Ch.1. Description of Motion
CH.1. DESCRIPTION OF MOTION
Multimedia Course on Continuum Mechanics Overview
1.1. Definition of the Continuous Medium 1.1.1. Concept of Continuum Lecture 1 1.1.2. Continuous Medium or Continuum 1.2. Equations of Motion 1.2.1 Configurations of the Continuous Medium 1.2.2. Material and Spatial Coordinates Lecture 2 1.2.3. Equation of Motion and Inverse Equation of Motion 1.2.4. Mathematical Restrictions 1.2.5. Example Lecture 3 1.3. Descriptions of Motion 1.3.1. Material or Lagrangian Description Lecture 4 1.3.2. Spatial or Eulerian Description 1.3.3. Example Lecture 5
2 Overview (cont’d)
1.4. Time Derivatives Lecture 6 1.4.1. Material and Local Derivatives 1.4.2. Convective Rate of Change Lecture 7 1.4.3. Example Lecture 8
1.5. Velocity and Acceleration 1.5.1. Velocity Lecture 9 1.5.2. Acceleration 1.5.3. Example
1.6. Stationarity and Uniformity 1.6.1. Stationary Properties Lecture 10 1.6.2. Uniform Properties
3 Overview (cont’d)
1.7. Trajectory or Pathline 1.7.1. Equation of the Trajectories 1.7.2. Example 1.8. Streamlines Lecture 11 1.8.1. Equation of the Streamlines 1.8.2. Trajectories and Streamlines 1.8.3. Example 1.8.4. Streamtubes
1.9. Control and Material Surfaces 1.9.1. Control Surface 1.9.2. Material Surface Lecture 12 1.9.3. Control Volume 1.9.4. Material Volume
4 1.1 Definition of the Continuous Medium Ch.1. Description of Motion
5 The Concept of Continuum
Microscopic scale: Matter is made of atoms which may be grouped in molecules. Matter has gaps and spaces.
Macroscopic scale: Atomic and molecular discontinuities are disregarded. Matter is assumed to be continuous.
6 Continuous Medium or Continuum
Matter is studied at a macroscopic scale: it completely fills the space, there exist no gaps or empty spaces.
Assumption that the medium and is made of infinite particles (of infinitesimal size) whose properties are describable by continuous functions with continuous derivatives.
7 Exceptions to the Continuous Medium
Exceptions will exist where the theory will not account for all the observed properties of matter. E.g.: fatigue cracks. In occasions, continuum theory can be used in combination with empirical information or information derived from a physical theory based on the molecular nature of material.
The existence of areas in which the theory is not applicable does not destroy its usefulness in other areas.
8 Continuum Mechanics
Study of the mechanical behavior of a continuous medium when subjected to forces or displacements, and the subsequent effects of this medium on its environment.
It divides into: General Principles: assumptions and consequences applicable to all continuous media. Constitutive Equations: define the mechanical behavior of a particular idealized material.
9 1.2 Equations of Motion
Ch.1. Description of Motion
10 Material and Spatial points, Configuration
A continuous medium is formed by an infinite number of particles which occupy different positions in space during their movement over time.
MATERIAL POINTS: particles
SPATIAL POINTS: fixed spots in space
The CONFIGURATION Ωt of a continuous medium at a given time (t) is the locus of the positions occupied by the material points of the continuous medium at the given time.
11 Configurations of the Continuous Medium
Ω0: non-deformed (or reference) Ω or Ωt: deformed (or present) configuration, at reference time t0. configuration, at present time t. Γ0 : non-deformed boundary. Γ or Γt : deformed boundary. X : Position vector of a particle at reference time. x : Position vector of the same particle at present time. ϕ ()X,t Γ t0 = 0 → reference time tT∈→[]0, current time Γ0
Initial, reference Ω or undeformed configuration X Ω0 x Present or deformed configuration
12 Material and Spatial Coordinates
The position vector of a given particle can be expressed in: Non-deformed or Reference Configuration XX 1 X =XY = ≡ material coordinates (capital letter) [] 2 XZ3
Deformed or Present Configuration xx 1 []x =xy2 = ≡ spatial coordinates (small letter) xz3
13 Equations of Motion
The motion of a given particle is described by the evolution of its spatial coordinates (or its position vector) over time. xx= ϕ (particle label,,tt)(= particle label ) xii= ϕ (particle label, ti){}∈ 1, 2, 3
φ (particle label, t) is the motion that takes the body from a reference configuration to the current one.
The Canonical Form of the Equations of Motion is obtained when the “particle label” is taken as its material coordinates not x=ϕ ()() X,,tt = xX T particle label ≡≡{XXX123} X xii= ϕ (){} XX123, , Xt , i∈ 1, 2, 3
14 Inverse Equations of Motion
The inverse equations of motion give the material coordinates as a function of the spatial ones.
ϕ (X,t) Γ
Γ0
Ω
−1 X ϕ (x,t) Ω0 x
not − X=ϕ 1 ( x,,tt) = Xx( ) −1 Xii= ϕ ( xxxt123, , ,) i∈{ 1, 2, 3}
15 Mathematical restrictions for φ and φ-1 defining a “physical” motion
Consistency condition ϕ ( XX ,0 ) = , as X is the position vector for t=0 Continuity condition 1 ϕ ∈ C , φ is continuous with continuous derivatives Biunivocity condition φ is biunivocal to guarantee that two particles do not occupy simultaneously the same spot in space and that a particle does not occupy simultaneously more than one spot in space. Mathematically: the “Jacobian” of the motion’s equations should be different from zero: ∂ϕ (X,t) ∂ϕ J = =deti ≠ 0 ∂∂ XXj The “Jacobian” of the equations of motion should be “strictly positive” ∂ϕ (X,t) ∂ϕ J = =deti > 0 density is always positive ∂∂ XXj (to be proven)
16 Example
The spatial description of the motion of a continuous medium is given by:
22tt x11= X e x= Xe −− xX( ,t) ≡ x = X e 22tt ≡=y Ye 22 =+=+22tt x355 X 13 t X e z Xt Ze
Find the inverse equations of motion.
17 2t x11= Xe −2t xX( ,t) ≡= x22 Xe Example - Solution 2t x3=5 Xt 13 + Xe
Check the mathematical restrictions: ϕ = Consistency Condition ( XX ,0 ) ? 20⋅ Xe11 X −⋅20 xX( ,0t=) = Xe22 = X = X ⋅+ 20⋅ 50X13 Xe X 3 1 Continuity Condition ϕ ∈ C ? Biunivocity Condition ?
∂∂∂xxx111 ∂∂∂XXX 123e2t 00 ∂x ∂∂∂xxx J=i =222=00e−−2t =⋅ ee 2 t 22 tt ⋅=≠ e e 2 t0 ∀ t ∂Xj ∂∂∂ XXX123 2t 50te ∂∂∂xxx333
∂∂∂XXX123 ∂ϕ (X,t) Density positive ? J = > 0 2t ∂X Je= > 0
18 2t x11= Xe −2t xX( ,t) ≡= x22 Xe Example - Solution 2t x3=5 Xt 13 + Xe
Calculate the inverse equations: x x= Xe22tt ⇒== X1 xe− 11 1e2t 1 x =−22tt ⇒==2 x22 Xe X 2−2t xe 2 e x− 5 Xt =+2t ⇒=31 =−−−22tt =− − 2 t − 4 t x35 Xt 13 X e X3 2t ( x355( xe 1) t) e xe3 txe 1 e
−2t X11= xe −12 t Xx≡==ϕ ( ,t) X22 xe −−24tt X33= x e − 5 tx 1 e
19 1.3 Descriptions of Motion
Ch.1. Description of Motion
20 Descriptions of Motion
The mathematical description of the particle properties can be done in two ways:
Material (Lagrangian) Description
Spatial (Eulerian) Description
21 Material or Lagrangian Description
The physical properties are described in terms of the material coordinates and time.
It focuses on what is occurring at a fixed material point (a particle, labeled by its material coordinates) as time progresses.
Normally used in solid mechanics.
22 Spatial or Eulerian Description
The physical properties are described in terms of the spatial coordinates and time.
It focuses on what is occurring at a fixed point in space (a spatial point labeled by its spatial coordinates) as time progresses.
Normally used in fluid mechanics.
23 Example
The equation of motion of a continuous medium is: x= X − Yt x= xX( ,t) ≡=+ y Xt Y z=−+ Xt Z
Find the spatial description of the property whose material description is:
XYZ++ ρ ( X,Y,Z,t ) = 1+ t 2
24 x= X − Yt x= xX( ,t) ≡=+ y Xt Y Example - Solution z=−+ Xt Z
Check the mathematical restrictions: Consistency Condition φ ( X , 0 ) = X ? XY−⋅0 X xX( ,0t=) = XY ⋅+ 0 = Y =X XZ⋅+0 Z 1 Continuity Condition φ ∈ C ? Biunivocity Condition ? ∂∂∂xxx ∂∂∂ XYZ10−t ∂x ∂∂∂yyy J=i = =t 1 0 = 111 ⋅⋅−⋅− 1( tt) ⋅ = 1 + t2 ≠ 0 ∀ t ∂X ∂∂∂ XYZ j −t 01 ∂∂∂zzz ∂∂∂XYZ ∂φ(X,t) Any diff. Vol. must be positive J = > 0 ? ∂X
Jt=+>102
25 x= X − Yt x= xX( ,t) ≡=+ y Xt Y Example - Solution z=−+ Xt Z
Calculate the inverse equations: x=−⇒ X Yt X =+ x Yt y−− Y y xt ⇒ + = ⇒2 +=− ⇒ = yY− x Yt Yt Y y xt Y 2 y=+⇒= Xt Y X tt1+ t y− xt x + xt22 +− yt xt x + yt X=+=+ x Yt x t = = 1+t2 11 ++ tt 22
22 x+ yt z + zt ++ xt yt z=−+ Xt Z ⇒ Z =+=+ z Xt z t = 11++tt22
x+ yt X = + 2 1 t y− xt ≡==ϕ −1 Xx( ,tY) 2 1+ t z+ zt22 ++ xt yt Z = 1+ t 2
26 Example - Solution
Calculate the property in its spatial description:
x+ yt X = + 2 1 t y− xt ≡==ϕ −1 Xx( ,tY) 2 1+ t z+ zt22 ++ xt yt Z = 1+ t 2
x+ yt y − xt z + zt22 ++ xt yt ++ XYZ+ + 11++tt22 1 + t 2 x++ y yt + yt22 ++ z zt ρ = = = ( X,Y,Z,t ) 22 2 11++tt (1+ t 2 )
22 XYZ++ xy+(11 ++ tt) + z( + t) ρρ=⇒= ( X,Y,Z,t) 2 2 ( x, y,z,t) 1+ t (1+ t 2 )
27 1.4 Time Derivatives
Ch.1. Description of Motion
28 Material and Local Derivatives
The time derivative of a given property can be defined based on the: Material Description Γ(X,t) TOTAL or MATERIAL DERIVATIVE Variation of the property w.r.t. time following a specific particle in the continuous medium. ∂Γ()X,t partial time derivative of the material derivative ≡→ ∂t material description of the propery
Spatial Description γ(x,t) LOCAL or SPATIAL DERIVATIVE Variation of the property w.r.t. time in a fixed spot of space.
∂γ ()x,t partial time derivative of the local derivative ≡→ ∂t spatial description of the propery
29 Convective Derivative
Remember: x=x(X,t), therefore, γ(x,t)=γ(x(X,t),t)=Γ(X,t) The material derivative can be computed in terms of spatial descriptions: not dDnot ∂Γ(X ,) t material derivative →=γγ()xx,,tt =() = = dt Dt ∂t d ∂∂γγ()xx,,tt∂γγ∂x () ∂∂x =γ ()xX(),,tt = + ⋅=i + ⋅ = dt ∂t ∂∂ x t ∂ t ∂x ∂t i ∂x ∇γ (x ,)t vx( ,)t ∇γ i ∂t i vx(,)tt⋅∇γ (,) x Generalising for any property: REMARK dtχχ()xx,,∂ () t The spatial Nabla operator = +vx()(),,tt ⋅∇χ x ∂ dt∂ t is defined as: ∇≡ eˆi ∂xi material local convective rate of derivative derivative change 30 (convective derivative) Convective Derivative
Convective rate of change or convective derivative is implicitly defined as: v ⋅∇( •)
The term convection is generally applied to motion related phenomena. If there is no convection (v=0) there is no convective rate of change and the material and local derivatives coincide. d (•) ∂•( ) v ⋅∇( •) =0 = dt∂ t
31 Example
Given the following equation of motion: x = X + Yt + Zt x(X,t) ≡ y = Y + 2Zt z = Z + 3Xt And the spatial description of a property ρ ( x , t ) = 3 x + 2 y + 3 t , Calculate its material derivative.
Option #1: Computing the material derivative from material descriptions Option #2: Computing the material derivative from spatial descriptions
32 x = X + Yt + Zt x(X,t) ≡ y = Y + 2Zt Example - Solution z = Z + 3Xt ρ(x,t) = 3x + 2y + 3t
Option #1: Computing the material derivative from material descriptions Obtain ρ as a function of X by replacing the Eqns. of motion into ρ(x,t) : ρρ(x,t) =( xX ( , t ), t) = ρ( X , t) = 3( X ++ Yt Zt) +2( Y + 2 Zt) + 3 t =3X +++ 3 Yt 27 Y Zt + 3 t Calculate its material derivative as the partial derivative of the material description:
dtρ∂(xX,,) ρ ( t) ∂ = =(3XYtYZtt +++ 3 27 +=++ 3) 373 YZ dt ∂∂t t x= xX( ,t)
dtρ∂(xX,,) ρ ( t) = =++33YZ 7 dt ∂t x= xX( ,t)
33 x = X + Yt + Zt x(X,t) ≡ y = Y + 2Zt Example - Solution z = Z + 3Xt ρ(x,t) = 3x + 2y + 3t
Option #2: Computing the material derivative from spatial descriptions dtρρ(xx,,) ∂ ( t) = +vx( ,,tt) ⋅∇ρ ( x ) dt∂ t Applying this on ρ(x,t) : ∂ρ(x,t) ∂ =(323x ++= yt) 3 ∂∂tt
T YZ+ ∂∂x ∂ ∂ T vx( ,t) = =( X ++ Yt Zt),( Y + 2 Zt) ,( Z + 3 Xt) =[ Y + Z,2 Z , 3 X] = 2 Z x= xX( ,t) ∂∂tt ∂ t ∂ t 3X T T ∂ρ(xx,,tt) ∂ρ( ) ∂ρ( x , t) ∂∂ ∂ ∇ρ=(x,,,t) =(323,x ++ yt) ( 323, x ++ yt) ( 323 x ++ yt) = ∂∂xy ∂ z ∂ x ∂ y ∂ z 3 T =[3, 2, 0] = 2 0 34 x = X + Yt + Zt x(X,t) ≡ y = Y + 2Zt Example - Solution z = Z + 3Xt ρ(x,t) = 3x + 2y + 3t
Option #2 The material derivative is obtained:
3 dtρ(x, ) =++3[YZ ,2,3]2 ZX=++ 33 Y 3 Z + 4 Z dt x= xX,t T ( ) 0 v ρ v⋅()ρ
dtρ(x, ) =++33YZ 7 dt x= xX( ,t)
35 1.5 Velocity and Acceleration
Ch.1. Description of Motion
36 Velocity
Time derivative of the equations of motion. Material description of the velocity: REMARK Time derivative of the equations of motion Remember the ∂xX(),t equations of motion VX(),t = are of the form: ∂t not x=ϕ ()() X,,tt = xX ∂xti ()X, Vt()X, = i ∈1, 2, 3 i ∂t
Spatial description of the velocity: Velocity is expressed in terms of x using the inverse equations of motion: VXx()(),,tt vx() , t
37 Acceleration
Material time derivative of the velocity field. Material description of acceleration: Derivative of the material description of velocity: ∂VX(),t AX(),t = ∂t ∂Vti ()X, At()X, = i ∈1, 2, 3 i ∂t Spatial description of acceleration: A(X,t) is expressed in terms of x using the inverse equations of motion: AXx()(),,tt ax(),t Or a(x,t) is obtained directly through the material derivative of v(x,t): dtvx(),,∂ vx() t ax(),t= = +vx()(),,tt ⋅∇ vx dt∂ t dtv,()xx∂ v,() t ∂v a()x, t=ii = +⋅v()xx ,ti () , ti ∈ 1, 2, 3 ik dt∂∂ t xk 38 Example
Consider a solid that rotates at a constant angular velocity ω and has the following equation of motion:
xR= sin()ω t +φ x (Rt ,φ→ ,) label of yR= cos()ω t +φ particle → (non - canonical equations of motion)
Find the velocity and acceleration of the movement described in both, material and spatial forms.
39 x = R sin(ωt + φ) Example - Solution y = R cos(ωt + φ)
Using the expressions sin(ab±=) sin a ⋅ cos b ± cos a ⋅ sin b cos(ab±=) cos a ⋅ cos b sin a ⋅ sin b The equation of motion can be rewritten as: xRtRt= sin ( ω +φ) = sin( ω) cos φ+ R cos( ω t) sin φ yRtRt= cos( ω +φ) = cos( ω) cos φ− Rt sin( ω) sin φ For t=0, the equation of motion becomes: XR= sin φ YR= cos φ Therefore, the equation of motion in terms of the material coordinates is: = Y = X xRtRt= sin ( ω +φ) = sin( ω) cos φ+ R cos( ω t) sin φ= XtYt cos( ω) + sin ( ω ) yRtRt= cos( ω +φ) = cos( ω) cos φ− Rt sin( ω) sin φ=− XtYt sin( ω) + cos( ω ) = Y = X
40 x= Xcos( ω+ tY) sin( ω t) Example - Solution y=− Xsin( ω+ tY) cos( ω t)
The inverse equation of motion is easily obtained xY−ωsin ( t) xX=cos( ω+ t) Y sin ( ω t) X = cos(ωt) xY−sin ( ω t) −+ yYcos( ω t) = −+yYcos( ω t) cos(ωωtt) sin ( ) y=− Xsin( ω+ tY) cos( ω t) X = sin (ωt)
xsin(ω− tY) sin22( ω=− t) y cos( ω+ tY) cos ( ω t)
xsin(ω+ ty) cos( ω= tY) ( cos22( ω+ t) sin ( ω t)) =1
xx−( sin( ω+ ty) cos( ω t)) sin ( ω t) x xsin2 (ω ty) cos( ωω t) sin ( t) X = =−− = cos(ωt) cos(ωωtt) cos( ) cos( ω t) 1−ω sin2 ( t) =x −ω ytsin ( ) cos(ωt) =cos( ωt) 41 Example - Solution
So, the equation of motion and its inverse in terms of the material coordinates are:
xX=cos( ω+ t) Y sin ( ω t) xX( ,t) →→ canonical equations of motion y=− Xsin( ω+ tY) cos( ω t)
Xx=cos( ω− t) y sin ( ω t) Xx( ,t) →→ inverse equations of motion Yx=sin( ω+ t) y cos( ω t)
42 xX=cos( ω+ t) Y sin ( ω t) xX( ,t) → Example - Solution y=− Xsin( ω+ tY) cos( ω t)
∂xX( ,t) Velocity in material description is obtained from VX( ,t) = ∂t
∂∂x =( Xcos( ω+ tY) sin ( ω t)) ∂xX( ,t) ∂∂tt VX( ,t) = = ∂t ∂∂y =( −Xsin( ω+ tY) cos( ω t)) ∂∂tt
Vx −X ω sin( ω+ tY) ω cos( ω t) VX( ,t) = = Vy −X ω cos( ω− tY) ω sin ( ω t)
43 Xx=cos( ω− t) y sin ( ω t) Yx=sin( ω+ t) y cos( ω t) xX=cos( ω+ t) Y sin ( ω t) Example - Solution y=− Xsin( ω+ tY) cos( ω t)
Velocity in spatial description is obtained introducing X(x,t) into V(X,t): y = ω+ ω xXcos( t) Y sin ( t) v x −Xsin( ω+ tY) cos( ω t) ωωy → vx( ,t) = VXx( ( ,, tt) ) = = = v −ω y=− Xsin( ω+ tY) cos( ω t) y −Xcos( ω− tY) sin ( ω t) ω x −x Alternative procedure (longer): 22 −ωxcos( ω t) sin( ω ty) +ω sin( ω t) +ω x sin( ω t) cos( ω ty) +ω cos ( ω t) vx,t = = ( ) 22 −ωxcos( ω+ω ty) sin( ω t) cos( ω−ω tx) sin( ω−ω ty) cos( ω t) sin ( ω t) ωx(sin(ω t) cos( ω− t) cos( ω t) sin( ω ty)) +ω( sin22( ω+ t) cos ( ω t)) =0 =1 = −ωxt(sin22( ω+) cos ( ω t)) +ωyt(sin( ω) cos( ω t) − cos( ω tt) sin ( ω )) =1 =0
vx ω y vx( ,t) = = v y −ω x 44 −X ω sin( ω+ tY) ω cos( ω t) VX( ,t) = Example - Solution −X ω cos( ω− tY) ω sin ( ω t)
∂VX( ,t) Acceleration in material description is obtained applying: AX( ,t) = ∂t
∂V x =−ωX 22 cos( ω− tY) ω sin ( ω t) ∂VX( ,t) ∂t AX( ,t) = = ∂t ∂V y =X ω22 sin ( ω− tY) ω cos( ω t) ∂t
Ax Xcos(ω+ tY) sin ( ω t) AX( ,t) = = −ω2 Ay −Xsin( ω+ tY) cos( ω t)
45 Xx=cos( ω− t) y sin ( ω t) Example - Solution Yx=sin( ω+ t) y cos( ω t)
(OPTION #1) Acceleration in spatial description is obtained by replacing the inverse equation of motion into A(X,t): ax ( ,t) = AXx( ( ,, tt) ) =
(xcos(ω− ty) sin( ω t)) cos( ω+ t) ( x sin( ω+ ty) cos( ω t)) sin ( ω t) = −ω 2 −(xcos( ω− ty) sin( ω t)) sin( ω+ t) ( x sin( ω+ ty) cos( ω t)) cos( ω t)
x(cos22(ω+ t) sin ( ω ty)) +( −sin( ω t) cos( ω+ t) cos( ω t) sin ( ω t)) 2 =1 =0 ax( ,t) = −ω x(−cos( ω t) sin( ω+ t) sin( ω t) cos( ω ty)) +( sin22( ω+ t) cos ( ω t)) =0 =1
2 ax −ω x ax,t = = ( ) 2 ay −ω y
46 vx ω y vx( ,t) = = v −ω Example - Solution y x
(OPTION #2): Acceleration in spatial description is obtained by directly calculating the material derivative of the velocity in spatial description: dtvx( ,,) ∂ vx( t) ax( ,t) = = +vx( ,,tt) ⋅∇ vx( ) dt∂ t ∂ ∂ ωy ∂x ax( ,t) = + [ ω yx ,, −ω] [ ω yx −ω ] = ∂t −ωx ∂ ∂y ∂∂ (ωyx) ( −ω ) 00∂∂xx −ω −ω2 x = + [ ωyx,, −ω ] = [ωyx −ω ] = 00∂∂ ω 2 (ωyx) ( −ω ) −ω y ∂∂yy −ω2 x ax,t = ( ) 2 −ω y
47 1.6 Stationarity and Uniformity
Ch.1. Description of Motion
48 Stationary properties
A property is stationary when its spatial description is not dependent on time. REMARK χχ()()xx,t = In certain fields, the term steady-state is The local derivative of a stationary property is zero. more commonly used. ∂χ ()x,t χχ()()xx,0t = = ∂t
The time-independence in the spatial description (stationarity) does not imply time-independence in the material description:
χχ()()xx,,tt= χ() XX= χ() REMARK This is easily understood if we consider, for example, a stationary velocity: vx()()(),t= vx = vxX() ,, tt = VX()
49 Example
Consider a solid that rotates at a constant angular velocity ω and has the following equation of motion: xR= sin ()ωϕ t + yR= cos()ωϕ t +
We have obtained: Velocity in spatial description
vx ω y stationary vx(),t = = v y −ω x Velocity in material description
Vx −X ω sin()() ω+ tY ω cos ω t VX(),t = = Vy −X ω cos()() ω− tY ω sin ω t
50 Uniform properties
A property is uniform when its spatial description is not dependent on the spatial coordinates. χχ(x,tt) = ( )
If its spatial description does not depend on the coordinates (uniform character of the property), neither does its material one. χχ(xX,,tt) = ( ) χ( tt) = χ( )
51 1.7 Trajectory (path-line)
Ch.1. Description of Motion
52 Trajectory or pathline
A trajectory or pathline is the locus of the positions occupied by a given particle in space throughout time.
REMARK A trajectory can also be defined as the path that a particle follows through space as a function of time.
53 Equation of the trajectories
The equation of a given particle’s trajectory is obtained particularizing the equation of motion for that particle, which is identified by it material coordinates X*. xX()()tt= ϕφ,= () t XX= * xt()()= ϕφX, t= () ti ∈ iii XX= * Also, from the velocity field in spatial description, v(x,t): A family of curves is obtained from: dtx () = vx()()t, t x= φ ()CCCt,,, [1] dt 123 Particularizing for a given particle by imposing the consistency condition in the reference configuration: x()t = XX= φ ()CCC,,,0 C= χ ()X[2] t=0 123 ii Replacing [2] in [1], the equation of the trajectories in canonical form
x= φϕ(CCCt123()()() XXX,,,) = () X , t 54 Example
Consider the following velocity field: ω y vx( ,t) = −ω x
Obtain the equation of the trajectories.
55 Example - Solution
We integrate the velocity field: dx( t) =v,x (x ty) = ω dtx( ) dt = vx( ,t) dt dy( t) =v,y (x tx) = −ω dt This is a crossed-variable system of differential equations. We derive the 2nd eq. and replace it in the 1st one,
d2 y( t) dx( t) = −ω = −ω2 ′′ +ω2 = 2 yt( ) yy0 dt dt
56 Example - Solution
The characteristic equation: r 22+ω =0
Has the characteristic solutions: rijj =±ω∈ {1, 2} And the solution of the problem is: iwt− iwt yt() = RealPartZe{ 12+ Ze} = C 1cos( ω+ t) C 2 sin ( ω t)
dy And, using = −ω x , we obtain dt 11dy x=− =−−ω( C12sin( ω+ tC) ωcos( ω t)) ωωdt So, the general solution is:
xCC( 12, , t) = C 1 sin( ω− t) C2 cos( ω t) yCC( 12, , t) = C 1 cos( ω+ t) C2 sin ( ω t)
57 xCC( 12, , t) = C 1 sin( ω− t) C2 cos( ω t) = ω+ ω Example - Solution yCC( 12, , t) C 1 cos( t) C2 sin ( t)
The canonical form is obtained from the initial conditions: = 0 = 1 X= xCC, ,0 = C sin ω⋅ 0 − C cos ω⋅ 0 =C ( 12) 1 ( ) 2 ( ) 2 = xX(CC12, ,0) Y= yCC( , ,0) = C cos( ω⋅ 0) + C sin( ω⋅ 0) = C 12 12 1 = 10=
This results in:
xY= sin( ω+ t) X cos( ω t) xX( ,)t → y= Y cos( ω− t) Xs in ( ω t)
58 1.8 Streamline
Ch.1. Description of Motion
59 Streamline
The streamlines are a family of curves which, for every instant in time, are the velocity field envelopes.
time – t 0 time – t1 Y Y REMARK Two streamlines can never cut each other. Is it true? X X
Streamlines are defined for any given time instant and change with the velocity field.
REMARK The envelopes of vector field are the curves whose tangent vector at each point coincides (in direction and sense but not necessarily in magnitude) with the corresponding vector of the vector field.
60 Equation of the Streamlines
The equation of the streamlines is of the type:
vz d x d y dz dx = = =λ = = d() ds v v y vvvx yz dλ vx Also, from the velocity field in spatial description, v(x,t*) at a given time instant t*: A family of curves is obtained from: dx() λ = vx()()λ,*t x= φλ(CCC′′′, , , ,* t) dλ 123
Where each group () CCC 123′′′ ,, identifies a streamline x(λ) whose points are obtained assigning values to the parameter λ. For each time instant t* a new family of curves is obtained.
61 Trajectories and Streamlines
For a stationary velocity field, the trajectories and the streamlines coincide – PROOF: 1. If v(x,t)=v(x): Eq. trajectories: dtx() = vx()()t, t x= φ ()CCCt,,, dt 123 Eq. streamlines: dx()λ = vx()()λ,*t x= φλ(CCC, , , ,* t) dλ 123 The differential equations only differ in the denomination of the integration parameter (t or λ), so the solution to both systems MUST be the same.
62 Trajectories and Streamlines
For a stationary velocity field, the trajectories and the streamlines coincide – PROOF: 2. If v(x,t)=v(x) the envelopes (i.e., the streamline) of the field do not vary throughout time.
A particle’s trajectory is always tangent to the velocity field it encounters at every time instant.
If a trajectory starts at a certain point in a streamline and the streamline does not vary with time and neither does the velocity field, the trajectory and streamline MUST coincide.
63 Trajectories and Streamlines
The inverse is not necessarily true: if the trajectories and the streamlines coincide, the velocity field is not necessarily
stationary – COUNTER-EXAMPLE: at Given the (non-stationary) velocity field: v(t0) = 0 The eq. trajectory are: a tC2 + at at 2 1 dx(t) = = 0dx( t0) = dt x(t0) dt 00 0 The eq. streamlines are: at at atλ + C′ dx(λ) 1 = λλ= 00ddx( ) x(t0) = dλ 00 0
64 Example
Consider the following velocity field:
x v =i i ∈{}1, 2, 3 i 1+ t
Obtain the equation of the trajectories and the streamlines associated to this vector field. Do they coincide? Why?
65 Example - Solution
dtx( ) = vx( (tt), ) dt Eq. trajectories: dxi ( t) = v,(x(tt) ) i∈ dt i Introducing the velocity field and rearranging:
dxii x dxi dt =i ∈ =i ∈ dt1+ t xti 1+
Integrating both sides of the expression: 11 dxi = dt ∫∫ lnxi= ln( 1 ++ t) ln Cii = ln C( 1 + ti) ∈ xti 1+
The solution: xii= C(1 +∈ ti) 66
Example - Solution
dx(λ ) = vx( (λ ),*t ) dλ Eq. streamlines: dxi ( t) * = v,i (x(λ ) ti) ∈ dλ Introducing the velocity field and rearranging:
dx x dx dλ ii=i ∈ i =i ∈ λ + + dt1 xti 1 Integrating both sides of the expression: λλ +K ++i 11tt Ki 11 λ xi = e = ee dxi = dλ ln xK= + ∫∫ ii = Ci xti 1+ 1+ t i ∈
The solution: λ 1+t xii= Ce i ∈ 67
Streamtube
A streamtube is a surface composed of streamlines which pass through the points of a closed contour fixed in space.
In stationary cases, the tube will remain fixed in space throughout time. In non-stationary cases, it will vary (although the closed contour line is fixed).
69 1.9 Control and Material Surfaces
Ch.1. Description of Motion
81 Control Surface
A control surface is a fixed surface in space which does not vary in time.
Σ=:{ xf( xyz ,,) = 0}
Mass (particles) can flow across a control surface.
82 Material Surface
A material surface is a mobile surface in the space constituted always by the same particles.
In the reference configuration, the surface Σ0 will be defined in terms of the material coordinates:
Σ=0 :{ X F() XYZ,,= 0}
The set of particles (material points) belonging the surface are the same at all times
In spatial description FXYZ()(, ,= FX (,),(,),(,)xxx tY tZ t) = f (,) x t = fxyzt (, , ,)
Σ=t :{ x f() xyzt,,,= 0}
The set of spatial points belonging to the the surface depends on time The material surface moves in space
84 Material Surface
Necessary and sufficient condition for a mobile surface in space, implicitly defined by the function f () xyzt ,,, , to be a material surface is that the material derivative of the function is zero: Necessary: if it is a material surface, its material description does not depend on time: dF∂ ()X ft()()x,→= f xX ( , ttF ),() X , t 0 ===ft()x , 0 dt ∂ t
Sufficient: if the material derivative of f(x,t) is null: d∂ Ft(X ,) ft()()x,→= f xX ( ,), ttF() X , t 0 ==ft()x , FtF(XX ,) ≡ ( ) dt ∂ t
The surface Σ= t :{ x ft()x,= 0} ={ XX F() = 0} contains always the same set the of particles (it is a material surface)
85 Control Volume
A control volume is a group of fixed points in space situated in the interior of a closed control surface, which does not vary in time. V = { f ()xx ≤ 0|: }
REMARK The function f(x) is defined so that f(x)<0 corresponds to the points inside V.
Particles can enter and exit a control volume.
87 Material Volume
A material volume is a (mobile) volume enclosed inside a material boundary or surface.
In the reference configuration, the volume V0 will be defined in terms of the material coordinates:
VF0 := { XX|() ≤ 0}
The particles X in the volume are the same at all times
In spatial description, the volume Vt will depend on time.
Vt := { xx| ft() ,≤ 0}
The set of spatial points belonging to the the volume depends on time The material volume moves in space along time
89 Material Volume
A material volume is always constituted by the same particles. This is proved by reductio ad absurdum:
If a particle is added into the volume, it would have to cross its material boundary.
Material boundaries are constituted always by the same particles, so, no particles can cross.
Thus, a material volume is always constituted by the same particles (a material volume is a pack of particles).
90 Chapter 1 Description of Motion
1.1 Definition of the Continuous Medium A continuous medium is understood as an infinite set of particles (which form part of, for example, solids or fluids) that will be studied macroscopically, that is, without considering the possible discontinuities existing at microscopic level (atomic or molecular level). Accordingly, one admits that there are no discon- tinuities between the particles and that the mathematical description of this medium and its properties can be described by continuous functions.
1.2 Equations of Motion The most basic description of the motion of a continuous medium can be achieved by means of mathematical functions that describe the position of each particle along time. In general, these functions and their derivatives are required to be continuous. Theory and Problems
Definition 1.1. Consider the following definitions: Continuum Mechanics for Engineers • Spatial point: Fixed© X. point Oliver in space. and C. Agelet de Saracibar • Material point: A particle. It may occupy different spatial points during its motion along time. • Configuration: Locus of the positions occupied in space by the particles of the continuous medium at a given time t.
The continuous medium is assumed to be composed of an infinite number of particles (material points) that occupy different positions in the physical space during its motion along time (see Figure 1.1). The configuration of the contin-
1 2CHAPTER 1. DESCRIPTION OF MOTION
Ω0 – reference configuration t0 – reference time Ωt – present configuration t – present time
Figure 1.1: Configurations of the continuous medium.
uous medium at time t, denoted by Ωt, is defined as the locus of the positions occupied in space by the material points (particles) of the continuous medium at the given time. A certain time t = t0 of the time interval of interest is referred to as the ref- erence time and the configuration at this time, denoted by Ω0, is referred to as initial, material or reference configuration1. Consider now the Cartesian coordinate system (X,Y,Z) in Figure 1.1 and the corresponding orthonormal basis {eˆ1,eˆ2,eˆ3}. In the reference configuration Ω0, the position vector X of a particle occupying a point P in space (at the reference time) is given by2,3
X = X1eˆ1 + X2eˆ2 + X3eˆ3 = Xieˆi, (1.1) where the components (X1,X2,X3) are referred to as material coordinates (of the particle) and can be collected in a vector of components denoted as4 ⎡ ⎤ TheoryX1 and Problems not ⎢ ⎥ def X ≡ [X]=⎣ X2 ⎦ = material coordinates. (1.2) Continuum MechanicsX3 for Engineers © X. Oliver and C. Agelet de Saracibar 1 In general, the time t0 = 0 will be taken as the reference time. 2 Notations (X,Y,Z) and (X1,X2,X3) will be used indistinctly to designate the Cartesian coordinate system. 3 Einstein or repeated index notation will be used in the remainder of this text. Every repe- tition of an index in the same monomial of an algebraic expression represents the sum over that index. For example, i=3 k=3 i=3 j=3 not not not ∑ Xieˆi = Xieˆi , ∑ aikbkj = aikbkj and ∑ ∑ aijbij = aijbij. i=1 k=1 i=1 j=1 4 Here, the vector (physical entity) X is distinguished from its vector of components [X]. Henceforth, the symbol not≡ (equivalent notation) will be used to indicate that the tensor and component notations at either side of the symbol are equivalent when the system of coordi- nates used remains unchanged.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Equations of Motion 3
5 In the present configuration Ωt , a particle originally located at a material point P (see Figure 1.1) occupies a spatial point P and its position vector x is given by x = x1eˆ1 + x2eˆ2 + x3eˆ3 = xieˆi, (1.3) where (x1,x2,x3) are referred to as spatial coordinates of the particle at time t, ⎡ ⎤ x1 not ⎢ ⎥ def x ≡ [x]=⎣ x2 ⎦ = spatial coordinates. (1.4) x3
The motion of the particles of the continuous medium can now be described by the evolution of their spatial coordinates (or their position vector) along time. Mathematically, this requires the definition of a function that provides for each particle (identified by its label) its spatial coordinates xi (or its spatial position vector x) at successive instants of time. The material coordinates Xi of the par- ticle can be chosen as the label that univocally characterizes it and, thus, the equation of motion x = ϕ (particle,t)=ϕ (X,t) not= x(X,t) (1.5) xi = ϕi (X1,X2,X3,t) i ∈ {1,2,3} is obtained, which provides the spatial coordinates in terms of the material ones. The spatial coordinates xi of the particle can also be chosen as label, defining the inverse equation of motion6 as X = ϕ−1 (x,t) not= X(x,t) , (1.6) = ϕ−1 ( , , , ) ∈ { , , } , Xi i x1 x2 x3 t i 1 2 3 which provides the materialTheory coordinates and in terms Problems of the spatial ones.
RemarkContinuum 1.1. There are Mechanics different alternatives for when Engineers choosing the la- bel that characterizes© X. a particle, Oliver even and though C. Agelet the option de Saracibar of using its material coordinates is the most common one. When the equation of motion is written in terms of the material coordinates as label (as in (1.5)), one refers to it as the equation of motion in canonical form.
5 Whenever possible, uppercase letters will be used to denote variables relating to the refer- ence configuration Ω0 and lowercase letters to denote the variables referring to the current configuration Ωt . 6 With certain abuse of notation, the function will be frequently confused with its image. Hence, the equation of motion will be often written as x = x(X,t) and its inverse equation as X = X(x,t).
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 4CHAPTER 1. DESCRIPTION OF MOTION
There exist certain mathematical restrictions to guarantee the existence of ϕ and ϕ−1, as well as their correct physical meaning. These restrictions are: • ϕ (X,0)=X since, by definition, X is the position vector at the reference time t = 0 (consistency condition). • ϕ ∈ C1 (function ϕ is continuous with continuous derivatives at each point and at each instant of time). • ϕ is biunivocal (to guarantee that two particles do not occupy simultaneously the same point in space and that a particle does not occupy simultaneously more than one point in space).
∂ϕ(X,t) not ∂ϕ(X,t) • The Jacobian of the transformation J = det = > 0. ∂X ∂X The physical interpretation of this condition (which will be studied later) is that every differential volume must always be positive or, using the principle of mass conservation (which will be seen later), the density of the particles must always be positive.
Remark 1.2. The equation of motion at the reference time t = 0 re- ( , )| = = = = sults in x X t t=0 X. Accordingly, x X, y Y, z Z is the equation of motion at the reference time and the Jacobian at this in- stant of time is7 ∂( ) ∂ xyz xi J (X,0)= = det = det[δij]=det1 = 1. ∂(XYZ) ∂Xj
Theory and Problems
Continuum Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar
Figure 1.2: Trajectory or pathline of a particle.
7 not The two-index operator Delta Kronecker = δij is defined as δij = 0 when i = j and δij = 1 = [ ] = δ when i j. Then, the unit tensor 1 is defined as 1 ij ij.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Equations of Motion 5
Remark 1.3. The expression x = ϕ (X,t), particularized for a fixed value of the material coordinates X, provides the equation of the trajectory or pathline of a particle (see Figure 1.2).
Example 1.1 – The spatial description of the motion of a continuous medium is given by ⎡ ⎤ ⎡ ⎤ x = X e2t x = Xe2t ⎢ 1 1 ⎥ ⎢ ⎥ ( , ) not≡ −2t = −2t x X t ⎣ x2 = X2e ⎦ ⎣ y = Ye ⎦ 2t 2t x3 = 5X1t + X3e z = 5Xt + Ze
Obtain the inverse equation of motion.
Solution The determinant of the Jacobian is computed as
∂ ∂ ∂ x1 x1 x1 ∂ ∂ ∂ X1 X2 X3 e2t 00 ∂ xi ∂x ∂x ∂x − 2t J = = 2 2 2 = 0e2t 0 = e = 0. ∂Xj ∂ ∂ ∂ X1 X2 X3 2t 5t 0e ∂x3 ∂x3 ∂x3 ∂ ∂ ∂ TheoryX1 X2 andX3 Problems The sufficient (but not necessary) condition for the function x = ϕ (X,t) to be biunivocalContinuum (that is, for Mechanics its inverse to exist) for is that Engineers the determinant of the Jacobian of the function© X. is not Oliver null. Inand addition, C. Agelet since thede JacobianSaracibar is positive, the motion has physical sense. Therefore, the inverse of the given spatial description exists and is determined by ⎡ ⎤ ⎡ ⎤ −2t ⎢ X1 ⎥ ⎢ x1e ⎥ = ϕ−1 ( , ) not≡ ⎢ ⎥ = ⎢ 2t ⎥. X x t ⎣ X2 ⎦ ⎣ x2e ⎦ −2t −4t X3 x3e − 5tx1e
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 6CHAPTER 1. DESCRIPTION OF MOTION
1.3 Descriptions of Motion The mathematical description of the properties of the particles of the continu- ous medium can be addressed in two alternative ways: the material description (typically used in solid mechanics) and the spatial description (typically used in fluid mechanics). Both descriptions essentially differ in the type of argument (material coordinates or spatial coordinates) that appears in the mathematical functions that describe the properties of the continuous medium. 1.3.1 Material Description In the material description8, a given property (for example, the density ρ)is described by a certain function ρ (•,t) : R3 ×R+ → R+, where the argument (•) in ρ (•,t) represents the material coordinates,
ρ = ρ (X,t)=ρ (X1,X2,X3,t). (1.7)
Here, if the three arguments X ≡ (X1,X2,X3) are fixed, a specific particle is being followed (see Figure 1.3) and, hence, the name of material description. 1.3.2 Spatial Description In the spatial description9, the focus is on a point in space. The property is de- scribed as a function ρ (•,t) : R3 × R+ → R+ of the point in space and of time,
ρ = ρ (x,t)=ρ (x1,x2,x3,t). (1.8) Then, when the argument x in ρ = ρ (x,t) is assigned a certain value, the evolu- tion of the density for the different particles that occupy the point in space along time is obtained (see Figure 1.3). Conversely, fixing the time argument in (1.8) results in an instantaneous distribution (like a snapshot) of the property in space. Obviously, the direct andTheory inverse equations and of Problems motion allow shifting from one
Continuum Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar
Figure 1.3: Material description (left) and spatial description (right) of a property.
8 Literature on this topic also refers to the material description as Lagrangian description. 9 The spatial description is also referred to as Eulerian description.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Descriptions of Motion 7 description to the other as follows. ρ (x,t)=ρ (x(X,t),t)=ρ (X,t) (1.9) ρ (X,t)=ρ (X(x,t),t)=ρ (x,t)
Example 1.2 – The equation of motion of a continuous medium is
x = X −Yt x = x(X,t) not≡ y = Xt +Y . z = −Xt + Z
Obtain the spatial description of the property whose material description is X +Y + Z ρ (X,Y,Z,t)= . 1 +t2 Solution The equation of motion is given in the canonical form since in the reference configuration Ω0 its expression results in
x = X x = X(X,0) not≡ y = Y . z = Z
The determinant of the Jacobian is
∂x ∂x ∂x
∂ ∂ ∂ X Y Z 1 −t 0 ∂ Theory and Problems = xi = ∂y ∂y ∂y = = + 2 = J ∂ t 10 1 t 0 Xj ∂X ∂Y ∂Z −t 01 ∂ ∂ ∂ Continuum Mechanicsz z z for Engineers ©∂ X.X Oliver∂Y and∂Z C. Agelet de Saracibar and the inverse equation of motion is given by ⎡ ⎤ x + yt ⎢ X = ⎥ ⎢ + 2 ⎥ ⎢ 1 t ⎥ ⎢ ⎥ ( , ) not≡ ⎢ y − xt ⎥ . X x t ⎢Y = ⎥ ⎢ 1 +t2 ⎥ ⎣ ⎦ z + zt2 + xt + yt2 Z = 1 +t2
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 8CHAPTER 1. DESCRIPTION OF MOTION
Consider now the material description of the property, X +Y + Z ρ (X,Y,Z,t)= , 1 +t2 its spatial description is obtained by introducing the inverse equation of mo- tion into the expression above,
x + yt + y + z + zt2 + yt2 ρ (X,Y,Z,t) ≡ = ρ (x,y,z,t). (1 +t2)2
1.4 Time Derivatives: Local, Material and Convective The consideration of different descriptions (material and spatial) of the proper- ties of the continuous medium leads to diverse definitions of the time derivatives of these properties. Consider a certain property and its material and spatial de- scriptions, Γ (X,t)=γ (x,t), (1.10) in which the change from the spatial to the material description and vice versa is performed by means of the equation of motion (1.5) and its inverse equa- tion (1.6).
Definition 1.2. The local derivative of a property is its variation along time at a fixed point in space. If the spatial description γ (x,t) of the property is available, the local derivative is mathematically written as10 Theory and∂γ Problems(x,t) local derivative not= . ∂t TheContinuummaterial derivative Mechanicsof a property is its for variation Engineers along time fol- lowing a specific particle© X. Oliver (material and point) C. of Agelet the continuous de Saracibar medium. If the material description Γ (X,t) of the property is available, the material derivative is mathematically written as d ∂Γ (X,t) material derivative not= Γ = . dt ∂t
10 The expression ∂ (•,t)/∂t is understood in the classical sense of partial derivative with respect to the variable t.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Time Derivatives: Local, Material and Convective 9
However, taking the spatial description of the property γ (x,t) and considering the equation of motion is implicit in this expression yields
γ (x,t)=γ (x(X,t),t)=Γ (X,t) . (1.11) Then, the material derivative (following a particle) is obtained from the spatial description of the property as d ∂Γ (X,t) material derivative not= γ (x(X,t),t)= . (1.12) dt ∂t Expanding (1.12) results in11 γ ( ( , ), ) ∂γ( , ) ∂γ ∂ ∂γ( , ) ∂γ ∂ d x X t t = x t + xi = x t + · x = ∂ ∂ ∂ ∂ ∂ ∂ dt t xi t t x t ( , ) (1.13) ∂γ(x,t) ∂γ v x t = + · v(x,t) , ∂t ∂x where the definition of velocity as the derivative of the equation of motion (1.5) with respect to time has been taken into account, ∂x(X,t) = V(X(x,t),t)=v(x,t) . (1.14) ∂t The deduction of the material derivative from the spatial description can be generalized for any property χ (x,t) (of scalar, vectorial or tensorial character) as12 dχ (x,t) ∂χ(x,t) = + v(x,t) · ∇χ (x,t) . (1.15) dt ∂t materialTheorylocal and Problemsconvective derivative derivative derivative Continuum Mechanics for Engineers Remark 1.4. The expression© X. Oliver in (1.15 and) implicitly C. Agelet defines de Saracibar the convec- tive derivative v · ∇(•) as the difference between the material and spatial derivatives of the property. In continuum mechanics, the term convection is applied to phenomena that are related to mass (or par- ticle) transport. Note that, if there is no convection (v = 0), the con- vective derivative disappears and the local and material derivatives coincide.
11 In literature, the notation D(•)/Dt is often used as an alternative to d(•)/dt. 12 The symbolic form of the spatial Nabla operator, ∇ ≡ ∂eˆi/∂xi , is considered here.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 10 CHAPTER 1. DESCRIPTION OF MOTION
Example 1.3 – Given the equation of motion
x = X +Yt+ Zt x(X,t) not≡ y = Y + 2Zt , z = Z + 3Xt
and the spatial description of a property, ρ (x,t)=3x + 2y + 3t, obtain the material derivative of this property.
Solution The material description of the property is obtained introducing the equation of motion into its spatial description, ρ (X,Y,Z,t)=3(X +Yt+ Zt)+2(Y + 2Zt)+3t = 3X +3Yt+7Zt+2Y +3t . The material derivative is then calculated as the derivative of the material description with respect to time, ∂ρ = 3Y + 7Z + 3 . ∂t An alternative way of deducing the material derivative is by using the concept of material derivative of the spatial description of the property, dρ ∂ρ = + v · ∇ρ with dt ∂t ∂ρ ∂x = 3 , v = =[Y + Z, 2Z, 3X]T and ∇ρ =[3, 2, 0]T . ∂t ∂t Replacing in the expressionTheory of the material and Problems derivative operator, dρ = 3 + 3Y + 7Z Continuum Mechanicsdt for Engineers © X. Oliver and C. Agelet de Saracibar is obtained. Note that the expressions for the material derivative obtained from the material description, ∂ρ/∂t, and the spatial description, dρ/dt, co- incide.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Velocity and Acceleration 11
1.5 Velocity and Acceleration
Definition 1.3. The velocity is the time derivative of the equation of motion.
The material description of velocity is, consequently, given by ⎧ ⎪ ∂x(X,t) ⎨ V(X,t)= ∂t ⎪ (1.16) ⎩⎪ ∂xi (X,t) V (X,t)= i ∈{1, 2, 3} i ∂t and, if the inverse equation of motion X = ϕ−1 (x,t) is known, the spatial de- scription of the velocity can be obtained as
v(x,t)=V(X(x,t),t) . (1.17)
Definition 1.4. The acceleration is the time derivative of the velocity field.
If the velocity is described in material form, the material description of the acceleration is given by ⎧ ⎪ Theory∂V( andX,t) Problems ⎨ A(X,t)= ∂t ⎪ (1.18) ⎩⎪ ∂Vi (X,t) ContinuumA (X Mechanics,t)= i for∈{1, Engineers2, 3} ©i X. Oliver∂ andt C. Agelet de Saracibar and, through the inverse equation of motion X = ϕ−1 (x,t), the spatial descrip- tion is obtained, a(x,t)=A(X(x,t),t). Alternatively, if the spatial description of the velocity is available, applying (1.15) to obtain the material derivative of v(x,t), dv(x,t) ∂v(x,t) a(x,t)= = + v(x,t) · ∇v(x,t) , (1.19) dt ∂t directly yields the spatial description of the acceleration.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 12 CHAPTER 1. DESCRIPTION OF MOTION
Example 1.4 – Consider the solid in the figure below, which rotates at a constant angular velocity ω and has the expression x = Rsin(ωt + φ) y = Rcos(ωt + φ)
as its equation of motion. Find the velocity and acceleration of the motion described both in material and spatial forms.
Solution The equation of motion can be rewritten as x = Rsin(ωt + φ)=Rsin(ωt)cosφ + Rcos(ωt)sinφ y = Rcos(ωt + φ)=Rcos(ωt)cosφ − Rsin(ωt)sinφ
and, since for t = 0, X = Rsinφ and Y = Rcosφ, the canonical form of the equation of motion and its inverse equation result in x = X cos(ωt)+Y sin(ωt) X = xcos(ωt) − ysin(ωt) and . y = −X sin(ωt)+TheoryY cos(ωt) and ProblemsY = xsin(ωt)+ycos(ωt)
Velocity in material description: Continuum Mechanics⎡ for Engineers ⎤ © X. Oliver∂x and C. Agelet de Saracibar ∂ ( , ) ⎢ = −Xω sin(ωt)+Yω cos(ωt) ⎥ x X t not ⎢ ∂t ⎥ V(X,t)= ) ≡ ⎣ ⎦ ∂t ∂y = −Xω cos(ωt) −Yω sin(ωt) ∂t
Velocity in spatial description: Replacing the canonical form of the equation of motion into the material description of the velocity results in
not ωy v(x,t)=V(X(x,t),t) ≡ . −ωx
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Velocity and Acceleration 13
Acceleration in material description: ∂V(X,t) A(X,t)= ∂t ⎡ ⎤ ∂v ⎢ x = −Xω2 cos(ωt) −Yω2 sin(ωt) ⎥ not ⎢ ∂ ⎥ A(X,t) ≡ ⎢ t ⎥ = ⎣ ∂ ⎦ vy = ω2 (ω ) − ω2 (ω ) ∂ X sin t Y cos t t X cos(ωt)+Y sin(ωt) = −ω2 −X sin(ωt)+Y cos(ωt)
Acceleration in spatial description: Replacing the canonical form of the equation of motion into the material description of the acceleration results in
−ω2x a(x,t)=A(X(x,t),t) not≡ . −ω2y
This same expression can be obtained if the expression for the velocity v(x,t) and the definition of material derivative in (1.15) are taken into account, dv(x,t) ∂v(x,t) a(x,t)= = + v(x,t) · ∇v(x,t)= dt ∂t ⎡ ⎤ ∂ ⎢ ⎥ not ∂ ωy ⎢ ∂ ⎥ ≡ + ωy , −ωx ⎢ x ⎥ ωy , −ωx , ∂t Theory−ωx and Problems⎣ ∂ ⎦ ∂y Continuum Mechanics⎡ for Engineers⎤ © X. Oliver and∂ C. Agelet∂ de Saracibar ⎢ (ωy) (−ωx) ⎥ −ω2 not 0 ⎢ ∂ ∂ ⎥ x a(x,t) ≡ + ωy , −ωx ⎢ x x ⎥ = . 0 ⎣ ∂ ∂ ⎦ −ω2y (ωy) (−ωx) ∂y ∂y Note that the result obtained using both procedures is identical.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 14 CHAPTER 1. DESCRIPTION OF MOTION
1.6 Stationarity
Definition 1.5. A property is stationary when its spatial description does not depend on time.
According to the above definition, and considering the concept of local deriva- tive, any stationary property has a null local derivative. For example, if the ve- locity for a certain motion is stationary, it can be described in spatial form as ∂v(x,t) v(x,t)=v(x) ⇐⇒ = 0 . (1.20) ∂t
Remark 1.5. The non-dependence on time of the spatial description (stationarity) assumes that, for a same point in space, the property being considered does not vary along time. This does not imply that, for a same particle, such property does not vary along time (the ma- terial description may depend on time). For example, if the velocity v(x,t) is stationary, v(x,t) ≡ v(x)=v(x(X,t)) = V(X,t) ,
and, thus, the material description of the velocity depends on time. In the case of stationary density (see Figure 1.4), for two particles labeled X1 and X2 that have varying densities along time, when oc- cupying a same spatial point x (at two different times t1 and t2) their density value will coincide,Theory and Problems ρ (X1,t1)=ρ (X2,t2)=ρ (x) . ThatContinuum is, for an observer Mechanics placed outside the for medium, Engineers the density of the fixed point in space© X.x Oliverwill always and be C. the Agelet same. de Saracibar
Figure 1.4: Motion of two particles with stationary density.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Trajectory 15
Example 1.5 – Justify if the motion described in Example 1.4 is stationary or not.
Solution The velocity field in Example 1.4 is v(x) not≡ [ωy , −ωx]T . Therefore, it is a case in which the spatial description of the velocity is not dependent on time and, thus, the velocity is stationary. Obviously, this implies that the velocity of the particles (whose motion is a uniform rotation with respect to the origin, with angular velocity ω) does not depend on time (see figure below). The direction of the velocity vector for a same particle is tangent to its circular trajectory and changes along time.
The acceleration (material derivative of the velocity), dv(x) ∂v(x) a(x)= = + v(x) · ∇v(x)=v(x) · ∇v(x) , dt ∂t appears due to the change in direction of the velocity vector of the particles and is known as the centripetal acceleration. Theory and Problems 1.7 Trajectory Continuum Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar Definition 1.6. A trajectory (or pathline) is the locus of the positions occupied in space by a given particle along time.
The parametric equation of a trajectory as a function of time is obtained by par- ticularizing the equation of motion for a given particle (identified by its material coordinates X∗, see Figure 1.5),
x(t)=ϕ (X,t) . (1.21) X=X∗
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 16 CHAPTER 1. DESCRIPTION OF MOTION
Figure 1.5: Trajectory or pathline of a particle.
Given the equation of motion x = ϕ (X,t), each point in space is occupied by a trajectory characterized by the value of the label (material coordinates) X. Then, the equation of motion defines a family of curves whose elements are the trajectories of the various particles. 1.7.1 Differential Equation of the Trajectories Given the velocity field in spatial description v(x,t), the family of trajectories can be obtained by formulating the system of differential equations that imposes that, for each point in space x, the velocity vector is the time derivative of the parametric equation of the trajectory defined in (1.21), i.e., ⎧ ⎪ dx(t) ⎨ = v(x(t), t) , ( ) = dt Find x t : ⎪ (1.22) ⎩⎪ dxi (t) = v (x(t), t) i ∈ {1, 2, 3} . dt i The solution to this first-order system of differential equations depends on three integration constants (C ,C ,C ), 1 2 3 x = φ (C ,C ,C , t) , Theory1 2 3 and Problems (1.23) x = φi (C1,C2,C3, t) i ∈ {1, 2, 3} .
These expressions constitute a family of curves in space parametrized by the Continuum( , , ) Mechanics for Engineers constants C1 C2 C3 . Assigning© X. Oliver a particular and C. value Agelet to these de Saracibar constants yields a member of the family, which is the trajectory of a particle characterized by the label (C1,C2,C3). To obtain the equation in canonical form, the consistency condition is im- posed in the reference configuration,
x(t) = X =⇒ X = φ (C1,C2,C3,0)=⇒ Ci = χi (X) i ∈ {1, 2, 3}, (1.24) t=0 and, replacing into (1.23), the canonical form of the equation of the trajectory,
X = φ (C1 (X),C2 (X),C3 (X), t)=ϕ (X,t) , (1.25) is obtained.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Trajectory 17
Example 1.6 – Given the velocity field in Example 1.5, v(x) not≡ [ωy , −ωx]T , obtain the equation of the trajectory.
Solution Using expression (1.22), one can write ⎧ ⎪ ( ) ⎨⎪ dx t ( ) = vx (x,t)=ωy , dx t = ( , )=⇒ dt v x t ⎪ dt ⎩⎪ dy(t) = v (x,t)=−ωx . dt y This system of equations is a system with crossed variables. Differentiating the second equation and replacing the result obtained into the first equation yields 2 d y(t) dx(t) = −ω = −ω2y(t)=⇒ y + ω2y = 0 . dt2 dt The characteristic equation of this second-order differential equation is 2 2 r + ω = 0 and its characteristic solutions are r j = ±iω j ∈ {1, 2}. Therefore, the y component of the equation of the trajectory is iwt −iwt y(t)=Real Part C1e +C2e = C1 cos(ωt)+C2 sin(ωt) .
The solution for x(t) is obtained from dy/dt = −ωx , which results in x = −dy/(ω dt) and, therefore, x(C1,C2,t)=C1 sin(ωt) −C2 cos(ωt) , y(C ,C ,t)=C cos(ωt)+C sin(ωt) . Theory1 2 1 and Problems2 This equation provides the expressions of the trajectories in a non-canonical form. The canonical form is obtained considering the initial condition, Continuum Mechanics for Engineers © X. Oliverx(C1,C and2,0)= C.X Agelet, de Saracibar that is, x(C1,C2,0)=−C2 = X ,
y(C1,C2,0)=C1 = Y . Finally, the equation of motion, or the equation of the trajectory, in canonical form x = Y sin(ωt)+X cos(ωt) y = Y cos(ωt) − X sin(ωt) is obtained.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 18 CHAPTER 1. DESCRIPTION OF MOTION
1.8 Streamline
Definition 1.7. The streamlines are a family of curves that, for every instant of time, are the velocity field envelopes13.
According to its definition, the tangent at each point of a streamline has the same direction (though not necessarily the same magnitude) as the velocity vector at that same point in space.
Remark 1.6. In general, the velocity field (in spatial description) will be different for each instant of time (v ≡ v(x,t)). Therefore, one must speak of a different family of streamlines for each instant of time (see Figure 1.6).
1.8.1 Differential Equation of the Streamlines Consider a given time t∗ and the spatial description of the velocity field at this time v(x,t∗). Let x(λ) be the equation of a streamline parametrized in terms of a certain parameter λ. Then, the vector tangent to the streamline is defined, for Theory and Problems
Continuum Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar
Figure 1.6: Streamlines at two different instants of time.
13 The envelopes of a vector field are the family of curves whose tangent vector has, at each point, the same direction as the corresponding vector of the vector field.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Streamline 19 each value of λ 14,bydx(λ)/dλ and the vector field tangency condition can be written as follows. ⎧ ⎪ dx(λ) ⎨ = v(x(λ), t∗) , (λ) = dλ Find x : ⎪ (1.26) ⎩⎪ dxi (λ) ∗ = v (x(λ), t ) i ∈ {1, 2, 3} . dλ i The expressions in (1.26) constitute a system of first-order differential equa- tions whose solution for each time t∗, which will depend on three integration ( , , ) constants C1 C2 C3 , provides the parametric expression of the streamlines, x = φ (C ,C ,C ,λ, t∗) , 1 2 3 (1.27) = φ ( , , ,λ, ∗) ∈ { , , } . xi i C1 C2 C3 t i 1 2 3 ( , , ) Each triplet of integration constants C1 C2 C3 identifies a streamline whose points, in turn, are obtained by assigning values to the parameter λ. For each time t∗ a new family of streamlines is obtained.
Remark 1.7. In a stationary velocity field (v(x,t) ≡ v(x)) the trajec- tories and streamlines coincide. This can be proven from two differ- ent viewpoints: • The fact that the time variable does not appear in (1.22)or(1.26) means that the differential equations defining the trajectories and those defining the streamlines only differ in the denomination of the integration parameter (t or λ, respectively). The solution to both systems must be, therefore, the same, except for the name of the parameterTheory used in each and type of Problems curves. • From a more physical point of view: a) If the velocity field is Continuumstationary, its envelopes Mechanics (the streamlines) for do Engineers not change along time; b) a given© particleX. Oliver moves and in C. space Agelet keeping de Saracibarthe trajectory in the direction tangent to the velocity field it encounters along time; c) consequently, if a trajectory starts at a certain point in a streamline, it will stay on this streamline throughout time.
14 It is assumed that the value of the parameter λ is chosen such that, at each point in space x, not only does dx(λ)/dλ have the same direction as the vector v(x,t), but it coincides therewith.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 20 CHAPTER 1. DESCRIPTION OF MOTION
1.9 Streamtubes
Definition 1.8. A streamtube is a surface formed by a bundle of streamlines that occupy the points of a closed line, fixed in space, and that does not constitute a streamline.
In non-stationary cases, even though the closed line does not vary in space, the streamtube and streamlines do change. On the contrary, in a stationary case, the streamtube remains fixed in space along time. 1.9.1 Equation of the Streamtube Streamlines constitute a family of curves of the type
x = f(C1,C2,C3,λ, t) . (1.28) The problem consists in determining, for each instant of time, which curves of the family of curves of the streamlines cross a closed line, which is fixed in the space Γ , whose mathematical expression parametrized in terms of a parameter s is Γ := x = g(s) . (1.29) To this aim, one imposes, in terms of the parameters λ ∗ and s∗, that a same point belong to both curves, ∗ ∗ g(s )=f(C1,C2,C3,λ , t) , (1.30) ( ∗)= ( , , ,λ ∗, ) ∈ { , , } . gi s Theoryfi C1 C2 C and3 t Problemsi 1 2 3 ∗ ∗ A system of three equations is obtained from which, for example, s , λ and C3 can be isolated, Continuum Mechanics∗ ∗ for Engineers © X.s Oliver= s (C and1,C2, C.t) Agelet, de Saracibar ∗ ∗ λ = λ (C1,C2, t) , (1.31)
C3 = C3 (C1,C2, t) . Introducing (1.31) into (1.30) yields ∗ x = f(C1, C2, C3 (C1,C2, t), λ (C1,C2, t), t)=h(C1,C2, t) , (1.32) which constitutes the parametrized expression (in terms of the parameters C1 and C2) of the streamtube for each time t (see Figure 1.7).
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Streaklines 21
Figure 1.7: Streamtube at a given time t.
1.10 Streaklines
∗ Definition 1.9. A streakline, relative to a fixed point in space x named spill point and at a time interval ti,t f named spill period, is the locus of the positions occupied at time t by all the particles ∗ that have occupied x over the time τ ∈ [ti,t] ti,t f .
The above definition corresponds to the physical concept of the color line (streak) that would be observed in the medium at time t if a tracer fluid were ∗ injected at spill point x throughout the time interval ti,t f (see Figure 1.8).
Theory and Problems
Continuum Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar
Figure 1.8: Streakline corresponding to the spill period τ ∈ ti,t f .
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1.10.1 Equation of the Streakline To determine the equation of a streakline one must identify all the particles that occupy point x∗ in the corresponding times τ. Given the equation of motion (1.5) and its inverse equation (1.6), the label of the particle which at time τ occupies the spill point must be identified. Then, x∗ = x(X,τ) =⇒ X = f(τ) (1.33) ∗ = ( ,τ) ∈ { , , } xi xi X i 1 2 3 and replacing (1.33) into the equation of motion (1.5) results in x = ϕ (f(τ), t)=g(τ, t) τ ∈ [ti,t] ti,t f . (1.34)
Expression (1.34) is, for each time t, the parametric expression (in terms of parameter τ) of a curvilinear segment in space which is the streakline at that time.
Example 1.7 – Given the equation of motion ⎧ ⎨ x =(X +Y)t2 + X cost , ⎩ y =(X +Y)cost − X ,
obtain the equation of the streakline associated with the spill point x∗ =(0,1) for the spill period [t0,+∞).
Solution The material coordinatesTheory of a particle and that has Problems occupied the spill point at time τ are given by ⎧ ⎪ −τ2 Continuum=( + )τ Mechanics2 + τ for⎨ X Engineers= , 0 X ©Y X. OliverX cos and= C.⇒ Ageletτ de2 + Saracibarcos2 τ ⎪ 1 =(X +Y)cosτ − X ⎩⎪ τ2 + cosτ Y = . τ2 + cos2 τ Therefore, the label of the particles that have occupied the spill point from the initial spill time t0 until the present time t is defined by ⎫ −τ2 ⎪ X = ⎬ τ2 + cos2 τ τ ∈ [ , ] [ ,∞)=[ , ] . ⎪ t0 t t0 t0 t τ2 + cosτ ⎭⎪ Y = τ2 + cos2 τ
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Material Surface 23
Then, replacing these into the equation of motion, the equation of the streak- line is obtained, ⎡ ⎤ cosτ −τ2 ⎢ x = t2 + cost ⎥ not ⎢ τ2 + cos2 τ τ2 + cos2 τ ⎥ x = g(τ,t) ≡ ⎣ ⎦ τ ∈ [t0,t] . cosτ −τ2 y = cost − τ2 + cos2 τ τ2 + cos2 τ
Remark 1.8. In a stationary problem, the streaklines are segments of the trajectories (or of the streamlines). The rationale is based on the fact that, in the stationary case, the trajectory follows the envelope of the velocity field, which remains constant along time. If one consid- ers a spill point x∗, all the particles that occupy this point will follow portions (segments) of the same trajectory.
1.11 Material Surface
Definition 1.10. A material surface is a mobile surface in space al- ways constituted by the same particles (material points).
In the reference configuration Ω0, surface Σ0 can be defined in terms of a func- tion of the material coordinatesTheoryF (X,Y and,Z) as Problems Σ := {X,Y,Z | F (X,Y,Z)=0} . (1.35) Continuum0 Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar
Remark 1.9. The function F (X,Y,Z) does not depend on time, which guarantees that the particles, identified by their label, that sat- isfy equation F (X,Y,Z)=0 are always the same in accordance with the definition of material surface.
The spatial description of the surface is obtained from the spatial description of F (X(x,t)) = f (x,y,z,t) as
Σt := {x,y,z | f (x,y,z,t)=0} . (1.36)
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 24 CHAPTER 1. DESCRIPTION OF MOTION
Remark 1.10. The function f (x,y,z,t) depends explicitly on time, which indicates that the points in space that are on the surface will vary along time. This time dependence of the spatial description of the surface confers the character of mobile surface in space to the surface (see Figure 1.9).
Remark 1.11. The necessary and sufficient condition for a mobile surface in space, defined implicitly by a function f (x,y,z,t)=0, to be material (to be always constituted by the same particles) is that the material derivative of f (x,y,z,t) is null,
df(x,t) ∂ f = + v · ∇ f = 0 ∀x ∈ Σ ∀t . dt ∂t t The condition is necessary because, if the surface is a material sur- face, its material description will not depend on time (F ≡ F (X)) and, therefore, its spatial description will have a null material deriva- tive. The condition of sufficiency is based on the fact that, if the ma- terial derivative of f (x,t) is zero, the corresponding material de- scription will not depend on time (F ≡ F (X)) and, therefore, the set of particles (identified by their material coordinates) that satisfy the condition F (X)=0 is always the same.
Theory and Problems
Continuum Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar
Figure 1.9: A material surface at two different instants of time.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Material Surface 25
Example 1.8 – In ocean waves theory, the condition that the free surface of the fluid in contact with the atmosphere is a material surface is imposed. This restriction implies that the free surface is always composed of the same particles, which is a reasonable hypothesis (especially in deep waters). De- termine how this condition is stated in terms of the velocity field of the fluid.
Solution Assuming that z = η (x,y,t) defines the elevation of the sea surface with re- spect to a reference level, the free surface of the water will be given by f (x,y,z,t) ≡ z − η (x,y,t)=0 .
The condition df/dt = 0 can be written as df ∂ f ∂ f ∂η = + v · ∇ f where = − and dt ∂t ∂t ∂t Theory and Problems ∂ ∂ ∂ T ∂ ∂ ∂ · ∇ not≡ [ , , ] f , f , f = f + f + f . v f vx vy vz ∂ ∂ ∂ vx ∂ vy ∂ vz ∂ Continuum Mechanicsx y z for Engineersx y z Then, © X. Oliver and C. Agelet de Saracibar df ∂ f ∂η ∂η ∂η = + v · ∇ f = − − v − v + v = 0 dt ∂t ∂t x ∂x y ∂y z
and, isolating vz leads to ∂η ∂η ∂η v = + v + v . z ∂t x ∂x y ∂y Therefore, the material surface condition results in a condition on the vertical component of the velocity field.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 26 CHAPTER 1. DESCRIPTION OF MOTION
1.12 Control Surface
Definition 1.11. A control surface is a fixed surface in space.
The mathematical description of a control surface is given by Σ := {x | f (x,y,z)=0} . (1.37) Obviously, a control surface is occupied by the different particles of the contin- uous medium along time (see Figure 1.10).
Figure 1.10: Movement of particles through a control surface along time.
1.13 Material Volume Theory and Problems Definition 1.12. A material volume is a volume enclosed by a closed material surface. Continuum Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar The mathematical description of a material volume (see Figure 1.11) is given, in the material description, by15
V0 := {X | F (X) ≤ 0} (1.38) and, in the spatial description, by
Vt := {x | f (x,t) ≤ 0}, (1.39)
15 It is assumed that function F (X) is defined such that F (X) < 0 corresponds to points in the interior of V0.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Control Volume 27 where F (X)= f (x(X,t),t) is the function that describes the material surface that encloses the volume.
Remark 1.12. A material volume is always constituted by the same particles. This is proven by reductio ad absurdum as follows. If a certain particle could enter or exit the material volume, it would be incorporated into the material surface during its motion (at least, for an instant of time). This would be contrary to the fact that the sur- face, being a material surface, is always constituted by the same par- ticles.
Figure 1.11: A material volume at two different instants of time.
1.14 Control Volume Theory and Problems
DefinitionContinuum 1.13. A control Mechanics volume is a group for of Engineers points in space situ- ated in the interior© of X. a closed Oliver control and surface. C. Agelet de Saracibar
It is a volume fixed in space that is occupied by the particles of the medium during its motion. The mathematical description of the control volume (see Fig- ure 1.12)is16 V := {x | f (x) ≤ 0} . (1.40)
16 It is assumed that function f (x) is defined such that f (x) < 0 corresponds to points in the interior of V.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 28 CHAPTER 1. DESCRIPTION OF MOTION
Figure 1.12: A control volume is occupied by different particles along time.
Theory and Problems
Continuum Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Problems and Exercises 29
PROBLEMS
Problem 1.1 – Justify whether the following statements are true or false. a) If the velocity field is stationary, the acceleration field is also stationary. b) If the velocity field is uniform, the acceleration field is always null.
Solution a) A stationary velocity field implies that the spatial description of velocity does not depend on time, ∂v(x,t) = 0 =⇒ v(x) . ∂t The acceleration is the material derivative of the velocity, therefore ∂v(x,t) a(x,t)= + v(x,t) · ∇v(x,t)=v(x) · ∇v(x) . ∂t The resulting expression does not depend on time. Thus, the statement is true. b) A uniform velocity field implies that the spatial description of velocity does not depend on the spatial coordinates, v(x,t)=⇒ v(t) . The material derivative ofTheory the velocity and results Problems in ∂v(x,t) ∂v(t) a(x,t)= + v(x,t) · ∇v(x,t)= , Continuum Mechanics∂t for Engineers∂t © X. Oliver and C. Agelet de Saracibar where the expression used for the gradient of the velocity field is ∂ ( ) [∇ ( )] = vi t = . v t ij 0 ∂x j Therefore, the statement is false because ∂v(t)/∂t is not necessarily zero.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 30 CHAPTER 1. DESCRIPTION OF MOTION
Problem 1.2 – Calculate the acceleration at time t = 2 in point (1,1,1) of the velocity field not − v ≡ x − z , z e t + e t , 0 T .
Solution Since the velocity field is given in its spatial expression and the acceleration is requested for a point x∗ =(1,1,1)T , the equation of motion is not needed. One can simply apply dv(x,t) ∂v(x,t) a(x,t)= = + v(x,t) · ∇v(x,t) , dt ∂t where ∂v not − ≡ 0 , z e t − e t , 0 T and ∂t ⎡ ⎤ ∂ ⎢ ⎥ ⎡ ⎤ ⎢ ∂ ⎥ ⎢ x ⎥ 100 ⎢ ⎥ ⎢ ⎥ not ⎢ ∂ ⎥ − ⎢ ⎥ ∇v ≡ ⎢ ⎥ x − z , z e t + e t , 0 = ⎣ 000⎦, such that ⎢ ∂y ⎥ ⎢ ⎥ −1 (e t + e−t) 0 ⎣ ∂ ⎦ ∂z v · ∇v not≡ [x − z , 0 , 0]T .
Therefore, the spatial expressionTheory for the and acceleration Problems field is not t −t T Continuuma ≡ Mechanicsx − z , z e − e for, Engineers0 © X. Oliver and C. Agelet de Saracibar and, for the given point at the given instant of time, the acceleration is ∗ not − T a(x = x , t = 2) ≡ 0 , e2 − e 2 , 0 .
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Problem 1.3 – The equation of a certain motion is 1 − 1 − x = X , y = (Y + Z)e t +(Y − Z)e t , z = (Y + Z)e t − (Y − Z)e t . 2 2 Calculate the accelerations that would be observed along time by: a) An observer located in the fixed point (1,1,1). b) An observer traveling with the particle that at time t = 0 occupied position (1,1,1). c) An observer located in point (1,1,1) that measures the accelerations as the difference between velocities at this point per unit of time.
Solution a) The spatial description of the acceleration in point x∗ =(1,1,1) must be obtained, ∗ ∗ ∗ ∂V(X(x ,t),t) a(x = x , t)=A(X(x ,t), t)= . ∂t The material expression of the velocity field is ⎡ ⎤ ⎢ ⎥ ⎢ 0 ⎥ ⎢ ⎥ ∂x(X,t) ⎢ ⎥ ( , )= =⇒ ( , ) not≡ ⎢ 1 − ⎥ . V X t ∂ V X t ⎢ ((Y + Z)e t − (Y − Z)e t) ⎥ t ⎢ 2 ⎥ ⎣ ⎦ 1 ((Y + Z)e t +(Y − Z)e−t) Theory and2 Problems Then, the material description of the acceleration is Continuum Mechanics⎡ for Engineers⎤ © X. Oliver and C. Agelet de Saracibar ⎢ ⎥ ⎢ 0 ⎥ ⎢ ⎥ ∂V(X,t) ⎢ ⎥ ( , )= not≡ ⎢ 1 − ⎥ . A X t ∂ ⎢ ((Y + Z)e t +(Y − Z)e t) ⎥ t ⎢ 2 ⎥ ⎣ ⎦ 1 ((Y + Z)e t − (Y − Z)e−t) 2 Careful observation of the expression obtained reveals that 1 − A = (Y + Z)e t +(Y − Z)e t = y and y 2
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 32 CHAPTER 1. DESCRIPTION OF MOTION