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 ...

22.08.2015 Views

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.

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.

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