Sediment Morphology, Distribution, and Recent Transport Dynamics in a Reforested Fragment
01/Aug/2017
Abstract Erosion generates large amounts of sediment, which may be deposited at the site of origin, on the slope of a hill, or along waterways. The transportability of each type of sediment by runoff and its potential for subsequent deposition largely depends on its morphological features and particle size distribution. The aim of this study is to describe and characterize the morphology and micromorphology of sediments deposited in a reforested area and to understand the dynamics of the transport process. […]
Water retention and availability in soils of the State of Santa Catarina-Brazil: effect of textural classes, soil classes and lithology
01/Dec/2013
The retention and availability of water in the soil vary according to the soil characteristics and determine plant growth. Thus, the aim of this study was to evaluate water retention and availability in the soils of the State of Santa Catarina, Brazil, according to the textural class, soil class and lithology. The surface and subsurface horizons of 44 profiles were sampled in different regions of the State and different cover crops to determine field capacity, permanent wilting point, available water […]
Effectiveness of fused magnesium potassium phosphate for marandu grass
01/Dec/2009
The current high price of KCl and great dependence on importation to satisfy the Brazilian demand indicate the need for studies that evaluate the efficiency of other K sources, particularly those based on domestic raw material. For this purpose, a greenhouse experiment was conducted with samples of a sandy clay loam Typic Haplustox, in a completely randomized 4 x 3 x 2 factorial design: four K rates (0, 60, 120, and 180 mg kg-1), three sources (potassium chloride (KCl), fused […]
Effect of soil grinding on available phosphorus content by Mehlich-1, bead and membrane ion exchange resins
01/Jun/2008
The ion exchange resin method used in some laboratories in Brazil requires soil grinding for the determination of available P. As a consequence of grinding, the extraction of internal labile P in aggregates is expected, increasing the concentration of available-P. On the other hand, finer grinding increases the exposure of soil particle surface, which creates additional sites for further P adsorption. The aim of this study was to evaluate extraction efficiency available-P by Mehlich-1, and anion exchange resin in beads […]
Quaternary evolution, particle distribution in soils and sedimentary environment in mangroves in São Paulo State, Brazil
01/Aug/2007
Particle distribution in soil or sediments of coastal plains contributes to the understanding of the sedimentation processes in estuaries. It is an important attribute for applications in studies of palaeoenvironmental reconstruction, geochemical cycles and environmental pollution such as heavy metal and oil spill contamination, which are relatively common in these sites due to human impact. With the objective of characterizing the sedimentary environments according to the particle size and the process of quaternary evolution, 14 mangroves along the São Paulo […]
Spatial variability of soil aggregation evaluated by fractal geometry and geostatistics
01/Feb/2004
This work explored the applicability of the fractal theory for studies into space variability of soil aggregation. Fractal geometry has become a model for soil size particle distribution. The distribution of soil aggregates in terms of its mass was obtained, and model parameters such as the fractal dimension D, which is a representative measure of the soil fragmentation (the larger its value, the larger the fragmentation), and the largest aggregate size RL were defined as descriptive tools for soil aggregation. […]
Reactivity of a slag in a distrofic red latosol
01/Feb/2004
The present study investigated the reactivity of a slag from steelworks in different particle size fractions, applied on an acid dystrophic Red Latosol, under laboratory conditions, in a 4 x 3 + 2 factorial scheme in four replications. Four particle sizes (material retained in the ABNT 5-10; 10-20; 20-50, and < 50 sieves), three doses of slag (0.00, 5.04, and 10.08 t ha-1, corresponding to 0.00, 1.01, and 2.02 g in 0.40 dm3 of soil per cup) and two control […]
