Steady-state flow refers to a condition where the flow of groundwater remains constant over time, meaning that the hydraulic conditions within a system do not change as time progresses. This concept is vital for understanding how groundwater systems behave under stable conditions, allowing for the application of various mathematical equations to describe flow, such as those derived from Darcy's Law. In this state, all variables like hydraulic head and flow rate remain constant, simplifying analysis and predictions in groundwater studies.
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