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Hydrologic Geochemical Correlations with Bacterial ...
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Hydrologic Geochemical Correlations with Bacterial Communities in a 52°C Hot Spring and its Outflow Channel, Thermopolis, Wyoming
Hydrologic Geochemical Correlations with Bacterial Communities in a 52°C Hot Spring and its Outflow Channel, Thermopolis, Wyoming
Name:Personal
Barlow, Brittany Role :Text(marcrelator)
creator
Barlow, Brittany Role :Text(marcrelator)
creator
Name:Personal
Christopherson, Jared Role :Text(marcrelator)
creator
Christopherson, Jared Role :Text(marcrelator)
creator
Name:Personal
Forbis, Sabrina Role :Text(marcrelator)
creator
Forbis, Sabrina Role :Text(marcrelator)
creator
Name:Personal
Gopher, Marietta Role :Text(marcrelator)
creator
Gopher, Marietta Role :Text(marcrelator)
creator
Name:Personal
Hammer, Selena Role :Text(marcrelator)
creator
Hammer, Selena Role :Text(marcrelator)
creator
Name:Personal
Smaglik, Suzanne M. Role :Text(marcrelator)
contributor
Smaglik, Suzanne M. Role :Text(marcrelator)
contributor
Name:Personal
McAllister, Steven J. Role :Text(marcrelator)
contributor
McAllister, Steven J. Role :Text(marcrelator)
contributor
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Origin Information
Place
Laramie, Wyoming
University of Wyoming (keyDate="yes")
2009-05-12
Laramie, Wyoming
University of Wyoming (keyDate="yes")
2009-05-12
Language:Text
eng
eng
Physical Description
born digtal
born digtal
abstract
The Big Spring in Hot Springs State Park, Thermopolis, Wyoming, flows at an average rate of about 14 million L/day at a temperature between 52 - 54°C. The spring is geologically controlled by an east-west trending fault. Water and microbial samples have been collected on a semi-regular basis from August 2008 to present. At each of 20 sites, water is tested in the field for temperature and pH. Two water samples are collected at each site. One sample is filtered (0.45 m) and the unfiltered sample is frozen for further analysis. Quantitative and semi-quantitative laboratory tests are performed on the filtered water samples. There is a clear correlation of decreasing temperature and pH with distance from the source. Phosphate, SiO2, Ca-Mg hardness, Cl- and total dissolved solids (TDS) show little variation and nitrate and dissolved oxygen are undetectable. The water becomes cloudy white about half way down the outflow, which may reflect the precipitation of sulfate and carbonate minerals with cooling temperature. The morphology of the microbial communities changes from purple and green cyanobacteria filaments at the source, to white filaments at the outflow and finally to mat with trapped gas (O2?) bubbles toward the cooling pond. note
From - Undergraduate Research Day 2009 - Celebration of Research - Abstracts
Subject
Hot Springs State Park
Hot Springs State Park
Subject
bacterial communities
bacterial communities
Related Item:series
Title Information
Undergrauate Research Day 2009
Undergrauate Research Day 2009
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http://digital.uwyo.edu/copyright.htm
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English :Code(ISO639-2B)
eng
English :Code(ISO639-2B)
eng