How can groundwater flow direction be determined at a site?

Prepare for the Site Characterization Exam 1 with flashcards, multiple-choice questions, and detailed explanations. Enhance your knowledge effectively and increase your chances of acing the exam!

Multiple Choice

How can groundwater flow direction be determined at a site?

Explanation:
Groundwater flow follows the hydraulic gradient, moving from higher hydraulic head to lower hydraulic head. To determine flow direction at a site, measure hydraulic heads at multiple wells across the area, ideally during the same groundwater conditions. Use those head values to compute the gradient between locations and plot head contours (equipotential lines) on a map. The flow direction is perpendicular to these contours, from high head toward low head, which aligns with Darcy’s law that relates flow to the gradient. Rainfall intensity tells you about recharge, not the current direction of groundwater movement. Soil color doesn’t indicate the subsurface hydraulic gradient, and surface temperature reflects near-surface conditions rather than subsurface flow.

Groundwater flow follows the hydraulic gradient, moving from higher hydraulic head to lower hydraulic head. To determine flow direction at a site, measure hydraulic heads at multiple wells across the area, ideally during the same groundwater conditions. Use those head values to compute the gradient between locations and plot head contours (equipotential lines) on a map. The flow direction is perpendicular to these contours, from high head toward low head, which aligns with Darcy’s law that relates flow to the gradient.

Rainfall intensity tells you about recharge, not the current direction of groundwater movement. Soil color doesn’t indicate the subsurface hydraulic gradient, and surface temperature reflects near-surface conditions rather than subsurface flow.

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