Specific Conductance Data for Selected Rivers and Creeks in Yellowstone National Park, beginning in 2010
Dates
Publication Date
2019-01-28
Start Date
2010
End Date
2018
Citation
McCleskey, R.B., and Stevens, E.B., 2019, Specific conductance cata for selected rivers and creeks in Yellowstone National Park, beginning in 2010: U.S. Geological Survey data release, https://doi.org/10.5066/F7BP011G.
Summary
This data release has been superseded by a more recent version, which can be found here: https://www.sciencebase.gov/catalog/item/5e860936e4b01d50927fa6dd Monitoring the chloride (Cl) flux in the major rivers draining Yellowstone National Park (YNP) provides a holistic view of the thermal output from the underlying magma chamber, and abrupt fluctuations in the Cl flux may signify changes in thermal activity. The U.S. Geological Survey (USGS) and the National Park Service (NPS) have collaborated on Cl flux monitoring of the major rivers since the 1970s. In the past, researchers collected water samples from the major rivers in YNP, but funding restrictions, winter conditions, and the great distances between sites limited the number [...]
Monitoring the chloride (Cl) flux in the major rivers draining Yellowstone National Park (YNP) provides a holistic view of the thermal output from the underlying magma chamber, and abrupt fluctuations in the Cl flux may signify changes in thermal activity. The U.S. Geological Survey (USGS) and the National Park Service (NPS) have collaborated on Cl flux monitoring of the major rivers since the 1970s. In the past, researchers collected water samples from the major rivers in YNP, but funding restrictions, winter conditions, and the great distances between sites limited the number of samples collected annually. Beginning in 2010, specific conductance, which is relatively easy to measure and can be automated, has been used as a proxy for Cl. The use of specific conductance probes at the various monitoring sites enables a more consistent estimation of Cl flux. Consistent monitoring is useful to identify changes in river chemistry due to geyser eruptions, rain events, or changes in thermal inputs caused by earthquakes or other natural events. The use of specific conductance as a proxy for Cl requires quantification of the relationship between specific conductance, Cl, and other geothermal solutes and the relationship needs to be periodically verified. This data release contains specific conductance measurements (every 15 minutes) and water chemistry data from monitoring sites along the Madison River, Firehole River, Gibbon River, Snake River, Gardner River, Fall River, Yellowstone River, and Tantalus Creek. For several sites, there are periods of time when specific conductance is not reported because the data was likely unreliable because the specific conductance probe failed or was fouled. There are also specific conductance and discharge data available from the U.S. Geological Survey National Water Information System (USGS NWIS, https://waterdata.usgs.gov/nwis/rt).
The following list details the sites included in this data release and the National Water Information System site identification numbers.
Yellowstone River near Corwin Springs, 06191500;
Gardner River near Mammoth, 06191000;
Firehole River near West Yellowstone, 06036905;
Firehole River at Old Faithful, 06036805;
Fall River near Squirrel, Idaho, 13046995;
Gibbon River at Madison Junction, 06037100;
Madison River near West Yellowstone, 06040000;
Snake River near Flagg Ranch WY, 13010065;
and Tantalus Creek at Norris Junction, 06036940.
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Purpose
To provide specific conductance and water chemistry data from the following chloride-flux monitoring sites: Yellowstone River near Corwin Springs, Gardner River near Mammoth, Firehole River near West Yellowstone, Firehole River at Old Faithful, Fall River near Squirrel, Idaho, Gibbon River at Madison Junction, Madison River near West Yellowstone, Snake River near Flagg Ranch, and Tantalus Creek at Norris Junction.
