Journal of Power and Energy Engineering, 2014, 2, 1-6
Published Online April 2014 in SciRes. http://www.scirp.org/journal/jpee
How to cite this paper: Wang, Z.R., Jin, J.S., Hang, Z.Y. and Hu, X.Z. (2014) Influence of Water Injection Fracturing on Crack
Damage in Soft Coal and Application in Gas Extraction. Journal of Power and Energy Engineering, 2, 1-6.
Influence of Water Injection Fracturing on
Crack Damage in Soft Coal and Application
in Gas Extraction
Zhirong Wang1, Jianshi Jin1, Zhongyang Hang1, Xiangzhi Hu2
1School of Environment and Water Conservancy Engineering, Zhengzhou University, Zhengzhou, China
2Gas Well Engineering Research Center of Henan, Zhengzhou, China
Email: email@example.com, firstname.lastname@example.org, email@example.com,
Received Novemb er 20 13
In order to study the hypotonic and rheological particularity of “three soft” coal seam in west He-
nan, China, this paper explored the stress and damage characteristics of crack in coal under condi-
tion of water injection fracturing based on ABAQUS platform; The cohesive element in T-P damage
evolution criterion was used to describe the approximately linear relationship between crack
width and extending distance in soft coal. The simulation results show that stress evolution and
crack damage in soft coal is a gradually developing process under condition of water injection
fracturing. When the static pressure is 4 - 10 MPa, and the injection time is about 1 - 2 hours, the
damage range of crack in soft coal can basically reach an ideal data of 80 - 100 m, and then greatly
improve the hypotonic performance of “three soft” coal seam.
“Three Soft” Coal Seam; Directional Water Injection Fracturing; Crack Damage; Gas Extraction
Coalbed methane (CBM) resources are very rich in Henan province, China. However, the technical problems
about low permeability, pressure, saturation and high metamorphic grade in Western Henan coal field especially
in “three soft” mining area have not been solved. By now the production of CBM and efficiency of wells are
very poor, the extraction rate remains around 25% and still can’t achieve efficient utilization of CBM . Water
fracturing technology is widely used in engineering fields especially in oil and gas extracting industry [2,3,4],
but theoretical research about coal seam with low permeability is rarely seen.
In recent years, with the development of rock mechanics test and computer simulation technology, many gas
permeability research achievements begin to appear in academia. W. J. Sommerton et al. studied the influence
of stress on the permeability of coal ; Chinese scholars Jupeng Tang, Yishan Pan  found the relation be-
tween effective stress and the seepage properties of CBM desorption through analytic seepage experiment re-
search of CBM under pressure.
Z. R. Wang et al.
So far, great progress has been made in the theory of gas seepage characteristics under stress and gas migra-
tion rule under low permeability condition also has been expounded, But systematic analysis of a series of basic
theories such as key geological problems about extraction technology of gas in soft coal and fracture law of soft
coal under water fracturing condition have not been formed, and research about stress and strain of soft coal un-
der water fracturing condition and dynamic cracking process of coal body after fracturing are still in blank. This
paper taking Gaocheng Coal Mine in Henan as an example, established numerical simulation method through
the secondary development of ABAQUS and combined with rock damage and Biot consolidation theory, then
discussed the theory and application of the stress and strain of soft coal after fracturing, damage extension of
crack and gas permeability.
2. Mathematical Model
Water fracturing is to inject high presser water into coal seam according to its occurrence, and make the
gas-containing layer produce fissure or larger pore along a certain direction after a period of static force effect,
and enhance its permeability -. When pressure water flow acts on the original crack or the near parts, it
will strongly affect the stress and seepage field nearby. Damage and fracture phenomenon begin to appear in the
cracks without gas and the coal near them, the permeability changes accordingly which makes the gas permeate
to the fracture channel. Gas permeation intensifies the damage of rock and this process is a typical migrate
process of CBM boost by the change of permeability of damaged rock caused by stress field. Now the study on
the permeability of broken rock is more mature and has achieved some results -. This paper will apply the
numerical simulation method under coupling condition of stress-damage-seepage to verify these results and ap-
ply to practice.
2.1. Creep Test Model
This paper analyzed the deformation of soft coal according to the creep defined by extended D-P model pro-
vided by ABAQUS. The creep rule in ABAQUS means creep is defined by equivalent uniaxial creep. Methods
provided by the software include time hardening power function method, user subroutine method, strain har-
dening power function method and Singh-Mitchell method, method mentioned in this paper is time hardening
power function. When the stress on materials remains the same, creep rate and strain are given as follows:
is creep rate,
is equivalent creep stress. Equation (1) can be seen as three-parameter consti-
tutive relation formula which describes the creep properties of coal, where parameter A reflects the magnitude
order of creep rate and the structure and combination of coal, parameter m controls the decrease rate of creep
over time, and parameter n reflects the effect of deviator strain on creep.
2.2. Damage-Permeability Coupling Model
The existing equations between permeability and stress or strain have some limitations, and it is very difficult to
analyze the variation trend of the permeability after rock broken. Therefore, damage mechanics can be intro-
duced to relate them together. Numerical model and the relationship between damage factor and porosity are
given as follows:
where n0 is initial porosity of rock mass, ns is porosity of rock which reaches ultimate strength. When material is
completely destroyed, namely n = ns, the damage variable D = 1; when there is no damage, namely n = n0, the
Z. R. Wang et al.
damage variable D = 0. The relationship between permeability and damage is given by:
The stress and strain are changing all the time during the process of hydraulic fracturing, therefore, the dy-
namic evolution between porosity and permeability must be taken into consideration, and evolution process can
be expressed by:
( )( )
where n0 is initial porosity, k0 is initial permeability coefficient, and both of them can be getting from geotech-
nical test and field test,
is the total volume strain of materials.
3. Numerical Simulation and Analysis
Take Gaocheng coal mine in Dengfeng, Henan, China, as an example, the 3D finite element numerical calcula-
tion model was established with ABAQUS and according to the main gas geology characteristics in mining area.
The geological parameters of this coal mine are as follows: the average thickness of main coal seam is 3.10 m,
its inclination is 20˚, and the thickness of coal seam in typical “three soft” area is about 4.5 m, the central part of
coal seam contains one layer of dirt band whose thickness is 0.33 m, and the burial depth of coal mine is 500 m
now. The measured gas pressure is 2.6 MPa, gas content is about 20.6 m3/t. Initial diffusion velocity of gas △P
= 17.42 L/min, permeability coefficient of coal seam
= 0.0053 m2/(MPa2·d).
The extraction test hole is chosen as center of directional fracturing simulation area, namely a cylinder with
height of 20 m and radius of 200 m. Type of high-pressure grouting pump is 2TGZ-120/105, and its maximum
grouting pressure is 10.5 MPa. The length of water injection pipe is 2 m, and its location is between floor and
dirt band, and the injection direction is along the occurrence of coal seam to the front of coal wall. Drucker-
Prager model was chosen as model of coal seam, initial porosity is 3.69%, initial permeability coefficient is 2.33
× 10−6 cm·s−1, viscosity coefficient of water is 1 × 10–6 kPaS, injection pressure is 5MPa and injection rate is 2.3
m3/min, time of simulation is 2 hours. The radial water flow through spiral tube finally formed a loose cylinder
with center of injection pipe, its radius is R, the model is shown in Figure 1.
3.1. Stress Evolution of Crack Damage
When the material of crack tip is elastic-plastic medium, the cloud picture of water pressure development
process (y = 10 m section) in each period is shown in Figure 2. The seepage in coal seam develops to the right
side along initial fissure and reaches 34 m in 30 min as shown in Figure 2(a), and a wide range of green high
stress zone appears at crack tip. This is mainly due to the effect of secondary stress caused by water injection,
and directly results in the change and adjustment of underground pore fissure, and then lead to additional see-
page of groundwater along the fissure. As injection continues and head loss increases, the fracture radius increas-
es gradually and reaches 58 m after 60 min and high stress zone decreases significantly (Figure 2(b)); The crack
expands to 80 m after 90 min, and the high stress zone at crack tip basically disappears and fracturing effect
Figure 1. Bedding injection fracturing model of soft coal.
Z. R. Wang et al.
Figure 2. The stress development nephogram of injection fracturing process in coal seam. (a) 30 min; (b) 60 min; (c) 90 min ;
(d) 120 min.
becomes worse and worse (Figure 2(c)); The whole high stress zone disappears after 120 min and the extension
of crack also stops at 107 m (Figure 2(d)).
3.2. Deformation Characteristics of Crack Damage
The relationship among fracture radius, injection pressure, time and their optimal combination are related to the
efficiency of gas extraction. Damage factor of cohesive element changes with the pressure, and damage dis-
placement around fracturing hole along fracturing direction is shown in Figure 3.
Figure 4 shows the extraction rates before and after fracturing, it indicates that the extraction rate differs sig-
nificantly before and after fracturing, and also differs when using different methods. Extraction rate of bedding
fracturing is the highest and up to 0.95 m3/s, rate of vertical fracturing comes the second, and rate of the coal
seam without fracturing is the lowest. The highest rates at the same time are basically 100 times of the lowest,
and the maximum multiple can be 131 while the minimum multiple is 68. Therefore, water fracturing can im-
prove the extraction rate and permeability of coal seam significantly, and the effect of bedding fracturing is most
3.3. Load Condition of Crack Damage
Under hydrostatic pressure value is 4MPa, the maximum principal stress damage coefficient on the left side of
coal seam reaches 0.948 and it is close to completely destroyed. As the pressure increases to 4.5 MPa, the dam-
age coefficient reaches critical value (D = 1), this pressure is slightly larger than the theoretical value as part of
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Figure 3. Da mage displacement around fracturing hole.
Figure 4. Comparison of extraction rate.
the pressure flow lost in fracturing process, and it is very close to the initial pressure of cohesive elements in this
paper. Therefore, the initial pressure of 4.5 MPa is reasonable (Figure 5).
When apply modified Taft seismic data on the model, and set pulse frequency at 10 Hz, the dynamic loads
values of cohesive elements with damage factor D =1 are slightly lower than the corresponding static values.
This indicates that cohesive elements are easier to fatigue, and faster to damage. From another point of view, the
difference between dynamic and static damage factors is very small, and the maximum difference is 0.1 (Figure
5), which shows that soft coal has good seismic and isolation effectiveness, namely the crack is difficult to close
4. Test Data and Extraction Effect
Ground directional water injection fracturing was conducted in 6 drill holes in the test field of Weicun coal mine
in Jiaozuo, Henan, China, on September 26, 2007. G10-002 hole is located in a certain mining working face, it’s
85 m away from F5 fault on the east and 110m away from F9 fault on the west. In order to avoid the influence of
two boundary faults, the design value of injection pressure is 5 MPa, injection time of east fault is 1.5 hours and
2 hours for the west one.
Test data from SN338HR digital seismograph indicate that length of crack at the east side of drilling hole is
82.4m and the length of the west one is 109.5 m, which fully verify the simulation results. As is shown in Table
1, because the location is closer to crack, extraction concentration of holes No.1, 19, 20 are 2 - 3 times that of
holes No.72, 166, and the average volumes are also much bigger.
Directional water injection fracturing can significantly improve gas extraction rate. Simulation calculation and
field test can indicate the follows:
Z. R. Wang et al.
Figure 5. Damage factors under different loads.
1) Water injection can lead to stress concentration at the crack tip and expand the damage zone of crack.
When injection pressure is 4 - 10 MPa and time is around 2 hours, the influence radius can basically reach an
ideal data of 80 - 100 m, and the initial extraction load could be 4.5 Mpa.
2) Water injection can promote the damage of crack, but the opening degree of crack is significantly affected
by confining pressure, the relationship between width of crack and extended distance is approximately linear.
3) Gas extraction efficiency after water injection can be improved 100 times, and extraction rate of single well
can reach 40% - 50%, and the fading period extends from 7 days to 1000 - 1500 days, which can basically meet
the monthly output target of 1000 - 2000 m3. This conclusion can provide valuable reference for similar projects
and has important strategic significance to the development and utilization of CBM.
 Wang, Z.R., Chen, L.X., Cheng, C.R. and Li, Z.X. (2007) Forecast of Gas Geological Hazards for “Three-Soft” Coal
Seams in Gliding Structural Areas. Journal of China University of Mining and Technology, 17, 484-488.
 Meyer, B.R. and Bazan, L.W. (2011) A Discrete Fracture Network Model for Hydraulically Induced Fractures Theory.
SPE Hydraulic Fracturing Technology Conference, The Woodlands, 24-26 January 2011, 216-225.
 Olson, J.E. and Dahi-Taleghani, A. (2009) Modeling Simultaneous Growth of Multiple Hydraulic Fractures and Their
Interaction with Natural Fractures. SPE Hydraulic Fracturing Technology Conference, The Woodlands, 19-21 January
 Wang, J.J., Zhang, H.P., Zhao, M.J. and Lin, X. (2009) Mechanisms of Hydraulic Fracturing in Cohesive Soil. Water
Science and Engineering, 2, 95-102.
 Sommerton, W.J., Soylemezoglu, I.M. and Dudley, R.C. (1975) Effect of Stress on Permeability of Coal. International
Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, 12, 129-145.
 Tang, J.P., Pan, Y.S., Li, C.Q. and Shi, Q. (2006) Experimental Study of Desorption and Seepage of Coalbed Methane
under Solid-Fluid Coupling. Journal of China University of Mining & Technology, 35, 274-278.
 Louis, C. (1969) A Study of Ground Water Flow in Jointed Rock and its Influence on the Stability of Rock Masses.
10th Edition, Imperial College of Science and Technology, London.
 Biot, M.A. (1941) General Theory of Three-Dimensional Consolidation. Journal of Applied Physics, 12, 155-164.
 Yin, G.Z., Li, X.Q., Zhao, H.B. and Li, X.S. (2008) Experimental Research on Effect of Geostress on Outburst Coal’s
Seepage. Chinese Journal of Rock Mechanics and Engineering, 27, 2557-2561.
 Hu, G.Z., Wang, H.T., Fan, X.G. and Yuan, Z.G. (2008) Investigation on Law of Methane Gas Flow in Coal with
Coal-Gas Outburst Hazard and Low Permeability. Chinese Journal of Rock Mechanics and Engineering, 28, 2527-