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The map shows borehole locations, geomorphic features and selected profiles (S1-S4) in the study area. Inset: Map of Gujarat state, rectangle shows the study area, and the star indicates epicentre of the 2001 Bhuj earthquake Mw 7.7.  

The map shows borehole locations, geomorphic features and selected profiles (S1-S4) in the study area. Inset: Map of Gujarat state, rectangle shows the study area, and the star indicates epicentre of the 2001 Bhuj earthquake Mw 7.7.  

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Article
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ABSTRACT Estimation of liquefaction resistance, also called Cyclic Resistance Ratio (CRR) of soil, is an important aspect of geotechnical earthquake engineering; it is one of the most important secondary effects of earthquake which causes severe damages to engineering structures. The liquefaction potential is estimated in terms of factor of safety...

Contexts in source publication

Context 1
... low land regions are further classified into flood plain, bad land, terrace, point bar, channel bar and recent channel. The Sabarmati river flows through the middle of the Ahmedabad city (Figure 1), which dries up in summer leaving only a small stream of water. Topographically, the study area is almost flat in nature except few small hills of Thaltej-Jodhpur Tekra. ...
Context 2
... order to study the subsurface lithological characteristics of the region, a total of 23 boreholes (11 of 80m depth, six of 40m depth and five of 35m depth) were drilled at different locations ( Figure 1). During drilling the soil samples, both disturbed and undisturbed, were collected for geotechnical investigation. ...
Context 3
... cross sections, two east-west (S1, S2) and two north- south (S3, S4), were made for vertical correlation of the subsurface lithology of the study area (Figure 1). The section Figure 2. Fine content, clay % and liquid limit. ...

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Citations

... Dixit et al. [9] evaluated the seismic soil liquefaction in terms of LPI for 142 sites in Mumbai city using SPT based on a simplified empirical procedure. Dwivedi et al. [10] estimated the liquefaction potential for Ahmedabad city using N-SPT for 23 boreholes based on the approach of Idriss and Boulanger [6]. Gurung and Chatterjee [12] conducted a study to assess Kolkata city's liquefaction potential by evaluating the factor of safety against liquefaction (F S ), based on the Standard Penetration Test N-SPT values using the deterministic approaches, as per Idriss and Boulanger [6] and IS 1893: Part 1 [13]. ...
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... Few studies for liquefaction potential based on SPT data for Kolkata region done by [2,10] and other region i.e. Roorkee Region by [14][15][16] Guwahati region [17] Mumbai [18] Ahmedabad region [19] and Chandigarh region [20]. [21] Developed relationship between SPT N and Shear wave velocity for Roorkee region. ...
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Liquefaction is the phenomena in which the saturated fine sand loses its shear strength and stiffness when a cyclic or an earthquake loading. The evaluation of liquefaction potential and seismic microzonation of a certain area can be done. Ground improvement requirement of a site is conducted after the evaluation of liquefaction potential of that site. The aim of the present study is to evaluate of liquefaction potential for AIIMS kalyani Campus, Kolkata. Kalyani is a city which comes under Nadia district, of west Bengal it is located around 50 km from Kolkata city. The main objective of the present study is to evaluate the liquefaction potential of AIIMS Kalyani Campus for different magnitudes of earthquake i.e. 7.5, 7.0 and 6.5 and peak ground acceleration (a max = 0.16g). For this purpose, the factor of safety against liquefaction was evaluated at different depths for the six sites in AIIMS Kalyani campus based on SPT-Based approached. It was found that the factor of safety against the liquefaction for magnitude of earthquake 6.5 is marginally greater than that 7.5 and 7.0 for all the sites. It can be observed that from the results that the FOS against for 6.5 magnitude earthquake is 21% greater than that for 7.0 magnitude earthquake.
... The SPT-N blow count and lithology were recorded during the sampling in the field and index properties of the disturbed and undisturbed samples of the soils, like grainsize analysis, Atterberg test, density, specific gravity was obtained and used for the seismic hazard assessment (Cavallaro et al. 2016). More than one thousand samples were collected (Dwivedi et al. 2017) and used for the seismic hazard assessment. The lithology of the study area generally varies from silty sand to clayey sand. ...
... The lithological variations delineated from 23 boreholes suggest that the Ahmedabad City area made up of different layers of gravel, sand, and silty-clay (Dwivedi et al. 2017). The sediment layers encountered in the boreholes have shown distinct variations in their thickness and shapes from location to location. ...
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Ahmedabad, the most populous city of Gujarat, assigned zone III in the seismic zone map of India (BIS 2002), has experienced moderate earthquakes in the past. Several high-rise buildings were collapsed or severely damaged in the city during 2001 Bhuj earthquake (Mw 7.6), which was 240 km from the city. Keeping this in view, micro-level seismic hazard assessment in the city is carried out using geotechnical, geological, and geophysical inputs, which may help in designing buildings and other civil engineering structures and will reduce the probability of loss of life and property in this region. A total of 23 boreholes, 11 boreholes of 80 m, 7 boreholes of 40 m and 5 boreholes of 35 m) were drilled at the different locations in the city. To estimate the shear-wave velocity, we have employed direct and indirect methods. PS logging is carried out in 11 boreholes, and shallow geophysical investigation (multi-channel analysis of surface waves, MASW) is carried out at 54 sites. The field and laboratory tests on soil samples, geophysical investigations, and seismotectonic information enabled us to estimate soil overburden thickness, shear-wave velocity, factor of safety against liquefaction, and site response in terms of amplification factor. The peak ground acceleration was estimated at engineering bed rock level (Vs 760 m/s) by PSHA. All this information is used in preparing an integrated seismic hazard (SH) map of the Ahmedabad City using analytical hierarchal process. The seismic hazard map is characterized into three broad categories: low, moderate, and high. The western part of the Ahmedabad shows the highest hazard. The northern and the eastern parts show moderate seismic hazard. It is observed that the presence of sand and flood plain deposits along the Sabarmati river increases the hazard. The study has also highlighted that the presence of a paleochannel increases the overall hazard, which is clearly visible in integrated hazard map.
... Rao and Satyam (2007) determined liquefaction studies for Delhi region based on SPT. Ahmad et al. (2015) conducted the SPT for liquefaction potential for Lucknow city and Dwivedi et al. (2017) carried out evaluation of liquefaction potential of sites in the Ahmedabad city. ...
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Before taking the task of any ground improvement, rational evaluation of the liquefaction potential of the zone becomes necessary. It is taken up on various considerations such as importance of the area, seismic vulnerability etc. The objectives of the present work are the assessment of liquefaction potential for Ramgarh Tal site in Gorakhpur city, India. Gorakhpur city is located along the banks of the Rapti River in the northeastern portion of the Indian state of Uttar Pradesh and is developing at a fast rate. This city lies in Zone IV of seismic zone in India. Thus, it is necessary to evaluate the liquefaction potential for designing of civil engineering structures and their foundations in the Gorakhpur city. In the present work, two different approaches namely the simplified method and the ground response analysis was employed to evaluate the cyclic shear ratio. For different depths for Ramgarh Tal Site, the factor of safety against liquefaction was examined using both the above-mentioned approaches. It was found that the ground response analysis gave significantly smaller factors of safety against liquefaction as compared to the simplified method. Thus, ground response analysis is more rational and results in smaller factor of safety against liquefaction. For safe design it is recommended to use this method in the analysis. Thus, it was concluded that use of simplified method for evaluating factor of safety against liquefaction might not be appropriate.