Use of blood residue as alternative source of phosphorus in sunflower (Helianthus annuus L. ) cultivation / [Utilização de resíduo de sangue como fonte alternativa de fósforo no cultivo de girassol (Helianthus annuus L. )]

The aim of this work was to increase the aerial part, biometry, and yield of achenes from sunflower plants on the effect of increasing doses of blood residue, as an alternative source of phosphorus (P), in a clayey-textured red Oxisol. The experimental design used was randomized blocks, with six treatments and four replications. The treatments consisted of five doses of blood residue (0, 6, 12, 24 and 48m3 ha-1) and a control treatment that received phosphate chemical fertilization, 80kg ha-1 of P2O5. The increasing doses of blood residue and chemical fertilization do not show disproportionality for P concentration in soil, leaf, plant height (PH), stem diameter (SD), chapter diameter (CD) and achene production. The analysis of the principal component (PC) revealed that the first PC presents the greatest accumulated variation (74%). Based on the first PC, the dose of 12m-3 ha-1 has greater influence for PH, SC, and CD. Due to the greater influence on the biometric characteristics of sunflower plants, the blood residue (12m-3 ha-1 = 98.4kg P ha-1), can be used as an alternative source of phosphorus for the cultivation of sunflower in clayey oxisols.

Objetivou-se com este trabalho verificar biometria de parte aérea, rendimento de aquênios de plantas de girassol sobre o efeito de doses crescentes de resíduo de sangue, como fonte alternativa de fósforo (P), em um Latossolo vermelho de textura argilosa. O delineamento experimento utilizado foi o de blocos casualizados, com seis tratamentos e quatro repetições. Os tratamentos foram constituídos por cinco doses de resíduo de sangue (0, 6, 12, 24 e 48m3 ha-1) e um tratamento que recebeu a adubação fosfatada química, 80kg ha-1 de P2O5. As doses crescentes de resíduo de sangue e adubação química não demostram desproporcionalidade para a concentração de P no solo, folha, altura de planta (AP), diâmetro de caule (DC), diâmetro de capítulo (DCP) e produção de aquênios. A análise de componentes (CP) principais revelou que o primeiro CP apresenta maior variação acumulada (74%). Baseado no primeiro CP, a dose de 12 m-3 ha-1exibe maior influência para AP, DC e DCP. Devido a maior influência sobre as características biométricas em plantas de girassol, o resíduo de sangue (12m-3 ha-1 = 98,4kg P ha-1), pode ser utilizado como fonte alternativa de fósforo para o cultivo de girassol em Latossolos de textura argilosa.

Mineralogical, chemical and electrochemical attributes of soils

A set of attributes endows the soils with distinctive characteristics and astute understanding is required in order to formulate suitable strategies for soil management. The aim of this study was to physically, chemically and mineralogically characterize samples of the main soil classes in Minas Gerais, Brazil, determine the point of zero salt effect (PZSE) and the point of zero charge (PZC), and ascertain the correlation between these factors and soil attributes. The soils evaluated presented different textural classes ranging from loamy sand (Entisol) to very clayey (some Oxisols and Ultisols). The soils differed substantially in terms of fertility, presenting a range from dystrophic (low fertility, base saturation < 50 %) to eutrophic character (fertility, base saturation >= 50 %), even within the same soil class, such as the Oxisols, which suggests the concurrence of the parent material. Highly weathered soils are predominant in Minas Gerais and these soils are composed predominantly of kaolinite, gibbsite, goethite and hematite. Traces of hydroxy-Al interlayered vermiculite and illite were also found in the Oxisols, Ultisols and Inceptisols. A correlation between the PZSE and the PZC in the A horizon was observed. A high degree of correlation was observed between the PZC and the exchangeable aluminum and the ratio of iron obtained by ammonium oxalate and dithionite-citrate (Feo/Fed) in both the A and B horizons of soil classes. The results obtained reinforce the importance of knowledge of soil attributes to the adoption of practices such as the management of phosphate fertilization in clayey soils and liming in soils rich in aluminum.(AU)

Mineralogical, chemical and electrochemical attributes of soils

A set of attributes endows the soils with distinctive characteristics and astute understanding is required in order to formulate suitable strategies for soil management. The aim of this study was to physically, chemically and mineralogically characterize samples of the main soil classes in Minas Gerais, Brazil, determine the point of zero salt effect (PZSE) and the point of zero charge (PZC), and ascertain the correlation between these factors and soil attributes. The soils evaluated presented different textural classes ranging from loamy sand (Entisol) to very clayey (some Oxisols and Ultisols). The soils differed substantially in terms of fertility, presenting a range from dystrophic (low fertility, base saturation = 50 %), even within the same soil class, such as the Oxisols, which suggests the concurrence of the parent material. Highly weathered soils are predominant in Minas Gerais and these soils are composed predominantly of kaolinite, gibbsite, goethite and hematite. Traces of hydroxy-Al interlayered vermiculite and illite were also found in the Oxisols, Ultisols and Inceptisols. A correlation between the PZSE and the PZC in the A horizon was observed. A high degree of correlation was observed between the PZC and the exchangeable aluminum and the ratio of iron obtained by ammonium oxalate and dithionite-citrate (Feo/Fed) in both the A and B horizons of soil classes. The results obtained reinforce the importance of knowledge of soil attributes to the adoption of practices such as the management of phosphate fertilization in clayey soils and liming in soils rich in aluminum.

Quality reference values for rare earth elements in soils from one of the last agricultural frontiers in Brazil

ABSTRACT: Environmental impacts caused by the addition of rare earth elements (REEs) to agricultural soils are a growing concern. The sedimentary basin of the Gurguéia River is located in one of the last agricultural frontiers in Brazil; nevertheless, data regarding quality reference values (QRVs) for REEs in soils are still scarce. The objective of this study was therefore to determine the natural concentration and establish the QRVs of REEs in soils of Gurguéia watershed, Brazil. Fifty-five composite soil samples were collected at sites under no or minimal anthropic interference. The average REE natural concentrations in soils from the Gurguéia watershed were lower than those found in other regions of Brazil and worldwide, following the order (mg kg1): Ce (14.01) > Nd (6.19) > La (5.52) > Pr (2.51) > Sm (1.45) > Gd (0.93) > Dy (0.63) > Er (0.42) > Yb (0.39) > Tb (0.28) > Eu (0.26) > Lu (0.20). The parent material was the main factor that controlled the distribution of REEs in soils. The QRVs in soils followed the order (mg kg1): Ce (18.8) > Nd (7.92) > La (6.32) > Pr (3.3) > Sm (1.97) > Gd (1.35) > Dy (0.85) > Er (0.55) > Yb (0.47) > Tb (0.37) > Lu (0.25). These values serve as a basis to assist the development of legislation, including REE thresholds for Brazilian soils.

Preconsolidation stress of gibbsitic and kaolinitic Oxisols under a multipractice conservationist coffee system / Pressão de pré-consolidação de Latossolos gibbsítico e caulinítico sob sistema de multipraticas conservacionista no cultivo cafeeiro

Our goal was to analyze the impact of a multipractice soil conservationist system on coffee production in tropical soils (LATOSSOLO VERMELHO-AMARELO caulinítico/kaolinitic Haplustox and LATOSSOLO VERMELHO-gibbsítico/gibbsitic Acrustox) in Minas Gerais, Brazil. In the experimental area, the soil management involved a set of multiple conservationist practices during cultivation for more than 3.5 yrs. Soil samples were collected at 0-5, 10-15, and 20-25 cm depths at two positions: planting rows and between rows. The soil physical and mechanical properties were determined, with a focus mainly on the preconsolidation stress model (preconsolidation stress versus matric tension). For the purpose of analysis, a split-split plot experimental design was implemented. A linear mixed regression model (LMR) was fitted, and Wald's test was performed (P < 0.05). An improvement of soil physical quality for both Oxisols was observed at the planting row position. The effects of multipractice soil management after 3.5 yrs of cultivation in association with increased gibbsite content could promote new soil structure organization, as revealed by LMR, resulting in more resilient soils (between rows) and increasing the resistance to external pressures on gibbsitic Acrustox. Overall, the findings herein are in concordance with global trends towards conservationist practices that may alleviate soil compaction in agricultural systems to maintain environmental sustainability.(AU)

Nosso objetivo foi analisar o impacto de um sistema de manejo do solo com multi-práticas conservacionistas para o cultivo cafeeiro em solos tropicais (LATOSSOLO VERMELHO-AMARELO caulinítico/ kaolinitic Haplustox and LATOSSOLO VERMELHO gibbsítico/ gibbsitic Acrustox) em Minas Gerais, Brasil. Na área experimental, o manejo do solo incluiu um conjunto de multi-práticas conservacionistas por mais de 3,5 anos. Amostras de solo foram coletadas em 0-5; 10-15; e profundidades de 20 a 25 cm em duas posições: linha e entrelinha. As propriedades físicas e mecânicas do solo foram determinadas, concentrando-se principalmente na modelagem da compactação (estresse de pré-consolidação versus tensão matricial). Para fins de análise, foi considerado o delineamento experimental de parcelas subsubdivididas. Foi ajustado o modelo de regressão linear mista (RLM), bem como o teste F de Wald (P < 0,05). Melhorias na qualidade física do solo em ambos os Latossolos foi observada na linha de plantio. Os efeitos do sistema de manejo multipráticas usado após 3,5 anos de cultivo associado ao maior conteúdo de gibbsita podem promover uma nova organização da estrutura do solo revelada pelo RLM, que resulta em solos mais resilientes (na entrelinha), melhorando a resistência às pressões externas aplicadas ao Latossolo gibbsítico. No geral, os resultados aqui apresentadas estão de acordo com as tendências globais em direção a práticas conservacionistas que podem aliviar a compactação do solo em sistemas agrícolas e manter a sustentabilidade ambiental.(AU)

Adsorption and desorption of arsenic and its immobilization in soils

Arsenic (As) is a naturally occurring chemical element considered toxic and carcinogenic by health and environmental protection agencies. Studies of As adsorption/desorption behavior in soils are important to predictions of As’ potential mobility in natural systems. The aim of this study was to assess the adsorption of As(V) in soils from Minas Gerais, Brazil, and determine its immobilization rate in order to identify soils with characteristics more favorable to its deployment as an As geochemical barrier. The adsorption experiment was performed using different As concentrations and the data pertaining to the maximum adsorption capacity of As(V) (MACAs) were determined by Langmuir and Freundlich isoterms. The Oxisols, due to their more oxidic mineralogy, especially more gibbsitic, and clayey texture, showed the highest MACAs, followed by Ultisols, Inceptisols, and Entisols. In terms of the desorption of As the Inceptisols were the soils that showed the most As desorption. Both As desorption and mobility was lower in the more oxidic and clayey soils. In all soils, the total amount of As was desorbed in due course, but the As release ratio tended to decrease with the passage of time. In general, soils with higher MACAs did not necessarily show less As desorption. For use as a geochemical barrier, as important as a high adsorption capacity of As by the soil is a low As desorption rate. The increase in As mobility may increase the risks of contaminating the supplies of water. To be a good As geochemical barrier the soil has to be a clayey Oxisol, with relatively high amounts of Fe and Al oxides, especially gibbsite.

Quality reference values for rare earth elements in soils from one of the last agricultural frontiers in Brazil

Environmental impacts caused by the addition of rare earth elements (REEs) to agricultural soils are a growing concern. The sedimentary basin of the Gurguéia River is located in one of the last agricultural frontiers in Brazil; nevertheless, data regarding quality reference values (QRVs) for REEs in soils are still scarce. The objective of this study was therefore to determine the natural concentration and establish the QRVs of REEs in soils of Gurguéia watershed, Brazil. Fifty-five composite soil samples were collected at sites under no or minimal anthropic interference. The average REE natural concentrations in soils from the Gurguéia watershed were lower than those found in other regions of Brazil and worldwide, following the order (mg kg−1): Ce (14.01) > Nd (6.19) > La (5.52) > Pr (2.51) > Sm (1.45) > Gd (0.93) > Dy (0.63) > Er (0.42) > Yb (0.39) > Tb (0.28) > Eu (0.26) > Lu (0.20). The parent material was the main factor that controlled the distribution of REEs in soils. The QRVs in soils followed the order (mg kg−1): Ce (18.8) > Nd (7.92) > La (6.32) > Pr (3.3) > Sm (1.97) > Gd (1.35) > Dy (0.85) > Er (0.55) > Yb (0.47) > Tb (0.37) > Lu (0.25). These values serve as a basis to assist the development of legislation, including REE thresholds for Brazilian soils.

Adsorption and desorption of arsenic and its immobilization in soils

Arsenic (As) is a naturally occurring chemical element considered toxic and carcinogenic by health and environmental protection agencies. Studies of As adsorption/desorption behavior in soils are important to predictions of As potential mobility in natural systems. The aim of this study was to assess the adsorption of As(V) in soils from Minas Gerais, Brazil, and determine its immobilization rate in order to identify soils with characteristics more favorable to its deployment as an As geochemical barrier. The adsorption experiment was performed using different As concentrations and the data pertaining to the maximum adsorption capacity of As(V) (MACAs) were determined by Langmuir and Freundlich isoterms. The Oxisols, due to their more oxidic mineralogy, especially more gibbsitic, and clayey texture, showed the highest MACAs, followed by Ultisols, Inceptisols, and Entisols. In terms of the desorption of As the Inceptisols were the soils that showed the most As desorption. Both As desorption and mobility was lower in the more oxidic and clayey soils. In all soils, the total amount of As was desorbed in due course, but the As release ratio tended to decrease with the passage of time. In general, soils with higher MACAs did not necessarily show less As desorption. For use as a geochemical barrier, as important as a high adsorption capacity of As by the soil is a low As desorption rate. The increase in As mobility may increase the risks of contaminating the supplies of water. To be a good As geochemical barrier the soil has to be a clayey Oxisol, with relatively high amounts of Fe and Al oxides, especially gibbsite.(AU)

Quality reference values for rare earth elements in soils from one of the last agricultural frontiers in Brazil

Environmental impacts caused by the addition of rare earth elements (REEs) to agricultural soils are a growing concern. The sedimentary basin of the Gurguéia River is located in one of the last agricultural frontiers in Brazil; nevertheless, data regarding quality reference values (QRVs) for REEs in soils are still scarce. The objective of this study was therefore to determine the natural concentration and establish the QRVs of REEs in soils of Gurguéia watershed, Brazil. Fifty-five composite soil samples were collected at sites under no or minimal anthropic interference. The average REE natural concentrations in soils from the Gurguéia watershed were lower than those found in other regions of Brazil and worldwide, following the order (mg kg−1): Ce (14.01) > Nd (6.19) > La (5.52) > Pr (2.51) > Sm (1.45) > Gd (0.93) > Dy (0.63) > Er (0.42) > Yb (0.39) > Tb (0.28) > Eu (0.26) > Lu (0.20). The parent material was the main factor that controlled the distribution of REEs in soils. The QRVs in soils followed the order (mg kg−1): Ce (18.8) > Nd (7.92) > La (6.32) > Pr (3.3) > Sm (1.97) > Gd (1.35) > Dy (0.85) > Er (0.55) > Yb (0.47) > Tb (0.37) > Lu (0.25). These values serve as a basis to assist the development of legislation, including REE thresholds for Brazilian soils.(AU)

Nutrient dynamics with application of humic substances and liming in irrigated soil filled columns / Dinâmica de nutrientes com a aplicação de substâncias húmicas e calagem em colunas de solo irrigadas

The objective of this work was to evaluate the retention of P, K, Ca and Mg nutrients, as well as pH and electrical conductivity in Oxisols. Soil samples were placed into columns, with addition of humic substances (soil with and without liming). The experiment was conducted in a greenhouse and the columns consisted of PVC tubes with 40 cm height x 5 cm diameter. The humic substances used were humic acid and fulvic acid, applied at rates of 0, 60, 120 and 240 L ha-¹, in soil with or without lime. Ten irrigation events were performed, simulating 32 mm rainfall. After that, samples were collected from the columns, at 0-20 and 20-40 cm depths, to identify the residual effect of the addition of humic substances. A completely randomized design was used for this experiment, with 2×2×4 factorial statistical model and 3 replications. The results showed that, under acidic soil conditions, the use of fulvic acid provides more significant P release (up to 40%) in soil when compared to humic acid. When the rate of 240 L ha-¹ is applied, the fulvic acid can release up to 83% of P in the soil.

Neste trabalho avaliou-se a retenção dos nutrientes P, K, Ca e Mg, além do pH e condutividade elétrica em Latossolos, inseridos em colunas e adicionados de substâncias húmicas (na ausência e presença de calagem). O experimento foi conduzido em casa de vegetação e as colunas foram compostas por colunas de PVC de 40 cm de altura e 5 cm de diâmetro. As substâncias húmicas utilizadas foram o ácido húmico e o ácido fúlvico aplicados nas doses 0, 60, 120 e 240 L ha-¹ em solo com ou sem calcário. Dez eventos de irrigação foram realizados simulando chuvas de 32 mm. Em seguida, amostras das colunas foram coletadas nas profundidades de 0-20 e 20-40 cm para identificar o efeito residual da adição de substâncias húmicas. O experimento foi em delineamento inteiramente casualizado, com modelo estatístico fatorial 2×2×4 com 3 repetições. Os resultados mostraram que em condições de solo ácido, o uso do ácido fúlvico é mais expressivo na liberação de P (até 40% de liberação) no solo quando comparado ao ácido húmico. E, quando utilizada a taxa de 240 L ha-¹, o ácido fúlvico pode liberar até 83% de P no solo.

Nutrient dynamics with application of humic substances and liming in irrigated soil filled columns / Dinâmica de nutrientes com a aplicação de substâncias húmicas e calagem em colunas de solo irrigadas

The objective of this work was to evaluate the retention of P, K, Ca and Mg nutrients, as well as pH and electrical conductivity in Oxisols. Soil samples were placed into columns, with addition of humic substances (soil with and without liming). The experiment was conducted in a greenhouse and the columns consisted of PVC tubes with 40 cm height x 5 cm diameter. The humic substances used were humic acid and fulvic acid, applied at rates of 0, 60, 120 and 240 L ha-¹, in soil with or without lime. Ten irrigation events were performed, simulating 32 mm rainfall. After that, samples were collected from the columns, at 0-20 and 20-40 cm depths, to identify the residual effect of the addition of humic substances. A completely randomized design was used for this experiment, with 2×2×4 factorial statistical model and 3 replications. The results showed that, under acidic soil conditions, the use of fulvic acid provides more significant P release (up to 40%) in soil when compared to humic acid. When the rate of 240 L ha-¹ is applied, the fulvic acid can release up to 83% of P in the soil.(AU)

Neste trabalho avaliou-se a retenção dos nutrientes P, K, Ca e Mg, além do pH e condutividade elétrica em Latossolos, inseridos em colunas e adicionados de substâncias húmicas (na ausência e presença de calagem). O experimento foi conduzido em casa de vegetação e as colunas foram compostas por colunas de PVC de 40 cm de altura e 5 cm de diâmetro. As substâncias húmicas utilizadas foram o ácido húmico e o ácido fúlvico aplicados nas doses 0, 60, 120 e 240 L ha-¹ em solo com ou sem calcário. Dez eventos de irrigação foram realizados simulando chuvas de 32 mm. Em seguida, amostras das colunas foram coletadas nas profundidades de 0-20 e 20-40 cm para identificar o efeito residual da adição de substâncias húmicas. O experimento foi em delineamento inteiramente casualizado, com modelo estatístico fatorial 2×2×4 com 3 repetições. Os resultados mostraram que em condições de solo ácido, o uso do ácido fúlvico é mais expressivo na liberação de P (até 40% de liberação) no solo quando comparado ao ácido húmico. E, quando utilizada a taxa de 240 L ha-¹, o ácido fúlvico pode liberar até 83% de P no solo.(AU)

Modeling boron adsorption on five soils before and after removal of organic matter

Boron- B concentrations that cause deficiency and those that cause toxicity appear to be very similar, compared to other nutrients, which can complicate successful management of this element in soils. In this study, B adsorption onto two Oxisols from Brazil (Rhodic Eutroperox and Anionic Acroperox), two Alfisols (Natric Palexeralf and Aridic Paleustalf) and an Entisol (Xeric Torrifluvent) from the United States of America were evaluated. The samples were treated with sodium hypochlorite in order to remove soil organic matter. Both treated and untreated samples were used to determine B adsorption isotherms using different B concentrations (0-4.630 mmol L–1) and NaNO3 (0.05 M) as background electrolyte solution at pH 7. Boron adsorption envelopes were also measured using 0.463 mmol L–1 B at three ionic strengths (0.05, 0.1 and 1M) and NaNO3 as background electrolyte solutions at different pH values (3-12). The cation exchange capacity, specific surface area, free Al and Fe oxides, organic and inorganic carbon content, mineralogy and particle size distribution of the soils were also determined. The Langmuir isotherm and the constant capacitance model were fit to the B adsorption data and the parameters obtained were related to the chemical attributes by multiple linear regression equations. Boron maximum adsorption capacity (BMAC) and the complexation constant for the SH3BO4– inner-sphere complex (LogKB–) could be predicted under all experimental conditions. The Alc content was the main soil chemical attribute associated with the BMAC under the conditions evaluated and the LogKB–(int) in untreated and treated samples.

Modeling boron adsorption on five soils before and after removal of organic matter

Boron- B concentrations that cause deficiency and those that cause toxicity appear to be very similar, compared to other nutrients, which can complicate successful management of this element in soils. In this study, B adsorption onto two Oxisols from Brazil (Rhodic Eutroperox and Anionic Acroperox), two Alfisols (Natric Palexeralf and Aridic Paleustalf) and an Entisol (Xeric Torrifluvent) from the United States of America were evaluated. The samples were treated with sodium hypochlorite in order to remove soil organic matter. Both treated and untreated samples were used to determine B adsorption isotherms using different B concentrations (0-4.630 mmol L–1) and NaNO3 (0.05 M) as background electrolyte solution at pH 7. Boron adsorption envelopes were also measured using 0.463 mmol L–1 B at three ionic strengths (0.05, 0.1 and 1M) and NaNO3 as background electrolyte solutions at different pH values (3-12). The cation exchange capacity, specific surface area, free Al and Fe oxides, organic and inorganic carbon content, mineralogy and particle size distribution of the soils were also determined. The Langmuir isotherm and the constant capacitance model were fit to the B adsorption data and the parameters obtained were related to the chemical attributes by multiple linear regression equations. Boron maximum adsorption capacity (BMAC) and the complexation constant for the SH3BO4inner-sphere complex (LogKB–) could be predicted under all experimental conditions. The Alc content was the main soil chemical attribute associated with the BMAC under the conditions evaluated and the LogKB–(int) in untreated and treated samples.(AU)

Influence of the sugarcane vinasse of the balance of charges in high weathered oxide soil of subtropical region in Brazil / Influência da vinhaça no balanço de cargas em Latossolo Veemelho distrófico da região subtropical do Brasil

Brazil is one of the largest sugarcane producers around the world, however the effects concerning environment issues in soil are still no well described. Soil electrochemical can provide important information about residues uses and environmental contamination, and then zero point of charge (ZPC) is a parameter that may demonstrate this variation. In this study, It was analyzed the soil behavior when submitted to sugarcane vinasse application in different doses simulating high and low doses application as regularly done by the manufactures in typical tropical weathered oxisols. To procedure ZPC test, microcosmsexperiment was managed with all parameters measured and controlled in a factorial design:2 soil depths (superficial group – 0.0 – 20.0 cm and sub-superficial group – 60.0 – 80.0 cm), 3 salt concentration (0.002; 0.02 and 0.2 mL NaCl), and 4vinasse doses (Without application; Low – 164.28 mL L-1; Intermediate – 328.57 mL L-1 and High 657.14 mL L-1), after incubation all the samples were measured electrochemically.Based on these analyses, data rised two main highlights: 1. vinasse low doses behaved like a buffer solution, 2. High doses in sub-superficial layer disturbed ZCP. Then, vinasse seems correlate with lixiviation capacity, and then over-applications can disrupt soil solution on this soil.

O Brasil é um dos maiores produtores de cana-de-açúcar do mundo, porém os efeitos relativos às questões ambientais do uso dos resíduos desta atividade no solo ainda não estão bem descritos. A eletroquímica do solo pode fornecer informações importantes sobre o impacto do uso de resíduos e contaminação ambiental, sendo o ponto de carga zero (ZPC) um parâmetro que pode demonstrar esta variação. Neste estudo, foi analisada a resposta do solo quando submetido à aplicação de vinhaça de cana-de-açúcar em diferentes doses, utilizando a aplicação de altas e baixas doses deste resíduo normalmente feita pelas indústrias sucroalcooleira em Latossolos tropicais intemperizados típicos. Para o teste de ZPC, o experimento laboratorial foi realizado com todos os parâmetros medidos e controlados em um planejamento fatorial: 2 profundidades de solo (grupo superficial - 0,0 - 20,0 cm e grupo subsuperficial - 60,0 - 80,0 cm), 3 concentração de solução salina (0,002; 0,02 e 0,2 mL NaCl) e 4 doses de vinhaça (Sem aplicação; Baixa - 164,28 mL L-1; Intermediário - 328,57 mL L-1 e Alta 657,14 mL L-1), após a incubação todas as amostras foram medidas eletroquimicamente e calculado o ZPC. Com base nessas análises, observou-se: 1. A dose mais baixa de vinhaça apresentou-se como uma solução tampão, 2. As doses altas na camada subsuperficial influenciaram a ZPC. Assim, a vinhaça parece estar correlacionada com a capacidade de lixiviação, desta forma, aplicações de altas doses de vinhaça nestes solos podem afetar eletronicamente a solução dos mesmos.

Influence of the sugarcane vinasse of the balance of charges in high weathered oxide soil of subtropical region in Brazil / Influência da vinhaça no balanço de cargas em Latossolo Veemelho distrófico da região subtropical do Brasil

Brazil is one of the largest sugarcane producers around the world, however the effects concerning environment issues in soil are still no well described. Soil electrochemical can provide important information about residues uses and environmental contamination, and then zero point of charge (ZPC) is a parameter that may demonstrate this variation. In this study, It was analyzed the soil behavior when submitted to sugarcane vinasse application in different doses simulating high and low doses application as regularly done by the manufactures in typical tropical weathered oxisols. To procedure ZPC test, microcosmsexperiment was managed with all parameters measured and controlled in a factorial design:2 soil depths (superficial group 0.0 20.0 cm and sub-superficial group 60.0 80.0 cm), 3 salt concentration (0.002; 0.02 and 0.2 mL NaCl), and 4vinasse doses (Without application; Low 164.28 mL L-1; Intermediate 328.57 mL L-1 and High 657.14 mL L-1), after incubation all the samples were measured electrochemically.Based on these analyses, data rised two main highlights: 1. vinasse low doses behaved like a buffer solution, 2. High doses in sub-superficial layer disturbed ZCP. Then, vinasse seems correlate with lixiviation capacity, and then over-applications can disrupt soil solution on this soil.(AU)

O Brasil é um dos maiores produtores de cana-de-açúcar do mundo, porém os efeitos relativos às questões ambientais do uso dos resíduos desta atividade no solo ainda não estão bem descritos. A eletroquímica do solo pode fornecer informações importantes sobre o impacto do uso de resíduos e contaminação ambiental, sendo o ponto de carga zero (ZPC) um parâmetro que pode demonstrar esta variação. Neste estudo, foi analisada a resposta do solo quando submetido à aplicação de vinhaça de cana-de-açúcar em diferentes doses, utilizando a aplicação de altas e baixas doses deste resíduo normalmente feita pelas indústrias sucroalcooleira em Latossolos tropicais intemperizados típicos. Para o teste de ZPC, o experimento laboratorial foi realizado com todos os parâmetros medidos e controlados em um planejamento fatorial: 2 profundidades de solo (grupo superficial - 0,0 - 20,0 cm e grupo subsuperficial - 60,0 - 80,0 cm), 3 concentração de solução salina (0,002; 0,02 e 0,2 mL NaCl) e 4 doses de vinhaça (Sem aplicação; Baixa - 164,28 mL L-1; Intermediário - 328,57 mL L-1 e Alta 657,14 mL L-1), após a incubação todas as amostras foram medidas eletroquimicamente e calculado o ZPC. Com base nessas análises, observou-se: 1. A dose mais baixa de vinhaça apresentou-se como uma solução tampão, 2. As doses altas na camada subsuperficial influenciaram a ZPC. Assim, a vinhaça parece estar correlacionada com a capacidade de lixiviação, desta forma, aplicações de altas doses de vinhaça nestes solos podem afetar eletronicamente a solução dos mesmos.(AU)

Mineralogy, magnetic susceptibility and geochemistry of Fe-rich Oxisols developed from several parent materials

Fe-rich Oxisols on mafic rocks in Brazil generally have high magnetic susceptibility with high contents of some trace elements. These are taxonomically similar soils; however, differences in magnetic and geochemical properties may affect agricultural or environmental usability and subsequent management. This study investigated the pedogenesis of Fe-rich Oxisols from various parent materials and evaluated the lithogenetic influence on magnetic susceptibility and trace elements contents. Soil samples were collected from Bw horizons in 13 Rhodic Oxisols and a Typic Oxisol developed from several parent materials in Minas Gerais State, Brazil. Soils were analyzed by X-ray diffractometry (XRD) and magnetometry. Soil chemical analyses consisted of sulfuric and total (tri-acid) digestions and selective Fe oxides dissolutions and statistical correlations were determined. Fe-rich Oxisols presented a typical mineralogical composition of highly weathered soils with structural stability. The results confirm the difficulty to identify accurately magnetic minerals in different grain sizes using XRD. However, coarse fractions still exert dominant influence on the magnetic properties of the Fe-rich Rhodic Oxisols. In addition, coarse fractions probably contribute to the enrichment of superparamagnetic particles for the clay fraction. Although highly weathered, Fe-rich Oxisols may have their geochemical attributes still controlled by the parent material, where trace elements seem to be correlated with the magnetic minerals in the coarse fractions. Thus, the natural replacement of some trace elements from soil-solution equilibrium reactions during plant development could be more effective in soils with higher magnetic particles concentrations in the coarse fractions.

Mineralogy, magnetic susceptibility and geochemistry of Fe-rich Oxisols developed from several parent materials

Fe-rich Oxisols on mafic rocks in Brazil generally have high magnetic susceptibility with high contents of some trace elements. These are taxonomically similar soils; however, differences in magnetic and geochemical properties may affect agricultural or environmental usability and subsequent management. This study investigated the pedogenesis of Fe-rich Oxisols from various parent materials and evaluated the lithogenetic influence on magnetic susceptibility and trace elements contents. Soil samples were collected from Bw horizons in 13 Rhodic Oxisols and a Typic Oxisol developed from several parent materials in Minas Gerais State, Brazil. Soils were analyzed by X-ray diffractometry (XRD) and magnetometry. Soil chemical analyses consisted of sulfuric and total (tri-acid) digestions and selective Fe oxides dissolutions and statistical correlations were determined. Fe-rich Oxisols presented a typical mineralogical composition of highly weathered soils with structural stability. The results confirm the difficulty to identify accurately magnetic minerals in different grain sizes using XRD. However, coarse fractions still exert dominant influence on the magnetic properties of the Fe-rich Rhodic Oxisols. In addition, coarse fractions probably contribute to the enrichment of superparamagnetic particles for the clay fraction. Although highly weathered, Fe-rich Oxisols may have their geochemical attributes still controlled by the parent material, where trace elements seem to be correlated with the magnetic minerals in the coarse fractions. Thus, the natural replacement of some trace elements from soil-solution equilibrium reactions during plant development could be more effective in soils with higher magnetic particles concentrations in the coarse fractions.(AU)

Microstructural strength of four subtropical soils evaluated by rheometry: properties, difficulties and opportunities

The structural strength of soils has been extensively described by physical and mechanical properties evaluated on the mesoscale for different soils and management conditions. However, changes in the organization of the soil matrix at the microstructural level, which can be obtained by rheometry, are still seldom used in soil mechanics. Our aim was to use the amplitude sweep test, a rheometry technique, to investigate the microstructural strength of four subtropical soils (two Oxisols, an Ultisol and a Vertisol) and to discuss difficulties with respect to the samples, water content, soil density and vertical force. The various rheological properties which reveal the soil microstructural strength were determined: deformation at the end of the linear viscoelastic range, LVE range (LVE), shear stress at the end of the LVE range (LVE), deformation at yield point, YP (YP), storage and loss moduli at YP (GGYP), maximum shear stress (max), and integral z. In general, soil elasticity (LVE and YP) and microstructural strength (LVE and max) were greater in the Oxisols and the Vertisol, which both possess high clay content, while the latter also contains expansive clay minerals. The lowest structural strength was observed in the Ultisol which had a high sand content. As rheological properties are related to soil properties such as particle size distribution and carbon content, they can be applied in the evaluation of the microstructural strength of clayey and sandy soils and allows for inferences regarding inter-particle shear strength. However, the test is not applicable to very dry soil samples and sample preparations can affect the results. We suggest a number of approaches to find solutions for these difficulties/problems.

Microstructural strength of four subtropical soils evaluated by rheometry: properties, difficulties and opportunities

The structural strength of soils has been extensively described by physical and mechanical properties evaluated on the mesoscale for different soils and management conditions. However, changes in the organization of the soil matrix at the microstructural level, which can be obtained by rheometry, are still seldom used in soil mechanics. Our aim was to use the amplitude sweep test, a rheometry technique, to investigate the microstructural strength of four subtropical soils (two Oxisols, an Ultisol and a Vertisol) and to discuss difficulties with respect to the samples, water content, soil density and vertical force. The various rheological properties which reveal the soil microstructural strength were determined: deformation at the end of the linear viscoelastic range, LVE range (LVE), shear stress at the end of the LVE range (LVE), deformation at yield point, YP (YP), storage and loss moduli at YP (GGYP), maximum shear stress (max), and integral z. In general, soil elasticity (LVE and YP) and microstructural strength (LVE and max) were greater in the Oxisols and the Vertisol, which both possess high clay content, while the latter also contains expansive clay minerals. The lowest structural strength was observed in the Ultisol which had a high sand content. As rheological properties are related to soil properties such as particle size distribution and carbon content, they can be applied in the evaluation of the microstructural strength of clayey and sandy soils and allows for inferences regarding inter-particle shear strength. However, the test is not applicable to very dry soil samples and sample preparations can affect the results. We suggest a number of approaches to find solutions for these difficulties/problems.(AU)

Tolerance of apple rootstocks to short-term waterlogging

ABSTRACT: Until few years ago there were limited options of apple rootstocks commercially available for Brazilian growers; although, new series of Geneva® rootstocks introduced recently present desirable features such as vigor control and wider lateral branch angle. On the main apple producing regions of Brazil, intermittent rainfall eventually occurs and waterlogged condition is frequent especially in high clay oxisols; in addition, little is known about the tolerance of rootstocks M.9, Marubakaido/M.9 interstock, G.202, G.213 and G.814 to waterlogging. Thus, the objective of this experiment was to evaluate the tolerance of these rootstocks to short-term waterlogging on root and aerial parameters. Potted Maxi Gala apple plants were kept under 48 hours of waterlogging weekly throughout 19 weeks to be compared with a normal hydric condition control. The evaluated variables were: leaf, stem and root dry matter, number and length of new root emission, and number of leaves, mean leaf size and chlorophyll content. Rootstocks G.202, G.814 and Marubakaido/M.9 interstock presented more tolerance to waterlogging, and the main defense mechanism was the emission of new adventitious roots.

RESUMO: Até pouco tempo, haviam poucas opções de porta-enxertos de macieira disponíveis comercialmente para produtores brasileiros. Contudo, com a nova série de porta-enxertos Geneva® introduzidos recentemente, características desejáveis foram apresentadas como, controle de vigor e ângulo de ramo aberto. Nas principais regiões produtoras de maçã no Brasil, chuvas intermitentes ocorrem eventualmente levando muitas áreas ao encharcamento, especialmente em locais com latossolos com elevados teores de argila. Em adição, pouco se sabe sobre a tolerância dos porta-enxertos M.9, Marubakaido com inter-enxerto de M.9, G.202, G.213 e G.814 ao encharcamento. Assim, o objetivo deste experimento foi avaliar a tolerância destes porta-enxertos ao encharcamento temporário através de parâmetros de raiz e parte aérea. Macieiras Maxi Gala, cultivadas em vasos, foram mantidas sob encharcamento semanalmente durante 48 horas por 19 semanas, para serem comparadas com o controle em condição hídrica normal. As variáveis analisadas foram: massa seca das folhas, caule e raiz, comprimento e número de raízes novas, número de folhas, tamanho de folha e teor de clorofila. Os porta-enxertos G.202, G.814 e Marubakaido com filtro de M.9 apresentaram maior tolerância ao encharcamento, sendo que o principal mecanismo de defesa para isso foi a maior emissão de raízes adventícias novas.