Temporal dynamics of soil water balance components in a karst range in southeastern Spain: estimation of potential recharge

This paper analyses the temporal dynamics of soil water balance components in a representative recharge area of the Sierra de Gádor (Almeria, southeastern Spain) in two hydrological years. Two approaches are used to estimate daily potential recharge (PR): Approach 1 based on deriving PR from the wat...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Hydrological sciences journal 2010-01, Vol.55 (5), p.737-753
Hauptverfasser: Cantón, Yolanda, Villagarcía, Luis, José Moro, María, Serrano-Ortíz, Penelope, Were, Ana, Javier Alcalá, Francisco, Kowalski, Andrew S., Solé-Benet, Alberto, Lázaro, Roberto, Domingo, Francisco
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 753
container_issue 5
container_start_page 737
container_title Hydrological sciences journal
container_volume 55
creator Cantón, Yolanda
Villagarcía, Luis
José Moro, María
Serrano-Ortíz, Penelope
Were, Ana
Javier Alcalá, Francisco
Kowalski, Andrew S.
Solé-Benet, Alberto
Lázaro, Roberto
Domingo, Francisco
description This paper analyses the temporal dynamics of soil water balance components in a representative recharge area of the Sierra de Gádor (Almeria, southeastern Spain) in two hydrological years. Two approaches are used to estimate daily potential recharge (PR): Approach 1 based on deriving PR from the water balance as the difference between measurements of rainfall (P) and actual evapotranspiration (E) obtained by eddy covariance; and Approach 2 with PR obtained from the dynamic pattern of the soil moisture (θ) recorded at two depths in the site's thin soil (average 0.35 m thickess). For the hydrological year 2003/04, which was slightly drier than the 30-year average, E accounted for 64% of rainfall and occurred mainly in late spring and early summer. The PR estimated by Approach 1 was 181 ± 18 mm year -1 (36% of rainfall), suggesting an effective groundwater recharge in the study area. In the unusually dry hydrological year 2004/05, E was about 215 mm year -1 , close to the annual rainfall input, and allowing very little (8 ± 12 mm year -1 ) PR according to Approach 1. Estimation of PR based on Approach 2 resulted in PR rates lower than those found by Approach 1, because Approach 2 does not take into account the recharge that occurs through preferential flow pathways (cracks, joints and fissures) which were not monitored with the θ probes. Moreover, using Approach 2, the PR estimates differed widely depending on the time scale considered: with daily mean θ data, PR estimation was lower, especially in late spring, while θ data at 30 min resolution yielded a more reliable prediction of the fraction of total PR resulting from the downward movement of soil water by gravity. Citation Cantón, Y., Villagarcía, L., Moro, M. J., Serrano-Ortíz, P., Were, A., Alcalá, F. J., Kowalski, A. S., Solé-Benet, A., Lázaro, R. & Domingo, F. (2010) Temporal dynamics of soil water balance components in a karst range in southeastern Spain: estimation of potential recharge. Hydrol. Sci. J. 55(5), 737-753.
doi_str_mv 10.1080/02626667.2010.490530
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_crossref_primary_10_1080_02626667_2010_490530</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>754886008</sourcerecordid><originalsourceid>FETCH-LOGICAL-a368t-fdbef573fff33fdd0f70bbb8cedd116ccfbe8f085dc42ecd7959d5a42f03b5013</originalsourceid><addsrcrecordid>eNp9kMFu1DAQhi0EEkvhDTj4gjilncSxk-WCUFWgUiUOlLM1scetIbGD7VW14uVxtC1HTpZG3ze_52fsbQvnLYxwAZ3qlFLDeQd11O9BCnjGdl0roRG9kM_ZbkOajXnJXuX8E0D0eyV27M8tLWtMOHN7DLh4k3l0PEc_8wcslPiEMwZD3MTKBQolcx848l-YcuEJwx1tgxwP5Z4wVyXw7yv68IFTLn7B4mPYdq6xVNvXpETmHtMdvWYvHM6Z3jy-Z-zH56vby6_Nzbcv15efbhoUaiyNsxM5OQjnnBDOWnADTNM0GrK2bZUxbqLRwSit6TsydtjLvZXYdw7EJKEVZ-z9ae-a4u9D_ZVefDY018MoHrIeZD-OCmCsZH8iTYo5J3J6TfWEdNQt6K1q_VS13qrWp6qr9u4xALPB2dVWjM__3E6A7DupKvfxxPngYlrwIabZ6oLHOaYnSfw36S_H1ZXs</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>754886008</pqid></control><display><type>article</type><title>Temporal dynamics of soil water balance components in a karst range in southeastern Spain: estimation of potential recharge</title><source>Taylor &amp; Francis Journals Complete</source><source>Alma/SFX Local Collection</source><creator>Cantón, Yolanda ; Villagarcía, Luis ; José Moro, María ; Serrano-Ortíz, Penelope ; Were, Ana ; Javier Alcalá, Francisco ; Kowalski, Andrew S. ; Solé-Benet, Alberto ; Lázaro, Roberto ; Domingo, Francisco</creator><creatorcontrib>Cantón, Yolanda ; Villagarcía, Luis ; José Moro, María ; Serrano-Ortíz, Penelope ; Were, Ana ; Javier Alcalá, Francisco ; Kowalski, Andrew S. ; Solé-Benet, Alberto ; Lázaro, Roberto ; Domingo, Francisco</creatorcontrib><description>This paper analyses the temporal dynamics of soil water balance components in a representative recharge area of the Sierra de Gádor (Almeria, southeastern Spain) in two hydrological years. Two approaches are used to estimate daily potential recharge (PR): Approach 1 based on deriving PR from the water balance as the difference between measurements of rainfall (P) and actual evapotranspiration (E) obtained by eddy covariance; and Approach 2 with PR obtained from the dynamic pattern of the soil moisture (θ) recorded at two depths in the site's thin soil (average 0.35 m thickess). For the hydrological year 2003/04, which was slightly drier than the 30-year average, E accounted for 64% of rainfall and occurred mainly in late spring and early summer. The PR estimated by Approach 1 was 181 ± 18 mm year -1 (36% of rainfall), suggesting an effective groundwater recharge in the study area. In the unusually dry hydrological year 2004/05, E was about 215 mm year -1 , close to the annual rainfall input, and allowing very little (8 ± 12 mm year -1 ) PR according to Approach 1. Estimation of PR based on Approach 2 resulted in PR rates lower than those found by Approach 1, because Approach 2 does not take into account the recharge that occurs through preferential flow pathways (cracks, joints and fissures) which were not monitored with the θ probes. Moreover, using Approach 2, the PR estimates differed widely depending on the time scale considered: with daily mean θ data, PR estimation was lower, especially in late spring, while θ data at 30 min resolution yielded a more reliable prediction of the fraction of total PR resulting from the downward movement of soil water by gravity. Citation Cantón, Y., Villagarcía, L., Moro, M. J., Serrano-Ortíz, P., Were, A., Alcalá, F. J., Kowalski, A. S., Solé-Benet, A., Lázaro, R. &amp; Domingo, F. (2010) Temporal dynamics of soil water balance components in a karst range in southeastern Spain: estimation of potential recharge. Hydrol. Sci. J. 55(5), 737-753.</description><identifier>ISSN: 0262-6667</identifier><identifier>EISSN: 2150-3435</identifier><identifier>DOI: 10.1080/02626667.2010.490530</identifier><identifier>CODEN: HSJODN</identifier><language>eng</language><publisher>Wallingford: Taylor &amp; Francis</publisher><subject>bilan hydrique du sol ; Earth sciences ; Earth, ocean, space ; evapotranspiration ; Exact sciences and technology ; humidité du sol ; Hydrology. Hydrogeology ; Marine ; Mediterranean ; Méditerranée ; potential recharge ; recharge potentielle ; Sierra de Gádor ; soil moisture ; soil water balance ; évapotranspiration</subject><ispartof>Hydrological sciences journal, 2010-01, Vol.55 (5), p.737-753</ispartof><rights>Copyright 2010 IAHS Press 2010</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a368t-fdbef573fff33fdd0f70bbb8cedd116ccfbe8f085dc42ecd7959d5a42f03b5013</citedby><cites>FETCH-LOGICAL-a368t-fdbef573fff33fdd0f70bbb8cedd116ccfbe8f085dc42ecd7959d5a42f03b5013</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.tandfonline.com/doi/pdf/10.1080/02626667.2010.490530$$EPDF$$P50$$Ginformaworld$$H</linktopdf><linktohtml>$$Uhttps://www.tandfonline.com/doi/full/10.1080/02626667.2010.490530$$EHTML$$P50$$Ginformaworld$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,59647,60436</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=23054256$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Cantón, Yolanda</creatorcontrib><creatorcontrib>Villagarcía, Luis</creatorcontrib><creatorcontrib>José Moro, María</creatorcontrib><creatorcontrib>Serrano-Ortíz, Penelope</creatorcontrib><creatorcontrib>Were, Ana</creatorcontrib><creatorcontrib>Javier Alcalá, Francisco</creatorcontrib><creatorcontrib>Kowalski, Andrew S.</creatorcontrib><creatorcontrib>Solé-Benet, Alberto</creatorcontrib><creatorcontrib>Lázaro, Roberto</creatorcontrib><creatorcontrib>Domingo, Francisco</creatorcontrib><title>Temporal dynamics of soil water balance components in a karst range in southeastern Spain: estimation of potential recharge</title><title>Hydrological sciences journal</title><description>This paper analyses the temporal dynamics of soil water balance components in a representative recharge area of the Sierra de Gádor (Almeria, southeastern Spain) in two hydrological years. Two approaches are used to estimate daily potential recharge (PR): Approach 1 based on deriving PR from the water balance as the difference between measurements of rainfall (P) and actual evapotranspiration (E) obtained by eddy covariance; and Approach 2 with PR obtained from the dynamic pattern of the soil moisture (θ) recorded at two depths in the site's thin soil (average 0.35 m thickess). For the hydrological year 2003/04, which was slightly drier than the 30-year average, E accounted for 64% of rainfall and occurred mainly in late spring and early summer. The PR estimated by Approach 1 was 181 ± 18 mm year -1 (36% of rainfall), suggesting an effective groundwater recharge in the study area. In the unusually dry hydrological year 2004/05, E was about 215 mm year -1 , close to the annual rainfall input, and allowing very little (8 ± 12 mm year -1 ) PR according to Approach 1. Estimation of PR based on Approach 2 resulted in PR rates lower than those found by Approach 1, because Approach 2 does not take into account the recharge that occurs through preferential flow pathways (cracks, joints and fissures) which were not monitored with the θ probes. Moreover, using Approach 2, the PR estimates differed widely depending on the time scale considered: with daily mean θ data, PR estimation was lower, especially in late spring, while θ data at 30 min resolution yielded a more reliable prediction of the fraction of total PR resulting from the downward movement of soil water by gravity. Citation Cantón, Y., Villagarcía, L., Moro, M. J., Serrano-Ortíz, P., Were, A., Alcalá, F. J., Kowalski, A. S., Solé-Benet, A., Lázaro, R. &amp; Domingo, F. (2010) Temporal dynamics of soil water balance components in a karst range in southeastern Spain: estimation of potential recharge. Hydrol. Sci. J. 55(5), 737-753.</description><subject>bilan hydrique du sol</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>evapotranspiration</subject><subject>Exact sciences and technology</subject><subject>humidité du sol</subject><subject>Hydrology. Hydrogeology</subject><subject>Marine</subject><subject>Mediterranean</subject><subject>Méditerranée</subject><subject>potential recharge</subject><subject>recharge potentielle</subject><subject>Sierra de Gádor</subject><subject>soil moisture</subject><subject>soil water balance</subject><subject>évapotranspiration</subject><issn>0262-6667</issn><issn>2150-3435</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><recordid>eNp9kMFu1DAQhi0EEkvhDTj4gjilncSxk-WCUFWgUiUOlLM1scetIbGD7VW14uVxtC1HTpZG3ze_52fsbQvnLYxwAZ3qlFLDeQd11O9BCnjGdl0roRG9kM_ZbkOajXnJXuX8E0D0eyV27M8tLWtMOHN7DLh4k3l0PEc_8wcslPiEMwZD3MTKBQolcx848l-YcuEJwx1tgxwP5Z4wVyXw7yv68IFTLn7B4mPYdq6xVNvXpETmHtMdvWYvHM6Z3jy-Z-zH56vby6_Nzbcv15efbhoUaiyNsxM5OQjnnBDOWnADTNM0GrK2bZUxbqLRwSit6TsydtjLvZXYdw7EJKEVZ-z9ae-a4u9D_ZVefDY018MoHrIeZD-OCmCsZH8iTYo5J3J6TfWEdNQt6K1q_VS13qrWp6qr9u4xALPB2dVWjM__3E6A7DupKvfxxPngYlrwIabZ6oLHOaYnSfw36S_H1ZXs</recordid><startdate>20100101</startdate><enddate>20100101</enddate><creator>Cantón, Yolanda</creator><creator>Villagarcía, Luis</creator><creator>José Moro, María</creator><creator>Serrano-Ortíz, Penelope</creator><creator>Were, Ana</creator><creator>Javier Alcalá, Francisco</creator><creator>Kowalski, Andrew S.</creator><creator>Solé-Benet, Alberto</creator><creator>Lázaro, Roberto</creator><creator>Domingo, Francisco</creator><general>Taylor &amp; Francis</general><general>IAHS Press</general><scope>IQODW</scope><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>20100101</creationdate><title>Temporal dynamics of soil water balance components in a karst range in southeastern Spain: estimation of potential recharge</title><author>Cantón, Yolanda ; Villagarcía, Luis ; José Moro, María ; Serrano-Ortíz, Penelope ; Were, Ana ; Javier Alcalá, Francisco ; Kowalski, Andrew S. ; Solé-Benet, Alberto ; Lázaro, Roberto ; Domingo, Francisco</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a368t-fdbef573fff33fdd0f70bbb8cedd116ccfbe8f085dc42ecd7959d5a42f03b5013</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2010</creationdate><topic>bilan hydrique du sol</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>evapotranspiration</topic><topic>Exact sciences and technology</topic><topic>humidité du sol</topic><topic>Hydrology. Hydrogeology</topic><topic>Marine</topic><topic>Mediterranean</topic><topic>Méditerranée</topic><topic>potential recharge</topic><topic>recharge potentielle</topic><topic>Sierra de Gádor</topic><topic>soil moisture</topic><topic>soil water balance</topic><topic>évapotranspiration</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Cantón, Yolanda</creatorcontrib><creatorcontrib>Villagarcía, Luis</creatorcontrib><creatorcontrib>José Moro, María</creatorcontrib><creatorcontrib>Serrano-Ortíz, Penelope</creatorcontrib><creatorcontrib>Were, Ana</creatorcontrib><creatorcontrib>Javier Alcalá, Francisco</creatorcontrib><creatorcontrib>Kowalski, Andrew S.</creatorcontrib><creatorcontrib>Solé-Benet, Alberto</creatorcontrib><creatorcontrib>Lázaro, Roberto</creatorcontrib><creatorcontrib>Domingo, Francisco</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Meteorological &amp; 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 &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; 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>Cantón, Yolanda</au><au>Villagarcía, Luis</au><au>José Moro, María</au><au>Serrano-Ortíz, Penelope</au><au>Were, Ana</au><au>Javier Alcalá, Francisco</au><au>Kowalski, Andrew S.</au><au>Solé-Benet, Alberto</au><au>Lázaro, Roberto</au><au>Domingo, Francisco</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Temporal dynamics of soil water balance components in a karst range in southeastern Spain: estimation of potential recharge</atitle><jtitle>Hydrological sciences journal</jtitle><date>2010-01-01</date><risdate>2010</risdate><volume>55</volume><issue>5</issue><spage>737</spage><epage>753</epage><pages>737-753</pages><issn>0262-6667</issn><eissn>2150-3435</eissn><coden>HSJODN</coden><abstract>This paper analyses the temporal dynamics of soil water balance components in a representative recharge area of the Sierra de Gádor (Almeria, southeastern Spain) in two hydrological years. Two approaches are used to estimate daily potential recharge (PR): Approach 1 based on deriving PR from the water balance as the difference between measurements of rainfall (P) and actual evapotranspiration (E) obtained by eddy covariance; and Approach 2 with PR obtained from the dynamic pattern of the soil moisture (θ) recorded at two depths in the site's thin soil (average 0.35 m thickess). For the hydrological year 2003/04, which was slightly drier than the 30-year average, E accounted for 64% of rainfall and occurred mainly in late spring and early summer. The PR estimated by Approach 1 was 181 ± 18 mm year -1 (36% of rainfall), suggesting an effective groundwater recharge in the study area. In the unusually dry hydrological year 2004/05, E was about 215 mm year -1 , close to the annual rainfall input, and allowing very little (8 ± 12 mm year -1 ) PR according to Approach 1. Estimation of PR based on Approach 2 resulted in PR rates lower than those found by Approach 1, because Approach 2 does not take into account the recharge that occurs through preferential flow pathways (cracks, joints and fissures) which were not monitored with the θ probes. Moreover, using Approach 2, the PR estimates differed widely depending on the time scale considered: with daily mean θ data, PR estimation was lower, especially in late spring, while θ data at 30 min resolution yielded a more reliable prediction of the fraction of total PR resulting from the downward movement of soil water by gravity. Citation Cantón, Y., Villagarcía, L., Moro, M. J., Serrano-Ortíz, P., Were, A., Alcalá, F. J., Kowalski, A. S., Solé-Benet, A., Lázaro, R. &amp; Domingo, F. (2010) Temporal dynamics of soil water balance components in a karst range in southeastern Spain: estimation of potential recharge. Hydrol. Sci. J. 55(5), 737-753.</abstract><cop>Wallingford</cop><pub>Taylor &amp; Francis</pub><doi>10.1080/02626667.2010.490530</doi><tpages>17</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0262-6667
ispartof Hydrological sciences journal, 2010-01, Vol.55 (5), p.737-753
issn 0262-6667
2150-3435
language eng
recordid cdi_crossref_primary_10_1080_02626667_2010_490530
source Taylor & Francis Journals Complete; Alma/SFX Local Collection
subjects bilan hydrique du sol
Earth sciences
Earth, ocean, space
evapotranspiration
Exact sciences and technology
humidité du sol
Hydrology. Hydrogeology
Marine
Mediterranean
Méditerranée
potential recharge
recharge potentielle
Sierra de Gádor
soil moisture
soil water balance
évapotranspiration
title Temporal dynamics of soil water balance components in a karst range in southeastern Spain: estimation of potential recharge
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-07T13%3A34%3A18IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Temporal%20dynamics%20of%20soil%20water%20balance%20components%20in%20a%20karst%20range%20in%20southeastern%20Spain:%20estimation%20of%20potential%20recharge&rft.jtitle=Hydrological%20sciences%20journal&rft.au=Cant%C3%B3n,%20Yolanda&rft.date=2010-01-01&rft.volume=55&rft.issue=5&rft.spage=737&rft.epage=753&rft.pages=737-753&rft.issn=0262-6667&rft.eissn=2150-3435&rft.coden=HSJODN&rft_id=info:doi/10.1080/02626667.2010.490530&rft_dat=%3Cproquest_cross%3E754886008%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=754886008&rft_id=info:pmid/&rfr_iscdi=true