Article

Experiment of fracture grouting in alluvium with physical model

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Abstract

Dams are mainly located at the deep alluvium, where large amount of sand and gravel is adverse to prevention of seepage and maintenance of stability of the dams. Therefore it is necessary to reinforce the dams by grouting, and the primary task is to do research on the laws of diffusion and distribution of the slurry in the alluvial layer. The present study is based on the traditional theory of grouting and the laws of diffusion and distribution of the slurry, the slurry splitting mechanism, the characteristics of soil reinforcement are obtained. In addition, it is found by on-site grouting model tests that the slurry is generally filling and splitting along the interface between the earth and rock, and mainly splitting in the horizontal direction in grouting reinforcement process. To improve the reinforcement effect, the repeated injection should be adopted in grouting process. The study results will facilitate future dam grouting reinforcement projects in alluvial layer.

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... Specifically, Hu et al. and Han et al. performed simulated grouting test in fractured rock mass and then obtained the uniaxial compressive strength of the rock mass after grouting [15][16], respectively. Cheng et al. carried out grouting field tests in the sedimentary layer to reveal the grouting reinforcement mechanism, as well as to obtain the strength of soil after grouting [17]. Besides, Yang et al. developed grouting tests in gravel to study the relationship between the compressive strength of consolidation body and the injection parameters, as well as the grout properties [18]. ...
... The experimental system can realize porous grouting and multi-step grouting in different media, which have a realtime monitoring of the internal physical parameters of the rock mass. These features are important to the study of the permeability and reinforcement mechanism of the grouting slurry [19][20][21]. AC. Houlsby simulated the flowing of slurry through a single crack. ...
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