scholarly journals Quality No-tillage System: The Importance of the Use of Cover Species in Reducing Compaction and Soil and Water Losses Due to Erosion

2019 ◽  
Vol 11 (2) ◽  
pp. 263
Author(s):  
Bruna de Villa ◽  
Deonir Secco ◽  
Luciene Kazue Tokura ◽  
Aracéli Ciotti de Marins ◽  
Pablo Chang ◽  
...  
Keyword(s):  
Surface Runoff ◽  
Soil Structure ◽  
Rainfall Intensity ◽  
Quality Management System ◽  
Water Infiltration ◽  
Effective Control ◽  
No Tillage ◽  
Water Losses ◽  
Tillage System ◽  
Soil And Water

Water and soil losses due to surface runoff depend on rainfall intensity and periods, vegetation cover, slope, and ramp length, in addition to conservation practices. The implementation of a quality planting system for the effective control of erosion while avoiding the disintegration of the soil structure by the direct impact of dropping is of paramount importance. Nevertheless, the current no-tillage system has led to the emergence of compacted layers in the soil, which reduce water infiltration, favoring surface runoff. Thus, it is necessary to optimize the use of soil cover species, aiming at reducing compaction and, subsequently, losses of water and soil that flow superficially. The purpose of this study is to highlight the importance of using a quality management system to reduce soil and water losses due to erosion caused by compaction. Furthermore, it is hoped that the study may contribute to the guidance of the best use and management of the soil for farmers.

scholarly journals Soil and Water Loss Rates in Oxisols Under No-tillage System in Western Paraná, Brazil

2018 ◽  
Vol 10 (10) ◽  
pp. 132
Author(s):  
Luana Salete Celante ◽  
Deonir Secco ◽  
Aracéli Ciotti de Marins ◽  
Daniela Trentin Nava ◽  
Flávio Gurgacz ◽  
...  
Keyword(s):  
Water Loss ◽  
Soil Loss ◽  
No Tillage ◽  
Linear Regression Models ◽  
Water Losses ◽  
Soil And Water Loss ◽  
Tillage System ◽  
Soil Losses ◽  
Soil And Water ◽  
Loss Rates

The objective of work was to quantify soil and water loss rates as a function of slope variation, correlating these rates with soybean yield. In addition to developing multiple linear regression models that associate water and soil loss rates in function of their physical attributes. The experiment was conducted in an Oxisols under a no-tillage system. The experiment was carried out in Cascavel, PR, Brazil. Four slopes (3.5%; 8.2%; 11.4% and 13.5%) were considered as treatments. The water and soil loss rates were monitored in the rainfall occurring during the crop development cycle. The water drained in each plot was collected in gutters made of polyvinyl chloride and stored in containers for the quantification of soil and water losses. The stepwise backward method was used to identify the variables that had a significant influence on water and soil losses. The unevenness of the terrain did not influence the soil and water loss rates. The maximum soil and water losses during the soybean cycle were, respectively, 0.01962 Mg ha-1 and 4.07 m3 ha-1. The maximum soil and water losses occurred when the precipitation volume was up to 82 mm. Soil and water losses showed a higher correlation with macroporosity and bulk density. Soybean grain yield showed a higher linear correlation with water, and soil loss and was higher at the slopes of 8.2% and 13.4%. The low water and soil losses demonstrate the soil capacity, managed under a no-tillage system, to minimize environmental impacts.

scholarly journals PERDAS DE SOLO E DE ÁGUA EM DIFERENTES SISTEMAS DE MANEJO EM LATOSSOLO VERMELHO

Nativa ◽  
2019 ◽  
Vol 7 (1) ◽  
pp. 64
Author(s):  
Stanley Vaz dos Santos ◽  
Eva De Melo Ferreira ◽  
Nori Paulo Griebeler ◽  
Wilson Mozena Leandro
Keyword(s):  
Soil Loss ◽  
Management Systems ◽  
No Tillage ◽  
Conventional System ◽  
Water Losses ◽  
Erosion Models ◽  
Tillage System ◽  
Second Year ◽  
Soil Losses ◽  
Soil And Water

O objetivo foi comparar as perdas de água e solo em diferentes sistemas de manejo, bem como determinar parâmetros de clima e de solo que possam estar associados a essas perdas e estimar perdas de solo por meio de modelos matemáticos. A área experimental consiste em 10 parcelas de 20 m2 (10 × 2 m), das quais nove foram trabalhadas inicialmente no sistema de plantio direto (SPD) e uma utilizada no sistema convencional (CO). Nestes moldes foram quantificadas as perdas de solo e água em diferentes safras. No final do segundo ano, das parcelas com SPD, cinco foram mantidas neste sistema, duas foram revolvidas na profundidade de 25 cm e reiniciadas no SPD e, em duas foi utilizado o sistema CO. Antes da utilização como sistema convencional, a parcela CO possuía plantio direto. Nas três safras estudadas o percentual infiltrado foi superior a 93% para o SPD e a 71% para o CO, considerando apenas as chuvas que propiciaram escoamento. As médias das perdas de solo na segunda safra foram de 2,27; 2,51; 14.61; e 14,79 t ha-1 e, de água, de 3,07; 5,51; 14,04; e 10,80 %, respectivamente para os sistemas de manejo SPD, CO e PDI.Palavras-chave: erosão hídrica, modelos de predição, erosividade. SOIL AND WATER LOSSES IN DIFFERENT MANAGEMENT SYSTEMS IN LATOSSOLOVERMELHO ABSTRACT: The objective was to compare soil and water losses in different management systems, as well as determine soil and climate parameters that could be associated with these losses and estimate soil losses through mathematical models. The experimental area consists of 10 plots of 20 m2 (10 × 2 m), of which nine were initially worked in the no-tillage system (SPD) and one in the conventional system (CO). Soils and water losses in different crops were quantified in these models. At the end of the second year, of the plots with SPD, five were kept in this system, two were revolved at 25 cm depth and restarted in the SPD and in two the CO system was used. Prior to use as a conventional system, the CO plot had no-tillage. In the three harvests studied, the percentage infiltrated was greater than 93% for the SPD and 71% for the CO, considering only the rains that caused the runoff. The average soil loss in the second harvest was 2.27; 2.51; 14.61; and 14.79 t ha-1 and, by water, 3.07; 5.51; 14.04; and 10.80%, respectively for the SPD, CO and PDI management systems.Keywords: hydric erosion, models of prediction, erosivity.

scholarly journals Water erosion and soil water infiltration in different stages of corn development and tillage systems

2015 ◽  
Vol 19 (11) ◽  
pp. 1072-1078 ◽  
Author(s):  
Daniel F. de Carvalho ◽  
Eliete N. Eduardo ◽  
Wilk S. de Almeida ◽  
Lucas A. F. Santos ◽  
Teodorico Alves Sobrinho
Keyword(s):  
Soil Water ◽  
Infiltration Rate ◽  
Water Infiltration ◽  
Soil Tillage ◽  
Tillage Systems ◽  
Water Losses ◽  
Development Stages ◽  
Soil Water Infiltration ◽  
Tillage System ◽  
Soil And Water

ABSTRACTThis study evaluated soil and water losses, soil water infiltration and infiltration rate models in soil tillage systems and corn (Zea mays, L.) development stages under simulated rainfall. The treatments were: cultivation along contour lines, cultivation down the slope and exposed soil. Soil losses and infiltration in each treatment were quantified for rains applied using a portable simulator, at 0, 30, 60 and 75 days after planting. Infiltration rates were estimated using the models of Kostiakov-Lewis, Horton and Philip. Based on the obtained results, the combination of effects between soil tillage system and corn development stages reduces soil and water losses. The contour tillage system promoted improvements in soil physical properties, favoring the reduction of erosion in 59.7% (water loss) and 86.6% (soil loss) at 75 days after planting, and the increase in the stable infiltration rate in 223.3%, compared with the exposed soil. Associated to soil cover, contour cultivation reduces soil and water losses, and the former is more influenced by management. Horton model is the most adequate to represent soil water infiltration rate under the evaluated conditions.

scholarly journals Relations between soil surface roughness, tortuosity, tillage treatments, rainfall intensity and soil and water losses from a red yellow latosol

2012 ◽  
Vol 36 (4) ◽  
pp. 1291-1298 ◽  
Author(s):  
Julieta Bramorski ◽  
Isabella C. De Maria ◽  
Renato Lemos e Silva ◽  
Silvio Crestana
Keyword(s):  
Surface Roughness ◽  
Water Retention ◽  
Soil Surface ◽  
No Tillage ◽  
Water Losses ◽  
Slope Length ◽  
Tillage Practices ◽  
Soil Surface Roughness ◽  
Tillage System ◽  
Soil And Water

The soil surface roughness increases water retention and infiltration, reduces the runoff volume and speed and influences soil losses by water erosion. Similarly to other parameters, soil roughness is affected by the tillage system and rainfall volume. Based on these assumptions, the main purpose of this study was to evaluate the effect of tillage treatments on soil surface roughness (RR) and tortuosity (T) and to investigate the relationship with soil and water losses in a series of simulated rainfall events. The field study was carried out at the experimental station of EMBRAPA Southeastern Cattle Research Center in São Carlos (Fazenda Canchim), in São Paulo State, Brazil. Experimental plots of 33 m² were treated with two tillage practices in three replications, consisting of: untilled (no-tillage) soil (NTS) and conventionally tilled (plowing plus double disking) soil (CTS). Three successive simulated rain tests were applied in 24 h intervals. The three tests consisted of a first rain of 30 mm/h, a second of 30 mm/h and a third rain of 70 mm/h. Immediately after tilling and each rain simulation test, the surface roughness was measured, using a laser profile meter. The tillage treatments induced significant changes in soil surface roughness and tortuosity, demonstrating the importance of the tillage system for the physical surface conditions, favoring water retention and infiltration in the soil. The increase in surface roughness by the tillage treatments was considerably greater than its reduction by rain action. The surface roughness and tortuosity had more influence on the soil volume lost by surface runoff than in the conventional treatment. Possibly, other variables influenced soil and water losses from the no-tillage treatments, e.g., soil type, declivity, slope length, among others not analyzed in this study.

scholarly journals Water infiltration rate in Yellow Latosol under different soil management systems

2015 ◽  
Vol 19 (11) ◽  
pp. 1021-1027 ◽  
Author(s):  
Jorge L. X. L. Cunha ◽  
Maria E. H. Coelho ◽  
Abel W. de Albuquerque ◽  
Cicero A. Silva ◽  
Antônio B. da Silva Júnior ◽  
...  
Keyword(s):  
Mathematical Models ◽  
Soil Water ◽  
Block Design ◽  
Infiltration Rate ◽  
Water Infiltration ◽  
Management Systems ◽  
No Tillage ◽  
Minimum Tillage ◽  
Soil Water Infiltration ◽  
Tillage System

ABSTRACTThe management systems affect soil structure, causing changes in porosity that can influence soil water infiltration. In order to study the water infiltration rate in a Yellow Latosol under different tillage systems and different mathematical models, an experiment was conducted from October to December 2012, at the Center for Agricultural Sciences at the Federal University of Alagoas, using a randomized block design with five replicates, in a split-plot scheme. In the plots, the management systems were evaluated (conventional tillage, no-tillage and minimum tillage) and, in the sub-plots, the empirical mathematical models of Kostiakov, Kostiakov-Lewis and Horton, and the ring method. The method used to measure soil water infiltration rate was adapted from the classic double-ring infiltrometer method. The minimum tillage system provided better results compared with the others, with water infiltration rate of 167 mm h-1, and the equation that best fitted the data of the ring infiltrometer was Kostiakov’s, in the no-tillage system.

scholarly journals Visual soil structure quality assessment on Oxisols under no-tillage system

2010 ◽  
Vol 67 (4) ◽  
pp. 479-482 ◽  
Author(s):  
Neyde Fabíola Balarezo Giarola ◽  
Alvaro Pires da Silva ◽  
Cássio Antônio Tormena ◽  
Bruce Ball ◽  
Jadir Aparecido Rosa
Keyword(s):  
Soil Structure ◽  
Structural Quality ◽  
Native Forest ◽  
No Tillage ◽  
Structure Quality ◽  
Physical Quality ◽  
Soil Physical Quality ◽  
Tillage System ◽  
Temperate Soils ◽  
Structure Assessment

Methods for evaluation the soil structure quality based on field evaluations are useful to determine strategies for soil management, with the advantage of requirement the use of little equipment and the possibility of immediate interpretation. A new methodology was recently developed to temperate soils for this purpose, called Visual Soil Structure Assessment (Ball et al., 2007). It was tested the hypothesis that it is possible to apply and advance in the interpretation of the results from use of Visual Soils Structure Assessment in cultivated Oxisols. Therefore the goal of this study was to apply, evaluate and enhance the potential of the methodology developed by Ball et al. (2007) in two Oxisols under long-term, no-till in Parana State, Brazil, as well as in a soil under native forest, used as reference of soil structural quality. The proposed implementation and progress in terms of structural quality for the distinct layers provided an assessment of soil physical quality more practical and detailed. This is useful to support the selection of appropriate techniques for mechanical and biological management systems in order to achieve the physical quality of soil suitable for crop development. Visual scores of soil structure quality proposed by Ball et al. (2007) can be applied to Brazilian Oxisols cultivated under no-tillage system.

Effect of Five Years of No-tillage and Mulch on Soil Properties and Tuber Yield of Cassava on an Acid Ultisol in South-eastern Nigeria

1990 ◽  
Vol 26 (2) ◽  
pp. 235-240 ◽  
Author(s):  
N. R. Hulugalle ◽  
R. Lal ◽  
M. Gichuru
Keyword(s):  
Soil Properties ◽  
Tuber Yield ◽  
Chemical Properties ◽  
Water Infiltration ◽  
No Tillage ◽  
South Eastern ◽  
Tillage System ◽  
Calcium Magnesium ◽  
Physical And Chemical ◽  
And Chemical Properties

SUMMARYThe effect of no-tillage and mulch on soil properties and tuber yield of cassava was studied over a five year period on an infertile, acid Ultisol in south-eastern Nigeria. Mulch was applied at a rate of 12 t ha−1as a split application once at planting and once six months after planting. No chemical fertilizers were used during the trial. Bulk density and proportion of micropores (pore radius, r, <1.4 µm) were greater, and proportion of macropores (r>14.4 µm) lower, with no-tillage. Water infiltration was increased by mulching, being greatest in tilled, mulched plots. Soil chemical properties were not significantly affected by tillage system, although levels of exchangeable calcium, magnesium and potassium were higher and acid saturation lower with mulching. Soil physical and chemical properties were best with tillage and mulching, and poorest when neither tillage nor mulch was used. Cassava tuber yield was unaffected by tillage system but increased by mulching.

scholarly journals Evaluation of water loss in transit and surface runoff in a Brazilian semi-arid basin

2020 ◽  
Vol 15 (4) ◽  
pp. 1
Author(s):  
Cristian Epifanio Toledo ◽  
João Carlos Mohn Nogueira ◽  
Alexandre De Amorim Camargo
Keyword(s):  
Water Loss ◽  
Surface Runoff ◽  
High Efficiency ◽  
Heterogeneous Environments ◽  
Runoff Coefficient ◽  
Water Losses ◽  
Proposed Model ◽  
Reservoir Basin ◽  
In Transit ◽  
Semi Arid

The objective of this work was to propose and evaluate a model to estimate transit water losses and surface runoff in a Brazilian semi-arid basin, fundamental components in the hydrological studies of the region, such as in the verification of hydrological connectivity. The study area was the Orós Reservoir Basin, located in the state of Ceará. The modeling of transit water loss and surface runoff were developed based on the work of Araújo and Ribeiro (1996) and Peter et al. (2014). In the proposed model, the parameter of loss in transit (k) was estimated at 0.027 km-1 for a section of the river basin, and when simulated for other stretches it provided good flow results at the end of the stretch, obtaining an NSE of 82%. The value of the runoff coefficient was estimated at 3% and when evaluating a spatial variation of this coefficient in the basin, the values varied from 2% to 12%, and the use of specialized runoff coefficient (RC) values promoted a higher NSE in the discharge simulation in the basin. It is concluded that the proposed model to estimate transit water losses and surface runoff demonstrated a high efficiency in the simulation of hydrological processes. The basin of Orós reservoir presented a high variability of the coefficient of surface runoff, justifying the need for a greater spatiality of this coefficient in heterogeneous environments.

Sign in / Sign up

Export Citation Format

Share Document