• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/18

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

18 Cards in this Set

  • Front
  • Back

Definition of Ground Water

Subsurface water that occurs beneath the water table in geological sediments and formations that are fully saturated.


Saturated zone = phreatic zone


Unsatrated zone = vadose zone or partially saturdated zone

Water table is

A capillary zone, so ground water is not necesarily also below the water table

Meteoric water

Derives from surface sources like water

Magmatic

Juvenile water formed as a result of magmatic processes. Juvenile water has not contracted the atmosphere.

Connate

Born together water has remained trapped in sedimentary rock since ages ago. Old and saline.

Aquiclude

Saturated and impermeable

Aquitard

Saturates and low permeability

Aquifuge

Impermeable and not containing nor transmiting water.

Aquifer dynamics

Rainwarer infiltrares porous soil and rock and flows through the underground toward lakes and other water bodies. During wet periods, water table is high and natural springs can occur.


During dry peroiods, evapouration discharges underground water in soils. Water tables fall and shallow wells dry up.


Water from streams and lake infiltrates and recharges the surfaes sol and rock.

Aquifer specific yield is

Volume of water drained from saturated unit volume by lowering water table by i unit

Aquifer specific storage is

volume of water remaining in satruated unit volume after gravity drainage.

Refer to storage calculations

blah

Issue with well pumping

Withdrawl of gw causes


-Subsidence


-ground collapse


-salt water intrusion



Predicition and prevention

Gravity and pressure drive flow, low permeabitlyt and lack of recharge resist flow.

Unconfined well pumpin g

Rate of flow is directly proportional to the drop in the water table, Greater drop means higher flow.

COnfined well pumping

Use dupit assumption and apply darcys law.

Types of aquifer well testing

Well performance


-Simple and effective


-Does not describe aquifer


Well and Observation wells


-Measures aquifer performance


-Can be used to predict effects on neighbouring wells



Aquifer test design

Measure pumping rate


Water depths


Time


and compare on two graphs :)


Mind the


-Rain


-Change in ATm pressure


-Stream flow