Please use this identifier to cite or link to this item: https://dspace.iiti.ac.in/handle/123456789/11421
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dc.contributor.authorNeelima Satyam, D.en_US
dc.date.accessioned2023-03-07T11:45:23Z-
dc.date.available2023-03-07T11:45:23Z-
dc.date.issued2023-
dc.identifier.citationZahoor, F., Seshagiri Rao, K., Wani, F. S., Andrabi, S. M., & Satyam, N. (2023). Evaluation of site effects using HVSR measurements along srinagar metro alignment, jammu and kashmir doi:10.1007/978-981-19-6998-0_34 Retrieved from www.scopus.comen_US
dc.identifier.isbn978-9811969973-
dc.identifier.issn2366-2557-
dc.identifier.otherEID(2-s2.0-85147995806)-
dc.identifier.urihttps://doi.org/10.1007/978-981-19-6998-0_34-
dc.identifier.urihttps://dspace.iiti.ac.in/handle/123456789/11421-
dc.description.abstractSrinagar metro rail is set to be constructed as part of the Mass Rapid Transport System planned for the cities of Srinagar and Jammu in Jammu and Kashmir. In this paper, we present results of single station microtremor (MHVSR) tests conducted at 27 locations along the three corridors proposed in the project. Microtremor recordings were analysed using Nakamura’s horizontal-to-vertical spectral ratio (HVSR) method. The results reveal that the fundamental frequency (f0) at the sites ranges between 0.21 and 1.16 Hz with peak H/V amplitude 2.01–5.89. At many locations, more than one peak was observed in HVSR curves signifying the presence of multiple impedance contrasts within the subsurface. Low frequency peak indicates an impedance contrast at deep depths, whereas peak at higher frequencies indicates shallow impedance contrast. Further, the results are compared with Vs30 (average shear wave velocity over 30 m depth) obtained at the same sites in a previous study by our group. It was found that f0 and Vs30 do not follow a direct correlation at majority of the sites. Locations like Batpora, Soura, Hazratbal, and Osmanabad are found to have low f0, despite having high Vs30 and characterized as site classes C and D according to NEHRP guidelines. The study concludes that these apparent anomalies essentially indicate that Vs30 might not be an appropriate proxy for site amplification, as was also pointed out by Castellaro et al. (2008) and several other authors. Consequently, a new site characterization procedure must be adopted which incorporates other parameters in addition to Vs30. © 2023, The Author(s), under exclusive license to Springer Nature Singapore Pte Ltd.en_US
dc.language.isoenen_US
dc.publisherSpringer Science and Business Media Deutschland GmbHen_US
dc.sourceLecture Notes in Civil Engineeringen_US
dc.subjectShear flowen_US
dc.subjectShear wavesen_US
dc.subjectWave propagationen_US
dc.subjectHorizontal-to-vertical spectral ratiosen_US
dc.subjectImpedance contrasten_US
dc.subjectJammu and Kashmiren_US
dc.subjectMicrotremorsen_US
dc.subjectSeismic site characterizationen_US
dc.subjectSeismic sitesen_US
dc.subjectSite characterizationen_US
dc.subjectSite effectsen_US
dc.subjectSrinagar metroen_US
dc.subjectTransport systemsen_US
dc.subjectLocationen_US
dc.titleEvaluation of Site Effects Using HVSR Measurements Along Srinagar Metro Alignment, Jammu and Kashmiren_US
dc.typeConference Paperen_US
Appears in Collections:Department of Civil Engineering

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