154 resultados para Erosão Hídrica
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Este estudo foi realizado com o objetivo de avaliar os estados de erosão acelerada do solo presente em áreas com canaviais e pomares de citros localizados na região administrativa de Ribeirão Preto - SP. Foram empregadas fotografias aéreas verticais, na escala aproximada de 1:40.000, do vôo da cobertura aerofotográfica da região citrícola do Estado de 1988. O estudo foi realizado identificando-se e delimitando-se todas as áreas de abrangência de cinco estados da erosão acelerada do solo presentes nos canaviais e pomares de citros. A presença da erosão acelerada severa a extremamente severa foi constatada tanto nos canaviais como nos pomares de citros, nas quatro unidades de solos de ocorrências principais na área de estudo. Os valores da extensão total das áreas de abrangência dos estados da erosão 2 a 5 (processos erosivos intensos a extremamente intensos) revelaram forte impacto sobre o desenvolvimento das culturas, degradando o solo agrícola e afetando a qualidade da água. As principais diferenças, quanto à extensão total das áreas de abrangência dos diferentes estados da erosão presente, foram identificadas principalmente entre os Argissolos e os Latossolos, e entre os dois estágios de desenvolvimento das culturas. As condições de solo exposto foram verificadas nas áreas recentemente plantadas com cana-de-açúcar ou citros, explicitando-se a grande necessidade de empregar, nessas condições, práticas conservacionistas.
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JUSTIFICATIVA E OBJETIVOS: O objetivo desta pesquisa foi estudar os efeitos agudos do contraste radiológico em situações de restrição de volume, avaliando-se os efeitos renais e cardiovasculares após a injeção intra-arterial de contraste radiológico de alta osmolaridade. MÉTODO: Participaram do estudo 16 cães anestesiados com tiopental sódico (15 mg.kg-1) e fentanil (15 µg.kg-1) em bolus, seguido de infusão contínua nas doses de 40 µg.kg-1.min-1 (tiopental sódico) e 0,1 µg.kg-1.min-1 (fentanil). Foi feita hidratação com solução de glicose a 5% (0,03 mL.kg-1.min-1) e a ventilação pulmonar foi controlada mecanicamente com ar comprimido. Foram verificados os seguintes atributos: freqüência cardíaca (FC); pressão arterial média (PAM); pressão da veia cava inferior (PVI); débito cardíaco (DC); hematócrito (Ht); fluxo plasmático efetivo renal (FPER); fluxo sangüíneo renal (FSR); ritmo de filtração glomerular (RFG); fração de filtração; resistência vascular renal (RVR); volume urinário (VU); osmolaridade plasmática e urinária; depuração osmolar, depuração de água livre e depuração de sódio e de potássio; sódio e potássio plasmáticos; excreção urinária e fracionária de sódio e potássio e temperatura retal. Estes atributos foram avaliados em quatro momentos: 30 (M1), 60 (M2), 90 (M3) e 120 (M4) minutos após o início da infusão de para-aminohipurato de sódio e creatinina (início da experiência). No momento 2, no grupo G1 foi feita injeção intra-arterial de solução fisiológica a 0,9% (1,24 mL.kg-1), e no grupo G2 foi injetado contraste radiológico (1,24 mL.kg-1) pela mesma via. RESULTADOS: O grupo G1 apresentou aumento da FC, do FPER, do FSR, da osmolaridade plasmática, da depuração de sódio e da excreção urinária de sódio; apresentou ainda diminuição da osmolaridade urinária, do potássio plasmático, da depuração de potássio e da temperatura retal. No grupo G2 ocorreu aumento da FC, da RVR, do VU, da depuração osmolar, da depuração de sódio e da excreção urinária e fracionária de sódio; ocorreu também redução do (a): hematócrito, ritmo de filtração glomerular, fração de filtração, osmolaridade urinária, depuração de água livre, sódio e potássio urinários, potássio plasmático e temperatura retal. CONCLUSÕES: Neste estudo, conclui-se que a injeção intra-arterial do contraste radiológico causou efeito bifásico na função renal. Inicialmente, provocou aumento da diurese e da excreção de sódio, mas, posteriormente, houve piora das condições hemodinâmicas e, conseqüentemente, da função renal, com aumento da resistência vascular renal e diminuição do ritmo de filtração glomerular.
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O estresse hídrico afeta profundamente o metabolismo celular vegetal. Neste trabalho, objetivou-se quantificar os efeitos da deficiência hídrica e sua recuperação sobre a atividade das enzimas do metabolismo do nitrogênio: redutase do nitrato (RN), glutamina sintetase (GS) e glutamato sintase (GOGAT) e sobre o acúmulo de prolina em plantas dos genótipos de milho BR 2121 e BR 205. O experimento foi conduzido em casa de vegetação, sob o delineamento inteiramente casualizado, com quatro repetições, utilizando-se vasos que continham 14,3kg de solo. Os tratamentos consistiram da combinação dos dois genótipos e quatro intervalos entre irrigações (1, 3, 5 e 7 dias). No dia da avaliação (49 dias após emergência), os tratamentos com intervalos entre 3 e 7 dias, haviam sido irrigados no dia anterior, caracterizando-se portanto como recuperação da deficiência hídrica leve e severa, respectivamente. As extrações e análises foram realizadas utilizando-se a terceira folha basípeta completamente expandida. As atividades das enzimas estudadas não diferiram entre os tratamentos de estresse hídrico, controle e recuperação do estresse moderado, entretanto as plantas sob recuperação do estresse severo apresentaram atividade enzimática superior à das plantas controle. O acúmulo de prolina livre nas folhas aumentou com o estresse hídrico e respondeu à recuperação do estresse apresentando redução. de modo geral, a atividade enzimática e o acúmulo de prolina apresentaram respostas inversas dentro dos tratamentos.
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Objetivando verificar a influência do teor de água do substrato na germinação de sementes de cebola (Allium cepa L.), conduziu-se um ensaio sob condições de ambiente de laboratório. Os efeitos de cinco níveis de água no substrato solo x areia (3:1), 20, 40, 60, 80 e 100% da capacidade de retenção foram avaliados através da porcentagem de emergência no 14° dia da semeadura e pesos da matéria verde e seca das plântulas normais. Para tanto, 200 sementes do cultivar Pira Ouro por tratamento, em quatro repetições de 50, foram semeadas a 1,5 cm de profundidade, mantendo-se constantes os níveis de água no substrato. Os resultados possibilitaram concluir que os níveis de umidade do solo indicados para germinação de sementes de cebola são de 40% e 60% da capacidade de retenção do substrato, por possibilitarem uma melhor emergência, peso da matéria verde e seca das plântulas.
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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
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Resultados de pesquisa envolvendo aspectos fisiológicos da pupunheira (Bactris gasipaes Kunth), fruteira nativa da América Tropical, são escassos. Procurando completar essa lacuna, um experimento sob deficiência hídrica foi conduzido em casa de vegetação, durante um período de 13 dias, utilizando plantas de 12 meses de idade. O objetivo principal foi avaliar as respostas da pupunheira à deficiência hídrica. As variáveis observadas foram: taxa de assimilação de CO2, transpiração, condutância estomática e potencial de água das folhas. As coletas dos dados foram realizadas diariamente em laboratório e sob fluxo de 1200 mim-2 s-1. Os resultados foram submetidos à análise de variância e de regressão. Verificou-se decréscimo no potencial de água da folha e nas trocas gasosas quando a irrigação foi interrompida por mais de seis dias. Valores mínimos foram obtidos no décimo dia, com redução de 92% da fotossíntese líquida, 87% da condutância estomática e 70% da transpiração. O menor potencial de água nas folhas (-1,9 MPa) foi também observado nesse período. Houve recuperação total de todas as variáveis dois dias após reirrigação, com exceção da condutância estomática. A diminuição da condutância estomática e a queda mais rápida da taxa de transpiração que a queda na fotossíntese, indicam a existência de mecanismos de aclimatação em pupunheira, no sentido de diminuir as perdas de água, quando sob condição de estresse hídrico moderado.
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The objective of this work was to identify the spatial variability of the natural erosion potential, soil loss and erosion risk in two intensely cultivated areas, in order to assess the erosion occurrence patterns. The soil of the area located at Monte Alto, São Paulo state, was classified as Paleudalf (PVA) with moderately slope, with different managements. The soil of the area located at Jaboticabal, São Paulo state, was classified as Haplortox(LV) with gentle slope and cultivated with sugarcane. A irregular grid was imposed on the experimental areas. Soil samples were obtained from 0-0.2 m depth at each grid point: 88 samples in Monte Alto area (1465 ha) and 128 samples at Jaboticabal area (2597 ha). In order to obtain the values of the studied variables USLE was applied at each grid point. Descriptive statistics were calculated, and geoestatistical analyses were performed for defining semivariograms. Kriging techniques to develop map showing spatial patterns in variability of selected soil attributes were used. All variables showed spatial dependence. The PVA soil showed higher erosion risk due to the slope and atual management compared to the soil LV.
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This study aimed at the elaboration of a database with information and a map of erosion vulnerability for ecological zoning for the upper Pardo River, Botucatu, SP, by using the Geographical Information System - SPRING. The map of erosion vulnerability was made from spectrally homogeneous regions, producing a grid of zone averages, which was then subdivided, resulting in a vulnerability map to erosion. The results allowed us to conclude that digital imaging produced valuable information for mapping of soil use and database formation. The GIS - SPRING was efficient at identifying soil and vulnerability erosion classes and 95% of the basin presents a moderately stable vulnerability degree, through the presence of medium young soils in gently waring reliefs and covered by 49.27% of pasture and 29.88% crops.
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The species Schizolobium amazonicum (Huber ex Ducke) commonly known as pinho-cuiabano or paricá, is one of the trees in Amazonian area used for plantings in degraded areas, reforestations and agroforestry systems. The present work evaluated the germinative behaviour of seeds of Schizolobium amazonicum in relation to the hydric stress, defining their levels of tolerance to those limitations in the environment. The seeds were collected from 30 trees in Alta Floresta-MT and submitted the dormancy treatment by submersion into water at 100°C for 1 minute; followed by treatment with fungicide Ridomil and Cercobin 0,25% each, then being left to germinate in a BOD camera at 30°C under a photoperiod of 12 hours. For evaluating the effect of different water potentials in the germinative process, polyethylene glicol (PEG 6000) was used and the salts NaCI and CaCl 2 used to simulate saline stress. The seeds were put to soak in potentials of 0 (control); -0.1 ; -0.2; -0.3; -0.4 and -0.5MPa. For each treatment 5 repetitions of 20 seeds were used in gerbox, placed between filter paper moistened with 20 mL of PEG, NaCI and CaCl 2 solutions. The solutions were changed at intervals of 24 hours for maintenance of the potential. The evaluations of percentages and germination speed were carry out daily for 8 days, being considered germinated the seeds that presented a 2mm root extension or longer. The data were submitted to analysis of variance and averages compared by the Tukey test at 5% probability. It was concluded that osmotic potentials between -0.4 and -0.5MPa inhibited the germination of seeds of Schizolobium amazonicum completely. The osmotic stress caused by CaCl 2, and PEG injured the germination more than did the stress caused by NaCl.
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Accelerated soil erosion is, at present, one of the most widespread environmental problems in the world. Geographic Information Systems (GIS) have become an essential tool in soil erosion studies and consequently in the development of appropriate soil conservation strategies. The objective of this paper was to assess the degree of soil erosion associated with land cover dynamics through GIS analysis and to validate the modeling with indicators of soil erosion. Universal Soil Loss Equation (USLE) model, GIS technology and ground-truth dataset (erosion indicators) were employed to elaborate the soil loss maps for four dates at Sorocaba Municipality (SP, Brazil). It was verified that, although the predicted soil loss rate is normally small along the study area, such rate is significantly greater than the soil formation rate. This shows a non-sustainable situation of soil and land cover management. Unplanned urban expansion seems be the main driving force that acts in increasing the erosion risk/occurrence along the study area.
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In the experimental area of the Department of Environmental Sciences (21.85° S; 48.43° W; 786 m), in the School of Agronomical Sciences, UNESP, Botucatu, SP, an experiment was carried out using peanut (Arachis hypogaea L), cv. IAC-TATU-ST, to quantify the crop daily water requirements. During the peanut crop cycle, the environmental variables, such as rainfall, air temperature, air relative humidity, soil matric potential, soil heat flux and radiation balance, have been registered continually. These measurements were used to calculate the daily crop evapotranspiration, by the Bowen ratio method. The water replacement required by the peanut crop was done the dripping irrigation system, oriented by a dynamic agrometeorological model that computes the entrance and exit of water in the soil. During the peanut crop cycle, 9.0 mm of water was used from sowing to emergence; 67.0 mm of water, in the growth stage; 166.0 mm, in the flowering stage; 124.0 mm in the final stage and 46.0 mm from physiological maturity to harvest. Oot of 412.0 mm of the total consumption, 246.0 mm of water was supplied by irrigation and 166.0 mm by the rain. The grain yield was 3.15 t ha-1 for 15% of humidity, and the water use efficiency was 0.764 kg m-3.
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The agricultural unpaved roads are important road structures for the economic and social agricultural development of the Nation, and the erosion provoked by rain water in the road bed and sides are closely related to bad draining, one of the main factors for their degradation. In order to make the draining system adequate, it is necessary to know about erodibility, infiltration capacity of water in the ground and adoption of mechanical slope abatement with grid elevation and water interception. This study presents drainage model through the construction of terraces with gradient transversally associated to the capitation basin in abruptic red dystrophic argisol soils, medium sandy texture, based on slops abatement techniques, elevating the road bed and deviating flow. The grain sized fractions of this ground (sand, silt, clay) and the aggregate stability indicated that this ground, under anthropic action, presents erosive processes resulting in superficial draining with ground hauling, sanding sources and courses of water situation below roads, providing great environmental impacts in the hydric bodies. The reduction of erosion problems in these unpaved roads is in the adoption of measures that intercept waters from the draining of their stream bed itself, as well as pluvial waters comings from adjacent areas of contribution, that are collected and conducted to inlaid terraces and capitation basis.
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The objective of this work was to verify the application of cluster analysis to evaluate soil erosion risk for different soil classes, soil slopes and soil managements. The study was conducted in a 33 ha section of a large field located in Carmo do Rio Claro County, MG, Brazil. The field had been managed in a corn/bean rotation under conventional tillage and under coffee plantation for seven years, both under sprinkle irrigation. Soil samples were obtained at every 10 m at 0.20 m depth along a transect of 1050 m. Soil erosion risk (A), natural potential erosion (PN), and erosion expectation (EE) were determined and submitted to a cluster and principal component analysis. The application of clustering analysis showed high correlation between the clusters and soil types. With clustering analysis plus principal components analysis, it was possible to identify groups of high and low soil erosion expectation, showing that the areas with higher soil erosion expectation are correlated to the soil class, soil slope and soil management. Among the studied variables, the natural potential erosion (PN) showed to be the most important factor to identify different soil erosion groups. The cluster analysis showed that 98% of the variables were classified within each group, and that they should be managed differently due to the soil erosive potential of each group,.
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This study aimed to determine the crop evapotranspiration (ETc) and crop coefficient (Kc) of fertigated sweet pepper, measured over time (15, 30, 45, 60, 75, 90 and 105 days after the transplant). The experiment was conducted on a battery of 40 drainage lysimeters, arranged in a 8 x 5 matrix, in the period October/2009 to January/2010, located in the Federal Rural University of Pernambuco (UFRPE) Campus in Recife, in a completely randomized factorial scheme 5 x 2, with four replications, being five irrigation depths (80, 90, 100, 110 and 120% of ETc) and two levels of potassium (80 and 120 kg K2O ha-1) where the experimental plot was composed of three plants in each lysimeter. The Mauchly Sphericity Test indicated multivariate variance analysis for the studied variables ETc (mm d-1) and Kc, the variables presented adjustment under quadratic effect of variation on observation times, when the irrigation depths were fixed, and descending linear adjustments under the variation of irrigation depths effect, when the times of observation were fixed in each potassium dose.
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Water deficit is one of the environmental factors that cause a great reduction in the upland rice grain yield. The objective of this study was to evaluate genotypes of upland rice with broad genetic diversity for tolerance to this stress and to identify secondary traits for evaluation of this tolerance. Sixty-four genotypes were evaluated during two years at the Experiment Station of EMATER, in Porangatu, GO, under well-watered and water deficit conditions. The genotypes showed differences in grain yield and were influenced differently by the water treatments, both under a mild water deficit in the first year and under a severe one in the second year. The genotype grain yield under water deficiency was significantly and positively correlated with tiller fertility, number of panicles m-2, 100-grain weight, and plant height, and negatively with spikelet sterility and the number of days for the occurrence of 50% panicle emergence. It was also observed that the most productive genotypes under water deficit conditions showed lower leaf temperature, indicating improved water status. Nine genotypes were productive in both water conditions and three were productive only when well-watered.