Tap water isotopes reflect urban water system structure and management practices Isotopic patterns linked to political boundaries and demographic factors across Salt Lake Valley Evaporation from city water sources increased by >9400 m3/day during unusually warm, dry years Supporting Information: Supporting Information S1 Correspondence to: Y. Jameel,
Tracers commonly used by UGS scientists include stable isotopes of water (oxygen-18 [δ 18 O] and deuterium [δ 2 H]), tritium (3 H), noble gases (helium, neon, argon, krypton, and xenon), and radiocarbon (carbon-14 [ 14 C] and carbon-13 [δ 13 C]). FIGURE: Piper diagram of water chemistry in bedrock wells in Ogden Valley, Weber County, Utah.
More information is available here. ArcGIS Grids. Downloadable water isotope data bundles for use in ArcGIS. Bundles include data site locations and raster datasets in ArcGIS Grid format.
For over 100 years, the U.S. Geological Survey has been collecting water data in Utah with support from Federal, State, and local Cooperators. A list of our current cooperators is available online . These pages provide access to water-resources data collected at approximately 1.5 million sites in all 50 States, the District of Columbia, and Puerto Rico. Utah will continue to host Isotopes in Spatial Ecology and Biogeochemistry (aka the SPATIAL Short Course), which extends on the fundamentals covered in IsoCamp to develop theory and techniques for applying isotope and biogeochemical tracer data to spatial problems at a range of scales. Gabe Bowen, University of Utah.
A strontium isotope baseline for inland southwestern Sweden. PLOS ONE 257 S 1400 E, Salt Lake City, Utah, USA 84112 http://stableisotopes.utah.edu/ lectures on water isotopes in #IsoCamp2018, #isocamp University of Utah Increased water-use efficiency and reduced CO2 uptake by plants during National Oceanic and Atmospheric Administration (NOAA); University of Utah Isotope abundance ratio measurements by inductively coupled plasma-sector field Sediment and water interactions with macrophyte element concentrations Post-doc Ecophysiology, University of Utah, 1988-1990 plants under changing ambient CO2: evidence from carbon isotope discrimination in paleo and CO2 enrichment studies. Simulated water budget of a small forested watershed in the Diffusion coefficient in water at 100#C salt (saltlager i Utah och saltdomer i.
Uta/M Utah/M Utahan/MS Ute/M Utica/M Utopia/MS Utopian/S Utrecht/M Utrillo/M Waterloo/SM Waters/M Watertown/M Watkins Watson/M Watt/MS Watteau/M isotherm/MS isothermal/Y isotonic isotope/SM isotopic isotropic isotropically
Water Isotopes: “Kinds” of Water. At first it might seem that kinds of water with the chemical structure H 2 O based on isotope differences only, are 9 in number: 1 H 2 16 O, H 2 16 O, 3 H 2 16 O, 1 H Tracers commonly used by UGS scientists include stable isotopes of water (oxygen-18 [δ 18 O] and deuterium [δ 2 H]), tritium (3 H), noble gases (helium, neon, argon, krypton, and xenon), and radiocarbon (carbon-14 [ 14 C] and carbon-13 [δ 13 C]). FIGURE: Piper diagram of water chemistry in bedrock wells in Ogden Valley, Weber County, Utah. - JPEG maps and GIS datasets of geographic water isotope ratio patterns.
av SM Bergström · Citerat av 52 — deeper-water successions such as that at Hunneberg, where the P. elegans Zone has a raphic studies using 13C, an isotope known to be preserved also in the famous Lower Ordovician section in western Utah, which is the reference
19 nov. 2013 — stocked with the mix of isotopes needed for fusion to occur, Nature reported. each day, 400 tonnes of groundwater flood Japan's stricken nuclear plant.
Over the past two decades, however, new data, data compilations, and quantitative methods have supported the application of isotopic data to address large-scale water cycle problems. Recent results have demonstrated the impact of climate variation on atmospheric water cycling, provided
Water isotope ratios are powerful tools for uncovering the mechanisms driving past, present, and future changes in the global water cycle. With the ability to “tag” moisture as it travels through the atmosphere, ocean, biosphere, and cryosphere, isotopes ratios provide insights into key processes that shape regional to global hydrological variability. Part of the Pre-Summit Webinar Series for the 2019 US CLIVAR Summit.
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Water isotope ratios are powerful tools for uncovering the mechanisms driving past, present, and future changes in the global water cycle. With the ability to “tag” moisture as it travels through the atmosphere, ocean, biosphere, and cryosphere, isotopes ratios provide insights into key processes that shape regional to global hydrological variability.
BRETT J. TIPPLE,1,2 GLEN N. MACKEY,3 SCOTT A. HYNEK,1,3 DIEGO P. FERNANDEZ, 3 AND JAMES R. EHLERINGER 1,2 1IsoForensics, Inc., 421 Wakara Way, Suite 100, Salt Lake City, Utah 84108 USA 2Department of Biology, University of Utah, 257 South 1400 East, Salt Lake City, Utah 84112 USA oxygen isotope composition of cellulose is affected not only by the oxygen isotope composition of medium water at the sites of cellulose formation, but also the oxygen isotope composition of water at sites of photosynthate production in leaves that carries a strong Fig. 1.
oxygen isotope composition of cellulose is affected not only by the oxygen isotope composition of medium water at the sites of cellulose formation, but also the oxygen isotope composition of water at sites of photosynthate production in leaves that carries a strong Fig. 1.
An interactive calculator allowing you to estimate water isotope values for any site.
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