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Registro Completo |
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Biblioteca(s): |
Embrapa Semiárido. |
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Data corrente: |
19/12/2022 |
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Data da última atualização: |
20/02/2024 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
ALVES, H. K. M. N.; SILVA. T. G. F. da; JARDIM, A. M. da R. F; SOUZA, L. S. B. de; ARAÚJO JÚNIOR, G. do N.; SOUZA, C. A. A. de; MOURA, M. S. B. de; ARAUJO, G. G. L. de; CAMPOS, F. S.; CRUZ NETO, J. F. da. |
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Afiliação: |
HYGOR KRISTOPH MUNIZ NUNES ALVES, UFRPE; THIERES GEORGE FREIRE DA SILVA, UFRPE - Serra Talhada, PE; ALEXANDRE MANIÇOBA DA ROSA FERRAZ JARDIM, UFRPE; LUCIANA SANDRA BASTOS DE SOUZA, UFRPE - Serra Talhada, PE; GEORGE DO NASCIMENTO ARAÚJO JÚNIOR, UFRPE; CARLOS ANDRÉ ALVES DE SOUZA, UFRPE; MAGNA SOELMA BESERRA DE MOURA, CPATSA; GHERMAN GARCIA LEAL DE ARAUJO, CPATSA; FLEMING SENA CAMPOS; JOSÉ FRANCISCO DA CRUZ NETO, UFRPE. |
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Título: |
The use of mulch in cultivating the forage cactus optimizesyield in less time and increases the water use efficiency ofthe crop. |
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Ano de publicação: |
2023 |
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Fonte/Imprenta: |
Irrigation and Drainage, v. 72, n. 1, p. 75-89. 2023. |
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DOI: |
https://doi.org/10.1002/ird.2758 |
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Idioma: |
Português |
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Conteúdo: |
Measurements of crop evapotranspiration (ETC) and crop coefficients (kC)incactus have not yet been adjusted for the phenological stage using conserva-tion practices (i.e. mulching). In this study, soil water dynamics, ETCandkCwere measured in the forage cactus under cultivation systems with (WM) andwithout (NM) the use of mulch in the semi-arid region of Brazil.Opuntiastrictawas subjected to irrigation depths based on a percentage of the referenceevapotranspiration (ET0) (rainfed, 25, 50, 75 and 100%) and to two systems ofcultivation: WM and NM. Over time, the phenophases (?Ph) were established;the soil water balance components were calculated and the crop yield wasevaluated at harvest. The use of 8.2 Mg ha1mulch led to almost no reducedwater consumption by the crop when compared to the NM system; however,the mulch did maximize yield, at 839C day, when irrigated with 50% ET0. ThekCvalue was higher under the WM system, with the differences decreasingthroughout the cycle (?PhI, 36%;?PhII, 27%;?PhIII, 23%;?PhIV-HT, 17%; and?PhIV-RF, 14%). Therefore, the use of mulch in cultivating the cactus opti-mized forage production in less time and significantly increased the water useefficiency of the crop |
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Palavras-Chave: |
Emissão de cladódio; Fenofase; Semiárido. |
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Thesagro: |
Cobertura Morta; Palma Forrageira; Solo. |
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Thesaurus Nal: |
Opuntia stricta. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/253182/1/The-use-of-mulch-in-cultivating-the-forage-cactus-optimizesyield-in-less-time-and-increases-the-water-use-efficiency-ofthe-crop.pdf
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Marc: |
LEADER 02228naa a2200325 a 4500
001 2149902
005 2024-02-20
008 2023 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1002/ird.2758$2DOI
100 1 $aALVES, H. K. M. N.
245 $aThe use of mulch in cultivating the forage cactus optimizesyield in less time and increases the water use efficiency ofthe crop.$h[electronic resource]
260 $c2023
520 $aMeasurements of crop evapotranspiration (ETC) and crop coefficients (kC)incactus have not yet been adjusted for the phenological stage using conserva-tion practices (i.e. mulching). In this study, soil water dynamics, ETCandkCwere measured in the forage cactus under cultivation systems with (WM) andwithout (NM) the use of mulch in the semi-arid region of Brazil.Opuntiastrictawas subjected to irrigation depths based on a percentage of the referenceevapotranspiration (ET0) (rainfed, 25, 50, 75 and 100%) and to two systems ofcultivation: WM and NM. Over time, the phenophases (?Ph) were established;the soil water balance components were calculated and the crop yield wasevaluated at harvest. The use of 8.2 Mg ha1mulch led to almost no reducedwater consumption by the crop when compared to the NM system; however,the mulch did maximize yield, at 839C day, when irrigated with 50% ET0. ThekCvalue was higher under the WM system, with the differences decreasingthroughout the cycle (?PhI, 36%;?PhII, 27%;?PhIII, 23%;?PhIV-HT, 17%; and?PhIV-RF, 14%). Therefore, the use of mulch in cultivating the cactus opti-mized forage production in less time and significantly increased the water useefficiency of the crop
650 $aOpuntia stricta
650 $aCobertura Morta
650 $aPalma Forrageira
650 $aSolo
653 $aEmissão de cladódio
653 $aFenofase
653 $aSemiárido
700 1 $aSILVA. T. G. F. da
700 1 $aJARDIM, A. M. da R. F
700 1 $aSOUZA, L. S. B. de
700 1 $aARAÚJO JÚNIOR, G. do N.
700 1 $aSOUZA, C. A. A. de
700 1 $aMOURA, M. S. B. de
700 1 $aARAUJO, G. G. L. de
700 1 $aCAMPOS, F. S.
700 1 $aCRUZ NETO, J. F. da
773 $tIrrigation and Drainage$gv. 72, n. 1, p. 75-89. 2023.
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Registro original: |
Embrapa Semiárido (CPATSA) |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Solos. Para informações adicionais entre em contato com cnps.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
15/08/2014 |
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Data da última atualização: |
10/11/2021 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 1 |
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Autoria: |
OLIVEIRA, F. S. de; SCHAEFER, C. E. G. R.; ABRAHÃO, W. A. P.; ALMEIDA, E. de P. C.; SIMAS, F. N. B. |
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Afiliação: |
Fábio Soares de Oliveira, Departamento de Geografia, Instituto de Geociências, Universidade Federal de Minas Gerais, UFMG.; Carlos Ernesto G.R. Schaefer, Departamento de Solos, Universidade Federal de Viçosa, UFV.; Walter Antônio Pereira Abrahão, Departamento de Solos, Universidade Federal de Viçosa, UFV.; ELIANE DE PAULA CLEMENTE ALMEIDA, CNPS; Felipe Nogueira Bello Simas, Departamento de Solos, Universidade Federal de Viçosa, UFV. |
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Título: |
Soil-geomorphology interactions and paleoclimatic implications of an ornithogenic soil toposequence on Rata Island, Fernando de Noronha Archipelago, South Atlantic. |
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Ano de publicação: |
2014 |
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Fonte/Imprenta: |
Journal of South American Earth Sciences, v. 52, p. 119-128, Jul. 2014. |
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DOI: |
https://doi.org/10.1016/j.jsames.2014.02.007 |
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Idioma: |
Inglês |
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Conteúdo: |
The formation of highly phosphatized soils on sites of avian activity is a common feature of oceanic islands. We characterized a toposequence of phosphatic soils on Rata Island, to evaluate the soil genesis based on local topographic variations. For this purpose, four soils ranging from the upper hill down to the lowest landscape position on the island, representing a range of parent materials (basalt and calcareous sands), were analyzed. In the lowest landscape position a shallow Regosol was identified, strongly influenced by birds and marine sprays, developed on 'karstified' Pleistocene calcarenites; the three other soils in the upper part of the toposequence are Ornithogenic Cambisols, ranging from a deep Cambisol profile on Basalt lava to intermediate Cambisols on mixed colluvial sediments of the basalt/ calcareous. The lowermost Regosol is associated with a rugged landscape with strong calcarenite dissolution and karstification. The soil phosphatization is clearly an inherited process of the Late Quaternary age, when climate conditions were different. Initial weathering took place in the last interglacial period, under wetter conditions during which the Tertiary basalts were strongly weathered, leaving corestones in a saprolitic, oxidized mass. In the late Pleistocene, a gentle surface distributed these weathering products along the pediment slopes as colluvial materials, whereas in the coastal areas aeolian processes formed large sand dunes composed of reworked calcareous sands from marine sources during a time of very low sea level. During this time, widespread bird activity accounted for secondary apatite formation on the surface of calcareous oolites. Finally, the Holocene warming was accompanied by increasing sea level, enhanced tropical weathering, Fe and Al mobility and variscite formation superimposed on degraded Ca-phosphates, forming two phase phosphatic aggregates. MenosThe formation of highly phosphatized soils on sites of avian activity is a common feature of oceanic islands. We characterized a toposequence of phosphatic soils on Rata Island, to evaluate the soil genesis based on local topographic variations. For this purpose, four soils ranging from the upper hill down to the lowest landscape position on the island, representing a range of parent materials (basalt and calcareous sands), were analyzed. In the lowest landscape position a shallow Regosol was identified, strongly influenced by birds and marine sprays, developed on 'karstified' Pleistocene calcarenites; the three other soils in the upper part of the toposequence are Ornithogenic Cambisols, ranging from a deep Cambisol profile on Basalt lava to intermediate Cambisols on mixed colluvial sediments of the basalt/ calcareous. The lowermost Regosol is associated with a rugged landscape with strong calcarenite dissolution and karstification. The soil phosphatization is clearly an inherited process of the Late Quaternary age, when climate conditions were different. Initial weathering took place in the last interglacial period, under wetter conditions during which the Tertiary basalts were strongly weathered, leaving corestones in a saprolitic, oxidized mass. In the late Pleistocene, a gentle surface distributed these weathering products along the pediment slopes as colluvial materials, whereas in the coastal areas aeolian processes formed large sand dunes composed of reworked calcare... Mostrar Tudo |
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Palavras-Chave: |
Paleogeograph; Phosphatization; Volcanic islands. |
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Thesaurus NAL: |
ornithogenic soils. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02738naa a2200229 a 4500
001 1992705
005 2021-11-10
008 2014 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1016/j.jsames.2014.02.007$2DOI
100 1 $aOLIVEIRA, F. S. de
245 $aSoil-geomorphology interactions and paleoclimatic implications of an ornithogenic soil toposequence on Rata Island, Fernando de Noronha Archipelago, South Atlantic.$h[electronic resource]
260 $c2014
520 $aThe formation of highly phosphatized soils on sites of avian activity is a common feature of oceanic islands. We characterized a toposequence of phosphatic soils on Rata Island, to evaluate the soil genesis based on local topographic variations. For this purpose, four soils ranging from the upper hill down to the lowest landscape position on the island, representing a range of parent materials (basalt and calcareous sands), were analyzed. In the lowest landscape position a shallow Regosol was identified, strongly influenced by birds and marine sprays, developed on 'karstified' Pleistocene calcarenites; the three other soils in the upper part of the toposequence are Ornithogenic Cambisols, ranging from a deep Cambisol profile on Basalt lava to intermediate Cambisols on mixed colluvial sediments of the basalt/ calcareous. The lowermost Regosol is associated with a rugged landscape with strong calcarenite dissolution and karstification. The soil phosphatization is clearly an inherited process of the Late Quaternary age, when climate conditions were different. Initial weathering took place in the last interglacial period, under wetter conditions during which the Tertiary basalts were strongly weathered, leaving corestones in a saprolitic, oxidized mass. In the late Pleistocene, a gentle surface distributed these weathering products along the pediment slopes as colluvial materials, whereas in the coastal areas aeolian processes formed large sand dunes composed of reworked calcareous sands from marine sources during a time of very low sea level. During this time, widespread bird activity accounted for secondary apatite formation on the surface of calcareous oolites. Finally, the Holocene warming was accompanied by increasing sea level, enhanced tropical weathering, Fe and Al mobility and variscite formation superimposed on degraded Ca-phosphates, forming two phase phosphatic aggregates.
650 $aornithogenic soils
653 $aPaleogeograph
653 $aPhosphatization
653 $aVolcanic islands
700 1 $aSCHAEFER, C. E. G. R.
700 1 $aABRAHÃO, W. A. P.
700 1 $aALMEIDA, E. de P. C.
700 1 $aSIMAS, F. N. B.
773 $tJournal of South American Earth Sciences$gv. 52, p. 119-128, Jul. 2014.
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