Lecture 7/8: Groundwater Flashcards
groundwater stats
provides a larger percentage of community and non-community public water systems, 80k Million gallons are withdrawn every day,
supplies 1/2 the US pop, 1/3 the world’s pop. 0.6% of total freshwater.
sources of groundwater contamination. what is the largest?
injection well, unlined landfill, septic tank, fertilizer, drinking water well, pumping well sewer leakage, salt-water intrusion, runoff (roads and agricultural),
Leaky underground storage tanks are the largest nation=wide (half of every underground storage tank leaks), followed by septic systems and landfills
characteristics of petroleum spills
- Mixtures: hundreds of different compounds, typically find benzene,toluene, ethylbenzene, and xylenes.
- Petroleum-related pollution threaten ground water uses, e.g.,benzene is a carcinogen
- Added compounds to boost performance may be potent pollutants, e.g., methyl tert-butyl ether (MTBE) is highly water soluble
- the most significant impacts occur in the uppermost aquifer.
Top 5 contaminants at superfund sites
Trichloroethylene, lead, toluene, benzene, PCBs
What are the challenges associated with Groundwater contamination?
- Can’t direct see or often measure controlling parameters
- difficult and expensive to measure anything
- Groundwater system operates at many scales, from
microscopic (pore) to regional water systems, to global
hydrosphere. - Dynamic system
- Complex physical, chemical, and biological processes
- Extremely limited validation of models
saturated vs unsaturated zones
unsaturated / vadose zone > capillary fringe > saturated zone (i.e. the water table)
describe the different characteristics of the A,B, and C horizon
A - organic layer, clay and sand
B and C - much less oxygen
soil size distribution
cobbles (100mm), gravel(10mm), sand(0.1mm), clay (smaller)
however different groups define this different ways
describe the hydrologic cycle
evapotranspiration
surface runoff
precipitation
infiltration
Precipitation = Surface Runoff + Evapotranspiration + Groundwater Recharge
Soil and Rock structure
A - well sorted sediment with high porosity
B - poorly sorted sediment deposit with low porosity
E - rock rendered porous by solution
F - rock rendered porous by fracturing
filtration mechanisms
surface filtration, straining, physical and chemical adsorption
the vadose zone
soil zone (organic rich A horizon), intermediate zone, capillary fringe, multiphase system, unsaturated,
Aquifer Recharge
areas that allow for recharge of groundwater through precipitation, arise because of permeability of soil, amount of rainfall, soil moisture content. These zones need protecting against contamination!
physical properties of soil
soil texture, infiltration rate, porosity, specific gravity, field capacity, crop extractable water,
Aquifer
flowing artisian, non-flowing artisian, water-table well
sand aquifer - water is found between pores, sand and gravel in alluvial valleys,
bedrock aquifers - sandstone, limestone. water within fissures and crevices
confined (artisian) vs unconfined (phreatic) - flowing means that well head or pressure is above surface, so water flows without pumping