RESUMO

Banana is a staple food and a major export commodity in the tropics. However, banana production systems are affected by the plant-soil relationships, where properties such as quality and quantity of soil organic matter play an important role in the dynamics of soil physical properties. In order to evaluate the effect of the soil organic carbon (SOC) content and its distribution in the water-stable of soil aggregates (WAS), and the physical fractions of the macro-organic matter, a study was conducted in lacustrine soils under Banana cv. 'Grand Nain' in Venezuela. Soil sampling was carried out in two batches differentiated by their textural class and crop production. A completely randomized design under a directed random sampling technique was carried out. In each condition, 12 composite samples were taken at depths 0-5 and 5-10 cm, respectively. WAS were separated into micro (< 250 µm) and macroaggregates (> 250 µm). Also, physical fractionation by size-density of the macro-organic matter into light (LF), intermediate (IF), and heavy (HF) fraction using a silica gel solution, and SOC, were determined and correlated with banana yield and other agronomic traits. A major proportion of aggregates > 250 µm were found in both conditions and depths. Organic Carbon within soil aggregates ranged between 29.7 and 35.3 g kg-1. The HF was superior to IF and LF; however, its C content was higher in the LF. The results allow inferring that the stability conferred to these soils is primarily associated with the presence of the snail, which shares the same size as the aggregates studied. High yields are associated with high C content in stable aggregates, as well as in the most labile fractions of macro-organic matter. These results highlight the importance of the use of organic fertilizers less recalcitrant as a strategy for sustainable management of banana cultivation.

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RESUMO

Mineral deficiencies in soil-plant-animal relations are linked to chemical properties and reproductiveproblems in grazing animals. The objective of this study was to determine the dynamics of K, Ca, and Mgin the green leaf biomass of two types of introduced forages, Brachiaria dyctioneura (Bd) and Centrosema macrocarpum (Cm), compared to the natural vegetation of the neotropical savannah (NS) in an agricultural ecosystem. The three types of vegetation, associated with the corn crop, served as livestock feed during the dry season. The soil’s nutrient content (0-15 cm depth), the production and nutritional dynamics of green leaf biomass, and leaf/stem relationships in the fields during the grazing period were determined. In the corn crop-livestock agroecosystem, K decreased (%) in concentration as the grazing period progressed, presenting the following trend: Bd>Cm>NS. The dynamics of Ca and Mg in green leaf biomass increased slightly (p<0.05) by the end of the grazing period for Bd and Cm, in contrast to a significant decrease in the natural vegetation of the savannah. The concentration of K in the soil did not reveal significant differences between ground cover and NS plants, and the soils under Cm evidenced thehighest percentage of Ca. A higher percentage of Mg was observed in the soil planted with Cm. For the three types of vegetation, an improvement was observed in the nutritional quality of the forage and soil and in the yield (kg/ha). These findings are valuable contributions within the context of production in savannas and to forage quality for livestock.

Deficiências minerais no eixo solo-planta-animal estão relacionadas as propriedades químicas e estão ligadas a problemas reprodutivos em animais em pastejo. O objetivo deste estudo foi determinar a dinâmica de K, Ca e Mg na biomassa foliar verde de dois tipos de forrageiras introduzidas (Brachiaria dyctioneura (Bd) e Centrosema macrocarpum (Cm)) em relação à vegetação natural do cerrado (NS) em um ecossistema agrícola. Os três tipos de vegetação, associados ao cultivo do milho, serviam de ração para o gado durante a estação seca. Foram determinados o conteúdo de nutrientes no solo (0-15 cm de profundidade), a produção de biomassa de folhas verdes e sua dinâmica nutricional e as relações folha-colmo nas lavouras durante o pastejo. No agroecossistema milho-pecuária, o K apresentou redução (%) em sua concentração com o avanço do período de pastejo, apresentando a seguinte tendência: Bd> Cm> NS. A dinâmica do Ca e Mg na biomassa foliar verde aumentou ligeiramente (p <0,05) ao final do período de pastejo em Bd e Cm, contrastando com uma diminuição significativa na vegetação natural do cerrado. A concentração de K no solo não apresentou diferenças significativas entre as plantas de cobertura e o NS, sendo que os solos sob Cm apresentaram a maior porcentagem de Ca. Uma maior porcentagem de Mg foi observada no solo plantado com Cm. Nos três tipos de vegetação examinados, observou-se melhora na qualidade nutricional da forragem e solo e na produtividade (kg/ha). Essas descobertas são contribuições valiosas nos contextos de produção das savanas e na qualidade da forragem para o gado.

Assuntos

RESUMO

Mineral deficiencies in soil-plant-animal relations are linked to chemical properties and reproductiveproblems in grazing animals. The objective of this study was to determine the dynamics of K, Ca, and Mgin the green leaf biomass of two types of introduced forages, Brachiaria dyctioneura (Bd) and Centrosema macrocarpum (Cm), compared to the natural vegetation of the neotropical savannah (NS) in an agricultural ecosystem. The three types of vegetation, associated with the corn crop, served as livestock feed during the dry season. The soils nutrient content (0-15 cm depth), the production and nutritional dynamics of green leaf biomass, and leaf/stem relationships in the fields during the grazing period were determined. In the corn crop-livestock agroecosystem, K decreased (%) in concentration as the grazing period progressed, presenting the following trend: Bd>Cm>NS. The dynamics of Ca and Mg in green leaf biomass increased slightly (p<0.05) by the end of the grazing period for Bd and Cm, in contrast to a significant decrease in the natural vegetation of the savannah. The concentration of K in the soil did not reveal significant differences between ground cover and NS plants, and the soils under Cm evidenced thehighest percentage of Ca. A higher percentage of Mg was observed in the soil planted with Cm. For the three types of vegetation, an improvement was observed in the nutritional quality of the forage and soil and in the yield (kg/ha). These findings are valuable contributions within the context of production in savannas and to forage quality for livestock.(AU)

Deficiências minerais no eixo solo-planta-animal estão relacionadas as propriedades químicas e estão ligadas a problemas reprodutivos em animais em pastejo. O objetivo deste estudo foi determinar a dinâmica de K, Ca e Mg na biomassa foliar verde de dois tipos de forrageiras introduzidas (Brachiaria dyctioneura (Bd) e Centrosema macrocarpum (Cm)) em relação à vegetação natural do cerrado (NS) em um ecossistema agrícola. Os três tipos de vegetação, associados ao cultivo do milho, serviam de ração para o gado durante a estação seca. Foram determinados o conteúdo de nutrientes no solo (0-15 cm de profundidade), a produção de biomassa de folhas verdes e sua dinâmica nutricional e as relações folha-colmo nas lavouras durante o pastejo. No agroecossistema milho-pecuária, o K apresentou redução (%) em sua concentração com o avanço do período de pastejo, apresentando a seguinte tendência: Bd> Cm> NS. A dinâmica do Ca e Mg na biomassa foliar verde aumentou ligeiramente (p <0,05) ao final do período de pastejo em Bd e Cm, contrastando com uma diminuição significativa na vegetação natural do cerrado. A concentração de K no solo não apresentou diferenças significativas entre as plantas de cobertura e o NS, sendo que os solos sob Cm apresentaram a maior porcentagem de Ca. Uma maior porcentagem de Mg foi observada no solo plantado com Cm. Nos três tipos de vegetação examinados, observou-se melhora na qualidade nutricional da forragem e solo e na produtividade (kg/ha). Essas descobertas são contribuições valiosas nos contextos de produção das savanas e na qualidade da forragem para o gado.(AU)

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Substitution of native savanna by Pinus caribaea (Pinaceae) plantations in Venezuela: effect on parameters that indicated changes in soil carbon content. A great extension (615 000 ha) of native savannas of the eastern plains of Venezuela have been replaced by plantations of Pinus caribaea var. hondurensis; however, only scarce information exists about the impact of this land use on carbon dynamics in soils. We studied the effect of temporal variability and the substitution on the total organic carbon (TOC), water-soluble carbon (WSC), microbial biomass C (Cmic), basal respiration (BR), microbial metabolic quotient (qCO2) and Cmic/Corg ratio. Selected chemical properties and biological parameters of soils were measured under 3 and 29 year old forest plantations of P. caribaea and an adjacent native savanna which was considered the control. At each site, nine soil composite samples were collected (0-10 cm depth). The studied parameters did not show a defined pattern in relation to temporal variability. Higher carbon preservation occurs in soil microbial biomass under pine plantations. The basal respiration rate and qCO2 suggests that there is a more efficient microbial carbon utilization in the plantations. The Cmic/Corg ratio shows that the microbial biomass has an important stock of soil carbon in pine plantations. The conversion of savannas to pine plantations can increase soil carbon in the eastern plains of Venezuela, but this must be balanced with the ecological importance of natural savannas ecosystems. Rev. Biol. Trop. 56 (4): 2041-2053. Epub 2008 December 12.

Una gran extensión (615000 has) de las sabanas nativas de los Llanos Orientales de Venezuela está siendo reemplazada por plantaciones de Pinus caribaea var. hondurensis; sin embargo, hasta ahora existe escasa información sobre el impacto de este manejo del suelo sobre los parámetros indicadores de la dinámica del carbono en el suelo. El objetivo de esta investigación fue determinar el efecto de la variabilidad temporal y la sustitución sobre el contenido de carbono orgánico total (COT), carbono hidrosoluble (CHS), carbono microbiano (Cmic), respiración basal (RB), cociente metabólico microbiano (qCO2) y la relación Cmic/Corg. Las propiedades químicas y parámetros biológicos seleccionados fueron determinados en plantaciones de P. caribaea de 3 y 29 años de edad y en una sabana nativa adyacente a estas plantaciones, la cual fue considerada como control. En cada sitio de muestreo recolectamos nueve muestras compuestas (0-10 cm de profundidad). Los parámetros estudiados no mostraron un patrón definido in relación a la variabilidad temporal. Hay mayor preservación del carbono dentro de la biomasa microbiana presente en suelos de Uverito en plantaciones de pinos. La tasa de respiración basal y el cociente metabólico indican que en estos suelos existe una comunidad microbiana poco activa, la cual es más eficiente en la utilización del carbono en las plantaciones de pino. La relación Cmic/Corg indica que en las plantaciones la biomasa microbiana constituye una importante reserva del carbono en el suelo. La sabana nativa a plantaciones de pino caribeño en estos suelos puede ser considerada un manejo efectivo para incrementar la calidad del suelo en los llanos orientales de Venezuela, siempre y cuando se tome en cuenta la importancia ecológica de las sabanas.

Assuntos

RESUMO

A great extension (615,000 ha) of native savannas of the eastern plains of Venezuela have been replaced by plantations of Pinus caribaea var. hondurensis; however, only scarce information exists about the impact of this land use on carbon dynamics in soils. We studied the effect of temporal variability and the substitution on the total organic carbon (TOC), water-soluble carbon (WSC), microbial biomass C (Cmic), basal respiration (BR), microbial metabolic quotient (qCO2) and Cmic/Corg ratio. Selected chemical properties and biological parameters of soils were measured under 3 and 29 year old forest plantations of P. caribaea and an adjacent native savanna which was considered the control. At each site, nine soil composite samples were collected (0-10 cm depth). The studied parameters did not show a defined pattern in relation to temporal variability. Higher carbon preservation occurs in soil microbial biomass under pine plantations. The basal respiration rate and qCO2 suggests that there is a more efficient microbial carbon utilization in the plantations. The Cmic/Corg ratio shows that the microbial biomass has an important stock of soil carbon in pine plantations. The conversion of savannas to pine plantations can increase soil carbon in the eastern plains of Venezuela, but this must be balanced with the ecological importance of natural savannas ecosystems.

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RESUMO

Las sabanas de Sudamérica con una superficie de 269×106ha extendidas en Brasil, Colombia, Venezuela, Guyana y Bolivia representan una de las mayores extensiones de tierra con potencial para la producción agrícola, constituyéndose en la principal alternativa para evitar la expansión agrícola hacia áreas de mayor fragilidad ecológica. Hasta hace unos 40 años estas sabanas estuvieron muy poco afectadas por la actividad antrópica, dedicándose principalmente a la ganadería extensiva. En los últimos 40 años las pasturas nativas de bajos requerimientos nutricionales están siendo reemplazadas por pastos africanos principalmente de los géneros Brachiaria y Andropogon. Igualmente, ha ocurrido una reforestación extensiva para producción de madera y papel con especies introducidas de Pinos y Eucaliptos que se adaptan muy bien a las condiciones agroclimáticas del trópico bi-estacional. La introducción de pastos y de cultivos anuales y perennes en sabanas ha sido posible solo, bajo un esquema de fertilización (N, P, K y encalado). Aunque las modificaciones al paisaje introducidas por los nuevos usos de la tierra son ahora en sitios alejados de los grandes centros urbanos y relativamente poco perceptibles, si se toma en consideración las grandes extensiones de tierras de sabanas que están siendo afectadas y las que lo serán por formar parte de proyectos agrícolas, será inevitable una modificación profunda de esos biomas. En este trabajo se hace una revisión preliminar comparativa del proceso de colonización agrícola en los llanos y cerrados. En la necesidad de generar indicadores ligados a los procesos biogeoquímicos afectados, se presentan tres estudios de casos para sabanas venezolanas

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Se presenta un modelo conceptual del funcionamiento de suelos de los Llanos Centrales Venezolanos, basado en las relaciones de estructura del suelo y de las fracciones activas y estabilizadas de la materia orgánica, que muestra como cambian los procesos del suelo según el manejo agronómico. se consideran dos tipos de labranzas constrastantes, la siembra directa sin labranza y con presencia de una cobertura vegetal, y la labranza convencional con fuerte mecanización para romper el suelo y enterrar cualquier tipo de cobertura o residuo. Se consideran variables externas (labranza y coberturas), variables de estado (fracciones de materia orgánica) y los procesos involucrados. Dada la acidez de los suelos, su baja fertilidad con limitaciones para el uso agrícola, y su uso cada vez mayor para producción de cereales, en especial maíz, se discuten los cambios en las fracciones de la materia orgánica por la intensidad de la labranza y la ubicación de los residuos vegetales, aspectos que influyen en la producción de CO² contribuyendo al efecto invernadero y que por otra parte, pueden intensificar los procesos de erosión y pérdida de nutrimientos, agravando los problemas de fertilidad y de degradación de los suelos. El sistema convencional de labranza aumenta la liberación de CO²e intensifica la degradación del suelo, disminuyendo la materia orgánica. Alternativamente, la siembra directa es conservacionista e incrementa los compartimientos activos y lentos que son fuente potencial de nutrimientos aumentando la fertilidad a mediano plazo, los procesos de descomposición microbiana son más lentos y las emisiones de CO² más bajas. El modelo de siembra directa es parecido al modelo de sabana virgen, tanto en las variables de estado relacionadas con la conservación como en los procesos de pérdida o conservación, siendo una alternativa de manejo que permite el uso más sostenible de los suelos de la sabana

Assuntos