Conservation of the Linear Momentum
CH.5. BALANCE PRINCIPLES
Multimedia Course on Continuum Mechanics Overview
Balance Principles Lecture 1 Convective Flux or Flux by Mass Transport Lecture 2 Lecture 3 Local and Material Derivative of a Volume Integral Lecture 4 Conservation of Mass Spatial Form Lecture 5 Material Form Reynolds Transport Theorem Lecture 6 Reynolds Lemma General Balance Equation Lecture 7 Linear Momentum Balance Global Form Lecture 8 Local Form
2 Overview (cont’d)
Angular Momentum Balance Global Spatial Lecture 9 Local Form Mechanical Energy Balance External Mechanical Power Lecture 10 Mechanical Energy Balance External Thermal Power Energy Balance Thermodynamic Concepts Lecture 11 First Law of Thermodynamics Internal Energy Balance in Local and Global Forms Lecture 12 Second Law of Thermodynamics Lecture 13 Reversible and Irreversible Processes Lecture 14 Clausius-Planck Inequality Lecture 15
3 Overview (cont’d)
Governing Equations Governing Equations Lecture 16 Constitutive Equations The Uncoupled Thermo-mechanical Problem
4 5.1. Balance Principles
Ch.5. Balance Principles
5 Balance Principles
The following principles govern the way stress and deformation vary in the neighborhood of a point with time. REMARK The conservation/balance principles: These principles are always Conservation of mass valid, regardless of the type of material and the range of Linear momentum balance principle displacements or deformations. Angular momentum balance principle Energy balance principle or first thermodynamic balance principle
The restriction principle: Second thermodynamic law
The mathematical expressions of these principles will be given in, Global (or integral) form Local (or strong) form
6 5.2. Convective Flux
Ch.5. Balance Principles
7 Convection
The term convection is associated to mass transport, i.e., particle movement. Properties associated to mass will be transported with the mass when there is mass transport (particles motion) convective transport
Convective flux of an arbitrary property A through a control surface S :
amountof crossing S Φ= A S unitof time
8 Convective Flux or Flux by Mass Transport
Consider: An arbitrary property of a continuum medium (of any tensor order) A The description of the amount of the property per unit of mass, Ψ () x , t (specific content of the property ) . A The volume of particles dV crossing a differential surface dS during the interval [] t , t + dt is dV=⋅=⋅ dS dhvn dt dS dm=ρρ dV =vn ⋅ dSdt Then, The amount of the property crossing the differential surface per unit of time is: Ψ dm d Φ= =ρ Ψ⋅vn dS S dt 9 Convective Flux or Flux by Mass Transport
Consider: An arbitrary property of a A continuum medium (of any tensor order) inflow vn⋅≤0 outflow The specific content of A (the amount vn⋅≥0 of per unit of mass) Ψ x , t . A ()
Then, The convective flux of through a spatial surface, S , with unit normal n is: A v is velocity Φ()t =ρ Ψ⋅vndS Where: S ∫s ρ is density
If the surface is a closed surface, SV = ∂ , the net convective flux is:
Φ∂ ()t =ρ Ψ⋅vndS = outflow - inflow V ∫∂V
10 Convective Flux
REMARK 1 The convective flux through a material surface is always null. REMARK 2 Non-convective flux (conduction, radiation). Some properties can be transported without being associated to a certain mass of particles. Examples of non-convective transport are: heat transfer by conduction, electric current flow, etc. Non-convective transport of a certain property is characterized by the non- convective flux vector (or tensor) qx () , t : non - convectiveflux =qn⋅=dS ; convectiveflux ρψ vn⋅dS ∫∫ss non-convective flux convective vector flux vector
11 Example
Compute the magnitude and the convective flux Φ S which correspond to the following properties: a) volume b) mass c) linear momentum d) kinetic energy
12 Φ =ρ Ψ⋅ S ()t ∫ vndS Example - Solution s
a) If the arbitrary property is the volume of the particles: ≡ V A The magnitude “property content per unit of mass” is volume per unit of mass, i.e., the inverse of density:
V 1 Ψ= = M ρ
The convective flux of the volume of the particles V through the surface S is:
1 Φ=ρ vn ⋅dS = vn ⋅ dS VOLUME FLUX S ∫∫ssρ
13 Φ =ρ Ψ⋅ S ()t ∫ vndS Example - Solution s
b) If the arbitrary property is the mass of the particles: ≡ M A The magnitude “property per unit of mass” is mass per unit of mass, i.e., the unit value:
M Ψ= =1 M
The convective flux of the mass of the particles M through the surface S is:
Φ=ρρ1 vn ⋅dS = vn ⋅ dS MASS FLUX S ∫∫ss
14 Φ =ρ Ψ⋅ S ()t ∫ vndS Example - Solution s
c) If the arbitrary property is the linear momentum of the particles: ≡ M v A The magnitude “property per unit of mass” is mass times velocity per unit of mass, i.e., velocity:
M v Ψ = = v M
The convective flux of the linear momentum of the particles M v through the surface S is:
Φ =ρ vvn() ⋅ dS MOMENTUM FLUX S ∫s
15 Φ =ρ Ψ⋅ S ()t ∫ vndS Example - Solution s
d) If the arbitrary property is the kinetic energy of the particles: 1 ≡ M v2 A 2 The magnitude “property per unit of mass” is kinetic energy per unit of mass, i.e.: 1 M v2 1 Ψ=2 = v2 M 2 1 The convective flux of the kinetic energy of the particles M v 2 through the surface S is: 2 1 Φ=ρ v2 () vn ⋅ dS KINETIC ENERGY FLUX S ∫s 2
16 5.3. Local and Material Derivative of a Volume Integral Ch.5. Balance Principles
17 Derivative of a Volume Integral
Consider: An arbitrary property of a continuum medium (of any tensor order) A The description of the amount of the property per unit of volume (density of the property ), µ () x , t A REMARK and Ψ are related The total amount of the property through . in an arbitrary volume, V , is: Q()t Q()() t= ∫ µ x, t dV V Q()tt+∆ The time derivative of this volume integral is: Qt()()+∆ t − Qt Qt′() = lim ∆→t 0 ∆t
18 Local Derivative of a Volume Integral
Consider: Q()t The volume integral Q()() t= ∫ µ x, t dV V Q()tt+∆ Control Volume, V The local derivative of Qt () is: µµ()()xx,,t+∆ t dV − t dV local not ∂ ∫∫ REMARK = µ ()x,t dV = lim VV ∫ ∆→t 0 derivative ∂∆t V t The volume is fixed in space (control volume). It can be computed as: µµ()()xx,t+∆ t dV − , t dV ∂ Qt()()+∆ t − Qt ∫∫ µ ()x,t dV = lim = lim VV= ∫ ∆→tt00∆→ ∂∆ttV ∆ t [µµ()()xx ,t+∆ t − ,] t dV ∫ µµ()()xx,,tt+∆ − t∂ µ() x , t = lim V = lim dV = dV ∆→tt00∆∫∫∆→ ∆∂ tVV tt ∂µx,t ∂t 19 Material Derivative of a Volume Integral
Consider: The volume integral Q()() t= ∫ µ x, t dV V
Q()tt+∆ The material derivative of Qt () is: Q()t material not d derivative = ∫ µ ()x,t dV = dt ≡ VVt µµ()()xx,,t+∆ t dV − t dV REMARK ∫∫Vt()+∆ t Vt() = lim The volume is mobile in space ∆→t 0 ∆ t and can move, rotate and It can be proven that: deform (material volume). dd∂∂µµ µ()x,t dV =µ dV + ∇⋅() µ vv dV = +∇⋅() µµ dV = + ∇⋅ v dV dt ∫∂∂t ∫∫ ∫t ∫dt VVt ≡ V V V V material local convective derivative of derivative of derivative of the integral the integral the integral
20 5.4. Conservation of Mass
Ch.5. Balance Principles
21 Principle of Mass Conservation
It is postulated that during a motion there are neither mass sources nor mass sinks, so the mass of a continuum body is a conserved quantity (for any part of the body).
The total mass () t of the system satisfies:M ()()t= tt +∆ >0 MM
Where: ()()t= ρ x, t dV∀∆ V ⊂ V ∆ tt M ∫ Vt ()()tt+∆ =ρ x, ttdVV +∆ ∀∆ ⊂ V ∆ tt+∆ tt +∆ M ∫ Vtt+∆ 22 Conservation of Mass in Spatial Form
Conservation of mass requires that the material time derivative of the mass () t be zero for any region of a material volume, M ()()tt+∆ − t d ′()t = lim MM= ρdV=0 ∀∆ V ⊂ V , ∀ t ∫∆⊂≡ M ∆→t 0 ∆t dt Vtt VV The global or integral spatial form of mass conservation principle: ddµ µµ()xv,t dV =( + ∇⋅ ) dV dt ∫∫dt VVt ≡ V ddρ ρρ(,)xvt dV = + ∇ ⋅dV =0 ∀∆ V ⊂ V , ∀ t ∫∫∆ ⊂≡ ∆⊂ dt VVVtt VVdt By a localization process we obtain the local or differential spatial form of mass conservation principle: for∆→ V dV(,)x t (localization process) CONTINUITY EQUATION dtρρ(,)xx∂ (,)t +(ρρ∇∇ ⋅vx )( ,t ) = + ⋅(vx )( ,t ) = 0 ∀∈ x Vt , ∀ dt ∂t 23 Conservation of Mass in Material Form
d F 1 d F =Fv∇ ⋅ ()∇ ⋅=v Consider the relations: dt F dt dV= F dV0 The global or integral material form of mass conservation principle can be rewritten as: ddρρ 1dtF ∂ ρ(X ,) t∂ FX( ,) ()(+ρρ ∇⋅vdV = + ) dV = (FX ( ,t ) +ρ) dV0 ∫∫V dt dtF dt ∫∂∂t t ∆VV0 ∂ρ F dV0 (X ,)t ∂ [ρ |FX |]( ,t ) ∂ t ∂t ∂ → ρ FX() ,t dV0=0 ∀∆ V00 ⊂ V , ∀ t ∫ ∂t ∆VV00⊂ The local material form of mass conservation principle reads : ∂ ρ ρ = ρρ= 0 FX()(),0t tt=0 XFtt=0 () X F() X ρ = ∀∈X Vt, ∀ ∂t t F 0 =1 t 24 5.5. Reynolds Transport Theorem
Ch.5. Balance Principles
25 dρ +ρ∇ ⋅=v 0 Reynolds Lemma dt
Consider: An arbitrary property of a continuum medium (of any tensor order) A The spatial description of the amount of the property per unit of mass, ψ () x , t (specific contents of ) A The amount of the property in the continuum body at time t A for an arbitrary material volume is: Q() t= ∫ ρψ dV VVt =
Using the material time derivative leads to, d d ddψρ Q′() t =ρψdV =()() ρψ + ρψ ∇∇ ⋅vvdV =ρ + ψ( +⋅ ρ ) dV dt ∫∫dt ∫dt dt VVt ≡ V V ddψρ =ρψ + Thus, dt dt =0 (continuity equation) ddψ REYNOLDS ρψdV= ρ dV dt ∫∫dt LEMMA VVt ≡ V 26 d ∂ µ()xv,t dV= µµ dV + ∇⋅() dV dt ∫∂t ∫∫ VVt ≡ V V Reynolds Transport Theorem
The amount of the property in the continuum body at time t for A an arbitrary fixed control volume is: Q() t= ∫ ρψ dV V Using the material time derivative leads to, d ∂ ()ρψ ρψ dV = dV +⋅∇ ()ρ ψ; v dV dt ∫∫∂t ∫ VVt ≡ V V dψ dψ = ∫ ρ dV = ∫ nv⋅()ρψ dV ρ V dt ∂V dt And, introducing the Reynolds Lemma ∂V and Divergence Theorem: dV dψ ∂ ()ρψ ∫∫ρ dV = dV +⋅ ∫ρψ vn dS VVdt ∂t ∂ V eˆ ρψ REMARK 3 ∫ dV eˆ 2 V
The Divergence Theorem: eˆ1 ∫ ∇⋅vdV = ∫∫ nv ⋅ dS = vn ⋅ dS V ∂∂ VV 27 dψ ∂ (ρψ ) ρ dV = dV +⋅ρψ vn dS ∫∫dt ∂t ∫ Reynolds Transport TheoremVV ∂ V
The eq. can be rewritten as: ∂ dψ REYNOLDS TRANSPORT ∫∫∫ρψ dV= ρ dV −⋅ ρψ vn dS ∂t VVdt ∂ V THEOREM
Change due to the net outward convective flux of through the Change (per unit of time) of A the total amount of . within boundary ∂ V . A dψ the control volume V at time t. ρ dt
Rate of change of the amount of property ∂V integrated over all particles that are fillingA dV the control volume V at time t.
eˆ ρψ 3 ∫ dV eˆ 2 V
eˆ1
28 Reynolds Transport Theorem
∂ dψ REYNOLDS TRANSPORT ∫∫∫ρψ dV= ρ dV −⋅ ρψ vn dS ∂t VVdt ∂ V THEOREM (integral form)
∂ dψ dψ ρψ dV= ρ dV −⋅ ρψ vn dS ρ ∂t ∫∫∫dt dt VV∂ V ∂V ∂ = (ρψ ) dV =∫∇ ⋅(ρψ v) dV ∫ V V ∂t dV ∂ dψ (ρψ ) dV = [ ρ −∇ ⋅ ( ρψ v)] dV∀∆ V ⊂ V ∀ t ∫∫∂t dt ∆⊂VV ∆⊂VV eˆ ρψ 3 ∫ dV eˆ 2 V ∂ dψ eˆ (ρψ )= ρ −∇ ⋅ ( ρψ vx) ∀∈Vt ∀ 1 ∂t dt REYNOLDS TRANSPORT THEOREM (local form)
29 5.6. General Balance Equation
Ch.5. Balance Principles
30 General Balance Equation
Consider: An arbitrary property of a continuum medium (of anyA tensor order) The amount of the property per unit of mass, ψ ()x,t The rate of change per unit of time of the amount of in the control volume V is due to: A kt(,)x a) Generation of the property per unit mas and time time due to a source: A b) The convective (net incoming) flux across the surface of the volume. source term c) The non-convective (net incoming) flux across the surface of the volume: jx(,)t A non-convective So, the global form of the general balance equation is: flux vector ∂ ρψ dV= ρ k dV − ρψ vn ⋅ dS −⋅ j n dS ∂t ∫∫∫AA ∫ VV∂∂ V V acb
31 ∂ ρψ dV= ρ k dV − ρψ vn ⋅−⋅ dS j n dS ∂t ∫∫AA ∫ ∫ General BalanceVV Equation ∂∂ V V
The global form is rewritten using the Divergence Theorem and the definition of local derivative: ∂ ∫∫ρψ dV + ρψ vn ⋅= dS ∂t VV∂ ∂ =()()ρψ +⋅∇∇ ρψ vjdV =( ρ k −⋅ ) dV ∫∫AA VV∂t dψ = ρ (Reynolds Theorem) dt dψ ρρ dV=( k −∇ ⋅j ) dV ∀∆ V ⊂ V ∀ t ∫∫AA ∆⊂VV dt ∆⊂VV The local spatial form of the general balance equation is: REMARK dψ dψ ρ =ρk −⋅∇ j For only convective transport () j0 = then ρ = ρ k dt AA A dt A and the variation of the contents of in a given particle is only due to the internal generation ρ k . A 32 dψ ρ =ρk −⋅∇ j dt AA ∂ dψ Example (ρψ )= ρ −∇ ⋅ ( ρ ψ vx) ∀∈V ∂t dt
If the property is associated to mass ≡ , then: A AM The amount of the property per unit of mass is ψ = 1 . The mass generation source term is k = 0 . M The mass conservation principle states that mass cannot be generated. The non-convective flux vector is j = 0 . M Mass cannot be transported in a non-convective form. dψ ρ =ρ k −⋅∇ j =0 dt AA =0 =0 Then, the local spatial form of the general balance equation is: dψ ∂ ∂ρ ρ =(ρψ ) +⋅∇ ( ρψ v) = 0 +⋅∇ (ρv )0 = dt ∂ ∂t t =11= ∂ρρd Two equivalent forms of +∇∇ ⋅()ρρv = + ⋅ vx =0 ∀∈Vt ∀ ∂t dt the continuity equation.
33 5.7. Linear Momentum Balance
Ch.5. Balance Principles
34 Linear Momentum in Classical Mechanics
Applying Newton’s 2nd Law to the discrete system formed by n particles, the resulting force acting on the system is: nn ndv Rt= fa = mm =i = () ∑∑iiii ∑ ii=11 = i= 1dt Resulting force mass conservation on the system dm principle: i = 0 nn dt d dmi dt() =∑∑miivv −=i P dt ii=11= dt dt = ()t linear momentum P For a system in equilibrium, R = 0, ∀ t : dt() P = 0 ()t= cnt CONSERVATION OF THE dt P LINEAR MOMENTUM
35 n Linear Momentum ()tm= v P ∑ ii in Continuum Mechanics i=1
The linear momentum of a material volume V t of a continuum medium with mass is: M ()()()()t= vx, td= ρ x ,, t vx tdV P ∫∫M M V
d= ρ dV M
36 Linear Momentum Balance Principle
The time-variation of the linear momentum of a material volume is equal to the resultant force acting on the material volume.
dt() d P = ρ vR dV= () t dt dt ∫ Vt
Where: body forces R()t=∫∫ρ bt dV + dS VV∂ surface forces
If the body is in equilibrium, the linear momentum is conserved: dt() R ()t = 0 P = 0 ()t= cnt dt P
37 Global Form of the Linear Momentum Balance Principle
The global form of the linear momentum balance principle: d dt() = ρρ+ = =P ∀∆ ⊂ ∀ R()t ∫∫ bt dV dS ∫ v dV V V, t ∆⊂ ∂∆⊂ dt ∆ ⊂ ≡ dt VV VV Vtt VV t P ( )
Introducing tn = ⋅ σ and using the Divergence Theorem, ∫∫tn dS=⋅=⋅σ dS ∫ ∇σ dV ∂∂VV V So, the global form is rewritten: ∫∫ρ bt dV+= dS ∆⊂VV ∂∆⊂VV d = ()ρρ bv +∇σ⋅dV = dV∀∆ V ⊂ V, ∀ t ∫∫dt 38 ∆⊂VV ∆VVVtt ⊂≡ Local Form of the Linear Momentum Balance Principle
Applying Reynolds Lemma to the global form of the principle: ddv ()∇⋅ σ+ρ bv dV = ρρ dV = dV∀∆ V ⊂ V, ∀ t ∫ dt ∫∫dt ∆⊂VV ∆VVVtt ⊂≡ ∆⊂VV
Localizing, the linear momentum balance principle reads:
∆→V dV(,)x t dtvx(,) ∇σ⋅ (,)xt +ρρ bx(,) t= = ρax (,)t ∀∈x Vt , ∀ dt LOCAL FORM OF THE LINEAR MOMENTUM BALANCE (CAUCHY’S EQUATION OF MOTION)
39 5.8. Angular Momentum Balance
Ch.5. Balance Principles
40 Angular Momentum in Classical Mechanics
Applying Newton’s 2nd Law to the discrete system formed by n particles, the resulting torque acting on the system is:
nn dvi MO()tm=∑∑ rfii ×= r i × i = ii=11= dt =0 nn n d dri dd =∑∑rvi ×−mm ii ×=ii v ∑ rvi ×= m ii L dt ii=11= dt dt i= 1dt = v = ()t i angularL momentum dt() M ()t = L O dt
For a system in equilibrium, M O = 0, ∀ t : dt() CONSERVATION OF THE L = 0 ∀t ()t= cnt dt L ANGULAR MOMENTUM
41 Angular Momentum in Continuum Mechanics
The angular momentum of a material volume V t of a continuum medium with mass is: M ()t=×=×r vx(),td xρ ()() x,,t vx tdV L ∫∫ M ≡x V M
d= ρ dV M
42 Angular Momentum Balance Principle
The time-variation of the angular momentum of a material volume with respect to a fixed point is equal to the resultant moment with respect to this fixed point.
dt() d = ×=ρ L rv dV MO ()t dt dt ∫ ≡ VVt ≡ x
Where: torque due to body forces =×ρ +× MO ()t ∫∫ r b dV rt dS VV∂ torque due to surface forces
43 Global Form of the Angular Momentum Balance Principle
The global form of the angular momentum balance principle: d (rb×ρρ ) dV +× ( rt ) dS = ( rv × ) dV ∫∫ dt ∫ V ∂≡V VVt
Introducing tn = ⋅ σ and using the Divergence Theorem, ∫∫ rt× dS = rn ×⋅σσ dS = ∫ r ×TT ⋅ n dS = ∫() r × σ ⋅ n dS = ∂∂VV ∂ V ∂ V =×⋅∫ ()r σ∇T dV V It can be proven that, REMARK T is the Levi-Civita ()r×σ∇ ⋅ = rm ×∇⋅σ + ijk permutation symbol. = = σ memmiˆ i; i ijk jk
44 Global Form of the Angular Momentum Balance Principle
Applying Reynolds Lemma to the right-hand term of the global form equation: Reynold's Lemma dd↓ d r×ρρ v dV =()rv ×dV = ρ()rv ×=dV dt ∫∫dt ∫dt VVtt≡ VV≡ V ddrv=0 d v =ρρ ×+×vrdV = r × dV ∫∫dt dt dt VV= v
Then, the global form of the balance principle is rewritten: dv ×ρσ +∇⋅σ + ˆ = × ρ ∫∫rb() ijk jk e i dV r dV VVdt
45 Local Form of the Angular Momentum Balance Principle
Rearranging the equation: =0 (Cauchy’s Eq.) dv r× ∇ ⋅σ− + ρρ b+ m dV = 0 mx(,)t dV= 0 ∀∆ V ⊂ V, ∀ t ∫∫ ∆⊂VV ∆⊂VVdt
Localizing
mx(,)t= 0 mi = ijkσ jk =0 ;i , jk , ∈{} 1, 2, 3 ; ∀∈x Vt , ∀ t i =10⇒⇒σ += σ σσ = 123 23 132 32 23 32 σ σσ =11 =− 11 12 13 i =20⇒⇒σ += σ σσ = σ ≡ σ12 σσ 22 23 231 31 213 13 31 13 = =− 11 σ13 σσ23 33 i =30⇒⇒σ += σ σσ = 312 12 321 21 12 21 = =− 11 T σσ(,)xxxt= (,) t ∀∈ Vtt , ∀ SYMMETRY OF THE CAUCHY’S STRESS TENSOR 46 5.9. Mechanical Energy Balance
Ch.5. Balance Principles
47 Power
Power, Wt () , is the work performed in the system per unit of time.
In some cases, the power is an exact time-differential of a function (then termed) energy : E dt() Wt()= E dt It will be assumed that the continuous medium absorbs power from the exterior through: Mechanical Power: the work performed by the mechanical actions (body and surface forces) acting on the medium. Thermal Power: the heat entering the medium.
48 External Mechanical Power
The external mechanical power is the work done by the body forces and surface forces per unit of time. In spatial form it is defined as: P() t=ρ bv ⋅ dV +⋅ tv dS e ∫∫VV∂
dr ρρb⋅=⋅ dV bv dV dt =v dr t⋅=⋅dS tv dS dt =v Mechanical Energy Balance
Using tn = ⋅ σ and the Divergence Theorem, the traction contribution reads, Divergence Theorem ↓ t⋅vndS = ⋅()σ⋅ vdS = ∇⋅()σ ⋅vdV = ()∇⋅σσ ⋅vv +: ∇ dV ∫∫∂∂VV ∫ V ∫ V n⋅σ = l spatial velocity Taking into account the identity: ld = + w =0 skew gradient tensor σσ:l= :d + σ :w symmetric
So, tv⋅dS =()∇ ⋅⋅σσvdV+ : d dV ∫∫∂VV ∫ V
50 dv ∇⋅= σ+ρρ b Mechanical Energy Balance dt
Substituting and collecting terms, the external mechanical power in spatial form is, ∫ tv⋅ dS ∂V
Pe () t=ρ bv ⋅+ dV ()∇⋅σσ ⋅vddV +: dV = ∫V ∫∫VV dv =∇⋅+⋅+()σσρρbvdvddV:: dV = ⋅+dV σdV ∫V ∫∫VVV ∫ dt =ρ dv dd112 dt =ρ (vv ⋅= )ρ ( v) dt 22dt v= v
Reynold's Lemma dd11↓ =ρρ22 +=σσ + Pe () t ∫( v)dV ∫:d dV ∫∫( v)dV:d dV Vdt 22 Vdt VV
51 Mechanical Energy Balance. Theorem of the expended power. Stress power
d 1 P( t) =ρρb ⋅ v dV +⋅ t v dS =v2dV +σ :d dV e ∫∫VV∂ dt ∫∫2 VVt ≡ V
external mechanical power P kinetic energy σ entering the medium K stress power d Pt( ) =( t) + P Theorem of the expended e dt K σ mechanical power REMARK The stress power is the mechanical power entering the system which is not spent in changing the kinetic energy. It can be interpreted as the work by unit of time done by the stress in the deformation process of the medium. A rigid solid will produce zero stress power ( d0 = ) .
52 External Thermal Power
The external thermal power is incoming heat in the continuum medium per unit of time. The incoming heat can be due to: Non-convective heat transfer across the volume’s surface. incoming heat − qx(,)t ⋅= n dS ∫ unit of time ∂V heat conduction flux vector
Internal heat sources heat generated by internal sources ρ r(,)x t dV = ∫ unit of time V specific internal heat production
53 External Thermal Power
The external thermal power is incoming heat in the continuum medium per unit of time. In spatial form it is defined as: =ρρ − ⋅ = −⋅∇ Qe () t∫∫∫ r dVqn dS ( rq ) dV V∂ VV =∫ nq ⋅ dS ∂V =∫(∇ ⋅q) dV V where: qx () , t is the non-convective heat flux vector per unit of spatial surface rt () x , is the internal heat source rate per unit of mass.
54 Total Power
The total power entering the continuous medium is:
d 1 PQ+= ρρv2dV+σ :d dV + r dV −q ⋅ n dS eedt ∫2 ∫ ∫∫ VVt ≡∂V V V
55 5.10. Energy Balance
Ch.5. Balance Principles
56 Thermodynamic Concepts
A thermodynamic system is a macroscopic region of the continuous medium, always formed by the same collection of continuous matter (material volume). It can be: ISOLATED SYSTEM OPEN SYSTEM Thermodynamic space
MATTER
HEAT
A thermodynamic system is characterized and defined by a set of thermodynamic variables µµ 1, 2, .... µ n which define the thermodynamic space.
The set of thermodynamic variables necessary to uniquely define a system is called the thermodynamic state of a system.
57 Thermodynamic Concepts
A thermodynamic process is the energetic development of a thermodynamic system which undergoes successive thermodynamic states, changing from an initial state to a final state → Trajectory in the thermodynamic space. If the final state coincides with the initial state, it is a closed cycle process.
A state function is a scalar, vector or tensor entity defined univocally as a function of the thermodynamic variables for a given system. It is a property whose value does not depend on the path taken to reach that specific value.
58 State Function
Is a function φµ () 1 ,..., µ n uniquely valued in terms of the “thermodynamic state”
or, equivalently, in terms of the thermodynamic variables { µµ 12 ,,, µ n }
Consider a function φµµ () 12 , , that is not a state function, implicitly defined in the thermodynamic space by the differential form:
δφ= f1()() µµ 12, df µ 1+ 2 µµ 12 , d µ 2 The thermodynamic processes Γ 1 and Γ 2 yield: φ =+= φ δφf (, µ µ ) δµ BA∫∫ΓΓ212 2 11 δφ≠≠ δφ φ' φ ∫∫ΓΓ B B 12 φBA'=+= φ δφf21(, µ µ2 ) δµ2 ∫∫ΓΓ22 For to be a state function, the differential form must be an exact differential: , i.e., must be integrable: The necessary and sufficient condition for this is the equality of cross-derivatives: ∂f ()µµ,..., ∂f ()µµ,..., in1 =jn1 ∀∈ij,{} 1,... n δφ= d φ ∂∂µµ 59 ji First Law of Thermodynamics
POSTULATES: 1. There exists a state function () t named total energy of the system, such that its E material time derivative is equal to the total power entering the system:
dd1 = + =ρρ2 +σ + −⋅ ()()()t: Pee t Q t ∫vdV ∫:d dV ∫∫ r dVq n dS dt E dt ≡∂2 VVt V VV Qt() Pte() e
2. There exists a function () t named the internal energy of the system, such that: U It is an extensive property, so it can be defined in terms of a specific internal energy (or internal energy per unit of mass) ut () x , : ()t:= ρ u dV U ∫ REMARK V d and d are exact differentials, The variation of the total energy of the system is: E K therefore, so is d = dd − . ddd UEK ()ttt=() + () Then, the internal energy is a dtE dt KU dt state function. 60 Global Form of the Internal Energy Balance
Introducing the expression for the total power into the first
postulate: = K dd1 ()t =ρρv2dV +σ :d dV + r dV −⋅q n dS dtE dt ∫2 ∫ ∫∫ VVt ≡∂V V V
Comparing this to the expression in the second postulate: ddd ()ttt=() + () dtE dt KU dt
The internal energy of the system must be: dd GLOBAL FORM =ρρ =σ + −⋅ ()t∫ u dV ∫:d dV ∫∫ r dVq n dS OF THE INTERNAL dtU dt ≡∂ VVt V V V ENERGY BALANCE Qt Ptσ () , e () stress power external thermal power 61 Local Spatial Form of the Internal Energy Balance
Applying Reynolds Lemma to the global form of the balance equation, and using the Divergence Theorem: d d du ()t =∫ρρu dV = ∫dV = ∫σ :d dV + ∫∫ρ r dV −⋅q n dS dtU dt ∆ ⊂ ≡ ∆ ⊂ ≡ dt ∆⊂ ∆⊂ ∂∆⊂ Vtt VV Vtt VV VV VV VV ()t ∫ ∇⋅q dV U ∂∆VV ⊂ du ⇒ ∫ρρdV = ∫σ :d dV+ ∫∫ r dV− ∇ ⋅q dV∀∆ V ⊂ V ∀ t ∆⊂VV dt ∆⊂VV ∆⊂VV ∆⊂VV Then, the local spatial form of the energy balance principle is obtained through localization ∆→ V dV (,) x t as: du LOCAL FORM OF THE ρρ=σ :d +() r −∇⋅ q ∀ x ∈ Vt, ∀ ENERGY BALANCE dt (Energy equation)
62 Second Law of Thermodynamics
The total energy is balanced in all thermodynamics processes following: ddd Pt()()+==+ Qt E KU eedt dt dt In an isolated system (no work can enter or exit the system) d dd Pt ()()+== Qt E 0 UK+=0 eedt dt dt
However, it is not established if the energy exchange can happen in both senses or not: dd dd UK><00 UK<00> dt dt dt dt
There is no restriction indicating if an imagined arbitrary process is physically possible or not.
63 Second Law of Thermodynamics
The concept of energy in the first law does not account for the observation that natural processes have a preferred direction of progress. For example:
If a brake is applied on a spinning wheel, the speed is reduced due to the conversion of kinetic energy into heat (internal energy). This process never occurs the other way round. dd UK><00 dt dt Spontaneously, heat always flows to regions of lower temperature, never to regions of higher temperature.
64 MMC - ETSECCPB - UPC 24/04/2017 Reversible and Irreversible Processes
A reversible process can be “reversed” by means of infinitesimal changes in some property of the system. It is possible to return from the final state to the initial state along the same path. A process that is not reversible is termed irreversible. REVERSIBLE PROCESS IRREVERSIBLE PROCESS
The second law of thermodynamics allows discriminating: IMPOSSIBLE thermodynamic processes REVERSIBLE POSSIBLE IRREVERSIBLE
65 Second Law of Thermodynamics
POSTULATES: 1. There exists a state function θ () x , t denoted absolute temperature, which is always positive.
2. There exists a state function S named entropy, such that: It is an extensive property, so it can be defined in terms of a specific entropy or entropy per unit of mass s : S( t )= ∫ ρ s(x , t ) dV V The following inequality holds true: nd dd r q Global form of the 2 S() t=ρρ s dV ≥ dV −⋅n dS Law of dt dt ∫∫θθ ∫ VV∂ V Thermodynamics = reversible process > irreversible process 66 Second Law of Thermodynamics
SECOND LAW OF THERMODYNAMICS IN CONTINUUM MECHANICS The rate of the total entropy of the system is equal o greater than the rate of heat per unit of temperature
nd dd r q Global form of the 2 S() t=ρρ s dV ≥ dV −⋅n dS Law of dt dt ∫∫θθ ∫ VV∂ V Thermodynamics
= reversible process = Γe ()t > irreversible process rate of the total amount of the entity heat, per unit =ρ −⋅ of time, (external thermal power) entering into the Qe () t∫∫ r dVqn dS VV∂ system
r q rate of the total amount of the entity heat per unit Γ=e ()tρ dV −⋅n dS of absolute temperature, ∫∫θθ per unit of time (external VV∂ heat/unit of temperature power) entering into the system
67 Second Law of Thermodynamics
Consider the decomposition of entropy into two (extensive) counterparts: Entropy generated inside the continuous medium:
St() = S()ie() t + S() () t dS dS()ie dS () = + dt dt dt
Entropy generated by interaction with the outside medium:
S ()ii= ∫ ρ s,() ()x t dV V S ()ee= ∫ ρ s,() ()x t dV V
68 Second Law of Thermodynamics
()e dS r q If one establishes, =Γ=ρ − ⋅ e ∫∫dVn dS dt VVθθ∂
Then the following must hold true: dS()ie dS() dS r q + =≥ρ dV −⋅n dS dt dt dt ∫∫θθ VV∂ ()e And thus, =dS dt dS()ie dS dS() dS r q = − = − ρ dV − ⋅n dS ≥0 ∀∆ V ⊂ V ∀ t ∫∫θθ dt dt dt dt ∆⊂VV ∂∆⊂VV
REPHRASED SECOND LAW OF THERMODYNAMICS : ()i The internally generated entropy of the system , St () , never decreases along time
69 Local Spatial Form of the Second Law of Thermodynamics
The previous eq. can be rewritten as:
dd ()i rq ρ s dV = ρρ s dV− dV − ⋅n dS ≥ 0 ∀∆ V ⊂ V ∀ t dt ∫dt ∫ ∫∫θθ ∆VVVtt ⊂tt ≡ ∆VVV ⊂ ≡ ∆⊂VV ∂∆⊂VV Applying the Reynolds Lemma and the Divergence Theorem:
ds()i ds r q ρdV= ρρ dV− dV −∇ ⋅dV ≥0 ∀∆ V ⊂ V ∀ t ∫ ∫ ∫∫θθ ∆⊂VV dt ∆⊂VV dt ∆⊂VV ∆⊂VV
Then, the local spatial form of the second law of thermodynamics is: nd ds()i ds r q Local (spatial) form of the 2 ρ= ρρ − −∇ ⋅ ≥0, ∀∈x Vt ∀ Law of Thermodynamics dt dt θθ (Clausius-Duhem inequality)
= reversible process > irreversible process
70 Local Spatial Form of the Second Law of Thermodynamics
q 11 Considering that, ∇∇⋅() = ⋅−qq ⋅ ∇θ REMARK θθ θ2 (Stronger postulate) Internally generated entropy can ()i The Clausius-Duhem inequality can be written as be generated locally, s , or by ()i local ()i = s = s thermal conduction, s , and ()i cond ds ds r 11 both must be non-negative. = −+∇∇ ⋅qq − ⋅θ ≥0 dt dt θ ρθ ρθ 2 = ()i ()i slocal = scond CLAUSIUS-PLANCK HEAT FLOW r 1 1 s −+∇ ⋅q ≥0 INEQUALITY −q ⋅≥∇θ 0 INEQUALITY θ ρθ ρθ 2
Because density and absolute temperature are always positive, it is deduced that q ⋅≤ ∇ θ 0 , which is the mathematical expression for the fact that heat flows by conduction from the hot parts of the medium to the cold ones. 71 Alternative Forms of the Clausius-Planck Inequality
Substituting the internal energy balance equation given by du not ρρ=ur =σ :dq + ρ −∇⋅ ∇⋅qd −ρρru =σ : − dt
into the Clausius-Planck inequality,
i ρθslocal :0= ρθ sr − ρ +∇⋅q ≥
yields, ρθsu+()σ :0d −≥ ρ −ρθ()us −+σ :0d ≥ Clausius-Planck Inequality in terms of the specific internal energy
72 5.11. Governing Equations
Ch.5. Balance Principles
74 Governing Equations in Spatial Form
Conservation of Mass. ρρ+ ∇⋅ = 1 eqn. v 0 Continuity Equation.
Linear Momentum Balance. ∇⋅σ +ρρbv = 3 eqns. First Cauchy’s Motion Equation.
T Angular Momentum Balance. σσ= 3 eqns. Symmetry of Cauchy Stress Tensor.
Energy Balance. ρρur =σ :dq + −∇⋅ 1 eqn. First Law of Thermodynamics.
−−+ρθ()usσ :d ≥0 Second Law of Thermodynamics. 1 Clausius-Planck Inequality. 2 restrictions −q ⋅≥∇θ 0 ρθ 2 Heat flow inequality 8 PDE + 2 restrictions
75 Governing Equations in Spatial Form
The fundamental governing equations involve the following variables: ρ density 1 variable
v velocity vector field 3 variables
σ Cauchy’s stress tensor field 9 variables u specific internal energy 1 variable
q 3 variables heat flux per unit of surface vector field θ absolute temperature 1 variable 19 scalar s specific entropy 1 variable unknowns At least 11 equations more (assuming they do not involve new unknowns), are needed to solve the problem, plus a suitable set of boundary and initial conditions.
76
Constitutive Equations in Spatial Form
σσ= ()v,,θ ζ Thermo-Mechanical Constitutive Equations. 6 eqns.
Entropy ss= ()v,,θ ζ Constitutive Equation. 1 eqn.
Thermal Constitutive Equation. q= qv(),θθ = −K ∇ Fourier’s Law of Conduction. 3 eqns.
uf= ()ρθ,,,v ζ Heat State Equations. (1+p) eqns. Fi (){}ρθ, ,ζ = 0 ip ∈ 1,2,..., Kinetic (19+p) PDE + set of new thermodynamic (19+p) unknowns variables:ζ = {} ζζ 12 , ,..., ζ p . REMARK 1 REMARK 2 The strain tensor is not considered an unknown as they These equations are can be obtained through the motion equations, i.e., εε = () v . specific to each material.
77 The Coupled Thermo-Mechanical Problem
Conservation of Mass. ρρ+ ∇⋅ = 1 eqn. v 0 Continuity Mass Equation.
16 scalar Linear Momentum Balance. 10 3 eqns. unknowns First Cauchy’s Motion Equation. equations
σ=σ( ε (v ),θ ) Mechanical constitutive equations. 6 eqns.
Energy Balance. 1 eqn. First Law of Thermodynamics.
Second Law of Thermodynamics. 2 restrictions. Clausius-Planck Inequality.
78 MMC - ETSECCPB - UPC The Uncoupled Thermo-Mechanical Problem
The mechanical and thermal problem can be uncoupled if
The temperature distribution θ () x , t is known a priori or does not intervene in the mechanical constitutive equations.
Then, the mechanical problem can be solved independently.
79 The Uncoupled Thermo-Mechanical Problem
Conservation of Mass. ρρ+ ∇⋅ = 1 eqn. v 0 Continuity Mass Equation.
10 scalar Linear Momentum Balance. Mechanical 3 eqns. unknowns First Cauchy’s Motion Equation. problem
σ=σ( ε (v ), θ ) Mechanical constitutive equations. 6 eqns.
Energy Balance. 1 eqn. First Law of Thermodynamics. Thermal problem Second Law of Thermodynamics. 2 restrictions. Clausius-Planck Inequality.
80 The Uncoupled Thermo-Mechanical Problem
Then, the variables involved in the mechanical problem are:
ρ density 1 variable
Mechanical v velocity vector field 3 variables variables σ Cauchy’s stress tensor field 6 variables u specific internal energy 1 variable
q heat flux per unit of surface vector field 3 variables Thermal variables θ absolute temperature 1 variable
s specific entropy 1 variable
81
Chapter 5 Balance Principles
5.1 Introduction Continuum Mechanics is based on a series of general postulates or principles that are assumed to always be valid, regardless of the type of material and the range of displacements or deformations. Among these are the so-called balance principles: • Conservation of mass • Balance of linear momentum • Balance of angular momentum • Balance of energy (or first law of thermodynamics) A restriction that cannot be rigorously understood as a balance principle must be added to these laws, which is introduced by the • Second law of thermodynamics Theory and Problems 5.2 Mass Transport or Convective Flux In continuumContinuum mechanics, the Mechanics term convection is for associated Engineers with mass transport in the medium, which derives© X. Oliver from the and motion C. Agelet of its particles. de Saracibar The continuous medium is composed of particles, some of whose properties are associated with the amount of mass: specific weight, angular momentum, kinetic energy, etc. Then, when particles move and transport their mass, a transport of the these properties occurs, named convective transport (see Figure 5.1). Consider A, an arbitrary (scalar, vector or tensor) property of the continuous medium, and Ψ (x,t), the description of the amount of said property per unit of mass of the continuous medium. Consider also S, a control surface, i.e., a surface fixed in space (see Figure 5.2). Due to the motion of the particles in the medium, these cross the surface along time and, in consequence, there exists a certain amount of the property A that, associated with the mass transport, crosses the control surface S per unit of time.
193 194 CHAPTER 5. BALANCE PRINCIPLES
Figure 5.1: Convective transport in the continuous medium.
Definition 5.1. The convective flux (or mass transport flux) of a generic property A through a control surface S is the amount of A that, due to mass transport, crosses the surface S per unit of time. A convective flux not= Φ = amount of crossing S of A through S S unit of time
Theory and Problems
Continuum Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar
Figure 5.2: Convective flux through a control surface.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Mass Transport or Convective Flux 195
Figure 5.3: Cylinder occupied by the particles that have crossed dS in the time inter- val [t, t + dt].
To obtain the mathematical expression of the convective flux of A through the surface S, consider a differential surface element dS and the velocity vector v of the particles that at time t are on dS (see Figure 5.3). In a time differential dt, these particles will have followed a pathline dx = vdt, such that at the instant of time t +dt they will occupy a new position in space. Taking now into account all the particles that have crossed dS in the time interval [t, t + dt], these will occupy a cylinder generated by translating the base dS along the directrix dx = vdt, and whose volume is given by dV = dS dh = v · n dt dS . (5.1) Since the volume (dV) of the particles crossing dS in the time interval [t, t + dt] is known, the mass crossing dS in this same time interval can be ob- tained by multiplying (5.1) by the density, dm = ρ dV = ρv · n dt dS . (5.2)
Finally, the amount of A crossing dS in the time interval [t, t + dt] is calculated by multiplying (5.2) by theTheory function Ψ and(amount Problems of A per unit of mass), Ψ dm = ρΨv · n dt dS . (5.3) Continuum Mechanics for Engineers Dividing (5.3)bydt yields© X. Oliverthe amount and of C. the Agelet property de that Saracibar crosses the differ- ential control surface dS per unit of time, Ψ dm d Φ = = ρΨv · n dS . (5.4) S dt Integrating (5.4) over the control surface S results in the amount of the property A crossing the whole surface S per unit of time, that is, the convective flux of the property A through S. convective flux Φ = ρΨv · n dS (5.5) of A through S S S
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 196 CHAPTER 5. BALANCE PRINCIPLES
Example 5.1 – Compute the magnitude Ψ and the convective flux ΦS corre- sponding to the following properties: a) volume, b) mass, c) linear momen- tum, d) kinetic energy.
Solution a) If the property A is the volume occupied by the particles, then Ψ is the volume per unit of mass, that is, the inverse of the density. Therefore, A ≡ Ψ = 1 Φ = · = . V and ρ lead to S v ndS volume flow rate S b) If the property A is the mass, then Ψ is the mass per unit of mass, that is, the unit. Therefore,
A ≡ M and Ψ = 1 lead to ΦS = ρ v · ndS . S c) If the property A is the linear momentum (= mass × velocity), then Ψ is the linear momentum per unit of mass, that is, the velocity. Therefore,
A ≡ mv and Ψ = v lead to ΦS = ρ v(v · n) dS . S (Note that in this case Ψ and the convective flux ΦS are vectors).
d) If the property A is the kinetic energy then Ψ is the kinetic energy per unit of mass. Therefore, 1 2 1 2 1 2 A ≡ m |v| andTheoryΨ = |v and| lead Problems to ΦS = ρ |v| (v · n) dS . 2 2 2 S Continuum Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar
Remark 5.1. In a closed control surface1, S = ∂V, the expression of the convective flux corresponds to the net outflow, defined as the outflow minus the inflow (see Figure 5.4), that is, A not= Φ = ρΨ · . net convective flux of ∂V v n dS ∂V
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Mass Transport or Convective Flux 197
Figure 5.4: Net outflow through a closed control surface.
Remark 5.2. The convective flux of any property through a material surface is always null. Indeed, the convective flux of any property is associated, by definition, with the mass transport (of particles) and, on the other hand, a material surface is always formed by the same particles and cannot be crossed by them. Consequently, there is no mass transport through a material surface and, therefore, there is no convective flux through it.
Remark 5.3. Some propertiesTheory can and be transported Problems within a continuous medium in a manner not necessarily associated with mass transport. This form of non-convective transport receives several names (con- duction,Continuum diffusion, etc.) Mechanics depending on the for physical Engineers problem being studied. A typical© example X. Oliver is heat and flux C. by conduction.Agelet de Saracibar The non-convective transport of a property is characterized by the non-convective flux vector (or tensor) q(x,t), which allows defining the (non-convective) flux through a surface S with unit normal vector n as non-convective flux = q · n dS . S
1 Unless stated otherwise, when dealing with closed surfaces, the positive direction of the unit normal vector n is taken in the outward direction of the surface.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 198 CHAPTER 5. BALANCE PRINCIPLES
5.3 Local and Material Derivatives of a Volume Integral Consider A, an arbitrary (scalar, vector or tensor) property of the continuous medium, and μ, the description of the amount of said property per unit of vol- 2 ume , amount of A μ (x,t)= . (5.6) unit of volume Consider an arbitrary volume V in space. At time t, the total amount Q(t) of the property contained in this volume is Q(t)= μ (x,t) dV . (5.7) V To compute the content of property A at a different time t + Δt, the following two situations arise: 1) A control volume V is considered and, therefore, it is fixed in space and crossed by the particles along time.
2) A material volume that at time t occupies the spatial volume Vt ≡ V is considered and, thus, the volume occupies different positions in space along time. Different values of the amount Q(t + Δt) are obtained for each case, and com- puting the difference between the amounts Q(t + Δt) and Q(t) when Δt → 0 yields Q(t + Δt) − Q(t) Q (t)= lim , (5.8) Δt→0 Δt resulting in two different definitions of the time derivative, which lead to the concepts of local derivative and material derivative of a volume integral. 5.3.1 Local DerivativeTheory and Problems
DefinitionContinuum 5.2. The local Mechanics derivative of the for volume Engineers integral, © X.Q Oliver(t)= μ and(x,t C.) dV Agelet, de Saracibar V is the time derivative of Q(t) when the volume V is a volume fixed in space (control volume), see Figure 5.5. The notation ∂ not= μ ( , ) local derivative ∂ x t dV t V will be used.
2 μ is related toΨ =(amount of A)/(unit of mass) through μ = ρΨ and has the same tensor order as the property A .
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Local and Material Derivatives of a Volume Integral 199
Figure 5.5: Local derivative of a volume integral.
The amount Q of the generic property A in the control volume V at times t and t + Δt is, respectively, Q(t)= μ (x,t) dV and Q(t + Δt)= μ (x,t + Δt) dV . (5.9) V V
Using (5.9) in addition to the concept of time derivative of Q(t) results in3 ∂ 1 Q (t)= μ (x,t) dV = lim Q(t + Δt) − Q(t) = ∂t Δt→0 Δt V ⎛ ⎞ 1 = lim ⎝ μ (x,t + Δt) dV − μ (x,t) dV⎠ = Δt→0 Δt V V μ ( , + Δ ) − μ ( , ) ∂μ( , ) = x t t x t = x t , limTheoryΔ and ProblemsdV ∂ dV Δt→0 t t V V ∂μ(x,t) local Continuum Mechanics for Engineersderivative © X. Oliver∂t and C. Agelet de Saracibarof μ (5.10) which yields the mathematical expression of the local derivative of a volume integral.
Local derivative of a volume integral ∂ ∂μ(x,t) (5.11) μ (x,t) dV = dV ∂t ∂t V V
3 Note that the integration domain does not vary when the volume V is considered as a control volume and, therefore, is fixed in space.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 200 CHAPTER 5. BALANCE PRINCIPLES
5.3.2 Material Derivative
Definition 5.3. The material derivative of the volume integral, Q(t)= μ (x,t) dV , V is the time derivative of Q(t) when the volume Vt is a material vol- ume (mobile in space), see Figure 5.6. The notation d material derivative not= μ (x,t) dV dt Vt will be used.
The content Q of the generic property A in the material volume Vt at times t and t+Δt is, respectively, Q(t)= μ (x,t) dV and Q(t + Δt)= μ (x,t + Δt) dV . (5.12)
Vt Vt+Δt
Then, the material derivative is mathematically expressed as4 d Q(t + Δt) − Q(t) Q (t)= μ (x,t) dV = lim = Δt→0 Δ dt ≡ t Vt ⎛ Vt V ⎞ (5.13) 1 = lim ⎝ μ (x,t + Δt) dV − μ (x,t) dV⎠ . Δt→0 Δt VTheoryt+Δt and ProblemsVt The following step consists in introducing two variable substitutions, each suitableContinuum for one of the two Mechanicsintegrals in (5.13), for which Engineers lead to the same integra- tion domain in both expressions.© X. Oliver These and variable C. Agelet substitutions de Saracibar are given by the equation of motion x = ϕ (X,t), particularized for times t and t + Δt, ⎧ ⎪ = ϕ ( , ) → ( ) = | ( , )| ( ) , ⎪ xt X t dx1 dx2 dx3 t F X t dX1 dX 2 dX3 ⎨⎪ dVt dV0 ⎪ = ϕ ( , + Δ ) → ( ) = | ( , + Δ )| ( ) , ⎪ xt+Δt X t t dx1 dx2 dx3 t+Δt F X t t dX1 dX2 dX3 ⎩⎪ dVt+Δt dV0 (5.14)
4 Note that the integration domains are now different at times t and t + Δt.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Local and Material Derivatives of a Volume Integral 201
Figure 5.6: Material derivative of a volume integral.
where the identity dVt = |F(X,t)| dV0 has been taken into account. The variable substitutions in (5.14) are introduced in (5.13), resulting in μ¯ ( , + Δ ) X t t d 1 μ (x,t) dV = lim μ (x(X,t + Δt),t + Δt) |F(X,t + Δt)| dV0 dt Δt→0 Δt Vt V0 − μ ( ( , ), ) | ( , )| = x X t t F X t dV0 V0 μ¯ (X,t) μ¯ (X,t + Δt) |F(X,t + Δt)| − μ¯ (X,t) |F(X,t)| = lim dV0 = Δt→0 Δt V0 ∂ d μ¯ (X,t) |F(X,t)| = μ (x,t) |F(x,t)| ∂t dt d = μ |F| dVTheory0 . and Problems dt V0 (5.15) Finally,Continuum expanding the last Mechanics integral in (5.15) for5 and Engineers considering the equality d |F|/dt = |F| ∇ · v yields© X. Oliver and C. Agelet de Saracibar d d dμ d |F| μ (x,t) dV = μ |F| dV0 = |F| + μ dV0 = dt dt dt dt Vt V0 V0 |F| ∇ · v dμ dμ = + μ∇ · v |F| dV = + μ∇ · v dV , dt 0 dt V V 0 dVt t (5.16)
5 The change of variable xt = ϕ (X,t) is undone here.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 202 CHAPTER 5. BALANCE PRINCIPLES that is6, d not d dμ μ (x,t) dV = μ (x,t) dV = + μ∇ · v dV . (5.17) dt dt dt V V ≡V V t Vt ≡V t
Recalling the expression of the material derivative of a property (1.15) results in ∂μ d μ ( , ) = + · ∇μ + μ∇ · = x t dV ∂ v v dV dt t Vt ≡V V ∇ · (μv) (5.18) ∂μ ∂ = dV + ∇ · (μv) dV = μ dV + ∇ · (μv) dV , ∂t ∂t V V V V where the expression of the local derivative (5.11) has been taken into account. Then, (5.18) produces the expression of the material derivative of a volume in- tegral.
Material derivative of a volume integral d ∂ μ (x,t) dV = μ dV + ∇ · (μv) dV dt ∂t (5.19) ≡ Vt V V V material local convective derivative derivative derivative
Remark 5.4. The formTheory of the material and derivative, Problems given as a sum of a local derivative and a convective derivative, that appears when differ- entiating properties of the continuous medium (see Chapter 1, Sec- tionContinuum1.4) also appears here Mechanics when differentiating for Engineersintegrals in the con- tinuous medium. Again,© X. Oliverthe convective and C. derivative Ageletis de associated Saracibar with the existence of a velocity (or motion) in the medium and, thus, with the possibility of mass transport.
6 The expression d μ (x,t) dV dt Vt ≡V denotes the time derivative of the integral over the material volume Vt (material derivative of the volume integral) particularized at time t, when the material volume occupies the spatial volume V.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Conservation of Mass. Mass continuity Equation 203
Figure 5.7: Principle of conservation of mass in a continuous medium.
5.4 Conservation of Mass. Mass continuity Equation
Definition 5.4. Principle of conservation of mass. The mass of a continuous medium (and, therefore, the mass of any material vol- ume belonging to this medium) is always the same.
Consider a material volume Vt that at times t and t + Δt occupies the volumes in space Vt and Vt+Δt, respectively (see Figure 5.7). Consider also the spatial description of the density, ρ (x,t). The mass enclosed by the material volume V at times t and t + Δt is, respectively, M(t)= ρ (x,t) dVTheoryand M( andt + Δt)= Problemsρ (x,t + Δt) dV . (5.20)
Vt Vt+Δt Continuum Mechanics forM Engineers( )=M( + Δ ) By virtue of the principle© of X. conservation Oliver and of C. mass, Agelett de Saracibart t must be satisfied.
5.4.1 Spatial Form of the Principle of Conservation of Mass. Mass Continuity Equation The mathematical expression of the principle of conservation of mass of the material volume M(t) is that the material derivative of the integral (5.20)is null, d M (t)= ρ dV = 0 ∀t . (5.21) dt Vt
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 204 CHAPTER 5. BALANCE PRINCIPLES
By means of the expression of the material derivative of a volume integral (5.17), the integral (or global) spatial form of the principle of conservation of mass results in
Global spatial form of the principle of conservation of mass d dρ , (5.22) ρ dV = + ρ ∇ · v dV = 0 ∀ΔV ⊂ V , ∀t dt dt t t Vt Vt (ΔVt ) (ΔVt ) which must be satisfied for Vt and, also, for any partial material volume ΔVt ⊂ Vt that could be considered. In particular, it must be satisfied for each of the ele- mental material volumes associated with the different particles in the continuous medium that occupy the differential volumes dVt. Applying (5.22) on each dif- 7 ferential volume dVt ≡ dV (x,t) yields dρ dρ (x,t) + ρ∇ · v dV = + ρ (x,t)∇ · v(x,t) dV (x,t)=0 dt dt dV(x,t) ∀x ∈ Vt, ∀t dρ =⇒ + ρ∇ · v = 0 dV ∀x ∈ V , ∀t dt t (5.23)
Local spatial form of the principle of conservation of mass (mass continuity equation) (5.24) dρ + ρ∇ · v = 0 dV ∀x ∈ V , ∀t dt t Theory and Problems which constitutes the so-called mass continuity equation. Replacing the expres- sion of the material derivative of the spatial description of a property (1.15)in (5.24) resultsContinuum in Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar ∂ρ ∂ρ + v · ∇ρ + ρ∇ · v = 0 =⇒ + ∇ · (ρv)=0 , (5.25) ∂t ∂t ∇ · (ρv) which yields an alternative expression of the mass continuity equation.
7 This procedure, which allows reducing a global (or integral) expression such as (5.22)to a local (or differential) one such as (5.24), is named in continuum mechanics localization process.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Conservation of Mass. Mass continuity Equation 205
⎫ ⎪ ∂ρ ⎪ + ∇ · (ρv)=0 ⎪ ∂t ⎪ ⎬⎪ ∂ρ ∂ (ρvi) ∀ ∈ , ∀ + = 0 i ∈{1,2,3} ⎪ x Vt t (5.26) ∂t ∂x ⎪ i ⎪ ⎪ ∂ρ ∂ (ρv ) ∂ (ρvy) ∂ (ρv ) ⎪ + x + + z = 0 ⎭ ∂t ∂x ∂y ∂z
5.4.2 Material Form of the Principle of Conservation of Mass From (5.22)8, dρ dρ 1 d |F| + ρ∇ · v dV = + ρ dV = dt dt |F| dt Vt Vt 1 dρ d |F| 1 d = |F| + ρ dV = ρ |F| dV = |F| dt dt |F| dt Vt Vt | | F dV0 d ρ |F| dt ∂ = ρ (X,t)|F(X,t)| dV ∀ΔV ⊂ V , ∀t , ∂t 0 0 0 V0 (5.27) where the integration domain is now the volume in the reference configura- tion, V0. Given that (5.27) must be satisfied for each and every part ΔV0 of V0,a localization process can be applied, which results in9 ∂ Theory and Problems ρ (X,t)|F(X,t)| = 0 ∀X ∈ V , ∀t ∂t 0 Continuum=⇒ ρ (X,t)|F(X, Mechanicst)| = ρ (X)|F(X)| for∀t Engineers © X. Oliver and C. Agelet de Saracibar =⇒ ρ ( , )| |( , ) = ρ ( , )| |( , ) =⇒ ρ | | = ρ | | . X 0 F X 0 X t F X t 0 F 0 t F t = 1 not= ρ | | not= ρ | | 0 F 0 t F t (5.28) Local material form of the mass conservation principle ρ ( )=ρ ( )| | ( ) ∀ ∈ , ∀ (5.29) 0 X t X F t X X V0 t
8 Here, the expression deduced in Chapter 2, d |F|/dt = |F| · ∇ · v , is considered. 9 ( , )= =⇒ | | = The equality F X 0 1 F 0 1 is used here.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 206 CHAPTER 5. BALANCE PRINCIPLES
5.5 Balance Equation. Reynolds Transport Theorem Consider A, an arbitrary (scalar, vector or tensor) property of the continuous medium, and Ψ (x,t), the description of the amount of said property per unit of mass. Then, ρΨ (x,t) is the amount of this property per unit of volume.
5.5.1 Reynolds’ Lemma Consider an arbitrary material volume of the continuous medium that at time t occupies the volume in space Vt ≡ V. The amount of the generic property A in the material volume Vt at time t is Q(t)= ρΨ dV . (5.30)
Vt ≡V The variation along time of the content of property A in the material volume Vt is given by the time derivative of Q(t), which using expression (5.17)ofthe material derivative of a volume integral (with μ = ρΨ ) results in d d (ρΨ) Q (t)= ρΨ dV = + ρΨ ∇ · v dV . (5.31) dt dt Vt ≡V μ V
Considering the expression of the material derivative of a product of functions, grouping terms and introducing the mass continuity equation (5.24) yields d dΨ dρ ρΨdV = ρ +Ψ + ρΨ ∇ · v dV = dt dt dt Vt ≡V V dΨ dρ (5.32) = ρ +Ψ + ρ∇ · v dV =⇒ dt dt V Theory and Problems =0 (mass continuity eqn.)
ContinuumReynolds’ Mechanics Lemma for Engineers ©d X. Oliver and C. AgeletdΨ de. Saracibar ρΨ dV = ρ dV (5.33) dt dt Vt ≡V V
5.5.2 Reynolds’ Theorem Consider the arbitrary volume V, fixed in space, shown in Figure 5.8. The amount of property A in this control volume is Q(t)= ρΨ dV . (5.34) V
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Balance Equation. Reynolds Transport Theorem 207
Figure 5.8: Reynolds Transport Theorem.
The variation of the amount of property A in the material volume Vt, which in- stantaneously coincides at time t with the control volume V (Vt ≡ V),isgivenby expression (5.19) of the material derivative of a volume integral (with μ = ρΨ) and by (5.11), d ∂ (ρΨ) ρΨ dV = dV + ∇ · (ρΨ v) dV . (5.35) dt ∂t Vt ≡V V V
Introducing the Reynolds’ Lemma (5.33) and the Divergence Theorem10 in (5.35) results in