Variability of particulate (SS, POC) and dissolved (DOC, NO3) matter during storm events in the Alegria agricultural watershed
The temporal variability of suspended sediment, nitrates (NO3) and dissolved (DOC) and particulate organic carbon concentrations was analysed in the Alegria agricultural watershed over a 2‐year period. Nine storm events were studied, including an exhaustive analysis of hydrometeorological conditions...
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Veröffentlicht in: | Hydrological processes 2014-02, Vol.28 (5), p.2855-2867 |
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description | The temporal variability of suspended sediment, nitrates (NO3) and dissolved (DOC) and particulate organic carbon concentrations was analysed in the Alegria agricultural watershed over a 2‐year period. Nine storm events were studied, including an exhaustive analysis of hydrometeorological conditions, quantification of fluxes, and concentration‐discharge hysteresis loop characterization. The overall aim was to study the variability in these components during storm events and determine the mechanisms (flow paths) affecting the trajectories, from the source to the stream. The forms, rotational patterns and trends of hysteretic loops were investigated, and relationships between hysteresis features and hydrological parameters were studied. The results revealed clear differences between particulate (suspended sediment, particulate organic carbon) and dissolved (DOC, NO3) matter transport responses. Movement of the particulate matter was attributed to surface water, as reflected in clockwise hysteresis loops, whereas dissolved matter showed, in general, counterclockwise hysteresis loops, indicating a time delay in the arrival of solutes to the stream. This could be related to subsurface flow paths for DOC and a groundwater source for NO3. Copyright © 2013 John Wiley & Sons, Ltd. |
doi_str_mv | 10.1002/hyp.9850 |
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Nine storm events were studied, including an exhaustive analysis of hydrometeorological conditions, quantification of fluxes, and concentration‐discharge hysteresis loop characterization. The overall aim was to study the variability in these components during storm events and determine the mechanisms (flow paths) affecting the trajectories, from the source to the stream. The forms, rotational patterns and trends of hysteretic loops were investigated, and relationships between hysteresis features and hydrological parameters were studied. The results revealed clear differences between particulate (suspended sediment, particulate organic carbon) and dissolved (DOC, NO3) matter transport responses. Movement of the particulate matter was attributed to surface water, as reflected in clockwise hysteresis loops, whereas dissolved matter showed, in general, counterclockwise hysteresis loops, indicating a time delay in the arrival of solutes to the stream. This could be related to subsurface flow paths for DOC and a groundwater source for NO3. 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Movement of the particulate matter was attributed to surface water, as reflected in clockwise hysteresis loops, whereas dissolved matter showed, in general, counterclockwise hysteresis loops, indicating a time delay in the arrival of solutes to the stream. This could be related to subsurface flow paths for DOC and a groundwater source for NO3. Copyright © 2013 John Wiley & Sons, Ltd.</description><subject>agricultural catchment</subject><subject>dissolved and particulate organic carbon</subject><subject>hysteresis</subject><subject>nitrates</subject><subject>storm-events</subject><subject>suspended sediment</subject><issn>0885-6087</issn><issn>1099-1085</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNpFkF1P2zAUhq1pSOvYpP2EI3EDUtMdN3HiXKLCKKjQSuxDcGO5yTE1pElnO0Bv9ttxBWI357159L5HD2PfOI444vj7arsZlVLgBzbgWJYJRyk-sgFKKZIcZfGJffb-HhEzlDhg_35rZ_XSNjZsoTOw0S7Yqm90IDi8vh7CYj45At3WUFvvu-aRajg8mU-GcDVPj2CtQyAHde9sewc-dG4N9Eht8GBbCCuC44bu4gLoeGNv6J1u4CnWO7-i-gvbM7rx9PUt99mvH6c_J9NkNj87nxzPkmpcSkx4agQazKplxjXmtaHcGFEawjzLCqzLZSWxxCLL8yLVlGfVmLiRGRckdWXKdJ8dvPZuXPe3Jx_Ufde7Nk4qnos4UURNkUpeqSfb0FZtnF1rt1Uc1U6timrVTq2a3ix2-Z-3PtDzO6_dg4p_FEL9uTpTl3JWXNyKqZLpC_o5fF0</recordid><startdate>20140228</startdate><enddate>20140228</enddate><creator>Cerro, Itsasne</creator><creator>Sanchez-Perez, José Miguel</creator><creator>Ruiz-Romera, Estilita</creator><creator>Antigüedad, Iñaki</creator><general>Blackwell Publishing Ltd</general><general>Wiley Subscription Services, Inc</general><scope>BSCLL</scope><scope>7QH</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>SOI</scope></search><sort><creationdate>20140228</creationdate><title>Variability of particulate (SS, POC) and dissolved (DOC, NO3) matter during storm events in the Alegria agricultural watershed</title><author>Cerro, Itsasne ; Sanchez-Perez, José Miguel ; Ruiz-Romera, Estilita ; Antigüedad, Iñaki</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2980-13f50f04cb41a06dfe6ff59fe064470d9bc8090746673ae64c2e1f8415e8acf93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>agricultural catchment</topic><topic>dissolved and particulate organic carbon</topic><topic>hysteresis</topic><topic>nitrates</topic><topic>storm-events</topic><topic>suspended sediment</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Cerro, Itsasne</creatorcontrib><creatorcontrib>Sanchez-Perez, José Miguel</creatorcontrib><creatorcontrib>Ruiz-Romera, Estilita</creatorcontrib><creatorcontrib>Antigüedad, Iñaki</creatorcontrib><collection>Istex</collection><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><jtitle>Hydrological processes</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Cerro, Itsasne</au><au>Sanchez-Perez, José Miguel</au><au>Ruiz-Romera, Estilita</au><au>Antigüedad, Iñaki</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Variability of particulate (SS, POC) and dissolved (DOC, NO3) matter during storm events in the Alegria agricultural watershed</atitle><jtitle>Hydrological processes</jtitle><addtitle>Hydrol. Process</addtitle><date>2014-02-28</date><risdate>2014</risdate><volume>28</volume><issue>5</issue><spage>2855</spage><epage>2867</epage><pages>2855-2867</pages><issn>0885-6087</issn><eissn>1099-1085</eissn><abstract>The temporal variability of suspended sediment, nitrates (NO3) and dissolved (DOC) and particulate organic carbon concentrations was analysed in the Alegria agricultural watershed over a 2‐year period. Nine storm events were studied, including an exhaustive analysis of hydrometeorological conditions, quantification of fluxes, and concentration‐discharge hysteresis loop characterization. The overall aim was to study the variability in these components during storm events and determine the mechanisms (flow paths) affecting the trajectories, from the source to the stream. The forms, rotational patterns and trends of hysteretic loops were investigated, and relationships between hysteresis features and hydrological parameters were studied. The results revealed clear differences between particulate (suspended sediment, particulate organic carbon) and dissolved (DOC, NO3) matter transport responses. Movement of the particulate matter was attributed to surface water, as reflected in clockwise hysteresis loops, whereas dissolved matter showed, in general, counterclockwise hysteresis loops, indicating a time delay in the arrival of solutes to the stream. This could be related to subsurface flow paths for DOC and a groundwater source for NO3. Copyright © 2013 John Wiley & Sons, Ltd.</abstract><cop>Chichester</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1002/hyp.9850</doi><tpages>13</tpages></addata></record> |
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subjects | agricultural catchment dissolved and particulate organic carbon hysteresis nitrates storm-events suspended sediment |
title | Variability of particulate (SS, POC) and dissolved (DOC, NO3) matter during storm events in the Alegria agricultural watershed |
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