Adaptation of the TIMBRE methodology for brownfields gully erosion analysis in urban areas.

Soil erosion is a concern in many parts of the world, causing environmental and social impacts. Aiming at obtaining indicators of the recovery of brownfields created by gullies in urban areas, this study adapts the Tailored Improvement of Brownfield Regeneration in Europe (TIMBRE) for the analysis and classification of areas affected by gullies in the city of Bauru, Brazil. The TIMBRE methodology assists in the decision-making of priority areas for remediation and their reinsertion in urban spaces. The inventory of areas affected by gullies was compiled based on the analysis of two image sets (2004 and 2020) available on Google Earth. For the classification of brownfields, three classes were considered: Class 1 - local potential for business development, Class 2 - attractiveness and marketing, and Class 3 - environmental risks. These results demonstrate a correlation between gullies and urban expansion. The inventory identified 175 gullies in the municipality's urban perimeter in 2004, which affected an area of over 64 ha. In 2020, the number of gullies increased to 189, but the affected area decreased to 62 ha due to the recovery of some large gullies. The proposed methodology identified the area of Quinta da Bela Olinda as the one with the highest scores in all three classifications. Quinta da Bela Olinda is the location that has a local potential for business development, as it is the most attractive brownfield, as well as the area with the highest environmental risk. This area should, thus, be prioritized by public management for remediation. In conclusion, the proposed method of analysis can be transferred to other areas with adaptations in the criteria used and, therefore, may facilitate the management of urban areas affected by gullies in other places around the world.

Total environment sentinels: Dragonflies as ambivalent/amphibiotic bioindicators of damage to soil and freshwater.

Discerning the impact of anthropogenic impacts requires the implementation of bioindicators that quantify the susceptibilities and vulnerabilities of natural terrestrial and aquatic ecosystems to perturbation and transformation. Although legal regulations in Brazil recognize the value of bioindicators in monitoring water quality, the depreciation of soil conditions has yet to receive adequate attention. Thus, our study aimed to evaluate the potential of odonates (dragonflies and damselflies) as amphibiotic bioindicators to reflect the correlation between the degradation of aquatic and terrestrial habitats in pasture-dominated landscapes. We assessed the relationship between the biotic indices of Odonata and the conservation status of preserved riparian landscapes adjacent to anthropogenically altered pastures in 40 streams in the Brazilian savannah. Our results support the hypothesis that Odonata species composition may be a surrogate indicator for soil and water integrity, making them promising sentinels for detecting environmental degradation and guiding conservation strategies in human-altered landscapes. Importantly, while the Zygoptera/Anisoptera species ratio is a useful bioindicator tool in Brazilian forest, it is less effective in the open savannah here, and so an alternative index is required. Importantly, while the Zygoptera/Anisoptera species ratio is a useful bioindicator tool in Brazilian forest, it is less effective in the open savannah here, and so an alternative index is required. On the other hand, our results showed the Dragonfly Biotic Index to be a suitable tool for assessing freshwater habitats in Brazilian savannah. We also identified certain bioindicator species at both ends of the environment intactness spectrum.

Grazing exclusion-induced changes in soil fungal communities in a highly desertified Brazilian dryland.

Soil desertification poses a critical ecological challenge in arid and semiarid climates worldwide, leading to decreased soil productivity due to the disruption of essential microbial community processes. Fungi, as one of the most important soil microbial communities, play a crucial role in enhancing nutrient and water uptake by plants through mycorrhizal associations. However, the impact of overgrazing-induced desertification on fungal community structure, particularly in the Caatinga biome of semiarid regions, remains unclear. In this study, we assessed the changes in both the total fungal community and the arbuscular mycorrhizal fungal community (AMF) across 1. Natural vegetation (native), 2. Grazing exclusion (20 years) (restored), and 3. affected by overgrazing-induced degradation (degraded) scenarios. Our assessment, conducted during both the dry and rainy seasons in Irauçuba, Ceará, utilized Internal Transcribed Spacer (ITS) gene sequencing via Illumina® platform. Our findings highlighted the significant roles of the AMF families Glomeraceae (∼71% of the total sequences) and Acaulosporaceae (∼14% of the total sequences) as potential key taxa in mitigating climate change within dryland areas. Moreover, we identified the orders Pleosporales (∼35% of the total sequences) and Capnodiales (∼21% of the total sequences) as the most abundant soil fungal communities in the Caatinga biome. The structure of the total fungal community differed when comparing native and restored areas to degraded areas. Total fungal communities from native and restored areas clustered together, suggesting that grazing exclusion has the potential to improve soil properties and recover fungal community structure amid global climate change challenges.

Nickel sources affect soil biological properties but do not affect sorghum growth.

Nickel (Ni) is an essential element, but it can be phytotoxic in high concentration, which may be caused by high availability in soil solution. The objective of this study was to evaluate the effect of sources and doses of Ni applied to a dystrophic Red Latosol cultivated with sorghum on i) the availability of the metal in the soil; ii) the impact on biological and biochemical properties of the soil; iii) the absorption and distribution in sorghum plants; and iv) crop productivity. The experiment was carried out within a completely randomized design with two nickel sources [nickel(II) nitrate, Ni(NO3)2 and nickel(III) oxide, Ni2O3], three doses (35, 70, and 140 mg Ni kg-1 soil), plus controls without Ni, with 3 replications. The concentrations of Ni in the soil, soil microbial biomass (SMB), basal soil respiration (BSR), metabolic quotient (qCO2), fluorescein diacetate (FDA) hydrolysis, and urease activity were determined. The concentrations of Ni in the leaf diagnostic and in the plant (shoot, root, and grains) were also measured. In the soil, the concentrations of available Ni remained between 0.21 and 54.01 mg Ni kg-1. Ni2O3 contributed very little to the increase in available Ni. SMB and the FDA hydrolysis were not affected by the Ni source or Ni dose, but BSR and qCO2 had significant increase with Ni application rates, suggesting the soil microorganisms faced stress. Soil urease activity was affected by Ni dose but not by Ni source. The dose of Ni as Ni(NO3)2 decreased the metal concentration in the plant, while that of Ni2O3 increased it. Nickel source did not affect dry mass production of the plants, but grain yield was affected in a dose-dependent manner when Ni2O3 was the source of Ni.

Development and properties of biodegradable film from peach palm (Bactris gasipaes).

Formulations of biodegradable films using macrocarpa peach palm flour (low amylose starch), chitosan and glycerol, were developed and the effects of the drying temperature on films by assessing their physicochemical, mechanical, barrier, optical, structural, antioxidant properties, and the biodegradability in soil were evaluated. Chitosan enhanced the mechanical properties of the films, but they showed no antimicrobial activity against the tested food-borne pathogens, except for Listeria monocytogenes, for which the inhibition zone was from 0.1 to 0.6 cm. Films with higher concentrations of peach palm flour are opaquer, with better antioxidant characteristics and content of phenolic compounds compared to films made with lower concentrations of flour. The films presented a yellowish color because of the carotenoids found in peach palm flour, 29.63 µg 100 g-1, and exhibited a C-type X-ray pattern, characteristic peak of materials where amylose and amylopectin are present. After 15 days in soil, the films lost 30% of their initial weight. Therefore, these results suggest that the development of films as food preservative is a promising field and that the material used in the study are suitable for their formulation.

Soil physicochemical properties change by age of the oil palm crop.

For decades there have been controversies related to the changes generated by oil palm plantations in the physicochemical properties of the soil, soil biota, and ecological interactions. Therefore, the present investigation evaluated root diameter and biomass at three ages of oil palm cultivation. Besides, we evaluated the effect of the ages on the physicochemical parameters of the soil in comparison with pasture plots. To know the diameter, fresh, and dry biomass of roots, soil sampling was carried out around the oil palm (3-, 5-, and 15-years-old) at distances of 1, 2, and 3 m from the trunk plant. Also, to know the changes in the properties of the soil, the sampling was carried out randomly in the same plots and the pasture plot (control). The results showed that both the diameter and the fresh and dry root biomass increased in 15-year-old plantations compared with 3- and 5-year-old. In addition, correlation analysis and principal component analysis indicated that the parameters evaluated are associated with the adult age of the oil palm. Also, the results of soil physicochemical showed that low soil fertility was associated with an increase in the age of the palm.

Modeling and quantification of soil compaction promoted by animal trampling in an integrated crop-livestock system / Modelagem e quantificação da compactação do solo promovida pelo pisoteio animal em sistema de integração lavoura-pecuária

At critical levels, animal trampling can physically degrade soil, leading to the loss of sustainability of agricultural production. Therefore, it is becomes necessary to model and quantify the soil compaction potential. In this context, the objective was to evaluate the occurrence of soil compaction promoted by animal trampling in crop-livestock integration system (ICL). The study was conducted in a field at Centro Tecnológico da Comigo in the municipality of Rio Verde, Goias state, Brazil, during the agricultural off-season. The experimental area was composed of 1.97 ha, which was equally divided into eight paddocks. Soil was sampled before the grazing phase and after each of four grazing cycles. The compressive behavior of the soil was evaluated by determining the pre-consolidation and critical pressures. The results showed that only the first cycle of grazing showed additional compaction in 14.59% of samples. No critical compaction was observed in the evaluated area. Animal trampling under the studied conditions is not responsible for the dissemination of structural soil degradation in crop-livestock integration systems and may contribute to physical improvement resulting from biological soil loosening.(AU)

Em níveis críticos, o pisoteio animal podem degradar fisicamente o solo, levando à perda de sustentabilidade da produção agrícola. Portanto, torna-se necessário modelar e quantificar o potencial de compactação do solo. Neste contexto, objetivou-se avaliar a ocorrência da compactação do solo promovida pelo pisoteio animal em sistema de integração lavoura-pecuária (ILP). O estudo foi conduzido a campo no Centro Tecnológico da Comigo no município de Rio Verde, Goiás, Brasil durante o período da segunda safra da agricultura. A área experimental foi composta de 1,97 hectares, dividida igualmente em oito piquetes. O solo foi amostrado antes da fase de pastejo e após cada um dos quatro ciclos de pastejo. Foi avaliado o comportamento compressivo do solo, a partir da determinação da pressão de pré-consolidação e da pressão crítica. Os resultados mostraram que somente o primeiro ciclo de pastejo apresentou compactação adicional e em 4,59% das amostras. Não houve compactação crítica na área avaliada. O pisoteio animal nas condições estudadas não é responsável pela disseminação da degradação estrutural do solo em sistemas de integração lavoura-pecuária, podendo contribuir eventualmente até com a melhoria física decorrente da descompactação biológica do solo.(AU)

Ecological Drawbacks of Nanomaterials Produced on an Industrial Scale: Collateral Effect on Human and Environmental Health.

Currently, hundreds of different nanomaterials with a broad application in products that make daily lives a little bit easier, in every aspect, are being produced on an industrial scale at thousands of tons per year. However, several scientists, researchers, politics, and ordinary citizens have stated their concern regarding the life cycle, collateral effects, and final disposal of these cutting-edge materials. This review summarizes, describes, and discusses all manuscripts published in the Journal Citation Reports during the last 10 years, which studied the toxicity or the effects of nanomaterials on human and environmental health. It was observed that 23.62% of the manuscripts analyzed found no ecological or human risks; 54.39% showed that several nanomaterials have toxicological effects on the ecosystems, human, or environmental health. In comparison, only 21.97% stated the nanomaterials had a beneficial impact on those. Although only 54.39% of the manuscripts reported unfavorable effects of nanomaterials on ecosystems, human, or environmental health, it is relevant because the potential damage is invaluable. Therefore, it is imperative to make toxicological studies of nanomaterials with holistic focus under strictly controlled real conditions before their commercialization, to deliver to the market only innocuous and environmentally friendly products.

Quantification of soil erosion using 7Be in a steep watershed used for natural grazing in Brazil.

Cosmogenic 7Be was used to evaluate soil loss in a mountainous micro-watershed near Belo Horizonte, Southwest Brazil. Two nearby sites were selected, a reference site in a flat area and an eroded site in a hill slope. At the reference site, soil samples were collected monthly throughout the year in order to evaluate seasonal variations of 7Be inventory in soil and its relation with the precipitation regime. Additionally, rainwater was collected and the expected 7Be soil content was predicted. At the reference site, the 7Be inventory shows seasonal variations, in accordance with the rainy season, and its distribution in the soil profile shows an exponential decrease in depth (h0 = 6.9 ± 0.6 kg m-2; r2 = 0.97). At the eroded site, two soil sampling campaigns were performed in order to measure soil erosion in the watershed. The estimated net erosion was 42.2 ± 3.7 t ha-1, indicating the loss of upper 5mm of soil per year. This corresponds to soil losses in the area in the range from moderate to severe erosion.

Soil degradation index developed by multitemporal remote sensing images, climate variables, terrain and soil atributes.

Studies on soil degradation are essential for environmental preservation. Since almost 30% of the global soils are degraded, it is important to study and map them for improving their management and use. We aimed to obtain a Soil Degradation Index (SDI) based on multi-temporal satellite images associated with climate variables, land use, terrain and soil attributes. The study was conducted in a 2598 km2 area in São Paulo State, Brazil, where 1562 soil samples (0-20 cm) were collected and analyzed by conventional methods. Spatial predictions of soil attributes such as clay, cation exchange capacity (CEC) and soil organic matter (OM) were performed using machine learning algorithms. A collection of 35-year Landsat images was used to obtain a multi-temporal bare soil image, whose spectral bands were used as soil attributes predictors. The maps of clay, CEC, climate variables, terrain attributes and land use were overlaid and the K-means clustering algorithm was applied to obtain five groups, which represented levels of soil degradation (classes from 1 to 5 representing very low to very high soil degradation). The SDI was validated using the predicted map of OM. The highest degradation level obtained in 15% of the area had the lowest OM content. Levels 1 and 4 of SDI were the most representative covering 24% and 23% of the area, respectively. Therefore, satellite images combined with environmental information significantly contributed to the SDI development, which supports decision-making on land use planning and management.

Una evaluación de las propiedades fisicoquímicas de suelo en sistema productivo de maíz - algodón y arroz en el Valle del Sinú en Colombia / An evaluation of soil physicochemical properties in corn - cotton, and rice production systems at the Sinu Valley in Colombia

RESUMEN Los sistemas de producción agrícolas en la subregión Valle del Sinú, en Colombia, en los últimos 50 años, se han basado en la siembra de cultivos en rotación o alternancia de maíz - algodón y arroz, y se caracterizan por el uso intensivo de implementos de mecanización e insumos agrícolas. El objetivo de este estudio fue evaluar las características fisicoquímicas de los suelos, bajo los sistemas productivos de maíz - algodón y arroz e identificar las principales limitantes de suelo, que afectan el desarrollo y la productividad de los cultivos, en la subregión Valle del Sinú. Para lo anterior, se realizaron muestreos de suelo en 64 sitios, distribuidos en cinco municipios del Valle del Sinú, evaluando propiedades físicas y químicas del suelo. El suelo en estudio pertenece al orden Inceptisol, moderadamente profundo, compuesto por arcillas expansivas y horizonte argílico. El suelo, se caracterizó por una reacción acida (5,82±0,87 a 6,78±0,34), contenido medio de MO. La media de la CIC varió en rango, de 18,45±2,94 a 22,85±4,36cmol(+) kg-1, la CE estuvo no salinos, variando de 0,29±0,09 a 0,91±1,70dS cm-1. Los contenidos de P, S, Ca, Mg y K fueron altos. La densidad aparente mostró valores promedios restrictivos para el desarrollo de raíces en cuatro de los cinco municipios, variando de 1,42±0,10 a 1,49±0,08g cm-3, excepto en San Carlos (1,33±0,14g cm-3). Los resultados obtenidos evidencian indicios de procesos de degradación de suelo, relacionados con el manejo de los suelos.

ABSTRACT The agricultural production systems in the Valle del Sinú subregion in Colombia, in the last 50 years, have been based on the sowing of crops in rotation and / or alternation of corn - cotton and rice, and are characterized by the intensive use of implements mechanization and agricultural inputs. The aim of this study was to evaluate the physicochemical characteristics of the soils under the corn - cotton and rice production systems and identifying the main soil limitations, which affect crop development and productivity, in the Sinú Valley Subregion. For the above, soil sampling was carried out at 64 sites distributed in five municipalities of the Sinú Valley, evaluating the physical and chemical properties of the soil. The soil under study belongs to the order Inceptisol, moderately deep, composed of expansive clays and argillic horizons. The soil was characterized by an acid reaction (5.82 ± 0.87 to 6.78 ± 0.34), average MO content. The mean of the CIC varied in the range of 18.45 ± 2.94 to 22.85 ± 4.36cmol(+) kg-1, the EC was not saline, varying from 0.29 ± 0.09 to 0.91 ± 1.70dS cm-1. The contents of P, S, Ca, Mg and K were high. The apparent density showed restrictive average values for root development in four of the five municipalities, ranging from 1.42 ± 0.10 to 1.49 ± 0.08g cm-3, except in San Carlos (1.33 ± 0.14g cm-3). The results obtained show evidence of soil degradation processes related to soil management.

Evaluation of gully development over several years using GIS and fractal analysis: a case study of the Palmital watershed, Minas Gerais (Brazil).

Soil erosion affects agricultural production by reducing the area of rural properties and altering the dynamics of watersheds. Gullies are a complex and irregular type of erosion form that can reach large dimensions, and studying gullies to stabilize erosion processes is a challenge. This study aims to understand their environmental relationships as a basis for future research and to recover land degraded by soil erosion. We combined mapping techniques using geographic information system (GIS) with temporal evolution of land use and fractal dimensions of gullies using FracLac to determine the stability of gullies in a watershed in south Minas Gerais (Brazil). We used R software to apply linear regressions and tested the statistics to verify the compatibility of the model. Environmental characteristics of the watershed contribute to the formation of gullies, but human activities influence the deflagration of these features. The temporal evolution of the land use demonstrated that nearly 50% of the watershed was used as pastures throughout the years, which contributed to soil degradation. The evolution of the fractal dimension showed fluctuations over the years, indicating that the gullies are not stable. The regressions suggest that the vegetation, geology, land use, channel order, and curvature may influence the fractal dimensions of gullies. We concluded that human activity influences the evolution of gullies; the use of techniques such as vegetation measures can contribute to the stabilization of gullies. We also concluded that fractal analysis is an interesting tool for performing environmental evaluations of irregular and complex features, such as gullies.

The stability of aggregates and organic carbon content after the application of gypsum, soil scarification and a succession of agricultural crops / A estabilidade dos agregados e do teor de carbono orgânico após a aplicação de gesso, escarificação do solo e uma sucessão de culturas agrícolas

Studies related to the monitoring of soil quality by physical attributes are important for the evaluation and maintenance of the sustainability of agricultural systems, besides indicating the appropriate management of the environment, aiming at its conservation and productivity. The objective of this study was to evaluate the stability of aggregates and organic carbon after the application of gypsum, soil scarification and a succession of crops. The treatments consisted of an absence and addition of gypsum, absence and presence of soil scarification, and three systems of crops in succession. The experimental design was made of randomized blocks, in a 2x2x4 factorial scheme, with eight replications. The aggregates were evaluated as stabled in water and soil organic carbon content. The treatment where gypsum was applied, as well as the soybean/maize/brachiaria/fallow (SMBF) succession system, presented better results in soil aggregation and higher levels of organic carbon.

Estudos relativos ao monitoramento da qualidade do solo pelos atributos físicos são importantes para a avaliação e manutenção da sustentabilidade dos sistemas agrícolas, além de sinalizar o manejo adequado do ambiente, visando à sua conservação e produtividade. Este trabalho teve por objetivo avaliar a estabilidade de agregados e teor de carbono orgânico, após a aplicação de gesso, escarificação do solo e sucessão de culturas. Os tratamentos consistiram na ausência e adição de gesso agrícola, ausência e presença de escarificação do solo, e três sistemas de sucessão de culturas. O delineamento experimental foi em blocos casualizados, em esquema fatorial 2x2x3 com oito repetições. Sendo avaliada a estabilidade dos agregados estáveis em água e teor de carbono orgânico do solo. O tratamento onde foi aplicado gesso agrícola e o sistema de sucessão SMBP apresentaram melhores resultados na agregação do solo e maiores teores de carbono orgânico.

Diversity of Fungi in Soils with Different Degrees of Degradation in Germany and Panama.

Soil degradation can have an impact on the soil microbiota, but its specific effects on soil fungal communities are poorly understood. In this work, we studied the impact of soil degradation on the richness and diversity of communities of soil fungi, including three different degrees of degradation in Germany and Panama. Soil fungi were isolated monthly using the soil-sprinkling method for 8 months in Germany and 3 months in Panama, and characterized by morphological and molecular data. Soil physico-chemical properties were measured and correlated with the observed values of fungal diversity. We isolated a total of 71 fungal species, 47 from Germany, and 32 from Panama. Soil properties were not associated with fungal richness, diversity, or composition in soils, with the exception of soil compaction in Germany. The geographic location was a strong determinant of the soil fungal species composition although in both countries there was dominance by members of the orders Eurotiales and Hypocreales. In conclusion, the results of this work do not show any evident influence of soil degradation on communities of soil fungi in Germany or Panama.

Farmers views on the use and management of soil and its relation to the return of erosion in non-tillage systems / Opinião dos agricultores sobre o uso e manejo do solo e sua relação com o retorno da erosão em sistemas de plantio direto

The non-tillage system (NTS), until now considered an effective management tool for the control of erosion, has gradually increased the loss of soil. The objective of this research is to identify and understand the probable causes of the return of erosion in rural properties under the NTS in three municipalities in northern Paraná. For this research, a questionnaire was used to collect information on soil management and the use of agricultural terraces. Data collection was completed with 145 landowners and NTS users, along with rural extension and agricultural cooperatives. The results demonstrated that the return of erosion is likely due to the absence of crop rotation in favor of repetitive year-to-year planting of the same plant species (early soybean/maize [second harvest]/wheat), soil revolving to decompress the surface layer, and the elimination of agricultural terraces and the consequential downslope planting.(AU)

O sistema plantio direto (SPD), até então considerado um manejo eficiente no controle da erosão, tem apresentado aumento gradativo da perda de solo. Assim, o estudo teve por objetivo levantar e entender as prováveis causas do retorno da erosão em áreas sob SPD, em propriedades rurais de três municípios do norte paranaense. Para tal, foi aplicado um questionário para o levantamento de informações referentes ao manejo do solo e uso do terraço agrícola. O levantamento de dados foi realizado com 145 proprietários de terras e usuários do SPD, selecionados junto à extensão rural e cooperativas agrícolas. Os resultados permitiram concluir que o retorno da erosão se deve a ausência de rotação de culturas em prol de uma repetitividade ano a ano da mesma espécie vegetal (soja precoce/milho segunda safra ou trigo); do revolvimento do solo para descompactação da camada superficial; da eliminação dos terraços agrícolas e consequente plantio em desnível.(AU)

High­magnesium waters and soils: Emerging environmental and food security constraints.

Food insecurity and declining availability of freshwater and new productive land in water-scarce areas and countries necessitate effective use of marginal-quality waters and underperforming soils. High­magnesium waters and soils are emerging examples of water quality deterioration and land degradation leading to environmental and food security constraints in several irrigation schemes. A ratio of magnesium-to-calcium > 1 in irrigation waters and an exchangeable magnesium percentage > 25% in soils are considered high enough to result in soil degradation and impact crop yields negatively. These soil and water resources occur in the Aral Sea Basin in Central Asian countries, the Cauca River Valley in Colombia, the Central Plateau Basin in Iran, the Indus Basin in Pakistan, the Indo-Gangetic Plains in India, the Murray-Darling Basin in Australia, and the Coastal Mountain Range in California, among others. With limited and scattered information, their occurrence remains hidden or unnoticed in many cases due to the lack of criteria in water quality assessment and soil classification systems. Managing high­magnesium waters and soils requires a source of calcium to mitigate magnesium effects, in addition to an effective drainage system for safe disposal of excess magnesium salts. There is a need to put high­magnesium waters and soils on the public policy agenda. Pertinent policies can catalyze stakeholders' involvement in supporting water and land quality monitoring systems and introducing innovative financial mechanisms to facilitate provision of calcium-supplying amendments in affected areas. Equally important would be strengthening institutional and professionals' capacity, enhancing institutional collaboration, encouraging private sector involvement in at-risk areas, and engaging local communities and farmers. These efforts will support the 2030 Sustainable Development Agenda. Eradicating extreme poverty and meeting the Sustainable Development Goals in water-scarce areas without adequately addressing underperforming land and water resources is highly unlikely.

Farmers views on the use and management of soil and its relation to the return of erosion in non-tillage systems / Opinião dos agricultores sobre o uso e manejo do solo e sua relação com o retorno da erosão em sistemas de plantio direto

The non-tillage system (NTS), until now considered an effective management tool for the control of erosion, has gradually increased the loss of soil. The objective of this research is to identify and understand the probable causes of the return of erosion in rural properties under the NTS in three municipalities in northern Paraná. For this research, a questionnaire was used to collect information on soil management and the use of agricultural terraces. Data collection was completed with 145 landowners and NTS users, along with rural extension and agricultural cooperatives. The results demonstrated that the return of erosion is likely due to the absence of crop rotation in favor of repetitive year-to-year planting of the same plant species (early soybean/maize [second harvest]/wheat), soil revolving to decompress the surface layer, and the elimination of agricultural terraces and the consequential downslope planting.

O sistema plantio direto (SPD), até então considerado um manejo eficiente no controle da erosão, tem apresentado aumento gradativo da perda de solo. Assim, o estudo teve por objetivo levantar e entender as prováveis causas do retorno da erosão em áreas sob SPD, em propriedades rurais de três municípios do norte paranaense. Para tal, foi aplicado um questionário para o levantamento de informações referentes ao manejo do solo e uso do terraço agrícola. O levantamento de dados foi realizado com 145 proprietários de terras e usuários do SPD, selecionados junto à extensão rural e cooperativas agrícolas. Os resultados permitiram concluir que o retorno da erosão se deve a ausência de rotação de culturas em prol de uma repetitividade ano a ano da mesma espécie vegetal (soja precoce/milho segunda safra ou trigo); do revolvimento do solo para descompactação da camada superficial; da eliminação dos terraços agrícolas e consequente plantio em desnível.

Soil, water, nutrients and soil organic matter losses by water erosion as a function of soil management in the Posses sub-watershed, Extrema, Minas Gerais, Brazil / Perdas de solo, água, nutrientes e matéria orgânica do solo por erosão hídrica em função do manejo na sub-bacia das Posses, Extrema, MG

Knowledge of the quantity and quality of the material lost by soil erosion due to soil management is a basic need to identify land management zones in catchments. The aim of this study was to investigate the influence of soil management on the quantity and quality of soil material lost by erosion in the Posses sub-watershed, Municipality of Extrema, State of Minas Gerais, Brazil. Water and sediments lost by natural rainfall erosion were sampled from erosion plots located on a Red-Yellow Argisol (PVA) under the following systems: bare soil, subsistence farming (maize/beans/pumpkin/jack-beans/fallow), degraded pasture, well-managed pasture, and reforestation set up in 2013; and in a Litholic Neosol (RL): reforestation set up in 2008, bare soil, and native forest. Ca, Mg, K, P, N and soil organic matter (SOM) contents were determined in sediment and soil samples (at 0-5 cm depth) for the determination of the runoff enrichment ratios. Management influences soil losses more so than water losses. Minor losses were found in reforestation set up in 2013 (soil); in well-managed pasture (water); and in reforestations (nutrients and SOM). These losses tend to stability with time. The general sequence of nutrient losses was N > Ca > Mg > K > P in PVA; and N > Ca > K > Mg > P in RL. Loss rates of SOM and N followed the order: bare soil > subsistence farming > degraded pasture > well-managed pasture >reforestation, in PVA; and bare soil > native forest > reforestation, in Argisol. Reforestation and wellmanagementpasture are effective conservation strategies in order to lower the erosion process in thePosses sub-watershed. Soil losses, as well as nutrients and organic matter losses were more influencedby soil management than water losses. The safeguarding native forest under Argisol is essential to theconservation of this pedoenvironment, especially in steep slopes.(AU)

O conhecimento da quantidade e qualidade de material perdido por erosão hídrica em função do manejo do solo constitui uma necessidade básica para a definição de zonas de manejo em áreas de recarga de água. O objetivo desse trabalho foi verificar a influência do manejo do solo sobre a quantidade e qualidade de material perdido por erosão hídrica na sub-bacia hidrográfica das Posses, Extrema-MG. Para isso, foram coletados água e sedimentos erodidos através de parcelas de erosão, instaladas, sob chuva natural, em Argissolo Vermelho-Amarelo (PVA) nos manejos: solo descoberto, rotação cultural (milho/feijão-de-porco/pousio), pastagens degradada e bem manejada, e reflorestamento implantado em 2013; e em Neossolo Litólico (RL) nos manejos: reflorestamento implantado em 2008, solo descoberto e mata nativa. Nas amostras de sedimentos e de solos (coletadas na profundidade de 0-5 cm) foram determinados os teores de Ca, Mg, K, P, N (NT) e de matéria orgânica do solo (MOS) e com isso, calculada a taxa de enriquecimento de enxurrada. O manejo exerce maior influência nas perdas de solo do que nas perdas de água. Menores perdas foram encontradas no reflorestamento implantado em 2013 (solo), pasto bem manejado (água) e reflorestamentos (nutrientes e matéria orgânica). Há uma tendência de estabilização dessas perdas com o tempo de implantação dos sistemas. A tendência geral das perdas de nutrientesno PVA foi NT > Ca > Mg > K > P; e no Argisol foi de NT > Ca > K > Mg > P. As taxas de perdasde MOS e NT seguem a ordem: solo descoberto > rotação cultural > pasto degradado > pasto bemmanejado > reflorestamento, no PVA; e solo descoberto > mata nativa > reflorestamento, no Argisol. Oreflorestamento e o manejo das pastagens são estratégias conservacionistas que minimizam as perdaspor erosão hídrica na sub-bacia das Posses, Extrema-MG. O manejo exerce maior influencia nas perdas de solo e de materiais a ele relacionados do que nas perdas de água. A manutenção da mata nativa sob...(AU)

Land use as a driver of soil fertility and biodiversity across an agricultural landscape in the Central Peruvian Andes.

Land use change and intensification in agricultural landscapes of the Andean highlands have resulted in widespread soil degradation and a loss in soil-based ecosystem services and biodiversity. This trend threatens the sustainability of farming communities in the Andes, with important implications for food security and biodiversity conservation throughout the region. Based on these challenges, we sought to understand the impact of current and future land use practices on soil fertility and biodiversity, so as to inform landscape planning and management decisions for sustainable agroecosystem management. We worked with local communities to identify and map dominant land uses in an agricultural landscape surrounding Quilcas, Peru. These land uses existed within two elevations zones (low-medium, 3200-3800 m, and high elevation, 3800-4300 m). They included three types of low-medium elevation forests (eucalyptus, alder, and mixed/native species), five pasture management types (permanent pasture, temporal pasture [in fallow stage], degraded pasture, high-altitude permanent pasture, and high-altitude temporal pasture [in fallow stage]) and six cropping systems (forage crops, maize/beans, and potato under four types of management). Soil fertility was evaluated in surface soils (0-20 cm) with soil physicochemical parameters (e.g., pH, soil organic matter, available nutrients, texture), while soil biological properties were assessed using the abundance and diversity of soil macrofauna and ground cover vegetation. Our results indicated clear impacts of land use on soil fertility and biological communities. Altitude demonstrated the strongest effect on soil physicochemical properties, but management systems within the low-mid elevation zone also showed important differences in soil biological communities. In general, the less-disturbed forest and pasture systems supported more diverse soil communities than the more intensively managed croplands. Degraded soils demonstrated the lowest overall soil fertility and abundance of soil macrofauna, but this may be reversible via the planting of alder forests. Our findings also indicated significant covariation between soil physicochemical parameters, soil macrofauna, and ground vegetation. This suggests that management for any one of these soil properties may yield unintended cascading effects throughout the soil subsystem. In summary, our findings suggest that shifts in land use across the landscape are likely to have important impacts on soil functioning and biodiversity.

Soil, water, nutrients and soil organic matter losses by water erosion as a function of soil management in the Posses sub-watershed, Extrema, Minas Gerais, Brazil / Perdas de solo, água, nutrientes e matéria orgânica do solo por erosão hídrica em função do manejo na sub-bacia das Posses, Extrema, MG

Knowledge of the quantity and quality of the material lost by soil erosion due to soil management is a basic need to identify land management zones in catchments. The aim of this study was to investigate the influence of soil management on the quantity and quality of soil material lost by erosion in the Posses sub-watershed, Municipality of Extrema, State of Minas Gerais, Brazil. Water and sediments lost by natural rainfall erosion were sampled from erosion plots located on a Red-Yellow Argisol (PVA) under the following systems: bare soil, subsistence farming (maize/beans/pumpkin/jack-beans/fallow), degraded pasture, well-managed pasture, and reforestation set up in 2013; and in a Litholic Neosol (RL): reforestation set up in 2008, bare soil, and native forest. Ca, Mg, K, P, N and soil organic matter (SOM) contents were determined in sediment and soil samples (at 0-5 cm depth) for the determination of the runoff enrichment ratios. Management influences soil losses more so than water losses. Minor losses were found in reforestation set up in 2013 (soil); in well-managed pasture (water); and in reforestations (nutrients and SOM). These losses tend to stability with time. The general sequence of nutrient losses was N > Ca > Mg > K > P in PVA; and N > Ca > K > Mg > P in RL. Loss rates of SOM and N followed the order: bare soil > subsistence farming > d

O conhecimento da quantidade e qualidade de material perdido por erosão hídrica em função do manejo do solo constitui uma necessidade básica para a definição de zonas de manejo em áreas de recarga de água. O objetivo desse trabalho foi verificar a influência do manejo do solo sobre a quantidade e qualidade de material perdido por erosão hídrica na sub-bacia hidrográfica das Posses, Extrema-MG. Para isso, foram coletados água e sedimentos erodidos através de parcelas de erosão, instaladas, sob chuva natural, em Argissolo Vermelho-Amarelo (PVA) nos manejos: solo descoberto, rotação cultural (milho/feijão-de-porco/pousio), pastagens degradada e bem manejada, e reflorestamento implantado em 2013; e em Neossolo Litólico (RL) nos manejos: reflorestamento implantado em 2008, solo descoberto e mata nativa. Nas amostras de sedimentos e de solos (coletadas na profundidade de 0-5 cm) foram determinados os teores de Ca, Mg, K, P, N (NT) e de matéria orgânica do solo (MOS) e com isso, calculada a taxa de enriquecimento de enxurrada. O manejo exerce maior influência nas perdas de solo do que nas perdas de água. Menores perdas foram encontradas no reflorestamento implantado em 2013 (solo), pasto bem manejado (água) e reflorestamentos (nutrientes e matéria orgânica). Há uma tendência de estabilização dessas perdas com o tempo de implantação dos sistemas. A tendência geral das perdas de nutrien