In 2016 the Iowa Watershed Approach (IWA) was created to increase community resiliency against flooding, to develop hydrologic assessments that would identify strategies to reduce flooding, and to implement those strategies within nine identified watersheds that experienced flooding between 2011 and 2013. One of the nine watersheds was the Upper Iowa watershed located in northeast Iowa. This thesis focuses on the work that has been done to create a hydrologic assessment of the Upper Iowa watershed. The hydrologic assessment identifies potential conservation practices, creates a hydrologic model to assess the hydrologic cycle over the past ten years, and identifies strategies to reduce flooding within the watershed. Many potential agricultural conservation practices within the Upper Iowa watershed were identified and trends relating to the soil, land use, and topography were determined. In addition, a methodology to compare potential conservation practices with existing conservation practices actually in place was developed including a tool to estimate the size of grassed waterways to NRCS design guidelines. The comparison validated the methodologies used to identify potential practice placements, identified locations where potential practices could be implemented, and showed how stakeholder preferences influence conservation implementation. Additionally, a hydrologic model of the Upper Iowa watershed was developed, using the new Generic Hydrologic Overland-Subsurface Toolset model and calibrated to simulate the time period of 2007 through 2016. The model was evaluated against water balance ratios and performance statistics calculated from measured data. The model achieved Nash Sutcliffe Efficiency scores for streamflow above 0.7 and percent bias scores between ±12% for the three wettest years of 2008, 2013, and 2016. With the calibrated model, the benefits of continuous cover crop implementation were investigated under current conditions and under increased extreme precipitation intensity expected from climate change over the next half century. The results of this investigation determined that continuous cover crops increased evapotranspiration within the early half of the year creating more storage within the soil. Thus the flood risk from convective storms during the summer was lowered. In addition, the benefits from cover crops in terms of peak flow and volume reductions were cumulative increasing each consecutive year and were proportional to the percentage of cover cropped area. Lastly, a scenario using cover crops in a future extreme precipitation environment resulted in a reduction of peak discharge to current conditions. The results of this thesis will guide both future work within the Upper Iowa watershed and contribute to the knowledge of hydrologic planning and modeling within agricultural watersheds.

Cette étude présente un modèle biophysique de fonctionnement de culture capable de traduire la dynamique de l'évolution de tout couvert végétal, sous différentes conditions abiotiques du milieu (température, eau et rayonnement) mais aussi de sols et de climats. L'approche développée pour le suivi de la cinétique de croissance et de développement des couverts reste très proche de la réalité physiologique de leurs fonctionnements mais aussi de celle liée aux interventions humaines qui se trouve alors compatible avec l'échelle de notre modélisation. Alors que l'utilisation d'une simple loi linéaire d'action de la température par les modèles de fonctionnements des cultures permet de prendre en partie l'effet de l'action de la température sur une gamme assez limitée de température active des espèces végétales, l'approche, assez originale, adoptée dans ce modèle permet l'utilisation d'une vraie loi d'action de la température sur les différents processus biologiques liés au développement et à la croissance, valable sur toute la gamme des températures biologiquement actives. Aussi, cette approche très générique permet de suivre la cinétique des vitesses d'évolution de toutes entités d'une plante, quelque que soit l'espèce ou la variété, et de travailler à n'importe quelle échelle de temps (jour, heure). L'adaptation du modèle logistique (largement utilisé pour décrire les processus biologiques) au contexte physiologique des plantes a permis une description assez originale de la dynamique de la croissance en fonction du développement, prenant en compte à tout moment l'effet d'une contrainte du milieu et sa rétroaction sur la dynamique d'évolution du couvert. La régulation de la croissance a été possible dans ce modèle de développement-croissance à travers la modulation de sa vitesse de croissance (processus le plus sensible au stress) en fonction de deux stress les plus importants chez les végétaux, soit l'eau et le rayonnement. A partir d'un petit nombre de paramètres facilement abordable en bibliographie, il est possible de caractériser la dynamique d'évolution de tout type de couvert végétal évaluant en conditions de sol et de climat variés. Couplé au modèle de bilan hydrique Bilhyna, ce dernier est capable de fonctionner sous différentes situations du milieu, conditions pluviales limitantes notamment, et de gérer ainsi le manque d'eau avec des apports possibles par irrigation de complément où limitées aux besoins tout au long de la croissance intègre alors la rétroaction d'une contrainte du milieu sur la dynamique de l'évolution du couvert. Pour étudier notre modèle, nous avons confronté dans un premier temps les sorties du modèle de loi d'action de la température sur les vitesses de développement aux résultats expérimentaux concernant les cultures du Lin, du maïs et du blé, issus de plusieurs travaux d'auteurs assez connus et tirés de la bibliographie. La confrontation des résultats modèle-mesures a donné des résultats très satisfaisants. Nous avons dans une seconde partie confronté les sorties de l'ensemble du modèle biophysique couplé à bilhyna aux mesures expérimentales que nous avons réalisé au champ sur une période de cinq années, et portant sur deux cultures : le sorgho et du blé. Nous avons ainsi suivi l'évolution de la dynamique de ces couverts à travers leurs trois composantes (LAI, la hauteur du couvert et la profondeur de ses racines) de même que celle des stocks d'eau du sol durant toute la période de la croissance des cultures. Les résultats de la confrontation des sorties du modèle avec les mesures expérimentales ont été assez satisfaisants. [Suite et fin du résumé dans la thèse]. / This study presents a biophysical model of crop functioning can translate the dynamics of the evolution of any cover crops under different abiotic conditions of the environment (temperature, water and radiation), soil and climate. The approach developed for monitoring the kinetics of growth and development of crops is very close to the physiological reality of their functioning but also those linked to human intervention which is then compatible with the scale of our modeling. While the use of a simple linear law of action of the temperature bay patterns crop functioning model can take part in the effect of the action of temperature on a fairly limited temperature range of plant species active, the original approach which was adopted in this model allows the use of a true law of action of temperature on various biological processes associated with the development and growth, valid over the entire temperature range biologically active. Also, this approach very generic allows to follow the kinetics of the speed of evolution of all entities of a plant, no matter the species or variety, and work at any scale of time (days, hours). The adaptation of the logistic model (widely used to describe biological processes) to the physiological context of the plants has a quite original description of the dynamics of growth in terms of development, taking into account at any time the effect of stress the environment and feedback on the dynamics of cover change. The regulation of growth was possible in this model of development-growth through the modulation of its rate of growth (a process most sensitive to stress) according to two of the most important stress in plants, water and radiation. From a small number of parameters easily affordable in the bibliography, it is possible to characterize the dynamic evolution of all types of vegetation in soil conditions and climate varied. Coupled with the water balance model Bilhyna, it is capable of operating in different situations of the environment, including limiting rained conditions, and managing the water shortage with possible contributions from supplemental irrigation or limited needs throughout growth, then incorporates the feedback of environmental constraints on the dynamics of the cover crop evolution. To study our model, we compared initially exits the model law action of temperature on development rates to the experimental results on flax, corn and wheat from several studies of authors known and fairly drawn from the bibliography. Comparing the results-model measures gave very satisfactory results. We have, in a second part, faced the outputs of the coupled biophysical model bilhyna to experimental measurements we have done in the field over a period of five years, and on two crops: sorghum and wheat. We have followed the evolution of the dynamics of these cover crop through their three components (LAI, canopy height and depth of its roots) as well as stocks of soil water during the entire period of growth cultures. The results of the comparison of model outputs with experimental measurements was quite satisfactory. Last and final summary in the thesis.

This research assessed the seasonal effects of contrasting tillage and crop rotation systems on soil ammonia oxidizing bacteria (AOB) and archaea (AOA). Four different cropping systems under till and no-till were analyzed in a 30 year-old agricultural field trial. Samples were collected during the 2010 growing season at times corresponding with agronomic events. Nucleic acids were preserved in the field and subsequently analyzed by quantitative real-time polymerase chain reactions (qPCR). Tillage decreased AOB activity and abundance in the plow layer (0-15 cm) immediately after fall moldboard plow events, but observed AOB dynamics at other times suggest tillage had a long-term distribution effect across depth (0-30 cm). AOA abundance was significantly greater in no-till plots at all times indicating tillage had longer-term effects on these communities. Crop rotation had minimal effect on AOB and AOA, but there was a noted yield advantage for corn following wheat, regardless of tillage treatment. / OMAFRA Highly Qualified Personnel Program, NSERC

Cabbage is one of the most important and widely grown crops in KwaZulu-Natal (KZN). In cabbage production, no clear cropping methods exist (other than succession cropping) to allow the soil to recover its fertility status naturally after the harvested has crop absorbed nutrients from the soil. Succession cropping system is extensively practiced by cabbage farmers. Succession cropping is when a succeeding vegetable crop is planted immediately after harvesting the preceding crop. This does not allow soil fertility status to be balanced by soil microbes in an environmentally friendly approach. Instead, synthetic fertilizers are heavily used to rectify soil fertility status and these have negative impacts on the soil in the long term, followed by yield decline. However, the economic downturns and green environment awareness have caused researchers and some farmers to focus more on developing environmentally healthy crop production technologies. A priority in this study was to elucidate effects of cover crops-green manure as rotational crops in cabbage production. The experimental site is located at Cedara Research Station. In 2009, soil samples were taken from the top 30 cm of the soil profile, in a zigzag pattern in 5 m x 5 m grids for fertility analysis. Results were used to determine nutrient deficiencies, and blanket application of phosphorus and potassium followed according to each grid’s deficiency. The study was divided into two cycles, with each cycle consisting of season one and season two. The study was conducted over a two year period. Cycle one, season one, 2009/2010 (Dec-Mar): four treatments (sunn hemp: planted at 50 kg/ha seeding rate; forage sorghum: planted at 50 kg/ha seeding rate; mixture of sunn hemp-forage sorghum: each planted at 25 kg/ha seeding rate and control: cabbage planted at 30 cm within rows x 60 cm between rows) were used. The statistical design of the study was a 4x4 Latin Square experiment repeated twice in adjacent fields (347 m2 each) 6 m apart, with a total of 32 plots. Each experimental plot was 8.5 m x 9 m. Genstat Package, 9th Edition was used for data analysis. Standard cabbage production recommendations were followed in control treatments. Cabbage yield was determined in all control plots. Weed coverage percentages were determined in all four treatments. Cycle one, season two, 2010, (Apr-Aug): all 32 plots from season one were each split into four, in a Split Plot design, resulting in a total of 128 plots in both fields. Nitrogen was applied at four different levels: 0, 80, 160 and 240 kg N/ha. Standard cabbage production methods were followed again as in the control treatment in season one. Cover crops were replaced by planting cabbage. Cabbage was repeated in the control plots. Cabbage yield, cabbage leaf nutrients, soil nitrate and ammonium nitrate and soil carbon to nitrogen (C:N) ratio were measured. Cycle two, season one, 2010 (Sep-Dec): The same method in cycle one, season one was repeated. Cycle two, season two, 2010/2011, (Dec-Apr): The same method in cycle one, season two was repeated. Although in this study there was visibly a large amount of residues left over after the trial was harvested, the use of a tractor-drawn slasher was not very effective. The slashed material was not chopped into smaller pieces, as it would if a roll-chopper had been used. A tractor-drawn slasher was used because it is a tool available to many farmers. As a result, it was not a simple process to transplant seedlings mechanically, due to the amount of organic matter that was in the soil after it had been incorporated. The mechanical planter pulled off, removed and became blocked by the residues, and as a result it was not able to operate as it would in normal soils. The residues removed soil from the furrows and that caused seedlings to fall over as all the soil for the root system support had been moved by the planter and stuck residues. The planter had to be assisted by hand planting seedlings that were not properly planted mechanically. Hence, from the operational perspective, the choice of tools for chopping were not effective in this study and this is something to be considered in future studies, where it will be necessary to compare different tools for planting and cover crop incorporation into the soil. During the present study, soil N content in different plots had significant differences (P=0.05). The control showed high levels of total N content, but this was not related to the low yields exhibited by cabbage after cabbage at all levels of N. Since, where there were cover crops, the N content was low, this could mean that N was immobilized, compared to the cabbage treatments where plenty of N was available. Immobilized N is thus not available for leaching, polluting the environment. The yield of cabbage was significantly lowest in controls. The study showed that cover crop-green manure use has a positive effect in terms of yield improvement. The cabbage yields from the sunn hemp plots at a 0 kgN/ha were significantly different from the yield of cabbage planted following cabbage at 240 kgN/ha N. The study also showed that N is not the only yield determinant in cabbage production. Too much N has a tendency to suppress cabbage yields. The cover crop-green manures selected for this study were shown to be ineffective in suppressing weeds. This was true even though the weed coverage percentage in each of the cover crop-green manure plots was above 65%, except for the cabbage crop. This study did not separate different weeds, but the most dominant weeds were Amaranthus hybridus (pigweed), Galinsoga parviflora (gallant soldier), Bidens pilosa (common blackjack) and Cyperus esculentus (yellow nutsedge). These weeds were effectively controlled in the cabbage sole crop by the use of herbicides and mechanical weeding. The result of cover crop-green manures not suppressing weeds was significantly associated with the cover crop-green manure seeding rate. This study has been a starting point in the development of cover crops-green manure as rotational crops in cabbage production. It is concluded that cover crop-green manure (sunn hemp and forage sorghum) used in this study for vegetable (cabbage) production has proven to be successful in improving yields. Yields obtained from cover crop-green manure treatments were better than yields obtained from - conventional tillage methods for cabbage production (control). However, in cabbage, weed suppression and soil N content, failed to improve significantly in response to the cover crop green manures used. The high plant population density under a cover crop, combined with weed population, may lead to high uptake of soil N for plant growth, leaving less N in the soil and in the plant. In the sole cabbage crop, because of low competition, there was adequate uptake of N for plant growth and yet the crop was not exhaustive of soil N. Further research is required in the following areas: comparison of cabbage with other vegetable crops in response to the effect of the selected cover crops; comparison of mechanical weeding and herbicide use as means of controlling weeds during cover crop-green manure growth; identification of dominant weeds in the presence and absence of cover crops, and monitoring of soil water relations and other fertiliser effects. / Thesis (M.Sc.)-University of KwaZulu-Natal, Pietermaritzburg, 2012.

Unintentional nitrogen (N) loss from agroecosystems produces greenhouse gases, induces eutrophication, and is costly for farmers; therefore, adoption of conservation agricultural management practices, such as no-till and cover cropping, has increased. This study assessed N loss via leaching, NH3 volatilization, N2O emissions, and N retention in plant and soil pools of corn conservation agroecosystems across a year. Three systems were evaluated: 1) an unfertilized organic system with cover crops Vicia villosa, Triticum aestivum, or a mix of the two; 2) an organic system with a Vicia cover crop employing three fertilization schemes (0 N, organic N, or a cover crop N-credit approach); 3) a conventional system with a Triticum cover crop and three fertilization techniques (0 N, urea N, or organic N). During cover crop growth, species affected N leaching but gaseous emissions were low across all treatments. During corn growth, cover crop and fertilizer approach affected N loss. Fertilized treatments had greater N loss than unfertilized treatments, and fertilizer type affected gaseous fluxes temporally and in magnitude. Overall, increased N availability did not always indicate greater N loss or yield, suggesting that N conserving management techniques can be employed in conservation agriculture systems without sacrificing yield.

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior / The southwest region of Rio Grande do Sul (RS) state has widespread areas with sandy soils in the process of sandification. In the present study, we report the effect of different intercropping in blackberry plants on the soil recuperation and crop productivity. The experiment was conducted in São Francisco de Assis located in southwest region of the RS. The soil was a typical Psament with 60 g kg-1 clay and 0.5 g kg-1 organic matter in the top 0- 10 cm layer. The crops that were intercropped with blackberry were jack bean (Canavalia ensiformis) / oat (Avena strigosa) (JB-O); Brachiaria (Brachiaria decumbens) (BRA) and native grass (NG). The soil recuperation was measured by assessing the C and N stocks in the soil and biological indicators such as the enzymatic activity and soil fauna in relation to traditional grazing native grass (GNP). Results showed that intercropping of crops with blackberry improved soil biological conditions in relation to the GNP. Intercropping of JB-O with blackberry resulted in high dry matter production and C and N accumulation in shoots. Similarly, among the crops BRA appeared to be the crop that has potential to increase C and N stocks in the soils. This effect could be explained the rooting system of this grass. The presence of NG under blackberry helped to achieve average fruit yield and could be used as a strategy to establish the cultivation of blackberry in this region. Moreover, blackberry showed adaptation to the ecological conditions of the sandy soils and can be considered as an alternative crop for 1) recovering and reducing the outspread of sandification 2) as a possible source of income for the farmers of this region. / Na região sudoeste do Rio Grande do Sul (RS) existem extensas áreas com solos arenosos em processo de arenização. O objetivo deste estudo foi de avaliar o efeito de diferentes culturas intercalares a amoreira-preta sobre a recuperação de solo em processo de arenização e produtividade da cultura na região Sudoeste do RS, no município de São Francisco de Assis. O solo do experimento foi um Neossolo Quartzarênico típico com 60 g kg-1 de argila e 0,5 g kg-1 de matéria orgânica na camada de 0-10 cm. Os tratamentos avaliados nas entrelinhas da amoreira-preta foram os seguintes: feijão-de-porco (Canavalia ensiformis)/aveia preta (Avena strigosa) (FP-AP); Brachiaria (Brachiaria decumbens) (BRA); e campo nativo (CN). A recuperação do solo no pomar foi medida através da avaliação da recuperação dos estoques de C e N no solo e de indicadores biológicos como, a atividade enzimática e a fauna do solo em relação ao campo nativo sob pastejo tradicional (CN-T). Os tratamentos FP-AP, BRA e CN nas entrelinhas da amoreira-preta resultaram em melhora das condições biológicas do solo em relação ao CN-T. A combinação de feijão-de-porco e aveia-preta nas entrelinhas da amoreirapreta apresentou maior produção de matéria seca da parte aérea e acúmulo de C e N. A BRA foi a espécie que se destacou quanto a capacidade de promover o aumento do estoque de C e N no solo na entrelinha da amoreira-preta. Efeito esse devido possivelmente ao sistema radicular agressivo desta gramínea. A permanência do CN nas entrelinhas da amoreira-preta, além de permitir a obtenção de média produtividade de frutos, se apresenta como uma alternativa para a redução no custo de implantação e condução do pomar com essa espécie frutífera na região dos solos arenosos do sudoeste do RS. A amoreira-preta apresentou adaptação às condições edafoclimáticas dos solos arenosos do sudoeste do RS, podendo ser considerada como alternativa para a recuperação e redução do avanço das áreas arenizadas e também como uma possibilidade de fonte de renda para o produtor rural desta região do estado.

Made available in DSpace on 2014-06-11T19:30:26Z (GMT). No. of bitstreams: 0 Previous issue date: 2010-06-05Bitstream added on 2014-06-13T20:40:23Z : No. of bitstreams: 1 arroyogarcia_r_dr_botfca.pdf: 1117377 bytes, checksum: 640c0531b51ae26f4c6122ba741bb333 (MD5) / Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) / O manejo inadequado do solo ocasiona a formação de camadas compactadas que prejudicam o desenvolvimento radicular das plantas, diminuindo a disponibilidade de água e nutrientes, enquanto que o acúmulo de carbono pode melhorar a qualidade do solo. Em sistemas com semeadura direta (SSD), com a menor mobilização do solo, pode-se usar, em rotação, plantas com sistema radicular vigoroso, capaz de crescer em condições adversas. Este trabalho teve como objetivo avaliar a ação de espécies de cobertura, gramíneas e uma leguminosa, em rotação com a cultura da soja, nos atributos físicos de um Latossolo, no acúmulo de carbono, nas diferentes frações da matéria orgânica e na produção da soja, em semeadura direta, ao longo de três anos. O experimento foi conduzido em um Latossolo Vermelho distroférrico de textura argilosa, na Fazenda Experimental Lageado, Unesp/Botucatu, nos anos agrícolas de 2006/2007, 2007/2008 e 2008/2009. No outonoinverno foram estabelecidas parcelas com braquiária (Brachiaria ruziziensis), sorgo granífero (Sorghum bicolor) e sorgo consorciado com braquiária. Na primavera, foram cultivados, em subparcelas, milheto (Pennisetum glaucum), cober crop [Sorghum bicolor (L.) Moench x Sorghum sudanense Piper Stapf], crotalária (Crotalaria juncea) ou pousio. A soja foi cultivada como safra de verão. Em março do primeiro ano foram retiradas amostras para caracterização da área experimental. Após o manejo das espécies cultivadas na primavera, no primeiro e terceiro ano, foram retiradas amostras indeformadas nas camadas de 0-5; 7,5-12,5; 15-20; 27,5-32,5 e 47,5-52,5 cm para determinação da densidade do solo, porosidade e curva de retenção de água no solo. Nas mesmas épocas, a estabilidade de agregados foi avaliada em amostras coletadas nas camadas de 0-5 e 5-10 cm. No terceiro ano do experimento, o intervalo hídrico ótimo (IHO) foi determinado... / Compacted layers resulting from inappropriate soil management may impair root growth, thus decreasing water and nutrient acquisition by crops. Conversely, soil quality is improved with soil carbon accumulation. In areas under no-till, crop rotation with plants with vigorous root systems may alleviate soil compaction, as well as increase soil carbon. In this experiment the effects of cover crops on soil physical properties, carbon accumulation, organic matter quality and soybean production under no-till in a compacted soil were studied for three years. The experiment was conducted on a clayey Rhodic Ferralsol, Lageado Experimental Farm, Unesp/Botucatu, in 2006/2007, 2007/2008 and 2008/2009. Congo grass (Brachiaria ruziziensis), grain sorghum (Sorghum bicolor) and a mix of both were cropped during fall-winter. Then, in the spring, pear millet (Pennisetum glaucum), cober crop [Sorghum bicolor (L.) Moench x Sorghum sudanense Piper Stapf] and indian hemp (Crotalaria juncea) were cropped and a treatment under fallow was set on sub-plots. Soybean was cropped as a summer crop. In March of the first year, samples were taken for characterization of the area. Right after spring crops were chemically desiccated in 2006 and 2008, undisturbed soil samples were taken from the layers 0-5; 7.5-12.5; 15-20; 27.5-32.5 and 47.5-52.5 cm to determine bulk density, porosity and water retention curve. At the same time, samples taken from the depths 0-5 and 5-10 cm were used to determine aggregate stability. In the third year, least limiting water range (LLWR) was evaluated in the 7.5-12.5 and 27.5-32.5 cm soil layers. Organic matter characterization was done in the third year, in the depths of 0-5 and 5-10 cm. Roots of spring crops were sampled in the layers 0-5; 5-10; 10-20; 20-40 and 40- 60 cm, one day before chemical desiccation in all growing seasons. Soybean roots were sampled in the same depths at R2 each... (Complete abstract click electronic access below)

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPES / The inclusion of cover crops in agricultural production systems has received attention for the ability to improve the multifunctionality of the soil. In order to improve soil structure and soil physical-hydric properties, especially soil water infiltration, the objective of this study was: (a) to evaluate the effect of different species of winter cover crops on soil physical properties and (b) to verify the relationship between punctual methods for the evaluation of water infiltration in the soil and the infiltration of water with natural rainfall on plot scale. For the first study the systems studied were: oat and vetch (AE) consortium, oat and turnip (AN), spontaneous vegetation (VE) and bare soil (SD). Soil samples with undisturbed structure were collected in the layers of 0 - 0,05; 0,05 - 0,1; 0,1 - 0,2 and 0,2 - 0,3 m to measure bulk density (DS), total porosity (Pt), macroporosity (Mac), microporosity (Mic), saturated soil hydraulic conductivity (Ksat) and permeability to air (Ka). Soil aggregation was also evaluated in the layers of 0 - 0.05 and 0.5 - 0.1 m. Soil water infiltration was determined by the concentric double ring method. For the second study, three treatments were used in the first study to determine the rate of stable infiltration of soil water (TIE) by the Cornell infiltrometer, double ring infiltrometer and infiltration in natural rainfall events. The results indicate that after the cultivation of winter cover crops, there are no changes in the physical properties evaluated, but there is evidence of improved water infiltration in the soil and the continuity and pore diameter in the treatments with cover crops. The TIE determined by the Cornell infiltrometer and double ring infiltrometer method is overestimated from 1.8 to 2.2 times that of natural rainfall. / A inclusão de plantas de cobertura em sistemas de produção agrícola tem recebido atenção pela habilidade de melhorar a multifuncionalidade do solo. Com vistas a melhoria da estrutura do solo e de propriedades físico-hídricas do solo, principalmente da infiltração de água no solo, objetivou-se com este trabalho: (a) avaliar o efeito de diferentes espécies de plantas de cobertura de inverno em propriedades físico-hídricas do solo e (b) verificar a relação entre métodos pontuais de avaliação da infiltração de água no solo com a infiltração de água com chuva natural em escala de parcela. Para o primeiro estudo os sistemas estudados foram: consorciação de aveia e ervilhaca (AE), consorciação de aveia e nabo (AN), vegetação espontânea (VE) e solo desnudo (SD). Amostras de solo com estrutura preservada foram coletadas nas camadas de 0 - 0,05; 0,05 - 0,1; 0,1 - 0,2; 0,2 - 0,3 m para avaliações da densidade do solo (Ds), porosidade total (Pt), macroporosidade (Mac), microporosidade (Mic), condutividade hidráulica do solo saturado (Ksat) e permeabilidade ao ar (Ka). Avaliou-se também a agregação do solo nas camadas de 0 - 0,05 e 0,5 - 0,1 m. A infiltração de água no solo foi determinada pelo método de duplo anel concêntrico. Para o segundo estudo foram utilizados três tratamentos do primeiro estudo para determinação da taxa de infiltração estável de água no solo (TIE) pelos métodos do infiltrômetro de Cornell, duplo anel concêntrico e a infiltração em eventos de chuva natural. Os resultados indicam que após um cultivo de plantas de cobertura de inverno ainda não são observadas alterações nas propriedades físicas avaliadas, porém há indícios de melhoria da infiltração de água no solo e na continuidade e diâmetro de poros nos tratamentos com plantas de cobertura. A TIE determinada pelo método de duplo anel concêntrico e infiltrômetro de Cornell é superestimada de 1,8 a 2,2 vezes em relação a determinada com chuva natural.

Made available in DSpace on 2014-06-11T19:33:38Z (GMT). No. of bitstreams: 0 Previous issue date: 2011-06-27Bitstream added on 2014-06-13T20:05:52Z : No. of bitstreams: 1 marcelo_av_dr_jabo.pdf: 1194015 bytes, checksum: 68c9171ad52d863ef75fe8bb9b03c925 (MD5) / Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq) / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES) / Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) / Em sistema de semeadura direta, os resíduos das culturas de entressafra são utilizados para protegerem a superfície do solo dos agentes erosivos e promoverem a ciclagem de nutrientes. O objetivo desse trabalho foi avaliar o efeito de sequências de culturas na quantidade, qualidade, decomposição e liberação de nutrientes dos resíduos vegetais de culturas de entressafra, bem como a cobertura do solo proporcionada pelos resíduos, na fertilidade do solo, nas frações particulada e associada aos minerais de C, nas substâncias húmicas do solo e na produtividade de milho e soja cultivados no verão, em região de clima tropical. O experimento foi conduzido em Jaboticabal, SP (48°15’22’’ W e 21°18’58’’ S), em um Latossolo Vermelho eutrófico. O delineamento experimental foi em faixas, com três repetições. Os tratamentos foram constituídos pela combinação de três sequências de culturas de verão (rotação soja-milho, monocultura de milho e monocultura de soja) com sete culturas de entressafra (milho, sorgo, girassol, crotalária, guandu, nabo forrageiro e milheto). O experimento foi iniciado em 2002 e o presente estudo se refere aos anos agrícolas 2008/2009 e 2009/2010. Avaliaram-se as quantidades de matéria seca e acúmulo de N, P, K, Ca, Mg e S pelas culturas de entressafra, bem como a dinâmica de decomposição e liberação dos nutrientes, por meio da utilização de sacolas de decomposição, com os seguintes períodos de avaliação: 15, 30, 60, 120 e 180 dias. A cobertura do solo foi avaliada após o manejo e ao final de cada ano agrícola. Amostras de solo foram coletadas nas camadas 0-10, 10-20 e 20-30 cm de profundidade em duas ocasiões, antes da semeadura das culturas de entressafra, em março, e de verão, em outubro, nos anos de 2008 e 2009. As amostras de solo foram submetidas às análises químicas para determinação dos teores... / In no-tillage system, the offseason crops residues are expected to maintain the soil covered in order to control soil erosion and to promote the nutrients cycling. The objective of this study was to evaluate the offseason crops dry matter quality and production, soil cover, residues decomposition and nutrient release and their effects on soil fertility, C content of humic substances, particulate and mineral associated organic matter fractions and summer maize and soybean yield. A field experiment has been carried out on a Rhodic Eutrudox at Jaboticabal, SP, Brazil (48°15’22’’ W and 21°18’58’’ S). A randomized split-block design with three replications was used. The treatments were the combination of three summer crops sequences (soybean-corn rotation, monoculture of corn and monoculture of soybean) with seven offseason crops (maize, grain sorghum, sunflower, sunn hemp, pigeon pea, oilseed radish and pearl millet). The cultivations started in 2002 and this study is related to 2008/2009 and 2009/2010 growing seasons. The offseason crops dry matter production and N, P, K, Ca, Mg and S accumulations were evaluated at management moment. The period of time to measure the residue decomposition and the nutrient release was 15, 30, 60, 120 and 180 days, using litter bags. The soil cover was evaluated after the offseason crops management and at the end of each growing season. The soil was sampled at 0-10, 10-20 and 20-30 cm soil depths in two occasions, before the offseason crops sowing, at March, and before the summer crops sowing, at October, in 2008 and 2009. Total organic C, pH, P, K, Ca, Mg and H+Al were determined in each soil samples. The soil samples obtained on October at 0-10 cm were submitted for physical and chemical organic matter fractionation, for particulate, mineral-associated, humic acid, fulvic acid and humin C content determination. The summer monoculture... (Complete abstract click electronic access below)

Made available in DSpace on 2014-06-11T19:33:39Z (GMT). No. of bitstreams: 0 Previous issue date: 2011-01-20Bitstream added on 2014-06-13T21:06:47Z : No. of bitstreams: 1 beraldo_jmg_dr_jabo.pdf: 1719744 bytes, checksum: a27050b0770082469a896d7df06651eb (MD5) / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES) / O sistema de semeadura direta (SSD) proporciona melhores condições físicas do solo favorecendo o armazenamento de água no solo (ARM). A hipótese do trabalho foi que o Latossolo Vermelho argiloso, em sequências de culturas de verão e inverno sob SSD afeta o ARM em decorrência da modificação nos atributos físicos do solo e que o tensiômetro de punção digital (TDig) pode ser usado para medir o potencial mátrico da água no solo. Os objetivos foram avaliar o ARM e os atributos físicos do solo em sequências de culturas de verão e de inverno sob SSD e medir o potencial mátrico da água no solo por meio do tensiômetro de mercúrio e do TDig. O delineamento foi em blocos, com três repetições, no esquema em faixas. Os tratamentos foram constituídos por três sequências de culturas de verão (rotação soja/milho e monocultura de milho e soja) e sete culturas de inverno (milho, girassol, nabo forrageiro, milheto, guandu, sorgo e crotalária). Foram instalados tensiômetros nas camadas de 0,2; 0,4 e 0,6 m. Foi determinada a densidade do solo, a distribuição de poros por tamanho nas camadas de 0-0,1 e 0,1-0,2 m e a infiltração de água na superfície do solo. Os dados foram submetidos à análise de variância e as médias comparadas pelo teste de Tukey. O TDig pode ser usado para avaliar o potencial mátrico da água no solo. O ARM não diferiu entre as sequências de culturas de verão e nas culturas de inverno houve diferença, principalmente após período de menor disponibilidade hídrica. A densidade e a porosidade do solo não foram influenciadas pelas culturas de verão e inverno. O diâmetro de poros entre 0,075 - 0,05 e 0,03 - 0,0375 mm na camada de 0,0-0,1 m diferiu entre as sequências de verão. A distribuição de poros por tamanho não foi influenciada pelas sequências de culturas de inverno. A maior infiltração de água no solo ocorreu na parcela sob monocultura de soja / No tillage system provides soil physical properties improvements, and soil water storage. The hypothesis of this study was that a Red Latosol (Oxisol), in summer and winter crops sequences under no-tillage system, can have its soil water storage influenced by changes in soil physical properties and digital tensiometer can be used to measure soil water matric potential. This study aimed to measure the soil matric potential using both mercury and digital tensiometers and to evaluate the soil water storage and physical properties on summer and winter crops sequences under no-tillage system. A completely randomized block was designed with three replications on a strips plan. The treatments were the combination of three summer crops sequences (soybean/maize rotation, corn and soybean monocultures) and seven winter crops (maize, sunflower, oilseed radish, millet, pigeon pea, sorghum and sunn hemp). Tensiometers were installed at a depth of 0.20; 0.40; 0.60 meters. Bulk density and pores distribution curves were determined from layers 0-0.1 and 0.1-0.2 depth and water infiltration at the soil surface. The data were submitted to variance analysis and means were compared by the Tukey test. The hypothesis was confirmed, therefore digital tensiometer can be used to measure soil water matric potential. The results showed no difference regarding soil water storage in summer crops sequences, especially after a period associated with lower water availability. Soil porosity and bulk density were not influenced by summer and winter crops sequences. The results indicated that the pores with diameter between 0,075 - 0,05 e 0,03 - 0,0375 mm from layer 0-0.1 m differed on summer crops sequences. No difference was observed by pores distribution curves between summer and winter crops sequences. The largest water infiltration occurred under the soybean monocultures plot