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The aim of this study was to assess the spatiotemporal variation in water quality in the Grande River and the Ondas River, in the city of Barreiras, Bahia, Brazil. Water samples were collected at 11 points along the rivers, and eight physical-chemical parameters (electrical conductivity, pH, alkalinity, apparent and true color, turbidity, dissolved oxygen, and biochemical oxygen demand) and three microbiological indicators (heterotrophic bacteria, total and thermotolerant coliforms) were analyzed. Spatiotemporal variation was assessed using the multivariate techniques of principal component analysis/factorial analysis (PCA/FA) and hierarchical cluster analysis (HCA). The results of the PCA/FA highlighted eight of the eleven parameters as the main ones responsible for the variations in water quality, with the greatest increase in these parameters being observed in the rainy season, especially among the points influenced by sewage discharges and by the influence of the urban area. The CA grouped the results from 11 points into three main groups: group 1 corresponded to points influenced by sewage discharges; group 2 grouped points with mainly urban influences; and group 3 grouped points in rural areas. These groupings showed the negative influence of urbanization and also statistically significant variations between the groups and periods. The most degraded conditions were in group 1, and the least degraded conditions were in group 3. Assessment of the variations between the monitoring periods showed that rainfall had a significant impact on the increase or decrease in the parameters assessed, as a result of surface runoff linked to urbanization and increased river flow.
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Monitoreo del Ambiente , Ríos , Calidad del Agua , Brasil , Ríos/química , Urbanización , Contaminantes Químicos del Agua/análisis , CiudadesRESUMEN
Quantifying infiltration and surface runoff at the hillslope scale is indispensable for soil conservation studies. However, the spatial and temporal variability of infiltration imposes a major constraint on surface runoff estimation. Point infiltration values do not fully express the complexity of the surface runoff in the landscape. Considering the need to improve the estimation of runoff volume from infiltration data, this study aimed to measure the apparent infiltration at hillslope-scale and compare it with two methods of infiltration estimative derived from point information. The study was carried out in six hydrological monitoring units paired. A set of hyetographs and hydrographs allowed the determination of apparent infiltration [Formula: see text] to each monitoring unit as a function of precipitation rate P. The measured [Formula: see text] values were used: (1) to evaluate the efficiency of the different land management in increasing infiltration; and (2) to evaluate the efficiency of two methods of hillslope-scale infiltration estimation based on point data: (a) derived from concentric rings method ([Formula: see text]), and (b) derived from a physically-based modeling ([Formula: see text]). Regarding the differences in land managements, terraces proved to be the most efficient land management practice, followed by phytomass addition. Regarding the methods, for precipitation rates greater than 40 [Formula: see text] the point infiltration-based [Formula: see text] underestimates apparent infiltration [Formula: see text] with PBIAS ranging from [Formula: see text] to [Formula: see text]. Even so, [Formula: see text] proved efficient in representing [Formula: see text] at less intense rainfall events. Nonetheless, the point infiltration-based method [Formula: see text] properly represented [Formula: see text] to all rainfall intensities (Nash-Sutcliffe coefficient [Formula: see text]).
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Suelo , Agua , Monitoreo del AmbienteRESUMEN
Pesticides reach aquatic ecosystems via surface runoff becoming one of the main contributors to their deterioration. Among the strategies to mitigate these impacts, the use of riparian strips is recommended, but the knowledge of how much each ecosystemic variable contributes to the process is still incipient. We analyzed the influence of terrain slope and vegetation in the attenuation of 2,4-Dichlorophenoxyacetic acid (2,4-D) toxicity in surface runoff using Lactuca sativa as a diagnostic organism. In addition, the differential effects of this herbicide were examined under laboratory conditions, with standardized water and ambient water as a dilution medium. The study was conducted in plots with different terrain slopes and presence/absence of vegetation. The herbicide was applied to each plot and rain was subsequently simulated. The runoff was collected at regular distances and the toxicity was measured. The runoff toxicity decreased with the distance from the application area in all plots, this reduction being greater in low-slope plots. No differences in attenuation of runoff toxicity were found between plots with and without vegetation. The data were incorporated into models to estimate the minimum widths of safety to reduce the toxicity of 2,4-D by 90% under these conditions, suggesting distances of 5 and 20 m for low-slope and high-slope zones, respectively. In laboratory experiments, lower relative toxicity of 2,4-D was detected when natural water was used as solvent. These results contribute to the design of sustainable agricultural practices.
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Plaguicidas , Ácido 2,4-Diclorofenoxiacético/toxicidad , Agricultura , Ecosistema , Plantas , Lluvia , Suelo , Movimientos del AguaRESUMEN
RESUMO Balanço hídrico é uma análise realizada com base em estudos sobre as entradas e saídas de água de uma bacia hidrográfica, e que tem grande importância por identificar o regime hidrológico e as possibilidades de utilização da bacia. Neste trabalho foi realizado o balanço hídrico de uma secção de bacia hidrográfica localizada no oeste do Paraná, em uma área de plantio de eucaliptos para corte, obtendo-se também os valores para o escoamento superficial por meio do método racional.
ABSTRACT Water balance consists in an analysis carried out based on studies on the inflows and outflows of a hydrographic basin, which is fundamental to identify the hydrological regime and the possibilities of using this basin. This study aims to verify the water balance of a section of a hydrographic basin located in Western Paraná, Brazil, in addition to obtaining the values for runoff by the rational method.
RESUMEN
This study evaluates the influence of physiographic characteristics on the peak flow to runoff volume ratio in watersheds belonging to the Cerrado and Atlantic Forest biomes, in the Center-South region of Brazil. Specifically, the peak flow and runoff volume values obtained in the outlet section are related to the physiographic characteristics of the watersheds. Using a geographic information system tool, 13 watersheds are delimited, and 38 variables are selected from each watershed. A recursive digital filter is used to separate the direct (surface) flow from base (groundwater) flow. Data are analyzed using multivariate statistics, which allows interpretation of the structure of a data set from the respective correlation matrices. The results indicate that the peak flow and runoff volume are strongly correlated with the physical characteristics of the watersheds and the types of anthropogenic activity in both biomes. Furthermore, the presence of woods and forests reduces the peak flow and runoff volume.
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Monitoreo del Ambiente , Bosques , Brasil , Ecosistema , Análisis MultivarianteRESUMEN
In addition to soil losses on hillslopes, unpaved rural roads, especially when poorly designed and maintained, can be a significant contributor to the erosive processes seen at the catchment scale. In areas with deep soils, the solutions primarily focus on channeling excess surface runoff into settling ponds or terraces. However, few studies have addressed runoff control from roads on steep slopes in areas of shallow soil. Modeling hydrological processes at the catchment scale is a useful strategy for choosing the most effective and least costly conservation practices to control surface runoff. This study applies a mathematical model to a monitored catchment in southern Brazil to better understand the effects of conservation practices on unpaved roads and their impact on the hydrological and erosive dynamics of a small rural catchment. We calibrated the LISEM model using data from eight stormwater events and evaluated how three different road conservation scenarios-low (LI), medium (MI), and high intensity (HI)-contributed to sediment yield (SY), surface runoff volume (Qe), and peak flow (Qp) reduction. The LI and MI scenarios involved installation of hydraulic structures to control the road surface runoff (i.e. road ditch graveling, diversion weirs and grass waterways) while the HI scenario added surface runoff control practices (grass strips) to surrounding crop fields, in addition to the practices included in the MI scenario. Based on these scenarios, the results showed a Qe reduction at the catchment outlet from - 3.5% (LI) to - 22.5% (HI). The Qp and SY varied from + 6.0% (LI) to - 292.5% (HI) and from + 20.0% (LI) to - 963.9% (HI), respectively. These results show that the low- and medium-intensity practices were not effective in controlling surface runoff from roads, based on the Qe, Qb, and SY observed at the catchment's outlet. On the other hand, when MI scenarios were complemented with practices to control surface runoff in the cultivated areas, a significant reduction in surface runoff (Qe and Qp) and SY was verified.
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Monitoreo del Ambiente , Suelo , Hidrología , Modelos Teóricos , PoaceaeRESUMEN
RESUMO A região semiárida do nordeste brasileiro é marcada por elevadas incertezas quanto à ocorrência de chuvas intensas, bem como por anos sequenciados de secas. Esses fenômenos naturais, somados à reduzida utilização de práticas conservacionistas, podem gerar degradação dos solos. Nesse contexto, o presente estudo objetivou avaliar a importância do uso de cobertura morta e espécies de oleaginosas não convencionais perenes (Moringa oleifera Lam. e Azadirachta indica A. Juss.) no controle da erosão do solo em parcelas de erosão, em condições de chuvas naturais. O estudo realizou-se durante os anos de 2016 e 2017 na bacia representativa do Mimoso, localizada no município de Pesqueira (PE), Brasil. Na área de estudo, instalaram-se três parcelas de erosão, cada uma com área igual a 40 m2 (2 × 20 m), que foram intensamente monitoradas no tocante à intensidade de precipitação, à umidade e à temperatura do solo, ao escoamento superficial e à produção de sedimentos. Para cada parcela experimental, adotaram-se os seguintes tratamentos: oleaginosas; oleaginosas + cobertura morta; solo descoberto. A cobertura do solo com oleaginosas e cobertura morta resultou em maior retenção de umidade do solo e menores valores de escoamento superficial e perdas de solo. O desenvolvimento da estrutura das oleaginosas diminuiu o impacto direto das gotas de chuva no solo, reduzindo as perdas de solo quando comparadas ao descoberto.
ABSTRACT The semiarid region of the Brazilian Northeast is marked by strong uncertainties regarding the occurrence of extreme rainfall, as well as the occurrence of sequenced year droughts. These natural phenomena, together with limited use of soil and water conservation practices, can generate soil degradation. In this context, the present study aimed to evaluate the importance of the use of mulch and non-conventional perennial oleaginous species (Moringa oleifera Lam. and Azadirachta indica A. Juss.) in soil erosion plots under natural rainfall. The study was conducted during the years of 2016 and 2017 in the representative basin of Mimoso, located in the municipality of Pesqueira, Pernambuco, Brazil. Three erosion plots each with an area of 40 m2 (2 m × 20 m), were installed in the study area, which were intensively monitored for rainfall intensity, soil moisture and temperature, runoff and sediment production. For each experimental plot, the following treatments were adopted: Oleaginous; Oleaginous + mulch; Bare soil. Soil cover with oleaginous species and mulch resulted in higher soil moisture and lower amounts of runoff and soil loss. The development of the tree structure of the oleaginous reduced the direct impact of raindrops on the soil surface, reducing the soil losses when compared to the bare soil.
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The green roofs are structures characterized by the application of vegetation cover in the buildings, using adequate waterproofing and drainage systems. It allows the reduction of surface runoff and delay in peak flow, contributing to the mitigation of flood events in urban areas. Therefore, this study aimed to evaluate the effect of the use of vegetal coverings on the surface runoff, taking into account quantitative and qualitative aspects, using an experimental module installed in the city of Porto Alegre, Brazil. The experimental station consisted of four modules: two horizontal modules with and without vegetation cover and two modules with slopes of 15° with and without vegetation cover. It was evaluated 19 precipitation events, and it was verified the volumes drained in each module after 3, 6 and 12 h from the beginning of precipitation. The water samples were collected in order to analyse the quality of the runoff from the experimental modules. The results have shown that the use of vegetal coverings can provide better distribution of the surface runoff, as well as a decrease of the speed of excess water release with no surface runoff in the first 3 h after the onset of rainfall in the horizontal module. Additionally, it was proved the reduction in drained volumes, with the flat module with vegetation cover being capable of retaining completely precipitations with volumes of approximately 22 mm. The vegetation cover module in roofs was the one that has presented better results regarding the reduction of the flow, presenting an average retention percentage of 91.7% for the first 3 h, indicating that the slope is an important factor. The physical-chemical analysis of the water shows that for all analysed modules, it is possible to use water for non-potable uses, although the water quality of the modules with vegetation cover is lower when compared to the water coming from the module without vegetation cover.
Asunto(s)
Lluvia , Calidad del Agua , Brasil , Ciudades , Conservación de los Recursos Naturales , Movimientos del AguaRESUMEN
RESUMO O estudo do escoamento superficial e transporte de poluentes é de grande importância, pois ajuda na prevenção de impactos ambientais, auxiliando em planejamentos a serem realizados pelo poder público. Neste trabalho, teve-se como objetivo estudar, em laboratório, a dinâmica do transporte de material (cloreto de sódio - NaCl) disposto sobre uma superfície impermeável, dissolvido pela aplicação de água via simulador de chuva, tendo como fonte de variação três variáveis independentes: declividade, intensidade de precipitação e posição do material. Utilizou-se o delineamento experimental de faces centradas, que contemplou diferentes cenários reproduzidos nos experimentos, onde se avaliou a influência das três variáveis independentes sobre às dependentes (tempo de transporte, valor de pico, tempo de pico e massa total transportada), cujas respostas foram monitoradas no exutório do modelo experimental. A análise de resultados obtidos permitiu identificar o efeito significativo da declividade e posição do material sobre todas as variáveis dependentes estudadas e ainda o efeito quadrático da declividade para o tempo de transporte e a massa total transportada. Já para a intensidade de precipitação, verificou-se influência apenas para o tempo de transporte, dentro dos intervalos de estudo com nível de significância de 95%. O modelo produzido para o tempo de transporte é capaz de explicar 90% da variabilidade dos dados, enquanto o para o valor de pico possui uma capacidade de explicação de 67,9%. O tempo de pico possui um modelo capaz de explicar 74,2% da variabilidade dos dados, e o modelo produzido para a massa total transportada possui uma capacidade de explicação de 62,4% da variabilidade dos dados.
ABSTRACT The study of surface runoff and transport of pollutants is of major importance, as it helps preventing environmental impacts, and supports planning tasks carried out by public authorities. The goal of this research was to study the dynamics of the transport of material (NaCl) on an impermeable surface, dissolved by the application of water through a rainfall simulator, having as its source of variation three independent variables: slope, rainfall intensity and position of the material. Face-centered experimental design was used, which contemplated different scenarios reproduced in the experiments, where the influence of the three independent variables on the dependent variables (transport time, peak value, peak time and total mass transported) was evaluated, whose responses were monitored at the outlet of the experimental model. The analysis of the results allowed to identify the significant effect of the slope and position of the material on all the dependent variables studied, as well as the quadratic effect of the slope for the transportation time and total mass transported. As for the rainfall intensity, only influence was observed for transportation time, within the study intervals with a level of significance of 95%. The resulting model is capable of explaining: 90% for transport time, 67.9% for peak value, 74.2% for peak time and 62.4% total mass transported.
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The aim of the current study is to assess possible erythrocyte mutagenic effects on Lithobates catesbeianus tadpoles exposed to water contaminated with 2,4-D. In order to do so, tadpoles were exposed to a predictive and environmentally relevant herbicide concentration (1.97 mg/L), which is likely to be found in lentic environments formed by superficial water runoffs in pasture areas where the herbicide was applied. The micronucleus test, as well as tests for other nuclear abnormalities, was conducted after 3, 5, and 9 days of exposure (d.e.). Changes in the biomass and mouth-cloaca length or interference in the larval development of the animals (in the three evaluated times) were not recorded. However, tadpoles exposed to 2,4-D showed the highest total number of nuclear abnormalities, as well as the highest frequency of binucleated erythrocytes and kidney-shaped nuclei (shortly after 3 d.e.). The micronucleus frequency was also higher in animals exposed to 2,4-D (in the 3rd, 5th, and 9th d.e.), as well as the frequency of binucleated cells (3rd, 5th, and 9th d.e.) presenting notched (9th d.e.) and blebbled (9th d.e.) nuclei in comparison to those of the control, after 5 and 9 days of exposure. Therefore, the current study is a pioneer in showing that 2,4-D has a mutagenic effect on L. catesbeianus tadpoles, even at low concentrations (environmentally relevant) and for a short period of time, a fact that may lead to direct losses in anuran populations living in areas adjacent to those subjected to 2,4-D herbicide application.
Asunto(s)
Ácido 2,4-Diclorofenoxiacético/toxicidad , Herbicidas/toxicidad , Larva/efectos de los fármacos , Mutagénesis/efectos de los fármacos , Mutágenos/toxicidad , Contaminantes Químicos del Agua/toxicidad , Animales , Relación Dosis-Respuesta a Droga , Eritrocitos/efectos de los fármacos , Larva/genética , Larva/crecimiento & desarrollo , Pruebas de Micronúcleos , Modelos Teóricos , Rana catesbeianaRESUMEN
The aim of this study was to evaluate the relationship between glyphosate and phosphate fertilizer application and their contribution to surface water runoff contamination. The study was performed in Aquic Argiudoll soil (Tezanos Pinto series). Four treatments were assessed on three dates of rainfall simulation after fertilizer and herbicide application. The soluble phosphorus in runoff water was determined by a colorimetric method. For the determination of glyphosate and aminomethylphosphonic acid (AMPA), a method based on fluorenylmethyloxycarbonyl (FMOC) group derivatization, solid phase extraction (SPE) purification, and ultrahigh-performance liquid chromatography-tandem mass spectrometry (UHPLC-MS/MS) was employed. The application of phosphorus fertilizer resulted in an increased loss of glyphosate by runoff after 1 day of application. These results suggest the need for further study to understand the interactions and to determine appropriate application timing with the goal of reducing the pollution risk by runoff.
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Fertilizantes/análisis , Glicina/análogos & derivados , Herbicidas/química , Fósforo/química , Contaminantes Químicos del Agua/química , Glicina/química , Cinética , Lluvia , Contaminantes del Suelo/química , GlifosatoRESUMEN
The objective of this work was to investigate the existence of critical slope lengths, associated with corn residue failure, at the rates of 8, 4, and, 2 Mg ha-1, in two modes of direct seeding: without and with shanks grooving in the seeding-fertilizing machine. Simulated rainfall of 75 mm h-1, applied with the rotating-boom simulator, and an Alfisol with 0.16 m m-1 slope steepness, were used. Initially only applied rain was used, until steady runoff occured. Increasingly, without interrupting and changing the intensity of the rain, increasing levels of extra-water inflow (six, 10 minutes each) were added to the experimental plots, to simulate progressively greater slope lengths. There was effective residue removal by surface runoff in all treatments, which led to believe the same failure or critical slope length existed in all of them, but this could not be confirmed by the theoretical erosion relationships. Even so, as a reference and as a measure of safety, real credit was given to what was visually observed, a failure in smaller residue level of extra flow in direct seeding without chisel planter was observed, and the opposite with the chisel planter, establishing critical slope lengths, respectively, of 64 m to 118 m and 171 m to 456 m, according to residue rates.
O objetivo deste trabalho foi investigar a existência de comprimentos críticos de declive, associados à falha do resíduo cultural de milho, nas doses de 8, 4 e 2 Mg ha-1, em dois modos de semeadura direta, sem e com hastes sulcadoras. Foi usada chuva simulada de 75 mm h-1, aplicada com o simulador de braços rotativos, e um Nitossolo Bruno com 0,16 m m-1 de declividade. Inicialmente aplicou-se somente chuva, até a enxurrada ficar constante. Em continuidade, sem interromper e mudar a intensidade da chuva, níveis crescentes de fluxo extra de água (seis, 10 minutos cada um) foram adicionados às parcelas experimentais, para simular comprimentos de declive progressivamente maiores. Observou-se efetiva remoção do resíduo de milho pela enxurrada em todos os tratamentos, sugerindo falha do mesmo ou existido comprimento crítico de declive em todos eles, mas isto não pôde ser confirmado pelas relações teóricas de erosão. Mesmo assim, como referência e por medida de segurança, deu-se crédito real ao observado visualmente e considerou-se falha do resíduo nos níveis menores de fluxo extra na semeadura direta sem hastes sulcadoras e nos níveis maiores de fluxo extra na semeadura direta com hastes sulcadoras, estabelecendo-se comprimentos críticos de declive, respectivamente, de 64 m a 118 m e 171 m a 456 m, conforme as doses de resíduo.
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Condición del Suelo , 24444 , Erosión Hídrica/análisis , Escorrentía , Inestabilidad de LaderasRESUMEN
The objective of this work was to investigate the existence of critical slope lengths, associated with corn residue failure, at the rates of 8, 4, and, 2 Mg ha-1, in two modes of direct seeding: without and with shanks grooving in the seeding-fertilizing machine. Simulated rainfall of 75 mm h-1, applied with the rotating-boom simulator, and an Alfisol with 0.16 m m-1 slope steepness, were used. Initially only applied rain was used, until steady runoff occured. Increasingly, without interrupting and changing the intensity of the rain, increasing levels of extra-water inflow (six, 10 minutes each) were added to the experimental plots, to simulate progressively greater slope lengths. There was effective residue removal by surface runoff in all treatments, which led to believe the same failure or critical slope length existed in all of them, but this could not be confirmed by the theoretical erosion relationships. Even so, as a reference and as a measure of safety, real credit was given to what was visually observed, a failure in smaller residue level of extra flow in direct seeding without chisel planter was observed, and the opposite with the chisel planter, establishing critical slope lengths, respectively, of 64 m to 118 m and 171 m to 456 m, according to residue rates.(AU)
O objetivo deste trabalho foi investigar a existência de comprimentos críticos de declive, associados à falha do resíduo cultural de milho, nas doses de 8, 4 e 2 Mg ha-1, em dois modos de semeadura direta, sem e com hastes sulcadoras. Foi usada chuva simulada de 75 mm h-1, aplicada com o simulador de braços rotativos, e um Nitossolo Bruno com 0,16 m m-1 de declividade. Inicialmente aplicou-se somente chuva, até a enxurrada ficar constante. Em continuidade, sem interromper e mudar a intensidade da chuva, níveis crescentes de fluxo extra de água (seis, 10 minutos cada um) foram adicionados às parcelas experimentais, para simular comprimentos de declive progressivamente maiores. Observou-se efetiva remoção do resíduo de milho pela enxurrada em todos os tratamentos, sugerindo falha do mesmo ou existido comprimento crítico de declive em todos eles, mas isto não pôde ser confirmado pelas relações teóricas de erosão. Mesmo assim, como referência e por medida de segurança, deu-se crédito real ao observado visualmente e considerou-se falha do resíduo nos níveis menores de fluxo extra na semeadura direta sem hastes sulcadoras e nos níveis maiores de fluxo extra na semeadura direta com hastes sulcadoras, estabelecendo-se comprimentos críticos de declive, respectivamente, de 64 m a 118 m e 171 m a 456 m, conforme as doses de resíduo.(AU)
Asunto(s)
Inestabilidad de Laderas , Erosión Hídrica/análisis , Condición del Suelo , Escorrentía , 24444RESUMEN
Eutrophication has become a major threat to water quality in the U.S., Europe, and Australasia. In most cases, freshwater eutrophication is accelerated by increased inputs of phosphorus (P), of which agricultural runoff is now a major contributor, due to intensification of crop and animal production systems since the early 1990s'. Once little information is available on the impacts of Brazilian agriculture in water quality, recent changes in crop and animal production systems in Brazil were evaluated in the context of probable implications of the fate of P in agriculture. Between 1993 and 2003, there was 33% increase in the number of housed animals (i.e., beef, dairy cows, swine, and poultry), most in the South Region (i.e., Paraná, Rio Grande do Sul, and Santa Catarina States), where 43 and 49% of Brazil's swine and poultry production is located, respectively. Although grazing-based beef production is the major animal production system in Brazil, it is an extensive system, where manure is deposited over grazed pastures; confined swine and poultry are intensive systems, producing large amounts of manure in small areas, which can be considered a manageable resource. This discussion will focus on swine and poultry farming. Based on average swine (100 kg) and poultry weights (1.3 kg), daily manure production (4.90 and 0.055 kg per swine and poultry animal unit, respectively), and manure P content (40 and 24 g kg-1 for swine and poultry, respectively), an estimated 2.5 million tones of P in swine and poultry manure were produced in 2003. Mostly in the South and Southeast regions of Brazil (62%), which represent only 18% of the country's land area. In the context of crop P requirements, there was 2.6 times more P produced in manure (1.08 million tones) than applied as fertilizer (0.42 million tonnes) in South Brazil in 2003. If it is assumed that fertilizer P use represents P added to meet crop needs and accounts for P sorbed by soil in unavailable forms each year, if swine and poultry manure were to replace fertilizer, there would be an annual P surplus of 0.66 million tonnes in the South region alone. These approximations and estimates highlight that, similarly to other parts of the world, there is a potential for surplus P to quickly accumulate in certain regions of Brazil. Unless measures are developed and implemented to utilize manure P, repeated annual surpluses will create an increasingly difficult problem to solve. These measures can be grouped as source and transport management. Source management attempts to decrease dietary P, use feed additives, manure treatment and composting, as well as careful management of the rate, timing, and method of manure applications. Transport management attempts to control the loss of P in runoff from soil to sensitive waters via use of conservation tillage, buffer or riparian zones, cover crops, and trapping ponds or wetlands. These measures are discussed in the contest of Brazil's climate, topography, and land use, and how successful remediation programs may be implemented at farm and watershed level.
Eutrofização dos mananciais de água se tornou uma preocupação nos Estados Unidos, Europa e Austrália. Na maioria dos casos, a eutrofização de mananciais de água é acelerada pelo aumento na quantidade de fósforo adicionada, o que tem estreita relação com o escorrimento superficial deste elemento, em função da intensificação dos sistemas de produção de culturas e animais a partir do início dos anos noventa. Em virtude de pouca informação com relação aos impactos da agricultura na qualidade da água, este artigo enfatiza modificações nos sistemas de produção de culturas e animais no Brasil no contexto das prováveis implicações quanto ao destino do fósforo no processo. Os dados apontam para um aumento de 33% no número de animais (gado de corte, gado de leite, suíno e frango) no período de 1993 - 2003, a maior parte deste aumento ocorrendo na região sul (Paraná, Rio Grande do Sul e Santa Catarina), onde se localizam 43% e 49% da produção de suínos e frangos, respectivamente. Enquanto a produção de gado de corte se dá predominantemente em sistema de pastejo a campo, com deposição do esterco sobre os pastos, a produção de suíno e frango ocorre em sistema intensivo de confinamento, o que resulta em elevadas quantidades de esterco em pequenas áreas. Assim sendo, a discussão irá focalizar na produção de suínos e frangos. Tendo em vista o peso médio de suíno (100 kg) e frango (1,3 kg), a produção diária de esterco (4,90 e 0,055 kg por suíno ou frango, respectivamente), e o conteúdo médio de P no esterco (40 e 24 g kg-1 para suíno e frango, respectivamente), estimou-se uma quantidade de 2,5 milhões de toneladas de fósforo nos estercos de suíno e frango, produzidas no Brasil em 2003. A maior parte foi produzida nas regiões sul e sudeste do Brasil (62% em conjunto), a qual representa apenas 18% da área do país. No contexto da exigência das culturas, os cálculos apontam para 2,6 vezes mais fósforo produzido nos estercos (1,08 milhões de toneladas) do que aplicado por meio de fertilizante (0,42 milhões de toneladas) na região sul em 2003. Diante do fato que a quantidade utilizada por fertilizantes representa o necessário para atender as exigências nutricionais das plantas, levando inclusive em consideração o fósforo adsorvido pelo solo, se o esterco de suíno e frango fosse considerado no sentido de substituir os fertilizantes aplicados, haveria uma sobra anual de 0,66 milhões de toneladas apenas na região sul. Estas aproximações e estimativas claramente indicam que, como em outras partes do mundo, existe potencial para esta sobra anual de fósforo rapidamente acumular em certas regiões do Brasil. A menos que medidas sejam desenvolvidas e implementadas para utilizar este esterco, repetidas sobras anuais irão conduzir a um problema de difícil resolução. Estas medidas podem ser agrupadas em dois tipos: as do manejo das fontes e as do transporte. As medidas que visam o manejo das fontes tendem a diminuir as quantidades de fósforo na dieta, usar aditivos no alimento, promover o tratamento e compostagem do esterco, bem como manejar com cuidado as doses, época, e método de aplicação dos estercos. As medidas visando o manejo no transporte objetivam controlar a perda de fósforo no escorrimento do solo para os corpos de água por meio da conservação do solo e resíduos, zonas vegetativas ribeirinhas de contenção, culturas de cobertura superficial, e pontes de aprisionamento ou áreas alagadas. Estas medidas são discutidas no contexto do clima, topografia, uso do solo, e ainda quanto ao sucesso dos programas de remediação a serem implementados em fazendas ou bacias hidrográficas.
RESUMEN
Eutrophication has become a major threat to water quality in the U.S., Europe, and Australasia. In most cases, freshwater eutrophication is accelerated by increased inputs of phosphorus (P), of which agricultural runoff is now a major contributor, due to intensification of crop and animal production systems since the early 1990s'. Once little information is available on the impacts of Brazilian agriculture in water quality, recent changes in crop and animal production systems in Brazil were evaluated in the context of probable implications of the fate of P in agriculture. Between 1993 and 2003, there was 33% increase in the number of housed animals (i.e., beef, dairy cows, swine, and poultry), most in the South Region (i.e., Paraná, Rio Grande do Sul, and Santa Catarina States), where 43 and 49% of Brazil's swine and poultry production is located, respectively. Although grazing-based beef production is the major animal production system in Brazil, it is an extensive system, where manure is deposited over grazed pastures; confined swine and poultry are intensive systems, producing large amounts of manure in small areas, which can be considered a manageable resource. This discussion will focus on swine and poultry farming. Based on average swine (100 kg) and poultry weights (1.3 kg), daily manure production (4.90 and 0.055 kg per swine and poultry animal unit, respectively), and manure P content (40 and 24 g kg-1 for swine and poultry, respectively), an estimated 2.5 million tones of P in swine and poultry manure were produced in 2003. Mostly in the South and Southeast regions of Brazil (62%), which represent only 18% of the country's land area. In the context of crop P requirements, there was 2.6 times more P produced in manure (1.08 million tones) than applied as fertilizer (0.42 million tonnes) in South Brazil in 2003. If it is assumed that fertilizer P use represents P added to meet crop needs and accounts for P sorbed by soil in unavailable forms each year, if swine and poultry manure were to replace fertilizer, there would be an annual P surplus of 0.66 million tonnes in the South region alone. These approximations and estimates highlight that, similarly to other parts of the world, there is a potential for surplus P to quickly accumulate in certain regions of Brazil. Unless measures are developed and implemented to utilize manure P, repeated annual surpluses will create an increasingly difficult problem to solve. These measures can be grouped as source and transport management. Source management attempts to decrease dietary P, use feed additives, manure treatment and composting, as well as careful management of the rate, timing, and method of manure applications. Transport management attempts to control the loss of P in runoff from soil to sensitive waters via use of conservation tillage, buffer or riparian zones, cover crops, and trapping ponds or wetlands. These measures are discussed in the contest of Brazil's climate, topography, and land use, and how successful remediation programs may be implemented at farm and watershed level.
Eutrofização dos mananciais de água se tornou uma preocupação nos Estados Unidos, Europa e Austrália. Na maioria dos casos, a eutrofização de mananciais de água é acelerada pelo aumento na quantidade de fósforo adicionada, o que tem estreita relação com o escorrimento superficial deste elemento, em função da intensificação dos sistemas de produção de culturas e animais a partir do início dos anos noventa. Em virtude de pouca informação com relação aos impactos da agricultura na qualidade da água, este artigo enfatiza modificações nos sistemas de produção de culturas e animais no Brasil no contexto das prováveis implicações quanto ao destino do fósforo no processo. Os dados apontam para um aumento de 33% no número de animais (gado de corte, gado de leite, suíno e frango) no período de 1993 - 2003, a maior parte deste aumento ocorrendo na região sul (Paraná, Rio Grande do Sul e Santa Catarina), onde se localizam 43% e 49% da produção de suínos e frangos, respectivamente. Enquanto a produção de gado de corte se dá predominantemente em sistema de pastejo a campo, com deposição do esterco sobre os pastos, a produção de suíno e frango ocorre em sistema intensivo de confinamento, o que resulta em elevadas quantidades de esterco em pequenas áreas. Assim sendo, a discussão irá focalizar na produção de suínos e frangos. Tendo em vista o peso médio de suíno (100 kg) e frango (1,3 kg), a produção diária de esterco (4,90 e 0,055 kg por suíno ou frango, respectivamente), e o conteúdo médio de P no esterco (40 e 24 g kg-1 para suíno e frango, respectivamente), estimou-se uma quantidade de 2,5 milhões de toneladas de fósforo nos estercos de suíno e frango, produzidas no Brasil em 2003. A maior parte foi produzida nas regiões sul e sudeste do Brasil (62% em conjunto), a qual representa apenas 18% da área do país. No contexto da exigência das culturas, os cálculos apontam para 2,6 vezes mais fósforo produzido nos estercos (1,08 milhões de toneladas) do que aplicado por meio de fertilizante (0,42 milhões de toneladas) na região sul em 2003. Diante do fato que a quantidade utilizada por fertilizantes representa o necessário para atender as exigências nutricionais das plantas, levando inclusive em consideração o fósforo adsorvido pelo solo, se o esterco de suíno e frango fosse considerado no sentido de substituir os fertilizantes aplicados, haveria uma sobra anual de 0,66 milhões de toneladas apenas na região sul. Estas aproximações e estimativas claramente indicam que, como em outras partes do mundo, existe potencial para esta sobra anual de fósforo rapidamente acumular em certas regiões do Brasil. A menos que medidas sejam desenvolvidas e implementadas para utilizar este esterco, repetidas sobras anuais irão conduzir a um problema de difícil resolução. Estas medidas podem ser agrupadas em dois tipos: as do manejo das fontes e as do transporte. As medidas que visam o manejo das fontes tendem a diminuir as quantidades de fósforo na dieta, usar aditivos no alimento, promover o tratamento e compostagem do esterco, bem como manejar com cuidado as doses, época, e método de aplicação dos estercos. As medidas visando o manejo no transporte objetivam controlar a perda de fósforo no escorrimento do solo para os corpos de água por meio da conservação do solo e resíduos, zonas vegetativas ribeirinhas de contenção, culturas de cobertura superficial, e pontes de aprisionamento ou áreas alagadas. Estas medidas são discutidas no contexto do clima, topografia, uso do solo, e ainda quanto ao sucesso dos programas de remediação a serem implementados em fazendas ou bacias hidrográficas.