lec.13.pptx basic concepts of kinematics and deformation

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10/3/12 1 13. BASIC CONCEPTS OF KINEMATICS AND DEFORMATION I Main Topics (see chapters 14 and 18 of Means, 1976) A Fundamental principles of conOnuum mechanics B PosiOon vectors and coordinate transformaOon equaOons C Displacement vectors and displacement equaOons D DeformaOon E Homogeneous and inhomogeneous strain 10/3/12 GG303 1 13. BASIC CONCEPTS OF KINEMATICS AND DEFORMATION 10/3/12 GG303 2 hUp://www.geology.wisc.edu/~maher/air/air07.htm TransiOon From ParOcle Mechanics to ConOnuum Mechanics hUp://www.lhup.edu/~dsimanek/scenario/collisionr.jpg Newton’s Pendulum Sheep Mountain AnOcline, Wyoming

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A Fundamental principles of continuum mechanics B Position vectors and coordinate transformation equations C Displacement vectors and displacement equations D Deformation E Homogeneous and inhomogeneous strain

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Page 1: Lec.13.pptx BASIC CONCEPTS OF KINEMATICS AND DEFORMATION

10/3/12  

1  

13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

I  Main  Topics  (see  chapters  14  and  18  of  Means,  1976)    

A  Fundamental  principles  of  conOnuum  mechanics    B  PosiOon  vectors  and  coordinate  transformaOon  equaOons    

C  Displacement  vectors  and  displacement  equaOons    D  DeformaOon  E  Homogeneous  and  inhomogeneous  strain  

10/3/12   GG303   1  

13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

10/3/12   GG303   2  

hUp://www.geology.wisc.edu/~maher/air/air07.htm  

TransiOon  From  ParOcle  Mechanics  to  ConOnuum  Mechanics    

hUp://www.lhup.edu/~dsimanek/scenario/collision-­‐r.jpg  

Newton’s  Pendulum   Sheep  Mountain  AnOcline,  Wyoming  

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13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

II  Fundamental  principles  of  conOnuum  mechanics    A  Number  of  parOcles  is  sufficiently  large  that  the  concept  of  bulk  material  behavior  is  meaningful  

10/3/12   GG303   3  

hUp://www.webelements.com/_media/elements/allotropes/C/C-­‐diamond.jpg  

hUp://www.gemstoneOlsoldout.com/images/diamond-­‐gemstone.jpg  

13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

II  Fundamental  principles  of  conOnuum  mechanics    B  Relates  natural  world  to  the  realm  of  mathemaOcs    

C  DensiOes  of  mass,  momentum,  and  energy  exist  (no  “holes”)    

10/3/12   GG303   4  

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13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

II    Fundamental  principles  of  conOnuum  mechanics    D  Examples  of  

conOnuous  properOes  1  Density  

 So  certain  deriva-ves  have  to  exist  

10/3/12   GG303   5  

ρ = limΔV→0

ΔmΔV

13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

II    Fundamental  principles  of  conOnuum  mechanics    D  Examples  of  conOnuous  properOes  (cont.)  2  Hydraulic  conducOvity  ("permeability")    

E  Scale  maUers  

10/3/12   GG303   6  

Note  that  the  concept  of  derivaOves  becomes  difficult  at  certain  scales  

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13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

II  Fundamental  principles  of  conOnuum  mechanics    

F    Variability    1  Heterogeneity:  

material  property  depends  on  posiOon  

10/3/12   GG303   7  

beg.utexas.edu  

Cathedral  Peak,  CA  

13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

II  Fundamental  principles  of  conOnuum  mechanics    

F    Variability    2  Anisotropy:  

material  property  depends  on  orientaOon  

10/3/12   GG303   8  

hUp://en.wikipedia.org/wiki/File:Gneiss.jpg  

Hand  sample  of  gneiss  

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13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

III  PosiOon  vectors  and  coordinate  transformaOon  equaOons    A  X  =  iniOal  (undeformed)  

posiOon  vector    B  X’  =  final  (current,  or  

deformed)  posiOon  vector  (at  Ome  Δt)    

C  Coordinate  transformaOon  equaOons  1  X’  =  f(X)  

Lagrangian:  final  posiOon  a    funcOon  of  iniOal  posiOon      

2  X  =  g(X’)    Eulerian:  iniOal  posiOon  a  funcOon  of  final  posiOon  

10/3/12   GG303   9  

13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

IV  Displacement  vector  (U)  A  U  =  X’  -­‐  X    

1  x-­‐component:  ux  or  u    2  y-­‐component:  uy  or  v    3  z-­‐component:  uz  or  w    

B  Lagrangian  U(X):  displacement  in  terms  of  iniOal  posiOon  

C  Eulerian  U(X’):  displacement  in  terms  of  final  posiOon  

10/3/12   GG303   10  

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13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

V  DeformaOon:  rigid  body  moOon  +  change  in  size  and/or  shape  A  Rigid  body  translaOon    

1  No  change  in  the  length  of  line  connecOng  any  points    

2  All  points  displaced  by  an  equal  vector  (equal  amount  and  direcOon);  no  displacement  of  points  relaOve  to  one  another    

3  [X']  =  [U]  +[X]    matrix  addiOon  (U  is  a  constant)    

10/3/12   GG303   11  

13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

V  DeformaOon:  rigid  body  moOon  +  change  in  size  and/or  shape  B  Rigid  body  rotaOon    

1  No  change  in  the  length  of  line  connecOng  any  points    

2  All  points  rotated  by  an  equal  amount  about  a  common  axis;  no  angular  displacement  of  points  relaOve  to  one  another    

3  [X']  =  [a][X]  matrix  mulOplicaOon;    rows  in  [a]  are  dir.  cosines!  

10/3/12   GG303   12  

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13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

V  DeformaOon:  rigid  body  moOon  +  change  in  size  and/or  shape  C  Change  in  size  and  /or  

shape  (distorOonal  strain)    1  At  least  some  line  

segments  connecOng  points  in  a  body  change  lengths  (i.e.,  the  relaOve  posiOons  of  points  changes)    

2          is  not  a  constant  throughout  the  body  (i.e.,        varies)  

10/3/12   GG303   13  

u

u

13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

C  Change  in  size  and  /or  shape  (distorOonal  strain)  –  cont.    3  Change  in  linear  dimension  

A  Extension  (or  elongaOon):  ε  

B  Stretch:  S  

C  QuadraOc  elongaOon:  λ  

D  All  are  dimensionless  

10/3/12   GG303   14  

ε = ΔLL0

= L1 − L0L0

S = L1L0

= L0L0

+ L1 − L0L0

= 1+ ε

λ = L1L0

⎛⎝⎜

⎞⎠⎟

2

= S2

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13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

C  Change  in  size  and  /or  shape  (distorOonal  strain)  –  cont.    3  Shear  strain:  γ  a  Describes  change  in  right  in  angle    between  originally  perpendicular  lines  

b          For  small  Ψ,  tanΨΨ  c  Dimensionless  

10/3/12   GG303   15  

γ = tanψ

13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

V  DeformaOon:  rigid  body  moOon  +  change  in  size  and/or  shape  (cont.)  

D  Change  in  volume  (dilaOonal  strain)    

1  DilaOon  (Δ)  

2  Dimensionless    

10/3/12   GG303   16  

Δ = ΔVV0

= V1 −V0V0

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13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

D  Change  in  volume  (dilaOonal  strain)  –  cont.    3  Example  

10/3/12   GG303   17  

Δ = ΔVVo

= V1 −VoVo

V0 =

ao 0 0

0 bo 0

0 0 co

= aoboco

V1 =

a1 0 0

0 b1 0

0 0 c1

=

a0(1+ ε1) 0 0

0 b0(1+ ε2) 0

0 0 c0(1+ ε3)

= a1b1c1

V1 = a0b0c0

(1+ ε1) 0 00 (1+ ε2 ) 00 0 (1+ ε3)

= a0b0c0

S1 0 00 S2 00 0 S3

= a0b0c0S1S2S3

Δ = V1 −V0

V0

= a0b0c0S1S2S3 − a0b0c0

a0b0c0

= S1S2S3 −1 ≈ ε1 + ε2 + ε3 For  small  strains  (ε<<1)  

13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

10/3/12   GG303   18  

VI  Homogeneous  and  inhomogenous  strain  

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13.  BASIC  CONCEPTS  OF  KINEMATICS  AND  DEFORMATION  

10/3/12   GG303   19  

VI  Homogeneous  and  inhomogenous  strain