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Laboratory simulation of groundwater hydraulic head in a karst aquifer system with conduit and fracture domains

机译:带裂缝和裂缝域的岩溶含水层系统地下水液压头的实验室模拟

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A karst analog model has been developed for simulating karst aquifer systems with fracture and conduit domains in the laboratory. In this study, sixty-four experiments under different recharging and discharging conditions were carried out with the analog setup to study flow in the karst analog model. The experiments did not only provide hydraulic head data but spring discharge process as well. The experimental results were used to obtain empirical models of water hydraulic head under different hydrological conditions, which together with the spring discharge analysis aided in developing a water hydraulic head prediction model for the analog model. The results showed that water hydraulic head increased with logarithm of time and declined in step-shaped style, which can be used in karst aquifer systems research. Consequently, the study provides useful information for a better understanding of flow in karst aquifer systems.
机译:已经开发了一种岩溶模拟模型,用于模拟喀斯特含水层系统,在实验室中使用骨折和导管域。 在这项研究中,在不同再充电和放电条件下进行了六十四个实验,以模拟设置进行了岩溶模拟模型的流动。 实验不仅提供液压头数据,而且还提供弹簧放电过程。 实验结果用于在不同水力条件下获得水液压的经验模型,其与弹簧放电分析相同,辅助模拟模型的水液头预测模型。 结果表明,水液头随着时间的对数而增加,在沼状风格中下降,可用于喀斯特含水层系统研究。 因此,该研究提供了更好地理解在喀斯特含水层系统中的流动的有用信息。

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