Made available in DSpace on 2017-07-25T19:30:47Z (GMT). No. of bitstreams: 1 Adriano Haliski.pdf: 1087998 bytes, checksum: 06568ec8622f2204e3d6d86c65fa29a8 (MD5) Previous issue date: 2015-02-19 / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior / Nitrogen fertilization can increase the efficiency of surface liming on soil acidity correction and benefit crop production in long term no-till systems. Because the soil organic matter content under no-till is high, especially in the soil surface layers, the aluminum (Al) toxicity may be low, even in high acidity conditions. This study was carried out with the purpose of evaluate the soil chemical attributes, grain yield, and critical levels for the development of soybean after surface application of lime and ammoniacal nitrogen (N-NH4NO3) in crops of autumn-winter predecessors. The experiment was conducted in Ponta Grossa, Parana State, Brazil, on a loamy, kaolinitic, thermic Typic Hapludox (Oxisol) under long term continuous no-till (26 years). The experimental design used was a randomized block, in a split plot arrangement, with three replications. In the plots, were applied, in May 2004, four rates of lime on the soil surface (0, 4, 8, and 12 t ha-1) and, in the subplots, were applied annually, since 2004, four rates of N-NH4NO3 (0, 60, 120 and 180 kg ha-1) in top dressing in the black oat or wheat crops. In crop rotation was used corn, soybeans or beans in the spring-summer season and black oat or wheat in the autumn-winter season. Soybean was sown in November 2007 (cv. CD 214 RR), 2009 (cv. CD 206 RR), 2010 (cv. BMX Apolo RR), 2012 (cv. NA 5909 RG), and 2013 (cv. BMX Ativa RR). Soil samples were collected annually before soybean sowing at the 0–0.05, 0.05–0.10, and 0.10–0.20 m depths. Surface liming increased pH and the contents of exchangeable Ca2+ and Mg2+, and reduced the content of exchangeable Al3+ to a depth of 0.20 m. Nitrogen fertilization reduced pH and the contents of exchangeable Ca2+ and Mg2+, especially to a depth of 0.10 m, and increased the content of exchangeable Al3+ to a depth of 0.20 m. Surface application of lime increased the soybean grain yields for all N-NH4NO3 rates used in black oat or wheat crops. In unlimed plots, acidification caused by nitrogen fertilization severely limited the soybean grain yield. The critical levels of pH in CaCl2, base saturation, exchangeable Al3+, and Al3+ saturation in the 0–0.20 m layer for soybean production were 4.9, 33%, 8.0 mmolc dm-3, and 30%, respectively. Surface application of lime proved to be a key practice to ensure high soybean yields when high ammoniacal fertilizer rates are applied frequently in no-till systems. / A adubação nitrogenada pode aumentar a eficiência da calagem superficial na correção da acidez do solo e beneficiar a produção das culturas em longo prazo no sistema plantio direto. Como no sistema plantio direto os teores de matéria orgânica são elevados, especialmente nas camadas superficiais do solo, a toxicidade de alumínio (Al) pode ser baixa, mesmo em condições de alta acidez. Este trabalho foi realizado com o objetivo de avaliar as alterações químicas do solo, a produtividade, e os níveis críticos para o desenvolvimento da cultura da soja após aplicação superficial de calcário e de nitrogênio amoniacal (N–NH4NO3) nas culturas antecessoras de outono–inverno. O experimento foi realizado em Ponta Grossa (PR), em um Latossolo Vermelho distrófico textura média manejado há 26 anos sob plantio direto no momento da instalação. O delineamento experimental foi o de blocos ao acaso, em parcelas subdivididas, com três repetições. Nas parcelas, foram aplicadas, em maio de 2004, quatro doses de calcário dolomítico na superfície (0, 4, 8 e 12 t ha-1) e, nas subparcelas, foram aplicadas, anualmente, desde 2004, quatro doses de N–NH4NO3 (0, 60, 120 e 180 kg ha-1) em cobertura nas culturas de aveia preta ou trigo. Na rotação de culturas foram utilizados milho, soja ou feijão na estação de primavera–verão e aveia preta ou trigo na estação de outono–inverno. A soja foi cultivada em novembro de 2007 (cv. CD 214 RR), 2009 (cv. CD 206 RR), 2010 (cv. BMX Apolo RR), 2012 (cv. NA 5909 RG) e 2013 (cv. BMX Ativa RR). Amostras de solo foram coletadas anualmente, antes da semeadura de soja, nas camadas de 0–0,05, 0,05–0,10 e 0,10– 0,20 m. A aplicação superficial de calcário elevou o pH e os teores de Ca2+ e Mg2+ trocáveis, e reduziu o teor de Al3+ trocável até a profundidade de 0,20 m. A adubação nitrogenada diminuiu o pH e os teores de Ca2+ e Mg2+ trocáveis, principalmente até a profundidade de 0,10 m, e elevou o teor de Al3+ trocável até a profundidade de 0,20 m. A aplicação superficial de calcário aumentou a produtividade de grãos de soja para todas as doses de N–NH4NO3 empregadas nas culturas de aveia preta ou trigo. Nas parcelas sem calagem, a acidificação provocada pela adubação nitrogenada limitou severamente a produtividade de grãos de soja. Os níveis críticos de pH em CaCl2, saturação por bases, Al3+ trocável e saturação por Al 3+, na camada de 0–0,20 m, para a produção de soja foram 4,9, 33%, 8,0 mmolc dm-3 e 30%, respectivamente. A calagem na superfície mostrou ser uma prática fundamental para garantir altos tetos de produtividade de soja quando altas doses de nitrogênio amoniacal são aplicadas com frequência no sistema plantio direto.

Ce travail a pour objectif de tester des solutions viables et durables pour la phytoremédiation de sols contaminés en éléments traces. Il inclut à la fois des données sur l'évaluation initiale et résiduelle des risques (biomonitoring) et sur des solutions de phytomanagement à long terme utilisant des plantes et microorganismes associés, en particulier la phytoextraction aidée couplant l’épuisement du pool labile de contaminants du sol, la production de matière première végétale et la restauration de services écosystémiques. La phytotoxicité du Cu, le rôle améliorant des amendements organiques et minéraux et la tolérance des plantes ont été examinés utilisant des essais biologiques ainsi qu’une technique de dilution du sol. L'utilité d’une lignée de mutant de tournesol (Helianthus annuus) et d’une lignée parental de tabac (Nicotiana tabacum) pour le biomonitoring de sols contaminés en Cu a été investiguée. Les paramètres biochimiques qui sont en relation avec le statut antioxidant des plantes et leurs réponses moléculaires à l’excès de Cu ont en général montré une plus grande sensibilité que les traits morphologiques. Le tabac est plus tolérant au Cu que le tournesol. Des bactéries endophytes issues de différentes sources, notamment des graines d’une population métallicole d’une graminée (Agrostis capillaris) peuvent stimuler la croissance du tournesol et du tabac aux expositions en Cu modérément en excès. Pour ces plantes annuelles, accumulatrices secondaires du Cu et à phénotype d’exclusion, l'augmentation de la capacité de phytoextraction de Cu par les parties aériennes s’effectue principalement par l’accroissement de la biomasse aérienne, plutôt que par celui de sa concentration en Cu. Par conséquent, une attention a été prêtée aux pratiques agricoles dans les essais en parcelles sur site. Plusieurs options d’amélioration ont été examinées in situ: l'application d’amendements du sol, l'utilisation de lignées de mutants et de variants somaclonaux, la rotation de cultures et des cultivars, la bioaugmentation, la fertilisation, l’irrigation, etc. Deux lignées de mutants et des cultivars commerciaux de tournesol ainsi qu’une lignée parentale de tabac ont montré un fort potentiel pour la phytoextraction du Cu, accompagné d’une production significative de graines et/ou autre biomasse valorisable. Les solutions de restauration écologique basées sur la phytoextraction, utilisant des plantes annuelles accumulatrices secondaires de Cu permettraient (1) la décontamination progressive des sols contaminés en Cu au cours des rotations culturales, (2) un retour financier lié à la valorisation de la biomasse végétale, et (3) la restauration de services écosystémiques. / This work aimed at assessing sustainable phytoremediation options for trace element-contaminated soils. It includes both the assessment of initial and residual risks (biomonitoring) and long-term sustainable decontamination options using plants and associated microbes, especially aided phytoextraction with the secondary purposes of producing plant-based feedstock and restoring ecosystem services. Copper phytotoxicity, the improving role of soil conditioners, and plant tolerance were tested using a bioassay as well as a fading technique. The usefulness of a mutant line of sunflower (Helianthus annuus) and a motherline of tobacco (Nicotiana tabacum) for the biomonitoring of Cu-contaminated soils was investigated. Biochemical parameters in relation to antioxidant status of plants and molecular responses to Cu excess generally showed a greater sensitivity than morphologic ones. Tobacco has a higher Cu tolerance than sunflower. Endophytic bacteria from various sources, notably from the seeds of metallicolous populations of grasses (Agrostis capillaris) can promote the growth of sunflower and tobacco exposed to Cu excess. For annual Cu-secondary accumulator plants with an excluder phenotype, increase in shoot Cu removal occurred primarily through increase in shoot biomass, rather than in shoot Cu concentration. Therefore, attention in field trials was paid to agricultural practices. Various improving options were tested in situ: application of soil amendments, the use of mutant lines and somaclonal variation, cultivars and crop rotation, bioaugmentation, fertilization, irrigation, etc. Two mutant lines and some commercial cultivars of sunflower as well as the motherline of tobacco showed a high potential for Cu phytoextraction as well as for plant-based feedstock. Ecological restoration options for Cu-contaminated soils based on phytoextraction using annual Cu-secondary accumulator plants with a high shoot biomass would (1) result in the progressive decontamination of Cu-contaminated soils during crop rotations, (2) provide a financial return through biomass valorization, and (3) promote ecosystem services.

La tsavorite, grossulaire vert à V-Cr-Mn, est contenue dans des gneiss et roches calco-silicatées graphiteux, souvent associés à des marbres dolomitiques, et appartenant à la ceinture métamorphique néoprotérozoïque mozambicaine. La tsavorite se trouve soit dans des nodules ou des veines de quartz (gisements primaires), soit dans des placers (gisements secondaires). L'étude minéralogique des tsavorites propose un nouveau protocole de certification de leur origine géographique, à partir du rapport V/Cr, de la teneur en Mn et du [delta]18 O. L'étude des gisements de Lemshuku et Namalulu en Tanzanie montre que le métamorphisme des protolithes sédimentaires riches en matière organique et évaporites s'est effectué à P = 7,0 ± 0,4 kbar et T = 677 ± 14°C, à 634 ± 22 Ma (datation U-Th-Pb sur monazite). Le bâti métamorphique s'est refroidi vers 500 Ma (datation 40Ar-39Ar sur muscovite). Deux stades de métasomatose sont reliés à la formation de la tsavorite : (i) une métasomatose de diffusion formant les nodules à P = 5,0-7,4 kbar et T = 580-691°C; (ii) une métasomatose calcique d'infiltration contemporaine de la formation des veines de quartz à P = 3,6-4,9 kbar et T = 505-587°C. Ces dernières sont datées in situ par la méthode Sm-Nd à 606 ± 36 Ma. Les évaporites continentales, déposées dans une sabkha de côte marine avec des sédiments silico-calcaires, sont transformées en tsavorite dans le cas des nodules, alors que les sels fondus sont associés à la formation des veines de quartz. Les minéralisations sont contrôlées par la lithostratigraphie et la tectonique / Tsavorite, a (V, Cr, Mn)-bearing green grossular, is hosted by graphitic gneisses or calc-silicates, often asssociated with dolomitic marbles, and belonging to the Metamorphic Neoproterozoic Mozambique Belt. Tsavorite is found either as nodules or in quartz veins (primary deposits), or in placers (secondary deposits). The mineralogical study of tsavorites suggests a new protocol to certificate their geographical origin, based on the V/Cr ratio, Mn content and delta18O. The study of the Lemshuku and Namalulu deposits in Tanzania has shown that the metamorphism of organic matter-rich and evaporites-rich sedimentary protoliths occurred at P = 7.0 ± 0.4 kbar and T = 677 ± 14°C, at 634 ± 22 Ma (U-Th-Pb dating on monazite). The metamorphic series cooled down at around 500 Ma (40Ar-39Ar dating on muscovite). Two metasomatic stages are linked to the formation of tsavorite : (i) diffusion metasomatism forming nodules at P = 5.0-7.4 kbar and T = 580-691°C; (ii) calcitic infiltration metasomatism forming quartz veins at P = 3.6-4.9 kbar and T = 505-587°C. These last have been dated in situ with Sm-Nd dating at 606 ± 36 Ma. Continental evaporites, deposited in a coastal marine sabkha with (Si, Ca)-bearing sediments, transformed into tsavorite in the case of the nodules, while the molten salts are associated with the formation of the quartz veins. The mineralisations are controlled by lithostratigraphy and structure