda _{i},!} and to rotate it to the new orientation ni{displaystyle mathbf {n} _{i},!}i.e.,
This is the case where a specimen is stretched in 1-direction with a stretch ratio of α=α1{displaystyle mathbf {alpha =alpha _{1}} ,!}. If the volume remains constant, the contraction in the other two directions is such that α1α2α3=1{displaystyle mathbf {alpha _{1}alpha _{2}alpha _{3}=1} ,!} or α2=α3=α−0.5{displaystyle mathbf {alpha _{2}=alpha _{3}=alpha ^{-0.5}} ,!}. Then:
Derivatives of the stretch with respect to the right Cauchy–Green deformation tensor are used to derive the stress-strain relations of many solids, particularly hyperelastic materials. These derivatives are
Physical interpretation of deformation tensors[edit]
Let X=XiEi{displaystyle mathbf {X} =X^{i}~{boldsymbol {E}}_{i}} be a Cartesian coordinate system defined on the undeformed body and let x=xiEi{displaystyle mathbf {x} =x^{i}~{boldsymbol {E}}_{i}} be another system defined on the deformed body. Let a curve X(s){displaystyle mathbf {X} (s)} in the undeformed body be parametrized using s∈[0,1]{displaystyle sin [0,1]}. Its image in the deformed body is x(X(s)){displaystyle mathbf {x} (mathbf {X} (s))}.
The concept of strain is used to evaluate how much a given displacement differs locally from a rigid body displacement.[1][10] One of such strains for large deformations is the Lagrangian finite strain tensoralso called the Green-Lagrangian strain tensor or Green – St-Venant strain tensordefined as
Derivation of the Lagrangian and Eulerian finite strain tensors
A measure of deformation is the difference between the squares of the differential line element dX{displaystyle dmathbf {X} ,!}in the undeformed configuration, and dx{displaystyle dmathbf {x} ,!}in the deformed configuration (Figure 2). Deformation has occurred if the difference is non zero, otherwise a rigid-body displacement has occurred. Thus we have,
where CKL{displaystyle C_{KL},!} are the components of the right Cauchy–Green deformation tensorC=FTF{displaystyle mathbf {C} =mathbf {F} ^{T}mathbf {F} ,!}. Then, replacing this equation into the first equation we have,
where EKL{displaystyle E_{KL},!}are the components of a second-order tensor called the Green – St-Venant strain tensor or the Lagrangian finite strain tensor,
where ∂XM∂xn{displaystyle {frac {partial X_{M}}{partial x_{n}}},!} are the components of the spatial deformation gradient tensorH{displaystyle mathbf {H} ,!}. Thus we have
where the second order tensor crs{displaystyle c_{rs},!} is called Cauchy's deformation tensorc=F−TF−1{displaystyle mathbf {c} =mathbf {F} ^{-T}mathbf {F} ^{-1},!}. Then we have,
Both the Lagrangian and Eulerian finite strain tensors can be conveniently expressed in terms of the displacement gradient tensor. For the Lagrangian strain tensor, first we differentiate the displacement vector u(X,t){displaystyle mathbf {u} (mathbf {X} ,t),!} with respect to the material coordinates XM{displaystyle X_{M},!} to obtain the material displacement gradient tensor∇Xu{displaystyle nabla _{mathbf {X} }mathbf {u} ,!}
which do not belong to the Seth–Hill class, but have the same 2nd-order approximation as the Seth–Hill measures at m=0{displaystyle m=0} for any value of n{displaystyle n}.[16]
The stretch ratio is a measure of the extensional or normal strain of a differential line element, which can be defined at either the undeformed configuration or the deformed configuration.
The stretch ratio for the differential element dX=dXN{displaystyle dmathbf {X} =dXmathbf {N} ,!} (Figure) in the direction of the unit vector N{displaystyle mathbf {N} ,!} at the material point P{displaystyle P,!}in the undeformed configuration, is defined as
where dx{displaystyle dx,!} is the deformed magnitude of the differential element dX{displaystyle dmathbf {X} ,!}.
Similarly, the stretch ratio for the differential element dx=dxn{displaystyle dmathbf {x} =dxmathbf {n} ,!} (Figure), in the direction of the unit vector n{displaystyle mathbf {n} ,!} at the material point p{displaystyle p,!}in the deformed configuration, is defined as
The normal strain eN{displaystyle e_{mathbf {N} },!} in any direction N{displaystyle mathbf {N} ,!} can be expressed as a function of the stretch ratio,
This equation implies that the normal strain is zero, i.e. no deformation, when the stretch is equal to unity. Some materials, such as elastometers can sustain stretch ratios of 3 or 4 before they fail, whereas traditional engineering materials, such as concrete or steel, fail at much lower stretch ratios, perhaps of the order of 1.1 (reference?)
Physical interpretation of the finite strain tensor[edit]
The diagonal components EKL{displaystyle E_{KL},!} of the Lagrangian finite strain tensor are related to the normal strain, e.g.
where ϕ12{displaystyle phi _{12},!} is the change in the angle between two line elements that were originally perpendicular with directions I1{displaystyle mathbf {I} _{1},!} and I2{displaystyle mathbf {I} _{2},!}respectively.
Under certain circumstances, i.e. small displacements and small displacement rates, the components of the Lagrangian finite strain tensor may be approximated by the components of the infinitesimal strain tensor
Derivation of the physical interpretation of the Lagrangian and Eulerian finite strain tensors
The stretch ratio for the differential element dX=dXN{displaystyle dmathbf {X} =dXmathbf {N} ,!} (Figure) in the direction of the unit vector N{displaystyle mathbf {N} ,!} at the material point P{displaystyle P,!}in the undeformed configuration, is defined as
where dx{displaystyle dx,!} is the deformed magnitude of the differential element dX{displaystyle dmathbf {X} ,!}.
Similarly, the stretch ratio for the differential element dx=dxn{displaystyle dmathbf {x} =dxmathbf {n} ,!} (Figure), in the direction of the unit vector n{displaystyle mathbf {n} ,!} at the material point p{displaystyle p,!}in the deformed configuration, is defined as
where NK{displaystyle N_{K},!} and NL{displaystyle N_{L},!} are unit vectors.
The normal strain or engineering strain eN{displaystyle e_{mathbf {N} },!} in any direction N{displaystyle mathbf {N} ,!} can be expressed as a function of the stretch ratio,
Thus, the normal strain in the direction I1{displaystyle mathbf {I} _{1},!} at the material point P{displaystyle P,!} may be expressed in terms of the stretch ratio as
The shear strainor change in angle between two line elements dX1{displaystyle dmathbf {X} _{1},!} and dX2{displaystyle dmathbf {X} _{2},!} initially perpendicular, and oriented in the principal directions I1{displaystyle mathbf {I} _{1},!} and I2{displaystyle mathbf {I} _{2},!}respectivelly, can also be expressed as a function of the stretch ratio. From the dot product between the deformed lines dx1{displaystyle dmathbf {x} _{1},!} and dx2{displaystyle dmathbf {x} _{2},!} we have
where θ12{displaystyle theta _{12},!} is the angle between the lines dx1{displaystyle dmathbf {x} _{1},!} and dx2{displaystyle dmathbf {x} _{2},!} in the deformed configuration. Defining ϕ12{displaystyle phi _{12},!} as the shear strain or reduction in the angle between two line elements that were originally perpendicular, we have
Deformation tensors in convected curvilinear coordinates[edit]
A representation of deformation tensors in curvilinear coordinates is useful for many problems in continuum mechanics such as nonlinear shell theories and large plastic deformations. Let x=x(ξ1,ξ2,ξ3){displaystyle mathbf {x} =mathbf {x} (xi ^{1},xi ^{2},xi ^{3})} denote the function by which a position vector in space is constructed from coordinates (ξ1,ξ2,ξ3){displaystyle (xi ^{1},xi ^{2},xi ^{3})}. The coordinates are said to be "convected" if they correspond to a one-to-one mapping to and from Lagrangian particles in a continuum body. If the coordinate grid is "painted" on the body in its initial configuration, then this grid will deform and flow with the motion of material to remain painted on the same material particles in the deformed configuration so that grid lines intersect at the same material particle in either configuration. The tangent vector to the deformed coordinate grid line curve ξi{displaystyle xi ^{i}} at x{displaystyle mathbf {x} } is given by
gi=∂x∂ξi{displaystyle mathbf {g} _{i}={frac {partial mathbf {x} }{partial xi ^{i}}}}
The three tangent vectors at x{displaystyle mathbf {x} } form a local basis. These vectors are related the reciprocal basis vectors by
To see how the Christoffel symbols are related to the Right Cauchy–Green deformation tensor let us similarly define two bases, the already mentioned one that is tangent to deformed grid lines and another that is tangent to the undeformed grid lines. Namely,
Some relations between deformation measures and Christoffel symbols[edit]
Let us consider a one-to-one mapping from X={X1,X2,X3}{displaystyle mathbf {X} ={X^{1},X^{2},X^{3}}} to x={x1,x2,x3}{displaystyle mathbf {x} ={x^{1},x^{2},x^{3}}} and let us assume that there exist two positive-definite, symmetric second-order tensor fields G{displaystyle {boldsymbol {G}}} and g{displaystyle {boldsymbol {g}}} that satisfy
The problem of compatibility in continuum mechanics involves the determination of allowable single-valued continuous fields on bodies. These allowable conditions leave the body without unphysical gaps or overlaps after a deformation. Most such conditions apply to simply-connected bodies. Additional conditions are required for the internal boundaries of multiply connected bodies.
We can show these are the mixed components of the Riemann–Christoffel curvature tensor. Therefore, the necessary conditions for C{displaystyle {boldsymbol {C}}}-compatibility are that the Riemann–Christoffel curvature of the deformation is zero.
Compatibility of the left Cauchy–Green deformation tensor[edit]
No general sufficiency conditions are known for the left Cauchy–Green deformation tensor in three-dimensions. Compatibility conditions for two-dimensional B{displaystyle {boldsymbol {B}}} fields have been found by Janet Blume.[17][18]
^A. Yavari, J.E. Marsden, and M. Ortiz, On spatial and material covariant balance laws in elasticity, Journal of Mathematical Physics, 47, 2006, 042903; pp. 1–53.
^Owens, Eduardo de Souza Neto, Djordje Peric, David (2008). Computational methods for plasticity : theory and applications. Chichester, West Sussex, UK: Wiley. p. 65. ISBN978-0-470-69452-7.
^The IUPAC recommends that this tensor be called the Cauchy strain tensor.
^Belytschko, Ted; Liu, Wing Kam; Moran, Brian (2000). Nonlinear Finite Elements for Continua and Structures (reprint with corrections, 2006 ed.). John Wiley & Sons Ltd. pp. 92–94. ISBN978-0-471-98773-4.
^Seth, B. R. (1962), "Generalized strain measure with applications to physical problems", IUTAM Symposium on Second Order Effects in Elasticity, Plasticity and Fluid Mechanics, Haifa, 1962.
^T.C. Doyle and J.L. Eriksen (1956). "Non-linear elasticity." Advances in Applied Mechanics 4, 53–115.
^Z.P. Bažant and L. Cedolin (1991). Stability of Structures. Elastic, Inelastic, Fracture and Damage Theories. Oxford Univ. Press, New York (2nd ed. Dover Publ., New York 2003; 3rd ed., World Scientific 2010).
^Z.P. Bažant (1998). "Easy-to-compute tensors with symmetric inverse approximating Hencky finite strain and its rate." Journal of Materials of Technology ASME120 (April), 131–136.
^Blume, J. A. (1989). "Compatibility conditions for a left Cauchy–Green strain field". J. Elasticity. 21: 271–308. doi:10.1007/BF00045780.
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