Darcy’s Law quantifies groundwater flow as a function of:
Mathematically, Darcy’s Law is expressed as:
\[ Q = K I A \]
where:
Although Darcy’s Law considers permeability, hydraulic gradient, and cross-sectional area, its primary purpose is to quantify the volume of water flowing per unit time in a porous medium.
Darcy’s Law is fundamental in hydrogeology, helping estimate groundwater movement and manage water resources effectively.
In the isochemical phase diagram shown below, the curved arrow represents the P-T path. The variance at peak metamorphism is _.
The units A to H marked on the figure represent different rock formations. Select the option that describes the chronological sequence from old to young.
Consider two intersecting, north-easterly striking and south-easterly dipping dikes Y1 and Y2, which are exposed on an east-west trending vertical wall of a granite (X) quarry as shown below.
The angle that the dikes make with the horizontal on the quarry wall is