Introduction to Groundwater, Karst and the Edwards Aquifer Water color by Kathy Rottier
Groundwater Zones
Alternate image of groundwater zones
Porosity
Permeability
Types of groundwater flow
Aquifer Recharge and Discharge
Groundwater flow timescales
Artesian groundwater systems
Water: the great dissolver and precipitator Dissolves:Precipitates: Limestone, gypsum, salt (makes caves and landscapes these rocks) Cave deposits (stalactites, travertine, etc) Cements that hold sedimentary rocks together (calcareous, siliceous, and ferruginous) Few minerals from sandstones, shales, and igneous and metamorphic rocks (does not make caves in these rocks) Spring and geyser deposits Concretions and geodes
Limestone Dissolution H 2 O + CO 2 = H 2 CO 3 water + carbon dioxide = carbonic acid H 2 CO3 + CaCO 3 = Ca HCO 3 - carbonic acid + calcium carbonate (limestone) = calcium ions + bicarbonate ions
Karst Development: Initial Stage
Karst Development: Intermediate Stage
Karst Development: Late Stage
Karst Terrain Mike Warton
Geologic History of the Edwards Aquifer
Uplifting and Earthquakes
The Edwards Aquifer
Barton Springs Segment (map view)
Barton Springs Segment (cross-section view)
Inner Space Caverns Photos by Marsha Willis
Longhorn Caverns ’Photos by Larry Jayroe
Photo Credit: City of Austin < bartonaerial.jpg>,accessed September 22, 2008
Barton Springs Pool
Example Hydrograph
Discharge at Barton Springs January 1980 – September 2008 Source: USGS,accessed September 19, 2008
Source: bcd071034cf8/original.jpg, accessed September 22, 2008 The End