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1دورية أكاديمية
المؤلفون: Yin Zhang, Qingfeng Miao, Ruiping Li, Minghai Sun, Xinmin Yang, Wei Wang, Yongping Huang, Weiying Feng
المصدر: Land, Vol 13, Iss 6, p 773 (2024)
مصطلحات موضوعية: Hetao Irrigation District, autumn irrigation, dry drainage, water and salt movement, Agriculture
وصف الملف: electronic resource
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2دورية أكاديمية
المؤلفون: Changshu Wang, Jingwei Wu, Wenzhi Zeng, Yan Zhu, Jiesheng Huang
المصدر: Water; Volume 11; Issue 1; Pages: 111
مصطلحات موضوعية: dry drainage system, water and salt balance, groundwater, evaporation, salinity
جغرافية الموضوع: agris
وصف الملف: application/pdf
العلاقة: Water, Agriculture and Aquaculture; https://dx.doi.org/10.3390/w11010111Test
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3دورية أكاديمية
مصطلحات موضوعية:
БИОГЕОХИМИЧЕСКИЕ БАРЬЕРЫ,ПЕРЕХВАТ АЗОТА,ДОМИНАНТНЫЕ И СУБДОМИНАНТНЫЕ УРОЧИЩА,"СУХОЙ" ДРЕНАЖ,ГАЛОГЕОХИМИЧЕСКАЯ ЁМКОСТЬ ЛАНДШАФТА (СОЛЕЁМКОСТЬ),BIOCHEMICAL BARRIERS,NITROGEN INTERCEPTION,DOMINANT AND SUBDOMINANT HOLES,"DRY" DRAINAGE,HALO GEOCHEMICAL CAPACITY OF LANDSCAPE (SALTS CAPACITY) وصف الملف: text/html
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المصدر: Природообустройство.
مصطلحات موضوعية:
БИОГЕОХИМИЧЕСКИЕ БАРЬЕРЫ,ПЕРЕХВАТ АЗОТА,ДОМИНАНТНЫЕ И СУБДОМИНАНТНЫЕ УРОЧИЩА,"СУХОЙ" ДРЕНАЖ,ГАЛОГЕОХИМИЧЕСКАЯ ЁМКОСТЬ ЛАНДШАФТА (СОЛЕЁМКОСТЬ),BIOCHEMICAL BARRIERS,NITROGEN INTERCEPTION,DOMINANT AND SUBDOMINANT HOLES,"DRY" DRAINAGE,HALO GEOCHEMICAL CAPACITY OF LANDSCAPE (SALTS CAPACITY) وصف الملف: text/html
الوصول الحر: https://explore.openaire.eu/search/publication?articleId=od______2806::92b4090b615447d820ade454e936f992Test
http://cyberleninka.ru/article_covers/16969564.pngTest -
5دورية أكاديمية
المؤلفون: Wu, J.W., Zhao, L.R., Huang, J.S., Yang, J.Z., Vincent, Bernard, Bouarfa, S., Vidal, A.
المساهمون: WUHAN UNIVERSITY CHN, Partenaires IRSTEA, Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Hydrosystèmes et Bioprocédés (UR HBAN), Centre national du machinisme agricole, du génie rural, des eaux et forêts (CEMAGREF), Gestion de l'Eau, Acteurs, Usages (UMR G-EAU), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Centre international d'études supérieures en sciences agronomiques (Montpellier SupAgro)-AgroParisTech-Centre national du machinisme agricole, du génie rural, des eaux et forêts (CEMAGREF)-Institut de Recherche pour le Développement (IRD France-Sud )-Centre International de Hautes Etudes Agronomiques Méditerranéennes - Institut Agronomique Méditerranéen de Montpellier (CIHEAM-IAMM), Centre International de Hautes Études Agronomiques Méditerranéennes (CIHEAM)-Centre International de Hautes Études Agronomiques Méditerranéennes (CIHEAM), Territoires, Environnement, Télédétection et Information Spatiale (UMR TETIS), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-AgroParisTech-Centre national du machinisme agricole, du génie rural, des eaux et forêts (CEMAGREF)
المصدر: ISSN: 1006-9321 ; EISSN: 1862-281X.
مصطلحات موضوعية: DRY DRAINAGE, FIELD EXPERIMENT, [SDE]Environmental Sciences
العلاقة: hal-02594874; https://hal.inrae.fr/hal-02594874Test; IRSTEA: PUB00031517
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المؤلفون: Jingwei Wu, Li-rong Zhao, Sami Bouarfa, Jinzhong Yang, Jiesheng Huang, Bernard Vincent, Alain Vidal
المساهمون: WUHAN UNIVERSITY CHN, Partenaires IRSTEA, Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Hydrosystèmes et Bioprocédés (UR HBAN), Centre national du machinisme agricole, du génie rural, des eaux et forêts (CEMAGREF), Gestion de l'Eau, Acteurs, Usages (UMR G-EAU), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Centre international d'études supérieures en sciences agronomiques (Montpellier SupAgro)-AgroParisTech-Centre national du machinisme agricole, du génie rural, des eaux et forêts (CEMAGREF)-Institut de Recherche pour le Développement (IRD [France-Sud])-Centre International de Hautes Etudes Agronomiques Méditerranéennes - Institut Agronomique Méditerranéen de Montpellier (CIHEAM-IAMM), Centre International de Hautes Études Agronomiques Méditerranéennes (CIHEAM)-Centre International de Hautes Études Agronomiques Méditerranéennes (CIHEAM), Territoires, Environnement, Télédétection et Information Spatiale (UMR TETIS), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-AgroParisTech-Centre national du machinisme agricole, du génie rural, des eaux et forêts (CEMAGREF)
المصدر: Science in China Series E: Technological Sciences
Science in China Series E: Technological Sciences, Springer Verlag, 2009, 52 (11), pp.3328-3334. ⟨10.1007/s11431-009-0341-8⟩مصطلحات موضوعية: Hydrology, Soil salinity, 0207 environmental engineering, 04 agricultural and veterinary sciences, 02 engineering and technology, 15. Life on land, Watertable control, 6. Clean water, Leaching model, Hydrology (agriculture), Drainage research, [SDE]Environmental Sciences, 040103 agronomy & agriculture, 0401 agriculture, forestry, and fisheries, Environmental science, DRY DRAINAGE, Drainage, 020701 environmental engineering, Soil salinity control, FIELD EXPERIMENT, Well drainage
الوصول الحر: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::39aa331f5b6d93bdf76585f93578da39Test
https://hal.inrae.fr/hal-02594874Test -
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مصطلحات موضوعية: long-term population dynamics, demography, Sonoran Desert, annual plants, seed bank
جغرافية الموضوع: Arizona. Site type: The site (725 m elevation) is a gently sloped creosote flat dominated by Larrea divaricata (creosote bush), which has 50% cover. The site is located in the Arizona Upland subdivision of the Sonoran Desert. Geography: The study site is located at the northwest base of Tumamoc Hill 1 mile west of downtown Tucson,
AZ (32'13" N, 20% silt, including sandy-clay soil at the base of the hill (54% sand, 22% silt, 10°/o silt, 111.01 W -110.89899000000001 E 32.2 N 32.2 S الوقت: 1. Site description: Permanent quadrats were established in 1982 at the northwest base of Tumamoc Hill at the Desert Laboratory of the University of Arizona in Tucson, Arizona. Site type: The site (725 m elevation) is a gently sloped creosote flat dominated by Larrea divaricata (creosote bush), which has 50% cover. The site is located in the Arizona Upland subdivision of the Sonoran Desert. Geography: The study site is located at the northwest base of Tumamoc Hill 1 mile west of downtown Tucson, AZ (32'13" N, 111'01" W). Habitat: See "Site type" above. The quadrats extend along a transect from a flat alluvial area and up the southeast side of a gently sloping (9°) hill,. Geology: Plots are located along a gently sloping bajada (fluvial piedmont) of consistent parent material, where a strong transition occurs in the age of the soil surface with elevation. The soil on the slope is composed of basaltic andesite (Phillips 1976) with a coarse sandy-loam texture (67% sand, 20% silt, 13% clay) and with fragments ofbasaltic rocks embedded in the surface. The surrounding lower areas have recently derived alluvial soil, including sandy-clay soil at the base of the hill (54% sand, 22% silt, 24% clay) and loamy-sand soil in a series of shallow (<0.5 m deep) and narrow (2-3 m wide) dry drainage channels (79% sand, 10°/o silt, 10% clay). The slope is rockier (50% gravel) than the base of the hill (20% gravel) or rivulets (25% gravel) (Pantastico-Caldas and Venable 1993). Watersheds/hydrology: N/A Site history: The 850 acre Desert laboratory site was fences in 1906 to protect it from cattle grazing and it has been an ecological preserve subsequently. Climate: The site receives ~300 mm of annual precipitation on average, about half of which falls during the summer monsoons (July–September), with the rest occurring sporadically through the remainder of the year (Bowers and Turner 1985)., 1982 to 2007
العلاقة: http://metacat.lternet.edu/knb/metacat/nceas.51.11/xmlTest; nceas.51.11; http://hdl.handle.net/10255/dryad.29203Test
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مصطلحات موضوعية: long-term population dynamics, demography, Sonoran Desert, annual plants, seed bank
جغرافية الموضوع: Arizona. Site type: The site (725 m elevation) is a gently sloped creosote flat dominated by Larrea divaricata (creosote bush), which has 50% cover. The site is located in the Arizona Upland subdivision of the Sonoran Desert. Geography: The study site is located at the northwest base of Tumamoc Hill 1 mile west of downtown Tucson,
AZ (32'13" N, 20% silt, including sandy-clay soil at the base of the hill (54% sand, 22% silt, 10°/o silt, 111.01 W -110.89899000000001 E 32.2 N 32.2 S الوقت: 1. Site description: Permanent quadrats were established in 1982 at the northwest base of Tumamoc Hill at the Desert Laboratory of the University of Arizona in Tucson, Arizona. Site type: The site (725 m elevation) is a gently sloped creosote flat dominated by Larrea divaricata (creosote bush), which has 50% cover. The site is located in the Arizona Upland subdivision of the Sonoran Desert. Geography: The study site is located at the northwest base of Tumamoc Hill 1 mile west of downtown Tucson, AZ (32'13" N, 111'01" W). Habitat: See "Site type" above. The quadrats extend along a transect from a flat alluvial area and up the southeast side of a gently sloping (9°) hill,. Geology: Plots are located along a gently sloping bajada (fluvial piedmont) of consistent parent material, where a strong transition occurs in the age of the soil surface with elevation. The soil on the slope is composed of basaltic andesite (Phillips 1976) with a coarse sandy-loam texture (67% sand, 20% silt, 13% clay) and with fragments ofbasaltic rocks embedded in the surface. The surrounding lower areas have recently derived alluvial soil, including sandy-clay soil at the base of the hill (54% sand, 22% silt, 24% clay) and loamy-sand soil in a series of shallow (<0.5 m deep) and narrow (2-3 m wide) dry drainage channels (79% sand, 10°/o silt, 10% clay). The slope is rockier (50% gravel) than the base of the hill (20% gravel) or rivulets (25% gravel) (Pantastico-Caldas and Venable 1993). Watersheds/hydrology: N/A Site history: The 850 acre Desert laboratory site was fences in 1906 to protect it from cattle grazing and it has been an ecological preserve subsequently. Climate: The site receives ~300 mm of annual precipitation on average, about half of which falls during the summer monsoons (July–September), with the rest occurring sporadically through the remainder of the year (Bowers and Turner 1985)., 1982 to 2007
العلاقة: http://metacat.lternet.edu/knb/metacat/reeves.51.2/xmlTest; reeves.51.2; http://hdl.handle.net/10255/dryad.28659Test
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مصطلحات موضوعية: long-term population dynamics, demography, Sonoran Desert, annual plants, seed bank
جغرافية الموضوع: Arizona. Site type: The site (725 m elevation) is a gently sloped creosote flat dominated by Larrea divaricata (creosote bush), which has 50% cover. The site is located in the Arizona Upland subdivision of the Sonoran Desert. Geography: The study site is located at the northwest base of Tumamoc Hill 1 mile west of downtown Tucson,
AZ (32'13" N, 20% silt, including sandy-clay soil at the base of the hill (54% sand, 22% silt, 10�/o silt, 111.1 W -110.9889 E 32.2 N 32.2 S الوقت: 1. Site description: Permanent quadrats were established in 1982 at the northwest base of Tumamoc Hill at the Desert Laboratory of the University of Arizona in Tucson, Arizona. Site type: The site (725 m elevation) is a gently sloped creosote flat dominated by Larrea divaricata (creosote bush), which has 50% cover. The site is located in the Arizona Upland subdivision of the Sonoran Desert. Geography: The study site is located at the northwest base of Tumamoc Hill 1 mile west of downtown Tucson, AZ (32'13" N, 111'01" W). Habitat: See "Site type" above. The quadrats extend along a transect from a flat alluvial area and up the southeast side of a gently sloping (9�) hill,. Geology: Plots are located along a gently sloping bajada (fluvial piedmont) of consistent parent material, where a strong transition occurs in the age of the soil surface with elevation. The soil on the slope is composed of basaltic andesite (Phillips 1976) with a coarse sandy-loam texture (67% sand, 20% silt, 13% clay) and with fragments ofbasaltic rocks embedded in the surface. The surrounding lower areas have recently derived alluvial soil, including sandy-clay soil at the base of the hill (54% sand, 22% silt, 24% clay) and loamy-sand soil in a series of shallow (<0.5 m deep) and narrow (2-3 m wide) dry drainage channels (79% sand, 10�/o silt, 10% clay). The slope is rockier (50% gravel) than the base of the hill (20% gravel) or rivulets (25% gravel) (Pantastico-Caldas and Venable 1993). Watersheds/hydrology: N/A Site history: The 850 acre Desert laboratory site was fences in 1906 to protect it from cattle grazing and it has been an ecological preserve subsequently. Climate: The site receives ~300 mm of annual precipitation on average, about half of which falls during the summer monsoons (July?September), with the rest occurring sporadically through the remainder of the year (Bowers and Turner 1985)., 1982 to 2007
العلاقة: http://metacat.lternet.edu/knb/metacat/reeves.52.1/xmlTest; reeves.52.1; http://hdl.handle.net/10255/dryad.28657Test
النص الكامل 