<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>D. Kirk Nordstrom</dc:contributor>
  <dc:contributor>R. Blaine McCleskey</dc:contributor>
  <dc:contributor>Martin A.A. Schoonen</dc:contributor>
  <dc:contributor>Yong Xu</dc:contributor>
  <dc:creator>James W. Ball</dc:creator>
  <dc:date>2001</dc:date>
  <dc:description>Fifty-eight water analyses are reported for samples collected from 19 hot springs and their&#13;
overflow drainages and one ambient-temperature acid stream in Yellowstone National Park (YNP)&#13;
during 1996-98. These water samples were collected and analyzed as part of research investigations&#13;
on microbially mediated sulfur oxidation in stream waters and sulfur redox speciation in hot springs&#13;
in YNP and chemical changes in overflow drainages that affect major ions, redox species, and trace&#13;
elements. The research on sulfur redox speciation in hot springs is a collaboration with the State&#13;
University of New York at Stony Brook, Northern Arizona University, and the U.S. Geological&#13;
Survey (USGS). One ambient-temperature acidic stream system, Alluvium Creek and its tributaries&#13;
in Brimstone Basin, was studied in detail. Analyses were performed adjacent to the sampling site, in&#13;
an on-site mobile laboratory truck, or later in a USGS laboratory, depending on stability and&#13;
preservability of the constituent.&#13;
Water temperature, specific conductance, pH, Eh, dissolved oxygen (D.O.), and dissolved&#13;
H2S were determined on-site at the time of sampling. Alkalinity and F were determined within a few&#13;
days of sample collection by titration and by ion-selective electrode, respectively. Concentrations of&#13;
S2O3 and SxO6 were determined as soon as possible (minutes to hours later) by ion chromatography&#13;
(IC). Concentrations of Cl, SO4, and Br were determined by IC within a few days of sample&#13;
collection. Concentrations of Fe(II) and Fe(total) were determined by ultraviolet/visible&#13;
spectrophotometry within a few days of sample collection. Densities were determined later in the&#13;
USGS laboratory. Concentrations of Li, Na, and K were determined by flame atomic absorption (Li)&#13;
and emission (Na, K) spectrometry. Concentrations of Al, As(total), B, Ba, Be, Ca, Cd, Co, Cr, Cu,&#13;
Fe(total), Mg, Mn, Ni, Pb, Si, Sr, V, and Zn were determined by inductively-coupled plasma optical&#13;
emission spectrometry. Trace concentrations of Cd, Se, As(total), Ni, and Pb were determined by&#13;
Zeeman-corrected graphite-furnace atomic-absorption spectrometry. Trace concentrations of&#13;
As(total) and As(III) were determined by hydride generation using a flow-injection analysis system.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr0149</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Water-Chemistry and On-Site Sulfur-Speciation Data for Selected Springs in Yellowstone National Park, Wyoming, 1996-1998</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>