No description available.

This thesis presents two interrelated studies that consider nutrient management and seasonal changes in recharge on agricultural lands within the context of source water protection. The research focuses first on the management of the risk to groundwater quality through the implementation of various nutrient management practices and secondly considers the dynamic nature of the transport pathway to the groundwater system associated with seasonal changes in climate and hydrology. The combined results provide insight into several of the key factors influencing the protection of groundwater sources within the agricultural landscape. Field work was completed between 2009 and 2010 on an agricultural field near the City of Woodstock, Ontario. The site is located within a source water protection area; the two-year travel time zone of the Thornton Well Field which represents the primary water supply for the City of Woodstock and which has experienced chronic increases in nitrate concentrations over the last few decades. The wells are completed in glacial overburden consisting of intermingling sand and gravel till aquifers which overly a limestone bedrock aquifer. Agricultural best or beneficial management practices (BMPs) field have been implemented and monitored since 2004. The BMPs were adopted in order to reduce nitrogen losses to the aquifer, and consisted of a reduction in nitrogen fertilizer application rates over a series of agricultural fields located near the well The first study is a one year experiment designed to compare alternative nutrient management practices for corn. Combinations of fertilizer treatments with or without a legume cover crop (red clover) were assessed. The fertilizer treatments studied were: a polymer coated urea (slow-release fertilizer) applied at planting, a conventional urea applied at planting, side-dress treatment of a solution of urea and ammonium nitrate in water containing 28% nitrogen with two different application rates applied in the early summer, and a control. The legume cover crop was incorporated in the soil in the previous fall, and acts as a slow release fertilizer as nitrogen is made available to the following crop as the plants decompose. Treatments were compared based on crop yield, overall economic return, and the potential for nitrate leaching. The potential for nitrate leaching was evaluated with bi-weekly shallow soil core during the growing season, and deep soil cores taken before planting, after harvest and the following spring. The deep cores allowed changes in nitrate storage below the rooting zone to be assessed. The results of this study highlight the importance of timing of fertilizer applications and rate of fertilizer applications. Treatments which provide a delay in the release or application of fertilizer, the polymer-coated urea, the calculator-rate side-dress and the clover cover crop, were found to be advantageous. The polymer-coated urea treatments and side-dress treatments were found to reduce leaching compared to the conventional urea treatment. Treatments with the clover cover crops were not found to reduce crop yields or increase leaching potential, and lower fertilizer costs associated to this practice were found to have a positive economic effect. Plots treated with the high-rate side-dress fertilizer application lost more nitrate to the subsurface compared to the other treatment options, and an economic disadvantage was observed as yields did not compensate for higher fertilizer costs. The study highlights the advantages of the different treatments under study, which may be used to inform policy makers and farmers in the selection of economically and environmentally sustainable nutrient management BMP options. Groundwater monitoring at the site over the years has indentified interesting recharge dynamics, particularly in the vicinity of an ephemeral stream which develops annually during spring and winter melt events in a low lying area of the study site. It was hypothesized that rapid recharge could occur beneath the stream allowing for surface water to quickly reach groundwater, posing a threat to municipal water wells. The current framework of source water protection does not take into account the potential risk posed by this type recharge event. At this field site, rapid infiltration associated with this type of event may pose a risk to drinking water quality due to the proximity of the stream to the pumping wells and the nature of the aquifer. The second study examines rapid groundwater recharge processes beneath the ephemeral stream during the course of a spring melt in 2010. The goals of the study were to quantify recharge at one location beneath the stream and to assess whether temperature variations above the water table can be used as a tracer to reasonably estimate recharge during a short live recharge event. A novel housing for the temperature sensors was designed in order to deploy and position them into gravelly materials within the vadose zone, which reduced the potential for the formation of preferential pathways and permitted the retrieval of the sensors at a later date. Field data were collected during the course of the spring melt period from a network of groundwater monitoring wells and subsurface temperature sensors. Spatial and temporal changes in groundwater geochemistry, hydraulic head and temperature were were used to characterize recharge dynamics at the field site. Recharge beneath a segment of the ephemeral stream was quantified through the numerical analysis of the field data using Hydrus 1-D, a one-dimensional numerical model designed to simulate soil water flow and heat transport in variably saturated porous media. Site specific data were used to create the model domain, provide estimates of physical parameters, and to define initial and time variable boundary conditions. Model parameters were first calibrated by simulating periods where it was expected that soils would be gravity drained with minimal soil water flow, and then further refined by simulating the period when the ephemeral stream was present. A final set of parameters was determined, and the initial gravity drained conditions were re-simulated. The model was able to reproduce field observations under different flow scenarios using the final set of parameters, suggesting that the conceptual model and final model domain representative of the actual field conditions. The successful simulation of the field data sets under the different flow scenarios also increases confidence in the uniqueness of the model results. The model estimated that 0.15 m of recharge occurred beneath the instrumented site during the period between March 9th and March 22nd of 2010 when the ephemeral stream was present. This represents approximately a third of the expected total annual recharge for this location. Regional changes in hydraulic head, groundwater temperature and groundwater chemistry provided additional insight into the dynamic nature of the recharge process during the spring meld period and further illustrated the spatial variability of the aquifers’ response to the stream. The study found that the use of temperature as a tracer provided useful and quantifiable insight into recharge phenomena. The results of this study suggest that high rates of rapid recharge occur beneath the ephemeral stream, and are spatially variable. This type of focused infiltration that occurs during the spring melt may represent a risk to municipal water quality if the infiltrating waters are carrying contaminants.

Zeolites have been used in agriculture since the 1960s, due to the effectiveness of these crystalline microporous solids as soil amendments for plant growth, their cation exchange capacity (CEC) and slow-release fertilizer properties. Most work on slow-release fertilizers has focused on natural Clinoptilolite, Phillipsite and Chabazite. The aim of this study was to synthesize zeolites, study their effectiveness as soil amendments and their ability to act as controlled release fertilizers to decrease nitrate leaching. Nitrate pollution of groundwater is a major agro-environmental concern. The zeolites Phillipsite and Linde-type F were synthesized from aluminosilicate gels; ion exchanged to introduce ammonium and characterized using X-ray diffraction (XRD), X-ray fluorescence (XRF), Thermo-gravimetric analysis (TGA) and Scanning electron microscopy (SEM) techniques, both before and after ion exchange. Ammoniumexchanged Phillipsites (natural and synthetic), ammonium-exchanged synthetic Linde-type F (the zeolite having highest affinity towards ammonium) and ammonium exchanged Phillipsites (high crystalline and high aluminium) were compared with conventional NPK fertilizer.Three glasshouse experiments were performed to study the effects of zeolite-amended soils on maize growth. Ion exchanged synthetic and natural Phillipsites were first used as soil amendments (w/w 2, 4, 8% zeolite to soil). Synthetic Phillipsite, at 2% loading, resulted in the most significant improvement in both plant growth and phased ammonium release. The synthetic ammonium-exchanged zeolites Phillipsite and Linde-type F (at w/w 1, 2, 4%) were then compared; synthetic Phillipsite, at 2% loading, again resulted in the most significant plant growth response with an increase (≥15%) in shoot dry weight and a decrease (≥30%) in nitrate leaching. Experiments using unexchanged synthetic Phillipsite (at w/w 2%), but with added NPK fertilizer, showed increased plant growth and decreased nitrate leaching, compared with parallel experiments containing unexchanged synthetic Linde-type F (at w/w 2%) and a conventional fertilizer amended soil. This revealed the beneficial effect of Phillipsite for soil amendment, even without ion exchange to the ammonium form. To study the physico-chemical properties affecting the release of ammonium from the Phillipsite framework; high crystalline/low aluminium and low crystalline/high aluminium forms were synthesized and ion exchanged. Both forms were introduced as soil amendments (at w/w 1 and 2%) and experiments showed that the lower zeolite crystallinity decreased cation exchange and therefore decreased nitrate leaching. Experimental results from the glasshouse experiments and cation exchange capacity (CEC) experiments suggest that synthetic Phillipsite, at lower loadings (1 and 2% w/w zeolite to soil) have most potential as soil amendments for both plant growth and controlled-release applications. This conclusion is supported by soil leachate and shoots dry weight analysis. Furthermore, Phillipsite, synthesized in a low crystalline and low ammonium form, may be an even better soil amendment for controlled release of ammonium, which will thereby further decrease nitrate pollution.

This thesis presents two interrelated studies that consider nutrient management and seasonal changes in recharge on agricultural lands within the context of source water protection. The research focuses first on the management of the risk to groundwater quality through the implementation of various nutrient management practices and secondly considers the dynamic nature of the transport pathway to the groundwater system associated with seasonal changes in climate and hydrology. The combined results provide insight into several of the key factors influencing the protection of groundwater sources within the agricultural landscape. Field work was completed between 2009 and 2010 on an agricultural field near the City of Woodstock, Ontario. The site is located within a source water protection area; the two-year travel time zone of the Thornton Well Field which represents the primary water supply for the City of Woodstock and which has experienced chronic increases in nitrate concentrations over the last few decades. The wells are completed in glacial overburden consisting of intermingling sand and gravel till aquifers which overly a limestone bedrock aquifer. Agricultural best or beneficial management practices (BMPs) field have been implemented and monitored since 2004. The BMPs were adopted in order to reduce nitrogen losses to the aquifer, and consisted of a reduction in nitrogen fertilizer application rates over a series of agricultural fields located near the well The first study is a one year experiment designed to compare alternative nutrient management practices for corn. Combinations of fertilizer treatments with or without a legume cover crop (red clover) were assessed. The fertilizer treatments studied were: a polymer coated urea (slow-release fertilizer) applied at planting, a conventional urea applied at planting, side-dress treatment of a solution of urea and ammonium nitrate in water containing 28% nitrogen with two different application rates applied in the early summer, and a control. The legume cover crop was incorporated in the soil in the previous fall, and acts as a slow release fertilizer as nitrogen is made available to the following crop as the plants decompose. Treatments were compared based on crop yield, overall economic return, and the potential for nitrate leaching. The potential for nitrate leaching was evaluated with bi-weekly shallow soil core during the growing season, and deep soil cores taken before planting, after harvest and the following spring. The deep cores allowed changes in nitrate storage below the rooting zone to be assessed. The results of this study highlight the importance of timing of fertilizer applications and rate of fertilizer applications. Treatments which provide a delay in the release or application of fertilizer, the polymer-coated urea, the calculator-rate side-dress and the clover cover crop, were found to be advantageous. The polymer-coated urea treatments and side-dress treatments were found to reduce leaching compared to the conventional urea treatment. Treatments with the clover cover crops were not found to reduce crop yields or increase leaching potential, and lower fertilizer costs associated to this practice were found to have a positive economic effect. Plots treated with the high-rate side-dress fertilizer application lost more nitrate to the subsurface compared to the other treatment options, and an economic disadvantage was observed as yields did not compensate for higher fertilizer costs. The study highlights the advantages of the different treatments under study, which may be used to inform policy makers and farmers in the selection of economically and environmentally sustainable nutrient management BMP options. Groundwater monitoring at the site over the years has indentified interesting recharge dynamics, particularly in the vicinity of an ephemeral stream which develops annually during spring and winter melt events in a low lying area of the study site. It was hypothesized that rapid recharge could occur beneath the stream allowing for surface water to quickly reach groundwater, posing a threat to municipal water wells. The current framework of source water protection does not take into account the potential risk posed by this type recharge event. At this field site, rapid infiltration associated with this type of event may pose a risk to drinking water quality due to the proximity of the stream to the pumping wells and the nature of the aquifer. The second study examines rapid groundwater recharge processes beneath the ephemeral stream during the course of a spring melt in 2010. The goals of the study were to quantify recharge at one location beneath the stream and to assess whether temperature variations above the water table can be used as a tracer to reasonably estimate recharge during a short live recharge event. A novel housing for the temperature sensors was designed in order to deploy and position them into gravelly materials within the vadose zone, which reduced the potential for the formation of preferential pathways and permitted the retrieval of the sensors at a later date. Field data were collected during the course of the spring melt period from a network of groundwater monitoring wells and subsurface temperature sensors. Spatial and temporal changes in groundwater geochemistry, hydraulic head and temperature were were used to characterize recharge dynamics at the field site. Recharge beneath a segment of the ephemeral stream was quantified through the numerical analysis of the field data using Hydrus 1-D, a one-dimensional numerical model designed to simulate soil water flow and heat transport in variably saturated porous media. Site specific data were used to create the model domain, provide estimates of physical parameters, and to define initial and time variable boundary conditions. Model parameters were first calibrated by simulating periods where it was expected that soils would be gravity drained with minimal soil water flow, and then further refined by simulating the period when the ephemeral stream was present. A final set of parameters was determined, and the initial gravity drained conditions were re-simulated. The model was able to reproduce field observations under different flow scenarios using the final set of parameters, suggesting that the conceptual model and final model domain representative of the actual field conditions. The successful simulation of the field data sets under the different flow scenarios also increases confidence in the uniqueness of the model results. The model estimated that 0.15 m of recharge occurred beneath the instrumented site during the period between March 9th and March 22nd of 2010 when the ephemeral stream was present. This represents approximately a third of the expected total annual recharge for this location. Regional changes in hydraulic head, groundwater temperature and groundwater chemistry provided additional insight into the dynamic nature of the recharge process during the spring meld period and further illustrated the spatial variability of the aquifers’ response to the stream. The study found that the use of temperature as a tracer provided useful and quantifiable insight into recharge phenomena. The results of this study suggest that high rates of rapid recharge occur beneath the ephemeral stream, and are spatially variable. This type of focused infiltration that occurs during the spring melt may represent a risk to municipal water quality if the infiltrating waters are carrying contaminants.

O sistema integração lavoura pecuária (ILP) atende muitas diretrizes para estabelecer um manejo sustentável de produção agropecuária. Consiste em integrar na mesma área, a produção agrícola e pecuária de forma que haja o cultivo de grãos e estabeleça uma pastagem para a criação de animais. O consórcio de milho com braquiária é uma tecnologia utilizada para se atingir os objetivos da ILP. Trata-se de técnica de cultivo de milho junto com a braquiária sem prejuízo ao milho, e que a braquiária possa se estabelecer na área após a colheita do milho. A eficiência da adubação nitrogenada (EAN) na cultura do milho é discutida na literatura em trabalhos que utilizaram fertilizantes marcados com 15N. Os dados são variados pelo motivo do nitrogênio ter dinâmica complexa no sistema produtivo. Trabalhos que avaliaram a EAN no consórcio de milho com braquiária são escassos na literatura internacional, e não se sabe quanto do fertilizante nitrogenado aplicado é absorvido pela planta forrageira, e se é necessário um aumento da dose para não ocorrer falta de nitrogênio neste sistema de produção. Esta tese foi realizada com os seguintes objetivos (i) avaliar a influência da braquiária no aproveitamento do fertilizante nitrogenado, em razão das formas de implantação do consórcio milho - braquiária utilizadas no Brasil, (ii) avaliar a eficiência do N proveniente de fertilizante de liberação gradual, (iii) verificar a possibilidade da aplicação a lanço de ureia revestida. A primeira pesquisa foi desenvolvida nas cidades de São Desidério-BA e Piracicaba-SP, e foi comprovado que a presença da braquiária não afetou a produtividade de milho nem a recuperação do 15N-fertilizante. As formas recomendadas para implantação do consórcio de milho com braquiária são: (i) braquiária semeada a lanço antes da semeadura do milho; (ii) braquiária no centro das entrelinhas de milho; (iii) braquiária junto com o fertilizante de semeadura do milho, (iv) braquiária junto com o fertilizante de cobertura incorporado nas entrelinhas. Não é necessário aumentar a dose do fertilizante nitrogenado em sistema de milho consorciado com braquiária, uma vez que a braquiária absorve no máximo 4,3 kg ha-1 do N-fertilizante. A segunda pesquisa foi realizada nas cidades de Taquarituba-SP e Uberlândia-MG, e demonstrou que a produtividade de milho e o acúmulo de N não variam com o uso de ureia de liberação controlada aplicadas a lanço e incorporada em relação à ureia comum. As ureias de liberação controlada não promovem maior recuperação do 15N-fertilizante pelo milho e pela braquiária em relação à ureia comum, nem a produção de biomassa da braquiária. O N do fertilizante absorvido pela braquiária consorciada com milho é menos de 1% de todo N acumulado no sistema, e no máximo 2% do N-fertilizante aplicado. As ureias de liberação controlada não viabilizam a aplicação a lanço, e dependem das mesmas condições climáticas que a ureia comum para obterem bom desempenho. / Crop-livestock integration system (CLI) attends many guidelines for establishing a sustainable agricultural production. CLI consists in integrating agricultural and livestock production in the same area, in order to establish a pasture for grazing animals after a grain production. Intercropping corn and palisadegrass is a technology used to obtain CLI objectives. In this technique the palisadegrass is cropped together with corn without affecting corn yield, and after harvest the palisadegrass grows in the area in order to form a pasture. Studies that evaluated nitrogen use efficiency (NUE) in maize in crop systems with labeled 15N-fertilizer shows varied data. This is due to nitrogen\'s complex dynamics in the production system. However, studies that evaluated NUE in corn intercropped with palisadegrass are scarce in the literature, and it is unknown how much of nitrogen fertilizer applied is uptake by the palisadegrass, and if an increase in nitrogen rate is necessary to avoid lack of nitrogen in production system. The aims of this thesis was to evaluate: (i) the influence of palisadegrass in the use of nitrogen fertilizer, according to forms of implantation of palisade grass used in Brazil, (ii) the efficiency of N from gradual release fertilizer,(iii) the viability of broadcast application of coated urea on intercropping system. The first study was conducted in the sites of Sao Desidério-BA and Piracicaba-SP, and it demonstrated that the presence of palisadegrass did not affect corn yield neither 15N-fertilizer recovery. Intercropping system can be established by the followings forms: (i) palisadegrass broadcasted before maize sown, (ii) placed between the rows of maize, (iii) palisadegrass applied together with corn fertilizer, (iv) with topdressing fertilizer in furrows. It is not necessary increase N rate in the intercropping system because palisadegrass uptakes at most of 4.3 kg ha-1 of N-fertilizer. The second research was conducted in two sites, Taquarituba-SP and Uberlândia-MG, and demonstrated that the use of coated urea did not differ in corn yield and N uptake in relation to the common urea, either when it was incorporated or broadcast applied. The coated urea neither promotes better recovery of the 15N-fertilizer by corn and braquiária in relation to the common urea, nor increases the palisadegrass biomass production. Nitrogen fertilizer uptake by palisadegrass represents less than 1% of total N uptake in the intercropping system, and a maximum of 2% of N-fertilizer applied The slow release urea does not enable the broadcast placement, and its efficiency depends upon the same climatic conditions of the common urea.

O sistema integração lavoura pecuária (ILP) atende muitas diretrizes para estabelecer um manejo sustentável de produção agropecuária. Consiste em integrar na mesma área, a produção agrícola e pecuária de forma que haja o cultivo de grãos e estabeleça uma pastagem para a criação de animais. O consórcio de milho com braquiária é uma tecnologia utilizada para se atingir os objetivos da ILP. Trata-se de técnica de cultivo de milho junto com a braquiária sem prejuízo ao milho, e que a braquiária possa se estabelecer na área após a colheita do milho. A eficiência da adubação nitrogenada (EAN) na cultura do milho é discutida na literatura em trabalhos que utilizaram fertilizantes marcados com 15N. Os dados são variados pelo motivo do nitrogênio ter dinâmica complexa no sistema produtivo. Trabalhos que avaliaram a EAN no consórcio de milho com braquiária são escassos na literatura internacional, e não se sabe quanto do fertilizante nitrogenado aplicado é absorvido pela planta forrageira, e se é necessário um aumento da dose para não ocorrer falta de nitrogênio neste sistema de produção. Esta tese foi realizada com os seguintes objetivos (i) avaliar a influência da braquiária no aproveitamento do fertilizante nitrogenado, em razão das formas de implantação do consórcio milho - braquiária utilizadas no Brasil, (ii) avaliar a eficiência do N proveniente de fertilizante de liberação gradual, (iii) verificar a possibilidade da aplicação a lanço de ureia revestida. A primeira pesquisa foi desenvolvida nas cidades de São Desidério-BA e Piracicaba-SP, e foi comprovado que a presença da braquiária não afetou a produtividade de milho nem a recuperação do 15N-fertilizante. As formas recomendadas para implantação do consórcio de milho com braquiária são: (i) braquiária semeada a lanço antes da semeadura do milho; (ii) braquiária no centro das entrelinhas de milho; (iii) braquiária junto com o fertilizante de semeadura do milho, (iv) braquiária junto com o fertilizante de cobertura incorporado nas entrelinhas. Não é necessário aumentar a dose do fertilizante nitrogenado em sistema de milho consorciado com braquiária, uma vez que a braquiária absorve no máximo 4,3 kg ha-1 do N-fertilizante. A segunda pesquisa foi realizada nas cidades de Taquarituba-SP e Uberlândia-MG, e demonstrou que a produtividade de milho e o acúmulo de N não variam com o uso de ureia de liberação controlada aplicadas a lanço e incorporada em relação à ureia comum. As ureias de liberação controlada não promovem maior recuperação do 15N-fertilizante pelo milho e pela braquiária em relação à ureia comum, nem a produção de biomassa da braquiária. O N do fertilizante absorvido pela braquiária consorciada com milho é menos de 1% de todo N acumulado no sistema, e no máximo 2% do N-fertilizante aplicado. As ureias de liberação controlada não viabilizam a aplicação a lanço, e dependem das mesmas condições climáticas que a ureia comum para obterem bom desempenho. / Crop-livestock integration system (CLI) attends many guidelines for establishing a sustainable agricultural production. CLI consists in integrating agricultural and livestock production in the same area, in order to establish a pasture for grazing animals after a grain production. Intercropping corn and palisadegrass is a technology used to obtain CLI objectives. In this technique the palisadegrass is cropped together with corn without affecting corn yield, and after harvest the palisadegrass grows in the area in order to form a pasture. Studies that evaluated nitrogen use efficiency (NUE) in maize in crop systems with labeled 15N-fertilizer shows varied data. This is due to nitrogen\'s complex dynamics in the production system. However, studies that evaluated NUE in corn intercropped with palisadegrass are scarce in the literature, and it is unknown how much of nitrogen fertilizer applied is uptake by the palisadegrass, and if an increase in nitrogen rate is necessary to avoid lack of nitrogen in production system. The aims of this thesis was to evaluate: (i) the influence of palisadegrass in the use of nitrogen fertilizer, according to forms of implantation of palisade grass used in Brazil, (ii) the efficiency of N from gradual release fertilizer,(iii) the viability of broadcast application of coated urea on intercropping system. The first study was conducted in the sites of Sao Desidério-BA and Piracicaba-SP, and it demonstrated that the presence of palisadegrass did not affect corn yield neither 15N-fertilizer recovery. Intercropping system can be established by the followings forms: (i) palisadegrass broadcasted before maize sown, (ii) placed between the rows of maize, (iii) palisadegrass applied together with corn fertilizer, (iv) with topdressing fertilizer in furrows. It is not necessary increase N rate in the intercropping system because palisadegrass uptakes at most of 4.3 kg ha-1 of N-fertilizer. The second research was conducted in two sites, Taquarituba-SP and Uberlândia-MG, and demonstrated that the use of coated urea did not differ in corn yield and N uptake in relation to the common urea, either when it was incorporated or broadcast applied. The coated urea neither promotes better recovery of the 15N-fertilizer by corn and braquiária in relation to the common urea, nor increases the palisadegrass biomass production. Nitrogen fertilizer uptake by palisadegrass represents less than 1% of total N uptake in the intercropping system, and a maximum of 2% of N-fertilizer applied The slow release urea does not enable the broadcast placement, and its efficiency depends upon the same climatic conditions of the common urea.

No description available.