2017
DOI: 10.1061/(asce)gm.1943-5622.0000918
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Determination of Thermal Regime in Sandy Soils: Mathematical Framework ATHERES

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Cited by 6 publications
(6 citation statements)
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“…Further, from Table 1, it can be observed that the k of the MSW varies between 0.01 and 1.50 W/(m K) (Bonany et al, 2013;Hanson et al, 2008;Yeşiller et al, 2015;Manjunatha et al, 2020;Nocko et al, 2021), which is, in general, higher than that of dry inorganic soils (k=0.27-0.38 W/m K) (Mondal et al, 2016(Mondal et al, , 2017. Such a higher value can be due to the higher moisture content and electrical conductivity of the leachate (Grellier et al, 2006), which is proportional to k (Schwarz and Bertermann, 2020).…”
Section: Thermal Properties Of Msw: Guiding Factor Of Landfill Firesmentioning
confidence: 92%
“…Further, from Table 1, it can be observed that the k of the MSW varies between 0.01 and 1.50 W/(m K) (Bonany et al, 2013;Hanson et al, 2008;Yeşiller et al, 2015;Manjunatha et al, 2020;Nocko et al, 2021), which is, in general, higher than that of dry inorganic soils (k=0.27-0.38 W/m K) (Mondal et al, 2016(Mondal et al, , 2017. Such a higher value can be due to the higher moisture content and electrical conductivity of the leachate (Grellier et al, 2006), which is proportional to k (Schwarz and Bertermann, 2020).…”
Section: Thermal Properties Of Msw: Guiding Factor Of Landfill Firesmentioning
confidence: 92%
“…A temperature of 60 ⁰ C was applied at the top surface of this column, as depicted in Fig1a. Furthermore, as depicted in Fig1b, the flux sensors, and thermocouples were embedded at 5 cm and 9 cm depths, respectively, in the sample (Mondal et al 2017). The heat gun was kept at a height of 400mm which ensured uniform heat application at the top surface of the column.…”
Section: Statement Of the Problemmentioning
confidence: 99%
“…Some of the broadly used approaches are Finite Element Method (FEM) ( Timlin et al 2002;Han and Huang 2002;Bittelli et al 2008,), Finite Volume Method (LeVeque 2002), Finite Difference Method (FDM) (Sharratt et al 1992;Han and Huang 2002;Wu and Sun 2004;Wang et al 2011), Force Restore Method (FRM) ( Liebethal and Foken 2007;Gao et al 2008). Moreover, different analytical methods like Harmonic Method, Laplace Transform Method, and Fourier Transform Method, have been considered by several researchers (Heusinkveld et al 2004;Gao et al 2007;Evett et al 2012;Wang et al 2012) to solve HTE in order to predict the thermal regime in soil mass (Mondal et al 2017). Nonetheless, the major hindrance of some of the abovementioned methods is that they involve complicated mathematics which is not convenient to the practising engineers.…”
Section: Introductionmentioning
confidence: 99%
“…This calls for extensive studies to establish the mechanism of heat migration in geomaterials, by measuring their thermal response, i.e., thermal regime, particularly, under variable temperature conditions. One of the ways to achieve this would be to quantify 'the zone of influence of the heat source,' by measuring the thermal flux, /, and temperature, h, over prolonged durations in the spatial domain [110,111,113]. This could be done quite efficiently with the help of flux sensors and MEMS-based temperature sensors [203], of extremely high precision.…”
Section: Monitoring and Simulation Of Heat Migrationmentioning
confidence: 99%
“…Also, a unified mathematical framework, ATHERES, has also been developed to estimate thermal regime in the dry soil mass. The proposed approach couples Taylor's series into the governing differential equation of one-dimensional heat conduction [113].…”
Section: Monitoring and Simulation Of Heat Migrationmentioning
confidence: 99%