Volume 36, Number 6, 2012
Arbuscular mycorrhiza and plant tolerance to stress
01/Dec/2012
Arbuscular mycorrhizal fungi (AMF) are soil fungi, obligate biotrophic fungi and form the most common mutualistic symbiosis in nature: the arbuscular mycorrhiza (AM). This association occurs on the roots of most plants, promoting improvements in plant growth and development and increasing tolerance and/or plant resistance to several adverse environmental agents. In addition, AMF can be a potential biological control agent of plant diseases. These fungi produce glomalin, a protein that plays a key role in soil stability and in the […]
Total organic carbon, microbial biomass and soil enzyme activity areas of agriculture, forestry and grassland in the middle Valley of Paraíba do Sul River (RJ)
01/Dec/2012
Soil characteristics such as total organic carbon (TOC), microbial biomass and enzymatic activity are influenced by many factors and have been suggested as suitable indicators of changes caused by different land use systems and soil management. The objective of this study was to evaluate the COT, microbial biomass and enzymatic activity of a typical Inceptisol in agricultural, forest and grassland areas in the Middle Valley of the Paraíba do Sul river (RJ). The systems evaluated were: annual agriculture (Agan); perennial […]
Geostatistical simulation for the spatial characterization of iron oxides in different landforms
01/Dec/2012
The clay minerals goethite and hematite are iron oxides serving as indicators of the soil environment, with great influence on the soil physical and chemical properties. Knowledge of spatial patterns of these oxides can help understand the interrelationships of cause and effect with soil properties. In this sense, the quality of the spatial estimates can affect the results and consequently the interpretation of the spatial patterns. This study aimed to evaluate the performance of the geostatistical estimation methods by ordinary […]
Correction of resistance to penetration by pedofunctions and a reference soil water content
01/Dec/2012
The soil penetration resistance is an important indicator of soil compaction and is strongly influenced by soil water content. The objective of this study was to develop mathematical models to normalize soil penetration resistance (SPR), using a reference value of gravimetric soil water content (U). For this purpose, SPR was determined with an impact penetrometer, in an experiment on a Dystroferric Red Latossol (Rhodic Eutrudox), at six levels of soil compaction, induced by mechanical chiseling and additional compaction by the […]
Biomass and decomposition of cover crop residues in monoculture and intercropping
01/Dec/2012
The use of cover crops in autumn/winter, in the Planalto region of Rio Grande do Sul, contributes to the success of the no-tillage system. However, information about the biomass production and decomposition of such species in the region is still scarce, especially for cover crop species in consortium. The experiment was conducted in Não-Me-Toque, RS, on an Oxisol, evaluating nine treatments of four cover crops in monoculture [rye (Secale cereale L.), oat (Avena strigosa Schreb), pea (Pisum sativum subsp. arvense), […]
Structural sustainability of cambisol under different land use system
01/Dec/2012
Incongruous management techniques have been associated with some significant loss of agricultural land to degradation in many parts of the world. Land degradation results in the alteration of physical, chemical and biological properties of the soil, thereby posing a serious threat to sustainable agricultural development. In this study, our objective is to evaluate the changes in a Cambisol structure under six land use systems using the load bearing capacity model. Sampling was conducted in Amazonas Region, Brazil, in the following […]
Physical attributes related to soil compaction under native vegetation of Southern Brazil
01/Dec/2012
The compaction caused by anthropic activities alters the soil physical properties, decreasing productivity and affecting the environment. Many studies on this topic have been conducted in agricultural soils; however there is little information in areas with native vegetation, where, usually, organic matter levels are higher. Thus, it is essential to evaluate the relationship between physical properties related to compaction under these conditions to establish reference values for the revegetation of native grassland or riparian forests. The objective was to relate […]
Pedotransfer functions for the curves of soil resistance to penetration
01/Dec/2012
Pedotransfer functions are regressions used to determine dependent soil properties by independent and easily measurable properties. In this sense, several pedotransfer functions were proposed in the literature, designed to predict the soil resistance to penetration. The purpose of this study was to compare the efficiency of five pedotransfer functions for the penetration resistance curve in the literature, by matching the data obtained from an impact penetrometer (field) and from an electronic penetrometer (laboratory) of a clay Oxisol, under different management […]
The efficiency of different estimation methods of hydro-physical limits
01/Dec/2012
The soil water available to crops is defined by specific values of water potential limits. Underlying the estimation of hydro-physical limits, identified as permanent wilting point (PWP) and field capacity (FC), is the selection of a suitable method based on a multi-criteria analysis that is not always clear and defined. In this kind of analysis, the time required for measurements must be taken into consideration as well as other external measurement factors, e.g., the reliability and suitability of the study […]
Infrared spectroscopy in determination of soil texture
01/Dec/2012
Since the 70s, spectroscopic techniques, especially those with infrared radiation (NIRS -Near Infrared Spectroscopy and DRIFTS – Diffuse Reflectance Fourier Transformed Spectroscopy) have been proposed for inorganic soil analysis, but only few methods found routine use in Brazil so far. This fact is probably due to the difficulty in building calibration models based on multivariate tools with real soil samples that have a complex composition that varies geographically and according to the management. The objective of this study was to […]