Summary: Groundwater Processes

Study material generic cover image
  • This + 400k other summaries
  • A unique study and practice tool
  • Never study anything twice again
  • Get the grades you hope for
  • 100% sure, 100% understanding
PLEASE KNOW!!! There are just 51 flashcards and notes available for this material. This summary might not be complete. Please search similar or other summaries.
Use this summary
Remember faster, study better. Scientifically proven.
Trustpilot Logo

Read the summary and the most important questions on Groundwater Processes

  • 1 Introduction

  • 1.1 Powerpoint

    This is a preview. There are 7 more flashcards available for chapter 1.1
    Show more cards here

  • What are three things you need to know about ground water?

    1. Resupplied by infiltration
    2. Often cleaner than surface water
    3. Accessed by wells
  • On what two things does the velocity of ground water depends on?

    1. Slope
    2. Permeability
  • What are typical artesian systems? (4 things)

    - Dunes with peat grow
    - Glacial systems with outwash (stuwwallen)
    - Permafrost systems 
    - Fracture zones in cristaline rock
  • 2 Principles of Saturated flow

  • 2.1 Powerpoint

    This is a preview. There are 4 more flashcards available for chapter 2.1
    Show more cards here

  • What is \/H (triangle)?

    A vector of H that point to the location where the increase of H is the strongest.
  • What are three limitations to Darcy's law?

    1. Neglectance of velocity head
    2. Doesn't work when reynolds number >1 
    3. Doesn't work when groundwater density (rho) varies spatially
  • When is the hydraulic head not a correct measure for energy?

    When the density differs.
  • 3 Permeability and resistance

  • 3.1 Powerpoint

    This is a preview. There are 2 more flashcards available for chapter 3.1
    Show more cards here

  • When is a layer isotropic?

    When the hydraulic conductivity K at each location is the same in all directions.
  • When is a layer heterogeneity?

    When the K is not the same at every location.
  • When is a layer anisotropy?

    When the value of K at a location depends on the direction.
  • What is shear flow?

    Flow rate varies perpendicular to flow direction.
PLEASE KNOW!!! There are just 51 flashcards and notes available for this material. This summary might not be complete. Please search similar or other summaries.

To read further, please click:

Read the full summary
This summary +380.000 other summaries A unique study tool A rehearsal system for this summary Studycoaching with videos
  • Higher grades + faster learning
  • Never study anything twice
  • 100% sure, 100% understanding
Discover Study Smart

Topics related to Summary: Groundwater Processes