Geochemical evidence for peat bog contribution to the streamflow generation process: case study of the Vltava River headwaters, Czech Republic
A geochemical approach using stable oxygen isotopes was used to understand streamflow generation processes in the highly peaty catchment of the Rokytka Brook in the headwaters of the Vltava River, Czech Republic. The contribution of water from peat bog areas to the total surface runoff was assessed...
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| Veröffentlicht in: | Hydrological sciences journal 2016-10, Vol.61 (14), p.2579-2589 |
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| container_issue | 14 |
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| container_title | Hydrological sciences journal |
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| creator | Kocum, Jan Oulehle, Filip Janský, Bohumír Bůzek, František Hruška, Jakub Vlček, Lukáš |
| description | A geochemical approach using stable oxygen isotopes was used to understand streamflow generation processes in the highly peaty catchment of the Rokytka Brook in the headwaters of the Vltava River, Czech Republic. The contribution of water from peat bog areas to the total surface runoff was assessed using a hydrological time series, as well as geochemical, hydrochemical and isotope-hydrological approaches for unit hydrogram separation by means of anion deficiency. Using data from the hydrological year 2008, the role of an existing peat bog in the runoff formation dynamics of the Rokytka Brook catchment was determined, and the hydrological cycle was described and assessed using stable
18
O/
16
O isotopes. The research findings strongly support the fact that peatland areas within the studied catchment do not significantly communicate hydraulically with surface streams, and their hydrological function in this region is insignificant.
Editor M. C. Acreman; Associate editor not assigned |
| doi_str_mv | 10.1080/02626667.2016.1140173 |
| format | Article |
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18
O/
16
O isotopes. The research findings strongly support the fact that peatland areas within the studied catchment do not significantly communicate hydraulically with surface streams, and their hydrological function in this region is insignificant.
Editor M. C. Acreman; Associate editor not assigned</description><identifier>ISSN: 0262-6667</identifier><identifier>EISSN: 2150-3435</identifier><identifier>DOI: 10.1080/02626667.2016.1140173</identifier><language>eng</language><publisher>Abingdon: Taylor & Francis</publisher><subject>Anions ; Bogs ; Case studies ; Catchment area ; Catchments ; experimental hydrology ; Freshwater ; geochemical approach ; Geochemistry ; Headwaters ; Hydrologic cycle ; Hydrological cycle ; Hydrology ; Isotopes ; Oxygen isotopes ; Peat ; Peatlands ; Rivers ; runoff formation ; stable oxygen isotopes ; Stream discharge ; Stream flow ; Streams ; Surface runoff ; Vltava River</subject><ispartof>Hydrological sciences journal, 2016-10, Vol.61 (14), p.2579-2589</ispartof><rights>2016 IAHS 2016</rights><rights>2016 IAHS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c418t-23c95607c28c0b0ec34ab1223c4badbfe44b579dd78233fcd0cd481e4ac4b9a93</citedby><cites>FETCH-LOGICAL-c418t-23c95607c28c0b0ec34ab1223c4badbfe44b579dd78233fcd0cd481e4ac4b9a93</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.tandfonline.com/doi/pdf/10.1080/02626667.2016.1140173$$EPDF$$P50$$Ginformaworld$$H</linktopdf><linktohtml>$$Uhttps://www.tandfonline.com/doi/full/10.1080/02626667.2016.1140173$$EHTML$$P50$$Ginformaworld$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,59646,60435</link.rule.ids></links><search><creatorcontrib>Kocum, Jan</creatorcontrib><creatorcontrib>Oulehle, Filip</creatorcontrib><creatorcontrib>Janský, Bohumír</creatorcontrib><creatorcontrib>Bůzek, František</creatorcontrib><creatorcontrib>Hruška, Jakub</creatorcontrib><creatorcontrib>Vlček, Lukáš</creatorcontrib><title>Geochemical evidence for peat bog contribution to the streamflow generation process: case study of the Vltava River headwaters, Czech Republic</title><title>Hydrological sciences journal</title><description>A geochemical approach using stable oxygen isotopes was used to understand streamflow generation processes in the highly peaty catchment of the Rokytka Brook in the headwaters of the Vltava River, Czech Republic. The contribution of water from peat bog areas to the total surface runoff was assessed using a hydrological time series, as well as geochemical, hydrochemical and isotope-hydrological approaches for unit hydrogram separation by means of anion deficiency. Using data from the hydrological year 2008, the role of an existing peat bog in the runoff formation dynamics of the Rokytka Brook catchment was determined, and the hydrological cycle was described and assessed using stable
18
O/
16
O isotopes. The research findings strongly support the fact that peatland areas within the studied catchment do not significantly communicate hydraulically with surface streams, and their hydrological function in this region is insignificant.
Editor M. C. Acreman; Associate editor not assigned</description><subject>Anions</subject><subject>Bogs</subject><subject>Case studies</subject><subject>Catchment area</subject><subject>Catchments</subject><subject>experimental hydrology</subject><subject>Freshwater</subject><subject>geochemical approach</subject><subject>Geochemistry</subject><subject>Headwaters</subject><subject>Hydrologic cycle</subject><subject>Hydrological cycle</subject><subject>Hydrology</subject><subject>Isotopes</subject><subject>Oxygen isotopes</subject><subject>Peat</subject><subject>Peatlands</subject><subject>Rivers</subject><subject>runoff formation</subject><subject>stable oxygen isotopes</subject><subject>Stream discharge</subject><subject>Stream flow</subject><subject>Streams</subject><subject>Surface runoff</subject><subject>Vltava River</subject><issn>0262-6667</issn><issn>2150-3435</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNp9kV9rFDEUxYMouFY_ghDwxQdnTSaZfz4pi7aFglBsX8Od5E43JTNZk8wu2w_hZzbTrS8-9OnCvb9zuJxDyHvO1py17DMr67Ku62ZdMl6vOZeMN-IFWZW8YoWQonpJVgtTLNBr8ibGe8aE7GqxIn_O0estjlaDo7i3BieNdPCB7hAS7f0d1X5KwfZzsn6iydO0RRpTQBgH5w_0DicM8HjcBa8xxi9UQ1yY2RypHx4Fty7BHui13WOgWwRzgIQhfqKbB9Rbeo27uXdWvyWvBnAR3z3NM3Lz4_uvzUVx9fP8cvPtqtCSt6kohe6qmjW6bDXrGWohoedlXsseTD-glH3VdMY0bSnEoA3TRrYcJWSgg06ckY8n3_zy7xljUqONGp2DCf0cFe-WDLuqajP64T_03s9hyt8pnt0r2XWizFR1onTwMQYc1C7YEcJRcaaWltS_ltTSknpqKeu-nnR2yqGPcPDBGZXg6HwYAkzaRiWet_gLS42bRA</recordid><startdate>20161025</startdate><enddate>20161025</enddate><creator>Kocum, Jan</creator><creator>Oulehle, Filip</creator><creator>Janský, Bohumír</creator><creator>Bůzek, František</creator><creator>Hruška, Jakub</creator><creator>Vlček, Lukáš</creator><general>Taylor & Francis</general><general>Taylor & Francis Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>SOI</scope></search><sort><creationdate>20161025</creationdate><title>Geochemical evidence for peat bog contribution to the streamflow generation process: case study of the Vltava River headwaters, Czech Republic</title><author>Kocum, Jan ; Oulehle, Filip ; Janský, Bohumír ; Bůzek, František ; Hruška, Jakub ; Vlček, Lukáš</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c418t-23c95607c28c0b0ec34ab1223c4badbfe44b579dd78233fcd0cd481e4ac4b9a93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Anions</topic><topic>Bogs</topic><topic>Case studies</topic><topic>Catchment area</topic><topic>Catchments</topic><topic>experimental hydrology</topic><topic>Freshwater</topic><topic>geochemical approach</topic><topic>Geochemistry</topic><topic>Headwaters</topic><topic>Hydrologic cycle</topic><topic>Hydrological cycle</topic><topic>Hydrology</topic><topic>Isotopes</topic><topic>Oxygen isotopes</topic><topic>Peat</topic><topic>Peatlands</topic><topic>Rivers</topic><topic>runoff formation</topic><topic>stable oxygen isotopes</topic><topic>Stream discharge</topic><topic>Stream flow</topic><topic>Streams</topic><topic>Surface runoff</topic><topic>Vltava River</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kocum, Jan</creatorcontrib><creatorcontrib>Oulehle, Filip</creatorcontrib><creatorcontrib>Janský, Bohumír</creatorcontrib><creatorcontrib>Bůzek, František</creatorcontrib><creatorcontrib>Hruška, Jakub</creatorcontrib><creatorcontrib>Vlček, Lukáš</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><jtitle>Hydrological sciences journal</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kocum, Jan</au><au>Oulehle, Filip</au><au>Janský, Bohumír</au><au>Bůzek, František</au><au>Hruška, Jakub</au><au>Vlček, Lukáš</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Geochemical evidence for peat bog contribution to the streamflow generation process: case study of the Vltava River headwaters, Czech Republic</atitle><jtitle>Hydrological sciences journal</jtitle><date>2016-10-25</date><risdate>2016</risdate><volume>61</volume><issue>14</issue><spage>2579</spage><epage>2589</epage><pages>2579-2589</pages><issn>0262-6667</issn><eissn>2150-3435</eissn><abstract>A geochemical approach using stable oxygen isotopes was used to understand streamflow generation processes in the highly peaty catchment of the Rokytka Brook in the headwaters of the Vltava River, Czech Republic. The contribution of water from peat bog areas to the total surface runoff was assessed using a hydrological time series, as well as geochemical, hydrochemical and isotope-hydrological approaches for unit hydrogram separation by means of anion deficiency. Using data from the hydrological year 2008, the role of an existing peat bog in the runoff formation dynamics of the Rokytka Brook catchment was determined, and the hydrological cycle was described and assessed using stable
18
O/
16
O isotopes. The research findings strongly support the fact that peatland areas within the studied catchment do not significantly communicate hydraulically with surface streams, and their hydrological function in this region is insignificant.
Editor M. C. Acreman; Associate editor not assigned</abstract><cop>Abingdon</cop><pub>Taylor & Francis</pub><doi>10.1080/02626667.2016.1140173</doi><tpages>11</tpages><oa>free_for_read</oa></addata></record> |
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| source | Taylor & Francis:Master (3349 titles); Alma/SFX Local Collection |
| subjects | Anions Bogs Case studies Catchment area Catchments experimental hydrology Freshwater geochemical approach Geochemistry Headwaters Hydrologic cycle Hydrological cycle Hydrology Isotopes Oxygen isotopes Peat Peatlands Rivers runoff formation stable oxygen isotopes Stream discharge Stream flow Streams Surface runoff Vltava River |
| title | Geochemical evidence for peat bog contribution to the streamflow generation process: case study of the Vltava River headwaters, Czech Republic |
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