Technical Papers
Sep 21, 2020

Closed-Form Solution to the Poromechanics of Deep Arbitrary-Shaped Openings Subjected to Rock Mass Alteration

Publication: International Journal of Geomechanics
Volume 20, Issue 12

Abstract

The aim of this paper is to propose a closed-form solution to the poromechanics problem of stress and pore pressure distribution around noncircular openings at great depth subjected to hydrostatic water pressure and far-field geostresses. The problem is solved by superposing the effects of fluid and solid skeleton obtained over simple circular geometries and generalizing the obtained expression to various geometries of mined ore bodies using complex variable functions and conformal mapping techniques. The principal stresses obtained analytically over the opening boundary and within the domain are compared with the results of finite-element analysis to verify the proposed approach. The comparison conducted for a representative noncircular opening indicates good agreement between the analytical and numerical methods. Hence, a parametric study is used to investigate in detail the stress variation under different opening dimensions, heterogeneous initial total stress conditions, and far-field pore pressure values. The proposed solution could be instrumental in the design of underground openings and deep mass alterations (that include local anthropogenic damage zones). It could also be used to provide reinforcement solutions where stresses can reach the mechanical stability thresholds.

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Acknowledgments

The first author would like to acknowledge financial support provided by the China Scholarship Council (CSC) under grant number 201606420056. The authors would like to thank the anonymous reviewers for their considerable effort in improving the paper.

Appendix. Detailed Derivation of the Coefficients an and bn

Substituting Eqs. (9), (12), and (13) into (7), the equation is derived as
ψ1(α)+ω(α)ω(α)¯ψ1(α)¯+χ1(α)¯=2Bω(α)Bω(α)¯
(28)
where: α = an arbitrary point on the unit circle boundary in the ξ plane. It can be expressed as α = e, thus α¯=eiθ=1/α.
Using Cauchy’s integral operator and integrating Eq. (28), the following equation is obtained:
12πiCψ1(α)αξdα+12πiCω(α)ω(α)¯ψ1(α)¯αξdα+12πiCχ1(α)¯αξdα=12πiCf0(α)αξdα
(29)
where the function f0(α) can be expressed as
f0(α)=2Bω(α)Bω(α)¯
(30)
The ψ1(α) in Eq. (29) is the boundary value of ψ1(ξ), which is an analytic function exterior to the unit circle. Therefore, the first integral term on the left hand side of Eq. (29) by using Cauchy’s integral is obtained as:
12πiCψ1(α)αξdα=ψ1(ξ)
(31)
The complex constant is omitted here and in what follows, since it does not contribute to the stresses. The right hand side (RHS) of Eq. (29) can be expressed as:
12πiCf0(α)αξdα=12πiC2Bω(α)αξdα+12πiCBω(α)¯αξdα
(32)
Expanding the first term on the right-hand side of Eq. (32) yields
12πiC2Bω(α)αξdα=2B12πiCc0α+c1α1++cnαnαξdα
(33)
Note that the first integrand (c−1α + c0) is a boundary value of an analytic function (c−1ξ + c0) interior to the unit circle, whereas the other terms are analytical functions exterior to the unit circle. The denominator (αξ) is also an analytical function interior to the unit circle, given that |ξ| > 1. Therefore, the integral of the first term is zero and the rest can be obtained using the Cauchy-Goursat theory:
12πiC2Bω(α)αξdα=2B12πiCc1α1++cnαnαξdα=2B(c1ξ+c2ξ2++cnξn)
(34)
Similarly, the second term on the right-hand side of Eq. (32) gives
12πiCBω(α)¯αξdα=B12πiCc1α1+c0+c1α++cnαnαξdα=B12πiCc1α1+c0αξdαB12πiCc1α++cnαnαξdα=B12πiCc1α1+c0αξdα=Bc1ξ
(35)
Combining Eqs. (34) and (35), the right-hand side of Eq. (29) can be expressed as
12πiCf0(α)αξdα=2B(c1ξ+c2ξ2++cnξn)+Bc1ξ
(36)
The analytic function of ψ1(ξ) is determined by
ψ1(ξ)+12πiCω(α)ω(α)¯ψ1(α)¯αξdα=2B(c1ξ+c2ξ2++cnξn)+Bc1ξ
(37)
By conjugating Eq. (28) and following a similar procedure, the analytic function of χ1(ξ) can be rewritten as
χ1(ξ)+12πiCω(α)¯ω(α)ψ1(α)αξdα=2Bc1ξ+B(c1ξ+c2ξ2++cnξn)
(38)
The second term in Eq. (37) can be expressed as
ω(α)ω(α)¯=c1α+c0+c1α1+c2α2++cnαnc1c1α22c2α3ncnαn+1=1αnc1αn+1+c0αn+c1αn1+c2αn2++cnc1c1α22c2α3ncnαn+1
(39)
and
ψ1(α)¯=a1¯α22a2¯α33a3¯α4nan¯αn+1=α2(a1¯2a2¯α3a3¯α2nan¯αn1)
(40)
As shown previously, the ratio ω(α)/ω(α)¯ has (n) order pole at the origin. Therefore, it can be written in the following form:
ω(α)ω(α)¯=dnαn+dn1αn1++d1α+j=0djαj
(41)
The product of ω(α)/ω(α)¯ and ψ1(α)¯ has (n − 2) order pole at the origin and it takes the form
ω(α)ω(α)¯ψ1(α)¯=kn2αn2+kn3αn3++k1α+j=0kjαj
(42)
Hence, the Cauchy integral is solved
12πiCω(α)ω(α)¯ψ1(α)¯αξdα=kn2ξn2kn3ξn3k1ξ
(43)
The coefficients dn and dj′ are known for a given conformal mapping function whereas kn and an¯ are unknown. Combining Eqs. (39), (41), and (42), the coefficient kn is expressed as
{k0=d2a1¯2d3a2¯(n1)dnan1¯k1=d3a1¯2d4a2¯(n2)dnan2¯kn2=dna1¯
(44)
Another set of equations is then required to obtain these coefficients. Substituting Eq. (43) into (37) yields
a1ξa2ξ2anξnkn2ξn2kn3ξn3k1ξ=2B(c1ξ+c2ξ2++cnξn)+Bc1ξ
(45)
therefore, kn can also be expressed as
{k1=a12Bc1Bc1k2=a22Bc2kn2=an22Bcn2an=2Bcn
(46)
where cn, B, and B′ are known. Combining Eqs. (44) and (46) the coefficient an is obtained. Therefore, the analytic function ψ1(ξ) is derived and the series number (n) is related to the conformal mapping terms.
Using the same procedure, the second term in Eq. (38) is written as
ω(α)¯ω(α)ψ1(α)=kn2¯αn2+kn3¯αn3++k1¯α+k0¯+j=1kj¯αj
(47)
To derive Eq. (47), the following equality is introduced:
g(α)=g(α)+g0(α)
(48)
where
g(α)=ω(α)¯ω(α)ψ1(α)g(α)=kn2¯αn2+kn3¯αn3++k1¯α+k0¯g0(α)=j=1kj¯αj
(49)
Therefore, the Cauchy integer of Eq. (48) reads
12πiCω(α)¯ω(α)ψ1(α)αξdα=12πiCg(α)αξdα=12πiCg(α)αξdα+12πiCg0(α)αξdα=g0(ξ)=g(ξ)g(ξ)
(50)
Substituting Eq. (50) into (38), the coefficient bn of analytic function χ1(ξ) in Eq. (15) is obtained.

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International Journal of Geomechanics
Volume 20Issue 12December 2020

History

Received: Nov 22, 2019
Accepted: Jul 31, 2020
Published online: Sep 21, 2020
Published in print: Dec 1, 2020
Discussion open until: Feb 21, 2021

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Ph.D. Candidate, Dept. of Civil, Environmental and Mining Engineering, Univ. of Western Australia, 35 Stirling Hwy, Crawley, WA 6009, Australia. ORCID: https://orcid.org/0000-0002-0900-189X.
Ali Karrech [email protected]
Associate Professor, Dept. of Civil, Environmental and Mining Engineering, Univ. of Western Australia, 35 Stirling Hwy, Crawley, WA 6009, Australia (corresponding author). Email: [email protected]
Associate Professor, Dept. of Civil, Environmental and Mining Engineering, Univ. of Western Australia, Perth WA 6009, Australia; Dept. of Petroleum and Geosciences, Norwegian Univ. of Science and Technology, Trondheim, Norway. ORCID: https://orcid.org/0000-0003-4556-4953.
Mohamed Elchalakani
Senior Lecturer, Dept. of Civil, Environmental and Mining Engineering, Univ. of Western Australia, 35 Stirling Hwy, Crawley, WA 6009, Australia.
Chongchong Qi
Ph.D. Candidate, Dept. of Civil, Environmental and Mining Engineering, Univ. of Western Australia, 35 Stirling Hwy, Crawley, WA 6009, Australia.

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