2015
DOI: 10.1016/j.fuel.2014.10.057
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Resources and economic analyses of underground coal gasification in India

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Cited by 40 publications
(13 citation statements)
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“…On the transition pore scale, the pore volumes of the HS coal samples vary slightly in the range of 50-100°C; in the range of 100-300°C, the pore volumes decrease significantly with the increase of the temperature, and the pore volumes of the XG coal samples decrease as a whole with an increase of the temperature, although the variation was small. On the mesopore scale, in the range of 50-200°C, the pore volumes of the HS and XG coal samples increase with the increase of the temperature 4 Geofluids but slowly in the range of 50-100°C and sharply in the range of 100-200°C; they also decrease sharply with the increase of the temperature in the range of 200-300°C; thus, the pore volumes of the XG coal samples change less than that of the HS coal samples. On the macropore scale, the pore volumes of the XG and HS coal samples remain almost unchanged in the range of 50-100°C, and within the range of 100-200°C, the pore volumes of the XG coal samples are almost unchanged; however, the pore volumes of the HS coal samples increase slightly with the increase of the temperature.…”
Section: The Variation Of the Pore Size Distribution With Thementioning
confidence: 96%
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“…On the transition pore scale, the pore volumes of the HS coal samples vary slightly in the range of 50-100°C; in the range of 100-300°C, the pore volumes decrease significantly with the increase of the temperature, and the pore volumes of the XG coal samples decrease as a whole with an increase of the temperature, although the variation was small. On the mesopore scale, in the range of 50-200°C, the pore volumes of the HS and XG coal samples increase with the increase of the temperature 4 Geofluids but slowly in the range of 50-100°C and sharply in the range of 100-200°C; they also decrease sharply with the increase of the temperature in the range of 200-300°C; thus, the pore volumes of the XG coal samples change less than that of the HS coal samples. On the macropore scale, the pore volumes of the XG and HS coal samples remain almost unchanged in the range of 50-100°C, and within the range of 100-200°C, the pore volumes of the XG coal samples are almost unchanged; however, the pore volumes of the HS coal samples increase slightly with the increase of the temperature.…”
Section: The Variation Of the Pore Size Distribution With Thementioning
confidence: 96%
“…In recent years, there have been many means to achieve coal conversion and comprehensive utilization, including underground coal gasification and geothermal mining [1,2]. Underground coal gasification is a kind of clean coal comprehensive utilization technology that is converted into combustible gas in situ by a thermochemical reaction [3,4]. This technology is one of the important ways to achieve coal conversion, which improves the energy structure, enhances the safety of coal mine production, and considerably improves the resource recovery rate [5,6].…”
Section: Introductionmentioning
confidence: 99%
“…2). Most of the coal reserves have high ash content (25-60%) 3 and are available at depths exceeding 300 m rendering them less suited for conventional mining techniques 4 . The advantage of pursuing the option of UCG is that the coal deposit present at great depth need not be removed and brought to surface.…”
Section: Globally the Sheen Of Coal-based Energy Production Is Slowlmentioning
confidence: 99%
“…It has been considered to be technologically feasible, economically attractive and environmentally friendly [3]. Up to now, numerous UCG laboratory experiments and field tests have been performed all around the world [4][5][6][7][8][9][10][11].…”
Section: Introductionmentioning
confidence: 99%