-The Rafael Fernandes experimental farm is located in the Alagoinha district, northwest of Mossoró, State of Rio Grande do Norte, Brazil, over two pedogenic formations of different edaphic characteristics, thus needing a more detailed description of its soil types, since this area hosts several experimental fields for researches on agriculture. The objective of this work was to characterize the morphological, physical, chemical and mineralogical features of the most representative soils of this farm, in order to understand its pedogenesis and define its classifications. The whole area was surveyed in order to assess its more representative pedogenic formations. Three soil profiles were classified and described, from which samples were collected in all horizons for physical, chemical and mineralogical analysis. The parent materials and the relief were the determining factors for pedogenic processes of desilication, podzolization and laterization, generating the three main soil types of the area, which were classified up to the 4 th categorical level and described as: Typic Rhodustults (P1), Rhodic Haplustox (P2) and Typic Plinthustalfs (P3).Keywords: Semiarid region. Weathering. Pedogenic processes. Barreiras Group. PEDOGÊNESE E CLASSIFICAÇÃO DE SOLOS DA FAZENDA EXPERIMENTAL "RAFAEL FERNANDES" NO MUNICÍPIO DE MOSSORÓ, RNRESUMO -A fazenda experimental Rafael Fernandes está localizada no distrito de Alagoinha e inserida entre duas pedoformas da região noroeste do município de Mossoró-RN, apresentando características edáficas distintas, o que gera a necessidade de descrições mais detalhadas acerca das classes de solos existentes na área, uma vez que a mesma dispõe de diversos campos experimentais com pesquisas na área de ciências agrárias. Assim, a realização do presente trabalho teve como objetivo a caracterização morfológica, física, química e mineralógica dos solos mais representativos da fazenda a fim de compreender a pedogênese e definir sua classificação. Foram realizadas viagens de reconhecimento de toda a área para a decisão das pedoformas mais representativas e assim definidos três perfis de solo, os quais foram descritos e coletadas as amostras em todos os horizontes para a realização das análises físicas, químicas e mineralógicas. Os resultados permitiram concluir que o material de origem e o relevo foram os fatores determinantes para a ocorrência dos processos pedogenéticos de latolização, podzolização e plintitização, gerando a identificação de três classes de solo principais na Fazenda Experimental que, classificados em 4° nível categórico, definiram-se como: Argissolo Vermelho Distrófico Típico (P1), Latossolo Vermelho Distrófico Argissólico (P2) e Plintossolo Argiluvico Eutrófico Típico (P3).
The unregulated use and increased demand in face of the demographic and economic growth of society caused reduction in the availability of water resources in quantity and quality. In this context, this work was carried out to verify the possibility of producing ornamental sunflower (Helianthus annuus L.) fertirrigated with wastewater from fish culture and its mixtures with tap water. Two experiments were conducted in 2017 in a greenhouse at Federal Rural do University of the Semiarid, in Mossoró, RN, Brazil, according to a completely randomized design with 12 replicates. The treatments consisted of dilutions of the fish's wastewater in tap water (0, 25, 50, 75 and 100%). Determinations of plant biomass and flower characteristics were performed. The statistical analysis of the data consisted of analysis of variance by the F test and regression analysis. The biomass of ornamental sunflower showed significant effect of the fish’s effluent dilutions, but, in general, characteristics of flowers were not influenced. The higher values of the variables of the ornamental sunflower evaluated in the first experiment, which received fertilization, indicate that the effluent did not supply the nutritional needs of the plants. The irrigation of the ornamental sunflower can be carried out with effluent from fish farming when there is another source of nutrients for the crop to produce flowers with satisfactory characteristics.
In Brazil, the state of Rio Grande do Norte has an important coastal zone and coastal Tableland areas along the Barreiras Formation, but there are few studies to locate and characterize soils with cohesive character. Therefore, this work was carried out to characterize pedons in the western and eastern mesoregions of the state, located in the Barreiras Formation and with different climatic conditions. The profile description and sample collection were carried out in March and April 2016. The characteristics of the profile identified were the sequence of horizons and their depth, soil color, texture, structure, consistency, and transition between horizons. The physical analyzes were of soil density and texture. The chemical analyzes consisted of: pH in water and in KCl, contents of available P, Na+, K+, Ca2+, Mg2+, potential acidity, and total organic carbon. Indices obtained were: base sum, effective cation exchange capacity, cation exchange capacity at pH 7.0, base saturation, exchangeable aluminum saturation, and exchangeable sodium percentage. The profiles were classified up to the fourth categorical level. The mineralogical assembly was identified in the clay fraction of the diagnostic horizons. The identification of the minerals was performed by X-ray diffraction. The pedons of the two regions presented distinct characteristics and pedogenesis, occurring laterization in the pedons of the western mesoregion and podzolization in the pedons of the eastern mesoregion, both without presence of cohesive character as a diagnostic attribute.
Um substrato com porosidade e capacidade de retenção de água adequadas possibilita maximizar a produtividade e qualidade das culturas produzidas em recipientes sob ambiente protegido. A fibra de coco é uma ótima alternativa, mas requer manejo cuidadoso da irrigação, podendo ser baseado no monitoramento do teor de água na zona radicular usando tensiômetros. Nesse sentido, objetivou-se com este trabalho determinar a curva de retenção de água em fibra de coco em vasos. A técnica usada foi a remoção de água por evaporação e medição da tensão da água com tensiômetros, com posterior pesagem dos vasos e cálculo do teor de água correspondente por diferença entre massa medida e massa do substrato seco. Um sistema de aquisição de dados foi usado para registrar as leituras dos transdutores de pressão dos tensiômetros. Os dados de tensão, quantidade de água e densidade do substrato foram usados para ajustar as curvas de retenção de água conforme modelos de regressão e o modelo de Van Genuchten. O uso de tensiômetros no substrato fibra de coco possibilitou determinar a curva de retenção de água de maneira rápida e prática, a partir de leituras de tensão quase contínuas entre 12 e 268 hPa, referentes a teores de água entre 0,37 e 0,05 cm3 cm-3. Assim, foi possível ajustar a curva de retenção de forma simples, usando modelos de regressão com elevados coeficientes de determinação. Os parâmetros hídricos obtidos do substrato são menores do que os referidos na literatura e úteis para o manejo adequado da irrigação em recipientes contendo o mesmo substrato.
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