2014
DOI: 10.1260/0144-5987.32.2.263
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Effects of Variogram Characteristics of Coal Permeability on CBM Production: A Case Study in Southeast Qinshui Basin, China

Abstract: The coalbed methane (CBM) resources of China are located mainly in 9 basins, Ordos, Qinshui, Jungar, Diandongqianxi, Erlian, Tuha, Tarim, Tianshan and Hailaer. Qinshui Basin, one of the richest CBM basins in China, has boosted its annual CBM production to 3×10 9 m 3 (106 Bcf). The coal seams in Qinshui Basin are significant with high gas content but strong heterogeneous permeabilities ranging from 0.1 to 10 mD. This paper investigates the effects of spatial distribution characteristics of coal permeability on … Show more

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Cited by 9 publications
(6 citation statements)
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“…The Shanxi formation consists of fluvial deposits of mudstone, siltstone, and sandstone, and the Taiyuan formation consists of mudstone, sandstone, and limestone. The average thickness of the two formations is ∼150 m, and the total net coal thickness varies from 6 m to 15 m. , Figure shows the stratigraphy and well logs of the two formations including coal seam No. 3 and coal seam No.…”
Section: Overview Of Qinshui and Ordos Basinsmentioning
confidence: 99%
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“…The Shanxi formation consists of fluvial deposits of mudstone, siltstone, and sandstone, and the Taiyuan formation consists of mudstone, sandstone, and limestone. The average thickness of the two formations is ∼150 m, and the total net coal thickness varies from 6 m to 15 m. , Figure shows the stratigraphy and well logs of the two formations including coal seam No. 3 and coal seam No.…”
Section: Overview Of Qinshui and Ordos Basinsmentioning
confidence: 99%
“…3 and coal seam No. 15 14 The Qinshui basin was formed during uplifting of the late Paleozoic platform, associated with orogeny in the Triassic Indosinian and Jurassic to Cretaceous Yanshanian. Surrounded by many mountain uplifts, the basin is a complex syncline striking from NNE to SSW.…”
Section: Overview Of Qinshui and Ordos Basinsmentioning
confidence: 99%
“…Through a comprehensive analysis of sandstone thickness, the thickness ratio of brittle-plastic rocks and permeability coefficients, a grade evaluation and zoning of the water richness of the area number 3-1 coal roof aquifer was completed (Zhou et al, 2014;Jun et al, 2015).…”
Section: A Zoning Study Of the Water Richness Of Area Number 3-1 Coal Roof Aquifermentioning
confidence: 99%
“…It is the most successful commercial CBM area in China, with one of the highest degrees of exploration and development within high-rank Chinese coal. The Taiyuan and Shanxi formations are the main coal-bearing strata in the Southern Qinshui basin, and they belong to the Permo-Carboniferous system (Zhou et al., 2014). The lithofacies of the Shanxi formation are composed largely of sandstones, mudstones, siltstones, and coal (Figure 1).…”
Section: Geological Settingsmentioning
confidence: 99%