Organic carbon and nitrogen stocks, pH and bulk density of a Latosol after three sewage sludge applications
01/Jun/2007
The high organic matter content in sewage sludge is one of the reasons for its utilization as soil amendment. This study aimed to evaluate the effect of consecutive sewage sludge applications on the amounts of carbon, total and mineral nitrogen, pH, and bulk density in a Latossol. Two soil layers (0-0,1 and 0,2-0,4 m) were evaluated after three corn cultivations in Jaguariúna (São Paulo State, Brazil), between 1999 and 2001. The treatments consisted of three consecutive applications of two sewage […]
Leaf senescence of common bean plants as affected by soil phosphorus supply
01/Jun/2007
Responses of leaf senescence to P supply could constitute adaptive mechanisms for plant growth under P-limiting conditions. The aim of this study was to evaluate the effects of soil P supply on leaf senescence of common bean (Phaseolus vulgaris L.). Eight P levels, ranging from 5 to 640 mg kg-1 P, were applied to pots containing four bean plants of cultivar Carioca in 10 kg of an Oxic Haplustult soil. Attached leaves were counted weekly, abscised leaves were collected every […]
Redox properties and functional groups of humic acids isolated from organic residues
01/Jun/2007
According to the system conditions, humic acids act as oxidants or as reductants. In natural systems the electron flow is directly associated with humus content and quality. Electrode potential and oxidation capacity inform about the intensity and capacity of the redox systems. In previous studies it has been assumed that free radicals participate in humic acid redox reactions. In our study six humic acids isolated from composed organic residues were titrated with an oxidant (I2) in inert atmosphere and specified […]
Fitting methods and semi-variogram models applied to the study of spatial variability of physical-hydric soil attributes
01/Jun/2007
The spatial variability and spatial dependence structure of physical water soil attributes (total porosity – VTP, saturated hydraulic conductivity – k0, drainable porosity – DP and soil moisture at field capacity – qcc) was evaluated for an Oxisol representative of Ribeirão Marcela watershed, in the Alto Rio Grande domain. Spherical and exponential semi-variograms were fitted by the weighted minimum square (WMS) and maximum likelihood (ML) methodologies. Undisturbed and disturbed physical water samples were collected from the 0-0.15 m layer for […]
Erodibility of a typic hapludox evaluated under field conditions
01/Jun/2007
The term soil erodibility (factor K in the Universal Soil Loss Equation – USLE) expresses the natural susceptibility of a soil to water erosion. The K factor stands for the soil loss rate per unit of rainfall erosivity (factor R in the USLE). Knowledge on the K factor, as well as about the other factors of the USLE, is important to establish soil conservation strategies since they permit the estimation of soil loss rates by water erosion under specific climate, […]
Microbial biomass carbon and nitrogen in response to different management systems cropped with corn in a red Latosol in the Cerrado
01/Jun/2007
The microbial biomass is a living component of the organic matter responsive to changes caused by different soil management systems. The objective of this long-term study was to determine microbial biomass carbon and nitrogen in response to different management systems in a clayey Red Latosol cultivated with corn in the Cerrado. The field experiment was conducted on an experimental area of Embrapa Cerrados, Planaltina, in the Federal District. Eight soil management systems with different implements and periods of crop residue […]
Microbial phosphorus in a soil under no-tillage as affected by soluble phosphorus addition
01/Jun/2007
The phosphorus cycle in the soil is controlled by physicochemical processes, such as adsorption and desorption, and by biological processes, such as immobilization and mineralization. This study was carried out to evaluate the seasonal variation of phosphorus in the soil microbial biomass (Pm) as related to rates and timing of soluble phosphate application. The experiment was carried out in May 2002 on an Oxisol under no-till for seven years, in Ibirubá, in the southern Brazil. Five rates of soluble phosphate […]
Relationship between soil attributes and elemental sulfur oxidation in 42 soil samples from Brazil
01/Jun/2007
The use of elemental S as fertilizer can reduce costs in agriculture, but elemental-S must first be oxidized to sulfate-S to become plant-available. Little information is found in the literature about the capacity of Brazilian soils to oxidize elemental-S. This study was carried out with the objective of determining the oxidation rates of 42 soils samples from different Brazilian states to verify how soil attributes affect oxidation. Samples were collected in the A horizon (0-20 cm layer) and incubated in […]
Recovery of physical attributes of an Ultisol as affected by soil tillage and sowing time in no-tillage
01/Jun/2007
The improvement in the structural soil quality under continuous no-tillage occurs concomitantly to soil (re)acidification. Surface compaction can sometimes occur, owing to machinery traffic, which has to be corrected by soil tilling. In a 12-year experiment under different soil management systems we evaluated the time it takes to recover the initial soil physical attributes that are affected by soil tillage by the occasion of lime reapplication. The experiment was set up on a Rhodic Paleudult (Ultisol) at the Agronomical Experimental […]
Mineralogical attributes of three soils under melon cultivation in the Apodi Tableland, Northeastern Brazil
01/Jun/2007
The present study aimed at characterizing the main soil types under melon crop in the Apodi Tableland, state of Rio Grande do Norte. This investigation focused on the mineralogical soil features as an attempt to generate information for adequate soil and crop management. Three soil types were selected: Typic Haplocambids, Typic Eutrotorrox and Arenic Kandiustults. The mineralogy of sand, silt and clay fractions was evaluated through X ray diffraction analyses and scanning electron microscopy in complementary, undisturbed samples. The mineralogical […]
