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11 Cards in this Set

  • Front
  • Back

Hydrogeology definition

Study of the distribution, movement, and quality of water through soil and rock

Water balance

dS/dT = flux in - flux out



Storage / time

Steady state

Flux in is equal to flux out

Recharge

Infiltration - Evapotranspiration

Porosity

The fraction of the material volume that is pore space



Phi = Vpore / Vtotal

Typical porostiy

Sand 25 - 50%


Silt 35 - 50%


Clay 40 - 70%

Effective porosity

The volume of interconected pore space

Primary Porosity

The porosity developed by the original sedimentation and cementation process by which the rock was created

Secondary Porosity

Created by processes other than primary compaction and cementation of the sediments (fracture)

Dynamic Porosity

Reduction in porosity due to chemical precipitation, bioclogging



Reduction due to dissolution

REV

Representative Elementary Volume



Small enough to exclude landscape scale heterogeneity large enough to contain statistically representative number of pores