Academic literature on the topic 'Stress field'

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Journal articles on the topic "Stress field"

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Saada, Georges. "Stress Field at Interfaces." Solid State Phenomena 59-60 (January 1998): 77–98. http://dx.doi.org/10.4028/www.scientific.net/ssp.59-60.77.

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Neff, Ellen P. "Stress in the field." Lab Animal 47, no. 11 (October 23, 2018): 308. http://dx.doi.org/10.1038/s41684-018-0186-5.

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Mittler, Ron. "Abiotic stress, the field environment and stress combination." Trends in Plant Science 11, no. 1 (January 2006): 15–19. http://dx.doi.org/10.1016/j.tplants.2005.11.002.

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Kim, Ho Kyeom, Martyn J. Pavier, and Anton Shterenlikht. "Plasticity and Stress Heterogeneity Influence on Mechanical Stress Relaxation Residual Stress Measurements." Advanced Materials Research 996 (August 2014): 249–55. http://dx.doi.org/10.4028/www.scientific.net/amr.996.249.

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Two common problems of mechanical strain relaxation(MSR) residual stress measurement methods are investigated in this work:(1) assumption of stress uniformity and (2) the effect of plasticity at relaxation. A new MSR technique, designed specifically for highly non-uniformin-plane residual stress fields, is applied in this work to measure the residual stress field resulted from pure bending of an Al7075 alloy.The method involves introducing a straight cut across the whole part in a single increment, and collecting full field displacement fields from the side surface. Application of a 2D high resolution digital image correlation (DIC) method proved successful in this work.The reconstructed residual stress agrees well with that predicted by FE modelling. It is shown that the direction of the propagation of the slit has a major influence on plastic flow during relaxation.The major conclusion from this work is that it is possible to substantially reduce, or completely eliminate, plastic flow on relaxation by careful planning of the slit orientation and the cutting schedule.
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Barker, D. B., R. J. Sanford, and R. Chona. "DeterminingK and related stress-field parameters from displacement fields." Experimental Mechanics 25, no. 4 (December 1985): 399–407. http://dx.doi.org/10.1007/bf02321339.

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Ravasoo, Arvi. "OS02W0110 Evaluation of plane inhomogeneous stress field by ultrasonic boundary measurements." Abstracts of ATEM : International Conference on Advanced Technology in Experimental Mechanics : Asian Conference on Experimental Mechanics 2003.2 (2003): _OS02W0110. http://dx.doi.org/10.1299/jsmeatem.2003.2._os02w0110.

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Saada, Georges. "Stress Field Associated with Interfaces." Materials Science Forum 189-190 (July 1995): 149–54. http://dx.doi.org/10.4028/www.scientific.net/msf.189-190.149.

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Godfrey, M. J. "Stress field in quantum systems." Physical Review B 37, no. 17 (June 15, 1988): 10176–83. http://dx.doi.org/10.1103/physrevb.37.10176.

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AONO, Yuuta, and Hiroshi NOGUCHI. "Stress field of cyclic notches." Proceedings of the 1992 Annual Meeting of JSME/MMD 2000 (2000): 677–78. http://dx.doi.org/10.1299/jsmezairiki.2000.0_677.

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CHEN, Dai-Heng. "Analysis of Singular Stress Field." Transactions of the Japan Society of Mechanical Engineers Series A 62, no. 600 (1996): 1862–69. http://dx.doi.org/10.1299/kikaia.62.1862.

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Dissertations / Theses on the topic "Stress field"

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Dölle, Michael. "Field effect transistor based CMOS stress sensors /." Tönning ; Lübeck Marburg : Der Andere Verlag, 2006. http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&doc_number=016086105&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA.

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Woolard, Deonna Faye. "Thermoelastic and photoelastic full-field stress measurement." W&M ScholarWorks, 1999. https://scholarworks.wm.edu/etd/1539623969.

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Photoelasticity is an optical technique that measures the difference of the principal stresses plus the principal stress direction. A complementary technique is thermoelasticity which measures the sum of the principal stresses. Combining these two full-field, non-contact nondestructive evaluation techniques allows the individual stress components to be measured. One of the main difficulties in merging these two measurement systems is in identifying an appropriate surface coating. Thermoelasticity demands a highly emissive surface, while photoelasticity requires a thick, stress-birefringent, transparent coating with a retro-reflective backing. Two coatings have been identified that can be used for combined thermoelastic and photoelastic stress measurements: PMMA and polycarbonate.;An anisotropic electromagnetic boundary value model was developed to understand more fully the mechanisms through which photoelastic stress patterns are produced. This model produced intensity contour maps which matched the fringe patterns observed in the laboratory, and allowed the effect of measurement errors on the calculated stress tensor to be quantified. One significant source of error was the retro-reflective backing, which depolarized the light and degraded the resulting photoelastic fringes. A quantitative analysis of the degraded fringes, to be used as a rating scheme for reflective backing materials, showed that the isoclinic lines shift position as a result of the backing roughness and oblique incidence. This is a concern when calculating the stress components through the combination of photoelasticity and thermoelasticity because the data maps are integrated at the pixel level. Small shifts in the photoelastic fringes result in incorrect information being assigned to some pixels and hence lead to uncertainties in the stress tensor components. Progress in the understanding of the depolarization at the reflective backing allows the specification of new materials that will minimize this effect, as well as the development of robust computer algorithms to correct for any remaining depolarization.
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Gao, Sui. "In-plane stress analysis using tensor field photoelasticity." Thesis, University of British Columbia, 2011. http://hdl.handle.net/2429/37059.

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Few experimental methods exist for evaluating all in-plane stress components in solid materials; because of the tensor nature of these quantities. Full field measurement of all three stress components is desirable, since plastic deformation or failure can result from any combination of the three. A new photoelastic stress measurement method is presented for evaluating all three in-plane stress components within a two-dimensional photoelastic material. The measurement method is based on the observation that the complex transmission factors that describe the optical phase changes due to stress-induced birefringence have a second order tensor character, similar to that of other tensor quantities such as stress and strain. The same transformation equations and Mohr’s circle construction can be applied to the rotation of optical axis. A Michelson type interferometer and phase shifting are used to quantify the phases of the complex transmission factors. Mohr’s circle calculation is applied to obtain the principal transmission factors and principal axis orientation. The principal stresses are then obtained from the principal transmission factors through the stresss optical relationship. The effectiveness of this technique is demonstrated by comparing the experimental and analytical results for a hollow circular ring under diametric compression.
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Cristiano, Elena <1988&gt. "Stress Field and Seismicity at Campi Flegrei Caldera." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2016. http://amsdottorato.unibo.it/7555/1/cristiano_elena_tesi2.pdf.

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Aim of this work is the study of the stress field in the Campi Flegrei caldera during the bradyseismic crisis of 1982-1984. n the first part of the work has been analysed old cretaceous and digital seismic datasets relative to 70th years, and the bradyseismic crisis of 1982-1984 where has been recorded the earthquakes linked to uplifts that interested Campi flegrei caldera during 1969-72 and 1982-84. The seismicity dataset has been used to made some analysis as location and focal mechanisms generation. The focal mechanisms are than analysed using two software to determine the principal state of stress that was predominant in that period. Then, starting from ground deformation data, relative to 1100 optical levelling measure done during the bradyseismic crisis, has been use the inversion method to modelling the source of the deformation. Has been used many model as the Mogi model, the penny shaped-crack, and the rectangular crack of Okada. Consequently, a joint inversion was applicate on ground deformation data and seismicity together to better understand the dynamic of the stress in the area.In the last part of the work, has been determined the excess of pore pressure in the Flegrean area, using focal mechanisms to study the influence of fluid pore pressure on change in the Coulomb stress of the area. Has been used the Coulomb-Navier criterion and Terakawa method (2010) to estimate the excess of pore pressure. Finally, in order to evaluate the reliability of the calculated pore pressures, was done thermo-fluid dynamic simulation and analysed the hydrothermal system of Campi Flegrei caldera. So, has been performed a series of simulation thermo-fluid dynamic injecting a flow in the system varying temperature, pressure and injection rate to model the Campi Flegrei caldera during the unrest.
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Cristiano, Elena <1988&gt. "Stress Field and Seismicity at Campi Flegrei Caldera." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2016. http://amsdottorato.unibo.it/7555/.

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Aim of this work is the study of the stress field in the Campi Flegrei caldera during the bradyseismic crisis of 1982-1984. n the first part of the work has been analysed old cretaceous and digital seismic datasets relative to 70th years, and the bradyseismic crisis of 1982-1984 where has been recorded the earthquakes linked to uplifts that interested Campi flegrei caldera during 1969-72 and 1982-84. The seismicity dataset has been used to made some analysis as location and focal mechanisms generation. The focal mechanisms are than analysed using two software to determine the principal state of stress that was predominant in that period. Then, starting from ground deformation data, relative to 1100 optical levelling measure done during the bradyseismic crisis, has been use the inversion method to modelling the source of the deformation. Has been used many model as the Mogi model, the penny shaped-crack, and the rectangular crack of Okada. Consequently, a joint inversion was applicate on ground deformation data and seismicity together to better understand the dynamic of the stress in the area.In the last part of the work, has been determined the excess of pore pressure in the Flegrean area, using focal mechanisms to study the influence of fluid pore pressure on change in the Coulomb stress of the area. Has been used the Coulomb-Navier criterion and Terakawa method (2010) to estimate the excess of pore pressure. Finally, in order to evaluate the reliability of the calculated pore pressures, was done thermo-fluid dynamic simulation and analysed the hydrothermal system of Campi Flegrei caldera. So, has been performed a series of simulation thermo-fluid dynamic injecting a flow in the system varying temperature, pressure and injection rate to model the Campi Flegrei caldera during the unrest.
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Blake, Kelly. "Crustal Stress Heterogeneity in the Vicinity of a Geothermal Field: Coso Geothermal Field, CA." Master's thesis, Temple University Libraries, 2011. http://cdm16002.contentdm.oclc.org/cdm/ref/collection/p245801coll10/id/152710.

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Geology
M.S.
Borehole induced structures seen in image logs from the Coso Geothermal Field, CA record variation in the azimuth of principal stress. Image logs of these structures from five boreholes were analyzed to quantify the stress heterogeneity for three geologically distinct locations: two boreholes within the Coso Geothermal Field (one in an actively produced volume), two on the margin of the Coso Geothermal Field and outside the production area, and a control borehole several tens of kilometers south of the Coso Geothermal Field. Average directions of Shmin and its standard deviation are similar along the eastern portion of the geothermal field at ~107 ± 28°; this is distinct from the western portion which has an azimuth of 081 ± 18° and also distinct from outside the geothermal field where the average azimuth is 092 ± 47°. These relationships suggest a correlation of stress orientation and heterogeneity with slip on the Coso Wash fault, suggesting that ~20 years of production has not affected the Shmin.orientation. The slope of power spectrum quantifies the length-scale dependence of stress rotations for the volume of the brittle crust penetrated by each borehole. Spectral analysis was applied to the depth variation of stress direction and it demonstrates that: (1) the data set contains distinct wavelengths of stress rotation, (2) that the relative power of these wavelengths in the total scaling of stress directions demonstrates a fractal distribution and (3) in a manner consistent with earthquakes causing the stress rotations. While the vertically averaged Shmin orientation for the three eastern boreholes varied by as little as 1°, the spectral slopes varied by 0.4 log (deg2 *m)(m) from the inside to the margin unproduced areas of the Coso Geothermal Field. The two boreholes inside the field had spectral slopes within one standard deviation, even though Shmin orientations were not parallel. These results suggest that at the kilometer length scale, the source of stress heterogeneity is dominated by proximity to recent fault slip, whereas the centimeter to meter stress heterogeneity is dominated by earthquake activity.
Temple University--Theses
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Bas, Gokcen. "Electric Field Analysis In Stress Controlled High Voltage Cables." Master's thesis, METU, 2005. http://etd.lib.metu.edu.tr/upload/12605778/index.pdf.

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The terminations and the joints are the basic accessories of the power cables. Power cables require electrical stress control when terminated. Since there are different types of terminations, the analysis should be done to choose the proper method for electric field control problem at the terminations. Throughout this study two different types of termination methods are investigated by using the finite element analysis program (ANSYS): Stress Controlled Termination Model with Deflector and Stress Control Tube (SCT). The results are compared with those obtained for a cable without stress control model termination. The numerical calculations are also compared with the measurements obtained by an experimental model: the electrolytic tank model.
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Riggenbach, Kane Ryan. "Finite Geometry Correction Factors for the Stress Field and Stress Intensities at Transverse Fillet Welds." Case Western Reserve University School of Graduate Studies / OhioLINK, 2012. http://rave.ohiolink.edu/etdc/view?acc_num=case1339121761.

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MYGDALSKYY, VOLODYMYR. "Analysis of stress field of box-like shells with cracks." 京都大学 (Kyoto University), 2002. http://hdl.handle.net/2433/149381.

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Hussey, I. W. "The influence of notch stress field on fatigue crack growth." Thesis, University of Portsmouth, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.372739.

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Books on the topic "Stress field"

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Ove, Stephansson, and SpringerLink (Online service), eds. Stress Field of the Earth’s Crust. Dordrecht: Springer Science+Business Media B.V., 2010.

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Zang, Arno, and Ove Stephansson. Stress Field of the Earth’s Crust. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-8444-7.

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Choudhury, Shuvasish, and Debojyoti Moulick. Response of Field Crops to Abiotic Stress. Boca Raton: CRC Press, 2022. http://dx.doi.org/10.1201/9781003258063.

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H, Ice Gillian, and James Gary D, eds. Measuring stress in humans: A practical guide for the field. Cambridge: Cambridge University Press, 2007.

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Radaj, Dieter. Heat Effects of Welding: Temperature Field, Residual Stress, Distortion. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992.

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Program, Canada Centre For Mineral and Energy Technology Mineral Research. Field Stress Determinations at Macassa Mine, Kirkland Lake, Ontario. S.l: s.n, 1985.

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Radaj, Dieter. Heat effects of welding: Temperature field, residual stress, distortion. Berlin: Springer, 1992.

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Y, Leshem Ya'acov, ed. Stress and stress coping in cultivated plants. Dordrecht: Kluwer Academic Publishers, 1994.

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Ballarini, R. Three-dimensional analysis of surface crack-Hertzian stress field interaction. Cleveland, Ohio: Lewis Research Center, 1989.

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Hussey, Ian W. The influence of notch stress field on fatigue crack growth. Portsmouth: Portsmouth Polytechnic,Department of Mechanical Engineering, 1986.

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Book chapters on the topic "Stress field"

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Eringen, A. Cemal. "Stress." In Microcontinuum Field Theories, 35–56. New York, NY: Springer New York, 1999. http://dx.doi.org/10.1007/978-1-4612-0555-5_2.

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Zang, Arno, and Ove Stephansson. "Global Stress." In Stress Field of the Earth’s Crust, 253–76. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-8444-7_11.

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Zang, Arno, and Ove Stephansson. "Stress Definition." In Stress Field of the Earth’s Crust, 17–35. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-8444-7_2.

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Zang, Arno, and Ove Stephansson. "Generic Stress Data." In Stress Field of the Earth’s Crust, 225–52. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-8444-7_10.

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Zang, Arno, and Ove Stephansson. "Rock Stress Terminology." In Stress Field of the Earth’s Crust, 63–87. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-8444-7_4.

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Zang, Arno, and Ove Stephansson. "Crustal Stress Models." In Stress Field of the Earth’s Crust, 89–111. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-8444-7_5.

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Zang, Arno, and Ove Stephansson. "Local Stress Data." In Stress Field of the Earth’s Crust, 195–223. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-8444-7_9.

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Cardy, John. "The Stress Tensor In Quenched Random Systems." In Statistical Field Theories, 215–22. Dordrecht: Springer Netherlands, 2002. http://dx.doi.org/10.1007/978-94-010-0514-2_20.

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Vavryčuk, Václav. "Earthquake Mechanisms and Stress Field." In Encyclopedia of Earthquake Engineering, 1–21. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-36197-5_295-1.

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Vavryčuk, Václav. "Earthquake Mechanisms and Stress Field." In Encyclopedia of Earthquake Engineering, 728–46. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-35344-4_295.

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Conference papers on the topic "Stress field"

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Ohkubo, Tadakatsu, Yoshihiko Hirotsu, and Kiyoshi Nikawa. "Molecular dynamics simulation of electromigration under electric field." In STRESS INDUCED PHENOMENA IN METALLIZATION. ASCE, 1998. http://dx.doi.org/10.1063/1.54684.

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Kodera, Masako, Sachiyo Ito, Masahiko Hasunuma, Shigeru Kakinuma, Shinichi Ogawa, Paul S. Ho, and Ehrenfried Zschech. "Nanometer-Scale Stress Field Evaluation of Cu∕ILD Structure by Cathodoluminescence Spectroscopy." In Stress-induced Phenomena in Metallization. AIP, 2007. http://dx.doi.org/10.1063/1.2815775.

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Abolfazlzadeh, Yousef, and Stephen McKinnon. "Stress field characterisation in Nickel Rim South Mine using seismic stress inversion." In Eighth International Conference on Deep and High Stress Mining. Australian Centre for Geomechanics, Perth, 2017. http://dx.doi.org/10.36487/acg_rep/1704_16_abolfazlzadeh.

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Luo, Y., and M. B. Dusseault. "Local Stress Estimates and Far-Field Stress History, Ordos, China." In SPE/ISRM Rock Mechanics in Petroleum Engineering. Society of Petroleum Engineers, 1998. http://dx.doi.org/10.2118/47321-ms.

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Okamoto, Kyosuke, Hitoshi Mikada, Tada-nori Goto, and Junichi Takekawa. "Stress field monitoring using seismic scattering." In SEG Technical Program Expanded Abstracts 2012. Society of Exploration Geophysicists, 2012. http://dx.doi.org/10.1190/segam2012-1272.1.

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Turcotte, Pascal. "Field behaviour of hybrid bolt at LaRonde Mine." In Fifth International Seminar on Deep and High Stress Mining. Australian Centre for Geomechanics, Perth, 2010. http://dx.doi.org/10.36487/acg_repo/1074_22.

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Yang, Shu-Xin, Lu-Yuan Huang, Rui Yao, and Qi Mi. "Numerical Simulation of Crustal Stress Field in China Based on Stress Measurement." In Near Surface Geophysics Asia Pacific Conference, Beijing, China 17-19 July 2013. Society of Exploration Geophysicists, Australian Society of Exploration Geophysicists, Chinese Geophysical Society, Korean Society of Earth and Exploration Geophysicists, and Society of Exploration Geophysicists of Japan, 2013. http://dx.doi.org/10.1190/nsgapc2013-132.

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"BIOFEEDBACK SYSTEMS FOR STRESS REDUCTION - Towards a Bright Future for a Revitalized Field." In Special Session on Biofeedback Systems for Stress Reduction. SciTePress - Science and and Technology Publications, 2012. http://dx.doi.org/10.5220/0003894904990504.

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Dimitriu, Laurentiu, Liliana Vornicu, and Ioan Micu. "Complex Generator of Anti-Stress Electromagnetic Field." In International Body Engineering Conference & Exhibition and Automotive & Transportation Technology Congress. 400 Commonwealth Drive, Warrendale, PA, United States: SAE International, 2002. http://dx.doi.org/10.4271/2002-01-2210.

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Aben, Hillar K., Siim J. Idnurm, Juri Josepson, Kalle-Juri E. Kell, and Alfred E. Puro. "Optical tomography of the stress tensor field." In Analytical Methods for Optical Tomography, edited by Gennady G. Levin. SPIE, 1992. http://dx.doi.org/10.1117/12.131894.

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Reports on the topic "Stress field"

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DeGiorgi, Virginia G. Stress Field Variations during Dynamic Loading. Fort Belvoir, VA: Defense Technical Information Center, October 1991. http://dx.doi.org/10.21236/ada242121.

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Larochelle, S., Y. Liu, and H. Kao. Poroelastic modeling of hydraulic fracturing induced earthquake stress field. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/297811.

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Girrens, S. P., J. G. Bennett, and D. M. Murphy. Poloidal field coil stress analysis for the ZTH machine. Office of Scientific and Technical Information (OSTI), February 1988. http://dx.doi.org/10.2172/6986062.

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Castillo, D. A. ,., and L. W. Younker. A High shear stress segment along the San Andreas Fault: Inferences based on near-field stress direction and stress magnitude observations in the Carrizo Plain Area. Office of Scientific and Technical Information (OSTI), January 1997. http://dx.doi.org/10.2172/490160.

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Boutros, Karim. Investigation of Lattice and Thermal Stress in GaN/A1GaN Field-Effect Transistors. Fort Belvoir, VA: Defense Technical Information Center, October 2006. http://dx.doi.org/10.21236/ada456241.

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Crawford, Timothy L., and Gennaro H. Crescenti. Spatial Variation of Wind Stress and Wave Field in the Shoaling Zone. Fort Belvoir, VA: Defense Technical Information Center, September 2000. http://dx.doi.org/10.21236/ada610178.

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Crawford, Timothy L., and Gennaro H. Crescenti. Spatial Variation of Wind Stress and Wave Field in the Shoaling Zone. Fort Belvoir, VA: Defense Technical Information Center, August 2001. http://dx.doi.org/10.21236/ada627971.

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Crawford, Timothy L. Spatial Variation of Waves, Stress and Wind Field in the Shoaling Zone. Fort Belvoir, VA: Defense Technical Information Center, September 1997. http://dx.doi.org/10.21236/ada633472.

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Boutros, Karim. Investigation of Lattice and Thermal Stress in GaN/AlGaN Field-Effect Transistors. Fort Belvoir, VA: Defense Technical Information Center, May 2007. http://dx.doi.org/10.21236/ada467566.

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Keeney-Walker, J., B. R. Bass, and J. D. Landes. An investigation of crack-tip stress field criteria of predicting cleavage-crack initiation. Office of Scientific and Technical Information (OSTI), September 1991. http://dx.doi.org/10.2172/5205137.

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