Magistrantūros studijų baigiamajame darbe pateikiami dirvožemio organinės anglies, humuso, C/N santykio, mikroorganizmų biomasės anglies, dirvožemio kvėpavimo tyrimų duomenys, įvertinant skirtingus žemės dirbimo būdus skirtingais dirvožemio gylio sluoksniais. Lyginami 2009 ir 2013 metų atliktų tyrimų duomenys. Darbo objektas – giliau karbonatingas giliau glėjiškas rudžemis, kuriame 2009 ir 2013 metais buvo žirnių (Pisum sativum L.) pasėlis, kur tirta skirtingo žemės dirbimo įtaka dirvožemio organinės anglies ir mikroorganizmų biomasės anglies sankaupoms. Darbo metodai: eksperimentai įrengti keturiais pakartojimais. Pradinių laukelių plotas – 126 m2, apskaitinių – 84 m2. Variantai pakartojimų blokuose išdėstyti rendomizuotai. Dirvožemio kvėpavimas ir mikroorganizmų biomasės sankaupos įvertintos 2009 ir 2013 m. birželio mėn. žirnių pasėliuose. Dirvožemio organinės anglies ir mikroorganizmų biomasės sankaupoms vertinti viršutinio ariamojo Ap (0-10 cm) horizonto jungtiniai ėminiai 3 pakartojimais buvo surinkti su 2-4 cm skersmens dirvožemio grąžtu. Eksperimento variantai: tradicinis žemės dirbimas, supaprastintas žemės dirbimas, tiesioginė sėja, ekologinė žemdirbystės sistema, kur taikytas tradicinis žemės dirbimas. Darbo rezultatai. Skirtingi žemės dirbimo būdai ir ekologinės žemdirbystės sistema, taikant tradicinį žemės dirbimo būdą, turėjo įtakos dirvožemio organinės anglies, humuso, C/N santykio, kvėpavimo ir mikroorganizmų biomasės anglies sankaupoms. Didžiausios org. C... [toliau žr. visą tekstą] / The master work presents the results on soil organic carbon, humus, C/N ration, microbial biomass carbon, soil respiration in soil with different soil tillage systems in two soil depths (0-10; 10-20 cm). Results were obtained in 2009 and 2013 and presented. Object of the research – The Endocalcari-Endohypogleyic Cambisol, where in 2009 and 2013 pea crops (Pisum sativum L.) have been growing. Soil tillage impact on soil organic carbon and microbial biomass carbon pools has been investigated. Method of the research – experiments was installed in four replications. Research area – 126 m2, research plot – 84 m2. Variants in blocks were rendomized. Soil respiration and microbial biomass pools were investigated in 2009 and 2013 in June in pea crops. Experiment variants were as followed: conventional tillage, reduced tillage, no tillage and ecological soil management with conventional tillage. Research results. Different soil tillage systems and ecological soil management system with conventional tillage had impact on soil organic carbon, humus, C/N ration, soil respiration and microbial biomass carbon pools. The highest org. C, humus, microbial biomass carbon concentrations and soil respiration intensity have been found in ecological soil management system. The fertilization with siderate crop may effect it mainly. The lower soil tillage intensity influenced the increase in org. C, humus concentration in 0-10 cm soil depth. In other hand, also along with lower tillage intensity... [to full text]

En agriculture de conservation (AC), les résidus de cultures sous forme de paillis à la surface du sol associés à la suppression du travail du sol sont une composante intrinsèque des systèmes de culture. L'objectif principal de ce travail était de comprendre les effets de la nature et de la décomposition de mulch de résidus s sur les services d'approvisionnement et de régulation fournis par les sols dans les agrosystèmes en AC de régions tempérées (France) et tropicales (Madagascar et le Brésil). Des études expérimentales ont été réalisées pour obtenir des paramètres de décomposition pour une large gamme représentative de la qualité des résidus végétaux des agrosystèmes étudiés et pour tester et améliorer un modèle de décomposition des mulchs. Ensuite nous avons utilisé le modèle PASTIS_MULCH qui simule les biotransformations C et N et le transport de solutés dans les sols lors de la décomposition des mulchs.Pour la gamme de résidus de tiges testées, la rétention d'eau maximale a varié considérablement et ceci a été expliqué par les caractéristiques physiques du résidu. Avec les données obtenues par une série d'incubations de décomposition de résidus, nous avons proposé un ensemble de paramètres biologiques unique pour le module de décomposition CANTIS, simulant une large gamme de qualité des résidus de culture. L'étude expérimentale dans les colonnes de sol a montré que le mulch de maïs + dolique se décompose plus rapidement que mulch de blé + luzerne. Un régime de pluies fines et fréquentes augmente la décomposition du mulch par rapport à des pluies plus rares et plus fortes et cela est dû au maintien de l'humidité du mulch.Les simulations de scénarios avec PASTIS_MULCH ont montré que la pluie et les conditions d'évaporation classent les résidus de culture vis-à-vis de la décomposition lorsque ceux-ci sont placés en mulch à la surface des sols, tandis que les caractéristiques chimiques des résidus classent ceux-ci vis-à-vis de la décomposition lorsqu'ils sont incorporés. Aucune des situations étudiées pourrait être définie au vu des résultats de simulation comme étant adaptée à toutes les conditions pédo-climatiques et agricoles. / In conservation agriculture (CA), crop residues mulches are associated to reduction or suppression of soil tillage and are an intrinsic component of CA. The objective of this work was to understand the effects of nature and decomposition of crop residue mulches on the provisioning and regulating services of agrosystems provided by soils under temperate (France) and tropical (Madagascar and Brazil) conditions. Experimental studies were realized to get decomposition parameters for a large range of residue quality representative of the agrosystems studied and to test and improve a MULCH model. Then we used PASTIS_MULCH model which simulates the C and N biotransformations and solutes transport in soils during mulch decomposition.For a range of plant-stem residues tested, the maximal water retention varied greatly and was only explained by the physical features of the residue. With a series of decomposition incubations, we proposed a single set of biological parameters for CANTIS decomposition module, simulating a large range of crop residue quality. Experimental study in soil columns showed that maize+dolichos mulch decomposed faster than wheat+alfalfa mulch. Frequent and light rain enhanced mulch decomposition compared to infrequent and heavy rain and this was due to the mulch remaining wetter with frequent rain.The simulations of scenarios with PASTIS showed that rain and evaporation conditions ranked crop residues decomposition when placed as mulches while the residue chemical characteristics ranked crop residues decomposition when incorporated. None of the situations studied would be defined as suitable in all pedo-climatic and agricultural conditions.

Orientador: Rogério Peres Soratto / Banca: Ciro Antonio Rosolem / Banca:Antonio Luiz Fancelli / Resumo: Com o aumento do cultivo de feijão no sistema plantio direto, torna-se necessário o conhecimento da reposta dessa cultura ao nitrogênio em solo sem preparo convencional por diferentes períodos de tempo, já que a disponibilidade desse nutriente pode ser alterada pelo sistema de manejo do solo. O objetivo foi avaliar o efeito da aplicação antecipada e/ou em cobertura do nitrogênio no feijoeiro cultivado em áreas com sistema plantio direto recém-implantado ou consolidado. O experimento foi conduzido durante o período "da seca", nos anos agrícolas 2007/08 e 2008/09, em um Nitossolo Vermelho, no município de Botucatu-SP. O delineamento experimental utilizado foi o de blocos casualizados em esquema de parcelas subdivididas, com quatro repetições. As parcelas foram representadas por quatro sistemas de manejo (SPDR: sistema plantio direto recém-implantado (a cultura do feijão será a primeira cultura a ser implantada no sistema de plantio direto); SPDC: sistema plantio direto consolidado (23 anos após a implantação); SPDR+N: sistema plantio direto recém-implantado com aplicação de 60 kg ha-1 de nitrogênio antecipado; SPDC+N: sistema plantio direto consolidado com aplicação de 60 kg ha-1 de nitrogênio antecipado). As subparcelas foram constituídas por quatro doses de nitrogênio em cobertura (0, 30, 60 e 120 kg ha-1). A adubação de cobertura foi efetuada no estádio fenológico V4, nos dois anos agrícolas. O tempo que a área permaneceu sob sistema plantio direto não influenciou a resposta do feijoeiro à adubação nitrogenada. A antecipação do N contribuiu para a manutenção da população de plantas almejada. A aplicação de N antecipado e em cobertura aumentou o número de vagens por planta, a massa dos grãos, o teor de proteína nos grãos e a produtividade de grãos do feijoeiro.Houve maior eficiência de uso do N quando este foi antecipado, do que quando... (Resumo completo, clicar acesso eletrônico abaixo) / Abstract: With the increase in common bean growth under no-tillage, it is necessary to know the response of this crop to nitrogen in soil without conventional tillage for different periods of time, since the availability of this nutrient can changed by the system of soil management. The aim of this study was to evaluate the effect of nitrogen early and/or sidedressed application for common bean crop, grown in newly implemented and established no-tillage system. The experiment was conducted during the dry period, in the 2007/08 and 2008/09 cropping seasons, on a Red Nitosol (Alfisol) located in Botucatu County, São Paulo State, Brazil. A randomized complete block design, in split-plot scheme, and four replications was used. The plots were composed by four management systems (NNT: newly implemented no-tillage system (common bean crop was the first to be cropped in no-tillage system); ENT: established no-tillage system (23 years without soil tillage); NNT+N: newly implemented notillage system with application of 60 kg ha-1 of nitrogen early at common bean sowing, and ENT+N established no-tillage system with application of 60 kg ha-1 of nitrogen early at common bean sowing). The subplots were composed by four sidedressed nitrogen doses (0, 30, 60, and 120 kg ha-1). The nitrogen sidedressing fertilization was performed in the V4 growth stage, in both cropping seasons. The time that area remained under no-tillage system did not influence the response of common bean plants to nitrogen fertilization. Nitrogen early application at common bean sowing contributed to maintaining the desired plant population. Nitrogen early and sidedressing application increased pods number per plant, grains weight,protein concentration in grains and grain yield of common bean. Nitrogen early application was more efficient than sidedressing application / Mestre

Made available in DSpace on 2014-06-11T19:31:36Z (GMT). No. of bitstreams: 0 Previous issue date: 2002-05-14Bitstream added on 2014-06-13T20:02:25Z : No. of bitstreams: 1 grego_cr_dr_botfca.pdf: 900852 bytes, checksum: fb58b3a71dd18b88537b458253727507 (MD5) / A adoção dos sistemas de manejo conservacionistas requer adaptações do solo e das culturas utilizadas, em função das variações edafoclimáticas encontradas nas regiões agrícolas, para que o processo se torne produtivo e viável. Diante deste contexto, foi desenvolvido o presente trabalho, no Município de Botucatu, SP, em Terra Roxa Estruturada ((NITOSSOLOS VERMELHOS - NV, EMBRAPA, 1999), durante o período de agosto de 1999 a maio de 2001. O objetivo foi avaliar a cultura da soja nos sistemas de manejo do solo: preparo convencional (uma gradagem pesada seguida de duas gradagens niveladoras); escarificação seguida de gradagem niveladora; escarificação; sistema de plantio direto com três épocas de dessecação da cobertura vegetal (30 e 10 dias antes da semeadura da soja e após a semeadura) empregando dois tipos de mecanismos sulcadores, disco duplo e haste sulcadora), para abertura do sulco de deposição de fertilizantes na semeadora-adubadora de plantio direto, em todos os sistemas de manejo do solo. Avaliou-se a densidade do solo, resistência do solo à penetração, cobertura vegetal, infestação de planta daninha, sulco de semeadura, emergência, nutrição, sistema radicular e produtividade da soja. O delineamento experimental foi em blocos ao acaso com parcelas subdivididas em faixas, sendo seis tratamentos primários constituídos pelos preparos e dois secundários constituídos por mecanismos sulcadores, com quatro repetições. A deficiência hídrica, no inverno e na primavera, impediu a formação de cobertura vegetal por triticale (X triticossecale Wittmack) e milheto (Penisetum americanum (L.) Leeke), por isso, a vegetação espontânea foi utilizada como alternativa de cobertura vegetal.... / The adoption of the conservation management systems requires the soil adaptation and the crop utilized as a function of the edafoclimatic variations found in agricultural areas, so that the process becomes productive and viable. In the light of this, the present work was developed in Botucatu of State São Paulo, Brazil, from August 1999 to May 2001 in Ultisol. The aim was to appraise the soybean crop in the soil management systems: conventional tillage (one harrow plowing followed by two harrow leveling); chiseling followed by harrow leveling; chiseling, no-tillage system with three seasons of weed blanket dessication (30 and 10 days before soybean seeding and after the seeding). Two kinds of furrow openers mechanisms, double disc and chisel opener were combined for the furrow for fertilizer application in no-tillage seeders / planters, in all soil management system. The soil physical properties density and strength, crop blanket, weeds, seeding furrow, emergence, nutrition, root systems and soybean grain yield were evaluated. The experiment was made randomized block with subdivided plots in strips, with six primary treatments, two secondary and with four repetitions. During the winter and spring, the hydro deficiency did not allow the covering formation for por triticale (X triticossecale Wittmack) and milhet (Penisetum americanum (L.) Leeke), so using the spontaneous vegetation was the choice...(Complete abstract, click electronicaccess below).

Submitted by Gabriela Lopes (gmachadolopesufpel@gmail.com) on 2017-03-07T17:22:05Z No. of bitstreams: 2 license_rdf: 0 bytes, checksum: d41d8cd98f00b204e9800998ecf8427e (MD5) Dissertação .pdf: 869153 bytes, checksum: c77e409bcab66ac0b63cb639fe500496 (MD5) / Approved for entry into archive by Aline Batista (alinehb.ufpel@gmail.com) on 2017-03-09T20:47:06Z (GMT) No. of bitstreams: 2 Dissertação .pdf: 869153 bytes, checksum: c77e409bcab66ac0b63cb639fe500496 (MD5) license_rdf: 0 bytes, checksum: d41d8cd98f00b204e9800998ecf8427e (MD5) / Made available in DSpace on 2017-03-09T20:47:06Z (GMT). No. of bitstreams: 2 Dissertação .pdf: 869153 bytes, checksum: c77e409bcab66ac0b63cb639fe500496 (MD5) license_rdf: 0 bytes, checksum: d41d8cd98f00b204e9800998ecf8427e (MD5) Previous issue date: 2014-02-21 / Os sistemas de preparo do solo e manejo da cobertura vegetal em área de produção de arroz irrigado por alagamento apresentam peculiaridades e potenciais distintos de emissão de metano e óxido nitroso do solo. Considerando uma área de arroz irrigado, o objetivo deste estudo foi avaliar a influência de sistemas de preparo do solo na emissão dos gases de efeito estufa metano e óxido nitroso, a fim de estabelecer sistemas com potenciais de mitigar a emissão desses gases. O experimento de campo foi realizado na Estação Experimental Terras Baixas da Embrapa Clima Temperado, Capão do Leão, RS. Foram avaliados três sistemas de preparo do solo: preparo convencional - ausência de manejo da palha e do solo no período de outono-inverno e preparo do solo na primavera, antes da semeadura do arroz; rolo-faca - manejo da palha com rolo-faca imediatamente após a colheita do arroz e semeadura direta na primavera; e preparo antecipado - preparo do solo no outono, dessecação e revolvimento do solo, por meio de gradagem superficial. As emissões de CH4 e N2O foram avaliadas nos períodos de entressafra e safra. As coletas dos gases de efeito estufa (GEE) foram realizadas, semanalmente, pelo método da câmara estática fechada. Com base nas emissões de CH4 e de N2O foi calculado o potencial de aquecimento global parcial (PAGp = CO2 equivalente). O sistema de preparo convencional foi mais eficiente que os demais em mitigar as emissões de GEE ao longo do ano. O sistema de preparo antecipado apresentou as maiores emissões de CH4, as quais se concentraram na época de cultivo do arroz. O período de safra representou a maior parte do PAGp anual (safra+entressafra). Devido à alta emissão de CH4, o sistema de preparo antecipado foi responsável pelo maior PAGp, seguido do manejo com rolo-faca, em função da elevada emissão de N2O e do sistema convencional, com menor PAGp anual. Os sistemas rolo-faca e convencional reduziram o PAGp em função das menores emissões de CH4 ao longo do ano. Embora os sistemas de manejo de solo e da cobertura vegetal apresentem potenciais distintos de emissão, vários fatores associados ao ambiente e às práticas de manejo regulam a produção e emissão de CH4 e N2O, estes fatores devem ser considerados caso a caso, na estimativa do potencial emissor e mitigador desses gases de efeito estufa. / The different soil tillage systems and cover crop management in areas of flooded irrigated rice show distinct peculiarities and potential of soil methane and nitrous oxide emissions. Considering an area of irrigated rice, this work aimed to evaluate the influence of soil tillage systems in the emission of greenhouse gases such as methane and nitrous oxide in order to establish systems with potential to mitigate these gases emissions. The field experiment was performed in the Lowlands Experimental Station at Embrapa Temperate Climate, Capão do Leão, RS. Three management systems were evaluated: conventional tillage - no straw management and soil tillage during autumn-winter and soil tillage in the spring, before rice sowing; knife roller - straw management with knife roller immediately after rice harvesting and no-till in the spring; and advance preparation – soil tillage in autumn, desiccation and soil disturbance by shallow disking. Emissions of CH4 and N2O were evaluated in the pre-harvest and harvest periods. The sampling of greenhouse gases (GG) was conducted weekly through the closed static chamber method. The partial global warming potential (PGWp = CO2 equivalent) was calculated based on CH4 and N2O emissions. Conventional tillage was more effective than the other systems to mitigate GG over the year. The advance preparation system showed the highest CH4 emissions, which were concentrated in the period of rice cultivation. The harvest period accounted for the largest portion of the annual PGWp (harvest+pre-harvest). Due to the high emission of CH4, the advance preparation system was responsible for the largest PGWp, followed by knife roller management, because of the high emission of N2O and by the conventional system, with lower annual PGWp. The knife roller and conventional systems reduced the PGWp due to lower CH4 emission throughout the year. Although soil and cover crop management systems show distinct emission potentials, several factors associated with the environment and management practices regulate the production and emission of CH4 and N2O. These factors must be considered case by case to estimate the transmitter and mitigation potential of these greenhouse gases.

Pour beaucoup de cultures, un sol non travaillé est une alternative de plus en plus crédible au travail intensif du sol, en particulier pour des raisons environnementales. Mais l’ananas (ananas comosus) présente un enracinement fragile très sensible à la structure, ce qui motive souvent un travail important du sol avant plantation. L’alternative d’une plantation sans travail du sol ne va donc pas de soi. L’objet de cette thèse est de répondre à la question de la faisabilité d’une culture d’ananas sans travail du sol, en remplaçant ce dernier par une plante de service « décompactante » dont les traits racinaires seraient favorables à la (re)structuration d’un sol compact. Le travail de cette thèse a donc porté sur l’évaluation de plusieurs espèces candidates, puis sur l’étude, au champ, des effets sur le sol de la plus prometteuse (Stylosanthes guianensis ). Enfin, dans le cadre d’un essai au champ comparant un système de culture innovant ananas sans travail du sol, on a étudié l’effet de la plante de service sur le fonctionnement de la culture de l’ananas. Dans un premier essai, c’est le Stylosanthes guianensis qui, comparé à huit autres espèces (Arachis pintoï, Brachiaria decumbens, Cajanus cajan, Crotalaria juncea, Cynodon dactylon, Eleusine coracana, Pueraria phaseoloides, et le maïs), a montré les traits racinaires les plus favorables à la structuration d’un sol compact. Les valeurs supérieures du diamètre racinaire moyen et de la densité de longueur racinaire (DRL) caractérisent les principaux traits impliqués. Dans un deuxième essai, les mesures de conductivité hydraulique, d’indice des vides du sol et d’analyse d’images de blocs de sol imprégné sur la répartition surfacique des différents types de porosité ont montré que la culture du Stylosanthes guianensis avait augmenté l’indice des vides du sol et provoqué l’apparition d’une porosité fissurale de grande taille, contribuant ainsi à l’amélioration de la structure du sol. Enfin, un troisième essai mettant en comparaison (i) un système de culture innovant où la culture d’ananas est implantée sans travail du sol après une culture de S. guianensis restructurante et (ii) un système conventionnel comportant un travail profond du sol (et pas de plante de service) a montré que le rendement en fruit est similaire dans les deux systèmes. Cet essai a permis de vérifier que l’enracinement de l’ananas en condition de sol non travaillé bénéficiait du précédent S. guianensis. / For many crops, direct drilling is a well-tried alternative facing the damaging effects of intensive tillage, mainly for environmental causes. But, pineapple (ananas comosus), presents a fragile rooting system which is very sensitive to soil structure. This leads frequently to intensive soil tillage before planting. Direct drilling is not so evident. The aim of this thesis is to give an answer to the feasibility of a no till system for pineapple cultivation, by using a plant with favorable roots traits for compacted soil (re)structuration. This work consisted in evaluating several candidate species, followed by the study, on the field, of the effects the most promising on soil (Stylosanthes guianensis). Finally, through a field experiment, comparing an innovating no till pineapple cultivation system we studied the use effects of Stylosanthes guianensis on the pineapple crop functioning. In a first experiment, Stylosanthes guianensis compared with eight other species (Arachis pintoï, Brachiaria decumbens, Cajanus cajan, Crotalaria juncea, Cynodon dactylon, Eleusine coracana, Pueraria phaseoloides and corn) showed better roots traits for structuring a compacted soil. Measures of average root diameter and root length density are the main implicated roots traits. In a second experiment, the measures of hydraulic conductivity, of the soil void ratio and the analysis of blocks of resin-impregnated soil on the surface distribution of the different type of porosity, all of this showed that Stylosanthes guianensis had increased the soil void ratio and had caused the creation of large-sized cracked porosity, thus contributing to the improvement of the soil structure. Finally, a third experiment involving a comparison between (i) an innovating cultivation system where pineapple is growing in a no till soil after a structuring crop of S. guianensis and (ii) a conventional system with deep tillage (without structuring crop), showed similar fruit yield. This experiment showed evidence that the rooting of pineapple in no till soil benefited from the previous Stylosanthes.

The soil C stock is a consequence of the balance between the C losses by the CO2 emission (associate to the heterotrofic microorganisms activity) and erosion, and to C inputs, associate to organic compounds input by the vegetal photosynthesis process. In order to evaluate the soil tillage and crop systems regarding to the C inputs by the residues and the C losses by the CO2 evolution and its consequences on the soil C stocks, a long term experiment (19 years) was carried out over a Rhodic Hapludox. This experiment is located in FUNDACEP, Cruz Alta, RS, Brazil. The main treatments were soil tillage systems: conventional tillage (CT) and no-tillage (NT). Subplots were tree commercial crop systems: winter wheat/soybean defined as monocropping system (R0), black oat/soybean/winter wheat/soybean defined as a winter crop rotation system (R1), and black oat/soybean/black oat+common vetch/maize/oil radish/winter wheat/soybean (R2) defined as intensive crop rotation system. The soil in NT system, averaged over crop systems, showed higher SOC and TN stocks and their particulate pools than the soil in CT on the shallow soil layer (0 - 5 cm), while the CT showed higher particulate organic carbon and nitrogen stocks (POC and PN) on the 5 - 10 cm layer. The soil in NT showed 1.6% more SOC than CT, averaged on the rotation systems, estimated by the layer equivalent method. To the mass equivalent method this difference increase to 4.5%. The crop rotation R2 associated to the NT (NT R2) showed higher mineral-associated carbon, SOC, mineral-associated N and TN stocks than the others treatments, on the 0 30 cm layer. The soil organic matter restoration was more influenced by the crop rotations systems, with high biomass input, than the tillage system adopted. This result most likely is due to differences in the biomass inputs. Once the NT, in averaged on crop systems, resulted in only 14% higher C addition than the CT. When associated to the R2 (NT R2) this difference increased to 68% compared to the CT without crop rotation (CT R0). The C-CO2 losses, evaluated by CO2 flux, were similar among treatments (soil tillage and crop systems), it is mostly influenced by the moisture and soil temperature. / O estoque de C no solo é conseqüência do balanço entre a saída de C pela emissão de CO2 (devido à atividade de microrganismos heterotróficos) e erosão e, a entrada de C, principalmente pela adição de compostos orgânicos sintetizados no processo de fotossíntese vegetal. Visando avaliar sistemas de preparo do solo e de culturas quanto a entrada de C orgânico pelos resíduos e saída pela evolução de CO2 e sua conseqüência no estoque de C orgânico no solo, foi desenvolvido essa pesquisa em experimento de longa duração (19 anos) sob Latossolo Vermelho distrófico típico. O experimento está situado na Fundação Centro de Experimentação e Pesquisa Fecotrigo (FUNDACEP), Cruz Alta, RS. Neste são conduzidos os preparos de solo convencional (PC) e plantio direto (PD) e, foram selecionados três sistemas comerciais de culturas: monocultura trigo/soja (R0); rotação de inverno aveia/soja/trigo/soja (R1) e, rotação de inverno e verão aveia/soja/aveia+ervilhaca/milho/nabo/trigo/soja (R2), em cada sistema de preparo do solo. As avaliações foram realizadas nas profundidades de 0-5, 5-10, 10-20 e 20-30 cm. O solo em PD, na média dos sistemas de culturas, apresentou maior teor e estoque de C orgânico e N total e fracionados que o solo em PC na camada superficial do solo (0-5 cm), enquanto que o solo sob PC apresentou, mais C orgânico e N total particulado (COP e NTP) na camada de 5-10 cm. O solo em PD apresentou 1,6% mais COT do que o solo sob PC, na camada de 0-30 cm, na média dos sistemas de culturas, pelo cálculo da camada equivalente. No método de cálculo da massa equivalente esta diferença aumentou para 4,5%. A rotação culturas R2 associada ao PD (PD R2) apresentou mais COAM, COT, NTAM e NT que os demais tratamentos, na camada de 0-30 cm. A recuperação do estoque de matéria orgânica do solo foi mais influenciada pelo sistema de rotação de culturas, que incluíram espécies de alto aporte de resíduos orgânicos, do que pelo sistema de preparo de solo. Este comportamento ocorreu devido às diferenças de aporte de resíduos vegetais. As culturas em PD, em média, forneceram apenas 14% mais C ao solo, do que as sob PC, mas quando associado à rotação de culturas R2 com PD (PD R2) esta diferença aumentou para 68% quando comparado a monocultura em PC (PC R0). A perda de C-CO2, avaliada pela evolução de CO2, foi similar entre os tratamentos (sistemas de preparo do solo e culturas), sendo influenciadas principalmente pela temperatura e umidade do solo.

Klimawandel und Bodendegradation üben Druck auf die Nahrungsmittelproduktion sowie auf die Fähigkeit des Bodens zur Minderung des Klimawandels beizutragen aus. Bodendegradation hat negative Auswirkungen auf die Bodenqualität. Ziel dieser Arbeit ist die Analyse der Effekte von landwirtschaftlich getriebener Bodendegradation, vor allem durch Pflügen und dem Umgang mit Ernterückständen. Es wird ein Überblick über das Thema Bodendegradation gegeben, gefolgt von Erweiterung des globalen Ökosystemmodells Lund-Potsdam-Jena-managed-Land (LPJmL) um eine detaillierte Prozessabbildung von Pflugpraktiken und Effekten von Ernterückständen. Diese ermöglicht die Analyse der Effekten von landwirtschaftlichen Managements auf die Anpassung und Minderung des Klimawandel. Das Modell kann die Effekte von naturerhaltender landwirtschaftlicher Bewirtschaftung (im Englischen bekannt als Conservation Agriculture) auf Kohlenstoffvorräte im Boden und CO2 Emissionen simulieren. Im letzten Teil wird die historische Dynamik der Entwicklung von Bodenkohlenstoff (engl.: Soil Organic Carbon – SOC) und die Effekte von Annahmen zum zukünftigen Management unter unterschiedlichen Klimaszenarien gezeigt. Die Ergebnisse zeigen, dass durch die historische Umwandlung von natürlicher Vegetation zu landwirtschaftlicher Fläche bis zu 215 Pg SOC im Boden verloren gegangen sind. Bis zum Ende des Jahrhunderts könnten weitere 38 Pg SOC zusätzlich verloren gehen, wird die heutige landwirtschaftliche Fläche nicht nachhaltig bewirtschaften. Die Bewirtschaftung mit dem Pflug zeigt einen geringen Einfluss auf die Kohlenstoffvorräte des Bodens, während die Wahl der Behandlung von Ernterückständen erheblich Einfluss hat. Die Rückführung von Ernterückständen hat positive Einflüsse auf Bodenwassergehalt und Ernteproduktivität, mit regionalen Unterschieden. Insgesamt zeigen 46% der heute Landwirtschaftsfläche das Potenzial zur Steigerung des Bodenkohlenstoff, während mindestens 52% Kohlenstoff im Boden verlieren könnten. / Climate change and increasing soil degradation put pressure on the global food production systems and the ability of land for climate change mitigation. Additionally, soil degradation has negative implications on soil quality. This thesis analyzes the effects of agricultural-driven global soil degradation, in particular tillage and residue management. At first, a review the state of knowledge on global soil degradation is provided. Soil organic carbon (SOC) decline is one of the major forms of soil degradation on cropland and a useful indicator of the status of soil degradation. Secondly, to study the effects of different pathways of agricultural management on biophysical and biogeochemical flows, the global ecosystem model Lund-Potsdam-Jena managed Land (LPJmL) is extended by a detailed representation of tillage practices and residue management. This improvement of LPJmL allows for the analysis of management-related effects on agricultural mitigation of climate change adaption and the reduction of environmental impacts. The model can simulate the effects of conservation practices on SOC stocks and CO2 emissions. And third, SOC development and the effects of different management assumptions under climate change is analyzed. This shows that approximately 215 Pg SOC was lost due to the historical conversion of natural land to cropland and up to 38 Pg SOC could be additionally lost on already existing cropland until the end of the century if cropland is not managed sustainably. The type of tillage system has small effects on the SOC stocks, while the choice of crop residue treatment is shown to be the main driver governing SOC development. Returning residues to the soil slows the decline of SOC, and positively affects soil moisture and crop productivity, with regional differences. In total, up to 46% of todays’ cropland shows the potential for SOC increase, while at least 52% of cropland today will undergo further SOC loss as a form of soil degradation.

Made available in DSpace on 2017-07-25T19:29:41Z (GMT). No. of bitstreams: 1 josiane.pdf: 937524 bytes, checksum: fac9597a15355333fedce082a07f433d (MD5) Previous issue date: 2006-05-17 / The objective of this study was to quantify the changes of the total carbon (C) and total nitrogen (N) stock, and the variation of the C pool’s in monthly soil samples, and the C balance and C sequestration rates provoked by the soil tillage systems. The soil samples were accomplished in a long term experiment implanted in 1988, in the experimental station of Fundação ABC located in Ponta Grossa city, Center-South area of the Paraná State. The soil tillage systems were comprised: a) Conventional Tillage (CT); b) Minimum Tillage (MT); c) No-tillage with chisel plow (NTCP) each three years; and d) No-tillage – Continuous (NTC). Soil samples for each treatments were obtained by digging 3 profiles of 20-cm x 50-cm (surface area) x 50-cm deep for each replicate, and collected from three depths (0,0- to 2.5- cm, 2.5- to 5-cm, 5- to 10-cm). In the samples collected in October of 2003, May of 2004 and November of 2004, the total organic carbon (TOC) and the total nitrogen in all of the depths was measured. The particle size fractionation was accomplished, separating the soil in fractions in the size of 2000 - 210 Wm, 210 - 53 Wm and <53 Wm. In all these fractions TOC was determined. The treatments had significant effects on TOC and TN contents and pools. The total C and N stock in NTC was superior to the other systems demonstrating larger maintenance of C in the soil. The larger concentration of C was observed in the 210 to 53 Wm particle size fraction in the NTC. In the 2000 - 210 Wm fraction of the 0,0-2,5 cm layer were observed larger changes in the C stock due to the management systems in the samples at all long year. The greatest change was accomplished to CT. In NTP, the stock of C was larger in all soil samples, indicating that the maintenance of the cultural residues in the associated surface protection of the aggregates allows larger accumulation of C. Although the C stock in the particle size fraction <53 Wm not to present significant differences among the management systems, and was observed the C migration of the coarse fractions (210-53 and 2000-210 Wm) to the recalcitrant particle size fraction, indicating a continuous C flow. The C balance model adjusted for the local conditions revealed that the oxidation rate acted by K2 is inferior to the simulations accomplished by other authors, demonstrating the importance of the local conditions. With this model, the minimum amount of crop residues to maintain NTC system in steady-state was 8,05 Mg ha-1 year-1 while in the PC treatment it won't be possible to reach the balance with the amount of crop residues placed in this long term experiment, being a deficient system. / RESUMO Este estudo teve por objetivo quantificar as alterações provocadas pela adoção de sistemas de manejo do solo sobre o estoque total de carbono (C) e nitrogênio (N), a variação do estoque do C nas épocas de coleta, o balanço de C e as taxas de seqüestro de C. As coletas do solo foram realizadas em um experimento de longa duração, implantado em 1988, na estação experimental da Fundação ABC em Ponta Grossa, Meso Região Centro-Oriental do Estado do Paraná. Os sistemas de manejo do solo foram avaliados: a) Preparo convencional (PC), Preparo mínimo (PM), plantio direto escarificado (PDE) e plantio direto permanente (PDP). As amostras foram coletadas em 12 épocas com intervalos mensais e nas profundidades de 0,0-2,5; 2,5-5,0 e 5,0-10 cm de profundidade. As amostras deformadas foram coletadas em mini-trincheiras nas camadas de 0,0-2,5 e 2,5-5,0 cm e na camada de 5,0- 10,0 cm com o auxílio do trado. Nas amostras coletadas em outubro de 2003, maio de 2004 e novembro de 2004 foi determinado o carbono orgânico total (COT) e o nitrogênio total (NT) em todas as profundidades amostradas. Nas amostras coletadas mensalmente foi realizado o fracionamento granulométrico da matéria orgânica, separando o solo em frações no tamanho 2000 – 210 Wm, 210 – 53 Wm e < 53 Wm. Em todas estas frações foi determinado o COT. O estoque total de C e N no PDP foi superior aos demais sistemas de manejo demonstrando maior manutenção do C no solo. O estoque de C nas frações granulométricas apresentaram diferenças significativas entre as camadas amostradas, observando-se maior concentração de C na fração 210 a 53 Wm do PDP. Na fração 2000 – 210 Wm da camada de 0,0-2,5 cm observaram-se maior alteração no estoque de C devido aos sistemas de manejo durante as épocas de coleta, sendo a maior amplitude de variação atribuída ao PC. No PDP, o estoque de C foi maior em todas as épocas de coleta indicando que a manutenção dos resíduos culturais na superfície associada à proteção dos agregados permite maior acúmulo de C. Embora o estoque de C na fração < 53 Wm não apresentar diferenças significativas entre os sistemas de manejo, observou-se uma migração do C das frações mais grosseiras (210-53 e 2000-210 Wm) para esta fração mais recalcitrante, indicando um fluxo contínuo de C. O modelo de balanço de C proposto por Henin e Dupuis (1945) e ajustado para as condições locais revelou que a taxa de oxidação representada pelo K2 é inferior às simulações realizadas por outros autores, demonstrando a importância das condições locais. Com este modelo, a quantidade mínima de resíduos culturais para manter sistema PDP em equilíbrio foi de 8,05 Mg ha-1 ano-1 enquanto no PC não será possível atingir o equilíbrio com a quantidade de resíduos culturais aportada, sendo um sistema deficitário.

Made available in DSpace on 2017-07-25T19:30:48Z (GMT). No. of bitstreams: 1 Jessica Alves dos Santos.pdf: 679249 bytes, checksum: 3ae55a8cf411c25ba8cb319cec75453b (MD5) Previous issue date: 2015-02-20 / Conselho Nacional de Desenvolvimento Científico e Tecnológico / The liming is essential for building soil fertility, enabling exploitation more sustainable of production systems. However, the efficiency and the residual effect of lime used are dependent on the degree of soil disturbance, which has been distinguished in conservation production systems. The objectives of this work are (i) quantify the yields of dry matter (DM) and content crude protein (CP) in maize silage during the years 2008-2014; and (ii) evaluate the changes in soil fertility attributes: active acidity (pH), potential acidity (H+Al), exchangeable acidity (Al3+) and base saturation (V) 24 and 60 months after of liming, in different methods tillage and uses of annual ryegrass during the autumn-winter. The experiment was conducted in Castro (PR) in an Oxisol dystrophic clayey. The design experimental was a randomized complete block design with split plots and four replications. In the plots were studied four methods of soil tillage: conventional tillage (CT), minimum tillage (MT), no-tillage (NT) and chiseled no-tillage (CNT). In the subplots were studied three purposes of use of annual ryegrass: cover crop (CC), silage (S) and grazing of the dairy heifers in integrated crop-livestock (ICL). In medium-term, the tillage methods (CT, MT, NT, and CNT) do not influence the yield of DM and CP content of maize silage. The uses annual ryegrass for S and ICL not influence yield of DM and provide high CP in corn silage. Using the preceding crop just as CC provides least amount of benefits systems to annual ryegrass production and maize silage. Lower acidity and higher V were observed in layer the 0-5 cm in NT. Compared to the NT, the CNT not improve the acidity and V. The annual ryegrass for the S and ICL provided, over time, decrease in the acidity of the soil in layers below 10 cm depth. The NT combined with ICL provides improvement in soil acidity conditions after 60 months after liming. / A correção da acidez é fundamental para a construção da fertilidade do solo, possibilitando a exploração mais sustentável dos sistemas de produção. Todavia, a eficiência e o efeito residual do corretivo utilizado são dependentes do grau de perturbação do solo, que tem sido distinto nos sistemas de produção. Os objetivos deste trabalho são (i) quantificar os rendimentos de matéria seca (MS) e teor de proteína bruta (PB) no milho silagem durante os anos 2008-2014; e (ii) avaliar as alterações nos atributos de fertilidade do solo: acidez ativa (pH), potencial (H+Al) e trocável (Al3+) e saturação por bases (V) aos 24 e 60 meses após a calagem, em diferentes métodos de preparo do solo e usos do azevém anual durante o outonoinverno. O experimento foi instalado no município de Castro (PR), em um Latossolo Bruno distrófico de textura argilosa. O delineamento experimental utilizado foi o de blocos completos casualizados, com parcelas subdivididas e quatro repetições. Nas parcelas (10 x 30 m) foram empregados quatro métodos de preparo do solo: cultivo convencional (CC), cultivo mínimo (CM), plantio direto (PD) e PD com subsolagem bianual (PDS). Nas subparcelas (10 x 10 m) foram estudadas três propósitos de uso do azevém anual: cobertura do solo (CS), silagem pré-secada (SPS) e pastejo animal em sistema integrado de produção agropecuária (SIPA). Em médio prazo, os métodos de preparo do solo (CC, CM, PD e PDS) não influenciam o rendimento de MS e teor de PB de milho silagem. Os usos de azevém anual para SPS e em SIPA não influenciam o rendimento de MS e proporcionam incremento nos teores de PB no milho silagem. O uso da cultura antecessora apenas como CS proporciona menor quantidade de benefícios aos sistemas de produção de azevém anual e milho silagem. No decorrer do período, menor acidez e maior V foram observadas na camada de 0-5 cm no PD. Quando comparado ao PD, o PDS não proporcionou melhoria nas condições de acidez e V. O azevém anual destinado à SPS e SIPA proporcionou, ao longo do tempo, diminuição da acidez do solo nas camadas abaixo de 10 cm de profundidade. O PD aliado ao SIPA proporciona melhoria nas condições de acidez do solo após 60 meses da aplicação do calcário.