Oxyanion Concentrations in Eastern Sierra Nevada Rivers - 3. Boron, Molybdenum, Vanadium, and Tungsten
Water samples were collected from 10 locations along the Truckee River system, 14 locations along the Walker River system, and 12 locations along the Carson River, and analyzed for B, Mo, V, W, Na, Cl, and pH. Boron concentrations ranged from approximately 2 μmol/kg in the upper reaches of the Truck...
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description | Water samples were collected from 10 locations along the Truckee River system, 14 locations along the Walker River system, and 12 locations along the Carson River, and analyzed for B, Mo, V, W, Na, Cl, and pH. Boron concentrations ranged from approximately 2 μmol/kg in the upper reaches of the Truckee River to almost 1,200 μmol/kg in Pyramid Lake. Molybdenum, V, and W had concentrations in the nanomolal range; Mo varied from a low of about 12 nmol/kg to a high of 3,200 nmol/kg (Walker Lake); V ranged from 9 nmol/kg to approximately 470 nmol/kg; and W varied from a low value around 0.8 nmol/kg (West Walker River) to 1,030 nmol/kg. The high concentrations of these oxyanion-forming trace elements in the rivers reflects (1) the relative stability of these oxyanions (e.g., MoO^sub 4^^sup 2-^, HVO^sub 4^^sup 2-^, WO^sub 4^^sup 2-^, B(OH)^sub 3^, and/or B(OH)^sub 4^^sup -^) in the alkaline, well oxygenated river and lake waters, (2) contributions of hydrothermal waters (especially for B), and (3) weathering of rocks/regolith with high concentrations of these elements. In the case of Mo, V, and W, each exhibited relatively conservative behavior in the upper, oxygenated reaches of all three rivers. During the study period the region experienced a prolonged drought such that the lower reaches of each river were typified by no flow or stagnant waters and probably low oxygen and/or anoxic conditions (although not measured). Reductive processes occurring in the low flow to stagnant reaches of each river could have led to removal of Mo, V, and W from solution as coprecipitates with Fe monosulfides, or via sorption to Fe oxides/oxyhydroxides and/or organic matter. Boron, however, exhibited essentially no or minor removal from these rivers, and instead was added to each river via B-rich hydrothermal waters (e.g., Steamboat Creek from Steamboat Hot Springs), or by B-rich groundwaters via base-flow during the extensive drought.[PUBLICATION ABSTRACT] |
doi_str_mv | 10.1023/A:1009622219482 |
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Boron, Molybdenum, Vanadium, and Tungsten</title><source>SpringerLink Journals</source><creator>Johannesson, Kevin H ; Lyons, W Berry ; Graham, Elizabeth Y ; Welch, Kathleen A</creator><creatorcontrib>Johannesson, Kevin H ; Lyons, W Berry ; Graham, Elizabeth Y ; Welch, Kathleen A</creatorcontrib><description>Water samples were collected from 10 locations along the Truckee River system, 14 locations along the Walker River system, and 12 locations along the Carson River, and analyzed for B, Mo, V, W, Na, Cl, and pH. Boron concentrations ranged from approximately 2 μmol/kg in the upper reaches of the Truckee River to almost 1,200 μmol/kg in Pyramid Lake. Molybdenum, V, and W had concentrations in the nanomolal range; Mo varied from a low of about 12 nmol/kg to a high of 3,200 nmol/kg (Walker Lake); V ranged from 9 nmol/kg to approximately 470 nmol/kg; and W varied from a low value around 0.8 nmol/kg (West Walker River) to 1,030 nmol/kg. The high concentrations of these oxyanion-forming trace elements in the rivers reflects (1) the relative stability of these oxyanions (e.g., MoO^sub 4^^sup 2-^, HVO^sub 4^^sup 2-^, WO^sub 4^^sup 2-^, B(OH)^sub 3^, and/or B(OH)^sub 4^^sup -^) in the alkaline, well oxygenated river and lake waters, (2) contributions of hydrothermal waters (especially for B), and (3) weathering of rocks/regolith with high concentrations of these elements. In the case of Mo, V, and W, each exhibited relatively conservative behavior in the upper, oxygenated reaches of all three rivers. During the study period the region experienced a prolonged drought such that the lower reaches of each river were typified by no flow or stagnant waters and probably low oxygen and/or anoxic conditions (although not measured). Reductive processes occurring in the low flow to stagnant reaches of each river could have led to removal of Mo, V, and W from solution as coprecipitates with Fe monosulfides, or via sorption to Fe oxides/oxyhydroxides and/or organic matter. Boron, however, exhibited essentially no or minor removal from these rivers, and instead was added to each river via B-rich hydrothermal waters (e.g., Steamboat Creek from Steamboat Hot Springs), or by B-rich groundwaters via base-flow during the extensive drought.[PUBLICATION ABSTRACT]</description><identifier>ISSN: 1380-6165</identifier><identifier>EISSN: 1573-1421</identifier><identifier>DOI: 10.1023/A:1009622219482</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Anoxic conditions ; Base flow ; Boron ; Drought ; Freshwater ; Hot springs ; Lakes ; Low flow ; Molybdenum ; Organic matter ; Rivers ; Trace elements ; Tungsten ; Vanadium ; Water analysis ; Water sampling</subject><ispartof>Aquatic geochemistry, 2000-01, Vol.6 (1), p.19-46</ispartof><rights>Kluwer Academic Publishers 2000</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a346t-9d8774763c3409bc7d83f45aa11e296ce444a2f53c4536fc3566449d377f34963</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Johannesson, Kevin H</creatorcontrib><creatorcontrib>Lyons, W Berry</creatorcontrib><creatorcontrib>Graham, Elizabeth Y</creatorcontrib><creatorcontrib>Welch, Kathleen A</creatorcontrib><title>Oxyanion Concentrations in Eastern Sierra Nevada Rivers - 3. Boron, Molybdenum, Vanadium, and Tungsten</title><title>Aquatic geochemistry</title><description>Water samples were collected from 10 locations along the Truckee River system, 14 locations along the Walker River system, and 12 locations along the Carson River, and analyzed for B, Mo, V, W, Na, Cl, and pH. Boron concentrations ranged from approximately 2 μmol/kg in the upper reaches of the Truckee River to almost 1,200 μmol/kg in Pyramid Lake. Molybdenum, V, and W had concentrations in the nanomolal range; Mo varied from a low of about 12 nmol/kg to a high of 3,200 nmol/kg (Walker Lake); V ranged from 9 nmol/kg to approximately 470 nmol/kg; and W varied from a low value around 0.8 nmol/kg (West Walker River) to 1,030 nmol/kg. The high concentrations of these oxyanion-forming trace elements in the rivers reflects (1) the relative stability of these oxyanions (e.g., MoO^sub 4^^sup 2-^, HVO^sub 4^^sup 2-^, WO^sub 4^^sup 2-^, B(OH)^sub 3^, and/or B(OH)^sub 4^^sup -^) in the alkaline, well oxygenated river and lake waters, (2) contributions of hydrothermal waters (especially for B), and (3) weathering of rocks/regolith with high concentrations of these elements. In the case of Mo, V, and W, each exhibited relatively conservative behavior in the upper, oxygenated reaches of all three rivers. During the study period the region experienced a prolonged drought such that the lower reaches of each river were typified by no flow or stagnant waters and probably low oxygen and/or anoxic conditions (although not measured). Reductive processes occurring in the low flow to stagnant reaches of each river could have led to removal of Mo, V, and W from solution as coprecipitates with Fe monosulfides, or via sorption to Fe oxides/oxyhydroxides and/or organic matter. Boron, however, exhibited essentially no or minor removal from these rivers, and instead was added to each river via B-rich hydrothermal waters (e.g., Steamboat Creek from Steamboat Hot Springs), or by B-rich groundwaters via base-flow during the extensive drought.[PUBLICATION ABSTRACT]</description><subject>Anoxic conditions</subject><subject>Base flow</subject><subject>Boron</subject><subject>Drought</subject><subject>Freshwater</subject><subject>Hot springs</subject><subject>Lakes</subject><subject>Low flow</subject><subject>Molybdenum</subject><subject>Organic matter</subject><subject>Rivers</subject><subject>Trace elements</subject><subject>Tungsten</subject><subject>Vanadium</subject><subject>Water analysis</subject><subject>Water sampling</subject><issn>1380-6165</issn><issn>1573-1421</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2000</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNpdjj1PwzAYhC0EEqUws1oMTE3xx2s7ZitV-ZAKlaCwVm8TB6VKbbCTiv57gmBiujvpudMRcs7ZmDMhrybXnDGrhRDcQi4OyIArIzMOgh_2XuYs01yrY3KS0oYx3pfYgFSLrz36Ong6Db5wvo3Y9inR2tMZptZFT19qFyPSJ7fDEulzvXMx0YzKMb0JMfgRfQzNfl06321H9A09lvWPQ1_SZeff-xF_So4qbJI7-9Mheb2dLaf32Xxx9zCdzDOUoNvMlrkxYLQsJDC7LkyZywoUIudOWF04AEBRKVmAkroqpNIawJbSmEqC1XJILn93P2L47FxqV9s6Fa5p0LvQpRU3oIS20IMX_8BN6KLvv616xCrImZXfIFljmA</recordid><startdate>20000101</startdate><enddate>20000101</enddate><creator>Johannesson, Kevin H</creator><creator>Lyons, W Berry</creator><creator>Graham, Elizabeth Y</creator><creator>Welch, Kathleen A</creator><general>Springer Nature B.V</general><scope>3V.</scope><scope>7QH</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>20000101</creationdate><title>Oxyanion Concentrations in Eastern Sierra Nevada Rivers - 3. Boron, Molybdenum, Vanadium, and Tungsten</title><author>Johannesson, Kevin H ; Lyons, W Berry ; Graham, Elizabeth Y ; Welch, Kathleen A</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a346t-9d8774763c3409bc7d83f45aa11e296ce444a2f53c4536fc3566449d377f34963</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2000</creationdate><topic>Anoxic conditions</topic><topic>Base flow</topic><topic>Boron</topic><topic>Drought</topic><topic>Freshwater</topic><topic>Hot springs</topic><topic>Lakes</topic><topic>Low flow</topic><topic>Molybdenum</topic><topic>Organic matter</topic><topic>Rivers</topic><topic>Trace elements</topic><topic>Tungsten</topic><topic>Vanadium</topic><topic>Water analysis</topic><topic>Water sampling</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Johannesson, Kevin H</creatorcontrib><creatorcontrib>Lyons, W Berry</creatorcontrib><creatorcontrib>Graham, Elizabeth Y</creatorcontrib><creatorcontrib>Welch, Kathleen A</creatorcontrib><collection>ProQuest Central (Corporate)</collection><collection>Aqualine</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Aquatic geochemistry</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Johannesson, Kevin H</au><au>Lyons, W Berry</au><au>Graham, Elizabeth Y</au><au>Welch, Kathleen A</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Oxyanion Concentrations in Eastern Sierra Nevada Rivers - 3. Boron, Molybdenum, Vanadium, and Tungsten</atitle><jtitle>Aquatic geochemistry</jtitle><date>2000-01-01</date><risdate>2000</risdate><volume>6</volume><issue>1</issue><spage>19</spage><epage>46</epage><pages>19-46</pages><issn>1380-6165</issn><eissn>1573-1421</eissn><abstract>Water samples were collected from 10 locations along the Truckee River system, 14 locations along the Walker River system, and 12 locations along the Carson River, and analyzed for B, Mo, V, W, Na, Cl, and pH. Boron concentrations ranged from approximately 2 μmol/kg in the upper reaches of the Truckee River to almost 1,200 μmol/kg in Pyramid Lake. Molybdenum, V, and W had concentrations in the nanomolal range; Mo varied from a low of about 12 nmol/kg to a high of 3,200 nmol/kg (Walker Lake); V ranged from 9 nmol/kg to approximately 470 nmol/kg; and W varied from a low value around 0.8 nmol/kg (West Walker River) to 1,030 nmol/kg. The high concentrations of these oxyanion-forming trace elements in the rivers reflects (1) the relative stability of these oxyanions (e.g., MoO^sub 4^^sup 2-^, HVO^sub 4^^sup 2-^, WO^sub 4^^sup 2-^, B(OH)^sub 3^, and/or B(OH)^sub 4^^sup -^) in the alkaline, well oxygenated river and lake waters, (2) contributions of hydrothermal waters (especially for B), and (3) weathering of rocks/regolith with high concentrations of these elements. In the case of Mo, V, and W, each exhibited relatively conservative behavior in the upper, oxygenated reaches of all three rivers. During the study period the region experienced a prolonged drought such that the lower reaches of each river were typified by no flow or stagnant waters and probably low oxygen and/or anoxic conditions (although not measured). Reductive processes occurring in the low flow to stagnant reaches of each river could have led to removal of Mo, V, and W from solution as coprecipitates with Fe monosulfides, or via sorption to Fe oxides/oxyhydroxides and/or organic matter. Boron, however, exhibited essentially no or minor removal from these rivers, and instead was added to each river via B-rich hydrothermal waters (e.g., Steamboat Creek from Steamboat Hot Springs), or by B-rich groundwaters via base-flow during the extensive drought.[PUBLICATION ABSTRACT]</abstract><cop>Dordrecht</cop><pub>Springer Nature B.V</pub><doi>10.1023/A:1009622219482</doi><tpages>28</tpages></addata></record> |
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subjects | Anoxic conditions Base flow Boron Drought Freshwater Hot springs Lakes Low flow Molybdenum Organic matter Rivers Trace elements Tungsten Vanadium Water analysis Water sampling |
title | Oxyanion Concentrations in Eastern Sierra Nevada Rivers - 3. Boron, Molybdenum, Vanadium, and Tungsten |
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