1000 resultados para Solos - Uso - Goias (Estado)
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O bioma Cerrado encontra-se descaracterizado e menos de três por cento de suas áreas originais está legalmente protegida. A anurofauna desse bioma não é muito rica quando comparado a outros biomas, porém há um grande número de espécies endêmicas. Aqui apresentamos uma lista de espécies de anuros registrados em uma lagoa em área de cerrado aberto do município de Borebi, região Centro-Oeste do estado de São Paulo, sudeste do Brasil. Durante 24 meses de estudo (2008 e 2009) caracterizamos a distribuição das espécies na lagoa estudada e descrevemos a variação sazonal das espécies. Foram registradas 27 espécies pertencentes a seis famílias: Bufonidae (duas espécies), Cycloramphidae (uma espécie), Hylidae (13 espécies), Leiuperidae (quatro espécies), Leptodactylidae (cinco espécies) e Microhylidae (duas espécies). A riqueza de espécies e abundância estiveram relacionadas com a precipitação. Dendropsophus minutus foi a espécie mais abundante e com registro de vocalização durante o ano inteiro. Rhinella ornata e Odontophrynus americanus foram restritas ao período seco e frio (abril a agosto). As outras espécies tiveram seu período de maior atividade nos meses chuvosos e quentes (setembro a março). A ocupação da lagoa variou com o tipo de vegetação e conforme a variação do seu volume de água, principalmente nos período de estiagem. A alta riqueza e abundância de anuros da lagoa pode ser resultado da ausência de peixes predadores, dos diversos tipos de microambientes do local e da ausência de outros corpos d'água próximos.
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Os cerradões no Pantanal ocorrem em áreas não inundáveis da planície e são importantes para a economia regional. Das áreas de cerradão são retiradas madeiras para construção de cercas, currais e galpões. Apesar da grande importância dos recursos vegetais do cerradão, existem poucas informações para embasar sua conservação e uso sustentável. Este trabalho teve como objetivos estudar a abundância, a distribuição das espécies arbóreas e correlações com a fertilidade do solo em áreas de cerradão (savana florestada) do Pantanal Sul Mato-grossense. Foram estudadas seis áreas de cerradão na sub-região da Nhecolândia, por meio de 30 pontos quadrantes, totalizando 120 árvores amostradas, com circunferência a altura do peito (CAP) > 15 cm, em cada área. As comparações florísticas, de abundância das espécies e de fertilidade do solo, foram efetuadas por análises de componentes principais (PCA). As áreas mostraram-se heterogêneas, apresentando diferentes níveis de fertilidade do solo, estrutura e composição da vegetação. Dois cerradões foram agrupados em termos de fertilidade do solo e de estrutura da vegetação, apresentando muitas árvores de Qualea grandiflora Mart., espécie que ocorreu associada a solos com maiores teores de fósforo. Outros dois cerradões apresentaram composição florística mais semelhante que os demais, apesar de ocorrerem em solos com diferentes níveis de fertilidade, indicando perturbação antrópica.
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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
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A região da Serra da Onça é localizada no nordeste do Estado de Minas Gerais, no vale formado pelos trabalhos dos rios São Francisco e seus afluentes Jequitaí e Rio das Velhas. Esta região é caracterizada por diversos ciclos erosivos. Uma topossequência representativa da área foi escolhida para este estudo, sendo constituida por 5 perfis de solos desenvolvidos de sedimentos Quaternários. 0 Perfil 1, um Typic Hapleustox, está localizado na superfície mais antiga. Os outros solos estão localizados no sedimento Holocênico, área aluvial do São Francisco. Estes solos são menos intemperizados e classificados como Plíntic Haplustult (Perfil 2), Oxic Plintaquult (Perfil 3); Fluventic Plinthustult (Perfil 4) e Fluventic Argiustol (Perfil 5). Análises mineralógicas foram efetuadas em todas as fraçõs do solo. O Perfil 1 apresenta, em sua fração areia, somente minerais resistentes ao intemperismo, enquanto que nos demais solos, menos intemperizados, ocorrem micas e plagioclásios. Tais minerais aumentam de acordo com a profundidade do solo e também do Perfil 1 ao Perfil 5 menos intemperizado. A caulinita é o mineral de argila dominante na fração argila de todos os solos estudados, com maior concentração no Perfil 1, mais intemperizado. Este mineral tende a decrescer em profundidade e na direção do Perfil 1. Micas, vermiculita e montmorilonita também ocorrem do Perfil 2 ao Perfil 5.
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CONTEXTO: O adequado diagnóstico do estado nutricional é de vital importância para a prescrição da terapia nutricional enteral no ambiente hospitalar. OBJETIVO: Avaliar indicadores do estado nutricional em pacientes ingressantes na terapia nutricional enteral em uma unidade hospitalar. MÉTODOS: Estudo transversal com 100 pacientes adultos, sendo analisado o estado nutricional de ingresso à terapia nutricional enteral, por meio do índice de massa corporal obtido do peso e estatura estimados a partir de fórmulas de predição, e de indicadores laboratoriais do estado metabólico e nutricional. RESULTADOS: do total, 29% dos pacientes foram classificados como desnutridos pelo índice de massa corporal, enquanto 80% dos mesmos apresentaram albumina abaixo do valor de referência (<3,2 g/dL). Não houve diferença na distribuição das causas de base da internação entre os grupos classificados quanto ao estado nutricional pelo índice de massa corporal, prevalecendo as doenças cardiovasculares e pulmonares entre as principais causas. As concentrações abaixo dos valores de referência de albumina não foram diferentes entre os grupos classificados pelo índice de massa corporal e pelo diagnóstico de internação. CONCLUSÃO: O índice de massa corporal estimado foi indicador específico do estado nutricional, porém pouco sensível, enquanto a albumina mostrou-se mais sensível, o que reafirma a necessidade da combinação de vários indicadores para obtenção de um adequado diagnóstico nutricional.
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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
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The purpose of this study was to evaluate methods for predicting availability of Zn in soils. Surface soil samples representing Podzolized soils from Lins and Marilia var. Marilia and var. Lins, medium texture Dark-Red Latosol, Dusky-Red Latosol and Terra Roxa Estruturada, were gathered from fields in Jaboticabal, SP, Brazil. Com was used as indicator plant in a greenhouse experiment. Availability of Zn was determined with: 0.5 M CaCl2, 2.0 N MgCl2, N CH3COONH4 (pH 6.0 and 4.8), 0.05 and 0.1 N HCl, 0.05 N H2SO4, 0.005 M DTPA (pH 7.3 and 6.0), 1.0% Na2-EDTA, 0.01 M EDTA + 1.0 M (NH4)2CO3 (pH 8.6) and 0.02 M EDTA + 0.5 M CH3COOH + 0.5 M CH3COONH4. By using the simple correlation coefficients (Zn extracted from soils x absorbed by plants it can be concluded that the complexant agents and acid solutions showed to be efficient. The salt solutions showed low extraction capacity, low correlation coefficients and less accuracy. By considering aspects as accuracy and easy management DTPA pH 7,3 and Na2-EDTA can be indicated as the most apropriates (r values, respectively, 0.873** and 0.868** and V.C. 7.52% and 7.98%).
Caracteristicas gerais e classificacao de solos basalticos da regiao Central do Estado de Sao Paulo.
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Giving a special emphasis on soil classification relative to their positions in the landscape, five soil profiles in the Barra Bonita-Jau area were characterized through morphological, granulometric and chemical routine soil analysis. It was observed that the soil structure gradually changes from strong blocks with cutans (lowlands and smooth parts - Jau). In this direction, the silt/clay ratio and the base saturation is reduced, and the aluminium saturation increases. -from English summary
Uso de macroalgas para avaliação da Poluição orgânica no Rio Preto, noroeste do estado de São Paulo.
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The Preto River, located in the northwest of São Paulo State, receives a total wastewater load of 15.150 kg DBO day-1, from which 13.685 kg DBO day-1 (90.5%) corresponds to domestic sewage, and the city of São José do Rio Preto contributes with 12.400 kg DBO day-1 (90% of domestic sewage). During the period from August 1990 through January 1991, monthly sampling was carried out to evaluate the use of macroalgae as bioindicator of organic pollution. Five sampling sites were established along the main river and the following variables were analised: temperature, conductance, turbidity, dissolved oxygen, BOD, COD, total and fecal coliforms, and composition and abundance of macroalgal communities. Data were submitted to analysis of variance, correlation coefficient, cluster analysis (four different approaches) and converted to biological indices (species deficit, relative pollution, saprobity, diversity and uniformity indices). A wide range in water quality was found (particularly for conductance, oxygen, BOD and COD) among the sampling sites, which were classified into three groups (polluted, moderately polluted and unpolluted/weakly polluted). As regards the occurrence and abundance of macroalgae the Rhodophyta were found only in unpolluted or weakly polluted sites, whereas Cyanophyta occurred mostly under high pollution load; the Chlorophyta species were observed under a wide range of conditions. Among the biological indices, saprobity was the most sensitive and correlated to all water variables and the other indices. Cluster analyses showed that the composition of macroalgal communities was consistent with the levels of organic pollution in the Preto River.
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The objective if this work was a survey of medicinal plants plus commonly cultivated in quintais in Amazon State, Brazil. The work was carried out in five counties at the Solimões/Amazonas and Negro Rivers, by questionnaires, interviews and collections of botanical materials, using the literature to define the geographic origins. It was showed 105 species of medicinal plants, with average of 13 per house. The Amazonian plants, in general wood plants, meaning 10,9 percent of the total of species that was survey, with predominance of the American continent plants out of Amazonian (38,2 per cent). The major group was herbaceous or shrubs exotic plants, aromatics. In general, the peoples unknown the origin of the species of medicinal plants that use day after day.
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The World Health Organization (WHO) recommends that prescriptions of medicaments must be one parameter utilized to know how the medication is used by people. To do so, one specific methodology has been indicated, that is, the selected indicators of the use the medicaments. We applied this methodology with the aim of presenting a descriptive study of the physician prescription in Pediatric Clinic of the Health Basics Units. The results obtained are: the average number of medicaments prescribed with prescription was 2.6; the percentage of the medicaments prescribed with the generic name was 32%; the percentage of the prescriptions with antibiotics was 44.6%; the percentage of the prescriptions with injections was 10.4%; the percentage of the medicaments prescribed that are part of the municipal list was 22.8%, 27.5% for the program Dose Certs of the secretary of the State of São Paulo, and 50.4% by adding by adding the two lists. The essentiality of the medicaments prescribed may be considered very low, because only 32.6% appear in the RENAME. The percentage of the medicaments really dispensed was 39.9%. The medicaments more prescribed, according to the classification of the Anatomic-Therapeutic-Chemical (ATC), were the ones which acted in Respiratory System (26.8%), followed by anti-infectives for systemic use (16.4%) and by medicaments with acted in Alimentary tract and metabolism (15.8%). The conclusion is that the prescribers are moved by commercial influence of the drug makers, first because of the low prescription of medicaments by their generic name, second by the low number of medicaments effectively dispensed and then the low concordance between the ones prescribed and the ones included in the lists patterned by Tabatinga and by the State of São Paulo.
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This study presents the results obtained in a field experiment carried out at Glicério, Northwest of São Paulo state, Brazil, whose objective was to analyze changes of selected soil physical properties and water infiltration rates on a Yellow-Red Latosol, under three different management conditions. The experimental design was arranged as completely randomized split-block with twelve treatments, which corresponded to four depths (0-0.05 m; 0.05-0.10 m; 0.10-0.20 m and 0.20-0.40 m) and three conditions of soil use and management with four replications. The soil surface conditions were: conventional tillage (one disking with moulboard plus two levelling passes with harrow), nine months before starting filed experiences; recent conventional tillage (also one disking with moulboard plus two levelling passes with harrow) and native forest. The conventional tillage areas were cropped for about fifteen years with annual cultures. The considered soil general physical properties were: macroporosity, microporosity, total porosity, bulk density, soil moisture and penetration resistance and, in addition; soil water infiltration rates were also recorded. According to our results, differences on general soil physical properties and infiltration rates appeared when both tilled sub-treatments and native forest were compared. Both, plots recently prepared by conventional tillage and those prepared by tillage but left nine months in rest, presented a statistically significant decrease of constant (final) water infiltration rates of 92.72% and 91.91% when compared with native forest plots.
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The mineralogical composition of the soil plow layer (0-20 cm) was analyzed for the following soil suborders (according to the Brazilian soil taxonomy): Neossolo Quartzarênico. Argissolo Vermelho-Amarelo, Cambissolo Háplico and Latossolo Vermelho-Amarelo which samples were collected from different regions of the Ceará State. The present study had the objectives of identifying potential sources of both total and non-exchangeable potassium forms for plants located at the different soil fractions. Then highest content of K occurred in the Cabissolo Háplico soil, including both the total and non-exchangeable K forms. In the Neossolo Quartzarênico. Argissolo Vermelho-Amarelo and Latossolo Vermelho-Amarelo, the highest contents of both forms of potassium were impregnated at the sand fraction. The amount of potassium found in the both sand and silt fractions has its origin in the orthoclase mineral which was detected in the mineralogical analysis. In the clay fractio, the origin of the potassium is illite and a inter-stratified mineral (mica+montmorillonite). As compared with the total content, the amount of non-exchangeable potassium is low for all the four soils. It was more concentrated at clay fraction of the Cambissolo soil. The potassium content sequence in the soil was the following: Cambissolo Háplico > Argissolo Vermelho-Amarelo > Neossolo Quartzarênico > Latossolo Vermelho-Amarelo. The results showed that the distribution of the forms of potassium among the soils differ as a function of the nature of the dominating minerals detected in the mineralogical analysis (illite and orthoclase) which was discussed above.