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Pre- and post-harvest fine root growth in Eucalyptus grandis stands installed in sandy and loamy soils

Por: Miranda Mello, Sergio Luis de.
Colaborador(es): Moraes Goncalves, José Leonardo de autor/a. Department of Forest Sciences, University of Sao Paulo, Brazil | Gava, José Luiz autor/a. Cia. Suzano of Cellulose and Paper, Brazil.
Tipo de material: TextoTextoEditor: Ámsterdam (Países Bajos) Elsevier 2007Descripción: 10 páginas : 8 ilustraciones, 4 tablas.ISSN: 0378-1127.Tema(s): EUCALYPTUS GRANDIS | RAICES | SISTEMA RADICULAR | CRECIMIENTO | COSECHA | TIPOS DE SUELOS | MEDICION | MODELOS | ECUACIONES ALOMETRICAS | ALOMETRIA | AGRICULTURA | ARBOLES | ROOTS | ROOT SYSTEMS | GROWTH | HARVESTING | SOIL TYPES | MEASUREMENT | MODELS | FORESTS | TREES | BRASILRecursos en línea: Haga clic para acceso en línea Resumen: Information about fine root dynamics before and after harvest is scarce in eucalypt plantations. Knowledge of root system functioning is important to achieve sustainable production of these fast-growing species. This work evaluated fine root turnover in 9-year-old Eucalyptus grandis stands growing on a loamy soil (RED) and in a sandy soil (QTZ). On each soil type, the experimental area was divided into three plots that corresponded to the following time sequence: mature forest before harvesting (MF), after harvesting in summer (HS) and after harvesting in winter (HW). Fine roots (diameter < 3 mm) were sampled by sequential coring. Root length was obtained by imaging processing, distinguishing fine roots with diameter < 1 mm (FR1) and diameter between 1 and 3 mm (FR2). Fine root decomposition was estimated with litter bags incubated in three plots per soil. Root length density was higher for FR1 in QTZ than in RED for all plot types. There was a significant seasonal difference in FR1 density (FRD1) at a depth of 0–10 cm in RED (from 2.3 to 4.4 cm cm−3) and QTZ (from 5.7 to 8.2 cm cm−3), in winter and summer, respectively. Fine root dynamics was significantly altered after harvesting, mainly in the surface layer in both soils. An approx. 50% decrease in FRD1 was observed 60 days after harvesting in the two soil types. Root mass loss in litter bags was faster in RED than in QTZ. Decomposition of fine roots was faster after harvesting, which was directly related to altered environmental conditions (water availability, soil temperature).
Tipo de ítem Ubicación actual Colección Signatura Estado Fecha de vencimiento Código de barras
Analítica Analítica Biblioteca Conmemorativa Orton
Colección CATIE Disponible BCO22048572

Bibliografía páginas 194-195

Information about fine root dynamics before and after harvest is scarce in eucalypt plantations. Knowledge of root system functioning is important to achieve sustainable production of these fast-growing species. This work evaluated fine root turnover in 9-year-old Eucalyptus grandis stands growing on a loamy soil (RED) and in a sandy soil (QTZ). On each soil type, the experimental area was divided into three plots that corresponded to the following time sequence: mature forest before harvesting (MF), after harvesting in summer (HS) and after harvesting in winter (HW). Fine roots (diameter < 3 mm) were sampled by sequential coring. Root length was obtained by imaging processing, distinguishing fine roots with diameter < 1 mm (FR1) and diameter between 1 and 3 mm (FR2). Fine root decomposition was estimated with litter bags incubated in three plots per soil. Root length density was higher for FR1 in QTZ than in RED for all plot types. There was a significant seasonal difference in FR1 density (FRD1) at a depth of 0–10 cm in RED (from 2.3 to 4.4 cm cm−3) and QTZ (from 5.7 to 8.2 cm cm−3), in winter and summer, respectively. Fine root dynamics was significantly altered after harvesting, mainly in the surface layer in both soils. An approx. 50% decrease in FRD1 was observed 60 days after harvesting in the two soil types. Root mass loss in litter bags was faster in RED than in QTZ. Decomposition of fine roots was faster after harvesting, which was directly related to altered environmental conditions (water availability, soil temperature).

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