Implication of groundwater fluctuation on the seasonal salt dynamic in the Harran Plain, south‐eastern Turkey
Identifieur interne : 000A51 ( Istex/Corpus ); précédent : 000A50; suivant : 000A52Implication of groundwater fluctuation on the seasonal salt dynamic in the Harran Plain, south‐eastern Turkey
Auteurs : M. A. Çullu ; S. Aydemi R ; M. Qadi R ; A. Almaca ; A. R. Öztürkmen ; A. Bi Lgi Ç ; N. A CaSource :
- Irrigation and Drainage [ 1531-0353 ] ; 2010-10.
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Abstract
Inefficient farm‐level water management aggravates groundwater fluctuation and salt accumulation particularly in arid and semi‐arid irrigated agriculture. Inappropriate water management practices in the Harran Plain are a good example. A study was carried out to investigate the effect of groundwater fluctuation on the seasonal salt dynamic in four widespread soil series in the Harran Plain with different natural drainage, south‐eastern Turkey. Four profiles were excavated and soil samples were collected seasonally up to 100 cm depth with 10 cm intervals. Similarly, irrigation and groundwater samples were collected from the fields where soil sampling was carried out. Significant seasonal variations in the salt dynamic were observed with the fluctuation levels of the groundwater. Total salt content at 1 m soil depth remained constant during the year, however salt fluctuation throughout the root zone in the growing season exceeded the threshold values of corn, wheat and cotton, commonly grown crops in the region, of 1.7, 6.0 and 7.7 dS m−1, respectively. However, soils with less water fluctuation showed lower salt accumulation in the root zone from May to October. Results also confirmed that soils can be non‐saline, but groundwater salinity, which may not be point specific, requires special attention. Copyright © 2009 John Wiley & Sons, Ltd.
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DOI: 10.1002/ird.507
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Aydemi R</name><affiliation><mods:affiliation>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey</mods:affiliation></affiliation></author><author><name sortKey="Qadi R, M" sort="Qadi R, M" uniqKey="Qadi R M" first="M." last="Qadi R">M. Qadi R</name><affiliation><mods:affiliation>International Centre for Agricultural Research in Dry Areas (ICARDA), Aleppo, Syrian Arab Republic</mods:affiliation></affiliation><affiliation><mods:affiliation>International Water Management Institute (IWMI), PO Box 2075, Colombo, Sri Lanka</mods:affiliation></affiliation></author><author><name sortKey="Almaca, A" sort="Almaca, A" uniqKey="Almaca A" first="A." last="Almaca">A. Almaca</name><affiliation><mods:affiliation>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey</mods:affiliation></affiliation></author><author><name sortKey="Ozturkmen, A R" sort="Ozturkmen, A R" uniqKey="Ozturkmen A" first="A. R." last="Öztürkmen">A. R. 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Inappropriate water management practices in the Harran Plain are a good example. A study was carried out to investigate the effect of groundwater fluctuation on the seasonal salt dynamic in four widespread soil series in the Harran Plain with different natural drainage, south‐eastern Turkey. Four profiles were excavated and soil samples were collected seasonally up to 100 cm depth with 10 cm intervals. Similarly, irrigation and groundwater samples were collected from the fields where soil sampling was carried out. Significant seasonal variations in the salt dynamic were observed with the fluctuation levels of the groundwater. Total salt content at 1 m soil depth remained constant during the year, however salt fluctuation throughout the root zone in the growing season exceeded the threshold values of corn, wheat and cotton, commonly grown crops in the region, of 1.7, 6.0 and 7.7 dS m−1, respectively. However, soils with less water fluctuation showed lower salt accumulation in the root zone from May to October. Results also confirmed that soils can be non‐saline, but groundwater salinity, which may not be point specific, requires special attention. Copyright © 2009 John Wiley & Sons, Ltd.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>M. A. Çullu</name><affiliations><json:string>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey</json:string><json:string>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey.===</json:string></affiliations></json:item><json:item><name>S. Aydemi̇r</name><affiliations><json:string>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey</json:string></affiliations></json:item><json:item><name>M. 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Inappropriate water management practices in the Harran Plain are a good example. A study was carried out to investigate the effect of groundwater fluctuation on the seasonal salt dynamic in four widespread soil series in the Harran Plain with different natural drainage, south‐eastern Turkey. Four profiles were excavated and soil samples were collected seasonally up to 100 cm depth with 10 cm intervals. Similarly, irrigation and groundwater samples were collected from the fields where soil sampling was carried out. Significant seasonal variations in the salt dynamic were observed with the fluctuation levels of the groundwater. Total salt content at 1 m soil depth remained constant during the year, however salt fluctuation throughout the root zone in the growing season exceeded the threshold values of corn, wheat and cotton, commonly grown crops in the region, of 1.7, 6.0 and 7.7 dS m−1, respectively. However, soils with less water fluctuation showed lower salt accumulation in the root zone from May to October. Results also confirmed that soils can be non‐saline, but groundwater salinity, which may not be point specific, requires special attention. 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A.</forename><surname>Çullu</surname></persName><affiliation>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey</affiliation><affiliation>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey.===</affiliation></author><author xml:id="author-2"><persName><forename type="first">S.</forename><surname>Aydemi̇r</surname></persName><affiliation>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey</affiliation></author><author xml:id="author-3"><persName><forename type="first">M.</forename><surname>Qadi̇r</surname></persName><affiliation>International Centre for Agricultural Research in Dry Areas (ICARDA), Aleppo, Syrian Arab Republic</affiliation><affiliation>International Water Management Institute (IWMI), PO Box 2075, Colombo, Sri Lanka</affiliation></author><author xml:id="author-4"><persName><forename type="first">A.</forename><surname>Almaca</surname></persName><affiliation>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey</affiliation></author><author xml:id="author-5"><persName><forename type="first">A. R.</forename><surname>Öztürkmen</surname></persName><affiliation>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey</affiliation></author><author xml:id="author-6"><persName><forename type="first">A.</forename><surname>Bi̇lgi̇ç</surname></persName><affiliation>Harran University, Faculty of Agriculture, Department of Agricultural Economics, Şanlıurfa, Turkey</affiliation></author><author xml:id="author-7"><persName><forename type="first">N.</forename><surname>Ağca</surname></persName><affiliation>Mustafa Kemal University, Faculty of Agriculture, Department of Soil Science, Antakya, Turkey</affiliation></author></analytic><monogr><title level="j">Irrigation and Drainage</title><title level="j" type="abbrev">Irrig. and Drain.</title><idno type="pISSN">1531-0353</idno><idno type="eISSN">1531-0361</idno><idno type="DOI">10.1002/(ISSN)1531-0361</idno><imprint><publisher>John Wiley & Sons, Ltd.</publisher><pubPlace>Chichester, UK</pubPlace><date type="published" when="2010-10"></date><biblScope unit="volume">59</biblScope><biblScope unit="issue">4</biblScope><biblScope unit="page" from="465">465</biblScope><biblScope unit="page" to="476">476</biblScope></imprint></monogr><idno type="istex">1B3D210E67A3EC64108D557A5316C2AAE99F397B</idno><idno type="DOI">10.1002/ird.507</idno><idno type="ArticleID">IRD507</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>2010</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Inefficient farm‐level water management aggravates groundwater fluctuation and salt accumulation particularly in arid and semi‐arid irrigated agriculture. Inappropriate water management practices in the Harran Plain are a good example. A study was carried out to investigate the effect of groundwater fluctuation on the seasonal salt dynamic in four widespread soil series in the Harran Plain with different natural drainage, south‐eastern Turkey. Four profiles were excavated and soil samples were collected seasonally up to 100 cm depth with 10 cm intervals. Similarly, irrigation and groundwater samples were collected from the fields where soil sampling was carried out. Significant seasonal variations in the salt dynamic were observed with the fluctuation levels of the groundwater. Total salt content at 1 m soil depth remained constant during the year, however salt fluctuation throughout the root zone in the growing season exceeded the threshold values of corn, wheat and cotton, commonly grown crops in the region, of 1.7, 6.0 and 7.7 dS m−1, respectively. However, soils with less water fluctuation showed lower salt accumulation in the root zone from May to October. Results also confirmed that soils can be non‐saline, but groundwater salinity, which may not be point specific, requires special attention. Copyright © 2009 John Wiley & Sons, Ltd.</p></abstract><abstract xml:lang="fr"><p>Une gestion de l'eau inefficace en agriculture irriguée aggrave les fluctuations de nappe et l'accumulation de sel dans les zones arides et semi‐arides. Les pratiques inappropriées de gestion des eaux dans la plaine de Harran sont un bon exemple. Une étude a été réalisée pour étudier l'effet de la fluctuation des eaux souterraines sur la dynamique saisonnière du sel dans quatre types de sols fréquents avec différents drainages naturels dans la plaine de Harran au sud‐est de la Turquie. Quatre profils ont été creusés et des échantillons de sol recueillies à chaque saison jusqu'à 100 cm de profondeur à intervalle de 10 cm. De même, des échantillons d'eau d'irrigation et d'eau souterraine ont été recueillis dans les champs où l'échantillonnage des sols a été réalisé. D'importantes variations saisonnières dans la dynamique de sel ont été observées avec la fluctuation des niveaux des eaux souterraines. La teneur globale en sel dans le sol à 1 m de profondeur est restée constante au cours de l'année, toutefois la fluctuation du sel dans la zone racinaire pendant la période de végétation a dépassé les seuils pour le maïs, le blé et le coton, les valeurs admises dans la région étant de 1.7, 6.0 et 7.7 dS m−1 respectivement. Toutefois, les sols avec moins de fluctuations d'eau ont montré moins d'accumulation de sel dans la zone racinaire de mai à octobre. Les résultats ont également confirmé que les sols peuvent être non‐salés, mais que la salinité des eaux souterraines non localisée nécessite une attention particulière. Copyright © 2009 John Wiley & Sons, Ltd.</p></abstract><textClass xml:lang="en"><keywords scheme="keyword"><list><head>keywords</head><item><term>salt movement</term></item><item><term>irrigated soils</term></item><item><term>salinity monitoring</term></item><item><term>salinization</term></item><item><term>groundwater fluctuation</term></item></list></keywords></textClass><textClass xml:lang="fr"><keywords scheme="keyword"><list><head>keywords</head><item><term>mouvement de sel</term></item><item><term>sols irrigués</term></item><item><term>suivi de la salinité salinisation</term></item><item><term>fluctuation des eaux souterraines</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>article-category</head><item><term>Research Article</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2008-06-08">Received</change><change when="2009-01-16">Registration</change><change when="2010-10">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/1B3D210E67A3EC64108D557A5316C2AAE99F397B/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley, elements deleted: body"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration><istex:document><component version="2.0" type="serialArticle" xml:lang="en"><header><publicationMeta level="product"><publisherInfo><publisherName>John Wiley & Sons, Ltd.</publisherName><publisherLoc>Chichester, UK</publisherLoc></publisherInfo><doi registered="yes">10.1002/(ISSN)1531-0361</doi><issn type="print">1531-0353</issn><issn type="electronic">1531-0361</issn><idGroup><id type="product" value="IRD"></id></idGroup><titleGroup><title type="main" xml:lang="en" sort="IRRIGATION AND DRAINAGE">Irrigation and Drainage</title><title type="short">Irrig. and Drain.</title></titleGroup></publicationMeta><publicationMeta level="part" position="40"><doi origin="wiley" registered="yes">10.1002/ird.v59:4</doi><numberingGroup><numbering type="journalVolume" number="59">59</numbering><numbering type="journalIssue">4</numbering></numberingGroup><coverDate startDate="2010-10">October 2010</coverDate></publicationMeta><publicationMeta level="unit" type="article" position="90" status="forIssue"><doi origin="wiley" registered="yes">10.1002/ird.507</doi><idGroup><id type="unit" value="IRD507"></id></idGroup><countGroup><count type="pageTotal" number="12"></count></countGroup><titleGroup><title type="articleCategory">Research Article</title><title type="tocHeading1">Research Articles</title></titleGroup><copyright ownership="publisher">Copyright © 2009 John Wiley & Sons, Ltd.</copyright><eventGroup><event type="manuscriptReceived" date="2008-06-08"></event><event type="manuscriptRevised" date="2009-01-16"></event><event type="manuscriptAccepted" date="2009-01-16"></event><event type="publishedOnlineEarlyUnpaginated" date="2010-08-19"></event><event type="firstOnline" date="2009-06-01"></event><event type="publishedOnlineFinalForm" date="2009-06-01"></event><event type="xmlConverted" agent="Converter:JWSART34_TO_WML3G version:2.3.20 mode:FullText mathml2tex" date="2010-09-21"></event><event type="xmlConverted" agent="Converter:WILEY_ML3G_TO_WILEY_ML3GV2 version:4.0.1" date="2014-03-13"></event><event type="xmlConverted" agent="Converter:WML3G_To_WML3G version:4.1.7 mode:FullText,remove_FC" date="2014-10-24"></event></eventGroup><numberingGroup><numbering type="pageFirst">465</numbering><numbering type="pageLast">476</numbering></numberingGroup><correspondenceTo>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey.===</correspondenceTo><linkGroup><link type="toTypesetVersion" href="file:IRD.IRD507.pdf"></link></linkGroup></publicationMeta><contentMeta><countGroup><count type="figureTotal" number="4"></count><count type="tableTotal" number="5"></count><count type="referenceTotal" number="27"></count></countGroup><titleGroup><title type="main" xml:lang="en">Implication of groundwater fluctuation on the seasonal salt dynamic in the Harran Plain, south‐eastern Turkey<link href="#fn1"></link></title><title type="short" xml:lang="en">GROUNDWATER FLUCTUATION AND SEASONAL SALT DYNAMIC, TURKEY</title></titleGroup><creators><creator xml:id="au1" creatorRole="author" affiliationRef="#af1" corresponding="yes"><personName><givenNames>M. A.</givenNames><familyName>Çullu</familyName></personName><contactDetails><email>macullu@harran.edu.tr</email></contactDetails></creator><creator xml:id="au2" creatorRole="author" affiliationRef="#af1"><personName><givenNames>S.</givenNames><familyName>Aydemi̇r</familyName></personName></creator><creator xml:id="au3" creatorRole="author" affiliationRef="#af2 #af3"><personName><givenNames>M.</givenNames><familyName>Qadi̇r</familyName></personName></creator><creator xml:id="au4" creatorRole="author" affiliationRef="#af1"><personName><givenNames>A.</givenNames><familyName>Almaca</familyName></personName></creator><creator xml:id="au5" creatorRole="author" affiliationRef="#af1"><personName><givenNames>A. R.</givenNames><familyName>Öztürkmen</familyName></personName></creator><creator xml:id="au6" creatorRole="author" affiliationRef="#af4"><personName><givenNames>A.</givenNames><familyName>Bi̇lgi̇ç</familyName></personName></creator><creator xml:id="au7" creatorRole="author" affiliationRef="#af5"><personName><givenNames>N.</givenNames><familyName>Ağca</familyName></personName></creator></creators><affiliationGroup><affiliation xml:id="af1" countryCode="TR" type="organization"><unparsedAffiliation>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey</unparsedAffiliation></affiliation><affiliation xml:id="af2" countryCode="SY" type="organization"><unparsedAffiliation>International Centre for Agricultural Research in Dry Areas (ICARDA), Aleppo, Syrian Arab Republic</unparsedAffiliation></affiliation><affiliation xml:id="af3" countryCode="LK" type="organization"><unparsedAffiliation>International Water Management Institute (IWMI), PO Box 2075, Colombo, Sri Lanka</unparsedAffiliation></affiliation><affiliation xml:id="af4" countryCode="TR" type="organization"><unparsedAffiliation>Harran University, Faculty of Agriculture, Department of Agricultural Economics, Şanlıurfa, Turkey</unparsedAffiliation></affiliation><affiliation xml:id="af5" countryCode="TR" type="organization"><unparsedAffiliation>Mustafa Kemal University, Faculty of Agriculture, Department of Soil Science, Antakya, Turkey</unparsedAffiliation></affiliation></affiliationGroup><keywordGroup xml:lang="en" type="author"><keyword xml:id="kwd1">salt movement</keyword><keyword xml:id="kwd2">irrigated soils</keyword><keyword xml:id="kwd3">salinity monitoring</keyword><keyword xml:id="kwd4">salinization</keyword><keyword xml:id="kwd5">groundwater fluctuation</keyword></keywordGroup><keywordGroup xml:lang="fr" type="author"><keyword xml:id="kwd6">mouvement de sel</keyword><keyword xml:id="kwd7">sols irrigués</keyword><keyword xml:id="kwd8">suivi de la salinité salinisation</keyword><keyword xml:id="kwd9">fluctuation des eaux souterraines</keyword></keywordGroup><fundingInfo><fundingAgency>Scientific and Technical Research Council of Turkey, TUBITAK</fundingAgency><fundingNumber>TOGTAG‐2510</fundingNumber></fundingInfo><abstractGroup><abstract type="main" xml:lang="en"><title type="main">Abstract</title><p>Inefficient farm‐level water management aggravates groundwater fluctuation and salt accumulation particularly in arid and semi‐arid irrigated agriculture. Inappropriate water management practices in the Harran Plain are a good example. A study was carried out to investigate the effect of groundwater fluctuation on the seasonal salt dynamic in four widespread soil series in the Harran Plain with different natural drainage, south‐eastern Turkey. Four profiles were excavated and soil samples were collected seasonally up to 100 cm depth with 10 cm intervals. Similarly, irrigation and groundwater samples were collected from the fields where soil sampling was carried out. Significant seasonal variations in the salt dynamic were observed with the fluctuation levels of the groundwater. Total salt content at 1 m soil depth remained constant during the year, however salt fluctuation throughout the root zone in the growing season exceeded the threshold values of corn, wheat and cotton, commonly grown crops in the region, of 1.7, 6.0 and 7.7 dS m<sup>−1</sup>, respectively. However, soils with less water fluctuation showed lower salt accumulation in the root zone from May to October. Results also confirmed that soils can be non‐saline, but groundwater salinity, which may not be point specific, requires special attention. Copyright © 2009 John Wiley & Sons, Ltd.</p></abstract><abstract type="main" xml:lang="fr"><p>Une gestion de l'eau inefficace en agriculture irriguée aggrave les fluctuations de nappe et l'accumulation de sel dans les zones arides et semi‐arides. Les pratiques inappropriées de gestion des eaux dans la plaine de Harran sont un bon exemple. Une étude a été réalisée pour étudier l'effet de la fluctuation des eaux souterraines sur la dynamique saisonnière du sel dans quatre types de sols fréquents avec différents drainages naturels dans la plaine de Harran au sud‐est de la Turquie. Quatre profils ont été creusés et des échantillons de sol recueillies à chaque saison jusqu'à 100 cm de profondeur à intervalle de 10 cm. De même, des échantillons d'eau d'irrigation et d'eau souterraine ont été recueillis dans les champs où l'échantillonnage des sols a été réalisé. D'importantes variations saisonnières dans la dynamique de sel ont été observées avec la fluctuation des niveaux des eaux souterraines. La teneur globale en sel dans le sol à 1 m de profondeur est restée constante au cours de l'année, toutefois la fluctuation du sel dans la zone racinaire pendant la période de végétation a dépassé les seuils pour le maïs, le blé et le coton, les valeurs admises dans la région étant de 1.7, 6.0 et 7.7 dS m<sup>−1</sup> respectivement. Toutefois, les sols avec moins de fluctuations d'eau ont montré moins d'accumulation de sel dans la zone racinaire de mai à octobre. Les résultats ont également confirmé que les sols peuvent être non‐salés, mais que la salinité des eaux souterraines non localisée nécessite une attention particulière. Copyright © 2009 John Wiley & Sons, Ltd.</p></abstract></abstractGroup></contentMeta><noteGroup><note xml:id="fn1"><p>Effet des fluctuations des eaux souterraines sur la dynamique saisonnière du sel dans la plaine Harran, sud‐est de la Turquie.</p></note></noteGroup></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Implication of groundwater fluctuation on the seasonal salt dynamic in the Harran Plain, south‐eastern Turkey</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>GROUNDWATER FLUCTUATION AND SEASONAL SALT DYNAMIC, TURKEY</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Implication of groundwater fluctuation on the seasonal salt dynamic in the Harran Plain, south‐eastern Turkey</title></titleInfo><name type="personal"><namePart type="given">M. A.</namePart><namePart type="family">Çullu</namePart><affiliation>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey</affiliation><affiliation>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey.===</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">S.</namePart><namePart type="family">Aydemi̇r</namePart><affiliation>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">M.</namePart><namePart type="family">Qadi̇r</namePart><affiliation>International Centre for Agricultural Research in Dry Areas (ICARDA), Aleppo, Syrian Arab Republic</affiliation><affiliation>International Water Management Institute (IWMI), PO Box 2075, Colombo, Sri Lanka</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">A.</namePart><namePart type="family">Almaca</namePart><affiliation>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">A. R.</namePart><namePart type="family">Öztürkmen</namePart><affiliation>Harran University, Faculty of Agriculture, Department of Soil Science, Şanlıurfa, Turkey</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">A.</namePart><namePart type="family">Bi̇lgi̇ç</namePart><affiliation>Harran University, Faculty of Agriculture, Department of Agricultural Economics, Şanlıurfa, Turkey</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">N.</namePart><namePart type="family">Ağca</namePart><affiliation>Mustafa Kemal University, Faculty of Agriculture, Department of Soil Science, Antakya, Turkey</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>John Wiley & Sons, Ltd.</publisher><place><placeTerm type="text">Chichester, UK</placeTerm></place><dateIssued encoding="w3cdtf">2010-10</dateIssued><dateCaptured encoding="w3cdtf">2008-06-08</dateCaptured><dateValid encoding="w3cdtf">2009-01-16</dateValid><copyrightDate encoding="w3cdtf">2010</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="figures">4</extent><extent unit="tables">5</extent><extent unit="references">27</extent></physicalDescription><abstract lang="en">Inefficient farm‐level water management aggravates groundwater fluctuation and salt accumulation particularly in arid and semi‐arid irrigated agriculture. Inappropriate water management practices in the Harran Plain are a good example. A study was carried out to investigate the effect of groundwater fluctuation on the seasonal salt dynamic in four widespread soil series in the Harran Plain with different natural drainage, south‐eastern Turkey. Four profiles were excavated and soil samples were collected seasonally up to 100 cm depth with 10 cm intervals. Similarly, irrigation and groundwater samples were collected from the fields where soil sampling was carried out. Significant seasonal variations in the salt dynamic were observed with the fluctuation levels of the groundwater. Total salt content at 1 m soil depth remained constant during the year, however salt fluctuation throughout the root zone in the growing season exceeded the threshold values of corn, wheat and cotton, commonly grown crops in the region, of 1.7, 6.0 and 7.7 dS m−1, respectively. However, soils with less water fluctuation showed lower salt accumulation in the root zone from May to October. Results also confirmed that soils can be non‐saline, but groundwater salinity, which may not be point specific, requires special attention. Copyright © 2009 John Wiley & Sons, Ltd.</abstract><abstract lang="fr">Une gestion de l'eau inefficace en agriculture irriguée aggrave les fluctuations de nappe et l'accumulation de sel dans les zones arides et semi‐arides. Les pratiques inappropriées de gestion des eaux dans la plaine de Harran sont un bon exemple. Une étude a été réalisée pour étudier l'effet de la fluctuation des eaux souterraines sur la dynamique saisonnière du sel dans quatre types de sols fréquents avec différents drainages naturels dans la plaine de Harran au sud‐est de la Turquie. Quatre profils ont été creusés et des échantillons de sol recueillies à chaque saison jusqu'à 100 cm de profondeur à intervalle de 10 cm. De même, des échantillons d'eau d'irrigation et d'eau souterraine ont été recueillis dans les champs où l'échantillonnage des sols a été réalisé. D'importantes variations saisonnières dans la dynamique de sel ont été observées avec la fluctuation des niveaux des eaux souterraines. La teneur globale en sel dans le sol à 1 m de profondeur est restée constante au cours de l'année, toutefois la fluctuation du sel dans la zone racinaire pendant la période de végétation a dépassé les seuils pour le maïs, le blé et le coton, les valeurs admises dans la région étant de 1.7, 6.0 et 7.7 dS m−1 respectivement. Toutefois, les sols avec moins de fluctuations d'eau ont montré moins d'accumulation de sel dans la zone racinaire de mai à octobre. Les résultats ont également confirmé que les sols peuvent être non‐salés, mais que la salinité des eaux souterraines non localisée nécessite une attention particulière. Copyright © 2009 John Wiley & Sons, Ltd.</abstract><note type="content">*Effet des fluctuations des eaux souterraines sur la dynamique saisonnière du sel dans la plaine Harran, sud‐est de la Turquie.</note><note type="funding">Scientific and Technical Research Council of Turkey, TUBITAK - No. TOGTAG‐2510; </note><subject lang="en"><genre>keywords</genre><topic>salt movement</topic><topic>irrigated soils</topic><topic>salinity monitoring</topic><topic>salinization</topic><topic>groundwater fluctuation</topic></subject><subject lang="fr"><genre>keywords</genre><topic>mouvement de sel</topic><topic>sols irrigués</topic><topic>suivi de la salinité salinisation</topic><topic>fluctuation des eaux souterraines</topic></subject><relatedItem type="host"><titleInfo><title>Irrigation and Drainage</title></titleInfo><titleInfo type="abbreviated"><title>Irrig. and Drain.</title></titleInfo><genre type="journal">journal</genre><subject><genre>article-category</genre><topic>Research Article</topic></subject><identifier type="ISSN">1531-0353</identifier><identifier type="eISSN">1531-0361</identifier><identifier type="DOI">10.1002/(ISSN)1531-0361</identifier><identifier type="PublisherID">IRD</identifier><part><date>2010</date><detail type="volume"><caption>vol.</caption><number>59</number></detail><detail type="issue"><caption>no.</caption><number>4</number></detail><extent unit="pages"><start>465</start><end>476</end><total>12</total></extent></part></relatedItem><identifier type="istex">1B3D210E67A3EC64108D557A5316C2AAE99F397B</identifier><identifier type="DOI">10.1002/ird.507</identifier><identifier type="ArticleID">IRD507</identifier><accessCondition type="use and reproduction" contentType="copyright">Copyright © 2009 John Wiley & Sons, Ltd.</accessCondition><recordInfo><recordContentSource>WILEY</recordContentSource><recordOrigin>John Wiley & Sons, Ltd.</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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