scholarly journals Spatial variability of soil physical attributes in integrated production systems in the Amazon region

2019 ◽  
Vol 54 ◽  
Author(s):  
Izabela de Lima Feitosa ◽  
Alexandre Martins Abdão dos Passos ◽  
Henrique Nery Cipriani ◽  
Marcelo Silva de Oliveira ◽  
Alaerto Luiz Marcolan ◽  
...  
Keyword(s):  
Soil Moisture ◽  
Spatial Variability ◽  
Production Systems ◽  
Penetration Resistance ◽  
Corn Plant ◽  
Agronomic Efficiency ◽  
Integrated Production ◽  
Moisture Contents ◽  
Soil Penetration Resistance ◽  
Physical Attributes

Abstract: The objective of this work was to analyze the spatial variability of soil physical attributes in integrated production systems and its relationship with the growth and yield of a corn (Zea mays) crop intercropped with palisade grass (Urochloa brizantha). The experiment was carried out in an integrated crop-livestock (ICL) system and in an integrated crop-livestock-forestry (ICLF) system, in a Plinthic Hapludox. The ICLF system was managed in alleys between eucalyptus (Eucalyptus spp.) rows, spaced at 18, 30, and 42 m. Corn grain and forage yields were positively correlated with soil clay and moisture contents, whereas grain yield was negatively correlated with soil penetration resistance. The lowest corn plant heights and grain yields were observed near eucalyptus rows. The average values for soil penetration resistance were below 2.0 MPa. Spatial variability was verified for: corn plant height, grain yield, and agronomic efficiency; forage intercropping; and soil moisture and silt contents, as well as penetration resistance. Greater grain and biomass yields were obtained at a 42-m distance between tree rows. The obtained results are indicative that corn traits and soil physical attributes were only slightly associated. The spatial distribution of the eucalyptus rows influences the agronomic efficiency of the intercrop and soil moisture contents.

scholarly journals INFLUÊNCIA DA PEDOFORMA NA VARIABILIDADE ESPACIAL DE ALGUNS ATRIBUTOS FÍSICOS E HÍDRICOS DE UM LATOSSOLO SOB CULTIVO DE CANA-DE-AÇÚCAR

Irriga ◽  
2004 ◽  
Vol 9 (1) ◽  
pp. 1-11 ◽  
Author(s):  
Zigomar Menezes de Souza ◽  
José Marques Júnior ◽  
Gener Tadeu Pereira ◽  
Luis Fernando Moreira
Keyword(s):  
Soil Moisture ◽  
Hydraulic Conductivity ◽  
Spatial Variability ◽  
Spatial Dependence ◽  
Penetration Resistance ◽  
Conventional Tillage ◽  
Saturated Hydraulic Conductivity ◽  
Soil Penetration Resistance ◽  
Occurrence Patterns ◽  
Very High

INFLUÊNCIA DA PEDOFORMA NA VARIABILIDADE ESPACIAL DE ALGUNS ATRIBUTOS FÍSICOS E HÍDRICOS DE UM LATOSSOLO SOB CULTIVO DE CANA-DE-AÇÚCAR[1]   Zigomar Menezes de Souza;  José Marques Júnior; Gener Tadeu Pereira; Luis Fernando MoreiraDepartamento de Solos e Adubos, Faculdade de Ciências Agrárias e Veterinárias, Universidade Estadual Paulista, Jaboticabal, SP,  [email protected]  1 RESUMO  O presente trabalho teve como objetivo avaliar a variabilidade espacial da condutividade hidráulica do solo saturado, resistência do solo à penetração e teor de água de um Latossolo Vermelho eutroférrico sob cultivo de cana de açúcar, utilizando-se métodos da estatística clássica, análises geoestatística e técnicas de interpolação de dados, com a finalidade de observar padrões de ocorrência destes atributos na paisagem. Foram feitas amostragens de solo nas profundidades de 0,0-0,2 m e 0,2-0,4 m, nos pontos de cruzamento de uma malha, com intervalos regulares de 10 m, perfazendo um total de 100 pontos. Os valores do coeficiente de variação para os dados apresentaram-se desde baixos (teor de água do solo), alto (resistência do solo à penetração) e muito alto (condutividade hidráulica do solo saturado). Observou-se a ocorrência de dependência espacial de todas as variáveis estudadas, com os maiores alcances na profundidade de 0,2-0,4 m. As variáveis condutividade hidráulica do solo saturado e teor de água do solo apresentaram grau moderado de dependência espacial, a resistência à penetração teve forte grau de dependência espacial. Pequenas variações nas formas do relevo condicionam variabilidade diferenciada para atributos físicos do solo.  UNITERMOS: geoestatística, krigagem, condutividade hidráulica do solo saturado, resistência do solo à penetração.   SOUZA, Z. M. de; MARQUES JUNIOR, J.; PEREIRA, G. T.; MOREIRA, L. F. INFLUENCE OF THE LANDSCAPE IN THE SPATIAL VARIABILITY OF THE HYDRAULIC CONDUCTIVITY, PENETRATION RESISTANCE AND SOIL MOISTURE IN THE SUGAR CANE CROP  2 ABSTRACT     The objective of this work was to evaluate spatial variability of saturated hydraulic conductivity, soil resistance to penetration and soil moisture in an area where sugarcane was planted under conventional tillage, using classic statistical methods, geostatistical analyses and data interpolation techniques, to assess occurrence patterns of these characteristics in the landscape. Soil was sampled depths of 0.0-0.2 m and 0.2-0.4 m, collected in intersections of a regular grid, with intervals of 10 m, in a total of 100 sampling points. Variation Coefficient (VC) were low for soil moisture, high soil for penetration resistance and very high for saturated hydraulic conductivity. All variables showed spatial dependence and the largest ones for depth of 0.2-0.4 m. Saturated hydraulic conductivity and soil moisture presented moderate spatial dependence, soil penetration resistance showed strong spatial dependence. Small variations in the landscape forms can define different spatial variability found for the physical characteristics of the soil.  KEYWORDS: geostatistics, kriging, saturated hydraulic conductivity, soil penetration resistance. 

scholarly journals Modeling and correction of soil penetration resistance for variations in soil moisture and soil bulk density

2016 ◽  
Vol 36 (3) ◽  
pp. 449-459 ◽  
Author(s):  
Wininton M. da Silva ◽  
Aloísio Bianchini ◽  
Cesar A. da Cunha
Keyword(s):  
Soil Moisture ◽  
Bulk Density ◽  
Linear Models ◽  
Clay Soil ◽  
Penetration Resistance ◽  
Soil Bulk Density ◽  
Good Representation ◽  
Soil Resistance ◽  
Soil Penetration Resistance ◽  
Resistance Value

ABSTRACT This study aimed to describe the behavior of models for adjusting data of soil penetration resistance for variations in soil moisture and soil bulk density. The study was carried out in Lucas do Rio Verde, MT, Brazil in a typic dystrophic red-yellow Latosol (Oxisol) containing 0.366 kg kg−1 of clay. Soil penetration resistance measurements were conducted in the soil moistures of 0.33 kg kg−1, 0.28 kg kg−1, 0.25 kg kg−1 and 0.22 kg kg−1. Soil penetration resistance behavior due to variations in soil moisture and soil bulk density was assessed by estimating the soil resistance values by non-linear models. There was an increase of the soil penetration resistance values as soil was losing moisture. For the same edaphic condition studied, small differences in the data of soil bulk density affect differently the response of soil resistance as a function of moisture. Both soil bulk density and soil moisture are essential attributes to explain the variations in soil penetration resistance in the field. The good representation of the critical soil bulk density curve as a limiting compression indicator requires the proper choice of the restrictive soil resistance value for each crop.

scholarly journals Geostatistical analysis for soil moisture content under the no tillage cropping system

2006 ◽  
Vol 63 (4) ◽  
pp. 341-350 ◽  
Author(s):  
Célia Regina Grego ◽  
Sidney Rosa Vieira ◽  
Aline Maria Antonio ◽  
Simone Cristina Della Rosa
Keyword(s):  
Soil Moisture ◽  
Moisture Content ◽  
Spatial Variability ◽  
Water Content ◽  
Spatial Dependence ◽  
Soil Moisture Content ◽  
No Tillage ◽  
Moisture Contents ◽  
Classical Statistics ◽  
Evaluation Point

Experiments in agriculture usually consider the topsoil properties to be uniform in space and, for this reason, often make inadequate use of the results. The objective of this study was to assess the variability for soil moisture content using geostatistical techniques. The experiment was carried out on a Rhodic Ferralsol (typic Haplorthox) in Campinas, SP, Brazil, in an area of 3.42 ha cultivated under the no tillage system, and the sampling was made in a grid of 102 points spaced 10 m x 20 m. Access tubes were inserted down to one meter at each evaluation point in order to measure soil moisture contents (cm³ cm-3) at depths of 30, 60 and 90 cm with a neutron moisture gauge. Samplings were made between the months of August and September of 2003 and in January 2004. The soil moisture content for each sampling date was analyzed using classical statistics in order to appropriately describe the central tendency and dispersion on the data and then using geostatistics to describe the spatial variability. The comparison between the spatial variability for different samplings was made examining scaled semivariograms. Water content was mapped using interpolated values with punctual kriging. The semivariograms showed that, at the 60 cm depth, soil water content had moderate spatial dependence with ranges between 90 and 110 m. However, no spatial dependence was found for 30 and 90 cm depths in 2003. Sampling density was insufficient for an adequate characterization of the spatial variability of soil moisture contents at the 30 and 90 cm depths.

SPATIAL VARIABILITY OF SOIL PENETRATION RESISTANCE AND TEMPERATURE IN AGRESTE PERNAMBUCO

2017 ◽  
Author(s):  
K. J. JIMENEZ ◽  
P. M. B. MENDES ◽  
A. A. A. MONTENEGRO ◽  
M. M. ROLIM ◽  
D. H. S. SOUZA ◽  
...  
Keyword(s):  
Spatial Variability ◽  
Penetration Resistance ◽  
Soil Penetration Resistance

scholarly journals Characterization of the soil compaction based on the mapping of the apparent electrical conductivity

2021 ◽  
Vol 29 ◽  
Author(s):  
Eduardo Leonel Bottega ◽  
Eder Luís Sari ◽  
Zanandra Boff de Oliveira ◽  
Alberto Eduardo Knies
Keyword(s):  
Electrical Conductivity ◽  
Spatial Variability ◽  
Soil Compaction ◽  
Penetration Resistance ◽  
Management Zones ◽  
Mean Values ◽  
Soil Penetration Resistance ◽  
Apparent Electrical Conductivity ◽  
Moisture Conditions

Based on the measurement of soil penetration resistance (PR), it is possible to identify compacted soil layers, where root growth may be harmed, affecting crop development and yield. The objective of this work was to analyze the use of management zones (MZ), delimited on the basis of mapping of the spatial variability of the soil apparent electrical conductivity (ECa), in the differentiation of soil compaction levels. The work was carried out in a 25.8-ha no-tillage area, cultivated under a center pivot. The ECa was measured under two soil moisture conditions (13.7 and 16.45%), using the Terram® equipment. Soil penetration resistance (PR) was measured using the SoloStar PLG5500 penetrograph. Based on the spatial variability ECa mapping, management zones (2, 3, and 4 zones) were delimited. The mean PR values ??of each MZ were compared by the t-test of means. It was possible to differentiate mean values ??of penetration resistance (PR), which vary from 0.9 to 2.10 MPa, from the characterization of management classes generated on the basis of the ECa spatial variability. The highest stratification of PR values ??was obtained as a function of sampling directed at delimited management zones when the soil had lower moisture content (13.7%). The highest mean PR values ??were obtained for the split of the ECa map into at least three classes. It was identified that for the study area there is no need to perform any mechanical decompaction operation.

scholarly journals Impact of recreational transformation of soil physical properties on micromolluscs in an urban park

2021 ◽  
Vol 29 (2) ◽  
pp. 78-87
Author(s):  
V. S. Budakova ◽  
N. V. Yorkina ◽  
P. M. Telyuk ◽  
A. K. Umerova ◽  
O. M. Kunakh ◽  
...  
Keyword(s):  
Electrical Conductivity ◽  
Soil Moisture ◽  
Physical Properties ◽  
Soil Properties ◽  
Principal Component ◽  
Feature Space ◽  
Penetration Resistance ◽  
Soil Physical Properties ◽  
Urban Park ◽  
Soil Penetration Resistance

The paper assesses the effect of transformation of soil physical properties on the abundance of micromolluscs in the conditions of an urban park. The studies were carried out in Novooleksandrivskiy Park (Melitopol, Ukraine). An experimental polygon was represented by 7 transects with 18 sampling points in each. The interval between the points in the transect, as well as the interval between transects, was 3 meters. The total area of the polygon was 1,134 m2. The tree species growing within the polygon were Quercus robur, Sophora japonica, and Acer campestre. Shrubs were represented by Ulmus laevis, Tilia cordata, Celtis occidentalis, and Morus nigra. The locations of the trees and shrubs were mapped. The crowns of tree and shrub plants formed a dense canopy and a shady light regime. The grass cover was practically absent. The soil mechanical resistance, soil aggregate-size distribution, electrical conductivity of soil, soil moisture and bulk density were measured. We recorded 618 individuals of Vallonia pulchella, 120 individuals of Cochlicopa lubrica, and 58 individuals of Acanthinula aculeata within the surveyed polygon. We extracted three principal components, which could explain 60.9% of the variation in the feature space of the soil properties. The principal component 1 explained 42.0% of the variation of the feature space and depended on the soil penetration resistance throughout the whole profile, aggregate composition, density, electric conductivity and moisture content of soil. This component reflected a tendency for soil penetration resistance and soil density to increase near recreational trails. The principal component 1 was used to indicate the gradient of recreational transformation of the soil. The principal component 2 was able to explain 10.6% of the variation in the feature space. It negatively correlated with the distance from the recreational trail, soil penetration resistance at the depth of 35 cm or more, soil electrical conductivity, and the proportion of aggregates greater than 3 mm in size. This component positively correlated with soil penetration resistance at 0–5 cm depth and the proportion of aggregates less than 0.5 mm in size. This component can be interpreted as a "halo" from the recreational trail, or a gradient of indirect soil transformations adjacent to the zone of intense recreational load. The principal component 3 was able to explain 8.3% of the variation in the feature space. It positively correlated with soil penetration resistance at the depth of 20–40 cm, the proportion of 0.5–7.0 mm aggregates, and soil moisture. It negatively correlated with the proportion of aggregates larger than 7 mm and smaller than 0.25 mm. This component indicated a variation in soil properties that was induced by causes independent of recreational exposure. The extracted gradients of soil properties significantly influenced the abundance of micromollusc populations. The abundance of all species decreased after increase in recreational load. Micromollusc species responded to direct recreational exposure as plateau (C. lubrica) and asymmetric unimodal responses (V. pulchella and A. aculeata).

scholarly journals Challenges and potential approaches for soil recovery in iron open pit mines and waste piles

2021 ◽  
Author(s):  
Rafael Silva Guedes ◽  
Sílvio Junio Ramos ◽  
Markus Gastauer ◽  
Cecílio Frois Caldeira Júnior ◽  
Gabriel Caixeta Martins ◽  
...  
Keyword(s):  
Native Species ◽  
Penetration Resistance ◽  
Open Pit ◽  
Native Forest ◽  
Open Pit Mines ◽  
Soil Penetration Resistance ◽  
Zn And Cu In ◽  
Physical Attributes ◽  
Iron Mining ◽  
Soil Recovery

Abstract The revegetation of areas impacted by iron mining may be hampered by a series of chemical and physical impediments exhibited by those areas. Physical problems, such as penetration resistance and steep slopes, may outweigh the chemical problems, such that both should be considered for soil recovery. This study aimed to evaluate the main soil attributes that are directly related to plant growth on areas affected by iron mining activities discussing possible solutions. For this purpose, chemical and physical attributes including penetration resistance on open pit mines, waste piles and native forest in Carajás Mineral Province were analysed. The results show that the open pits had low to medium levels of P and low levels of organic matter and of the micronutrients B, Zn and Cu. In the waste piles, the chemical parameters were less hindering than in the open pits. Soil penetration resistance in open pits was higher than in the waste piles and the forest; however, there was a reduction of up to 69% in soil resistance in open pits in the rainy season. The principal chemical problems observed in mine pits can be easily corrected, although the inclination of open pit slopes in combination with elevated soil density increase the risks of losses of fertilizers and seeds by runoff. Penetration resistance is the most serious problem for the development of plants in mine pits, although the use of irrigation water can help to maintain tolerable levels of resistance in soil for proper root growth of native species.

scholarly journals MACHINE TRAFFIC AND SOIL PENETRATION RESISTANCE IN GUAVA TREE ORCHARDS

2018 ◽  
Vol 31 (4) ◽  
pp. 980-986 ◽  
Author(s):  
Wilson José Oliveira de Souza ◽  
Danilo Eduardo Rozane ◽  
Henrique Antunes de Souza ◽  
William Natale ◽  
Paulo André Fernandes dos Santos
Keyword(s):  
Spatial Variability ◽  
Normal Distribution ◽  
Ordinary Kriging ◽  
Penetration Resistance ◽  
Sampling Grid ◽  
Soil Penetration Resistance ◽  
Sampling Points ◽  
Type 3

ABSTRACT The study was conducted in irrigated commercial orchards of ‘Paluma’ and ‘Pedro Sato’ guavas, which were mapped with a Garmin GPS unit (Cx60). Sixty five sampling points were marked on a 21 x 21 m sampling grid. Gravimetric humidity and soil penetration resistance (SPR) were evaluated with the help of an automated penetrometer rod with a type 3 cone at a 45º angle (maximum SPR 15,100 kPa). Data with non-normal distribution were analyzed by geostatistics and interpolation by ordinary kriging. SPR values were higher where machine traffic occurs than on the lines where the crop is planted. There was spatial variability of the SPR among the layers evaluated, with the layer between 0.10-0.20 m, on the line of the machine traffic, presenting a higher SPR (>4000 kPa).

scholarly journals Data Grouping Method for the Purpose of Forecasting the Mechanical Strength of Plastic Soils

Agronomy ◽  
2020 ◽  
Vol 10 (4) ◽  
pp. 578
Author(s):  
Dariusz Błażejczak ◽  
Jan Jurga ◽  
Jarosław Pytka
Keyword(s):  
Soil Moisture ◽  
Moisture Content ◽  
Bulk Density ◽  
Field Measurements ◽  
Penetration Resistance ◽  
Soil Bulk Density ◽  
Regression Equations ◽  
Soil Penetration Resistance ◽  
Small Set ◽  
Data Grouping

The aim of this work was to develop a method of data grouping (DGM) that enables the selection of regression equations for forecasting soil penetration resistance based on an easily available and small set of input data: soil moisture content, soil bulk density and the grain size distribution of the soil. Models for forecasting the penetration resistance were created by selecting regression equations for specific intervals of granulometric variability of soil fractions. A field measurements campaign was conducted and soil samples were taken from the subsoil on 43 profiles, at depths of 25–30, 35–40, 45–50 and 55–60 cm. It was found that the dry bulk density is much less useful for predicting the penetration resistance of plastic soils than soil moisture. The study also showed that it is possible to forecast the soil penetration resistance on the basis of the gravimetric moisture content and the soil specific surface.

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