Comportamento geoquímico do fósforo em sistemas lacustres tropicais

Considerando a multiplicidade dos impactos ambientais associados às albufeiras pretendeu-se verificar a disponibilidade da utilização, como recurso agrícola, dos sedimentos desenvolvidos sob clima tropical. Estudaram-se duas albufeiras, Três Marias e Tucuruí situadas no Brasil, cujos materiais depositados apresentam forte componente siltosa e argilosa. Possuindo valores de matéria orgânica considerados médios, as amostras têm valores de pH (H20) ácidos, elevados teores de Fe203 e Ah03 e baixa diversidade de minerais argilosos (apenas ilite e caulinite). Apesar das quantidades totais de fósforo serem significativas, os valores da forma disponível deste elemento não ultrapassam o 1%. Através da análise de clusters, correlações de Pearson e fraccionamento químico do fósforo inorgânico, concluiu-se que o elemento que influencia a retenção deste elemento nos sedimentos é o ferro. Embora com baixos teores de fósforo sob forma imediatamente disponível, os sedimentos apresentam boa qualidade para fins agrícolas pois, para diferentes variáveis, ultrapassam os valores médios dos solos minerais. ABSTRACT; considering the diversity of environmental impacts related to dam reservoirs, this study aims at verifying the suitability of sediments accumulated in tropical climates, as agricultural resource. We have studied two Brazilian reservoirs, Três Marias and Tucuruí, whose sediments were classified, respectively, as silty clay and clayey silt. The accumulated material has medium contents of organic matter, acid values of pH(H20), high contents of Fe203 and Al203, and low diversity of clay mineral groups (only illite and kaolinite). Although sediments have significant amounts of phosphorus, the available form of this element never exceeds 1%. Data on statistical analysis of clusters, Pearson correlations and chemical fractionation of inorganic phosphorus, indicates that phosphorus adsorption capacity of sediments is predominantly associated with Fe. Even considering the low levels of the readily available form of phosphorus, for most variables, sediments exceed medium values for mineral soils, making this material advantageous for plant nutrition.

The influence of particles recycling on the geochemistry of sediments in a large tropical dam lake in the Amazonian region, Brazil

The influence of particles recycling on the geochemistry of sediments in a large tropical dam lake in the Amazonian region, Brazil. Article in Journal of South American Earth Sciences 72 · December 2016 DOI: 10.1016/j.jsames.2016.09.012 1st Rita Fonseca 16.85 · Universidade de Évora 2nd Catarina Pinho 3rd Manuela Oliveira 22.6 · Universidade de Évora Abstract As a result of over-erosion of soils, the fine particles, which contain the majority of nutrients, are easily washed away from soils, which become deficient in a host of components, accumulating in lakes. On one hand, the accumulation of nutrients-rich sediments are a problem, as they affect the quality of the overlying water and decrease the water storage capacity of the system; on the other hand, sediments may constitute an important resource, as they are often extremely rich in organic and inorganic nutrients in readily available forms. In the framework of an extensive work on the use of rock related materials to enhance the fertility of impoverish soils, this study aimed to evaluate the role on the nutrients cycle, of particles recycling processes from the watershed to the bottom of a large dam reservoir, at a wet tropical region under high weathering conditions. The study focus on the mineralogical transformations that clay particles undergo from the soils of the drainage basin to their final deposition within the reservoir and their influence in terms of the geochemical characteristics of sediments. We studied the bottom sediments that accumulate in two distinct seasonal periods in Tucuruí reservoir, located in the Amazonian Basin, Brazil, and soils from its drainage basin. The surface layers of sediments in twenty sampling points with variable depths, are representative of the different morphological sections of the reservoir. Nineteen soil samples, representing the main soil classes, were collected near the margins of the reservoir. Sediments and soils were subjected to the same array of physical, mineralogical and geochemical analyses: (1) texture, (2) characterization and semi-quantification of the clay fraction mineralogy and (3) geochemical analysis of the total concentration of major elements, organic compounds (organic C and nitrogen), soluble fractions of nutrients (P and K), exchangeable fractions (cation exchange capacity, exchangeable bases and acidity) and pH(H2O).