Abstract:This study investigates the effect of conventional tillage and application of the monoculture of sugar cane on soil health. Variables like density, moisture, texture, consistency limits, and preconsolidation stress were taken as indicators of soil quality. The measurements were made at a 120 × 120 m field cropped with sugar cane under conventional tillage. The objective of this work was to characterize the soil and to study the spatial dependence of the physical and mechanical attributes. Then, undisturbed soi… Show more
“…According to Rossetto et al (2010), sugarcane monoculture leads to biodiversity loss and affects local and regional fauna and flora. Furthermore, soil tillage is traditionally with use of various agricultural machinery mainly made with disc plows, dish harrows and subsoilers (Portilho et al, 2011;Tavares et al, 2015;Surendran et al, 2016) that negatively affect soil aggregation and reduce biological activity (Benito et al, 2008). In addition to modifying soil physico-chemical characteristics, sugarcane cultivation also produces environmental chemical contamination and soil compaction (Iwai et al, 2008;Nurhidayati et al, 2012;Siqueira et al, 2013).…”
Soil macrofauna organisms are recognized as ecological indicators of soil management practices. Sugarcane monoculture can have negative impacts on soil, including biodiversity loss, which should be evaluated. In that sense, the aim of this was to determine the diversity macrofauna under sugarcane (Saccharum spp.) annual growth cycle (2012-2013) comparing two different natural vegetation areas (Sandbank and Atlantic forest). The study areas are located at Usina Santa Teresa in Goiana municipality, in Zona Mata Norte of the Pernambuco State (Brazil). Soil macrofauna samples were collected in January, April and August 2013. In order to collect soil macrofauna samples, 5 pitfall traps were placed in the field for 7 days. Descriptive statistics and biodiversity indices were used to carry out data analysis. The presence and biodiversity indices were affected by the hydrological regime. Sugarcane harvest with straw burning initially promoted soil macrofauna taxa better adapted to system drastic changes. Moreover, as sugarcane growth year went by, soil macrofauna biodiversity indices similar to those reported at natural vegetation areas (Sandbank and Atlantic Forest) were observed.
“…According to Rossetto et al (2010), sugarcane monoculture leads to biodiversity loss and affects local and regional fauna and flora. Furthermore, soil tillage is traditionally with use of various agricultural machinery mainly made with disc plows, dish harrows and subsoilers (Portilho et al, 2011;Tavares et al, 2015;Surendran et al, 2016) that negatively affect soil aggregation and reduce biological activity (Benito et al, 2008). In addition to modifying soil physico-chemical characteristics, sugarcane cultivation also produces environmental chemical contamination and soil compaction (Iwai et al, 2008;Nurhidayati et al, 2012;Siqueira et al, 2013).…”
Soil macrofauna organisms are recognized as ecological indicators of soil management practices. Sugarcane monoculture can have negative impacts on soil, including biodiversity loss, which should be evaluated. In that sense, the aim of this was to determine the diversity macrofauna under sugarcane (Saccharum spp.) annual growth cycle (2012-2013) comparing two different natural vegetation areas (Sandbank and Atlantic forest). The study areas are located at Usina Santa Teresa in Goiana municipality, in Zona Mata Norte of the Pernambuco State (Brazil). Soil macrofauna samples were collected in January, April and August 2013. In order to collect soil macrofauna samples, 5 pitfall traps were placed in the field for 7 days. Descriptive statistics and biodiversity indices were used to carry out data analysis. The presence and biodiversity indices were affected by the hydrological regime. Sugarcane harvest with straw burning initially promoted soil macrofauna taxa better adapted to system drastic changes. Moreover, as sugarcane growth year went by, soil macrofauna biodiversity indices similar to those reported at natural vegetation areas (Sandbank and Atlantic Forest) were observed.
“…So, these machines must apply pressures to the soil between 275 and 172 kPa in the friability region (0.19-0.31 kg kg −1 ), respectively, to avoid soil compaction. Reference [15], evaluating preconsolidation pressure in Acrisol under sugarcane cultivation, concluded that the load limit machines apply, aiming to remain within the soil support capacity, 126.28 kPa for a moisture content of 0.10 kg kg −1 or >75.70 kPa for moisture of 0.19 kg kg −1 .…”
Section: Comparison Of Models Between Layers Within the Managementmentioning
confidence: 99%
“…This indicates that specific management regions of σ p may be monitored by soil water content and σ p mapping enables the identification of management limits. Reference [15] also found spatial variability structure in sugarcane soil and highlighted that preconsolidation stress maps may indicate areas that support heavier equipment and areas that can tolerate only lighter vehicles before further compaction occurs. Soil compaction susceptibility becomes critical under excess water in the soil, reducing its load-bearing capacity [7,10,15,20].…”
Section: Spatial Variability Of Preconsolidation Pressurementioning
confidence: 99%
“…On the other hand, the preconsolidation pressure can be employed to measure soil structural sustainability, estimate the history of the stress on the soil, and assess its loadbearing capacity [5,10,15,16]. Lower loads than the preconsolidation pressure produces elastic or recoverable deformations, while higher pressures generate plastic or nonrecoverable deformations and reflect their susceptibility to compaction [17].…”
The change in land use and the expansion of mechanized sugarcane production systems have led to an increase in soil compaction levels. Preconsolidation pressure may be used as a useful measure for soil mechanical state, management, and planning of mechanization systems. This study aimed to assess the soil compressive behavior, soil physical properties, and spatial variability of preconsolidation pressure of an Oxisol in sugarcane fields under burned harvest and mechanized harvest and the effects of land use change. The physical soil attributes (granulometry, soil water content, bulk density, total porosity, and macro and microporosity) and preconsolidation pressure were evaluated at 0.00–0.10-m, 0.10–0.20-m, and 0.20–0.30-m layers. The soil load-bearing capacity models were constructed from σp values for soil water contents. We mapped the assessed soil attributes from crossing points in a sampling mesh with regular 10 m intervals in each area and evaluated them via geostatistics. Land-use change towards sugarcane production systems promoted soil compaction. The mechanized harvesting system increased the soil load-bearing capacity in the water range corresponding to the friability region in subsurface layers. The preconsolidation pressure and soil water content exhibited spatial dependence in the sugarcane areas, regardless of the management system employed in the harvesting operations.
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