Effects of fluid composition in fluid injection experiments in porous media

IF 3.5 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Charalampos Konstantinou , Hassan Farooq , Giovanna Biscontin , Panos Papanastasiou
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Abstract

Experiments on fluid flow in porous media, using fluids loaded with solids of various grain sizes, have been conducted in a modified Hele-Shaw setup. This setup utilised weakly cemented porous media with specific hydraulic and mechanical properties. Fluid injection in coarse granular media with clean or low-concentration fine particles, results in infiltration only, with pressure close to the material tensile strength, while injection in finer granular material causes damage alongside infiltration, with the fluid pressure still close to the material tensile strength. When larger particle sizes or higher particle concentrations are used in the mixture, the fluid travels further within the porous medium, primarily influenced by the grain size of the granular medium. In the latter case, the Darcy flow equation with an effective permeability term can be employed to determine the pressure differential. For the largest particle sizes included in the fluid, the equation is still applicable, but the effective permeability requires adjustment for particle size within the fluid rather than the granular medium. This is crucial when the injection point is locally clogged. The experiments show that fracturing conditions are controlled by different mechanisms. Dimensional and statistical analysis was used to classify the injection pressures to regimes predicted by fracturing theory or by Darcy law with modified effective permeabilities. The findings show that both the material properties and fluid composition are important designing parameters.

多孔介质中流体注入实验中流体成分的影响
在改进的 Hele-Shaw 装置中进行了多孔介质中的流体流动实验,使用的流体中装有不同粒度的固体。该装置利用了具有特定水力和机械特性的弱胶结多孔介质。在含有清洁或低浓度细颗粒的粗颗粒介质中注入流体时,仅会导致渗透,压力接近材料的抗拉强度;而在较细颗粒材料中注入流体时,则会在渗透的同时造成破坏,流体压力仍接近材料的抗拉强度。当混合物中使用的颗粒尺寸较大或颗粒浓度较高时,流体会在多孔介质中移动得更远,这主要受到颗粒介质粒度的影响。在后一种情况下,可以使用带有有效渗透项的达西流动方程来确定压差。对于流体中的最大粒径,该方程仍然适用,但有效渗透率需要根据流体而非颗粒介质中的粒径进行调整。当注入点局部堵塞时,这一点至关重要。实验表明,压裂条件受不同机制的控制。利用尺寸和统计分析将注入压力划分为压裂理论或达西定律与修正有效渗透率所预测的两种情况。研究结果表明,材料特性和流体成分都是重要的设计参数。
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来源期刊
Journal of contaminant hydrology
Journal of contaminant hydrology 环境科学-地球科学综合
CiteScore
6.80
自引率
2.80%
发文量
129
审稿时长
68 days
期刊介绍: The Journal of Contaminant Hydrology is an international journal publishing scientific articles pertaining to the contamination of subsurface water resources. Emphasis is placed on investigations of the physical, chemical, and biological processes influencing the behavior and fate of organic and inorganic contaminants in the unsaturated (vadose) and saturated (groundwater) zones, as well as at groundwater-surface water interfaces. The ecological impacts of contaminants transported both from and to aquifers are of interest. Articles on contamination of surface water only, without a link to groundwater, are out of the scope. Broad latitude is allowed in identifying contaminants of interest, and include legacy and emerging pollutants, nutrients, nanoparticles, pathogenic microorganisms (e.g., bacteria, viruses, protozoa), microplastics, and various constituents associated with energy production (e.g., methane, carbon dioxide, hydrogen sulfide). The journal''s scope embraces a wide range of topics including: experimental investigations of contaminant sorption, diffusion, transformation, volatilization and transport in the surface and subsurface; characterization of soil and aquifer properties only as they influence contaminant behavior; development and testing of mathematical models of contaminant behaviour; innovative techniques for restoration of contaminated sites; development of new tools or techniques for monitoring the extent of soil and groundwater contamination; transformation of contaminants in the hyporheic zone; effects of contaminants traversing the hyporheic zone on surface water and groundwater ecosystems; subsurface carbon sequestration and/or turnover; and migration of fluids associated with energy production into groundwater.
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