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What is Understanding Groundwater Hydrology about?

Groundwater flows through the subsurface due to gravity and the slope of the water table. When it rains, the water table rises dramatically, causing nearby streams to increase in flow. This is because rainfall percolates down and raises the water table. In 1856, Henry Darcy discovered through experiments that the rate of groundwater flow is proportional to the hydraulic gradient and the hydraulic conductivity of the medium. This relationship is expressed mathematically as Darcy

Author

Rizkyy Rachmalya Zainal

Language

EN