Abstract

Triaxial rheological tests are performed on mudstones collected from the soft interlayer in the Three Gorges Reservoir Area. In the tests, both dry and saturated conditions are considered, and a complete rheological process is then observed. Based on such laboratory observations of stress-strain, a four-element rheological constitutive model is developed, which is composed of (i) the Hook element, (ii) the Kelvin element, (iii) the viscoelastic-plastic body, and (iv) the nonlinear viscous body (HKCV model). The HKCV model adopts the one-dimensional and three-dimensional equations that are derived. The rheological parameters required are identified, allowing the successful development of the HKCV model. A comparison with the laboratory test observations and the existing model estimates shows that the estimates of the HKCV model are relatively consistent with the observations of the triaxial rheological test. The HKCV model better characterizes the rheological process than the three existing models. However, the HKCV model has the limitation of requiring more parameters than the existing models.

Highlights

  • Many rocks involve moisture [1]

  • A significant example of this effect is that of the rock mass in the ree Gorges Reservoir Area [9]

  • Mudstone specimens used for the rheological tests were collected from the soft interlayer in the Majiagou landslide in the ree Gorges Reservoir Area, China

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Summary

Introduction

Many rocks involve moisture [1]. Moisture has multiple effects on a rock, such as softening and lubrication [2, 3]. Approximately 69% of the reservoir area suffered rockslide hazard during the impoundment of the ree Gorges Reservoir [10, 11], which is closely related to the rheological effect under water-rock interaction of the mudstone formation. Despite numerous rheological constitutive models for multiple types of rock [15, 16, 17], a special model for mudstone, considering moisture content, is still required. The laboratory triaxial rheological tests are conducted on the mudstone specimens collected from the interlayer in the ree Gorges Reservoir Area. Both dry and saturated conditions are considered. The developed model estimates are compared with the laboratory test observations and the existing model estimates

Test Equipment and Method
45 MPa 35 MPa 40 MPa
The Developed HKCV Rheological
Comparison with the Observation of Test and the Estimates of Existing Models
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