Ground Water 1 Flashcards
why use GW
- excellent source of potable water
- largest available reservoir of fresh water
- resilient to drought
GW uses
- large use in irrigation
- supplies baseflow to rivers and streams
- augment river flow in droughts
GW characteristics
- areally distributed
- slow response
- low capital but high operational (pumping costs)
- lack of data thus loads of interpolation
potential sources of GW contamination
- petrol/sewage leaks
- nitrates (agriculture)
- landfill
water as a mineral
- anarchic behaviour
- lead to a bunch of legisation
aquifer materials
principle
- chalk
- sandstone
- limestone
superficial
- glacial deposits
- river deposits
- weathering deposits
aquifer definition
geological formation capable of yielding economic quantities of water through wells
ground water resource evalation
Exploration
- surface/subsurface geological/geophysical data
- surface hydrological data
- hydrogeological data
Evaluation
- getting parameters
- determine yield
Exploration
- well installation
- observation well construction: well screen, gravel pack, development
aiming towards a sustainable reservoir
well installation techniques
Shallow
- hand dug
- driven
- bored
Deep = drilling
- cable tool
- rotary
- reverse rotary
getting aquifer parameter
- pumping test = transmissivity, storativity, specific yield
- piezometer test = permeability
- lab tests = permeability, porosity, alpha?
evaluation: yield
well = max pumping without lowering the water level to below inlet
aquifer = max withdrawal with acceptable reduction in acquifer hydraulic head
catchment = same as aquifer plus no unacceptable changes to the basins hydrological cycle
- forms basis for safe yield
sustainable yield
- less than annual recharge (rainfall, leakages from lakes n dat, artificial)
- doesnt lower the water table to allow intrusion of water at undesirable quality
catchment water balance
- sustainable lead to a rate of change of ground storage as zero
in general: pumping leads to reduced discharge and increased recharge
groundwater footprinit
indication of how stressed an aquifer is