UDC 539.4:620.17
Shear to Normal Stress Fundamental Science (on Strength Criteria Generally Considering Relations between the Shear and Normal Limiting Stresses)
by
© Ph. D. & Dr. Sc. Lev Gelimson
Academic Institute for Creating Fundamental Sciences (Munich, Germany)
Strength Monograph
The “Collegium” All World Academy of Sciences Publishers
Munich (Germany)
2009
The influence of the relations between the shear and normal limiting stresses on strength is substantial. General theories for considering these relations in strength criteria are created along with general power strength sciences and lead to discovering new strength phenomena. Universalized criteria can fit both convex and nonconvex limiting surfaces.
Keywords: shear limiting stress, normal limiting stress, tension, compression.
0. Introduction. The τL/σL ratio of shear τL and normal σL limiting stresses of materials [1–5] takes different positive values not greater than 1 often with substantial deviations from 1/2 and 3-1/2 predefined by the most common Tresca and Huber-von Mises-Hencky criteria [1–4]. The lower (inner) (Tresca's criterion [6]) and upper (outer) (Ishlinsky's deviatoric stress criterion [7]) bounds of all the convex (by Drucker's postulate [8]) limiting surfaces are well-known [9]. Yu [10, 11] proposed his twin-shear yield criterion coinciding with Ishlinsky's deviatoric stress criterion [7], showed that all the convex limiting surfaces correspond to relations 1/2 ≤ τL/σL ≤ 2/3, and generalized these bounds for σLt ≠ σLc . Yu also proposed his twin-shear unified strength theory [10, 11] generalizing that criterion and fitting data τL/σL = 0.376, 0.432, 0.451, and 0.474 [12–14], as well as τL/σL = 0.727 and up to 0.82 [12, 15, 16] for materials with nonconvex limiting surfaces. Data τL/σL = 0.71 and 0.74 for steel [17, 18], τL/σL = 0.25 and 0.27 for magnesium and 0.69 for bronze [17], τL/σL = 0.40 and 0.42 for alloys and 0.67 for steel [19], τL/σL = 0.65 and up to 0.76 for iron [20], as well as up to 1 for brittle building materials [1], etc. are available, too.
In fundamental material strength sciences [21–25], general power strength sciences including general linear strength science generalizing Yu’s twin shear unified strength theory [10, 11] also fit all these and other data with scattering, e.g. via the following general strength criteria very simple.
Use the principal stresses σ1 ≥ σ2 ≥ σ3 (regulated by this ordering) at a material's point along with limiting stress values σL such as yield stress σy or ultimate strength σL , namely σLt in tension and σLc in compression with σLc ≥ 0 and α = σLt/σLc if σLt ≠ σLc . If the equivalent stress σe in a strength criterion is a symmetric function of the principal stresses, use nonregulated principal stresses σ1n , σ2n , and σ3n without any predefined relations, which is very useful analytically and graphically.
Fundamental material strength sciences give whole hierarchies of universal strength laws of nature and are based on general sciences of dimensionless relative (reduced) principal stresses σj° [21–25]. They are introduced via dividing each usual principal stress σj (j = 1, 2, 3) by the modulus (absolute value) |σjL| of its individual limiting value σjL of the same sign in the same direction by vanishing the remaining two principal stresses under the same remaining load conditions:
σj° = σj / |σjL| (j = 1, 2, 3).
The inequalities σ1° ≥ σ2° ≥ σ3° necessary if σe° nonsymmetrically depends on σ1°, σ2°, and σ3° always hold for an isotropic material. For an anisotropic material, reindexing σ1°, σ2°, and σ3° can be necessary to provide those inequalities.
Dependently on the essence of a certain strength criterion, safety and failure areas determined by it, and their limiting surface, also consider one-sided limitations for σe and σe° and their values even imaginary if they indicate still greater reserves than vanishing σe . Naturally extend σe and σe° by accepting their negative values with σe ≤ σL and σe° ≤ 1 and use nonnegative |σe| and |σe°|.
1. Applying general linear strength science. This science exhaustively represents all piecewise linear strength criteria via initial general linear form
σe° = a0 + a1σ1° + a2σ2° + a3σ3° + ∑i=1N b1i|c00i + c11iσ1° + c21iσ2° + c31iσ3° + b2i|c02i + c12iσ1° + c22iσ2° + c32iσ3° + b3i|c03i + c13iσ1° + c23iσ2° + c33iσ3° + ... || ... | ≤ 1
where a0 , a1 , a2 , a3 , bhi , c0hi , c1hi , c2hi , c3hi are any constants with omitting unnecessary indices and renaming constants if this is useful; h = 1, 2, ... , H are nesting levels; H and N are any nonnegative integers. By H = 1,
σe° = a0 + a1σ1° + a2σ2° + a3σ3° + ∑i=1N bi|c0i + c1iσ1° + c2iσ2° + c3iσ3°| ≤ 1.
For determining the constants, use the unstressed (σ° = 0) state (σ1° = σ2° = σ3° = 0), intermediate nonlimiting (0 < σ° < 1), and limiting (σ° = 1) stress states under uniaxial tension (σ1° = σ° ≥ 0, σ2° = σ3° = 0), uniaxial compression (σ1° = σ2° = 0, σ3° = -σ° ≤ 0), and pure shear (σ1° = σ°τL/σLt ≥ 0, σ2° = 0, σ3° = - σ°τL/σLc ≤ 0) as standard strength tests.
1.1. Applying the general pure linear form of strength criteria. N = 0 leads to the initial and final general pure linear forms of strength criteria
σe° = a0 + a1σ1° + a2σ2° + a3σ3° ≤ 1, σe° = σ1° + aσ2° - σ3° ≤ 1
with any constant a, to τL/σL = 1/2 like Tresca's criterion [1–4] by σLt = σLc = σL , and generally to 1/τL = 1/σLt + 1/σLc in its universalization via σe°. In fundamental material strength sciences [21–25], this final form is already known due to general stress criteria correction science with adding a homogeneous linear combination of the principal stresses to the expression of σe and using the standard tests data. Allowing negative values of σe° brings clear generalization replacing Tresca's prism (by a = 0) with a pyramid (by a ≠ 0) physically realistic by a > 0. Hence the pure linear form of strength criteria is the simplest one which has clear physical sense, generalizes many known pure linear strength criteria, and considers Bridgman's phenomenon for pressure-dependent materials [5]. But this form leads to the predefined relation between the normal and shear strengths and to a monotonic dependence of σe on σ2 with contradicting many test data [3, 4, 10–20].
1.2. Applying general pure one-modulus linear form of strength criteria. a0 = a1 = a2 = a3 = 0 and N = H = 1 lead to their initial and final forms
σe° = |σe°| = |c0 + c1σ1° + c2σ2° + c3σ3°| ≤ 1, σe° = |σe°| = |σ1° + aσ2° - σ3°| ≤ 1
and to the same relations 1/τL = 1/σLt + 1/σLc and (by σLt = σLc = σL) τL/σL = 1/2.
Using the modulus gives a two-sided pyramid by a ≠ 0 and nothing new by a = 0.
1.3. Applying general mixed linear homogeneous form of strength criteria. N = H = 1 and a0 = c0 = 0 lead to their initial form
σe° = a1σ1° + a2σ2° + a3σ3° + b|c1σ1° + c2σ2° + c3σ3°| ≤ 1,
to the key role of the sign of difference τL/σLt - σLc/(σLt + σLc) (which equals τL/σL - 1/2 by σLt = σLc = σL), to b = τL(σLt + σLc)/(σLtσLc) - 1, and to the final form
σe° = (1 - (τL(σLt + σLc)/(σLtσLc) - 1)|c1|)σ1° + aσ2° - (1 - (τL(σLt + σLc)/(σLtσLc) - 1)|c3|)σ3° + (τL(σLt + σLc)/(σLtσLc) - 1)|c1σ1° + c2σ2° + c3σ3°| ≤ 1.
Only for materials with τL/σLt = σLc/(σLt + σLc) (τL/σL = 1/2 by σLt = σLc = σL), there are additional strength criteria using any c1 and c3 with c1c3 ≤ 0 and any b. Hence even for such materials, moduli can be used and give additional strength criteria.
1.4. Applying general mixed linear form of strength criteria. N = H = 1 lead to their initial form
σe° = a0 + a1σ1° + a2σ2° + a3σ3° + b|c0 + c1σ1° + c2σ2° + c3σ3°| ≤ 1
and, only for materials with τL/σLt = σLc/(σLt + σLc) (τL/σL = 1/2 by σLt = σLc = σL), to additional criteria
- bc0 + (1 - bc1)σ1° + a2σ2° + (-1 - bc3)σ3° + b|c0 + c1σ1° + c2σ2° + c3σ3°| ≤ 1.
Hence namely such materials allow more simulation possibilities than others, which expresses strength phenomena specific for such materials only.
2. Applying general power strength sciences. Fundamental material strength sciences [21–25] include general power strength sciences naturally generalizing general linear strength science and possibly using moduli and radicals which both can be also nesting. Use, e.g., the homogeneous powers of the shear stresses (with clear generalizing Hosford’s criterion [1–4]):
σe = [a13(σ1 - σ3)k + a12(σ1 - σ2)k + a23(σ2 - σ3)k]1/k ≤ σL (k > 0).
Uniaxial limiting stresses in tension and compression give strength criteria forms
σe = {a(σ1 - σ3)k + (1 - a)[(σ1 - σ2)k + (σ2 - σ3)k]}1/k ≤ σL ,
σe° = {a(σ1° - σ3°)k + (1 - a)[(σ1° - σ2°)k + (σ2° - σ3°)k]}1/k ≤ 1.
Pure shear reduced limiting stresses σ1° = τL/σLt , σ2° = 0 , σ3° = -τL/σLc give (k ≠ 1)
σe° = {(σLtkσLck/τLk - σLtk - σLck)/[(σLt + σLc)k - σLtk - σLck](σ1° - σ3°)k +
[(σLt + σLc)k - σLtkσLck/τLk]/[(σLt + σLc)k - σLtk - σLck][(σ1°- σ2°)k + (σ2° - σ3°)k]}1/k ≤ 1.
In the simplest case k = 2 and then additionally by σLt = σLc = σL , we have criteria
σe° = {[σLtσLc/(2τL2) - (σLt2 + σLc2)/(2σLtσLc)](σ1° - σ3°)2 +
[(σLt2 + σLc2)/(2σLtσLc) - σLtσLc/(2τL2)][(σ1°- σ2°)2 + (σ2° - σ3°)2]}1/2 ≤ 1,
σe° = {[σL2/(2τL2) - 1](σ1° - σ3°)2 + [2 - σL2/(2τL2)][(σ1°- σ2°)2 + (σ2° - σ3°)2]}1/2 ≤ 1
which fit the above and any other data on the relation between the shear and normal limiting stresses for any materials. Additionally simply consider the influence of adding isotropic stress states, e.g. hydrostatic pressure, via adding aσ2° (generally, any function g(σ2°) vanishing at σ2°) to the both last expressions of σe° with no influence on the limiting stresses in uniaxial tension and compression and pure shear. The obtained strength criteria fit strength test data on many artificial materials under static and variable loading [1–4, 29, 30] with average relative errors of about 10 %. The same holds for comprehensive polyaxial strength test data on natural materials very different: Dunham dolomite, Solenhofen limestone, and Mizuho trachyte [31], coarse grained dense marble [32, 33], Shirahama sandstone and Yuubari shale [34], KTB deep hole amphibolite [35], Westerly granite [36], fine-grained Rozbark sandstone [37], and Soignies limestone [38]. For these data in triaxial compression only, no complication of this form is necessary and, by the principle of tolerable simplicity [21–28], reasonable.
General power strength sciences can still better than general linear strength science fit triaxial strength data in all areas and, unlike it, admit symmetric functions σe of σ1 , σ2 , σ3 and using σ1n , σ2n , σ3n with clear advantages. The initial form of power strength criteria with general homogeneous symmetric polynomials Pi(σ1n°, σ2n°, σ3n°) of power i is
σe° = [∑i=0N aiPi(σ1n°, σ2n°, σ3n°)]1/N ≤ 1.
In the unstressed state, σe° = 0 is natural and leads to a0 = 0. Case N = 2 gives form
σe° = [a1(σ1n° + σ2n° + σ3n°) + a2(σ1n°2 + σ2n°2 + σ3n°2) +
b2(σ1n°σ2n° + σ1n°σ3n° + σ2n°σ3n°)]1/2 ≤ 1
further generalizing the universalization of the Huber-von Mises-Hencky criterion
σe° = [σ1n°2 + σ2n°2 + σ3n°2 - (σ1n°σ2n° + σ1n°σ3n° + σ2n°σ3n°)]1/2 ≤ 1
in fundamental strength sciences. a1(σ1n° + σ2n° + σ3n°) corresponds to the typical idea to consider adding isotropic stress states, e.g. under hydrostatic pressure. But it does not work at all with using strength data in uniaxial tension and compression even by replacing σL with a general constant C at least by materials with σLt = σLc and hence by any materials. This is obvious due to fundamental material strength sciences with σLt° = σLc° = 1, to the nonuniversality of this approach, and to unlimited σe when σLc - σLt is very small. Using any function g(σ2) with g(0) = 0 universally works but brings asymmetry of function σe of the principal stresses.
Megamathematics [24, 26–28] solves these general problems with perpetuating limiting surface continuity and the symmetry of σe as a function of the principal stresses. Fundamental material strength sciences replace usual σ1 + σ2 + σ3 and reduced σ1n° + σ2n° + σ3n° “hydrostatic sums” with their continuous functions f and f° vanishing at -σLc , 0, σLt and -1, 0, 1, respectively. Using uniaxial tension and compression data and renaming the constants leads to
σe° = [σ1n°2 + σ2n°2 + σ3n°2 - a(σ1n°σ2n° + σ1n°σ3n° + σ2n°σ3n°) +
bf°(σ1n° + σ2n° + σ3n°)]1/2 ≤ 1.
Constant a provides considering true values of τL/σL and not only predefined 3-1/2 by a = 1. This leads by b = 0 to ellipsoidal (by -2 < a < 1) and hyperboloidal (by a > 1) limiting surfaces and to “hydrostatic” strength limited in compression and unlimited in tension with concavity everywhere, respectively. This clearly contradicts strength test data and Drucker’s postulate [8]. The Huber-von Mises-Hencky cylinder [1–4] lies between those limiting surfaces as their limiting case. But using b ≠ 0 with piecewise linear functions, namely
f(σ1 + σ2 + σ3) = σ1 + σ2 + σ3 + σLc if σ1 + σ2 + σ3 ≤ -σLc ,
f(σ1 + σ2 + σ3) = 0 if -σLc ≤ σ1 + σ2 + σ3 ≤ σLt ,
f(σ1 + σ2 + σ3) = σ1 + σ2 + σ3 - σLt if σ1 + σ2 + σ3 ≥ σLt ;
f°(σ1n° + σ2n° + σ3n°) = σ1n° + σ2n° + σ3n°+ 1 if σ1n° + σ2n° + σ3n° ≤ -1,
f(σ1n° + σ2n° + σ3n°) = 0 if -1 ≤ σ1n° + σ2n° + σ3n° ≤ 1,
f(σ1n° + σ2n° + σ3n°) = σ1n° + σ2n° + σ3n°- 1 if σ1n° + σ2n° + σ3n° ≥ 1,
transforms those types of limiting surfaces to paraboloidal. Hence this quadratic form of strength criteria realizes the idea of independently considering the influences of τL/σL and of adding an isotropic stress state, e.g. hydrostatic pressure, on σe , can give a limiting surface of the paraboloidal type physically adequate in all triaxial stress areas, still better fits the same strength test data, and, by the principle of tolerable simplicity [21–28], needs no complication. Moreover, to truly compare the complexities of different strength criteria, represent them in forms namely with symmetric functions σe of σ1 , σ2 , σ3 because representing limiting surfaces needs σ1n , σ2n , σ3n . Hence quadratic strength criteria can be even simpler than linear and especially piecewise linear strength criteria whose namely linear forms can give functions σe of σ1 , σ2 , σ3 nonsymmetric only.
It is very important that using f(σ1 + σ2 + σ3) and f°(σ1n° + σ2n° + σ3n°) has no influence on uniaxial tension and compression as well as on pure shear and hence on the value of the τL/σL ratio fully determined by a strength criterion with vanishing the factors by f(σ1 + σ2 + σ3) and f°(σ1n° + σ2n° + σ3n°).
3. Applying an approach using combined bending and torsion. To correct the Tresca and von Mises criteria [1–4] via taking the τL/σL ratio of shear τL and normal σL limiting stresses into account, consider combined bending and torsion with normal σ and shear τ stresses and the principal stresses σ1 ≥ σ2 ≥ σ3 :
σ1 = [σ + (σ2 + 4τ2)1/2]/2, σ2 = 0, σ3 = [σ - (σ2 + 4τ2)1/2]/2.
The value of τL/σL is 1/2 and 3-1/2 by the Tresca and Huber-von Mises-Hencky criteria [1–4]
σe = σ1 - σ3 ≤ σL , σe = [σ12 + σ22 + σ32 - (σ1σ2 + σ1σ3 + σ2σ3)]1/2 ≤ σL
giving two particular and one unified criteria
σe = (σ2 + 4τ2)1/2 ≤ σL , σe = (σ2 + 3τ2)1/2 ≤ σL ; σe = [σ2 + (σL/τL)2τ2]1/2 ≤ σL .
To understand the naturalness of the last one, divide all its parts by σL :
(σe° = ) σe/σL = [(σ/σL)2 + (τ/τL)2]1/2 ≤ σL/σL ( = 1).
For the general case of a triaxial stress state by using its three principal directions 1, 2, and 3 with vanishing all the shear stresses, first consider the Huber-von Mises-Hencky criterion. To take additional constant τL/σL of a material into account, generalize this criterion with trying to perpetuate the symmetry of the occurrences of the principal stresses. A natural possibility is to vary the factors by the sums σ12 + σ22 + σ32 and σ1σ2 + σ1σ3 + σ2σ3 . Uniaxial tension and compression give that the first factor has to be 1. Hence additionally include unknown factor k:
σe = [σ12 + σ22 + σ32 + k(σ1σ2 + σ1σ3 + σ2σ3)]1/2 ≤ σL .
To determine k, use the same combined bending and torsion once more:
σe = [σ2 + (2 - k)τ2]1/2 ≤ σL , k = 2 - (σL/τL)2,
σe = {σ12 + σ22 + σ32 + [2 - (σL/τL)2](σ1σ2 + σ1σ3 + σ2σ3)}1/2 ≤ σL .
For the Tresca criterion [1–4], it is impossible to keep the criterion’s linear form by its generalization providing considering the true value of the τL/σL ratio. We proved this above. The cause is that the factors 1 and -1 in this criterion are unique to provide its applicability to uniaxial tension and compression, and introducing σ2 brings nothing for our purpose at least in the particular case of combined bending and torsion (due to vanishing σ2) and thus cannot solve, all the more, the general problem. Now it is natural to choose a quadratic form similar to that for the Huber-von Mises-Hencky criterion [1–4]:
σe = [(σ1 - σ3)2 + kσ1σ3]1/2 ≤ σL , σe = [σ2 + (4 - k)τ2]1/2 ≤ σL , k = 4 - (σL/τL)2,
σe ={(σ1 - σ3)2 + [4 - (σL/τL)2]σ1σ3}1/2 ≤ σL , σe ={σ12 + σ32 +[2 - (σL/τL)2]σ1σ3}1/2 ≤ σL .
Experimental data on strength of ductile materials is often placed between the curves given by the Tresca and Huber-von Mises-Hencky criteria [1–4]. Expecting more criterion precision by smaller deviation of the σL/τL ratio from its pre-defined value gives the unified criterion as the linear combination
σe ={[(σL/τL)2 - 3](σ1 - σ3) + [4 - (σL/τL)2][σ12 + σ22 + σ32 - (σ1σ2 + σ1σ3 + σ2σ3)]}1/2 ≤ σL .
The unified criterion using their above forms already corrected is
σe = [(σL/τL)2 - 3]{σ12 + σ32 + [2 - (σL/τL)2]σ1σ3]}1/2 +
[4 - (σL/τL)2]{σ12 + σ22 + σ32 + [2 - (σL/τL)2](σ1σ2 + σ1σ3 + σ2σ3)}1/2 ≤ σL .
Such a linear unification approach is not the only. To naturally extend it, a power unification approach can be also used.
And the Hosford exponential unification [1–4]
σe = {[(σ1 - σ2)k + (σ2 - σ3)k + (σ1 - σ3)k]/2}1/k ≤ σL
gives the Tresca and Huber-von Mises-Hencky criteria by k = 1 and k = 2. For them, to provide these values of k using the same predefined values of the ratio σL/τL , naturally choose k = 5 - (σL/τL)2. For further generalizations, introduce the notation (with apparently extending to any sets of variables and function values)
f[x, y | f(a, b) = v, f(c, d) = w]
for any function f taking, e.g., values v and w by values a, b and c, d of its variables x, y, respectively. Then choose f[σL/τL | f(2) = 1, f(31/2) = 0], g[σL/τL | g(2) = 0, g(31/2) = 1], and h[σL/τL | h(2) = 1, h(31/2) = 2] instead of k = (σL/τL)2 - 3, k = 4 - (σL/τL)2, and k = 5 - (σL/τL)2, respectively.
And in general linear strength science [21–25], for a material with strengths σLt in tension and σLc (σLc ≥ 0) in compression, sign(τL/σLt - σLc/(σLt + σLc)) plays the key role. If σLt = σLc = σL , then it is sign(τL/σL - 1/2). General power strength sciences generalizing that science can fit any relations between the shear and normal limiting stresses for materials with convex and nonconvex limiting surfaces.
Basic Results and Conclusions
1. The relations between the shear and normal limiting stresses for distinct materials are very different.
2. Many known strength criteria predefine the relations between the shear and normal limiting stresses and cannot fit their true relations for many materials.
3. In fundamental material strength science, general linear strength theory and its natural generalization, namely general power strength theory, correctly consider and express known physical phenomena in material science, have clear physical sense, use single formulae possibly with moduli, and fit the true relations between the shear and normal limiting stresses for many materials. These theories generalize many known strength criteria, determine their applicability ranges, and provide independently fitting both the influence of adding isotropic stress states and the true relations between the shear and normal limiting stresses for many materials.
4. The relation between the shear and normal limiting stresses is critical for choosing a suitable form of strength criteria.
5. The linear, piecewise linear with one modulus, and quadratic forms of strength criteria are the simplest ones and provide many advantages.
6. General power strength theory including general linear strength theory provides fundamental material strength science with initial strength criteria to discover the hierarchies of strength laws of nature. These theories are very suitable, allow generally representing and processing test data, and reduce time and cost expense by polyaxial strength tests.
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