XRD--残余应力测试课件.ppt
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1、BSSM WorkshopPART IIThe sin2 Method Using Laboratory X-RaysJudith ShackletonSchool of Materials,University of ManchesterThe sin2 Method What are We Measuring?We measure the ELASTIC Strain.We measure the ELASTIC Strain.We can determineWe can determine Magnitude of the stress,Magnitude of the stress,I
2、ts directionIts direction Its natureIts nature Compressive or tensileCompressive or tensile We use the planes of the crystal lattice as an atomic We use the planes of the crystal lattice as an atomic scale“strain gauge”scale“strain gauge”The sin2 Method How Does it Work?We measure We measure STRAINS
3、TRAIN ()not not STRESS STRESS()We We CALCULTE STRESSCALCULTE STRESS from the from the STRAINSTRAIN&the&the ELASTIC CONSTANTSELASTIC CONSTANTS We use the planes We use the planes d dhklhkl,of the crystal lattice as a ,of the crystal lattice as a strain gaugestrain gauge We can measure the change in W
4、e can measure the change in d d-spacing,-spacing,d dStrain=Strain=d/dd/dChanges in d-spacing with StressConsider a bar which is in tensionConsider a bar which is in tension The The d d-spacings of the planes normal to the applied stress increase,as-spacings of the planes normal to the applied stress
5、 increase,as the stress is tensilethe stress is tensile The The d d-spacings of the planes parallel to the applied stress decrease,due-spacings of the planes parallel to the applied stress decrease,due to Poisson strainto Poisson strainMeasuring Elastic&InelasticStrainPrimarily we are measuring macr
6、o stressesPrimarily we are measuring macro stresses This is a uniform displacement of the lattice planesThis is a uniform displacement of the lattice planes These cause a VERY SMALL shift in the position,the These cause a VERY SMALL shift in the position,the Bragg angle 2Bragg angle 2,of the reflect
7、ion&we can measure of the reflection&we can measure this(Only Just!)this(Only Just!)Inelastic stresses cause peak broadening,which Inelastic stresses cause peak broadening,which can be measured.This is an extensive subject,not can be measured.This is an extensive subject,not covered here.covered her
8、e.Which Materials Can We Measure?Works on any poly-crystalline solid which Works on any poly-crystalline solid which gives a high angle Bragg reflectiongives a high angle Bragg reflection MetalsMetals Ceramics(not easy!)Ceramics(not easy!)Multi-phase materials Multi-phase materials Not usually appli
9、ed to polymers,as no suitable Not usually applied to polymers,as no suitable reflections,can add a metallic powder,reported reflections,can add a metallic powder,reported in the literaturein the literatureWhy use the sin2 MethodThe AdvantagesMost ImportantA stress free A stress free d d-spacing is N
10、OT required for the-spacing is NOT required for the bi-axial case which is almost always usedbi-axial case which is almost always usedOther advantagesOther advantages Low cost(compared with neutrons&synchrotrons,Low cost(compared with neutrons&synchrotrons,but not hole drilling)but not hole drilling
11、)Non-destructive,unlike hole drillingNon-destructive,unlike hole drilling Easy to do&fairly fool proof(if you are careful!)Easy to do&fairly fool proof(if you are careful!)DisadvantagesMost ImportantSurface method only,X-ray beam penetration Surface method only,X-ray beam penetration depth 10 to 20
12、microns,at bestdepth 10 to 20 microns,at bestFor depth profiling must electro-polish,gives For depth profiling must electro-polish,gives 1-1.5mm1-1.5mmOther DisadvantagesOther Disadvantages Affected by grain size,texture(preferred Affected by grain size,texture(preferred orientation)&surface roughne
13、ssorientation)&surface roughness Doesnt work on amorphous materials(obviously!)Doesnt work on amorphous materials(obviously!)Basic TheoryConsider a unit cube(quite a big one!)embedded in a componentNotation,(ij)the stress component acting on face i in direction(parallel to axis)jBasic Theory The nor
14、mal stresses act normal to the cube faces&the two The normal stresses act normal to the cube faces&the two subscripts are the same subscripts are the same e.g.e.g.(22)(22)The shear stresses(twisting forces)act parallel to the cube The shear stresses(twisting forces)act parallel to the cube faces&the
15、 two subscripts are differentfaces&the two subscripts are different e.g.e.g.(31)(31)or in the general case or in the general case (ij)(ij)We measure normal stresses&shear stresses,but thats not We measure normal stresses&shear stresses,but thats not what we want,we dont get all of the information!Wh
16、y?what we want,we dont get all of the information!Why?Basic TheoryNormal StressesFrom elastic theory of isotropic materials,the 3 normal strains are given by,1111=1 1 1111-(2222+3333)E E 2222=1 1 2222-(3333+1111)E E 3333=1 1 3333-(1111+2222)E E The strain in The strain in anyany direction is a funct
17、ion of the direction is a function of the stressstress in the in the others!.Ideally,we should measure more than one others!.Ideally,we should measure more than one directiondirectionPrincipal StressesWe should measure We should measure more than one directionmore than one direction to get to get a
18、complete picture of the stress in the component a complete picture of the stress in the component If we measure 3 directions or more we can If we measure 3 directions or more we can calculate the PRINCIPAL STRESSESS,these are calculate the PRINCIPAL STRESSESS,these are the directions on which no she
19、ar stress actsthe directions on which no shear stress actsWe do this by rotating the sample through an angle We do this by rotating the sample through an angle ,in its own plane,exact details&diagrams later,in its own plane,exact details&diagrams laterHow the Sin2 Method WorksSample in“Bragg Conditi
20、on”Diffraction Diffraction vector,normal to vector,normal to sample surfacesample surfacednWe measure the We measure the d d-spacing with the spacing with the angle of incidence angle of incidence()&the angle of&the angle of reflection of the X-reflection of the X-ray beam(with ray beam(with respect
21、 to the respect to the sample surface)sample surface)equal.These planes equal.These planes are parallel to the are parallel to the free surface&free surface&unstressed,but not unstressed,but not unstrainedunstrained Also called focussed geometryAlso called focussed geometryHow the Sin2 Method WorksD
22、iffraction vector,titled with respect to sample surfaceTilt the sample through an angle and measure the d-spacing again.These planes are not parallel to the free surface.Their d-spacing is changed by the stress in the sample.dDefocused geometryHow the Sin2 Method WorksWe tilt the sample through an a
23、ngle psi,We tilt the sample through an angle psi,to to measure magnitude the normal&shear stressesmeasure magnitude the normal&shear stresses We use a range of values of We use a range of values of (called offsets)for(called offsets)for example,from 0 to 45example,from 0 to 45 in steps of 5 in steps
24、 of 5 NEVERNEVER use the“Double Exposure Method”which use the“Double Exposure Method”which uses just one uses just one offsetsoffsets.Not enough data points!.Not enough data points!We rotate the the sample through an angle,We rotate the the sample through an angle,to to determine the directions of t
25、he principle stressesdetermine the directions of the principle stressesNo Stress Free d-Spacing Needed The Approximation The depth of penetration of the X-ray beam in the sample The depth of penetration of the X-ray beam in the sample is small,typically 20is small,typically 20 We can say that there
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