A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...
A Look at Amazon Basin Seasonal Dynamics with the Biophysical ... A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...
LATERAL VARIATIONS IN THE CHEMICAL PROPERTIES OF THE TERRAFIRM SOILS, ESECAFLOR EXPERIMENT (CAXIUANÃ, PARÁ STATE)Simone Baía Pereira (MPEG/LBA)Maria de Lourdes Ruivo (MPEG/LBA)The relationships between water exclusion, properties of soil and forest cycle areinvestigated by “The Impact of drought on water and carbon dioxide fluxes from brazilianrain forest – ESECAFLOR project, located in Ferreira Penna Scientific Station (Caxiuanã,Pará). Treatment (B) and control (A) plots were established in the forest. Each plot had fourtrenches (A1, A2, A3, A4 and B1, B2, B3, B4). In A and B plots there are not lateralappreciable changes. In this study were evaluate the seasonal variability from the selectedchemical properties in the surface soils (0-25 cm) the samples were collected the early rainyseason (January /2000) and dry season (Jane/2001). The organic carbon content (plot A)was significantly higher in the rain season, increased diagonally in the both plots. In the dryseason, the organic carbon content is smaller compared with rain season. The observationsin dry period indicate small increase in the pH values. The increase tendency ofexchangeable Ca 2+ and Mg 2+ and pH is contrary between the A and B plots. In dry season,A1 trench showed the low valor of organic carbon (7.05 g/Kg), exchangeables Ca 2+ (0.112cmolc/dm 3 ) and Mg 2+ (0.112 cmolc/dm 3 ) and high value pH (4.7); and B3 trench exhibitedorganic carbon content near to minimal value (5.04 g/Kg) and pH is maximum (4.4).Clearly indicate an association with minimal percentage of humid, 18.6 and 14.7%, to Aand B plots, respectively. These observations, probably, indicate the A1 and B3 trencheshas major altitude, in relation to other trenches, cause higher weathering and aeration.Consequently, fast decomposition of organic matter. The increase pH may be due to theretreat weak acids of the environment, and decrease of the exchangeables cations.
- Page 268: The contribution of pioneer tree sp
- Page 272: Response of photosynthesis to diffe
- Page 276: 1 Trumbore et al., 1996
- Page 280: Effect of Soil Texture on Carbon Dy
- Page 284: Relationship Between Litter Product
- Page 288: Regrowth Biomass Estimation in the
- Page 292: Effects of Interannual Climate Vari
- Page 296: Carbon balance and vegetation dynam
- Page 300: SOIL CARBON STOCKS INFLUENCED BY LI
- Page 304: Drought effects on net primary prod
- Page 308: COARSE WOOD DEBRIS DEPOSITION, DECO
- Page 312: Soil properties and carbon sequestr
- Page 316: Patiño, S. 1,2,a , Mercado, L. 2 ,
- Page 322: Isotopic Signature of Nitrous Oxide
- Page 326: Ecosystem degradation due to fire &
- Page 330: AbstractMulti-temporal Analysis of
- Page 334: ABSTRACT - Second International LBA
- Page 338: Mapping Biomass Loss from Forest Fi
- Page 342: Spatial and Temporal Drivers of Fir
- Page 346: A new method to detect forest fire
- Page 350: Forest Canopy Damage from Selective
- Page 354: AcknowledgementsSupport of this res
- Page 358: Carbon Storage in Soils from Degrad
- Page 362: An improved soil water budget model
- Page 366: PATTERNS OF TREE MORTALITY IN FORES
LATERAL VARIATIONS IN THE CHEMICAL PROPERTIES OF THE TERRAFIRM SOILS, ESECAFLOR EXPERIMENT (CAXIUANÃ, PARÁ STATE)Simone Baía Pereira (MPEG/LBA)Maria de Lourdes Ruivo (MPEG/LBA)The rel<strong>at</strong>ionships between w<strong>at</strong>er exclusion, properties of soil and forest cycle areinvestig<strong>at</strong>ed by “The Impact of drought on w<strong>at</strong>er and carbon dioxide fluxes from brazilianrain forest – ESECAFLOR project, loc<strong>at</strong>ed in Ferreira Penna Scientific St<strong>at</strong>ion (Caxiuanã,Pará). Tre<strong>at</strong>ment (B) and control (A) plots were established in <strong>the</strong> forest. Each plot had fourtrenches (A1, A2, A3, A4 and B1, B2, B3, B4). In A and B plots <strong>the</strong>re are not l<strong>at</strong>eralappreciable changes. In this study were evalu<strong>at</strong>e <strong>the</strong> seasonal variability from <strong>the</strong> selectedchemical properties in <strong>the</strong> surface soils (0-25 cm) <strong>the</strong> samples were collected <strong>the</strong> early rainyseason (January /2000) and dry season (Jane/2001). The organic carbon content (plot A)was significantly higher in <strong>the</strong> rain season, increased diagonally in <strong>the</strong> both plots. In <strong>the</strong> dryseason, <strong>the</strong> organic carbon content is smaller compared <strong>with</strong> rain season. The observ<strong>at</strong>ionsin dry period indic<strong>at</strong>e small increase in <strong>the</strong> pH values. The increase tendency ofexchangeable Ca 2+ and Mg 2+ and pH is contrary between <strong>the</strong> A and B plots. In dry season,A1 trench showed <strong>the</strong> low valor of organic carbon (7.05 g/Kg), exchangeables Ca 2+ (0.112cmolc/dm 3 ) and Mg 2+ (0.112 cmolc/dm 3 ) and high value pH (4.7); and B3 trench exhibitedorganic carbon content near to minimal value (5.04 g/Kg) and pH is maximum (4.4).Clearly indic<strong>at</strong>e an associ<strong>at</strong>ion <strong>with</strong> minimal percentage of humid, 18.6 and 14.7%, to Aand B plots, respectively. These observ<strong>at</strong>ions, probably, indic<strong>at</strong>e <strong>the</strong> A1 and B3 trencheshas major altitude, in rel<strong>at</strong>ion to o<strong>the</strong>r trenches, cause higher we<strong>at</strong>hering and aer<strong>at</strong>ion.Consequently, fast decomposition of organic m<strong>at</strong>ter. The increase pH may be due to <strong>the</strong>retre<strong>at</strong> weak acids of <strong>the</strong> environment, and decrease of <strong>the</strong> exchangeables c<strong>at</strong>ions.