Système d'information stratégique et agriculture (serveur d'exploration)

Attention, ce site est en cours de développement !
Attention, site généré par des moyens informatiques à partir de corpus bruts.
Les informations ne sont donc pas validées.

Groundwater Recharge at Five Representative Sites in the Hebei Plain, China

Identifieur interne : 000577 ( Main/Merge ); précédent : 000576; suivant : 000578

Groundwater Recharge at Five Representative Sites in the Hebei Plain, China

Auteurs : Xiaohui Lu [République populaire de Chine] ; Menggui Jin [République populaire de Chine] ; Martinus Th. Van Genuchten [Brésil] ; Bingguo Wang [République populaire de Chine]

Source :

RBID : ISTEX:8348BBA5E6BEEC232427941FBD9EDCC33CB2BB37

Abstract

Accurate estimates of groundwater recharge are essential for effective management of groundwater, especially when supplies are limited such as in many arid and semiarid areas. In the Hebei Plain, China, water shortage is increasingly restricting socioeconomic development, especially for agriculture, which heavily relies on groundwater. Human activities have greatly changed groundwater recharge there during the past several decades. To obtain better estimates of recharge in the plain, five representative sites were selected to investigate the effects of irrigation and water table depth on groundwater recharge. At each site, a one‐dimensional unsaturated flow model (Hydrus‐1D) was calibrated using field data of climate, soil moisture, and groundwater levels. A sensitivity analysis of evapotranspirative fluxes and various soil hydraulic parameters confirmed that fine‐textured surface soils generally generate less recharge. Model calculations showed that recharge on average is about 175 mm/year in the piedmont plain to the west, and 133 mm/year in both the central alluvial and lacustrine plains and the coastal plain to the east. Temporal and spatial variations in the recharge processes were significant in response to rainfall and irrigation. Peak time‐lags between infiltration (rainfall plus irrigation) and recharge were 18 to 35 days in the piedmont plain and 3 to 5 days in the central alluvial and lacustrine plains, but only 1 or 2 days in the coastal plain. This implies that different time‐lags corresponding to different water table depths must be considered when estimating or modeling groundwater recharge.

Url:
DOI: 10.1111/j.1745-6584.2009.00667.x

Links toward previous steps (curation, corpus...)


Links to Exploration step

ISTEX:8348BBA5E6BEEC232427941FBD9EDCC33CB2BB37

Le document en format XML

<record>
<TEI wicri:istexFullTextTei="biblStruct">
<teiHeader>
<fileDesc>
<titleStmt>
<title xml:lang="en">Groundwater Recharge at Five Representative Sites in the Hebei Plain, China</title>
<author>
<name sortKey="Lu, Xiaohui" sort="Lu, Xiaohui" uniqKey="Lu X" first="Xiaohui" last="Lu">Xiaohui Lu</name>
</author>
<author>
<name sortKey="Jin, Menggui" sort="Jin, Menggui" uniqKey="Jin M" first="Menggui" last="Jin">Menggui Jin</name>
</author>
<author>
<name sortKey="Van Genuchten, Martinus Th" sort="Van Genuchten, Martinus Th" uniqKey="Van Genuchten M" first="Martinus Th." last="Van Genuchten">Martinus Th. Van Genuchten</name>
</author>
<author>
<name sortKey="Wang, Bingguo" sort="Wang, Bingguo" uniqKey="Wang B" first="Bingguo" last="Wang">Bingguo Wang</name>
</author>
</titleStmt>
<publicationStmt>
<idno type="wicri:source">ISTEX</idno>
<idno type="RBID">ISTEX:8348BBA5E6BEEC232427941FBD9EDCC33CB2BB37</idno>
<date when="2011" year="2011">2011</date>
<idno type="doi">10.1111/j.1745-6584.2009.00667.x</idno>
<idno type="url">https://api.istex.fr/document/8348BBA5E6BEEC232427941FBD9EDCC33CB2BB37/fulltext/pdf</idno>
<idno type="wicri:Area/Istex/Corpus">000D01</idno>
<idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000D01</idno>
<idno type="wicri:Area/Istex/Curation">000C41</idno>
<idno type="wicri:Area/Istex/Checkpoint">000178</idno>
<idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Checkpoint">000178</idno>
<idno type="wicri:doubleKey">0017-467X:2011:Lu X:groundwater:recharge:at</idno>
<idno type="wicri:Area/Main/Merge">000577</idno>
</publicationStmt>
<sourceDesc>
<biblStruct>
<analytic>
<title level="a" type="main" xml:lang="en">Groundwater Recharge at Five Representative Sites in the Hebei Plain, China</title>
<author>
<name sortKey="Lu, Xiaohui" sort="Lu, Xiaohui" uniqKey="Lu X" first="Xiaohui" last="Lu">Xiaohui Lu</name>
<affiliation wicri:level="1">
<country xml:lang="fr">République populaire de Chine</country>
<wicri:regionArea>School of Earth Sciences and Engineering, Hohai University, Nanjing, Jiangshu, 210098</wicri:regionArea>
<wicri:noRegion>210098</wicri:noRegion>
</affiliation>
<affiliation wicri:level="1">
<country wicri:rule="url">République populaire de Chine</country>
</affiliation>
</author>
<author>
<name sortKey="Jin, Menggui" sort="Jin, Menggui" uniqKey="Jin M" first="Menggui" last="Jin">Menggui Jin</name>
<affiliation wicri:level="1">
<country wicri:rule="url">République populaire de Chine</country>
</affiliation>
</author>
<author>
<name sortKey="Van Genuchten, Martinus Th" sort="Van Genuchten, Martinus Th" uniqKey="Van Genuchten M" first="Martinus Th." last="Van Genuchten">Martinus Th. Van Genuchten</name>
<affiliation wicri:level="1">
<country xml:lang="fr">Brésil</country>
<wicri:regionArea>Department of Mechanical Engineering, LTTC/COPPE, Federal University of Rio de Janeiro, UFRJ, Rio de Janeiro, RJ 21945‐970</wicri:regionArea>
<wicri:noRegion>RJ 21945‐970</wicri:noRegion>
</affiliation>
</author>
<author>
<name sortKey="Wang, Bingguo" sort="Wang, Bingguo" uniqKey="Wang B" first="Bingguo" last="Wang">Bingguo Wang</name>
<affiliation wicri:level="1">
<country wicri:rule="url">République populaire de Chine</country>
</affiliation>
</author>
</analytic>
<monogr></monogr>
<series>
<title level="j">Groundwater</title>
<idno type="ISSN">0017-467X</idno>
<idno type="eISSN">1745-6584</idno>
<imprint>
<publisher>Blackwell Publishing Ltd</publisher>
<pubPlace>Oxford, UK</pubPlace>
<date type="published" when="2011-03">2011-03</date>
<biblScope unit="volume">49</biblScope>
<biblScope unit="issue">2</biblScope>
<biblScope unit="page" from="286">286</biblScope>
<biblScope unit="page" to="294">294</biblScope>
</imprint>
<idno type="ISSN">0017-467X</idno>
</series>
<idno type="istex">8348BBA5E6BEEC232427941FBD9EDCC33CB2BB37</idno>
<idno type="DOI">10.1111/j.1745-6584.2009.00667.x</idno>
<idno type="ArticleID">GWAT667</idno>
</biblStruct>
</sourceDesc>
<seriesStmt>
<idno type="ISSN">0017-467X</idno>
</seriesStmt>
</fileDesc>
<profileDesc>
<textClass></textClass>
<langUsage>
<language ident="en">en</language>
</langUsage>
</profileDesc>
</teiHeader>
<front>
<div type="abstract" xml:lang="en">Accurate estimates of groundwater recharge are essential for effective management of groundwater, especially when supplies are limited such as in many arid and semiarid areas. In the Hebei Plain, China, water shortage is increasingly restricting socioeconomic development, especially for agriculture, which heavily relies on groundwater. Human activities have greatly changed groundwater recharge there during the past several decades. To obtain better estimates of recharge in the plain, five representative sites were selected to investigate the effects of irrigation and water table depth on groundwater recharge. At each site, a one‐dimensional unsaturated flow model (Hydrus‐1D) was calibrated using field data of climate, soil moisture, and groundwater levels. A sensitivity analysis of evapotranspirative fluxes and various soil hydraulic parameters confirmed that fine‐textured surface soils generally generate less recharge. Model calculations showed that recharge on average is about 175 mm/year in the piedmont plain to the west, and 133 mm/year in both the central alluvial and lacustrine plains and the coastal plain to the east. Temporal and spatial variations in the recharge processes were significant in response to rainfall and irrigation. Peak time‐lags between infiltration (rainfall plus irrigation) and recharge were 18 to 35 days in the piedmont plain and 3 to 5 days in the central alluvial and lacustrine plains, but only 1 or 2 days in the coastal plain. This implies that different time‐lags corresponding to different water table depths must be considered when estimating or modeling groundwater recharge.</div>
</front>
</TEI>
</record>

Pour manipuler ce document sous Unix (Dilib)

EXPLOR_STEP=$WICRI_ROOT/Wicri/Agronomie/explor/SisAgriV1/Data/Main/Merge
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000577 | SxmlIndent | more

Ou

HfdSelect -h $EXPLOR_AREA/Data/Main/Merge/biblio.hfd -nk 000577 | SxmlIndent | more

Pour mettre un lien sur cette page dans le réseau Wicri

{{Explor lien
   |wiki=    Wicri/Agronomie
   |area=    SisAgriV1
   |flux=    Main
   |étape=   Merge
   |type=    RBID
   |clé=     ISTEX:8348BBA5E6BEEC232427941FBD9EDCC33CB2BB37
   |texte=   Groundwater Recharge at Five Representative Sites in the Hebei Plain, China
}}

Wicri

This area was generated with Dilib version V0.6.28.
Data generation: Wed Mar 29 00:06:34 2017. Site generation: Tue Mar 12 12:44:16 2024