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...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Aquatic geochemistry 2000-01, Vol.6 (1), p.19-46
Hauptverfasser: Johannesson, Kevin H, Lyons, W Berry, Graham, Elizabeth Y, Welch, Kathleen A
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 46
container_issue 1
container_start_page 19
container_title Aquatic geochemistry
container_volume 6
creator Johannesson, Kevin H
Lyons, W Berry
Graham, Elizabeth Y
Welch, Kathleen A
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
format Article
fullrecord <record><control><sourceid>proquest</sourceid><recordid>TN_cdi_proquest_miscellaneous_17452694</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>17452694</sourcerecordid><originalsourceid>FETCH-LOGICAL-a346t-9d8774763c3409bc7d83f45aa11e296ce444a2f53c4536fc3566449d377f34963</originalsourceid><addsrcrecordid>eNpdjj1PwzAYhC0EEqUws1oMTE3xx2s7ZitV-ZAKlaCwVm8TB6VKbbCTiv57gmBiujvpudMRcs7ZmDMhrybXnDGrhRDcQi4OyIArIzMOgh_2XuYs01yrY3KS0oYx3pfYgFSLrz36Ong6Db5wvo3Y9inR2tMZptZFT19qFyPSJ7fDEulzvXMx0YzKMb0JMfgRfQzNfl06321H9A09lvWPQ1_SZeff-xF_So4qbJI7-9Mheb2dLaf32Xxx9zCdzDOUoNvMlrkxYLQsJDC7LkyZywoUIudOWF04AEBRKVmAkroqpNIawJbSmEqC1XJILn93P2L47FxqV9s6Fa5p0LvQpRU3oIS20IMX_8BN6KLvv616xCrImZXfIFljmA</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>745954809</pqid></control><display><type>article</type><title>Oxyanion Concentrations in Eastern Sierra Nevada Rivers - 3. 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 &amp; Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric &amp; 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 &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric &amp; 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>
fulltext fulltext
identifier ISSN: 1380-6165
ispartof Aquatic geochemistry, 2000-01, Vol.6 (1), p.19-46
issn 1380-6165
1573-1421
language eng
recordid cdi_proquest_miscellaneous_17452694
source SpringerLink Journals
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
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-14T10%3A56%3A25IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Oxyanion%20Concentrations%20in%20Eastern%20Sierra%20Nevada%20Rivers%20-%203.%20Boron,%20Molybdenum,%20Vanadium,%20and%20Tungsten&rft.jtitle=Aquatic%20geochemistry&rft.au=Johannesson,%20Kevin%20H&rft.date=2000-01-01&rft.volume=6&rft.issue=1&rft.spage=19&rft.epage=46&rft.pages=19-46&rft.issn=1380-6165&rft.eissn=1573-1421&rft_id=info:doi/10.1023/A:1009622219482&rft_dat=%3Cproquest%3E17452694%3C/proquest%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=745954809&rft_id=info:pmid/&rfr_iscdi=true