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Conservation agriculture plays an important role in the sustainability of production systems, notably for globally significant crops such as cotton. This study explores the integration of the no-tillage system (NTS) with integrated pest management (IPM) by incorporating cover crops. The aim is to assess the impact of these living or dead covers on the management of insect populations, the indices diversity of phytophagous insects and natural enemies, and to investigate the population fluctuation of these arthropods, considering a variety of crops in the NTS before and after cotton planting. The trial, conducted over two consecutive cropping seasons in Mato Grosso do Sul State, Brazil, employed a randomised block design with four repetitions. The treatments included cover crops with the highest potential for use in the region, such as millet (Pennisetum glaucum glaucum L.), corn (Zea mays L.), brachiaria (Urochloa ruziziensis), black velvet bean (Stizolobium aterrimum), forage sorghum (Sorghum bicolor L.), and white oats (Avena sativa L.) and a mix of white oats with brachiaria. The results indicated that the black velvet bean stands out as the most effective cover crop, providing the best performance in terms of non-preference to the attack of the evaluated pest insects. Conversely, brachiaria proves to be more susceptible to infestations of Dalbulus maidis (DeLong and Wolcott) (Hemiptera: Cicadellidae), and Diabrotica speciosa (Germar, 1824) (Coleoptera: Chrysomelidae). The study underscores the relevance of the judicious choice of cover crops in IPM and in promoting agricultural biodiversity, creating a strategic tool to enhance the sustainability and efficiency of the cotton production system in the context of the NTS.

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Soil organic carbon is critical to reducing anthropogenic CO2 emissions, highlighting the importance of carbon sequestration on agricultural lands. No-till agricultural practices have been shown to be effective in improving soil quality and sequestering carbon, thereby supporting global efforts to mitigate climate change. Based on the edaphoclimatic conditions of the region, five reference areas were selected, with different characteristics in terms of conditions (A1, A2, A3, A4, and A5) in 5 different farms in the municipality of Rio Verde, GO, Brazil. Soil and biomass samples left by the crop after harvest were collected. These areas represent 3 priority management systems in the Cerrado region of central Brazil, namely: no-till with soybean and maize in sequence in a rainfed system; no-till with soybean and maize in sequence in a central pivot irrigation system; first cut sugar cane; second cut sugar cane. In October 2022, 15 points per area were sampled for soil carbon stock estimation and for chemical and physical characterization purposes along linear transects. Transect sampling approach is widely used in soil attributes studies for comparison and data collection. Biomass samples were used to estimate soil biomass accumulation and carbon stock indices. The physic-chemical parameters of the soil in each area were determined through a complete analysis of the 0-20 cm profile. By presenting a new dataset of soil organic carbon stocks and carbon credits from several long-term no-till areas in central Brazil, this article contributes to the knowledge of the potential of conservation management systems for carbon trading, providing insights into their current contributions and future modelling.

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This study aimed to evaluate the impact of long-term liquid dairy manure (LDM) application on the activity and structure of soil bacterial and archaea communities in two cropping seasons over 1 year of a no-till crop rotation system. The experiment was run in a sandy clay loam texture Oxisol, in Brazil, including LDM doses of 60, 120, and 180 m3 ha-1 year-1, installed in 2005. Soil sampling was conducted during spring 2018 and autumn 2019 at 0-10-cm depth. Microbial biomass carbon and nitrogen, 16S rRNA gene sequencing, microbial respiration and quotient were performed. Over the 14-year period, LDM application increased soil microbial community activity. Analysis of 16S rRNA gene sequencing revealed dominance by Proteobacteria, Acidobacteria, and Actinobacteria phyla (67% in spring and 70% in autumn). Genera Pirulla and Nitrososphaera showed enrichment at LDM doses of 120 and 180 m3 ha-1 year-1 doses, respectively. During spring, following black oat cropping, shifts in the relative abundance of Bacteroidetes, Proteobacteria, Firmicutes, Gemmatimonadetes, Verrucomicrobia, Chloroflexi, Actinobacteria, and AD3 phyla were observed due to LDM application, correlating with soil chemical indicators such as pH, K, Ca, Mn, and Zn. Our findings indicate that plant development strongly influences microbial community composition, potentially outweighing the impact of LDM. Our findings indicate that the application of liquid dairy manure alters the soil bacterial activity and community; however, this effect depends on the developing plant.

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The growth of cover crops can contribute to the increase in phosphorus content at depth by root decomposition. The aim of this work was to verify the effect of cover crops on soil phosphorus availability and use by successive plants, and the accumulation of soil P in a no-tillage system conducted for 14 years. This research was carried out during the 2016/2017 and 2017/2018 crop seasons, whose treatments have been installed and maintained since 2003. The experimental design was a randomized block design, and the plots consisted of spring crops: pearl millet, forage sorghum, sunn hemp, and additionally, a fallow/chiseling area. The evaluation of available P was determined by P fractionation. In general, in the two years of evaluation, the accumulation of P in the shoot dry matter was higher in sunn hemp growth, on average 25% higher than pearl millet in 2016 and 40% higher than sorghum in 2017. The highest contents of labile inorganic P were in the sorghum-soybean and fallow/chiseling-soybean successions, with values higher than 50 mg kg-1 of P in the 0-0.1 m soil layer. However, in the other layers analyzed, the cover crops obtained higher availability of labile inorganic P. The systems using cover crops recovered 100% of the P fertilized in soybean.

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Edaphic factors can modulate the effects of microbial inoculants on crop yield promotion. Given the potential complexity of microbial inoculant responses to diverse soil management practices, we hypothesize that sustainable management of soil and water irrigation may improve soil quality and enhance the effects of plant growth-promoting bacteria (PGPB). Consequently, the primary objective was to assess the effectiveness of microbial inoculants formulated with Herbaspirillum seropedicae (Hs) and Azospirillum brasilense (Ab) on maize growth in soils impacted by different historical conservation management systems. We evaluated two soil management systems, two irrigation conditions, and four treatments: T0 - without bioinoculant and 100% doses of NPK fertilization; T1 - Hs + humic substances and 40% of NPK fertilization; T2 - Ab and 40% of NPK fertilization; T3 - co-inoculation (Hs + Ab) and 40% of NPK fertilization. Using a reduced fertilization dose (40% NPK) associated with microbial inoculants proved efficient in increasing maize shoot dry mass : on average, there was a 16% reduction compared to the treatment with 100% fertilization. In co-inoculation (Hs + Ab), the microbial inoculants showed a mutualistic effect on plant response, higher than isolate ones, especially increasing the nitrogen content in no-tillage systems irrigated by swine wastewater. Under lower nutrient availability and higher biological soil quality, the microbial bioinputs positively influenced root development, instantaneous water use efficiency, stomatal conductance, and nitrogen contents.

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Argentina is a Latin American country which encounters soil degradation problems. The most productive regions have implemented conservative land practices (no-till). However, agricultural frontier has been displaced to marginal lands with arid and semiarid climates, with the consequent disappearance in many areas of native forest and land degradation. In this work, the fallout of gamma-emitting radionuclides, 137Cs and 7Be, was jointly used to assess changes in soil erosion in a recently converted semiarid ecosystem into agricultural land. 137Cs was utilized to estimate the erosion over the past 60 years, whereas 7Be was employed to estimate the erosion after the conversion of the area to cultivated land and soil tillage. For 137Cs the Proportional Model (PM), the Mass Balance Model II (MBMII) and the MODERN model were used, for 7Be the Profile Distribution Model (PDM) and the MODERN model were used. 137Cs indicates mean erosional rates of 8.2, 10.5 and 6.5 Mg ha-1 a-1, using MBMII, PM and MODERN, respectively, and that a soil layer between 0.5 and 0.8 mm was annually lost by erosion. By applying a 7Be tracer, we measured erosion rates of 2.4 and 3.3 Mg ha-1 (with PDM and Modern, respectively), indicating the loss of the upper 0.2 mm of soil. This erosion can be attributed to a few heavy rainfalls that occurred within the past 90 days. The results suggest that current land management practices have led to an increase in soil erosion. This could be attributed to the fact that the soil remains bare after crop harvest, which may compromise its conservation and future productivity.

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Soil management systems can directly interfere with crop yield via changes in the soil's physical and hydraulic properties. However, short- to medium-term experiments of conduction do not always demonstrate the modifications of the management systems in these properties. Thus, the aim of this study was to evaluate the physical properties of the soil in a long-term management system and to relate it to the storage and availability of water to plants, verifying its effect on soybean yield. The experiment was conducted in randomized blocks in a split-plot scheme with four replications. Plots were composed by soil management (conventional tillage and no-tillage), and subplots represented three soil depths (0.0-0.1, 0.1-0.2, and 0.2-0.4 m). The soil's physical and hydraulic properties, root development, and soybean yield were evaluated. The no-tillage system not only presented higher bulk density and soil resistance to compaction up to a depth of 0.2 m but also greater root development. This management also did not affect the process of water infiltration in the soil and presented an increase in soybean grain yield by 6.5%. The long-term no-tillage system (33 years) offers less risk of water stress to soybean plants; it contributes to greater grain yield of this crop when compared to the conventional tillage system.

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The bulk density values indicative of compaction in clayey soils correspond to a wide range of values (1.30-1.47 Mg m-3), due to the diverse types of soil management. Our hypothesis is that if we consider bulk density values within similar management groups (those that fall to the ground and those that do not fall), the values will be more accurate within each management group. Our objective in this work was to analyze using the concepts of (Yates & Cochran, 1938; Whitehead, 2002) what is a suitable statistical way of grouping these results to reach a consensus regarding a tested hypothesis, the greatest number of density values surveyed between 1977 and 2021, considered for the study of compaction in clayey Oxisols under different managements, to verify whether our hypothesis will be confirmed. We selected 1,521 studies with bulk densities in the literature, corresponding to 44 years (1977 and 2021), which were analyzed by a statistical technique that integrates the results of two or more independent studies on the same subject and combines them into a summary measure (portion forestry). From the data collected in the literature, it was possible to separate two groups of bulk density and management in clayey soils indicative of compaction: the managements that perform little or no manipulation of the soil, such as pasture and no-tillage, densities between 1.41-1.45 Mg.m-3 (average 1.43 Mg m-3), and for the others, such as conventional plowing and minimum tillage, soil densities between 1.31-1.38 Mg.m-3 (average 1.35 Mg m-3). Finally, we conclude that compaction must be analyzed considering the texture and type of soil management.(AU)

Os valores de densidade do solo indicativos de compactação em solos argilosos correspondem a uma ampla faixa de valores (1,30-1,47 Mg m-3), devido aos diversos tipos de manejo do solo. Nossa hipótese é que se considerarmos os valores de densidade do solo dentro de grupos de manejo semelhantes (os que caem no chão e os que não caem), os valores serão mais precisos dentro de cada grupo de manejo. Nosso objetivo neste trabalho foi analisar usando os conceitos de (Yates & Cochran, 1938; Whitehead, 2002) qual é uma forma estatística adequada de agrupar esses resultados para chegar a um consenso sobre uma hipótese testada, o maior número dos valores de densidade levantados entre 1977 e 2021, considerados para o estudo da compactação em Latossolos argilosos sob diferentes manejos, para verificar se nossa hipótese será confirmada. Selecionamos 1.521 estudos com densidades do solo na literatura, correspondentes a 44 anos (1977 e 2021), que foram analisados por uma técnica estatística que integra os resultados de dois ou mais estudos independentes sobre o mesmo assunto e os combina em uma medida resumida (forest plot). A partir dos dados levantados na literatura, foi possível separar dois grupos de densidade do solo e manejo em solos argilosos indicativos de compactação: os manejos que realizam pouca ou nenhuma manipulação do solo, como pastagem e plantio direto, densidades entre 1,41 -1,45 Mg.m-3 (média 1,43 Mg m-3), e para as demais, como aração convencional e preparo mínimo, densidades de solo entre 1,31-1,38 Mg.m-3 (média 1,35 Mg m-3). Por fim, concluímos que a compactação deve ser analisada considerando a textura e o tipo de manejo do solo.(AU)

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Glyphosate-resistant weeds are difficult to manage and can serve as hosts for pests that threaten cultivated crops. Chrysodeixis includens (Walker) (Lepidoptera: Noctuidae) is one of the main polyphagous pests of soybean in Brazil that can benefit from weeds' presence during season and off-season. Despite its pest status, little is known about C. includens survival and development on alternative hosts, including those resistant to glyphosate. Therefore, we assessed the biology, reproduction, preference, and survival at different feeding periods of C. includens on seven glyphosate-resistant weeds (Sumatran fleabane, Italian ryegrass, sourgrass, goosegrass, smooth pigweed, wild poinsettia, hairy beggarticks) commonly found in Brazilian agroecosystems, under laboratory conditions. Our results showed that C. includens survival and reproduction were similar on soybean and wild poinsettia. Survival and reproduction were lower on smooth pigweed and hairy beggarticks. Also, these plants prolonged the larval stage. Larvae did not pupate when fed on sourgrass, goosegrass, Italian ryegrass, and Sumatran fleabane. However, on Sumatran fleabane their biomass was higher. The mean generation time was lower on wild poinsettia. This weed was preferred to soybean. An antifeeding factor was observed on Sumatran fleabane. Larvae fed for 11 days on soybean, wild poinsettia and smooth pigweed developed into pupae. In agricultural systems, farmers must pay attention to the management of these weeds, especially wild poinsettia, smooth pigweed, and hairy beggarticks, to interrupt the cycle of this pest, since these plants can serve as main sources of infestation for the soybean crop.

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ABSTRACT: With the gradual transfer of an enormous young and middle age labor force from agricultural field to non-agricultural sectors, the negative role of land fragmentation (LF), which is related to food security, is increasingly reflecting in the process of agricultural modernization. Meanwhile, the positive roles of farmers' combined-tillage in production are gradually emerging. Based on the above background, this study explained the relationship among farmers' combined-tillage, LF and agricultural production efficiency (APE). The study used survey date and the SFA-QR model to empirically investigate the effects of LF and farmers' combined-tillage on APE. Furthermore, this article analyzed the moderating effect of farmers' combined-tillage on the relationship between LF and APE. The results demonstrated that: (1) Farmers combined-tillage improves the APE significantly, especially on low and medium efficiency households; (2) LF has a negative impact on APE, especially on low and medium efficiency households; (3) Combined-tillage could alleviate the adverse effects of LF on APE. In this regard, the paper also proposed some suggestions to face the adverse effects of LF and promote farmers' combined-tillage in production.

RESUMO: Com a transferência gradual de enorme força de trabalho jovem e de meia idade do campo agrícola para os setores não agrícolas, o papel negativo da fragmentação da terra (LF), relacionada à segurança alimentar, está cada vez mais refletido no processo de modernização agrícola. Enquanto isso, os papéis positivos da lavoura combinada dos agricultores na produção estão surgindo gradualmente. Com base no histórico acima, o objetivo deste estudo é explicar a relação entre o plantio direto dos agricultores, LF e eficiência da produção agrícola (APE). O estudo usou dados do levantamento e o modelo SFA-QR para investigar empiricamente os efeitos da FL e do plantio direto dos agricultores sobre o APE. Além disso, este artigo analisou o efeito moderador do plantio combinado dos agricultores na relação entre LF e APE. Os resultados demonstram que: (1) A lavoura combinada dos agricultores melhora significativamente o APE, especialmente em domicílios de baixa e média eficiência; (2) LF tem um impacto negativo na APE, especialmente em domicílios de baixa e média eficiência; (3) A lavoura combinada pode aliviar os efeitos adversos do LF no APE. Nesse sentido, o trabalho também propõe algumas sugestões para enfrentar os efeitos adversos da FL e promover o plantio combinado dos agricultores na produção.

RESUMEN

A utilização de plantas de cobertura de solo, em especial de verão em janelas entressafras, é uma prática pouco comum por competirem com as culturas de importância econômica. O objetivo foi avaliar o uso de plantas de cobertura, na cobertura do soloe supressão de plantas espontâneas na entressafra milho-trigo no noroeste do Rio Grande do Sul. Para isso, utilizou-se crotalária espectabilis, mucuna-cinza, feijão-de-porco, tremoço, trigo-mourisco, milheto, consórcio de milheto e crotalária (50%) e pousio (testemunha). As espécies foram semeadas após a colheita do milho safra com 0,45 m de espaçamento entre linhas em blocos ao acaso com seis repetições. A taxa de cobertura do solo foi analisada aos 30, 45, 60, 75 e 90 dias após a semeadura. A matéria seca foi determinada na plena floração de cada cultura, separada em talos/colmos e folhas e secos a 65ºC. A incidência de plantas espontâneas foi avaliada no momento de plena floração. No período entressafra o milheto, consórcio de milheto + crotalária, mucuna-cinza e feijão-de-porco apresentam maior eficiência de cobertura do solo, ambos atingindo 100% de cobertura de solo. Os maiores acúmulos de matéria seca foram do milheto (11.204 kg.ha-1) e consórcio (9291 kg.ha-1). As culturas mais eficientes para a supressão de plantas espontâneas foram o milheto, o consórcio e a mucuna-cinza. A crotalária e trigo-mourisco apresentarambaixo desempenho, logo, não são recomendadas para cultivo solteiro na entressafra milho-trigo.(AU)

The use of cover crops, especially in summer in off-season, is an uncommon practice because they compete with crops of economic importance. The objective was to evaluate the use of cover crops, soil cover and suppression of weeds in the corn-wheat off-season in northwest of Rio Grande do Sul. For this, sunn hemp, gray mucuna, jack bean, lupine, buckwheat, millet, millet, and sunn hemp intercrop (50%) and fallow (control) were used. The species were sown after harvesting the corn crop with 0.45 m spacing between rows in randomized blocks with six replications. The soil cover rate was analyzed at 30, 45, 60, 75 and 90 days after sowing. Dry matter was determined at full flowering of each crop, separated into stalks/stems and leaves, and dried at 65ºC. The incidence of weeds was evaluated at the time of full flowering. In the off-season, millet, millet + crotalaria, gray mucuna and jack bean intercropped have greater soil cover efficiency, both reaching 100% soil cover. The highest accumulations of dry matter were from millet (11,204 kg.ha-1) and intercropped (9291 kg.ha-1). The most efficient crops for the suppression of weeds were pearl millet, intercropped and gray mucuna. Sunn hemp and buckwheat showed low performance; therefore, they are not recommended for single cultivation in the corn-wheat off-season.(AU)

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The knowledge and characterization of aggregate stability are relevant to select adequate management and to avoidits degradation. Thus, this studyaimed to characterize the spatial variability of aggregate stability in cohesive soilsunder crop conservation systems. The experiment was performed intwo different areas of soybean production: no-tillage System (NTS) and livestock farming integration system (LFI), In each production area, a sampling mesh composed of 50 collection points, with a regular spacing of 40 m, at 0.00-0.20 mdepth, wascarried out. The results were expressed as a percentage of aggregates retained in sieves 2; 1; 0.5 and 0.25 mm, the values obtained were used to calculate the Mean Geometric Diameter (MGD) and Mean Weight Diameter (MWD). In the LFI system, which had a strong degree of spatial dependence (DSD), the attributes showed a moderate DSD, except for MWD. Generally, the reachedvalues of the attributes in the LFI system were lower than those found in the NTS system, showing less variability in the management system with no-tillage. Spatial distribution of the kriging maps demonstrated the LFI system leading to the formation of larger aggregates in the soil when compared to ones to the same attributes in the NTS. All attributes showed a strong to moderatespatial dependence. The soil managed with the LFI system revealed greater aggregate stability when compared to the NTS, which in turn presented less spatial variability than the LFI system and shows a more homogeneous soil.(AU)

O conhecimento e a caracterização da estabilidade dos agregados são relevantes para selecionar um manejo adequado e evitar sua degradação. Portanto, este estudoteve como objetivo caracterizar a variabilidade espacial da estabilidade de agregados em solos coesos sob sistemas de conservação de culturas. O experimento foi conduzido em duas áreas distintas de produção de soja: sistema de plantio direto (NTS) e sistema de integração pecuária (LFI). Foi realizada uma amostragem de 50 pontos de coleta, com espaçamento regular de 40 m, na profundidade de 0,00-0,20 m, em cada área de produção.Os resultados foram expressos como porcentagem de agregados retidos nas peneiras 2; 1; 0,5 e 0,25 mm, os valores obtidos foram utilizados para calcular o Diâmetro Médio Geométrico (DMM) e o Diâmetro Peso Médio (DMM). No sistema LFI, que possuía alto grau de dependência espacial (DDS), os atributos apresentaram um DSD moderado, exceto para MWD. De maneira geral, os valores de escopo dos atributos no sistema LFI foram inferiores aos encontrados no sistema NTS, apresentando menor variabilidade no sistema de manejo do plantio direto. A distribuição espacial dos mapas de krigagem mostrou que o sistema LFI leva à formação de agregados maiores no solo em comparação com outros com os mesmos atributos no NTS. Todos os atributos apresentaram dependência espacial de forte a moderada. O solo manejado com o sistema LFI revelou maior estabilidade dos agregados em relação ao NTS, que por sua vez apresentou menor variabilidade espacial do que o sistema LFI e apresenta um solo mais homogêneo.(AU)

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With the gradual transfer of an enormous young and middle age labor force from agricultural field to non-agricultural sectors, the negative role of land fragmentation (LF), which is related to food security, is increasingly reflecting in the process of agricultural modernization. Meanwhile, the positive roles of farmers' combined-tillage in production are gradually emerging. Based on the above background, this study explained the relationship among farmers' combined-tillage, LF and agricultural production efficiency (APE). The study used survey date and the SFA-QR model to empirically investigate the effects of LF and farmers' combined-tillage on APE. Furthermore, this article analyzed the moderating effect of farmers' combined-tillage on the relationship between LF and APE. The results demonstrated that: (1) Farmers combined-tillage improves the APE significantly, especially on low and medium efficiency households; (2) LF has a negative impact on APE, especially on low and medium efficiency households; (3) Combined-tillage could alleviate the adverse effects of LF on APE. In this regard, the paper also proposed some suggestions to face the adverse effects of LF and promote farmers' combined-tillage in production.

Com a transferência gradual de enorme força de trabalho jovem e de meia idade do campo agrícola para os setores não agrícolas, o papel negativo da fragmentação da terra (LF), relacionada à segurança alimentar, está cada vez mais refletido no processo de modernização agrícola. Enquanto isso, os papéis positivos da lavoura combinada dos agricultores na produção estão surgindo gradualmente. Com base no histórico acima, o objetivo deste estudo é explicar a relação entre o plantio direto dos agricultores, LF e eficiência da produção agrícola (APE). O estudo usou dados do levantamento e o modelo SFA-QR para investigar empiricamente os efeitos da FL e do plantio direto dos agricultores sobre o APE. Além disso, este artigo analisou o efeito moderador do plantio combinado dos agricultores na relação entre LF e APE. Os resultados demonstram que: (1) A lavoura combinada dos agricultores melhora significativamente o APE, especialmente em domicílios de baixa e média eficiência; (2) LF tem um impacto negativo na APE, especialmente em domicílios de baixa e média eficiência; (3) A lavoura combinada pode aliviar os efeitos adversos do LF no APE. Nesse sentido, o trabalho também propõe algumas sugestões para enfrentar os efeitos adversos da FL e promover o plantio combinado dos agricultores na produção.

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O dejeto de suíno (DLS) é usado como fertilizante cujos nutrientes são perdidos por erosão e contaminam o ambiente se o dejeto é usado inadequadamente. Objetivou-se avaliar o efeito de DLS nosolo e na erosão, num Nitossolo Bruno. Os tratamentos, 0; 50; 100; e 200 m³ ha-1de DLS foram aplicados superficialmente após a semeadura uma vez em cada um dos cinco cultivos, e na palhada do último cultivo, totalizando 0, 250, 500 e 1000 m³ ha-1, na aveia (Avena strigosa), milho (Zea mays), nabo (Raphanus sativus L.) e soja (Glycine max), e nos resíduos de aveia. A chuva simulada (65 mm h-1e 75 minutos) foi aplicada três vezes no milho e quatro vezes no nabo, na soja, e nos resíduos, com um simulador debraços rotativos. Antes e depois da pesquisa, determinou-se o teor de K, Ca e Mg no solo. As chuvas aplicadas em cada momento compuseram um teste (T). O T1 ocorreu após a aplicação do DLS e os demais testes em intervalos que variaram entre 14 e 70 dias, em função do clima. Durante o escoamento, em intervalos de cincominutos coletaram-se amostras de enxurrada para determinar as perdas de água e o teor de K, Ca e Mg na água. O DLS não influenciou o teor dos nutrientes no solo. O teore as perdas totais dos nutrientes foram maiores com 1000 m3ha-1de DLS do que na ausência do dejeto. Com o aumento de escoamento, diminuiu o teor na enxurrada e aumentou a perda total, a qual aumentou também com o aumento de teor dos nutrientes na enxurrada. Recomenda-se aplicar menos do que 500 m3ha-1de DLS total no solo, mesmo em aplicações intervalares, devido à elevada perda de K, Ca e Mg pela erosão hídrica.(AU)

Pigg slurry (PS) is used as a fertilizer whose nutrients are lost through erosion and contaminate the environment if the manure is used inappropriately. The objective was to evaluate the effect of PS on soil and erosion, in a Alfisol soil. The treatments, 0; 50; 100; and 200 m³ ha-1of PS were applied superficially after sowing once in each of the five crops, and in the straw of the last crop, totaling 0, 250, 500 and 1000 m³ ha-1, in oat (Avena strigosa), corn (Zea mays), turnip (Raphanus sativusL.) and soybean (Glycine max), and in oat residues. The simulated rain (65 mm h-1and 75 minutes) was applied three times to corn and four times to turnip, soybeans, and residues, with a rotating arms simulator. Before and after the research, the content of K, Ca and Mg in thesoil was determined. The rainfall applied at each moment made up a test (T). T1 occurred after the application of the PS and the other tests at intervals that varied between 14 and 70 days, depending on the weather. During the runoff, at five-minute intervals, runoff samples were collected to determine water losses and the content of K, Ca and Mg in the water. The PS did not influence the nutrient content in the soil. The content and total losses of nutrients were higher with 1000 m3ha-1of PS than in theabsence of manure. With the increase in runoff, the content inthe runoff decreased and the total loss increased, which also increased with the increase in the nutrient content in the runoff. It is recommended to apply less than 500 m3ha-1of total PS inthe soil, even in interval applications, due to the high loss of K, Ca and Mg by water erosion.(AU)

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Pigg slurry (PS) is used as a fertilizer whose nutrients are lost through erosion and contaminate the environment if the manure is used inappropriately. The objective was to evaluate the effect of PS on soil and erosion, in a Alfisol soil. The treatments, 0; 50; 100; and 200 m³ ha-1 of PS were applied superficially after sowing once in each of the five crops, and in the straw of the last crop, totaling 0, 250, 500 and 1000 m³ ha-1, in oat (Avena strigosa), corn (Zea mays), turnip (Raphanus sativus L.) and soybean (Glycine max), and in oat residues. The simulated rain (65 mm h-1 and 75 minutes) was applied three times to corn and four times to turnip, soybeans, and residues, with a rotating arms simulator. Before and after the research, the content of K, Ca and Mg in the soil was determined. The rainfall applied at each moment made up a test (T). T1 occurred after the application of the PS and the other tests at intervals that varied between 14 and 70 days, depending on the weather. During the runoff, at five-minute intervals, runoff samples were collected to determine water losses and the content of K, Ca and Mg in the water. The PS did not influence the nutrient content in the soil. The content and total losses of nutrients were higher with 1000 m3 ha-1 of PS than in the absence of manure. With the increase in runoff, the content in the runoff decreased and the total loss incr

O dejeto de suíno (DLS) é usado como fertilizante cujos nutrientes são perdidos por erosão e contaminam o ambiente se o dejeto é usado inadequadamente. Objetivou-se avaliar o efeito de DLS no solo e na erosão, num Nitossolo Bruno. Os tratamentos, 0; 50; 100; e 200 m³ ha-1 de DLS foram aplicados superficialmente após a semeadura uma vez em cada um dos cinco cultivos, e na palhada do último cultivo, totalizando 0, 250, 500 e 1000 m³ ha-1, na aveia (Avena strigosa), milho (Zea mays), nabo (Raphanus sativus L.) e soja (Glycine max), e nos resíduos de aveia. A chuva simulada (65 mm h-1 e 75 minutos) foi aplicada três vezes no milho e quatro vezes no nabo, na soja, e nos resíduos, com um simulador de braços rotativos. Antes e depois da pesquisa, determinou-se o teor de K, Ca e Mg no solo. As chuvas aplicadas em cada momento compuseram um teste (T). O T1 ocorreu após a aplicação do DLS e os demais testes em intervalos que variaram entre 14 e 70 dias, em função do clima. Durante o escoamento, em intervalos de cinco minutos coletaram-se amostras de enxurrada para determinar as perdas de água e o teor de K, Ca e Mg na água. O DLS não influenciou o teor dos nutrientes no solo. O teor e as perdas totais dos nutrientes foram maiores com 1000 m3 ha-1 de DLS do que na ausência do dejeto. Com o aumento de escoamento, diminuiu o teor na enxurrada e aumentou a perda total, a qual aumentou também

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ABSTRACT: Weedy rice (Oryza sativa L.) is the most problematic weed in rice fields due to the few control management alternatives to control it, because of the genetic similarity with the crop. Different cropping systems (regarding soil preparation before sowing) have been used as options to control the persistence and emergence of the weed seedbank. Therefore, the objective of this study was to evaluate the longevity and vertical distribution of weedy rice seeds in the soil seedbank after 22 years of different rice cropping systems. Data was analyzed as a two-way factorial, with cropping systems carried out for 22 years [no-tillage (NT), conventional tillage (CT), wet direct-seeded (WDS)] as one factor and sampling depth (0-2, 2-5, 5-10 and 10-20 cm) as the other factor. The number of whole and deteriorated seeds per m-2 were assessed, as well as the viability (%). No effect between the systems were detected up to 5 cm, however at 5-10 cm CT and WDS showed higher amount of seeds, and WDS at 10-20 cm. As the sampling depth increased, NT showed fewer amount of seeds, while less reduction of the soil seedbank was observed in WDS. CT and WDS spread viable seeds in the soil profile from 0 to 20 cm depth. After 22 years there are viable weedy rice seeds up to 10 cm of depth in the three cropping systems and there is no difference among them up to 5 cm of depth, demonstrating the serious problem of the seedbank for this species.

RESUMO: O arroz daninho (Oryza sativa L.) é a principal planta daninha do arroz cultivado e, devido à similaridade genética com a cultura, são poucas as alternativas de controle. Uma possibilidade são os sistemas de cultivo, em razão da influência na emergência e sobrevivência da espécie no banco de sementes do solo. Diante disso, o trabalho objetivou avaliar a longevidade e a distribuição das sementes de arroz daninho no perfil do solo, após 22 anos de cultivo, sob diferentes sistemas. Os tratamentos foram arranjados em esquema fatorial, em que o fator A foi composto por três sistemas de cultivo, realizados consecutivamente durante 22 anos, sendo esses: semeadura direta (SD), sistema convencional (SC) e pré-germinado (PG); e, o fator B composto por quatro profundidades de amostragem: 0-2, 2-5, 5-10 e 10-20 cm. As variáveis avaliadas foram: o número de sementes íntegras e deterioradas m-2; e, a porcentagem de viabilidade. Não foi verificado efeito dos sistemas até 5 cm, mas a 5-10 cm SC e PG mostraram maior quantidade de sementes, e PG a 10-20 cm. A SD proporcionou diminuição de sementes íntegras conforme aumentou a profundidade de amostragem, enquanto o sistema PG elimina menos sementes do banco de sementes do solo. Os sistemas SC e PG distribuem sementes viáveis no perfil do solo de 0 a 20 cm de profundidade. Após 22 anos, nos três sistemas de cultivo há sementes de arroz daninho viáveis até 10 cm de profundidade, sendo igual a quantidade de sementes viáveis até cinco centímetros de profundidade.

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Background: Agriculture is essential for food security. However, conventional agriculture alters the water and carbon cycle and soil properties. We investigated the effect of conventional management (CM) and sustainable management (SM) on the carbon and water cycle in crops of nopal (Np) and wheat (Wh). Methods: A micrometeorological eddy covariance tower was installed to measure water use through evapotranspiration (ET) and the net exchange of CO2 during the crop's development. Gross primary productivity (GPP), water use efficiency (WUE), and soil properties were obtained. Results: The results showed that both agricultural managements influenced the carbon flux of the ecosystem, with a lower GPP and Reco in the nopal field (1.85 and 0.99 mmol C m-2 s-1, respectively), compared to the wheat field (6.34 and 1.8 mmol C m-2 s-1, respectively). It was mainly attributed to the metabolic plant differences, phenological stages, and wheat biomass developed during the winter. On the other hand, the accumulated ET in the SM-Wh plots was lower than SM-Np. Therefore, the crops subjected to sustainable practices use water more efficiently with 1.42 and 1.03 g C m-3 H2O for nopal and wheat, respectively. In regard to soil properties, it was observed that tillage alters microbial activity affecting organic matter and carbon. It can be concluded that the differences in agricultural management for both crops altered the carbon and water cycle and soil quality. In addition, implementing good agricultural practices allows more efficient use of water by the plant, higher retention of water in the soil, and less ET.

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Increasing the diversity of plant species in agricultural production areas favors the maintenance or improvement of soil quality, particularly for soils with a sandy texture. This beneficial effect is related to the formation of aggregates of different origins. This study aimed to (i) verify whether soil use and management affect the proportion of biogenic (Bio) and physicogenic (Phy) aggregates and (ii) verify whether biogenic aggregation is more likely to lead to soil improvement than physicogenic aggregation. Three management systems were evaluated (permanent pasture, PP; no-tillage system, NT; and no-tillage + Brachiaria system, NT + B) as well as a reference area (Atlantic Forest biome vegetation, NF). According to their origin or formation pathway, the aggregates were separated, identified, and classified as Bio (formed by biological processes) and Phy (resulting from chemical and physical actions). The differentiation between Bio and Phy aggregates was performed based on the visualization of morphological features, such as shape, size, presence of roots, porosity, and subunit arrangements, and junctions. Only the PP area was able to promote greater aggregate formation of biological origin, with greater amounts of Bio aggregates. The highest total organic carbon (TOC) contents and the least negative δ13C values were also quantified in the aggregates of the PP area. The NT + B system provided an increase in the TOC content of its aggregates in comparison with aggregates in the NT and NF areas. Among the formation pathways, the Bio aggregates had the highest TOC and soil organic matter fractions contents and the most negative δ13C values. Perennial forage grasses vegetation was more important than the plant species diversity in favoring Bio aggregate formation. The beneficial effect of Brachiaria can be observed when incorporated as part of intercropping with corn in grain production systems. The biogenic aggregates favored the concentration of more labile soil organic matter fractions. The results of this study can provide important theoretical information for future studies focused on the combination of different plant species in agricultural food production areas on sandy-textured soils.

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This study aimed to evaluate the occurrence of mycorrhizal fungi and glomalin content in soil under different cover crops with and without the application of nitrogen in the cover. The following cover plants were used: Crotalaria juncea (Crotalaria juncea L.), wild beans from Ceará (Canavalia brasiliensis Mart. ex Benth.), Guandú 'BRS mandarin' [Cajanus cajan (L.) Millsp.], millet 'BR05' [Pennisetum glaucum (L.) R.Br.] and sorghum 'BR 304' [Sorghum bicolor (L.) Moench]. The absolute control of the experiment was the treatment without the use of cover crops, that is, the vegetation of spontaneous occurrence in the area. The experimental design was randomized blocks in subplots with three replications. Spore density, mycorrhizal colonization rate, easily extractable glomalin, and species present in the rhizosphere of the cover crops were determined. No differences were found in the diversity of mycorrhizal fungi associated with the different cover crops studied or in the values of spore density, root colonization, or glomalin content. Nitrogen application did not influence the mycorrhizal activity in the investigated cover crops. The most frequent species associated with cover crops were Scutellospora pellucida and Scutellospora persica in C. juncea; Gigaspora sp. on Sorghum; Glomus macrocarpum in Guandu; G. macrocarpum and Glomus clavisporum in millet; and Glomus microaggregatum and Glomus tortuosum in Spontaneous Vegetation.

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Soils are dynamic and complex systems in their natural state, which are subjected to profound changes due to management. Additionally, agricultural soils are continuously exposed to wetting and drying (W-D) cycles, which can cause modifications in the complexity of their pores. Thus, we explore how successive W-D cycles can affect the pore network of an Oxisol under contrasting managements (conventional tillage-CT, minimum tillage-MT, no tillage-NT, and secondary forest-F). The complexity of the soil pore architecture was evaluated using a 3D multifractal approach combined with lacunarity, Shannon's entropy, and pore geometric parameters. Our results showed that the multifractal approach effectively identified and quantified the changes produced in the soil pore architecture by the W-D cycles. The lacunarity curves revealed important aspects of the modifications generated by these cycles. Samples under F, NT, and MT suffered the most significant changes. Pore connectivity and tortuosity were largely affected by the cycles in F and NT. Our findings demonstrated that the 3D geometric parameters and normalized Shannon's entropy are complementary types of analysis. According to the adopted management, they allowed us to separate the soil into two groups according to their similarities (F and NT; CT and MT).

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