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Abstract: This work deals with 2D thermal modeling in order to delineate the crustal thermal structure of central India along two Deep Seismic Sounding (DSS) profiles, namely Khajuriakalan–Pulgaon and Ujjan–Mahan, traversing the Narmada-Son-Lineament (NSL) in an almost north–south direction. Knowledge of the crustal structure and P-wave velocity distribution up to the Moho, obtained from DSS studies, has been used for the development of the thermal model. Numerical results reveal that the Moho temperature in this region of central India varies between 500 and 580°C. The estimated heat flow density value is found to vary between 46 and 49mW/m2. The Curie depth varies between 40 and 42km and is in close agreement with the Curie depth (40±4km) estimated from the analysis of MAGSAT data. Based on the present work and previous work, it is suggested that the major part of peninsular India consisting of the Wardha–Pranhita Godavari graben/basin, Bastar craton and the adjoining region of the Narmada Son Lineament between profiles I and III towards the north and northwest of the Bastar craton are characterized with a similar mantle heat flow density value equal to ∼23mW/m2. Variation in surface heat flow density values in these regions are caused by variation in the radioactive heat production and fluid circulation in the upper crustal layer. [Copyright &y& Elsevier]

The heat generation and temperature rise due to the anaerobic degradation of municipal solid waste (MSW) for selected landfills across India have been estimated in this paper. MSW was quantitatively characterized into carbohydrates, proteins, fats using landfill degradation and transport (LDAT) model equations' and the physical composition of MSW. The heat released due to the breakdown of per kg of carbohydrates, proteins, fats were calculated using chemical equations involved in the anaerobic degradation process. The heat released per tonne of MSW degradation and temperature rise for selected cases was calculated. Moisture content and carbohydrates percentage were crucial parameters in estimating the heat generation as Mavallipura landfilled MSW having 43% carbohydrates and moisture content of 17% released maximum heat of 1116.81 × 10 3 kJ/t of MSW and Pirana landfill MSW having 12.98% carbohydrates and moisture content of 29.03% released minimum heat of 391.82 × 10 3 kJ/t of MSW. This generated heat may cause several issues, such as landfill fires, temperature rise in the surrounding areas of landfill, air pollution leading to global warming and other environmental issues. The heat generated from the biodegradation process is a renewable energy resource that can be systematically extracted from the waste mass and used for direct heating purpose in nearby facilities or for augmenting industrial processes having suitable technologies like combined heat and power gas engines, geothermal heat extraction system, etc. This study concludes that the total quantity of heat released depends on the quantity of carbohydrates present in waste and not on total organic content., (Copyright © 2019 Elsevier B.V. All rights reserved.)