Technical Papers
Jul 29, 2024

Slurry Support Mechanism for Shield Tunneling Considering Slurry Infiltration and Cutter-Disk Cutting Effect

Publication: International Journal of Geomechanics
Volume 24, Issue 10

Abstract

This study aims to clarify the mechanism of slurry support and its effect at different stages of slurry infiltration in shield construction. The analysis of various expressions of slurry support throughout the entire excavation cycle is based on the theories of slurry infiltration effects and the cutting action of the cutters. Furthermore, the limit support pressure calculation method at the tunnel face is modified considering the slurry support mechanism observed during different slurry infiltration stages. Some of the main conclusions drawn are as follows. (1) When slurry deep infiltration occurs, the main form of slurry support is the seepage force acting on the soil skeleton. At this stage, the limit support pressure from the filter cake model will not be sufficient to meet the tunnel face stability requirements. (2) The effectiveness of slurry support is influenced by both the slurry infiltration state and the cutting action of the cutterhead. Slurry infiltration and shield tunneling together create a quasi-static equilibrium state, in which slurry support is effective only when the infiltration velocity corresponding to this state is greater than the critical velocity. (3) And the influence of shield tunneling parameters on the slurry support mechanism is significant. Compared with the cutter’s penetration degree, the cutter’s rotational speed has a more pronounced effect on the conversion rate of slurry support pressure at the shield tunnel face.

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Data Availability Statement

Some or all data, models, or codes that support the findings of this study are available from the corresponding author upon reasonable request.

Acknowledgments

The authors would like to thank the anonymous reviewer for valuable and constructive comments and suggestions. The first author acknowledges the financial support from the Fundamental Research Funds for the Central Universities (N2201017) and the China Postdoctoral Science Foundation (Grant No. 2023M730524).

Notation

The following symbols are used in this paper:
A
cross-sectional area of the elementary volume;
a
empirical coefficient obtained from the test;
C
slurry concentration;
Cr
stagnation rate of slurry particles within the elementary volume, i.e., the volume of slurry particles stagnated in a unit slurry volume;
Cs
volume fraction of slurry particles in the slurry suspension inside the elementary volume of porous media;
Cw
slurry suspension volume fraction inside the elementary volume;
C0
initial slurry particles volume fraction;
dx
elementary thickness;
d10
effective particle size of soil mass;
Fi,j
triangular surface element;
fsg
slurry stagnation gradient;
g
gravity acceleration;
k
soil permeability coefficient;
kG
slurry pressure gradient coefficient;
kw
soil permeability coefficient to water;
L
length of the soil skeleton;
Lf
slip failure zone width;
l
slurry infiltration distance;
lmax
maximum penetration distance of the slurry;
Msr
stagnated slurry particles mass in soil pores;
Msu
stagnated slurry particles mass in suspension state in the soil;
Mw
mass of the slurry carrier fluid flowing in from the left boundary of the elementary volume;
Ms
slurry particle mass flowing in from the left side of the elementary volume;
Ms
slurry particle mass flowing out from the right side of the elementary volume;
Mw
mass of the slurry carrier fluid flowing in from the right boundary of the elementary volume;
Mwp
water mass change due to the pore-water pressure change within the elementary volume;
Mwr
water mass change in the elementary volume of porous media;
ΔMs
mass difference between the inflow and outflow of bentonite slurry particles;
ΔMw
mass difference between the inflow and outflow of the slurry carrier fluid on both sides of the elementary volume;
Nγ
dimensionless parameter reflecting the soil gravity;
Nc
dimensionless parameter reflecting the soil cohesion;
n
soil porosity in the infiltration zone;
n0
initial soil porosity before the slurry infiltration;
p
pore-water pressure within the elementary volume;
pA
constant slurry overpressure;
px
seepage force;
p0
original pore-water pressure in the layers;
Δp
slurry pressure difference between the slurry chamber and the layers;
Ri,j
pole diameter corresponding to the triangular surface element Fi,j at the center of gravity on the slip surface (Fig. 14);
S
cutter's penetration degree;
tcut
time interval of cutter cycle cutting;
tf
specific time;
tfil
time used for slurry film formation and development;
tpen
time used for deep penetration in each cutting time interval tcut;
v
slurry macroscopic penetration velocity inside the elementary volume;
vcr
critical tunneling speed;
vf
corresponding slurry penetration speed;
WD
internal dissipation work of the slip system;
WP
power generated by the slurry seepage force generated by the pore-water pressure gradient applied to the slip damage zone in front of the tunnel working face;
Wγ
gravity power of the slip system in the slip region below the water table when considering groundwater action;
WσvH
equivalent load power of the possible additional load on the ground surface;
α
compression coefficient of the soil skeleton;
β
compression coefficient of the water;
βi,j
angle between the motion velocity of the slip system and the horizontal direction;
γw
unit weight of water;
γ′
soil buoyant unit weight;
ɛi,j
angle between the velocity and the vertical direction;
λ
filtration coefficient of the stratum;
μ
dynamic viscosity coefficient of slurry;
μs
water storage coefficient of the porous medium;
μw
dynamic viscosity coefficient of water;
ρw
slurry carrier fluid (water) density;
σA
limit slurry support pressure;
σE
equivalent load that integrates the surface additional load and soil arch effect;
τs
slurry static yield strength; and
ω
rotational angular velocity of the slip system.

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Go to International Journal of Geomechanics
International Journal of Geomechanics
Volume 24Issue 10October 2024

History

Received: Jul 14, 2023
Accepted: Apr 15, 2024
Published online: Jul 29, 2024
Published in print: Oct 1, 2024
Discussion open until: Dec 29, 2024

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Assistant Professor, School of Resources and Civil Engineering, Northeastern Univ., Shenyang 110004, China (corresponding author). ORCID: https://orcid.org/0000-0001-7425-1134. Email: [email protected]
Runsheng Yang [email protected]
Master’s Student, School of Resources and Civil Engineering, Northeastern Univ., Shenyang 110004, China. Email: [email protected]
Shuhong Wang [email protected]
Professor, School of Resources and Civil Engineering, Northeastern Univ., Shenyang 110004, China. Email: [email protected]
Professor, School of Resources and Civil Engineering, Northeastern Univ., Shenyang 110004, China. Email: [email protected]
Assistant Professor, School of Mechanical Engineering, Shenyang Jianzhu Univ., Shenyang 110168, China. ORCID: https://orcid.org/0000-0001-9138-9928. Email: [email protected]

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