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Poisson's ratio

In materials science and solid mechanics, Poisson's ratio (nu) is a measure of the Poisson effect, the deformation (expansion or contraction) of a material in directions perpendicular to the specific direction of loading. The value of Poisson's ratio is the negative of the ratio of transverse strain to axial strain. For small values of these changes, is the amount of transversal elongation divided by the amount of axial compression. Most materials have Poisson's ratio values ranging between 0.0 and 0.5. For soft materials,[1] such as rubber, where the bulk modulus is much higher than the shear modulus, Poisson's ratio is near 0.5. For open-cell polymer foams, Poisson's ratio is near zero, since the cells tend to collapse in compression. Many typical solids have Poisson's ratios in the range of 0.2–0.3. The ratio is named after the French mathematician and physicist Siméon Poisson.

Poisson's ratio of a material defines the ratio of transverse strain (x direction) to the axial strain (y direction)

Origin edit

Poisson's ratio is a measure of the Poisson effect, the phenomenon in which a material tends to expand in directions perpendicular to the direction of compression. Conversely, if the material is stretched rather than compressed, it usually tends to contract in the directions transverse to the direction of stretching. It is a common observation when a rubber band is stretched, it becomes noticeably thinner. Again, the Poisson ratio will be the ratio of relative contraction to relative expansion and will have the same value as above. In certain rare cases,[2] a material will actually shrink in the transverse direction when compressed (or expand when stretched) which will yield a negative value of the Poisson ratio.

The Poisson's ratio of a stable, isotropic, linear elastic material must be between −1.0 and +0.5 because of the requirement for Young's modulus, the shear modulus and bulk modulus to have positive values.[3] Most materials have Poisson's ratio values ranging between 0.0 and 0.5. A perfectly incompressible isotropic material deformed elastically at small strains would have a Poisson's ratio of exactly 0.5. Most steels and rigid polymers when used within their design limits (before yield) exhibit values of about 0.3, increasing to 0.5 for post-yield deformation which occurs largely at constant volume.[4] Rubber has a Poisson ratio of nearly 0.5. Cork's Poisson ratio is close to 0, showing very little lateral expansion when compressed and glass is between 0.18 and 0.30. Some materials, e.g. some polymer foams, origami folds,[5][6] and certain cells can exhibit negative Poisson's ratio, and are referred to as auxetic materials. If these auxetic materials are stretched in one direction, they become thicker in the perpendicular direction. In contrast, some anisotropic materials, such as carbon nanotubes, zigzag-based folded sheet materials,[7][8] and honeycomb auxetic metamaterials[9] to name a few, can exhibit one or more Poisson's ratios above 0.5 in certain directions.

Assuming that the material is stretched or compressed in only one direction (the x axis in the diagram below):

 

where

  •   is the resulting Poisson's ratio,
  •   is transverse strain
  •   is axial strain

and positive strain indicates extension and negative strain indicates contraction.

Poisson's ratio from geometry changes edit

Length change edit

 
Figure 1: A cube with sides of length L of an isotropic linearly elastic material subject to tension along the x axis, with a Poisson's ratio of 0.5. The green cube is unstrained, the red is expanded in the x direction by ΔL due to tension, and contracted in the y and z directions by ΔL'.

For a cube stretched in the x-direction (see Figure 1) with a length increase of   in the x direction, and a length decrease of   in the y and z directions, the infinitesimal diagonal strains are given by

 

If Poisson's ratio is constant through deformation, integrating these expressions and using the definition of Poisson's ratio gives

 

Solving and exponentiating, the relationship between   and   is then

 

For very small values of   and  , the first-order approximation yields:

 

Volumetric change edit

The relative change of volume ΔV/V of a cube due to the stretch of the material can now be calculated. Using   and  :

 

Using the above derived relationship between   and  :

 

and for very small values of   and  , the first-order approximation yields:

 

For isotropic materials we can use Lamé's relation[10]

 

where   is bulk modulus and   is Young's modulus.

Width change edit

 
Figure 2: The blue slope represents a simplified formula (the top one in the legend) that works well for modest deformations, ∆L, up to about ±3. The green curve represents a formula better suited for larger deformations.

If a rod with diameter (or width, or thickness) d and length L is subject to tension so that its length will change by ΔL then its diameter d will change by:

 

The above formula is true only in the case of small deformations; if deformations are large then the following (more precise) formula can be used:

 

where

  •   is original diameter
  •   is rod diameter change
  •   is Poisson's ratio
  •   is original length, before stretch
  •   is the change of length.

The value is negative because it decreases with increase of length

Characteristic materials edit

Isotropic edit

For a linear isotropic material subjected only to compressive (i.e. normal) forces, the deformation of a material in the direction of one axis will produce a deformation of the material along the other axis in three dimensions. Thus it is possible to generalize Hooke's Law (for compressive forces) into three dimensions:

 
 
 

where:

  •  ,  , and   are strain in the direction of  ,   and   axis
  •  ,  , and   are stress in the direction of  ,   and   axis
  •   is Young's modulus (the same in all directions:  ,  , and   for isotropic materials)
  •   is Poisson's ratio (the same in all directions:  ,   and   for isotropic materials)

these equations can be all synthesized in the following:

 

In the most general case, also shear stresses will hold as well as normal stresses, and the full generalization of Hooke's law is given by:

 

where   is the Kronecker delta. The Einstein notation is usually adopted:

 

to write the equation simply as:

 

Anisotropic edit

For anisotropic materials, the Poisson ratio depends on the direction of extension and transverse deformation

 
 

Here   is Poisson's ratio,   is Young's modulus,   is unit vector directed along the direction of extension,   is unit vector directed perpendicular to the direction of extension. Poisson's ratio has a different number of special directions depending on the type of anisotropy.[11][12]

Orthotropic edit

Orthotropic materials have three mutually perpendicular planes of symmetry in their material properties. An example is wood, which is most stiff (and strong) along the grain, and less so in the other directions.

Then Hooke's law can be expressed in matrix form as[13][14]

 

where

  •   is the Young's modulus along axis  
  •   is the shear modulus in direction   on the plane whose normal is in direction  
  •   is the Poisson ratio that corresponds to a contraction in direction   when an extension is applied in direction  .

The Poisson ratio of an orthotropic material is different in each direction (x, y and z). However, the symmetry of the stress and strain tensors implies that not all the six Poisson's ratios in the equation are independent. There are only nine independent material properties: three elastic moduli, three shear moduli, and three Poisson's ratios. The remaining three Poisson's ratios can be obtained from the relations

 

From the above relations we can see that if   then  . The larger Poisson's ratio (in this case  ) is called the major Poisson's ratio while the smaller one (in this case  ) is called the minor Poisson's ratio. We can find similar relations between the other Poisson's ratios.

Transversely isotropic edit

Transversely isotropic materials have a plane of isotropy in which the elastic properties are isotropic. If we assume that this plane of isotropy is  , then Hooke's law takes the form[15]

 

where we have used the plane of isotropy   to reduce the number of constants, i.e.,  .

The symmetry of the stress and strain tensors implies that

 

This leaves us with six independent constants  . However, transverse isotropy gives rise to a further constraint between   and   which is

 

Therefore, there are five independent elastic material properties two of which are Poisson's ratios. For the assumed plane of symmetry, the larger of   and   is the major Poisson's ratio. The other major and minor Poisson's ratios are equal.

Poisson's ratio values for different materials edit

 
Influences of selected glass component additions on Poisson's ratio of a specific base glass.[16]
Material Poisson's ratio
rubber 0.4999[17]
gold 0.42–0.44
saturated clay 0.40–0.49
magnesium 0.252–0.289
titanium 0.265–0.34
copper 0.33
aluminium-alloy 0.32
clay 0.30–0.45
stainless steel 0.30–0.31
steel 0.27–0.30
cast iron 0.21–0.26
sand 0.20–0.455
concrete 0.1–0.2
glass 0.18–0.3
metallic glasses 0.276–0.409[18]
foam 0.10–0.50
cork 0.0
Material Plane of symmetry            
Nomex honeycomb core  , ribbon in   direction 0.49 0.69 0.01 2.75 3.88 0.01
glass fiber-epoxy resin   0.29 0.32 0.06 0.06 0.32

Negative Poisson's ratio materials edit

Some materials known as auxetic materials display a negative Poisson's ratio. When subjected to positive strain in a longitudinal axis, the transverse strain in the material will actually be positive (i.e. it would increase the cross sectional area). For these materials, it is usually due to uniquely oriented, hinged molecular bonds. In order for these bonds to stretch in the longitudinal direction, the hinges must ‘open’ in the transverse direction, effectively exhibiting a positive strain.[19] This can also be done in a structured way and lead to new aspects in material design as for mechanical metamaterials.

Studies have shown that certain solid wood types display negative Poisson's ratio exclusively during a compression creep test.[20][21] Initially, the compression creep test shows positive Poisson's ratios, but gradually decreases until it reaches negative values. Consequently, this also shows that Poisson's ratio for wood is time-dependent during constant loading, meaning that the strain in the axial and transverse direction do not increase in the same rate.

Media with engineered microstructure may exhibit negative Poisson's ratio. In a simple case auxeticity is obtained removing material and creating a periodic porous media.[22] Lattices can reach lower values of Poisson's ratio,[23] which can be indefinitely close to the limiting value −1 in the isotropic case.[24]

More than three hundred crystalline materials have negative Poisson's ratio.[25][26][27] For example, Li, Na, K, Cu, Rb, Ag, Fe, Ni, Co, Cs, Au, Be, Ca, Zn Sr, Sb, MoS  and other.

Poisson function edit

At finite strains, the relationship between the transverse and axial strains   and   is typically not well described by the Poisson ratio. In fact, the Poisson ratio is often considered a function of the applied strain in the large strain regime. In such instances, the Poisson ratio is replaced by the Poisson function, for which there are several competing definitions.[28] Defining the transverse stretch   and axial stretch  , where the transverse stretch is a function of the axial stretch (i.e.,  ) the most common are the Hencky, Biot, Green, and Almansi functions

 

Applications of Poisson's effect edit

One area in which Poisson's effect has a considerable influence is in pressurized pipe flow. When the air or liquid inside a pipe is highly pressurized it exerts a uniform force on the inside of the pipe, resulting in a hoop stress within the pipe material. Due to Poisson's effect, this hoop stress will cause the pipe to increase in diameter and slightly decrease in length. The decrease in length, in particular, can have a noticeable effect upon the pipe joints, as the effect will accumulate for each section of pipe joined in series. A restrained joint may be pulled apart or otherwise prone to failure.[citation needed]

Another area of application for Poisson's effect is in the realm of structural geology. Rocks, like most materials, are subject to Poisson's effect while under stress. In a geological timescale, excessive erosion or sedimentation of Earth's crust can either create or remove large vertical stresses upon the underlying rock. This rock will expand or contract in the vertical direction as a direct result of the applied stress, and it will also deform in the horizontal direction as a result of Poisson's effect. This change in strain in the horizontal direction can affect or form joints and dormant stresses in the rock.[29]

Although cork was historically chosen to seal wine bottle for other reasons (including its inert nature, impermeability, flexibility, sealing ability, and resilience),[30] cork's Poisson's ratio of zero provides another advantage. As the cork is inserted into the bottle, the upper part which is not yet inserted does not expand in diameter as it is compressed axially. The force needed to insert a cork into a bottle arises only from the friction between the cork and the bottle due to the radial compression of the cork. If the stopper were made of rubber, for example, (with a Poisson's ratio of about 1/2), there would be a relatively large additional force required to overcome the radial expansion of the upper part of the rubber stopper.

Most car mechanics are aware that it is hard to pull a rubber hose (e.g. a coolant hose) off a metal pipe stub, as the tension of pulling causes the diameter of the hose to shrink, gripping the stub tightly. (This is the same effect as shown in a Chinese finger trap.) Hoses can more easily be pushed off stubs instead using a wide flat blade.

See also edit

References edit

  1. ^ For soft materials, the bulk modulus (K) is typically large compared to the shear modulus (G) so that they can be regarded as incompressible, since it is easier to change shape than to compress. This results in the Young's modulus (E) being   and hence  .Jastrzebski, D. (1959). Nature and Properties of Engineering Materials (Wiley International ed.). John Wiley & Sons, Inc.
  2. ^ Lakes, R. and Wojciechowski, K.W., 2008. Negative compressibility, negative Poisson's ratio, and stability. Physica Status Solidi B, 245(3), pp.545-551.
  3. ^ Gercek, H. (January 2007). "Poisson's ratio values for rocks". International Journal of Rock Mechanics and Mining Sciences. 44 (1): 1–13. Bibcode:2007IJRMM..44....1G. doi:10.1016/j.ijrmms.2006.04.011.
  4. ^ Park, RJT. Seismic Performance of Steel-Encased Concrete Piles
  5. ^ Mark, Schenk (2011). Folded Shell Structures, PhD Thesis (PDF). University of Cambridge, Clare College.
  6. ^ Wei, Z. Y.; Guo, Z. V.; Dudte, L.; Liang, H. Y.; Mahadevan, L. (2013-05-21). "Geometric Mechanics of Periodic Pleated Origami" (PDF). Physical Review Letters. 110 (21): 215501. arXiv:1211.6396. Bibcode:2013PhRvL.110u5501W. doi:10.1103/PhysRevLett.110.215501. PMID 23745895. S2CID 9145953.
  7. ^ Eidini, Maryam; Paulino, Glaucio H. (2015). "Unraveling metamaterial properties in zigzag-base folded sheets". Science Advances. 1 (8): e1500224. arXiv:1502.05977. Bibcode:2015SciA....1E0224E. doi:10.1126/sciadv.1500224. ISSN 2375-2548. PMC 4643767. PMID 26601253.
  8. ^ Eidini, Maryam (2016). "Zigzag-base folded sheet cellular mechanical metamaterials". Extreme Mechanics Letters. 6: 96–102. arXiv:1509.08104. doi:10.1016/j.eml.2015.12.006. S2CID 118424595.
  9. ^ Mousanezhad, Davood; Babaee, Sahab; Ebrahimi, Hamid; Ghosh, Ranajay; Hamouda, Abdelmagid Salem; Bertoldi, Katia; Vaziri, Ashkan (2015-12-16). "Hierarchical honeycomb auxetic metamaterials". Scientific Reports. 5: 18306. Bibcode:2015NatSR...518306M. doi:10.1038/srep18306. ISSN 2045-2322. PMC 4680941. PMID 26670417.
  10. ^ Mott, P. H.; Roland, C. M. (3 April 2012). "Limits to Poisson's ratio in isotropic materials—general result for arbitrary deformation". Physica Scripta. Chemistry Division, Naval Research Laboratory. 87 (5): 055404. arXiv:1204.3859. doi:10.1088/0031-8949/87/05/055404. S2CID 55920779.
  11. ^ Epishin, A.I.; Lisovenko, D.S. (2016). "Extreme values of Poisson's ratio of cubic crystals". Technical Physics. 61 (10): 1516–1524. Bibcode:2016JTePh..61.1516E. doi:10.1016/j.mechmat.2019.03.017. S2CID 140493258.
  12. ^ Gorodtsov, V.A.; Lisovenko, D.S. (2019). "Extreme values of Young's modulus and Poisson's ratio of hexagonal crystals". Mechanics of Materials. 134: 1–8. doi:10.1016/j.mechmat.2019.03.017. S2CID 140493258.
  13. ^ Boresi, A. P, Schmidt, R. J. and Sidebottom, O. M., 1993, Advanced Mechanics of Materials, Wiley.
  14. ^ Lekhnitskii, S. G. (1981). Theory of elasticity of an anisotropic elastic body. Mir Publishing. p. 36.
  15. ^ Tan, S. C., 1994, Stress Concentrations in Laminated Composites, Technomic Publishing Company, Lancaster, PA.
  16. ^ Fluegel, Alexander. "Poisson's Ratio Calculation for Glasses". www.glassproperties.com. from the original on 23 October 2017. Retrieved 28 April 2018.
  17. ^ P. H. Mott; C. M. Roland (20 October 2009). "Limits to Poisson's ratio in isotropic materials" (PDF). Physical Review B. 80 (13): 132104. arXiv:0909.4697. Bibcode:2009PhRvB..80m2104M. doi:10.1103/PhysRevB.80.132104. (PDF) from the original on 2014-10-31. Retrieved 2014-09-24.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  18. ^ Journal of Applied Physics 110, 053521 (2011)
  19. ^ Lakes, Rod. "Negative Poisson's ratio". silver.neep.wisc.edu. from the original on 16 February 2018. Retrieved 28 April 2018.
  20. ^ Ozyhar, Tomasz; Hering, Stefan; Niemz, Peter (March 2013). "Viscoelastic characterization of wood: Time dependence of the orthotropic compliance in tension and compression". Journal of Rheology. 57 (2): 699–717. Bibcode:2013JRheo..57..699O. doi:10.1122/1.4790170. ISSN 0148-6055.
  21. ^ Jiang, Jiali; Erik Valentine, Bachtiar; Lu, Jianxiong; Niemz, Peter (2016-11-01). "Time dependence of the orthotropic compression Young's moduli and Poisson's ratios of Chinese fir wood" (PDF). Holzforschung. 70 (11): 1093–1101. doi:10.1515/hf-2016-0001. hdl:20.500.11850/122097. ISSN 1437-434X. S2CID 137799672.
  22. ^ Carta, Giorgio; Brun, Michele; Baldi, Antonio (2016). "Design of a porous material with isotropic negative Poisson's ratio". Mechanics of Materials. 97: 67–75. doi:10.1016/j.mechmat.2016.02.012.
  23. ^ Cabras, Luigi; Brun, Michele (2016). "A class of auxetic three-dimensional lattices". Journal of the Mechanics and Physics of Solids. 91: 56–72. arXiv:1506.04919. Bibcode:2016JMPSo..91...56C. doi:10.1016/j.jmps.2016.02.010. S2CID 85547530.
  24. ^ Cabras, Luigi; Brun, Michele (2014). "Auxetic two-dimensional lattices with Poisson's ratio arbitrarily close to -1". Proceedings of the Royal Society A. 470 (2172): 20140538. arXiv:1407.5679. Bibcode:2014RSPSA.47040538C. doi:10.1098/rspa.2014.0538. S2CID 119321604.
  25. ^ Goldstein, R.V.; Gorodtsov, V.A.; Lisovenko, D.S. (2013). "Classification of cubic auxetics". Physica Status Solidi B. 250 (10): 2038–2043. Bibcode:2013PSSBR.250.2038G. doi:10.1002/pssb.201384233. S2CID 117802510.
  26. ^ Goldstein, R.V.; Gorodtsov, V.A.; Lisovenko, D.S. (2011). "Variability of elastic properties of hexagonal auxetics". Doklady Physics. 56 (12): 602–605. doi:10.1134/S1028335811120019. S2CID 120998323.
  27. ^ Goldstein, R.V.; Gorodtsov, V.A.; Lisovenko, D.S.; Volkov, M.A. (2015). "Auxetics among 6-constant tetragonal crystals". Letters on Materials. 5 (4): 409–413. doi:10.22226/2410-3535-2015-4-409-413.
  28. ^ Mihai, L. A.; Goriely, A. (2017-11-03). "How to characterize a nonlinear elastic material? A review on nonlinear constitutive parameters in isotropic finite elasticity". Proceedings of the Royal Society A. 473 (2207): 20170607. Bibcode:2017RSPSA.47370607M. doi:10.1098/rspa.2017.0607. PMC 5719638. PMID 29225507.
  29. ^ "Lecture Notes in Structural Geology – Effective Stress". Retrieved 2019-07-03.
  30. ^ Silva, et al. "Cork: properties, capabilities and applications" 2017-08-09 at the Wayback Machine, Retrieved May 4, 2017

External links edit

  • Meaning of Poisson's ratio
  • Negative Poisson's ratio materials
  • More on negative Poisson's ratio materials (auxetic) 2018-02-08 at the Wayback Machine
Conversion formulae
Homogeneous isotropic linear elastic materials have their elastic properties uniquely determined by any two moduli among these; thus, given any two, any other of the elastic moduli can be calculated according to these formulas, provided both for 3D materials (first part of the table) and for 2D materials (second part).
3D formulae             Notes
         
         
         
         
         
           
         
         
           

There are two valid solutions.
The plus sign leads to  .

The minus sign leads to  .

         
          Cannot be used when  
         
         
         
         
2D formulae             Notes
         
         
         
         
         
         
         
          Cannot be used when  
         
         



poisson, ratio, materials, science, solid, mechanics, displaystyle, measure, poisson, effect, deformation, expansion, contraction, material, directions, perpendicular, specific, direction, loading, value, negative, ratio, transverse, strain, axial, strain, sma. In materials science and solid mechanics Poisson s ratio n displaystyle nu nu is a measure of the Poisson effect the deformation expansion or contraction of a material in directions perpendicular to the specific direction of loading The value of Poisson s ratio is the negative of the ratio of transverse strain to axial strain For small values of these changes n displaystyle nu is the amount of transversal elongation divided by the amount of axial compression Most materials have Poisson s ratio values ranging between 0 0 and 0 5 For soft materials 1 such as rubber where the bulk modulus is much higher than the shear modulus Poisson s ratio is near 0 5 For open cell polymer foams Poisson s ratio is near zero since the cells tend to collapse in compression Many typical solids have Poisson s ratios in the range of 0 2 0 3 The ratio is named after the French mathematician and physicist Simeon Poisson Poisson s ratio of a material defines the ratio of transverse strain x direction to the axial strain y direction Contents 1 Origin 2 Poisson s ratio from geometry changes 2 1 Length change 2 2 Volumetric change 2 3 Width change 3 Characteristic materials 3 1 Isotropic 3 2 Anisotropic 3 3 Orthotropic 3 4 Transversely isotropic 4 Poisson s ratio values for different materials 4 1 Negative Poisson s ratio materials 5 Poisson function 6 Applications of Poisson s effect 7 See also 8 References 9 External linksOrigin editPoisson s ratio is a measure of the Poisson effect the phenomenon in which a material tends to expand in directions perpendicular to the direction of compression Conversely if the material is stretched rather than compressed it usually tends to contract in the directions transverse to the direction of stretching It is a common observation when a rubber band is stretched it becomes noticeably thinner Again the Poisson ratio will be the ratio of relative contraction to relative expansion and will have the same value as above In certain rare cases 2 a material will actually shrink in the transverse direction when compressed or expand when stretched which will yield a negative value of the Poisson ratio The Poisson s ratio of a stable isotropic linear elastic material must be between 1 0 and 0 5 because of the requirement for Young s modulus the shear modulus and bulk modulus to have positive values 3 Most materials have Poisson s ratio values ranging between 0 0 and 0 5 A perfectly incompressible isotropic material deformed elastically at small strains would have a Poisson s ratio of exactly 0 5 Most steels and rigid polymers when used within their design limits before yield exhibit values of about 0 3 increasing to 0 5 for post yield deformation which occurs largely at constant volume 4 Rubber has a Poisson ratio of nearly 0 5 Cork s Poisson ratio is close to 0 showing very little lateral expansion when compressed and glass is between 0 18 and 0 30 Some materials e g some polymer foams origami folds 5 6 and certain cells can exhibit negative Poisson s ratio and are referred to as auxetic materials If these auxetic materials are stretched in one direction they become thicker in the perpendicular direction In contrast some anisotropic materials such as carbon nanotubes zigzag based folded sheet materials 7 8 and honeycomb auxetic metamaterials 9 to name a few can exhibit one or more Poisson s ratios above 0 5 in certain directions Assuming that the material is stretched or compressed in only one direction the x axis in the diagram below n d e t r a n s d e a x i a l d e y d e x d e z d e x displaystyle nu frac d varepsilon mathrm trans d varepsilon mathrm axial frac d varepsilon mathrm y d varepsilon mathrm x frac d varepsilon mathrm z d varepsilon mathrm x nbsp where n displaystyle nu nbsp is the resulting Poisson s ratio e t r a n s displaystyle varepsilon mathrm trans nbsp is transverse strain e a x i a l displaystyle varepsilon mathrm axial nbsp is axial strainand positive strain indicates extension and negative strain indicates contraction Poisson s ratio from geometry changes editLength change edit nbsp Figure 1 A cube with sides of length L of an isotropic linearly elastic material subject to tension along the x axis with a Poisson s ratio of 0 5 The green cube is unstrained the red is expanded in the x direction by DL due to tension and contracted in the y and z directions by DL For a cube stretched in the x direction see Figure 1 with a length increase of D L displaystyle Delta L nbsp in the x direction and a length decrease of D L displaystyle Delta L nbsp in the y and z directions the infinitesimal diagonal strains are given by d e x d x x d e y d y y d e z d z z displaystyle d varepsilon x frac dx x qquad d varepsilon y frac dy y qquad d varepsilon z frac dz z nbsp If Poisson s ratio is constant through deformation integrating these expressions and using the definition of Poisson s ratio gives n L L D L d x x L L D L d y y L L D L d z z displaystyle nu int L L Delta L frac dx x int L L Delta L frac dy y int L L Delta L frac dz z nbsp Solving and exponentiating the relationship between D L displaystyle Delta L nbsp and D L displaystyle Delta L nbsp is then 1 D L L n 1 D L L displaystyle left 1 frac Delta L L right nu 1 frac Delta L L nbsp For very small values of D L displaystyle Delta L nbsp and D L displaystyle Delta L nbsp the first order approximation yields n D L D L displaystyle nu approx frac Delta L Delta L nbsp Volumetric change edit The relative change of volume DV V of a cube due to the stretch of the material can now be calculated Using V L 3 displaystyle V L 3 nbsp and V D V L D L L D L 2 displaystyle V Delta V L Delta L left L Delta L right 2 nbsp D V V 1 D L L 1 D L L 2 1 displaystyle frac Delta V V left 1 frac Delta L L right left 1 frac Delta L L right 2 1 nbsp Using the above derived relationship between D L displaystyle Delta L nbsp and D L displaystyle Delta L nbsp D V V 1 D L L 1 2 n 1 displaystyle frac Delta V V left 1 frac Delta L L right 1 2 nu 1 nbsp and for very small values of D L displaystyle Delta L nbsp and D L displaystyle Delta L nbsp the first order approximation yields D V V 1 2 n D L L displaystyle frac Delta V V approx 1 2 nu frac Delta L L nbsp For isotropic materials we can use Lame s relation 10 n 1 2 E 6 K displaystyle nu approx frac 1 2 frac E 6K nbsp where K displaystyle K nbsp is bulk modulus and E displaystyle E nbsp is Young s modulus Width change edit nbsp Figure 2 The blue slope represents a simplified formula the top one in the legend that works well for modest deformations L up to about 3 The green curve represents a formula better suited for larger deformations If a rod with diameter or width or thickness d and length L is subject to tension so that its length will change by DL then its diameter d will change by D d d n D L L displaystyle Delta d over d nu frac Delta L L nbsp The above formula is true only in the case of small deformations if deformations are large then the following more precise formula can be used D d d 1 1 D L L n displaystyle Delta d d left 1 left 1 frac Delta L L right nu right nbsp where d displaystyle d nbsp is original diameter D d displaystyle Delta d nbsp is rod diameter change n displaystyle nu nbsp is Poisson s ratio L displaystyle L nbsp is original length before stretch D L displaystyle Delta L nbsp is the change of length The value is negative because it decreases with increase of lengthCharacteristic materials editIsotropic edit For a linear isotropic material subjected only to compressive i e normal forces the deformation of a material in the direction of one axis will produce a deformation of the material along the other axis in three dimensions Thus it is possible to generalize Hooke s Law for compressive forces into three dimensions e x x 1 E s x x n s y y s z z displaystyle varepsilon xx frac 1 E left sigma xx nu left sigma yy sigma zz right right nbsp e y y 1 E s y y n s x x s z z displaystyle varepsilon yy frac 1 E left sigma yy nu left sigma xx sigma zz right right nbsp e z z 1 E s z z n s x x s y y displaystyle varepsilon zz frac 1 E left sigma zz nu left sigma xx sigma yy right right nbsp where e x x displaystyle varepsilon xx nbsp e y y displaystyle varepsilon yy nbsp and e z z displaystyle varepsilon zz nbsp are strain in the direction of x displaystyle x nbsp y displaystyle y nbsp and z displaystyle z nbsp axis s x x displaystyle sigma xx nbsp s y y displaystyle sigma yy nbsp and s z z displaystyle sigma zz nbsp are stress in the direction of x displaystyle x nbsp y displaystyle y nbsp and z displaystyle z nbsp axis E displaystyle E nbsp is Young s modulus the same in all directions x displaystyle x nbsp y displaystyle y nbsp and z displaystyle z nbsp for isotropic materials n displaystyle nu nbsp is Poisson s ratio the same in all directions x displaystyle x nbsp y displaystyle y nbsp and z displaystyle z nbsp for isotropic materials these equations can be all synthesized in the following e i i 1 E s i i 1 n n k s k k displaystyle varepsilon ii frac 1 E left sigma ii 1 nu nu sum k sigma kk right nbsp In the most general case also shear stresses will hold as well as normal stresses and the full generalization of Hooke s law is given by e i j 1 E s i j 1 n n d i j k s k k displaystyle varepsilon ij frac 1 E left sigma ij 1 nu nu delta ij sum k sigma kk right nbsp where d i j displaystyle delta ij nbsp is the Kronecker delta The Einstein notation is usually adopted s k k l d k l s k l displaystyle sigma kk equiv sum l delta kl sigma kl nbsp to write the equation simply as e i j 1 E s i j 1 n n d i j s k k displaystyle varepsilon ij frac 1 E left sigma ij 1 nu nu delta ij sigma kk right nbsp Anisotropic edit For anisotropic materials the Poisson ratio depends on the direction of extension and transverse deformation n n m E n s i j a b n i n j m a m b displaystyle nu mathbf n mathbf m E left mathbf n right s ij alpha beta n i n j m alpha m beta nbsp E 1 n s i j a b n i n j n a n b displaystyle E 1 mathbf n s ij alpha beta n i n j n alpha n beta nbsp Here n displaystyle nu nbsp is Poisson s ratio E displaystyle E nbsp is Young s modulus n displaystyle mathbf n nbsp is unit vector directed along the direction of extension m displaystyle mathbf m nbsp is unit vector directed perpendicular to the direction of extension Poisson s ratio has a different number of special directions depending on the type of anisotropy 11 12 Orthotropic edit Main article Orthotropic material Orthotropic materials have three mutually perpendicular planes of symmetry in their material properties An example is wood which is most stiff and strong along the grain and less so in the other directions Then Hooke s law can be expressed in matrix form as 13 14 ϵ x x ϵ y y ϵ z z 2 ϵ y z 2 ϵ z x 2 ϵ x y 1 E x n y x E y n z x E z 0 0 0 n x y E x 1 E y n z y E z 0 0 0 n x z E x n y z E y 1 E z 0 0 0 0 0 0 1 G y z 0 0 0 0 0 0 1 G z x 0 0 0 0 0 0 1 G x y s x x s y y s z z s y z s z x s x y displaystyle begin bmatrix epsilon xx epsilon yy epsilon zz 2 epsilon yz 2 epsilon zx 2 epsilon xy end bmatrix begin bmatrix tfrac 1 E x amp tfrac nu yx E y amp tfrac nu zx E z amp 0 amp 0 amp 0 tfrac nu xy E x amp tfrac 1 E y amp tfrac nu zy E z amp 0 amp 0 amp 0 tfrac nu xz E x amp tfrac nu yz E y amp tfrac 1 E z amp 0 amp 0 amp 0 0 amp 0 amp 0 amp tfrac 1 G yz amp 0 amp 0 0 amp 0 amp 0 amp 0 amp tfrac 1 G zx amp 0 0 amp 0 amp 0 amp 0 amp 0 amp tfrac 1 G xy end bmatrix begin bmatrix sigma xx sigma yy sigma zz sigma yz sigma zx sigma xy end bmatrix nbsp where E i displaystyle E i nbsp is the Young s modulus along axis i displaystyle i nbsp G i j displaystyle G ij nbsp is the shear modulus in direction j displaystyle j nbsp on the plane whose normal is in direction i displaystyle i nbsp n i j displaystyle nu ij nbsp is the Poisson ratio that corresponds to a contraction in direction j displaystyle j nbsp when an extension is applied in direction i displaystyle i nbsp The Poisson ratio of an orthotropic material is different in each direction x y and z However the symmetry of the stress and strain tensors implies that not all the six Poisson s ratios in the equation are independent There are only nine independent material properties three elastic moduli three shear moduli and three Poisson s ratios The remaining three Poisson s ratios can be obtained from the relations n y x E y n x y E x n z x E z n x z E x n y z E y n z y E z displaystyle frac nu yx E y frac nu xy E x qquad frac nu zx E z frac nu xz E x qquad frac nu yz E y frac nu zy E z nbsp From the above relations we can see that if E x gt E y displaystyle E x gt E y nbsp then n x y gt n y x displaystyle nu xy gt nu yx nbsp The larger Poisson s ratio in this case n x y displaystyle nu xy nbsp is called the major Poisson s ratio while the smaller one in this case n y x displaystyle nu yx nbsp is called the minor Poisson s ratio We can find similar relations between the other Poisson s ratios Transversely isotropic edit Transversely isotropic materials have a plane of isotropy in which the elastic properties are isotropic If we assume that this plane of isotropy is y z displaystyle y z nbsp then Hooke s law takes the form 15 ϵ x x ϵ y y ϵ z z 2 ϵ y z 2 ϵ z x 2 ϵ x y 1 E x n y x E y n z x E z 0 0 0 n x y E x 1 E y n z y E z 0 0 0 n x z E x n y z E y 1 E z 0 0 0 0 0 0 1 G y z 0 0 0 0 0 0 1 G z x 0 0 0 0 0 0 1 G x y s x x s y y s z z s y z s z x s x y displaystyle begin bmatrix epsilon xx epsilon yy epsilon zz 2 epsilon yz 2 epsilon zx 2 epsilon xy end bmatrix begin bmatrix tfrac 1 E x amp tfrac nu yx E y amp tfrac nu zx E z amp 0 amp 0 amp 0 tfrac nu xy E x amp tfrac 1 E y amp tfrac nu zy E z amp 0 amp 0 amp 0 tfrac nu xz E x amp tfrac nu yz E y amp tfrac 1 E z amp 0 amp 0 amp 0 0 amp 0 amp 0 amp tfrac 1 G rm yz amp 0 amp 0 0 amp 0 amp 0 amp 0 amp tfrac 1 G rm zx amp 0 0 amp 0 amp 0 amp 0 amp 0 amp tfrac 1 G rm xy end bmatrix begin bmatrix sigma xx sigma yy sigma zz sigma yz sigma zx sigma xy end bmatrix nbsp where we have used the plane of isotropy y z displaystyle y z nbsp to reduce the number of constants i e E y E z n x y n x z n y x n z x displaystyle E y E z nu xy nu xz nu yx nu zx nbsp The symmetry of the stress and strain tensors implies that n x y E x n y x E y n y z n z y displaystyle frac nu xy E x frac nu yx E y nu yz nu zy nbsp This leaves us with six independent constants E x E y G x y G y z n x y n y z displaystyle E x E y G xy G yz nu xy nu yz nbsp However transverse isotropy gives rise to a further constraint between G y z displaystyle G yz nbsp and E y n y z displaystyle E y nu yz nbsp which is G y z E y 2 1 n y z displaystyle G yz frac E y 2 1 nu yz nbsp Therefore there are five independent elastic material properties two of which are Poisson s ratios For the assumed plane of symmetry the larger of n x y displaystyle nu xy nbsp and n y x displaystyle nu yx nbsp is the major Poisson s ratio The other major and minor Poisson s ratios are equal Poisson s ratio values for different materials edit nbsp Influences of selected glass component additions on Poisson s ratio of a specific base glass 16 Material Poisson s ratiorubber 0 4999 17 gold 0 42 0 44saturated clay 0 40 0 49magnesium 0 252 0 289titanium 0 265 0 34copper 0 33aluminium alloy 0 32clay 0 30 0 45stainless steel 0 30 0 31steel 0 27 0 30cast iron 0 21 0 26sand 0 20 0 455concrete 0 1 0 2glass 0 18 0 3metallic glasses 0 276 0 409 18 foam 0 10 0 50cork 0 0Material Plane of symmetry n x y displaystyle nu rm xy nbsp n y x displaystyle nu rm yx nbsp n y z displaystyle nu rm yz nbsp n z y displaystyle nu rm zy nbsp n z x displaystyle nu rm zx nbsp n x z displaystyle nu rm xz nbsp Nomex honeycomb core x y displaystyle x text y nbsp ribbon in x displaystyle x nbsp direction 0 49 0 69 0 01 2 75 3 88 0 01glass fiber epoxy resin x y displaystyle x text y nbsp 0 29 0 32 0 06 0 06 0 32Negative Poisson s ratio materials edit Some materials known as auxetic materials display a negative Poisson s ratio When subjected to positive strain in a longitudinal axis the transverse strain in the material will actually be positive i e it would increase the cross sectional area For these materials it is usually due to uniquely oriented hinged molecular bonds In order for these bonds to stretch in the longitudinal direction the hinges must open in the transverse direction effectively exhibiting a positive strain 19 This can also be done in a structured way and lead to new aspects in material design as for mechanical metamaterials Studies have shown that certain solid wood types display negative Poisson s ratio exclusively during a compression creep test 20 21 Initially the compression creep test shows positive Poisson s ratios but gradually decreases until it reaches negative values Consequently this also shows that Poisson s ratio for wood is time dependent during constant loading meaning that the strain in the axial and transverse direction do not increase in the same rate Media with engineered microstructure may exhibit negative Poisson s ratio In a simple case auxeticity is obtained removing material and creating a periodic porous media 22 Lattices can reach lower values of Poisson s ratio 23 which can be indefinitely close to the limiting value 1 in the isotropic case 24 More than three hundred crystalline materials have negative Poisson s ratio 25 26 27 For example Li Na K Cu Rb Ag Fe Ni Co Cs Au Be Ca Zn Sr Sb MoS2 displaystyle 2 nbsp and other Poisson function editAt finite strains the relationship between the transverse and axial strains e trans displaystyle varepsilon text trans nbsp and e axial displaystyle varepsilon text axial nbsp is typically not well described by the Poisson ratio In fact the Poisson ratio is often considered a function of the applied strain in the large strain regime In such instances the Poisson ratio is replaced by the Poisson function for which there are several competing definitions 28 Defining the transverse stretch l trans e trans 1 displaystyle lambda text trans varepsilon text trans 1 nbsp and axial stretch l axial e axial 1 displaystyle lambda text axial varepsilon text axial 1 nbsp where the transverse stretch is a function of the axial stretch i e l trans l trans l axial displaystyle lambda text trans lambda text trans lambda text axial nbsp the most common are the Hencky Biot Green and Almansi functions n Hencky ln l trans ln l axial n Biot 1 l trans l axial 1 n Green 1 l trans 2 l axial 2 1 n Almansi l trans 2 1 1 l axial 2 displaystyle begin aligned nu text Hencky amp frac ln lambda text trans ln lambda text axial 6pt nu text Biot amp frac 1 lambda text trans lambda text axial 1 6pt nu text Green amp frac 1 lambda text trans 2 lambda text axial 2 1 6pt nu text Almansi amp frac lambda text trans 2 1 1 lambda text axial 2 end aligned nbsp Applications of Poisson s effect editOne area in which Poisson s effect has a considerable influence is in pressurized pipe flow When the air or liquid inside a pipe is highly pressurized it exerts a uniform force on the inside of the pipe resulting in a hoop stress within the pipe material Due to Poisson s effect this hoop stress will cause the pipe to increase in diameter and slightly decrease in length The decrease in length in particular can have a noticeable effect upon the pipe joints as the effect will accumulate for each section of pipe joined in series A restrained joint may be pulled apart or otherwise prone to failure citation needed Another area of application for Poisson s effect is in the realm of structural geology Rocks like most materials are subject to Poisson s effect while under stress In a geological timescale excessive erosion or sedimentation of Earth s crust can either create or remove large vertical stresses upon the underlying rock This rock will expand or contract in the vertical direction as a direct result of the applied stress and it will also deform in the horizontal direction as a result of Poisson s effect This change in strain in the horizontal direction can affect or form joints and dormant stresses in the rock 29 Although cork was historically chosen to seal wine bottle for other reasons including its inert nature impermeability flexibility sealing ability and resilience 30 cork s Poisson s ratio of zero provides another advantage As the cork is inserted into the bottle the upper part which is not yet inserted does not expand in diameter as it is compressed axially The force needed to insert a cork into a bottle arises only from the friction between the cork and the bottle due to the radial compression of the cork If the stopper were made of rubber for example with a Poisson s ratio of about 1 2 there would be a relatively large additional force required to overcome the radial expansion of the upper part of the rubber stopper Most car mechanics are aware that it is hard to pull a rubber hose e g a coolant hose off a metal pipe stub as the tension of pulling causes the diameter of the hose to shrink gripping the stub tightly This is the same effect as shown in a Chinese finger trap Hoses can more easily be pushed off stubs instead using a wide flat blade See also editLinear elasticity Hooke s law Impulse excitation technique Orthotropic material Shear modulus Young s modulus Coefficient of thermal expansionReferences edit For soft materials the bulk modulus K is typically large compared to the shear modulus G so that they can be regarded as incompressible since it is easier to change shape than to compress This results in the Young s modulus E being E 3 G displaystyle E 3G nbsp and hence n 0 5 displaystyle nu 0 5 nbsp Jastrzebski D 1959 Nature and Properties of Engineering Materials Wiley International ed John Wiley amp Sons Inc Lakes R and Wojciechowski K W 2008 Negative compressibility negative Poisson s ratio and stability Physica Status Solidi B 245 3 pp 545 551 Gercek H January 2007 Poisson s ratio values for rocks International Journal of Rock Mechanics and Mining Sciences 44 1 1 13 Bibcode 2007IJRMM 44 1G doi 10 1016 j ijrmms 2006 04 011 Park RJT Seismic Performance of Steel Encased Concrete Piles Mark Schenk 2011 Folded Shell Structures PhD Thesis PDF University of Cambridge Clare College Wei Z Y Guo Z V Dudte L Liang H Y Mahadevan L 2013 05 21 Geometric Mechanics of Periodic Pleated Origami PDF Physical Review Letters 110 21 215501 arXiv 1211 6396 Bibcode 2013PhRvL 110u5501W doi 10 1103 PhysRevLett 110 215501 PMID 23745895 S2CID 9145953 Eidini Maryam Paulino Glaucio H 2015 Unraveling metamaterial properties in zigzag base folded sheets Science Advances 1 8 e1500224 arXiv 1502 05977 Bibcode 2015SciA 1E0224E doi 10 1126 sciadv 1500224 ISSN 2375 2548 PMC 4643767 PMID 26601253 Eidini Maryam 2016 Zigzag base folded sheet cellular mechanical metamaterials Extreme Mechanics Letters 6 96 102 arXiv 1509 08104 doi 10 1016 j eml 2015 12 006 S2CID 118424595 Mousanezhad Davood Babaee Sahab Ebrahimi Hamid Ghosh Ranajay Hamouda Abdelmagid Salem Bertoldi Katia Vaziri Ashkan 2015 12 16 Hierarchical honeycomb auxetic metamaterials Scientific Reports 5 18306 Bibcode 2015NatSR 518306M doi 10 1038 srep18306 ISSN 2045 2322 PMC 4680941 PMID 26670417 Mott P H Roland C M 3 April 2012 Limits to Poisson s ratio in isotropic materials general result for arbitrary deformation Physica Scripta Chemistry Division Naval Research Laboratory 87 5 055404 arXiv 1204 3859 doi 10 1088 0031 8949 87 05 055404 S2CID 55920779 Epishin A I Lisovenko D S 2016 Extreme values of Poisson s ratio of cubic crystals Technical Physics 61 10 1516 1524 Bibcode 2016JTePh 61 1516E doi 10 1016 j mechmat 2019 03 017 S2CID 140493258 Gorodtsov V A Lisovenko D S 2019 Extreme values of Young s modulus and Poisson s ratio of hexagonal crystals Mechanics of Materials 134 1 8 doi 10 1016 j mechmat 2019 03 017 S2CID 140493258 Boresi A P Schmidt R J and Sidebottom O M 1993 Advanced Mechanics of Materials Wiley Lekhnitskii S G 1981 Theory of elasticity of an anisotropic elastic body Mir Publishing p 36 Tan S C 1994 Stress Concentrations in Laminated Composites Technomic Publishing Company Lancaster PA Fluegel Alexander Poisson s Ratio Calculation for Glasses www glassproperties com Archived from the original on 23 October 2017 Retrieved 28 April 2018 P H Mott C M Roland 20 October 2009 Limits to Poisson s ratio in isotropic materials PDF Physical Review B 80 13 132104 arXiv 0909 4697 Bibcode 2009PhRvB 80m2104M doi 10 1103 PhysRevB 80 132104 Archived PDF from the original on 2014 10 31 Retrieved 2014 09 24 a href Template Cite journal html title Template Cite journal cite journal a CS1 maint multiple names authors list link Journal of Applied Physics 110 053521 2011 Lakes Rod Negative Poisson s ratio silver neep wisc edu Archived from the original on 16 February 2018 Retrieved 28 April 2018 Ozyhar Tomasz Hering Stefan Niemz Peter March 2013 Viscoelastic characterization of wood Time dependence of the orthotropic compliance in tension and compression Journal of Rheology 57 2 699 717 Bibcode 2013JRheo 57 699O doi 10 1122 1 4790170 ISSN 0148 6055 Jiang Jiali Erik Valentine Bachtiar Lu Jianxiong Niemz Peter 2016 11 01 Time dependence of the orthotropic compression Young s moduli and Poisson s ratios of Chinese fir wood PDF Holzforschung 70 11 1093 1101 doi 10 1515 hf 2016 0001 hdl 20 500 11850 122097 ISSN 1437 434X S2CID 137799672 Carta Giorgio Brun Michele Baldi Antonio 2016 Design of a porous material with isotropic negative Poisson s ratio Mechanics of Materials 97 67 75 doi 10 1016 j mechmat 2016 02 012 Cabras Luigi Brun Michele 2016 A class of auxetic three dimensional lattices Journal of the Mechanics and Physics of Solids 91 56 72 arXiv 1506 04919 Bibcode 2016JMPSo 91 56C doi 10 1016 j jmps 2016 02 010 S2CID 85547530 Cabras Luigi Brun Michele 2014 Auxetic two dimensional lattices with Poisson s ratio arbitrarily close to 1 Proceedings of the Royal Society A 470 2172 20140538 arXiv 1407 5679 Bibcode 2014RSPSA 47040538C doi 10 1098 rspa 2014 0538 S2CID 119321604 Goldstein R V Gorodtsov V A Lisovenko D S 2013 Classification of cubic auxetics Physica Status Solidi B 250 10 2038 2043 Bibcode 2013PSSBR 250 2038G doi 10 1002 pssb 201384233 S2CID 117802510 Goldstein R V Gorodtsov V A Lisovenko D S 2011 Variability of elastic properties of hexagonal auxetics Doklady Physics 56 12 602 605 doi 10 1134 S1028335811120019 S2CID 120998323 Goldstein R V Gorodtsov V A Lisovenko D S Volkov M A 2015 Auxetics among 6 constant tetragonal crystals Letters on Materials 5 4 409 413 doi 10 22226 2410 3535 2015 4 409 413 Mihai L A Goriely A 2017 11 03 How to characterize a nonlinear elastic material A review on nonlinear constitutive parameters in isotropic finite elasticity Proceedings of the Royal Society A 473 2207 20170607 Bibcode 2017RSPSA 47370607M doi 10 1098 rspa 2017 0607 PMC 5719638 PMID 29225507 Lecture Notes in Structural Geology Effective Stress Retrieved 2019 07 03 Silva et al Cork properties capabilities and applications Archived 2017 08 09 at the Wayback Machine Retrieved May 4 2017External links editMeaning of Poisson s ratio Negative Poisson s ratio materials More on negative Poisson s ratio materials auxetic Archived 2018 02 08 at the Wayback Machine Conversion formulaeHomogeneous isotropic linear elastic materials have their elastic properties uniquely determined by any two moduli among these thus given any two any other of the elastic moduli can be calculated according to these formulas provided both for 3D materials first part of the table and for 2D materials second part 3D formulae K displaystyle K nbsp E displaystyle E nbsp l displaystyle lambda nbsp G displaystyle G nbsp n displaystyle nu nbsp M displaystyle M nbsp Notes K E displaystyle K E nbsp 3 K 3 K E 9 K E displaystyle tfrac 3K 3K E 9K E nbsp 3 K E 9 K E displaystyle tfrac 3KE 9K E nbsp 3 K E 6 K displaystyle tfrac 3K E 6K nbsp 3 K 3 K E 9 K E displaystyle tfrac 3K 3K E 9K E nbsp K l displaystyle K lambda nbsp 9 K K l 3 K l displaystyle tfrac 9K K lambda 3K lambda nbsp 3 K l 2 displaystyle tfrac 3 K lambda 2 nbsp l 3 K l displaystyle tfrac lambda 3K lambda nbsp 3 K 2 l displaystyle 3K 2 lambda nbsp K G displaystyle K G nbsp 9 K G 3 K G displaystyle tfrac 9KG 3K G nbsp K 2 G 3 displaystyle K tfrac 2G 3 nbsp 3 K 2 G 2 3 K G displaystyle tfrac 3K 2G 2 3K G nbsp K 4 G 3 displaystyle K tfrac 4G 3 nbsp K n displaystyle K nu nbsp 3 K 1 2 n displaystyle 3K 1 2 nu nbsp 3 K n 1 n displaystyle tfrac 3K nu 1 nu nbsp 3 K 1 2 n 2 1 n displaystyle tfrac 3K 1 2 nu 2 1 nu nbsp 3 K 1 n 1 n displaystyle tfrac 3K 1 nu 1 nu nbsp K M displaystyle K M nbsp 9 K M K 3 K M displaystyle tfrac 9K M K 3K M nbsp 3 K M 2 displaystyle tfrac 3K M 2 nbsp 3 M K 4 displaystyle tfrac 3 M K 4 nbsp 3 K M 3 K M displaystyle tfrac 3K M 3K M nbsp E l displaystyle E lambda nbsp E 3 l R 6 displaystyle tfrac E 3 lambda R 6 nbsp E 3 l R 4 displaystyle tfrac E 3 lambda R 4 nbsp 2 l E l R displaystyle tfrac 2 lambda E lambda R nbsp E l R 2 displaystyle tfrac E lambda R 2 nbsp R E 2 9 l 2 2 E l displaystyle R sqrt E 2 9 lambda 2 2E lambda nbsp E G displaystyle E G nbsp E G 3 3 G E displaystyle tfrac EG 3 3G E nbsp G E 2 G 3 G E displaystyle tfrac G E 2G 3G E nbsp E 2 G 1 displaystyle tfrac E 2G 1 nbsp G 4 G E 3 G E displaystyle tfrac G 4G E 3G E nbsp E n displaystyle E nu nbsp E 3 1 2 n displaystyle tfrac E 3 1 2 nu nbsp E n 1 n 1 2 n displaystyle tfrac E nu 1 nu 1 2 nu nbsp E 2 1 n displaystyle tfrac E 2 1 nu nbsp E 1 n 1 n 1 2 n displaystyle tfrac E 1 nu 1 nu 1 2 nu nbsp E M displaystyle E M nbsp 3 M E S 6 displaystyle tfrac 3M E S 6 nbsp M E S 4 displaystyle tfrac M E S 4 nbsp 3 M E S 8 displaystyle tfrac 3M E S 8 nbsp E M S 4 M displaystyle tfrac E M S 4M nbsp S E 2 9 M 2 10 E M displaystyle S pm sqrt E 2 9M 2 10EM nbsp There are two valid solutions The plus sign leads to n 0 displaystyle nu geq 0 nbsp The minus sign leads to n 0 displaystyle nu leq 0 nbsp l G displaystyle lambda G nbsp l 2 G 3 displaystyle lambda tfrac 2G 3 nbsp G 3 l 2 G l G displaystyle tfrac G 3 lambda 2G lambda G nbsp l 2 l G displaystyle tfrac lambda 2 lambda G nbsp l 2 G displaystyle lambda 2G nbsp l n displaystyle lambda nu nbsp l 1 n 3 n displaystyle tfrac lambda 1 nu 3 nu nbsp l 1 n 1 2 n n displaystyle tfrac lambda 1 nu 1 2 nu nu nbsp l 1 2 n 2 n displaystyle tfrac lambda 1 2 nu 2 nu nbsp l 1 n n displaystyle tfrac lambda 1 nu nu nbsp Cannot be used when n 0 l 0 displaystyle nu 0 Leftrightarrow lambda 0 nbsp l M displaystyle lambda M nbsp M 2 l 3 displaystyle tfrac M 2 lambda 3 nbsp M l M 2 l M l displaystyle tfrac M lambda M 2 lambda M lambda nbsp M l 2 displaystyle tfrac M lambda 2 nbsp l M l displaystyle tfrac lambda M lambda nbsp G n displaystyle G nu nbsp 2 G 1 n 3 1 2 n displaystyle tfrac 2G 1 nu 3 1 2 nu nbsp 2 G 1 n displaystyle 2G 1 nu nbsp 2 G n 1 2 n displaystyle tfrac 2G nu 1 2 nu nbsp 2 G 1 n 1 2 n displaystyle tfrac 2G 1 nu 1 2 nu nbsp G M displaystyle G M nbsp M 4 G 3 displaystyle M tfrac 4G 3 nbsp G 3 M 4 G M G displaystyle tfrac G 3M 4G M G nbsp M 2 G displaystyle M 2G nbsp M 2 G 2 M 2 G displaystyle tfrac M 2G 2M 2G nbsp n M displaystyle nu M nbsp M 1 n 3 1 n displaystyle tfrac M 1 nu 3 1 nu nbsp M 1 n 1 2 n 1 n displaystyle tfrac M 1 nu 1 2 nu 1 nu nbsp M n 1 n displaystyle tfrac M nu 1 nu nbsp M 1 2 n 2 1 n displaystyle tfrac M 1 2 nu 2 1 nu nbsp 2D formulae K 2 D displaystyle K mathrm 2D nbsp E 2 D displaystyle E mathrm 2D nbsp l 2 D displaystyle lambda mathrm 2D nbsp G 2 D displaystyle G mathrm 2D nbsp n 2 D displaystyle nu mathrm 2D nbsp M 2 D displaystyle M mathrm 2D nbsp Notes K 2 D E 2 D displaystyle K mathrm 2D E mathrm 2D nbsp 2 K 2 D 2 K 2 D E 2 D 4 K 2 D E 2 D displaystyle tfrac 2K mathrm 2D 2K mathrm 2D E mathrm 2D 4K mathrm 2D E mathrm 2D nbsp K 2 D E 2 D 4 K 2 D E 2 D displaystyle tfrac K mathrm 2D E mathrm 2D 4K mathrm 2D E mathrm 2D nbsp 2 K 2 D E 2 D 2 K 2 D displaystyle tfrac 2K mathrm 2D E mathrm 2D 2K mathrm 2D nbsp 4 K 2 D 2 4 K 2 D E 2 D displaystyle tfrac 4K mathrm 2D 2 4K mathrm 2D E mathrm 2D nbsp K 2 D l 2 D displaystyle K mathrm 2D lambda mathrm 2D nbsp 4 K 2 D K 2 D l 2 D 2 K 2 D l 2 D displaystyle tfrac 4K mathrm 2D K mathrm 2D lambda mathrm 2D 2K mathrm 2D lambda mathrm 2D nbsp K 2 D l 2 D displaystyle K mathrm 2D lambda mathrm 2D nbsp l 2 D 2 K 2 D l 2 D displaystyle tfrac lambda mathrm 2D 2K mathrm 2D lambda mathrm 2D nbsp 2 K 2 D l 2 D displaystyle 2K mathrm 2D lambda mathrm 2D nbsp K 2 D G 2 D displaystyle K mathrm 2D G mathrm 2D nbsp 4 K 2 D G 2 D K 2 D G 2 D displaystyle tfrac 4K mathrm 2D G mathrm 2D K mathrm 2D G mathrm 2D nbsp K 2 D G 2 D displaystyle K mathrm 2D G mathrm 2D nbsp K 2 D G 2 D K 2 D G 2 D displaystyle tfrac K mathrm 2D G mathrm 2D K mathrm 2D G mathrm 2D nbsp K 2 D G 2 D displaystyle K mathrm 2D G mathrm 2D nbsp K 2 D n 2 D displaystyle K mathrm 2D nu mathrm 2D nbsp 2 K 2 D 1 n 2 D displaystyle 2K mathrm 2D 1 nu mathrm 2D nbsp 2 K 2 D n 2 D 1 n 2 D displaystyle tfrac 2K mathrm 2D nu mathrm 2D 1 nu mathrm 2D nbsp K 2 D 1 n 2 D 1 n 2 D displaystyle tfrac K mathrm 2D 1 nu mathrm 2D 1 nu mathrm 2D nbsp 2 K 2 D 1 n 2 D displaystyle tfrac 2K mathrm 2D 1 nu mathrm 2D nbsp E 2 D G 2 D displaystyle E mathrm 2D G mathrm 2D nbsp E 2 D G 2 D 4 G 2 D E 2 D displaystyle tfrac E mathrm 2D G mathrm 2D 4G mathrm 2D E mathrm 2D nbsp 2 G 2 D E 2 D 2 G 2 D 4 G 2 D E 2 D displaystyle tfrac 2G mathrm 2D E mathrm 2D 2G mathrm 2D 4G mathrm 2D E mathrm 2D nbsp E 2 D 2 G 2 D 1 displaystyle tfrac E mathrm 2D 2G mathrm 2D 1 nbsp 4 G 2 D 2 4 G 2 D E 2 D displaystyle tfrac 4G mathrm 2D 2 4G mathrm 2D E mathrm 2D nbsp E 2 D n 2 D displaystyle E mathrm 2D nu mathrm 2D nbsp E 2 D 2 1 n 2 D displaystyle tfrac E mathrm 2D 2 1 nu mathrm 2D nbsp E 2 D n 2 D 1 n 2 D 1 n 2 D displaystyle tfrac E mathrm 2D nu mathrm 2D 1 nu mathrm 2D 1 nu mathrm 2D nbsp E 2 D 2 1 n 2 D displaystyle tfrac E mathrm 2D 2 1 nu mathrm 2D nbsp E 2 D 1 n 2 D 1 n 2 D displaystyle tfrac E mathrm 2D 1 nu mathrm 2D 1 nu mathrm 2D nbsp l 2 D G 2 D displaystyle lambda mathrm 2D G mathrm 2D nbsp l 2 D G 2 D displaystyle lambda mathrm 2D G mathrm 2D nbsp 4 G 2 D l 2 D G 2 D l 2 D 2 G 2 D displaystyle tfrac 4G mathrm 2D lambda mathrm 2D G mathrm 2D lambda mathrm 2D 2G mathrm 2D nbsp l 2 D l 2 D 2 G 2 D displaystyle tfrac lambda mathrm 2D lambda mathrm 2D 2G mathrm 2D nbsp l 2 D 2 G 2 D displaystyle lambda mathrm 2D 2G mathrm 2D nbsp l 2 D n 2 D displaystyle lambda mathrm 2D nu mathrm 2D nbsp l 2 D 1 n 2 D 2 n 2 D displaystyle tfrac lambda mathrm 2D 1 nu mathrm 2D 2 nu mathrm 2D nbsp l 2 D 1 n 2 D 1 n 2 D n 2 D displaystyle tfrac lambda mathrm 2D 1 nu mathrm 2D 1 nu mathrm 2D nu mathrm 2D nbsp l 2 D 1 n 2 D 2 n 2 D displaystyle tfrac lambda mathrm 2D 1 nu mathrm 2D 2 nu mathrm 2D nbsp l 2 D n 2 D displaystyle tfrac lambda mathrm 2D nu mathrm 2D nbsp Cannot be used when n 2 D 0 l 2 D 0 displaystyle nu mathrm 2D 0 Leftrightarrow lambda mathrm 2D 0 nbsp G 2 D n 2 D displaystyle G mathrm 2D nu mathrm 2D nbsp G 2 D 1 n 2 D 1 n 2 D displaystyle tfrac G mathrm 2D 1 nu mathrm 2D 1 nu mathrm 2D nbsp 2 G 2 D 1 n 2 D displaystyle 2G mathrm 2D 1 nu mathrm 2D nbsp 2 G 2 D n 2 D 1 n 2 D displaystyle tfrac 2G mathrm 2D nu mathrm 2D 1 nu mathrm 2D nbsp 2 G 2 D 1 n 2 D displaystyle tfrac 2G mathrm 2D 1 nu mathrm 2D nbsp G 2 D M 2 D displaystyle G mathrm 2D M mathrm 2D nbsp M 2 D G 2 D displaystyle M mathrm 2D G mathrm 2D nbsp 4 G 2 D M 2 D G 2 D M 2 D displaystyle tfrac 4G mathrm 2D M mathrm 2D G mathrm 2D M mathrm 2D nbsp M 2 D 2 G 2 D displaystyle M mathrm 2D 2G mathrm 2D nbsp M 2 D 2 G 2 D M 2 D displaystyle tfrac M mathrm 2D 2G mathrm 2D M mathrm 2D nbsp Retrieved from https en wikipedia org w index php title Poisson 27s ratio, wikipedia, wiki, book, books, library,

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