Evaluation of leaching potential of tebuthiuron using bioindicator plants / Estudo da lixiviação do herbicida tebuthiuron com plantas bioindicadoras

The last destination of most herbicides used in agricultural systems is the soil. This is a dynamic interaction; herbicides can remain in the soil solution or be carried through the soil profile, reaching the water table. The objective of this work was to evaluate the leaching potential of the tebuthiuron herbicide using bioindicator plants grown in an Oxisol of sandy loam texture and in an Entisol of clay texture, after the occurrence of natural rainfall events. A complete randomized experimental design was used, in a 3×8 factorial arrangement, with four replications. The treatments consisted of three accumulated natural rainfall depths (30-40, 60-80, and 100-120 mm) and eight soil profile layers (0-3, 3-6, 6-9, 9-12, 12-15, 15-20, 20-25, and 25-30 cm). Soil samples were collected after the tebuthiuron herbicide application - 750 for clayey soil, and 600 g ha-1 for the sandy loam soil -and the rainfall events. PVC pipes with length of 30 cm and diameter of 15 cm were introduced into the soil profile for sampling. The pipes with soil columns were carefully removed by digging around them, to maintain the soil original integrity during collection and, subsequently, cut longitudinally for sowing the bioindicator species - cucumber (Cucumis sativus L.), and lettuce (Lactuca sativa L.). Then, the phytotoxicity in the bioindicator plants grown in these soils were evaluated at 5, 7, 10, and 12 days after sowing, using a grading scale of 0 to 100%. The mobility of the tebuthiuron herbicide was low in both soils, regardless of the rainfall depth, and the cucumber was the most suitable plant species to use as a bioindicator.(AU)

O solo é o destino final da maioria dos herbicidas utilizados no sistema agrícola e, sendo esta relação dinâmica, eles podem permanecer na solução ou ser carregados no perfil do solo, podendo atingir o lençol freático. O objetivo deste trabalho foi avaliar o potencial de lixiviação do herbicida tebuthiuron por meio de plantas bioindicadoras e após a ocorrência de precipitações pluviométricas naturais, em solos com texturas franco arenoso (Latossolo Vermelho-Amarelo) e argiloso (Neossolo Litólico). O delineamento experimental foi o inteiramente casualizado em um esquema fatorial 3 x 8 com quatro repetições, sendo três níveis de precipitação pluviométrica (30-40, 60-80 e 100-120 mm) e oito de profundidade do perfil do solo (0-3, 3-6, 6-9, 9-12, 12-15, 15-20, 20-25 e 25-30 cm). As coletas das amostras ocorreram após a aplicação do herbicida tebuthiuron nas doses de 750 e 600 g ha-1 para o solo argiloso e arenoso, respectivamente, e posterior acúmulo das precipitações. Para a coleta das amostras foram introduzidas, no perfil do solo, colunas de PVC com 30 cm de altura e 15 cm de diâmetro. As colunas foram retiradas cuidadosamente escavando-se ao seu redor, mantendo a integridade original do solo durante a coleta. Posteriormente, as colunas foram separadas com corte longitudinal, para a semeadura das espécies bioindicadoras pepino (Cucumis sativus L.) e alface (Lactuca sativa L.). Para as avaliações das plantas bioindicadoras nas colunas, adotou-se a escala de notas de 0 a 100% de fitotoxicidade, aos 5, 7, 10 e 12 dias após a semeadura. A mobilidade do herbicida tebuthiuron mostrou-se reduzida em ambos os tipos de solo estudado, independentemente da precipitação pluvial, e as plantas de pepino mostraram-se mais adequadas para serem utilizadas como espécie bioindicadora.(AU)

Evaluation of leaching potential of tebuthiuron using bioindicator plants / Estudo da lixiviação do herbicida tebuthiuron com plantas bioindicadoras

The last destination of most herbicides used in agricultural systems is the soil. This is a dynamic interaction; herbicides can remain in the soil solution or be carried through the soil profile, reaching the water table. The objective of this work was to evaluate the leaching potential of the tebuthiuron herbicide using bioindicator plants grown in an Oxisol of sandy loam texture and in an Entisol of clay texture, after the occurrence of natural rainfall events. A complete randomized experimental design was used, in a 3×8 factorial arrangement, with four replications. The treatments consisted of three accumulated natural rainfall depths (30-40, 60-80, and 100-120 mm) and eight soil profile layers (0-3, 3-6, 6-9, 9-12, 12-15, 15-20, 20-25, and 25-30 cm). Soil samples were collected after the tebuthiuron herbicide application - 750 for clayey soil, and 600 g ha-1 for the sandy loam soil -and the rainfall events. PVC pipes with length of 30 cm and diameter of 15 cm were introduced into the soil profile for sampling. The pipes with soil columns were carefully removed by digging around them, to maintain the soil original integrity during collection and, subsequently, cut longitudinally for sowing the bioindicator species - cucumber (Cucumis sativus L.), and lettuce (Lactuca sativa L.). Then, the phytotoxicity in the bioindicator plants grown in these soils were evaluated at 5, 7, 10, and 12 days after sowing, using a grading scale of 0 to 100%. The mobility of the tebuthiuron herbicide was low in both soils, regardless of the rainfall depth, and the cucumber was the most suitable plant species to use as a bioindicator.(AU)

O solo é o destino final da maioria dos herbicidas utilizados no sistema agrícola e, sendo esta relação dinâmica, eles podem permanecer na solução ou ser carregados no perfil do solo, podendo atingir o lençol freático. O objetivo deste trabalho foi avaliar o potencial de lixiviação do herbicida tebuthiuron por meio de plantas bioindicadoras e após a ocorrência de precipitações pluviométricas naturais, em solos com texturas franco arenoso (Latossolo Vermelho-Amarelo) e argiloso (Neossolo Litólico). O delineamento experimental foi o inteiramente casualizado em um esquema fatorial 3 x 8 com quatro repetições, sendo três níveis de precipitação pluviométrica (30-40, 60-80 e 100-120 mm) e oito de profundidade do perfil do solo (0-3, 3-6, 6-9, 9-12, 12-15, 15-20, 20-25 e 25-30 cm). As coletas das amostras ocorreram após a aplicação do herbicida tebuthiuron nas doses de 750 e 600 g ha-1 para o solo argiloso e arenoso, respectivamente, e posterior acúmulo das precipitações. Para a coleta das amostras foram introduzidas, no perfil do solo, colunas de PVC com 30 cm de altura e 15 cm de diâmetro. As colunas foram retiradas cuidadosamente escavando-se ao seu redor, mantendo a integridade original do solo durante a coleta. Posteriormente, as colunas foram separadas com corte longitudinal, para a semeadura das espécies bioindicadoras pepino (Cucumis sativus L.) e alface (Lactuca sativa L.). Para as avaliações das plantas bioindicadoras nas colunas, adotou-se a escala de notas de 0 a 100% de fitotoxicidade, aos 5, 7, 10 e 12 dias após a semeadura. A mobilidade do herbicida tebuthiuron mostrou-se reduzida em ambos os tipos de solo estudado, independentemente da precipitação pluvial, e as plantas de pepino mostraram-se mais adequadas para serem utilizadas como espécie bioindicadora.(AU)

Carbon sequestration in clay and silt fractions of Brazilian soils under conventional and no-tillage systems

The capacity of soils to sequestrate carbon (C) is mainly related to the formation of organo-mineral complexes. In this study, we investigated the influence of soil management systems on the C retention capacity of soil with an emphasis on the silt and clay fractions of two subtropical soils with different mineralogy and climate. Samples from a Humic Hapludox and a Rhodic Hapludox, clayey soils cultivated for approximately 30 years under no-tillage (NT) and conventional tillage (CT) were collected from six layers distributed within 100-cm soil depth from each site and from an adjacent native forest. After the removal of particulate organic matter (POM), the suspension ( 53 µm) was sonicated, the silt and clay fractions were separated in accordance with Stokes' law and the carbon content of whole soil and physical fractions was determined. In the Humic Hapludox, the clay and silt fractions under NT showed a higher maximum C retention (72 and 52 g kg-1, respectively) in comparison to those under CT (54 and 38 g kg-1, respectively). Moreover, the C concentration increase in both fractions under NT occurred mainly in the topsoil (up to 5 cm). The C retention in physical fractions of Rhodic Hapludox varied from 25 to 32 g kg-1, and no difference was observed whether under an NT or a CT management system. The predominance of goethite and gibbsite in the Humic Hapludox, as well as its exposure to a colder climate, may have contributed to its greater C retention capacity. In addition to the organo-mineral interaction, a mechanism of organic matter self-assemblage, enhanced by longer periods of soil non-disturbance, seems to have contributed to the carbon stabilization in both soils.

Arbuscular mycorrhizal fungi in saline soils: vertical distribution at different soil depth

Arbuscular mycorrhizal fungi (AMF) colonize land plants in every ecosystem, even extreme conditions such as saline soils. In the present work we report for the first time the mycorrhizal status and the vertical fungal distribution of AMF spores present in the rhizospheric soil samples of four species of Chenopodiaceae (Allenrolfea patagonica, Atriplex argentina, Heterostachys ritteriana and Suaeda divaricata) at five different depths in two saline of central Argentina. Roots showed medium, low or no colonization (0-50%). Nineteen morphologically distinctive AMF species were recovered. The number of AMF spores ranged between 3 and 1162 per 100 g dry soil, and AMF spore number decreased as depth increased at both sites. The highest spore number was recorded in the upper soil depth (0-10 cm) and in S. divaricata. Depending of the host plant, some AMF species sporulated mainly in the deep soil layers (Glomus magnicaule in Allenrolfea patagonica, Septoglomus aff. constrictum in Atriplex argentina), others mainly in the top layers (G. brohultti in Atriplex argentina and Septoglomus aff. constrictum in Allenrolfea patagonica). Although the low percentages of colonization or lack of it, our results show a moderate diversity of AMF associated to the species of Chenopodiaceae investigated in this study. The taxonomical diversity reveals that AMF are adapted to extreme environmental conditions from saline soils of central Argentina.

Carbon sequestration in clay and silt fractions of Brazilian soils under conventional and no-tillage systems

The capacity of soils to sequestrate carbon (C) is mainly related to the formation of organo-mineral complexes. In this study, we investigated the influence of soil management systems on the C retention capacity of soil with an emphasis on the silt and clay fractions of two subtropical soils with different mineralogy and climate. Samples from a Humic Hapludox and a Rhodic Hapludox, clayey soils cultivated for approximately 30 years under no-tillage (NT) and conventional tillage (CT) were collected from six layers distributed within 100-cm soil depth from each site and from an adjacent native forest. After the removal of particulate organic matter (POM), the suspension ( 53 µm) was sonicated, the silt and clay fractions were separated in accordance with Stokes' law and the carbon content of whole soil and physical fractions was determined. In the Humic Hapludox, the clay and silt fractions under NT showed a higher maximum C retention (72 and 52 g kg-1, respectively) in comparison to those under CT (54 and 38 g kg-1, respectively). Moreover, the C concentration increase in both fractions under NT occurred mainly in the topsoil (up to 5 cm). The C retention in physical fractions of Rhodic Hapludox varied from 25 to 32 g kg-1, and no difference was observed whether under an NT or a CT management system. The predominance of goethite and gibbsite in the Humic Hapludox, as well as its exposure to a colder climate, may have contributed to its greater C retention capacity. In addition to the organo-mineral interaction, a mechanism of organic matter self-assemblage, enhanced by longer periods of soil non-disturbance, seems to have contributed to the carbon stabilization in both soils.(AU)

Gypsum effects on soil chemical properties under two management systems / Efeito do gesso nas propriedades químicas do solo sob dois sistemas de manejo

The combination of gypsum application and soil management may influence soil chemical properties. In this context, the aim of this paper was to evaluate soil chemical properties under two management systems and residual gypsum in soil after 55 months from treatment application. This experiment was developed in FCA/UFGD in Dourados-MS, Brazil under a randomized block design with subdivided plots and four replications. Main plots, subplots and subsubplots consisted of tillage systems (conventional and no tillage), gypsum application and soil depth (0-0,05, 0,05-0,10, 0,10-0,15, 0,15-0,20 and 0,20-0,30 m), respectively. There were no effects of residual gypsum on calcium levels. The combination of no tillage system and residual gypsum increased potassium and sulfur as well as reduced potential acidity. However, residual gypsum increased soil potential acidity in conventional system. No tillage system increased calcium levels in the depths 0-0.05 and 0.05-0.10 m, organic matter down to 0.05 m, sulfur accumulation in the depths 0.05-0.10 and 0.10-0.15 m, sum of bases and base saturation in the depth 0.05-0.10. Conversely, magnesium levels in the depth 0.10-0.15 m, phosphorus from 0.05 to 0.15 m, potential acidity from 0.05 to 0.10 m and ECC in the depth 0.10-0.15 m were decreased. Effects of residual gypsum increased sulfur and base saturation from 0.20 to 0.30 m, but decreased magn

A combinação de gessagem e manejo do solo podem influenciar as propriedades químicas do solo. Neste contexto, o objetivo deste trabalho foi avaliar as propriedades químicas do solo submetido a dois manejos do solo e ao efeito residual de gesso, após 55 meses de implantação dos tratamentos. Desenvolvido em uma área experimental da FCA/UFGD de Dourados, MS, o experimento foi disposto no delineamento de blocos casualizados com os fatores arranjados em parcela subsubdividida. A parcelas, sub-parcelas e sub-subparcelas receberam os níveis dos fatores sistema plantio direto e convencional, gesso e profundidade 0-0,05, 0,05-0,10, 0,10-0,15, 0,15-0,20 e 0,20-0,30 m, respectivamente, com quatro repetições. Não houve efeito residual de gesso para cálcio. O plantio direto com efeito residual de gesso aumentou o teor de potássio, enxofre e reduziu a acidez potencial. O plantio convencional com efeito residual de gesso aumentou a acidez potencial do solo. O plantio direto promoveu aumento de cálcio (em 0-0,05 e 0,05-0,10 m), aumento do teor de matéria orgânica (em 0-0,05 m), acúmulo de enxofre (em 0,05-0,10 e 0,10-0,15 m) , aumento da soma de base e saturação por base (em 0,05-0,10 m,) e redução de magnésio (em 0,10-0,15 m), fósforo (em 0,05-0,10 e 0,10-0,15 m), acidez potencial (em 0,05-0,10 m) e CTC (em 0,10-0,15 m). O efeito residual de gesso acumulou mais enxofre e saturação por base na

Gypsum effects on soil chemical properties under two management systems / Efeito do gesso nas propriedades químicas do solo sob dois sistemas de manejo

The combination of gypsum application and soil management may influence soil chemical properties. In this context, the aim of this paper was to evaluate soil chemical properties under two management systems and residual gypsum in soil after 55 months from treatment application. This experiment was developed in FCA/UFGD in Dourados-MS, Brazil under a randomized block design with subdivided plots and four replications. Main plots, subplots and subsubplots consisted of tillage systems (conventional and no tillage), gypsum application and soil depth (0-0,05, 0,05-0,10, 0,10-0,15, 0,15-0,20 and 0,20-0,30 m), respectively. There were no effects of residual gypsum on calcium levels. The combination of no tillage system and residual gypsum increased potassium and sulfur as well as reduced potential acidity. However, residual gypsum increased soil potential acidity in conventional system. No tillage system increased calcium levels in the depths 0-0.05 and 0.05-0.10 m, organic matter down to 0.05 m, sulfur accumulation in the depths 0.05-0.10 and 0.10-0.15 m, sum of bases and base saturation in the depth 0.05-0.10. Conversely, magnesium levels in the depth 0.10-0.15 m, phosphorus from 0.05 to 0.15 m, potential acidity from 0.05 to 0.10 m and ECC in the depth 0.10-0.15 m were decreased. Effects of residual gypsum increased sulfur and base saturation from 0.20 to 0.30 m, but decreased magn

A combinação de gessagem e manejo do solo podem influenciar as propriedades químicas do solo. Neste contexto, o objetivo deste trabalho foi avaliar as propriedades químicas do solo submetido a dois manejos do solo e ao efeito residual de gesso, após 55 meses de implantação dos tratamentos. Desenvolvido em uma área experimental da FCA/UFGD de Dourados, MS, o experimento foi disposto no delineamento de blocos casualizados com os fatores arranjados em parcela subsubdividida. A parcelas, sub-parcelas e sub-subparcelas receberam os níveis dos fatores sistema plantio direto e convencional, gesso e profundidade 0-0,05, 0,05-0,10, 0,10-0,15, 0,15-0,20 e 0,20-0,30 m, respectivamente, com quatro repetições. Não houve efeito residual de gesso para cálcio. O plantio direto com efeito residual de gesso aumentou o teor de potássio, enxofre e reduziu a acidez potencial. O plantio convencional com efeito residual de gesso aumentou a acidez potencial do solo. O plantio direto promoveu aumento de cálcio (em 0-0,05 e 0,05-0,10 m), aumento do teor de matéria orgânica (em 0-0,05 m), acúmulo de enxofre (em 0,05-0,10 e 0,10-0,15 m) , aumento da soma de base e saturação por base (em 0,05-0,10 m,) e redução de magnésio (em 0,10-0,15 m), fósforo (em 0,05-0,10 e 0,10-0,15 m), acidez potencial (em 0,05-0,10 m) e CTC (em 0,10-0,15 m). O efeito residual de gesso acumulou mais enxofre e saturação por base na