Sierra Nevada Flashcards
What is the difference between permeability vs. porosity?
Permeability: ability to allow water to flow through rock
Porosity: refers to ability to store water within holes (pores) within rock
What is a confined aquifer?
- Water is stored in porous rock surrounded by impermeable rock
- Means water can’t flow away or aquifer be replenished
What is an unconfined aquifer?
- Porous rock surrounded by permeable
- means water can percolate and flow out of aquifer
What do the Rockies act as?
- a watershed (AKA drainage basin)
- Colorado River basin flows into West -> Mexico
- Great Plains basin is in East
- Includes Ogallala Aquifer
What inputs are there into river basins?
- Rainfall (convectional or frontal)
- Location determined by proximity to ocean (frontal) or topography (convectional)
- eg. Mountains create rain shadows
- Location determined by proximity to ocean (frontal) or topography (convectional)
- Rocky Mountain snowpack meltwater feeds river seasonally
What affects the output from river basins?
- Level of interception (may vary due to extent of deforestation)
- Level of runoff
- eg. Caliche in Great Plains reduces infiltration
- Geology
- Only unconfined aquifers will be replenished
What are the reasons for variation in hydrological balance of river basins?
- Anthropogenic:
- Eg. Human extraction of water from confined aquifers
- Secular: LT climate change (reduction of water in Colorado Basin and Great Plains)
- Periodity:
- Annual, seasonal, monthly, diurnal changes to water flow
- Stochastic:
- random factors eg. localised thunderstorms
What is the main input of water into the Colorado River basin?
- Rain from North Pacific Ocean front systems
- cold frontal systems leave snow on the Sierra Nevada
- Rain shadow effect on east side of SN (Death Valley/Mojave desert)
- snowmelt during summer provides runoff
What is caliche?
- impermeable layer of calcium carbonate on bottom of aquifer
- prevents it from being recharged
What has happened to the water table in the Great Plains?
- dropped by 1.5m/yr
- wells have been deepened to access water
- in some places water has been totally drained
What sort of aquifer is the High Plains aquifer?
- unconfined
- parts of the aquifer is covered by a caliche layer
- permeability is allowed by playa lakes
What are the main uses of water in the Colorado River Basin?
Irrigation:
- 2.1m acres to 15.5m acres in 2015
What is grown in the Colorado River Basin?
- wheat (largest in US)
- ethanol
- cotton
- cheese (largest in world)
Why is there water insecurity in the Colorado River Basin?
- The High Plains aquifer is unconfined for now
- deterioration of playa soils is increasing though
- region is semi-arid, evaporation rate is high
- steady winds are also present —> evaporation
- increased evaporation is increasing amount of caliche in soil
- making aquifer more confined
What are Playa Lakes?
- lakes which have soil that does not contain caliche
- allows for aquifer to be recharged
- farming destroys playa
- creates layer of caliche as soil moisture evaporates