979 resultados para Fazenda Caiuá
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Cet article traite de la possibilité de proposer le Trésor à la justice pour annuler une décision administrative définitive sur les questions fiscales. Il s'agit d'un sujet qui s'oppose au principe de la vérité matérielle - qui doit prévaloir en cas d'impôt - avec une certitude morale représentée par la chose jugée administrative. Commence par le processus administratif d'impôt comme une garantie constitutionnelle du contribuable, insérée dans le panorama d une compétence adoptée dans la législation brésilienne en tant que pilier de l'Etat de droit démocratique. Met l'accent sur la position du Trésor avant l'autorité de la chose jugée administrative, ce qui démontre la fragilité de La décision finale sur les questions fiscales. Décrit les effets de la révision (ou de l'annulation) dês actes administratifs, en particulier la libération de l'impôt et de la décision administrative qui vise à le confirmer. Enfin, nous discuterons de la composition et la légitimité du contentieux administratif, en conclusion, avec le soutien de la prévalence d'un fait important dans le cãs d'impôt, est non seulement possible, mais le Trésor devrait examiner leurs propres actions si nécessaire
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This thesis deals with the sedimentological/stratigraphic and structural evolution of the sedimentary rocks that occur in the NW continental border of the Potiguar Basin. These rocks are well exposed along coastal cliffs between the localities of Lagoa do Mato and Icapuí, Ceará State (NE Brazil). The sedimentological/stratigraphic study involved, at the outcrop scale, detailed facies descriptions, profile mapping of the vertical succession of different beds, and columnar sections displaying inferred lateral relationships. The approach was complemented by granulometric and petrographic analyses, including the characterization of heavy mineral assemblages. The data set allowed to recognize two kinds of lithological units, a carbonate one of very restricted occurrence at the base of the cliffs, and three younger, distinct siliciclastic units, that predominate along the cliffs, in vertical and lateral extent. The carbonate rocks were correlated to the late Cretaceous Jandaíra Formation, which is covered by the siliciclastic Barreiras Formation. The Barreiras Formation occurs in two distinct structural settings, the usual one with nondeformed, subhorizontal strata, or as tilted beds, affected by strong deformation. Two lithofacies were recognized, vertically arranged or in fault contacts. The lower facies is characterized by silty-argillaceous sandstones with low-angle cross bedding; the upper facies comprises medium to coarse grained sandstones, with conglomeratic layers. The Tibau Formation (medium to coarse-grained sandstones with argillite intercalations) occurs at the NW side of the studied area, laterally interlayered with the Barreiras Formation. Eolic sediments correlated to the Potengi Formation overly the former units, either displaying an angular unconformity, or simply an erosional contact (stratigraphic unconformity). Outstanding structural features, identified in the Barreiras Formation, led to characterize a neocenozoic stress field, which generated faults and folds and/or reactivated older structures in the subjacent late cretaceous (to paleogene, in the offshore basin) section. The structures recognized in the Barreiras Formation comprise two distinct assemblages, namely a main extensional deformation between the localities of Ponta Grossa and Redonda, and a contractional style (succeeded by oblique extensional structures) at Vila Nova. In the first case, the structural assemblage is dominated by N-S (N±20°Az) steep to gently-dipping extensional faults, displaying a domino-style or listric geometry with associated roll-over structures. This deformation pattern is explained by an E-W/WNW extension, contemporaneous with deposition of the upper facies of the Barreiras Formation, during the time interval Miocene to Pleistocene. Strong rotation of blocks and faults generated low-angle distensional faults and, locally, subvertical bedding, allowing to estimate very high strain states, with extension estimates varying between 40% up to 200%. Numerous detachment zones, parallel to bedding, help to acommodate this intense deformation. The detachment surfaces and a large number of faults display mesoscopic features analoguous to the ones of ductile shear zones, with development of S-C fabrics, shear bands, sigmoidal clasts and others, pointing to a hydroplastic deformation regime in these cases. Local occurrences of the Jandaíra limestone are controled by extensional faults that exhume the pre-Barreiras section, including an earlier event with N-S extension. Finally, WNWtrending extensional shear zones and faults are compatible with the Holocene stress field along the present continental margin. In the Vila Nova region, close to Icapuí, gentle normal folds with fold hinges shallowly pluging to SSW affect the lower facies of the Barreiras Formation, displaying an incipient dissolution cleavage associated with an extension lineation at high rake (a S>L fabric). Deposition of the upper facies siliciclastics is controlled by pull-apart graben structures, bordered by N-NE-trending sinistral-normal shear zones and faults, characterizing an structural inversion. Microstructures are compatible with tectonic deformation of the sedimentary pile, burried at shallow depths. The observed features point to high pore fluid pressures during deformation of the sediments, producing hydroplastic structures through mechanisms of granular flow. Such structures are overprinted by microfractures and microfaults (an essentially brittle regime), tracking the change to microfracturing and frictional shear mechanisms accompanying progressive dewatering and sediment lithification. Correlation of the structures observed at the surface with those present at depth was tested through geophysical data (Ground Penetrating Radar, seismics and a magnetic map). EW and NE-trending lineaments are observed in the magnetic map. The seismic sections display several examples of positive flower structures which affect the base of the cretaceous sediments; at higher stratigraphic levels, normal components/slips are compatible with the negative structural inversion characterized at the surface. Such correlations assisted in proposing a structural model compatible with the regional tectonic framework. The strong neogenepleistocene deformation is necessarily propagated in the subsurface, affecting the late cretaceous section (Açu and Jandaíra formations), wich host the hydrocarbon reservoirs in this portion of the Potiguar Basin. The proposed structural model is related to the dextral transcurrent/transform deformation along the Equatorial Margin, associated with transpressive terminations of E-W fault zones, or at their intersections with NE-trending lineaments, such as the Ponta Grossa-Fazenda Belém one (the LPGFB, itself controlled by a Brasiliano-age strike-slip shear zone). In a first step (and possibly during the late Cretaceous to Paleogene), this lineament was activated under a sinistral transpressional regime (antithetic to the main dextral deformation in the E-W zones), giving way to the folds in the lower facies of the Barreiras Formation, as well as the positive flower structures mapped through the seismic sections, at depth. This stage was succeeded (or was penecontemporaneous) by the extensional structures related to a (also sinistral) transtensional movement stage, associated to volcanism (Macau, Messejana) and thermal doming processes during the Neogene-Pleistocene time interval. This structural model has direct implications to hydrocarbon exploration and exploitation activities at this sector of the Potiguar Basin and its offshore continuation. The structure of the reservoirs at depth (Açu Formation sandstones of the post-rift section) may be controlled (or at least, strongly influenced) by the deformation geometry and kinematics characterized at the surface. In addition, the deformation event recognized in the Barreiras Formation has an age close to the one postulated for the oil maturation and migration in the basin, between the Oligocene to the Miocene. In this way, the described structural cenario represents a valid model to understand the conditions of hydrocarbon transport and acummulation through space openings, trap formation and destruction. This model is potentially applicable to the NW region of the Potiguar Basin and other sectors with a similar structural setting, along the brazilian Equatorial Atlantic Margin
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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
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O presente trabalho estudou a intoxicação acidental por arsênico em um lote de 24 vacas Girolando, as quais tiveram acesso a pasto pulverizado com herbicida à base de metano arsonato ácido monossódico (MSMA). Os bovinos apresentaram apatia, anorexia e diarreia profusa. Foram necropsiados na fazenda dois animais de 14 que morreram. Os principais achados macroscópicos foram úlceras abomasais e congestão renal. No exame microscópico, as principais lesões observadas foram abomasite e omasite necro-hemorrágica multifocal acentuada e, nos rins, necrose tubular difusa. As concentrações médias de arsênico em vacas com sinais clínicos foram 1,19±0,40, 10,52±2,16 e 76,06±48,37ppm no sangue, leite e fezes, respectivamente. Os níveis de arsênico encontrados em dois animais necropsiados foram 25,58 e 23,85ppm em fígado, e 28,71 e 35,94ppm em rins, respectivamente. No feto de uma vaca necropsiada, os níveis de arsênico mensurados no fígado e rim foram 9,0 e 8,92ppm, respectivamente. A concentração de arsênico no capim do piquete pulverizado foi 111,58ppm. No Brasil, o uso MSMA na composição de pesticidas e herbicidas é permitido somente para uso agrícola, mas não pecuário. A utilização desse ou de outros produtos à base de arsênico na pecuária pode causar altos índices de mortalidade no rebanho, além de diminuição da produção e contaminação de produtos de origem animal.
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Great part of the gold mineralizations are associated with shearing zones through which circulate a great volume of fluids, that interact with the host rocks, originating leaching or precipitation of chemical elements, including gold. The studied mineralizations are inserted in the Seridó Belt. The tungsten mineralization in Brejuí Mine is hosted in calcsilicate rocks from Jucurutu Formation. The São Francisco auriferous mineralization has as host rocks mica-schists from Seridó Formation, while the Ponta da Serra and Fazenda Simpático mineralizations are hosted in orthogneisses of this fold belt basement. The research conducted on these mineralizations had the purpose of integrate the data of chemical elements behavior during the shearing/mineralizing event, and its influence on the isotopic systems Rb-Sr and Sm-Nd. The studies of chemical mobility in the auriferous mineralizations showed that elements that during the shearing displayed in general an immobile behavior were Al, Ti and Zr. Among the elements that were mobilized during the event, K and Rb showed mass gain in ali belts of transformed rocks, while the elements Ca, Na and Sr normally lost mass. Petrographic studies showed that the minerais biotite and plagioclase, in all investigated mineralizations, played an important role in the chemical reactions occurred in the transformed rocks to the generation of muscovite, cordierite and sillimanite, justifying the input of K to the formation of muscovite, and the release of Na and Ca from plagioclase to the fluid phase. In the São Francisco auriferous mineralization, the results of the Rb-Sr isotopic analysis yielded ages of 645 ± 19 Ma and 596 ± 17 Ma, with both samples, from original and transformed rocks. Two ages, 569 ± 20 Ma. and 554 ± 19 Ma., were obtained with samples frem the transformed rocks domain. These ages suggest that there were two metamorphic pulses during the emplacement of the mineralized shearing zone. The Sm-Nd data yielded TDM ages of 1,31 Ga and 1,26 Ga with 3Nd (0,6 Ga) of -0,26 e -0,40 for the original and final transformed rocks, respectively. In case of the orthogneisses of Caicó Complex, e.g. the Ponta da Serra and Fazenda Simpático mineralizations, the Rb-Sr data did not yield ages with geological significance. In the Ponta da Serra mineralization, the Sm-Nd isotopic data yielded T DM ages of 2,56 Ga and 2,63 Ga to the original rocks and of 2,71 Ga to the mineralized sheared rock, and values of 3Nd (2,0 Ga) between -3,70 e -5,42 to the original and sheared rock, respectively. In the Fazenda Simpático, Sm-Nd data yielded TDM between 2,65 and 2,69 Ga with values of 3Nd (2,0 Ga) between -5,25 e -5,52. Considering the Sm-Nd data, the TDM ages may be admitted as the age of the parental magma extraction, producer of the protoliths of the orthogneisses from Ponta da Serra and Fazenda Simpático mineralizations. The chemical mobility studies showed that in the basement hosted mineralizations, Rb achieved mass while Sr lost mass, as Sm as well as Nd were strongly mobilized. The Sm/Nd ratio remained constant, however, confirming the isochemical character of those elements. In the basement mineralizations, Rb-Sr ages are destituted of geological significance, because of the partial opening of the isotopic system during the tectono-metamorphic transformations. In the tungsten mineralization, the diagram Sm-Nd constructed with the whole-rock data of calcsilicatic and the high-temperature paragenesis (garnet, diopside and iron-pargasitic hornblende) indicated an 631 ± 24 Ma age, while with the whole-rock data and low-temperature paragenesis (vesuvianite, epidote and calcite), a 537 ± 107 Ma age was obtained. These ages, associated with the petrographic observations, suggest that there was a time gap among the hydrothernal events responsible by the formation of the high and low temperature paragenesis in the calcsilicatic rocks mineralized in scheelite
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The town of Sobral is located at the northwest part of the Ceará State, 250 km away from its capital, Fortaleza. In January 2008, an intense seismic activity began near Sobral with one event with magnitude 4,2mb on May 21. Since the start of its seismic activity, all events were recorded by the SBBR station (located on EMBRAPA Caprinos Farm), which operates in the region since August 2007. After this event, monitoring the seismic activity was carried out with the deployment of a local three component digital seismographic network, from June 5, 2008 until September 24. Initially, this network was composed of six seismographic stations. Later additional five stations were deployed until August 26 2008. This local network detected approximately 2,800 earthquakes. In this study we analyzed 581 earthquakes recorded by at least three stations for hypocentral and focal mechanism determination, and to contribute to a better explanation of the seismicity which in this region. To determine the hypocenters, we used a half-space model, with vP = 6,00 km/s and vP/vS = 1,71. From the hypocentral determination, it was revealed an active seismic zone with depth ranging between 1 and 8 km, 6 km long in E - W direction. The determination of fault planes and focal mechanism was obtained using the programs FPFIT and PLAN, which allowed comparison between their respective results in order to obtain more accurate results. A set of 24 earthquakes were selected to determine fault using PLAN planes and focal mechanisms using FPFIT. With the aid of detailed map of hypocenters this set, it was possible to identify three structures. Therefore, the set of 24 earthquakes were divided into three subsets. The type of mechanism was predominantly strike-slip with a dextral direction. Although the region has two tectonic structures near the site of the study area: the Café- Ipueiras Fault (normal fault) and the Sobral-Pedro II Lineament (dextral strike-slip fault) it was not possible to correlate the seismicity founded with those structures
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The present dissertação had as objective to study the ambient management in the Farms Saint Rita, Tahim Agropesca and Agropesca Rigomoleiro, in the Great River of the North. For this we use as theoretical tool some fundantes concepts of geographic science, the space, and as concepts auxiliary of ambient management, of estuaries as the half natural one and of manguezais as ecosystem. The study if it gave taking in consideration a model of flow of activities of a typical farm following the way of the residues produced since the beginning until its final destination, in a suitable script of SCHERER (1999). The considered flow established a sequence activities where it is identified the material of entrance, the process of management, the residues of exit and the destination of the residues to the long one of the phase of culture of the shrimp. From it was there had been elaborated a series of managemental pictures with the data raised in the three farms, of different transports and concludes that the ambient management of these farms does not follow the formal standards of a system of typical ambient management. Collating with the system of considered by norm ISO14000 the study it disclosed that all the companies are in a situation of not conformity and that the impacts on the environment continue being many significant ones. However, it is possible to implant norm ISO14000 because some procedures implanted for the farms are correct of the point of view of the ambient management
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OBJETIVOS: Traçar o perfil do usuário da Sala de Recursos para Deficiente Visual na cidade de Assis - SP, avaliar a porcentagem de deficientes visuais empregados e comparar o emprego com idade, gênero, tipo de deficiência e doença causadora da deficiência, entre dois períodos: de 1984 a 1996 e de 1997 a 2009. MÉTODOS: Foi realizado estudo retrospectivo dos prontuários médicos e da ficha escolar dos portadores de deficiência visual que frequentaram a Sala de Recursos para Deficiente Visual, no período de 1984 a 2009 na cidade de Assis - SP, divididos em dois períodos de 1984 a 1996 (G1) e de 1997 a 2009 (G2). Analisaram-se dados demográficos, a doença que provocou a baixa visão, o tipo de deficiência visual (cegueira ou baixa visão), escolaridade, recursos ópticos, frequência à Sala de Recursos para Deficiente Visual e taxa de emprego. Foi feita associação da taxa de emprego com: idade, gênero, raça/cor, tipo de deficiência e doença nos dois diferentes períodos. RESULTADOS: Foram encontrados 149 deficientes visuais sendo: 61,07% homens, 38,9% mulheres, 82,5% brancos e 17,4% não brancos e a mediana da idade foi de 18 anos. Dos 149 deficientes visuais, 63,75% eram portadores de baixa visão e 36,24% portadores de cegueira. As principais doenças que levaram à deficiência visual dos 149 pacientes foram em ordem decrescente: retinocoroidite por toxoplasmose (17,40%), atrofia óptica congênita (12,10%), alta hipermetropia (8,72%), retinose pigmentar e alta miopia (6,71% cada uma) e glaucoma congênito e catarata congênita (6,04% cada uma). A frequência à Sala de Recursos para Deficiente Visual foi boa em mais de 50% dos pacientes. Estavam trabalhando regularmente 44,7% e 12,3% dos maiores de 14 anos respectivamente nos períodos de 1984 - 1996 e de 1997 - 2009. Não houve diferença entre os dois períodos quanto às características demográficas, tipo de deficiência e doenças, havendo correlação da taxa de emprego apenas com a idade (pacientes com média de idade maior apresentavam maior porcentagem de emprego). CONCLUSÕES: Os deficientes visuais eram na maioria homens, brancos, portadores de baixa visão e portadores de toxoplasmose ocular. Quase metade (44,7%) dos pacientes com mais de 14 anos encontrava-se trabalhando regularmente até 1996 sugerindo que esforços conjuntos de oftalmologistas e educadores auxilia na inclusão social destes pacientes. A taxa de emprego caiu no período de 1997 a 2009 e a de aposentados aumentou.
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O objetivo deste estudo foi avaliar a influência do transporte fluvial na incidência de lesões tissulares em carcaças de bovinos abatidos no Pantanal Sul Mato-Grossense, por meio da quantificação do número e tamanho das lesões, bem como a identificação e determinação da idade das lesões em função do tempo ocorrido e a localização dessas lesões nos principais cortes comerciais brasileiros. Apurou-se que, do total de 88 carcaças avaliadas, 83 (94,3%) tiveram uma ou mais lesões, totalizando 253 lesões que resultaram na remoção de 39,988 kg de carne, com média geral de 0,454 kg por animal. Com relação ao tamanho das lesões, as maiores médias foram encontradas em animais oriundos das condições I e II. Foi encontrada a maior média em bovinos procedentes da condição II para a idade de lesões em carcaças. Foi constituída diferença na freqüência de lesões nos cortes comerciais nas condições avaliadas. Conclui-se que o sistema de transporte dos bovinos no Pantanal influenciou a incidência de lesões. O aumento do tempo de transporte, associado à longa distância e ao jejum, durante o manejo da fazenda até o frigorífico, provocaram maior número de lesões, porém de menor tamanho.
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Objetivou-se avaliar as alterações físicas, produção de ovos e mortalidade de codornas poedeiras submetidas a muda forçada, durante um período de jejum. Utilizou-se um delineamento inteiramente ao acaso, com quatro tratamentos (0, 1, 2, e 3) dias de jejum, com três repetições de 36 aves por parcela. No início e ao final do período de jejum 2 aves por parcela foram abatidas, pesadas individualmente e sacrificadas para retirada e avaliação do ovário, oviduto, e fígado. Os resultados mostraram que no período de jejum de três dias houve uma redução de 25,64% no peso vivo, a produção de ovos caiu a 2,81% e a mortalidade foi de 4,60%.
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Utilizaram-se onze capivaras (Hydrochoerus hydrochaeris), cinco machos e seis fêmeas, sadias, com dois anos de idade, criadas em regime de cativeiro na Fazenda Experimental Lageado da FMVZ - UNESP de Botucatu - SP, submetidas à anestesia dissociativa com midazolam e quetamina, para o estabelecimento de valores hematológicos. Este estudo compreendeu a determinação dos valores normais de eritrograma, leucograma, proteína plasmática total e fibrinogênio.Os valores médios encontrados para machos e fêmeas foram, respectivamente, 3,62 e 3,71x10(6)/mil para eritrócitos, 15,0 e 15,4g/dl para hemoglobina, 48 e 49% para volume globular, 4630 e 5200/mil para leucócitos, 6,3 e 6,4g/dl para proteína plasmática total e 240 e 316,6mg/dl para fibrinogênio. Observou-se, desse modo, a ausência de diferenças entre os sexos.
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Aspectos macroscópicos e morfométricos dos testículos em catetos e queixadas. Este trabalho objetiva fornecer dados macroscópicos e morfométricos dos testículos dos catetos e queixadas. O material utilizado consistiu de catetos e queixadas oriundos da Fazenda Devaneio Pró-Fauna, Iguape, SP (Reg.1/3593/08480). em 33 queixadas e 20 catetos, após o abate, os testículos foram colhidos e tomados dados morfométricos como: comprimento, largura e espessura (com o auxílio de um paquímetro). Os testículos são ovalados, localizados na região pélvica, inclinados dorso-caudalmente e possuem posição intermediária. O mediastino testicular esta no centro do testículo, ligeiramente desviado para a margem epididimária deste, e termina na extremidade capitata. Os queixadas adultos possuem em média 30,92 ± 3,82 kg de peso corporal e 78,89 ± 4,77 cm de comprimento corporal, enquanto os jovens apresentam 22,93 ± 2,07 kg e 71,57 ± 3,95 cm de comprimento. Os resultados demonstram que no grupo de queixadas adultos estudado o testículo direito teve comprimento, largura e espessura médios de 5,36 ± 0,64cm; 3,64 ± 0,64cm e 3,30 ± 0,52cm respectivamente, enquanto que o esquerdo teve 5,45 ± 0,77cm; 3,68 ± 0,59cm e 3,32 ± 0,54cm. Nos queixadas jovens os valores encontrados foram de 3,20 ± 0,44cm, 2,12 ± 0,26cm e 2,11 ± 0,40cm, e de 3,23 ± 0,47cm; 2,21 ± 0,39cm e 1,99 ± 0,36cm, para a largura, comprimento e espessura dos testículos direito e esquerdo respectivamente. Já para os catetos o testículo direito teve comprimento, largura e espessura de 4,36 ± 0,38cm; 2,74 ± 0,27cm e 2,33 0,46cm respectivamente, enquanto que o esquerdo teve 4,19 ± 0,36cm; 2,68 ± 0,31cm e 2,34 ± 0,28cm. Os dados analisados não tiveram diferenças significativas (p<0,05) entre os valores encontrados para os testículos direito e esquerdo pelo testes de Qui-dradado.
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Este trabalho teve como objetivo verificar se o horário de colheita da erva-cidreira brasileira [Lippia alba (Mill.) N. E. Br.], fenotipo carvona-limoneno, tem influência sobre a produção de massa foliar, rendimento e composição do óleo essencial. Foram avaliados cinco horários de colheita quando a cultura estava com 145 dias desde o transplante: 8:00, 10:00, 12:00, 14:00 e 16:00 h com cinco repetições, distribuídos em blocos casualizados. O experimento foi conduzido na Fazenda Experimental Lageado da FCA-UNESP/Botucatu no Setor de Horticultura do Departamento de Produção Vegetal. A colheita foi realizada a 15 cm da superfície do solo e o óleo essencial obtido através de hidrodestilação, em aparelho tipo Clevenger. Levou-se em consideração os fatores agronômicos e o rendimento obtido por hidrodestilação. O óleo essencial foi analisado em cromatógrafo gasoso acoplado a espectrômetro de massas (CG/EM). Os resultados foram submetidos à análise de variância (Teste F) e as médias comparadas pelo teste de Tukey. Não houve diferença estatística para produção de massa foliar, teor de óleo essencial e produtividade de óleo essencial em massa fresca e seca. No entanto, entre os compostos majoritários do óleo essencial das folhas, carvona e limoneno, a melhor produtividade de carvona foi obtida às 10:00 h, em matéria fresca (2,050 L ha-1) e em matéria seca (2,068 L ha-1), e para o limoneno às 16:00 h, em matéria fresca (1,068 L ha-1) e em matéria seca (1,060 L ha-1).
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Aiming to study the affect of commercial biorregulators Stimulate (R) e X-Cyte (R) over sprouting uniformity of Superior Seedless grape cultivar, pruned in May 22, 2006, a field trial was carried out at at Koshiyama farm, in Juazeiro municipality (Bahia State / Northeastern Brazil). The trial was carried out in randomized blocks with four replications and three useful plants per plot, six stakes per plant were evaluated. Forty-eight hours after yield prun, the stakes were sprayed with T1: Dormex (R) (5%); T2: Dormex (R) (5%) + Nitro Plus 9 (R); T3: Stimulate (R) (0,5%); T4: Stimulate (R) (0,5%) + Nitro Plus 9 (R); T5: Stimulate (R) (1,0%); T6: Stimulate (R) (1,0%) + Nitro Plus 9 (R); T7: X-Cyte (R) (0,25%); T8: X-Cyte (R) (0,25%) + Nitro Plus 9 (R); T9: X-Cyte (R) (0,5%); T10: X-Cyte (R) (0,5%) + Nitro Plus 9 (R); T11: X-Cyte (R) (0,25%) + Stimulate (R) (0,5%); T12: X-Cyte (R) (0,25%) + Stimulate (R) (0,5%) + Nitro Plus 9 (R), Nitro Plus 9 (R) used at a rate of 100 L ha(-1) via ferti-irrigation. Results show that Stimulate (R) and X-Cyte (R), when compared to the commercial product Dormex (R) commercially, did not show significant effects on the sprouts number after sproutings and proportion of grown stems; products that as an alternative the Dormex (R) in yield the grape 'Superior Seedless', at the studied conditions.
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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)