DYNAMIC FRACTURE OF GAS-BEARING COAL SEAM DURING ZONAL DISINTEGRATION

2020 ◽  
Vol 56 (6) ◽  
pp. 932-946
Author(s):  
V. N. Odintsev ◽  
V. V. Makarov
2021 ◽  
Author(s):  
Vibhas J. Pandey ◽  
Sameer Ganpule ◽  
Steven Dewar

Abstract The Walloons coal measures located in Surat Basin (eastern Australia) is a well-known coal seam gas play that has been under production for several years. The well completion in this play is primarily driven by coal permeability which varies from 1 Darcy or more in regions with significant natural fractures to less than 1md in areas with underdeveloped cleat networks. For an economic development of the latter, fracturing treatment designs that effectively stimulate numerous and often thin coals seams, and enhance inter-seam connectivity, are a clear choice. Fracture stimulation of Surat basin coals however has its own challenges given their unique geologic and geomechanical features that include (a) low net to gross ratio of ~0.1 in nearly 300 m (984.3 ft) of gross interval, (b) on average 60 seams per well ranging from 0.4 m to 3 m in thickness, (c) non-gas bearing and reactive interburden, and (d) stress regimes that vary as a function of depth. To address these challenges, low rate, low viscosity, and high proppant concentration coiled tubing (CT) conveyed pinpoint stimulation methods were introduced basin-wide after successful technology pilots in 2015 (Pandey and Flottmann 2015). This novel stimulation technique led to noticeable improvements in the well performance, but also highlighted the areas that could be improved – especially stage spacing and standoff, perforation strategy, and number of stages, all aimed at maximizing coal coverage during well stimulation. This paper summarizes the findings from a 6-well multi-stage stimulation pilot aimed at studying fracture geometries to improve standoff efficiency and maximizing coal connectivity amongst various coal seams of Walloons coal package. In the design matrix that targeted shallow (300 to 600 m) gas-bearing coal seams, the stimulation treatments varied in volume, injection rate, proppant concentration, fluid type, perforation spacing, and standoff between adjacent stages. Treatment designs were simulated using a field-data calibrated, log-based stress model. After necessary adjustments in the field, the treatments were pumped down the CT at injection rates ranging from 12 to 16 bbl/min (0.032 to 0.042 m3/s). Post-stimulation modeling and history-matching using numerical simulators showed the dependence of fracture growth not only on pumping parameters, but also on depth. Shallower stages showed a strong propensity of limited growth which was corroborated by additional field measurements and previous work in the field (Kirk-Burnnand et al. 2015). These and other such observations led to revision of early guidelines on standoff and was considered a major step that now enabled a cost-effective inclusion of additional coal seams in the stimulation program. The learnings from the pilot study were implemented on development wells and can potentially also serve as a template for similar pinpoint completions worldwide.


2018 ◽  
Vol 56 ◽  
pp. 334-341 ◽  
Author(s):  
Gang Wang ◽  
Xuelin Liu ◽  
Hao Xu ◽  
Mengmeng Wu ◽  
Rui Wang ◽  
...  

2019 ◽  
Vol 59 (2) ◽  
pp. 846
Author(s):  
Reydick Balucan ◽  
Zhenhua Jing ◽  
Jim Underschultz ◽  
Karen Steel

Many prospective coal seams have limited permeability and are thus marginal for economic coal seam gas (CSG) extraction. To enhance seam permeability, various CSG stimulation techniques, including hydraulic fracturing, cavity well completions and horizontal wells, have been used commercially, but these techniques are not successful everywhere. Alternately, oxidant stimulation to enhance coal seam permeability may have potential benefit. In this paper, we report the oxidation of a cubic coal sample from the gas-bearing Bandanna Formation with 1% NaClO. Permeability variation were measured over time with core stimulation/flooding tests. Coal structural changes, captured via X-ray microcomputed tomography (µCT), were used to analyse and model the impact of oxidant stimulation on coal permeability. We found that NaClO stimulation was able to widen fracture aperture and generate additional cracks and/or void space. Analyses of the coal after reaction indicated improved pore connectivity. This resulted in a significantly higher permeability, as shown by both core flood tests and flow modelling/simulations using GeoDict’s FlowDict module. Although this paper confirms oxidant stimulation has the potential to improve coal seam permeability, the optimum volume and reaction time, pressure and temperature conditions and suitability for use in various coal types requires further research.


2019 ◽  
Vol 60 (3) ◽  
pp. 560-568
Author(s):  
E. P. Feldman ◽  
N. A. Kalugina ◽  
O. V. Chesnokova
Keyword(s):  

2014 ◽  
Vol 962-965 ◽  
pp. 213-216
Author(s):  
Guo Ping Jiang

In this paper, four general directions are described to make evaluations and their resource potential; those are coal structure and coal level, gas content of deep coalbed, the coalbed thickness and distribution and the buried depth of coalbed. Coalfields of the study area are mainly Permian and Carboniferous coal seam of Shanxi Formation coal and Benxi group 11 # coal, coal seam depth 1370-1812m. No. 3 coal-seam average layer thickness of 1.6 m, the monolayer most 2 m thick; No. 11 coal-seam in the average layer thickness of 3 m, single-layer thickness of 4.5 m. Predict the amount of coal resources of 17.3 one hundred million t. Predict coal-bed methane resources of 27.68 billion cubic reserve abundance of 104 million square / km2 in. The exploration results show that this region has good development prospects.


2019 ◽  
Vol 23 (4) ◽  
pp. 359-364
Author(s):  
Yunlan He ◽  
Xikai Wang ◽  
Hongjie Sun ◽  
Zhenguo Xing ◽  
Shan Chong ◽  
...  

To identify the lithology of coal seam roof and explore the influence of these roofs on the enrichment of coalbed methane, low-frequency rock petrophysics experiments, seismic analyses and gas-bearing trend analyses were performed. The results show that the sound wave propagation speed in rock at seismic frequencies was lower than that at ultrasound frequencies. Additionally, the P-wave velocities of gritstone, fine sandstone, argillaceous siltstone and mudstone were 1,651 m/s, 2,840 m/s, 3,191 m/s and 4,214 m/s, respectively. The surface properties of the coal seam roofs were extracted through 3D seismic wave impedance inversion. The theoretical P-wave impedance was calculated after the tested P-wave velocity was determined. By matching the theoretical P-wave impedance of the four types of rocks with that of the coal seam roofs, we identified the lithology of the roofs. By analyzing known borehole data, we found that the identified lithology was consistent with that revealed by the data. By comparing and analyzing the coal seam roof lithology and the gas-bearing trends in the study area, we discovered that the coal seam roof lithology was related to the enrichment of coalbed methane. In the study area, areas with high gas contents mainly coincided with roof zones composed of mudstone and argillaceous siltstone, and those with low gas contents were mainly associated with fine sandstone roof areas. Thus, highly compact areas of coal seam roof are favorable for the formation and preservation of coalbed methane. 


2019 ◽  
Vol 29 (2) ◽  
pp. 327-333 ◽  
Author(s):  
Wang Gang ◽  
Wang Rui ◽  
Wu Mengmeng ◽  
Fan Cheng ◽  
Song Xiang

2015 ◽  
Vol 13 ◽  
pp. 278-281 ◽  
Author(s):  
D.D.R. Owen ◽  
R. Millot ◽  
Ph. Négrel ◽  
K. Meredith ◽  
M.E. Cox

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