2017
DOI: 10.1590/18069657rbcs20160426
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Sampling Design of Soil Physical Properties in a Conilon Coffee Field

Abstract: Establishing the number of samples required to determine values of soil physical properties ultimately results in optimization of labor and allows better representation of such attributes. The objective of this study was to analyze the spatial variability of soil physical properties in a Conilon coffee field and propose a soil sampling method better attuned to conditions of the management system. The experiment was performed in a Conilon coffee field in Espírito Santo state, Brazil, under a 3.0 × 2.0 × 1.0 m (… Show more

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Cited by 8 publications
(5 citation statements)
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“…Ceddia et al (2009) found low values of coefficient of variation for soil density and sand (<10%) and high values for silt and clay (>40%). Santos et al (2017) studied the physical attributes of a sandy textured Oxisol cultivated with conilon coffee and found a lower coefficient of variation for macropores (27.60%), total sand (8.72%), silt (18.43%), and clay (18.30%) when compared to the results obtained in our study, being the result of differences in the soil type found in the area. Carmo et al (2016), studying the quality of the beverage coffee as a function of soil color and attributes of an Ultisol (Argissolo Vermelho Amarelo, Brazilian Soil Classification System) from sandstone in the State of São Paulo, verified coefficients of variation for clay that ranged from 17 to 24%.…”
Section: Resultscontrasting
confidence: 56%
See 1 more Smart Citation
“…Ceddia et al (2009) found low values of coefficient of variation for soil density and sand (<10%) and high values for silt and clay (>40%). Santos et al (2017) studied the physical attributes of a sandy textured Oxisol cultivated with conilon coffee and found a lower coefficient of variation for macropores (27.60%), total sand (8.72%), silt (18.43%), and clay (18.30%) when compared to the results obtained in our study, being the result of differences in the soil type found in the area. Carmo et al (2016), studying the quality of the beverage coffee as a function of soil color and attributes of an Ultisol (Argissolo Vermelho Amarelo, Brazilian Soil Classification System) from sandstone in the State of São Paulo, verified coefficients of variation for clay that ranged from 17 to 24%.…”
Section: Resultscontrasting
confidence: 56%
“…Souza et al (2006) investigated an optimum sampling density for the physical attributes in an Oxisol (Latossolo Vermelho eutroférrico, Brazilian Soil Classification System) under sugarcane cultivation by using the Cline (1944) formula and observed that higher number of samples are required to characterize Ds (9 points ha −1 ), TPV (49 points ha −1 ), microporosity (59 points ha −1 ), and macroporosity (131 points ha −1 ) on an ultra-detailed scale (1 ha). Santos et al (2017), using the same methodology for the study of sampling density in areas cultivated with conilon coffee in the State of Espírito Santo, found similar results regarding the number of samples needed to characterize Ds, MA, and clay content. Oliveira et al (2014) compared the sampling densities obtained from the range of the semivariogram and the formula proposed by Cline (1944) and observed a significant difference between sampling densities of both methodologies, with that proposed by Cline (1944) presenting the highest number of samples required (376 vs. 4 points ha −1 ).…”
Section: Attributementioning
confidence: 59%
“…Soil sampling was done using Edelman auger at a depth of 0-0.20 m at five different points in a plot using the zigzag method [24] and bulked to make a composite sample. The composite samples from all plots were labeled, packed, and taken to the laboratory for analysis.…”
Section: Soil Sampling and Laboratory Analysismentioning
confidence: 99%
“…A elevada variabilidade de P (Figura 1) gerou um número impraticável de amostras simples para formar uma amostra composta representativa da unidade de amostragem, mesmo quando se aumentou o volume das amostras simples e se aceitou um desvio em torno da média de 20% (Tabela 2). Outro fato importante é que a amostragem de solo não é realizada separadamente para cada característica química, assim, a precisão final obtida após o processo de amostragem dependerá das características do solo analisadas, concordando com Santos et al (2017) e Rozane et al (2011).…”
Section: unclassified
“…Uma amostragem representativa é aquela que melhor caracteriza uma área de interesse, realizada por meio da coleta de um número de pontos que alia precisão na estimativa e minimiza o esforço (SANTOS et al, 2017). Assim, para que a amostragem seja eficiente e econômica, deve-se trabalhar com amostras simples e compostas de solo.…”
Section: Introductionunclassified