lesson 3 Flashcards
Hydrological Cycle
INFILTRATION
PERCOLATION
Most readily occurs through open fractures such as joints in exposed rock
and the gaping cracks
INFILTRATION
Once the water has penetrated the surface, it may commence on a downward journey towards the water table
PERCOLATION
Fluid Storage and Mobility
POROSITY
PERMEABILITY
Is the proportion of void space in the material, unfilled by solid material to
the total volume
POROSITY
Measure how readily fluids pass through the material. It is related to the extent to which pores or cracks are interconnected
PERMEABILITY
Subsurface Waters
SATURATED ZONE
UNSATURATED ZONE
WATER TABLE
phreatic zone is the zone where the voids of the soil are fully occupied by
water. It is where the groundwater is found and at most, a few kilometers
into the crust
SATURATED ZONE
Or vadose zone is the zone mostly above the saturated zone, where rocks or soil in which the pore spaces are filled partly with water
UNSATURATED ZONE
Is the top surface of the saturated zone, where the saturated zone is not confined by overlaying impermeable rocks.
WATER TABLE
Aquifers and Groundwater Flow
AQUIFER
CONFINED AQUIFER
UNCONFINED AQUIFER
DARCY’S LAW AND GROUNDWATER FLOW
Is a rock or soil that holds enough water and transmits it rapidly enough to
be useful as a source of water.
AQUIFER
Is bounded above and below by low-permeability rocks (aquitards).
CONFINED AQUIFER
Directly overlain by permeable rocks and soil
UNCONFINED AQUIFER
States how readily the groundwater can move through rocks and soil, and
this movement basely is governed by permeability. Groundwater flows from
areas of higher hydraulic head to lower.
DARCY’S LAW AND GROUNDWATER FLOW