Abstract

This research experimentally studied the effects of various fracture roughness (characterized by the fractal dimension D) and normal stress (normal loads FN) applied to fracture on ultrafine cement grout nonlinear flow behavior through rough-walled plexiglass fractured sample. A high-precision and effective sealing self-made apparatus was developed to perform the stress-dependent grout flow tests on the plexiglass sample containing rough-walled fracture (fracture apertures of arbitrary variation were created by high-strength springs and normal loads according to design requirements). The real-time data acquisition equipment and high-precision self-made electronic balance were developed to collect the real-time grouting pressure P and volumetric flow rate Q, respectively. At each D, the grouting pressure P ranged from 0 to 0.9 MPa, and the normal loads FN varied from 1124.3 to 1467.8 N. The experimental results show that (i) the Forchheimer equation was fitted very well to the results of grout nonlinear flow through rough-walled fractures. Besides, both nonlinear coefficient (a) and linear coefficient (b) in Forchheimer’s equation increased with increase of D and FN, and the larger the FN was, the larger the amplitude was. (ii) For normalized transmissivity, with the increase of Re, the decline of the T/T0−β curves mainly went through three stages: viscous regime, weak inertia regime, and finally strong inertia regime. For a certain D, as the normal load FN increased, the T/T0−β curves generally shifted downward, which shows good agreement with the single-phase flow test results conducted by Zimmerman. Moreover, with the increase of D, the Forchheimer coefficient β decreased. However, within smaller FN, β decreased gradually with increasing D and eventually approached constant values. (iii) At a given FN, Jc increased with increasing D.

Highlights

  • Fractured rock masses (Figure 1(a)) are widely distributed in underground engineering due to geological action or excavation disturbance, which may bring serious safety hazard to the engineering stability [1,2,3,4]

  • The nonlinear flow behavior (J-Q), nonlinear flow regime, nonlinear and linear coefficients, normalized transmissivity (T/T0 − β), Forchheimer coefficient (β), and critical hydraulic gradient (Jc) for grout flow through fractures were obtained

  • The main experimental results were as follows: (1) The correlation between grout hydraulic gradient J and volume flow rate Q was demonstrated to be nonlinear based on the flow tests, which was fitted by the Forchheimer equation

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Summary

Introduction

Fractured rock masses (Figure 1(a)) are widely distributed in underground engineering due to geological action or excavation disturbance, which may bring serious safety hazard to the engineering stability [1,2,3,4]. Li et al [30] experimentally investigated the hydromechanical behavior of rock joints by using a parallel-plate model containing contact areas and artificial fractures They presented some empirical relations to evaluate the influences of contact area and surface roughness on the fluid flow behavior through rock fractures. From these studies, we found that the formula accepted by most researchers for nonlinear flow through rough-walled fractures is Forchheimer’s equation [31]:. In order to study the grout flow behavior through the rough-walled fractures, a high-precision and effective sealing self-made apparatus was developed to perform stress-dependent grout flow tests on the plate specimens with fractures made of high-transparency plexiglass and high-strength springs. Based on the test results, the cement grout nonlinear flow behavior through rough-walled rock fractures with different D and normal loads was analyzed

Grout Flow Testing System
Material Preparation
Results and Analysis
Conclusions
Weak inertia effect
Full Text
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