990 resultados para Fruticultura tropical


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Família. Gênero. Espécies. Euterpe oleraceae. Euterpe precatoria. Propagação. Preparo da muda. Plantio e adubação. Tratos culturais. Colheita. Beneficiamento e comercialização.

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2001

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A otimização da rede de estradas secundárias em função das distâncias ideais de arraste não tem sido considerada na elaboração dos planos de manejo de floresta tropical. No Estado do Acre, as florestas com potencial de manejo, possuem diferentes tipologias, volume comercial e potencialmente aproveitáveis por hectare, topografia e solos variados. Isto implicará sempre diferentes densidades ideais de construção de estradas florestais para manejo, tornando necessária a utilização de metodologia que defina o menor custo e dano ao povoamento. Este trabalho tem a finalidade de fornecer suporte técnico à planificação de redes de estradas para o manejo em florestas tropicais, abordando os principais elementos necessários as planejamento e sugerindo uma sistemática de trabalhos para elaboração de um projeto.

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Este trabalho visa basicamente sugerir uma sequência de metodológica de trabalho para o planejamento adequado do arraste mecanizado, baseado no proposto em Braz & Oliveira (1996), e métodos existentes.

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O objetivo do presente trabalho é apresentar um breve relato da situação da fruticultura estadual e despertar o interesse pelo potencial de aproveitamento de diversas fruteiras nativas, no estado do Acre.

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O gênero Citrus L. e afins, especialmente Poncirus Raf., Fortunella Swingle, Microcitrus Swingle, Eremocitrus Swingle e Clymenia Swingle, constituem o que se denomina por citros, em razão de produzirem frutos semelhantes à laranja ou ao limão. Esse complexo grupo de plantas apresenta ampla variabilidade de formas, as quais foram se acumulando ao longo de milênios, seja em razão de seu cultivo desde a Antiguidade, por diversas civilizações, seja em decorrência da preservação pela própria natureza, como consequência da embriogenia nucelar. Os frutos cítricos variam em tamanho, desde os relativamente muito pequenos àqueles muito grandes. Dentre os menores encontram-se os kumquats (Fortunella spp.) e as limas ácidas [C. aurantiifolia (Christm.) Swingle], cujas dimensões dificilmente ultrapassam 5 cm. No extremo oposto estão as toranjas [C. maxima (Burm.) Merr.] e as cidras (C. medica L.), que podem atingir 30 cm em diâmetro ou comprimento.

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Discussion Conclusions Materials and Methods Acknowledgments Author Contributions References Reader Comments (0) Figures Abstract The importance of mangrove forests in carbon sequestration and coastal protection has been widely acknowledged. Large-scale damage of these forests, caused by hurricanes or clear felling, can enhance vulnerability to erosion, subsidence and rapid carbon losses. However, it is unclear how small-scale logging might impact on mangrove functions and services. We experimentally investigated the impact of small-scale tree removal on surface elevation and carbon dynamics in a mangrove forest at Gazi bay, Kenya. The trees in five plots of a Rhizophora mucronata (Lam.) forest were first girdled and then cut. Another set of five plots at the same site served as controls. Treatment induced significant, rapid subsidence (−32.1±8.4 mm yr−1 compared with surface elevation changes of +4.2±1.4 mm yr−1 in controls). Subsidence in treated plots was likely due to collapse and decomposition of dying roots and sediment compaction as evidenced from increased sediment bulk density. Sediment effluxes of CO2 and CH4 increased significantly, especially their heterotrophic component, suggesting enhanced organic matter decomposition. Estimates of total excess fluxes from treated compared with control plots were 25.3±7.4 tCO2 ha−1 yr−1 (using surface carbon efflux) and 35.6±76.9 tCO2 ha−1 yr−1 (using surface elevation losses and sediment properties). Whilst such losses might not be permanent (provided cut areas recover), observed rapid subsidence and enhanced decomposition of soil sediment organic matter caused by small-scale harvesting offers important lessons for mangrove management. In particular mangrove managers need to carefully consider the trade-offs between extracting mangrove wood and losing other mangrove services, particularly shoreline stabilization, coastal protection and carbon storage.

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Tropical cyclones (TCs) are among the most devastating weather systems affecting the United States and Central America (USCA). Here we show that the Interdecadal Pacific Oscillation (IPO) strongly modulates TC activity over the North Atlantic (NA) and eastern North Pacific (eNP). During positive IPO phases, less (more) TCs were observed over NA (eNP), likely due to the presence of stronger (weaker) vertical wind shear and the resulting changes in genesis potential. Furthermore, TCs over NA tend to keep their tracks more eastward and recurve at lower latitudes during positive IPO phases. Such variations are largely determined by changes in steering flow instead of changes in genesis locations. Over the eNP, smaller track variations are observed at different IPO phases with stable, westward movements of TCs prevailing. These findings have substantial implications for understanding decadal to inter-decadal fluctuations in the risk of TC landfalls along USCA coasts.

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© 2015. American Geophysical Union. All Rights Reserved.The role of surface and advective heat fluxes on buoyancy-driven circulation was examined within a tropical coral reef system. Measurements of local meteorological conditions as well as water temperature and velocity were made at six lagoon locations for 2 months during the austral summer. We found that temperature rather than salinity dominated buoyancy in this system. The data were used to calculate diurnally phase-averaged thermal balances. A one-dimensional momentum balance developed for a portion of the lagoon indicates that the diurnal heating pattern and consistent spatial gradients in surface heat fluxes create a baroclinic pressure gradient that is dynamically important in driving the observed circulation. The baroclinic and barotropic pressure gradients make up 90% of the momentum budget in part of the system; thus, when the baroclinic pressure gradient decreases 20% during the day due to changes in temperature gradient, this substantially changes the circulation, with different flow patterns occurring during night and day. Thermal balances computed across the entire lagoon show that the spatial heating patterns and resulting buoyancy-driven circulation are important in maintaining a persistent advective export of heat from the lagoon and for enhancing ocean-lagoon exchange.

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The Moorea Coral Reef Long Term Ecological Research project funded by the US National Science Foundation includes multidisciplinary studies of physical processes driving ecological dynamics across the fringing reef, back reef, and fore reef habitats of Moorea, French Polynesia. A network of oceanographic moorings and a variety of other approaches have been used to investigate the biological and biogeochemical aspects of water transport and retention processes in this system. There is evidence to support the hypothesis that a low-frequency counterclockwise flow around the island is superimposed on the relatively strong alongshore currents on each side of the island. Despite the rapid flow and flushing of the back reef, waters over the reef display chemical and biological characteristics distinct from those offshore. The patterns include higher nutrient and lower dissolved organic carbon concentrations, distinct microbial community compositions among habitats, and reef assemblages of zooplankton that exhibit migration behavior, suggesting multigenerational residence on the reef. Zooplankton consumption by planktivorous fish on the reef reflects both retention of reef-associated taxa and capture by the reef community of resources originating offshore. Coral recruitment and population genetics of reef fishes point to retention of larvae within the system and high recruitment levels from local adult populations. The combined results suggest that a broad suite of physical and biological processes contribute to high retention of externally derived and locally produced organic materials within this island coral reef system. © 2013 by The Oceanography Society. All rights reserved.