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A Filtration Model for Constant Flux Permeation of Bentonite Grout through Granular Soil

机译:膨润土灌浆通过粒状土壤的恒定通量过滤模型

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The flow of suspensions through porous media is a complex phenomenon owing to the diversity of the mechanisms involved. It is important to determine the filtration behavior to understand the decline in injectivity of suspension as flow progresses and for that, knowledge of the rate of particle deposition is crucial. In this paper, a numerical model has been developed for the permeation of bentonite suspension grout through granular soil. The filtration model defines the rate of deposition of solid particles which depends on the rheology and concentration of grout, particle size and shape of suspended particle, grain size distribution of porous media, and physio-chemical interaction of grout with the porous medium through which it is flowing. The novelty of the newly proposed numerical model is that it accounts for the change in rheology of grout and the porosity and permeability of the porous medium as a function of the deposition of particles, none of which has been considered in the past. In this paper, six filtration models were used with different filtration coefficients and solid deposition empirical relationships. It was found that using a filtration coefficient that increases linearly with cumulative solid deposition was best suited to model the filtration mechanism of bentonite suspension grout permeation in granular soil. Bentonite content profile along the height of the sand column determined numerically using the proposed filtration model was similar to that obtained from the experimental results from post-permeation analysis.
机译:由于所涉及的机制的多样性,悬浮液通过多孔介质的流动是一个复杂的现象。重要的是确定过滤行为,以了解随着流动的进行,悬浮液的注入量会下降,为此,了解颗粒沉积的速率至关重要。本文研究了膨润土悬浮灌浆在颗粒状土壤中渗透的数值模型。过滤模型定义了固体颗粒的沉积速率,该速率取决于水泥浆的流变学和浓度,悬浮颗粒的粒径和形状,多孔介质的粒径分布以及水泥浆与通过它的多孔介质之间的物理化学相互作用正在流动。新提出的数值模型的新颖之处在于,它解决了灌浆流变学以及多孔介质的孔隙率和渗透率随颗粒沉积的变化,过去没有考虑过。在本文中,使用了六个具有不同过滤系数和固体沉积经验关系的过滤模型。已发现,使用随累积固体沉积量线性增加的过滤系数,最适合于模拟膨润土悬浮灌浆在颗粒状土壤中渗透的过滤机理。使用提议的过滤模型通过数值确定的沿砂柱高度的膨润土含量曲线与渗透后分析的实验结果相似。

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