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ANBAZHAGAN, P.
- Effective Depth of Soil Column for Site Response Analysis of Deep Soil Sites
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Authors
Affiliations
1 School of Civil Engineering LPU, Jalandhar, Punjab − 144411, IN
2 Department of Civil Engineering, IISc, C V Raman Ave, Devasandra Layout, Bangalore − 560012, Karnataka, IN
1 School of Civil Engineering LPU, Jalandhar, Punjab − 144411, IN
2 Department of Civil Engineering, IISc, C V Raman Ave, Devasandra Layout, Bangalore − 560012, Karnataka, IN
Source
Indian Journal of Science and Technology, Vol 9, No 44 (2016), Pagination:Abstract
Background: Seismic site response analyses are routinely performed for shallow soil deposits. In the seismic site response studies, depth of input motion which is also called as the depth of half-space or bedrock and is one of the important parameters which influence the amplification and attenuation characteristics of any particular site. Objectives: Finding the exact location of bedrock for deep soil deposits is difficult and uneconomical. Hence, there is a need to identify the effective depth of soil column for deep soil sites to get representative site response parameters. Statistical Analysis: In the present study, recorded bedrock and surface earthquake data with soil profiles is used to identify the matching modulus and damping curves for widely available deep soil types and investigated the depth of half-space for site response study of deep soil sites. Eleven deep soil profiles having minimum depth of 100m and maximum depth of 800 m with different sets of recorded earthquake time histories from Kiban Kyoshin network are used for the study. Nonlinear site response analyses were carried out using the program DEEPSOIL. Suitable shear modulus and damping curves are identified by a parametric study of varying shear modulus and damping curves for a matching computed response spectrum with the measured response spectrum. Soil properties and model curves are frozen for each profile, which are further used to identify the depth of half space. Findings: Perfect matching layer having shear wave velocity and depth has been analysed, the study indicated that location of half-space is independent of depth factor. However, it is noticed in the study that computed response spectrum is close to the measured response spectrum when input is given for layer having shear wave velocity of 760 m/s±100.This layer represents a depth of half space for site response analysis of the deep soil column. Application: We can utilize the finding to perform for better accuracy and consistent results based on current findings and same can be used for site response studies.Keywords
Earthquake, Effective Depth of Soil Column, Input Motion, Response Spectrum, Site Response.- Establishing Empirical Correlation between Sediment Thickness and Resonant Frequency using HVSR for the Indo-Gangetic Plain
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Authors
Affiliations
1 Department of Civil Engineering, Indian Institute of Science, Bengaluru 560 012, IN
1 Department of Civil Engineering, Indian Institute of Science, Bengaluru 560 012, IN
Source
Current Science, Vol 117, No 9 (2019), Pagination: 1482-1491Abstract
In this study, microtremor survey was carried out at 31 locations of Indo-Gangetic Plains (IGP) using a pair of portable three-component short-period seismometers (Guralp CMG-6T-1) and Kelunji Echo Pro digital data acquisition system. The acquired raw data was processed to obtain the average H/V ratio of the ambient vibration spectrum. The frequency corresponding to the first peak of the average H/V spectrum was taken as resonant frequency of that particular site. A comparison was made between the resonant frequencies obtained from peak of the H/V spectrum with those obtained using the source–receiver function from previously published work. The results were in good agreement with each other. An empirical equation has been established for the IGP by relating resonance frequency with sediment thickness, using available data from nearby boreholes drilled up to bedrock. The empirical equation was compared with other equations available for deep soil sites, i.e. sites with soil thickness more than 750 m. Further, a combined equation was developed for the digitized data taken from previously published works of deep soil sites. Finally, it has been found that the regionspecific equation gives better estimate of sediment thickness than the other empirical equations; but in absence of such a region-specific equation, the proposed combined equation can be used for a quick preliminary assessment of sediment thickness of a deep soil region.Keywords
HVSR Method, Indo-Gangetic Plains, Microtremor, Resonant Frequency, Sediment Thickness.References
- Andrews, D. J., Separation of source and propagation spectra of seven mammoth lakes after-shocks, In Proceedings of Workshop 16 Dynamic characteristics of faulting, 1982, pp. 82– 591.
- Iwata, T., Separation of source, propagation and site effects from observed S-waves. Zisin, Ser. 2, 1986, 39, 579–593.
- Çelebi, M., Topographical and geological amplifications determined from strong-motion and aftershock records of the 3 March 1985 Chile earthquake. B. Seismol. Soc. Am., 1987, 77, 1147– 1167.
- Field, E. H., Hough, S. E. and Jacob, K. H., Using microtremors to assess potential earthquake site response: a case study in Flushing Meadows, New York City. B. Seismol. Soc. Am., 1990, 80, 1456– 1480.
- Hough, S. E., Seeber, L., Lerner-Lam, A., Armbruster, J. C. and Guo, H., Empirical Green's function analysis of Loma Prieta aftershocks. B. Seismol. Soc. Am., 1991, 81, 1737–1753.
- Takemura, M., Kato, K., Ikeura, T. and Shima, E., Site amplification of S-waves from strong motion records in special relation to surface geology. J. Phys. Earth, 1991, 39, 537–552.
- Kato, K., Takemura, M., Ikeura, T., Urao, K. and Uetake, T., Preliminary analysis for evaluation of local site effects from strong motion spectra by an inversion method. J. Phys. Earth, 1992, 40, 175–191.
- Tai, M., Iwasaki, Y. and Oue, M., Separation of source, propagation and local site effects from accelerographs and its application to predict strong ground motion by summing small events. In Proceedings of the 10th World Conference on Earthquake Engineering, 1992, vol. 2, pp. 747–750.
- Kowada, A., Tai, M., Iwasaki, Y. and Irikura, K., Evaluation of horizontal and vertical strong ground motions using empirical site-specific amplification and phase characteristics. J. Struct. Constr. Eng., 1998, 97–104.
- Nakamura, Y., A method for dynamic characteristics estimation of subsurface using microtremor on the ground surface. QR Railway Tech. Res. Inst., 1989, 30, 25–33.
- Paudyal, Y. R., Yatabe, R., Bhandary, N. P. and Dahal, R. K., Basement topography of the Kathmandu Basin using microtremor observation. J. Asian Earth Sci., 2013, 62, 627–637.
- Field, E. and Jacob, K., The theoretical response of sedimentary layers to ambient seismic noise. Geophys. Res. Lett., 1993, 20, 2925–2928.
- Lachet, C. and Bard, P. Y., Numerical and theoretical investigations on the possibilities and limitations of Nakamura’s technique. J. Phys. Earth, 1994, 42, 377–397.
- Ibs-von Seht, M. and Wohlenberg, J., Microtremor measurements used to map thickness of soft sediments. B. Seismol. Soc. Am., 1999, 89, 250–259.
- Bour, M., Fouissac, D., Dominique, P. and Martin, C., On the use of microtremor recordings in seismic microzonation. Soil Dyn. Earthq. Eng., 1998, 17, 465–474.
- Delgado, J., Casado, C. L., Estevez, A., Giner, J., Cuenca, A. and Molina, S., Mapping soft soils in the Segura river valley (SE Spain): a case study of microtremors as an exploration tool. J. Appl. Geophys., 2000, 45, 19–32.
- Tuladhar, R., Cuong, N. N. H. and Yamazaki, F., Seismic microzonation of Hanoi, Vietnam using microtremor observations. In 13th world conference on earthquake engineering Vancouver, BC, Canada, 2004, p. 2539.
- Hasancebi, N. and Ulusay, R., Evaluation of site amplification and site period using different methods for an earthquake-prone settlement in Western Turkey. Eng. Geol., 2006, 87, 85–104.
- Langston, C. A., Chiu, S. C. C., Lawrence, Z., Bodin, P. and Horton, S., Array observations of microseismic noise and the nature of H/V in the Mississippi embayment. B. Seismol. Soc. Am., 2009, 99, 2893–2911.
- Mucciarelli, M., Ambient noise measurements following the 2011 Christchurch earthquake: relationships with previous microzonation studies, liquefaction, and nonlinearity. Seismol. Res. Lett., 2011, 82, 919–926.
- Paudyal, Y. R., Bhandary, N. P. and Yatabe, R., Seismic microzonation of densely populated area of Kathmandu Valley of Nepal using microtremor observations. J. Earthq. Eng., 2012, 16, 1208– 1229.
- Paudyal, Y. R., Yatabe, R., Bhandary, N. P. and Dahal, R. K., A study of local amplification effect of soil layers on ground motion in the Kathmandu Valley using microtremor analysis. Earthq. Eng. Eng. Vib., 2012, 11, 257–268.
- Dinesh, B. V., Nair, G. J., Prasad, A. G. V., Nakkeeran, P. V. and Radhakrishna, M. C., Estimation of sedimentary layer shear wave velocity using micro-tremor H/V ratio measurements for Bangalore city. Soil Dyn. Earthq. Eng., 2010, 30, 1377–1382.
- Sukumaran, P., Parvez, I. A., Sant, D. A., Rangarajan, G. and Krishnan, K., Profiling of late Tertiary–early Quaternary surface in the lower reaches of Narmada valley using microtremors. J. Asian Earth Sci., 2011, 41, 325–334.
- Natarajan, T. and Rajendran, K., Estimates of site response based on spectral ratio between horizontal and vertical components of ambient vibrations in the source zone of 2001 Bhuj earthquake. J. Asian Earth Sci., 2015, 98, 85–97.
- Natarajan, T. and Rajendran, K., Site responses based on ambient vibrations and earthquake data: a case study from the meizoseismal area of the 2001 Bhuj earthquake. J. Seismol., 2017, 21, 335– 347.
- Sant, D. A., Parvez, I. A., Rangarajan, G., Patel, S. J., Bhatt, M. N. and Salam, T. S., Subsurface profiling along Banni Plains and bounding faults, Kachchh, Western India using microtremors method. J. Asian Earth Sci., 2017, 146, 326–336.
- Joshi, A. U. et al., Subsurface profiling of granite pluton using microtremor method: southern Aravalli, Gujarat, India. Int. J. Earth Sci., 2018, 107, 191–201.
- Burrard, S. G., On the origin of the Indo-Gangetic trough, commonly called the Himalayan foredeep. Proc. R. Soc. London A, 1915, 91, 220–238.
- Singh, M., The Gangar River: Fluvial Geomorphology, Sedimentation Processes and Geochemical Studies, Doctoral dissertation, Heidelberg University, 1995.
- GSI, Seismo-tectonic Atlas of India and its Environs, Geological Survey of India, 2000.
- Sastri, V. V., Bhandari, L. L., Raju, A. T. R. and Datta, A. K., Tectonic framework and subsurface stratigraphy of the Ganga basin. Geol. Soc. India, 1971, 12, 222–233.
- Srivatsava, A. B., District resource maps of Geological Survey of India, Kanpur, Uttar Pradesh, India, 2001.
- Srinivas, D., Srinagesh, D., Chadha, R. K. and Ravi Kumar, M., Sedimentary thickness variations in the Indo-Gangetic foredeep from inversion of receiver functions. B. Seismol. Soc. Am., 2013, 103, 2257–2265.
- Manglik, A., Adilakshmi, L., Suresh, M. and Thiagarajan, S., Thick sedimentary sequence around Bahraich in the northern part of the central Ganga foreland basin. Tectonophysics, 2015, 653, 33–40.
- Konno, K. and Ohmachi, T., Ground-motion characteristics estimated from spectral ratio between horizontal and vertical components of microtremor. B. Seismol. Soc. Am., 1998, 88, 228– 241.
- SESAME Guideline for the implementation of the H/V spectral ratio technique on ambient vibrations: measurements, processing and interpretation. SESAME European research project, 2004, WP12, pp 1–62.
- Srinagesh, D., Singh, S. K., Chadha, R. K., Paul, A., Suresh, G., Ordaz, M. and Dattatrayam, R. S., Amplification of seismic waves in the central Indo-Gangetic basin, India. B. Seismol. Soc. Am., 2011, 101, 2231–2242.
- Parolai, S., Bormann, P. and Milkereit, C., New relationships between Vs, thickness of sediments, and resonance frequency calculated by the H/V ratio of seismic noise for the Cologne area (Germany). B. Seismol. Soc. Am., 2002, 92, 2521–2527.
- Hinzen, K. G., Weber, B. and Scherbaum, F., On the resolution of H/V measurements to determine sediment thickness, a case study across a normal fault in the Lower Rhine Embayment, Germany. J. Earthq. Eng., 2004, 8, 909–926.
- Birgören, G., Özel, O. and Siyahi, B., Bedrock depth mapping of the coast south of Istanbul: comparison of analytical and experimental analyses. Turk. J. Earth Sci., 2009, 18, 315–329.
- Özalaybey, S., Zor, E., Ergintav, S. and Tapırdamaz, M. C., Investigation of 3-D basin structures in the Izmit Bay area (Turkey) by single-station microtremor and gravimetric methods. Geophys. J. Int., 2011, 186, 883–894.
- Biswas, R., Baruah, S. and Bora, D. K., Mapping sediment thickness in Shillong City of Northeast India through empirical relationship. J. Earthq., 2015, 572619-1-8.
- Del Monaco, F., Durante, F., Macerola, L. and Tallini, M., Quaternary sedimentary cover thickness versus seismic noise resonance frequency in Western L’ Aquila Plain, 2015; http://www3.ogs.trieste.it/gngts/files/2015/S22/Riassunti/DelMonaco.pdf
- Khan, S. and Khan, M. A., Mapping sediment thickness of Islamabad city using empirical relationships: Implications for seismic hazard assessment. J. Earth Syst. Sci., 2016, 125, 623–644.
- An Inexpensive Foldscopic Approach for Quantitative Evaluation of the Shape of Sand Particles
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PDF Views:75
Authors
Kunjari Mog
1,
P. Anbazhagan
1
Affiliations
1 Department of Civil Engineering, Indian Institute of Science, Bengaluru 560 012, IN
1 Department of Civil Engineering, Indian Institute of Science, Bengaluru 560 012, IN
Source
Current Science, Vol 124, No 4 (2023), Pagination: 457-466Abstract
Shape is a fundamental key property of any object and an important physical attribute that remains ignored, although its importance has been accepted for quite some time and is not accounted for in standard soil classification guidelines. One of the reasons for this could be the lack of inexpensive microscopic instruments or image scanners in most laboratories. This study quantifies particle shape characteristics using a cost-effective foldscope approach. Four different types of sand were used in this study and results were compared against scanning electron microscopy (SEM) measurements. In addition, the effect of the number of particles and resolution on the analysis is discussed. It was found that the foldscope-based approach yielded consistent results with SEM in measuring the aspect ratio and roundness parameter (except circularity). The variation between the two approaches was found to be less than 5% for both aspect ratio and roundness; however, a significant difference was observed in the case of circularity (more than 50%) due to the influence of resolutionKeywords
Foldscope, Image Analysis, Particle Shape, Resolution, Sand.References
- Yang, J. and Gu, X. Q., Shear stiffness of granular material at small strains: does it depend on grain size? Géotechnique, 2013, 63(2), 165–179.
- Cho, G. C., Dodds, J. and Santamarina, J. C., Particle shape effects on packing density, stiffness, and strength: natural and crushed sands. J. Geotech. Geoenviron. Eng., 2006, 132(5), 591–602.
- Senetakis, K., Anastasiadis, A. and Pitilakis, K., Normalized shear modulus reduction and damping ratio curves of quartz sand and rhyolitic crushed rock. Soils Found., 2013, 53(6), 879–893.
- Payan, M., Senetakis, K., Khoshghalb, A. and Khalili, N., Effect of gradation and particle shape on small-strain Young’s modulus and Poisson’s ratio of sands. Int. J. Geomech., 2017, 17(5), 04016120.
- Shimobe, S. and Moroto, N., A new classification chart for sand liquefaction. In Earthquake Geotechnical Engineering, A. A. Balkema, Brookfield, The Netherlands, 1995, pp. 315–320.
- Cubrinovski, M. and Ishihara, K., Maximum and minimum void ratio characteristics of sands. Soils Found., 2002, 42(6), 65–78.
- Lu, Z., Yao, A., Su, A., Ren, X., Liu, Q. and Dong, S., Re-recognizing the impact of particle shape on physical and mechanical properties of sandy soils: a numerical study. Eng. Geol., 2019, 253, 36–46.
- Krumbein, W. C. and Sloss, L. L., Stratigraphy and Sedimentation: Soil Science, 1951, vol. 71, no. 5, p. 401.
- Cox, M. R. and Budhu, M., A practical approach to grain shape quantification. Eng. Geol., 2008, 96(1–2), 1–16.
- Cybulski, J. S., Clements, J. and Prakash, M., Foldscope: origami-based paper microscope. PLoS ONE, 2014, 9(6), e98781.
- Anbazhagan, P. et al., Reconnaissance report on geotechnical effects and structural damage caused by the 3 January 2017 Tripura earth quake, India. Nat. Hazards, 2019, 98(2), 425–450.
- Foldscope Instruments: Foldscope Instrument Instruction Manual, 2017; www.foldscope.com/pages/user-guide.
- Ferreira, T. and Rasband, W., ImageJ User Guide, ImageJ/Fiji, 2012, 1, 155–161.
- Đuriš, M., Arsenijević, Z., Jaćimovski, D. and Radoičić, T. K., Optimal pixel resolution for sand particles size and shape analysis. Powder Technol., 2016, 302, 177–186.
- Russell, R. D. and Taylor, R. E., Roundness and shape of Mississippi River sands. J. Geol., 1937, 45(3), 225–267.
- Bowman, E. T., Soga, K. and Drummond, W., Particle shape characterization using Fourier descriptor analysis. Geotechnique, 2001, 51(6), 545–554.
- Carter, R. M. and Yan, Y., Measurement of particle shape using digital imaging techniques. J. Phys.: Conf. Ser., 2005, 15(1), 177–182.
- Whiteside, T. G., Boggs, G. S. and Maier, S. W., Comparing object-based and pixel-based classifications for mapping savannas. Int. J. Appl. Earth Observ. Geoinfor., 2011, 13(6), 884–893.
- Memarian, H., Balasundram, S. K. and Khosla, R., Comparison between pixel-and object-based image classification of a tropical landscape using Système Pour l’Observation de la Terre-5 imagery. J. Appl. Remote Sensing, 2013, 7(1), 073512.
- Berhane, T. M., Lane, C. R., Wu, Q., Anenkhonov, O. A., Chepinoga, V. V., Autrey, B. C. and Liu, H., Comparing pixel- and object-based approaches in effectively classifying wetland-dominated landscapes. Remote Sensing, 2017, 10(1), 46.
- Sukumaran, B. and Ashmawy, A. K., Quantitative characterization of the geometry of discrete particles. Geotechnique, 2001, 51(7), 619–627.
- Vangla, P. and Latha, G. M., Influence of particle size on the friction and interfacial shear strength of sands of similar morphology. Int. J. Geosynth. Ground Eng., 2015, 1(1), 6.