Étude des récepteurs aux estrogènes dans les ostéoblastes de patients atteints de Scoliose Idiopathique de l'Adolescent

Plusieurs éléments de la pathogenèse de la scoliose idiopathique de l’adolescent indiquent que les estrogènes pourraient intervenir dans le développement et la progression de cette maladie. Ce projet avait donc pour but d’explorer l’expression et la fonctionnalité des récepteurs aux estrogènes ERα et ERβ ainsi que leurs isoformes dans les ostéoblastes de patients scoliotiques et sains. L’induction des gènes de facteurs influençant la minéralisation et la différenciation des ostéoblastes par les estrogènes a également été étudié. Par immunofluorescence, nous avons remarqué une augmentation de la présence protéique de ERβ dans les ostéoblastes de patients SIA comparé aux sujets contrôles. Les récepteurs aux estrogènes provenant des ostéoblastes des patients sont fonctionnels tout comme ceux des contrôles et aucune différence dans l'interaction ADN-protéine n’a été observée. Il y a également une augmentation de l’expression génique de l’ostéopontine, l’ostéocalcine, le collagène de type I, la phosphatase alkaline et BMP2 dans les ostéoblastes des patients SIA. Un début de minéralisation in vitro a été observé dans les ostéoblastes de patients SIA et contrôles. ERα et ERβ sont présents et fonctionnels dans les ostéoblastes des patients SIA et sains. Leur expression est variable, mais ces variations existent chez les patients SIA et les contrôles. L’implication des estrogènes dans la SIA ne serait donc pas au niveau des récepteurs aux estrogènes mais au niveau de l’interactions des estrogènes avec d’autres facteurs étiologiques tels que la mélatonine, la formation/résorption osseuse ou autres facteurs neuro-endocriniens.

Le rôle de la signalisation Wnt dans le phénotype anormal des ostéoblastes ostéoarthrosiques

L’ostéoarthrose (OA) est une pathologie de forte incidence affectant les articulations. Elle est caractérisée principalement par une dégradation du cartilage articulaire, un déséquilibre au niveau du remodelage osseux et une sclérose de l’os sous-chondral. L’étiologie de cette pathologie reste encore méconnue, cependant il semble de plus en plus que tous les tissus composant l’articulation soient affectés dans cette pathologie. L’importance du rôle de l’os dans le développement de l’OA est incontestable et représente donc une cible thérapeuthique intéressante. Des études effectuées par tomodensitométrie ont démontré une structure et une organisation anormales du tissu osseux des patients OA. Parallèlement, les cultures primaires d’ostéoblastes (Ob) humains OA issus de l’os sous-chondral démontrent un phénotype altéré et une faible minéralisation in vitro. La signalisation Wnt, essentielle dans l’embryogenèse, a montré avoir un rôle clé dans la régulation de l’ostéogenèse en régulant notamment la différenciation terminale des Ob. Le facteur de croissance transformant-β1 (TGF-β1), un facteur agissant notamment sur la prolifération et sur le début de la différenciation des Ob, est surexprimé par les Ob OA et pourrait moduler cette signalisation. Aussi, deux populations de patients OA peuvent être différenciées in vitro par la production de prostaglandines E2 (PGE2) par leurs Ob et les PGE2, dans une étude sur le cancer colorectal, ont montré moduler la signalisation Wnt. Notre hypothèse de travail est que l’activation de la voie de signalisation Wnt/β-caténine est diminuée dans les Ob OA. Cette diminution est responsable de la sous-minéralisation et de l’altération du phénotype des Ob humains OA. Par ailleurs, DKK2, dont l’expression est contrôlée par TGF-β1, est responsable de la diminution de l’activité Wnt/β-caténine et les PGE2 peuvent en partie corriger cette situation. L’objectif général de cette étude est d’une part, de démontrer le rôle de TGF-β1, DKK2 et de PGE2 sur l’altération de la signalisation Wnt/β-caténine et d’autre part, de démontrer le lien entre TGF-β1 et DKK2 et l’effet de ces derniers sur le phénotype des Ob. Dans cette étude on a montré que la signalisation canonique Wnt est altérée dans les Ob OA et que cela était responsable de l’altération du phénotype des Ob OA. On a montré, parmi les acteurs de la signalisation Wnt, que l’expression de l’antagoniste Dickkopf-1 (DKK1) était relativement similaire entre les Ob OA et normaux contrairement à celle de l’antagoniste DKK2 qui était augmentée et à celle de l’agoniste Wnt7B qui était diminuée dans les Ob OA. On a également montré que les PGE2 pouvaient potentialiser l’activité de la signalisation Wnt dans les Ob OA. L’inhibition de DKK2 a permis d’augmenter l’activité de la signalisation Wnt et de corriger le phénotype anormal ainsi que d’augmenter la minéralisation des Ob OA. L’inhibition de TGF-β1, un facteur aussi surexprimé dans les Ob OA, a également permis la correction du phénotype et l’augmentation de la minéralisation dans les Ob OA. L’inhibition de TGF-β1 a aussi menée à l’inhibition de DKK2. Le contraire ne fût pas observé démontrant ainsi la régulation de DKK2 par TGF-β1. En conclusion, la signalisation canonique Wnt est diminuée dans les Ob OA et cela est dû au niveau élevé de DKK2 dans ces Ob. TGF-β1 régule positivement DKK2 et donc la surexpression de TGF-β1 entraîne celle de DKK2 ce qui a pour conséquences d’altérer le phénotype des Ob. Les PGE2 ont aussi montré pouvoir potentialiser l’activité de la signalisation Wnt et auraient donc un rôle positif. Ensemble, ces données suggèrent que ces altérations au niveau des Ob OA pourraient être responsables de la structure osseuse anormale observée chez les patients OA.

Évaluation du potentiel de séquestration de carbone dans le sol de cultures intensives sur courtes rotations de saules dans le sud du Québec

Dans la dernière décennie, plusieurs hectares de terre agricole ont été convertis à la culture intensive sur courtes rotations (CICR) de saules dans le sud du Québec (Canada). Peu d’études ont été réalisées afin de déterminer comment se comporte la dynamique du carbone organique (Corg) dans le sol suivant cette conversion. Nous avons donc comparé la quantité du Corg et de deux pools labiles de carbone (carbone extractible à l’eau chaude et les sucres aminés) entre des CICR en phase initiale d’établissement (1-2 ans) et des parcelles appariées représentant le système de culture qui prévalait avant la transformation en culture de saules (culture fourragère) et d’autres cultures d’intérêt. La même chose a été faite pour une CICR en exploitation (depuis 9 ans) à un autre site. La quantité de Corg du sol n’était pas différente entre les CICR et les parcelles sous culture fourragère. Une plus haute concentration de sucres aminés dans le Corg total des CICR en établissement, par rapport aux autres parcelles sur le même site, permet de soupçonner que les perturbations liées à l’établissement ne mènent pas à une minéralisation accrue du Corg à court terme. La proportion de sucres aminés fongiques, qui diminue théoriquement lors de perturbations, était aussi plus élevée sous la plus jeune culture. Sous la CICR de neuf ans, le Corg était redistribué dans le profil vertical et les pools labiles étaient de plus petite taille (à une profondeur de 20-40 cm) comparativement à une parcelle témoin. La conversion d’une culture fourragère en plantation de saules en CICR n’a pas mené à la formation d’un puits de carbone. L’étude laisse entrevoir qu’un tel puits pourrait être créé si la conversion se faisait à partir d’un aménagement impliquant la culture en rotation de plantes annuelles et des labours.

Contrôle de l'expression de la protéine PHEX et rôle de PHEX et FGF23 dans la minéralisation par les cellules MC3T3

PHEX est une protéine importante dans le processus de minéralisation osseuse. Des mutations ou la délétion d’une partie de ce gène causent l’hypophosphatémie liée au chromosome X (XLH). Cette maladie est caractérisée par une hypophosphatémie, accompagnée de défauts de minéralisation, de rachitisme et de lésions ostéomalaciques. Avec l’hypophosphatémie, les taux circulants de vitamine D devraient être augmentés, ce qui n’est pas le cas d’où une régulation anormale de la production de vitamine D a lieu. Cependant, malgré le fait que cette protéine soit une peptidase, aucun substrat physiologique n’a encore été répertorié pour PHEX. PHEX est une protéine membranaire de type II de la famille M13 des métalloendopeptidases à zinc possédant un court domaine N-terminal cytosolique, un segment transmembrannaire d’environ 20 acides aminés et une large portion C-terminale extracellulaire où se trouve le site actif de l’enzyme. PHEX est exprimée de façon majoritaire dans les os et dans les dents et elle apparaît à l’initiation de la minéralisation. Les patients souffrant de XLH et la souris Hyp, qui est un modèle animal de la maladie humaine, montrent des quantités importantes de la protéine FGF23. De plus, FGF23 est impliqué dans une autre maladie reliée au métabolisme du phosphate, l’hypophosphatémie rachitique autosomale dominante (ADHR) où des mutations de FGF23 causent sensiblement les mêmes symptômes que XLH. FGF23 est produit principalement par les ostéoblastes et les ostéocytes. FGF23 cause une hypophosphatémie par la diminution de l’expression du cotransporteur NaPi de type II, responsable de la réabsorption du phosphate rénal. L’hypothèse proposée dans la littérature serait que PHEX activerait ou inactiverait des peptides importants pour la minéralisation osseuse. Plus spécifiquement, l’activation ou l’inactivation de ces peptides aurait pour rôle de réguler les quantités de FGF23. Selon l’hypothèse mentionnée précédemment, la régulation de PHEX pourrait donc avoir un effet sur la minéralisation. Une quantité croissante de données sur la régulation de PHEX sont maintenant disponibles. Par exemple, la vitamine D diminue l’expression de PHEX tandis que les glucocorticoïdes et l’hormone de croissance augmentent son expression. Dans une première étude, nous avons voulu déterminer si un peptide relié à la minéralisation osseuse, le PTHrP1-34, pouvait réguler l’expression de PHEX. Nous avons déterminé que le PTHrP1-34 peut réguler de façon négative l’expression de PHEX dans les cellules UMR-106, une lignée cellulaire ostéoblastique. Cette régulation passe par la voie de l’AMPc/protéine kinase A. De plus, cette diminution d’expression est également observée au jour 7 dans des cultures primaires d’ostéoblastes de rat en minéralisation. Par la suite, nous avons étudié un mutant de PHEX, le mutant E4Q retrouvé chez un patient souffrant de XLH, où la mutation se retrouve dans le domaine cytosolique de PHEX. Cette mutation n’interfère pas avec le site catalytique de l’enzyme puisque ce mutant de PHEX peut tout aussi bien cliver un substrat synthétique que la protéine sauvage. Il a été déterminé que cette mutation annule un motif di-acide. Nous avons démontré que ce motif di-acide est responsable de la liaison de PHEX à COPII, responsable de la formation de vésicules de sécrétion. De plus, il semblerait que ce motif soit important, probablement par son interaction avec COPII, à l’incorporation de PHEX dans des vésicules de calcification, lesdites vésicules étant importantes dans le processus de minéralisation. Finalement, des essais de compétitions ont démontré que la minéralisation pouvait être perturbée lorsque l’on surexprimait la queue cytosolique sauvage de PHEX, contrairement à la queue mutée. Ceci suggère possiblement que l’interaction avec COPII menant à l’incorporation de PHEX dans les vésicules de calcification ou d’autres protéines comprenant de tels motifs pourrait être importante pour la minéralisation. Finalement, la dernière étude porte sur la protéine FGF23. Nous avons démontré, par la surexpression de FGF23 dans la lignée MC3T3 d’ostéoblastes de souris, que cette surexpression a un effet sur la sénescence de ces cellules. En effet, des essais de sénescence ont montré l’augmentation de celle-ci lorsque FGF23 est surexprimé. Par contre, la prolifération n’est pas altérée. De plus, il semblerait que la différenciation soit plus rapide, tel qu’observé par une minéralisation survenant plus tôt, mais n’étant pas plus importante. Bref, la surexpression de FGF23 semblerait faire en sorte que les ostéoblastes se différencient plus rapidement et passent donc à un état de sénescence prématuré comparativement aux cellules sauvages. Ceci est en accord avec la littérature où KLOTHO, un cofacteur de FGF23 permettant sa liaison avec une plus grande affinité sur son récepteur, lorsqu’inactivé démontre un phénotype similaire au vieillissement incluant un phénotype de sénescence.

Caractérisation de nouveaux mécanismes transcriptionnels impliqués dans la biologie osseuse

Le développement et l'homéostasie des os requièrent l'orchestration spatio-temporelle d'un grand nombre de signaux moléculaires. Ces signaux entraînent l'activation ou l'inhibition de différents facteurs de transcription, lesquels sont en mesure de contrôler la prolifération et la différenciation des ostéoblastes et des chondrocytes. L'intégrité de ces différents mécanismes se doit d'être maintenu tout au long de la vie. Ainsi, une anomalie dans l'un de ces mécanismes conduit à l'apparition de pathologies osseuses et métaboliques telles qu’une hypophosphatémie, l'ostéoporose ou l'ostéoarthrite (OA). Afin d'en apprendre davantage sur la biologie osseuse, le projet décrit dans cette thèse a pour objectif de caractériser de nouveaux mécanismes de régulation transcriptionnelle pour deux gènes importants dans le développement des os et le maintien de leur intégrité. Il s’agit du Paired-like Homeodomain Transcription Factor 1 (PITX1) et du Phosphate-regulating gene with homology to endopeptidase on the X chromosome (PHEX). Le premier mécanisme présenté dans cette thèse concerne la régulation transcriptionnelle du gène PITX1, un facteur de transcription à homéodomaine nécessaire, notamment, au développement des os des membres inférieurs et au maintien de l'intégrité du cartilage articulaire chez l'adulte. Ainsi, dans les chondrocytes articulaires, on note que l'expression de PITX1 est assurée par le recrutement du facteur de transcription E2F1 à deux éléments de réponse présents dans la région proximale du promoteur de PITX1. Aussi, dans les chondrocytes articulaires de patients souffrant d'OA, dans lesquels l'expression de PITX1 est fortement diminuée, un mécanisme de répression transcriptionnelle, lequel implique la protéine multifonctionnelle Prohibitin (PHB1), semble être activé. En effet, dans ces chondroytes, on note une forte accumulation nucléaire de PHB1 comparativement aux chondrocytes articulaires de sujets sains. Le second mécanisme présenté dans cette thèse concerne la répression transcriptionnelle de PHEX, la peptidase mutée dans le syndrome d'hypophosphatémie lié au chromosome X (X-Linked Hypophosphatemia, XLH), lequel se caractérise par une hypophosphatémie et une ostéomalacie. Le traitement d'ostéoblastes à la Parathyroid hormone-related protein (PTHrP) permet d’observer la répression de PHEX. Afin de caractériser le mécanisme responsable de cette répression, des expériences de gènes rapporteurs ont révélé la présence de deux éléments de réponse pour le répresseur transcriptionnel E4BP4 dans le promoteur de PHEX. La suppression de l'expression d'E4BP4 par l'utilisation d'ARN d'interférence a permis de valider que ce facteur de transcription est responsable de la répression de PHEX suite au traitement d'ostéoblastes à la PTHrP. En somme ces nouveaux mécanismes de régulation transcriptionnelle permettent de mieux comprendre la régulation de l'expression de PITX1 et de PHEX. Aussi, cette nouvelle implication de PHB1 dans la pathogenèse de l'OA offre de nouvelles possibilités de traitement et pourrait servir pour le diagnostic précoce de cette pathologie. Enfin, la caractérisation d'E4BP4 en tant que médiateur pour la répression de PHEX par la PTHrP suggère que ce répresseur transcriptionnel pourrait être impliqué dans le contrôle de la minéralisation des os et des niveaux de phosphate sanguin.

Vacuum-ultraviolet photochemically initiated modification of polystyrene surfaces: morphological changes and mechanistic investigations

Vacuum-ultraviolet (VUV) irradiation (kexc: 172 ± 12 nm) of polystyrene films in the presence of oxygen produced not only oxidatively functionalized surfaces, but generated also morphological changes. Whereas OH- and C=O-functionalized surfaces might be used for e.g. secondary functionalization, enhanced aggregation or printing, processes leading to morphological changes open new possibilities of microstructurization. Series of experiments made under different experimental conditions brought evidence of two different reaction pathways: introduction of OH- and C=O-groups at the polystyrene pathways is mainly due to the reaction of reactive oxygen species (hydroxyl radicals, atomic oxygen, ozone) produced in the gas phase between the VUV-radiation source and the substrate. However, oxidative fragmentation leading to morphological changes, oxidation products of low molecular weight and eventually to mineralization of the organic substrate is initiated by electronic excitation of the polymer leading to C–C-bond homolysis and to a complex oxidation manifold after trapping of the C-centred radicals by molecular oxygen. The pathways of oxidative functionalization or fragmentation could be differentiated by FTIR-ATR analysis of irradiated polystyrene surfaces before and after washing with acetonitrile and microscopic fluorescence analysis of the surfaces secondarily functionalized with the N,N,N-tridodecyl-triaza-triangulenium (TATA) cation. Ozonization of the polystyrene leads to oxidative functionalization of the polymer surface but cannot initiate the fragmentation of the polymer backbone. Oxidative fragmentation is initiated by electronic excitation of the polymer (contact-mode AFM analysis), and evidence of the generation of intermediate C-centred radicals is given e.g. by experiments in the absence of oxygen leading to cross-linking (solubility effects, optical microscopy, friction-mode AFM) and disproportionation (fluorescence).

Characterization of polyhydroxyalkanoates accumulating vibrios from marine benthic environments and production studies of polyhydroxyalkanoates by Vibrio sp. BTKB33

The present work deals with the characterization of polyhydroxyalkanoates accumulating vibrios from marine benthic environments and production studies of polyhydroxyalkanoates by vibrio sp.BTKB33. Vibrios are a group of (iram negative, curved or straight motile rods that normally inhabit the aquatic environments.The present study therefore aimed at evaluating the occurrence of PHA accumulating vibrios inhabiting marine benthic environments; characterizing the potential PHA accumulators employing phenotypic and genotypic approaches and molecular characterization of the PHA synthase gene. The study also evaluated the PHA production in V:'hri0 sp. strain BTKB33, through submerged fennentation using statistical optimization and characterized the purified biopolymer. Screening for PHA producing vibrios from marine benthic environments. Characterization of PHA producers employing phenotypic and genotypic approaches.The incidence of PHA accumulation in Vibrio sp. isolated from marine sediments was observed to be high, indicating that the natural habitat of these bacteria are stressful. Considering their ubiquitous nature, the ecological role played by vibrios in maintaining the delicate balance of the benthic ecosystem besides returning potential strains, with the ability to elaborate a plethora of extracellular enzymes for industrial application, is significant. The elaboration of several hydrolytic enzymes by individuals also emphasize the crucial role of vibrios in the mineralization process in the marine environment. This study throws light on the extracellular hydrolytic enzyme profile exhibited by vibrios. It was concluded that apart from the PHA accumulation, presence of exoenzyme production and higher MAR index also aids in their survival in the highly challenging benthic enviromnents. The phylogenetic analysis of the strains and studies on intra species variation within PHA accumulating strains reveal their diversity. The isolate selected for production in this study was Vibrio sp. strain BTKB33, identified as V.azureus by 16S rDNA sequencing and phenotypic characterization. The bioprocess variables for PHA production utilising submerged fermentation was optimized employing one-factor-at-a-time-method, PB design and RSM studies. The statistical optimization of bioprocess variables revealed that NaCl concentration, temperature and incubation period are the major bioprocess variables influencing PHA production and PHA content. The presence of Class I PHA synthase genes in BTKB33 was also unveiled. The characterization of phaC genes by PCR and of the extracted polymer employing FTIR and NMR analysis revealed the presence of polyhydroxybutyrate, smallest known PI-IAs, having wider domestic, industrial and medical application. The strain BTKB33 bearing a significant exoenzyme profile, can thus be manipulatedin future for utilization of diverse substrates as C- source for PHA production. In addition to BTKB33, several fast growing Vibrio sp. having PHA accumulating ability were also isolated, revealing the prospects of this environment as a mine for novel PHA accumulating microbes. The findings of this study will provide a reference for further research in industrial production of PHAs from marine microorganisms .

Marine Microbial Enzymes

3.4. Lipase (EC-3.1. 1.3) 3.5. Other Known Enzymes 3.6. Extremozymes (Enzymes from extremophiles) 3.7. Recognition of Valuable Extremozymes 4. Enzymes as Tools in Biotechnology 4.1. Restriction Enzymes from Marine Bacteria 4.2. Other Nucleases from Marine Bacteria 4.3. Bacteriolytic Enzyme by Bacteriophage from Seawater 5. Innovations in Enzyme Technology 5.1. Enzyme Engineering 5.2. Immobilization Technology 5.3. Gene Cloning for Marine Enzymes 6. Future Prospects

Synthesis, Characterization and Applications of Modified TiO2 Systems

This thesis is divided in to 9 chapters and deals with the modification of TiO2 for various applications include photocatalysis, thermal reaction, photovoltaics and non-linear optics. Chapter 1 involves a brief introduction of the topic of study. An introduction to the applications of modified titania systems in various fields are discussed concisely. Scope and objectives of the present work are also discussed in this chapter. Chapter 2 explains the strategy adopted for the synthesis of metal, nonmetal co-doped TiO2 systems. Hydrothermal technique was employed for the preparation of the co-doped TiO2 system, where Ti[OCH(CH3)2]4, urea and metal nitrates were used as the sources for TiO2, N and metals respectively. In all the co-doped systems, urea to Ti[OCH(CH3)2]4 was taken in a 1:1 molar ratio and varied the concentration of metals. Five different co-doped catalytic systems and for each catalysts, three versions were prepared by varying the concentration of metals. A brief explanation of physico-chemical techniques used for the characterization of the material was also presented in this chapter. This includes X-ray Diffraction (XRD), Raman Spectroscopy, FTIR analysis, Thermo Gravimetric Analysis, Energy Dispersive X-ray Analysis (EDX), Scanning Electron Microscopy(SEM), UV-Visible Diffuse Reflectance Spectroscopy (UV-Vis DRS), Transmission Electron Microscopy (TEM), BET Surface Area Measurements and X-ray Photoelectron Spectroscopy (XPS). Chapter 3 contains the results and discussion of characterization techniques used for analyzing the prepared systems. Characterization is an inevitable part of materials research. Determination of physico-chemical properties of the prepared materials using suitable characterization techniques is very crucial to find its exact field of application. It is clear from the XRD pattern that photocatalytically active anatase phase dominates in the calcined samples with peaks at 2θ values around 25.4°, 38°, 48.1°, 55.2° and 62.7° corresponding to (101), (004), (200), (211) and (204) crystal planes (JCPDS 21-1272) respectively. But in the case of Pr-N-Ti sample, a new peak was observed at 2θ = 30.8° corresponding to the (121) plane of the polymorph brookite. There are no visible peaks corresponding to dopants, which may be due to their low concentration or it is an indication of the better dispersion of impurities in the TiO2. Crystallite size of the sample was calculated from Scherrer equation byusing full width at half maximum (FWHM) of the (101) peak of the anatase phase. Crystallite size of all the co-doped TiO2 was found to be lower than that of bare TiO2 which indicates that the doping of metal ions having higher ionic radius into the lattice of TiO2 causes some lattice distortion which suppress the growth of TiO2 nanoparticles. The structural identity of the prepared system obtained from XRD pattern is further confirmed by Raman spectra measurements. Anatase has six Raman active modes. Band gap of the co-doped system was calculated using Kubelka-Munk equation and that was found to be lower than pure TiO2. Stability of the prepared systems was understood from thermo gravimetric analysis. FT-IR was performed to understand the functional groups as well as to study the surface changes occurred during modification. EDX was used to determine the impurities present in the system. The EDX spectra of all the co-doped samples show signals directly related to the dopants. Spectra of all the co-doped systems contain O and Ti as the main components with low concentrations of doped elements. Morphologies of the prepared systems were obtained from SEM and TEM analysis. Average particle size of the systems was drawn from histogram data. Electronic structures of the samples were identified perfectly from XPS measurements. Chapter 4 describes the photocatalytic degradation of herbicides Atrazine and Metolachlor using metal, non-metal co-doped titania systems. The percentage of degradation was analyzed by HPLC technique. Parameters such as effect of different catalysts, effect of time, effect of catalysts amount and reusability studies were discussed. Chapter 5 deals with the photo-oxidation of some anthracene derivatives by co-doped catalytic systems. These anthracene derivatives come underthe category of polycyclic aromatic hydrocarbons (PAH). Due to the presence of stable benzene rings, most of the PAH show strong inhibition towards biological degradation and the common methods employed for their removal. According to environmental protection agency, most of the PAH are highly toxic in nature. TiO2 photochemistry has been extensively investigated as a method for the catalytic conversion of such organic compounds, highlighting the potential of thereof in the green chemistry. There are actually two methods for the removal of pollutants from the ecosystem. Complete mineralization is the one way to remove pollutants. Conversion of toxic compounds to another compound having toxicity less than the initial starting compound is the second way. Here in this chapter, we are concentrating on the second aspect. The catalysts used were Gd(1wt%)-N-Ti, Pd(1wt%)-N-Ti and Ag(1wt%)-N-Ti. Here we were very successfully converted all the PAH to anthraquinone, a compound having diverse applications in industrial as well as medical fields. Substitution of 10th position of desired PAH by phenyl ring reduces the feasibility of photo reaction and produced 9-hydroxy 9-phenyl anthrone (9H9PA) as an intermediate species. The products were separated and purified by column chromatography using 70:30 hexane/DCM mixtures as the mobile phase and the resultant products were characterized thoroughly by 1H NMR, IR spectroscopy and GCMS analysis. Chapter 6 elucidates the heterogeneous Suzuki coupling reaction by Cu/Pd bimetallic supported on TiO2. Sol-Gel followed by impregnation method was adopted for the synthesis of Cu/Pd-TiO2. The prepared system was characterized by XRD, TG-DTG, SEM, EDX, BET Surface area and XPS. The product was separated and purified by column chromatography using hexane as the mobile phase. Maximum isolated yield of biphenyl of around72% was obtained in DMF using Cu(2wt%)-Pd(4wt%)-Ti as the catalyst. In this reaction, effective solvent, base and catalyst were found to be DMF, K2CO3 and Cu(2wt%)-Pd(4wt%)-Ti respectively. Chapter 7 gives an idea about the photovoltaic (PV) applications of TiO2 based thin films. Due to energy crisis, the whole world is looking for a new sustainable energy source. Harnessing solar energy is one of the most promising ways to tackle this issue. The present dominant photovoltaic (PV) technologies are based on inorganic materials. But the high material, low power conversion efficiency and manufacturing cost limits its popularization. A lot of research has been conducted towards the development of low-cost PV technologies, of which organic photovoltaic (OPV) devices are one of the promising. Here two TiO2 thin films having different thickness were prepared by spin coating technique. The prepared films were characterized by XRD, AFM and conductivity measurements. The thickness of the films was measured by Stylus Profiler. This chapter mainly concentrated on the fabrication of an inverted hetero junction solar cell using conducting polymer MEH-PPV as photo active layer. Here TiO2 was used as the electron transport layer. Thin films of MEH-PPV were also prepared using spin coating technique. Two fullerene derivatives such as PCBM and ICBA were introduced into the device in order to improve the power conversion efficiency. Effective charge transfer between the conducting polymer and ICBA were understood from fluorescence quenching studies. The fabricated Inverted hetero junction exhibited maximum power conversion efficiency of 0.22% with ICBA as the acceptor molecule. Chapter 8 narrates the third order order nonlinear optical properties of bare and noble metal modified TiO2 thin films. Thin films were fabricatedby spray pyrolysis technique. Sol-Gel derived Ti[OCH(CH3)2]4 in CH3CH2OH/CH3COOH was used as the precursor for TiO2. The precursors used for Au, Ag and Pd were the aqueous solutions of HAuCl4, AgNO3 and Pd(NO3)2 respectively. The prepared films were characterized by XRD, SEM and EDX. The nonlinear optical properties of the prepared materials were investigated by Z-Scan technique comprising of Nd-YAG laser (532 nm,7 ns and10 Hz). The non-linear coefficients were obtained by fitting the experimental Z-Scan plot with the theoretical plots. Nonlinear absorption is a phenomenon defined as a nonlinear change (increase or decrease) in absorption with increasing of intensity. This can be mainly divided into two types: saturable absorption (SA) and reverse saturable absorption (RSA). Depending on the pump intensity and on the absorption cross- section at the excitation wavelength, most molecules show non- linear absorption. With increasing intensity, if the excited states show saturation owing to their long lifetimes, the transmission will show SA characteristics. Here absorption decreases with increase of intensity. If, however, the excited state has strong absorption compared with that of the ground state, the transmission will show RSA characteristics. Here in our work most of the materials show SA behavior and some materials exhibited RSA behavior. Both these properties purely depend on the nature of the materials and alignment of energy states within them. Both these SA and RSA have got immense applications in electronic devices. The important results obtained from various studies are presented in chapter 9.

Produktion und Nutzung von mikrobiellen Residuen als labile Zwischenspeicher für Nährstoffe

Mit dem Ziel, die Bildung und den Verbrauch von mikrobiellen Residuen zu ermitteln, wurden zwei Inkubationsversuche durchgeführt. Die Versuchsdauer betrug jeweils 67 Tage, wobei an den Tagen 5, 12, 33, 38, 45 und 67 Proben entnommen und auf Ct, Cmik, CO2 sowie die δ13C-Werte, Nt, Nmin und Ergosterol untersucht wurden. In Versuch 1 wurden als leicht umsetzbare Kohlenstoffquelle 3 mg C4-Kohlenstoff g-1Boden in Form von Rohrzucker bzw. Maiscellulose und als N-Ausgleich 200 µg NH4NO3-N g-1Boden hinzugegeben. Der verwendete Boden war ein Lößboden. In Versuch 2 wurden 3 mg C4-Kohlenstoff g-1Boden in Form von Rohrzucker und 100 µg NH4NO3-N g-1Boden in den Boden eingearbeitet. Als Substrat wurde hier ein gebrannter Lößboden verwendet. Bei beiden Versuchen erfolgte an Tag 33 nochmals eine Zugabe von 3 mg C3-Kohlenstoff g-1Boden in Form von Cellulose. Die Zugabe des C4-Kohlenstoffs führte in beiden Versuchen zu einer Zunahme des C4-Anteils in der mikrobiellen Biomasse. Insgesamt wurden im ersten Versuch ca. 78 % des C4-Kohlenstoffs und im zweiten Versuch ca. 64 % mineralisiert. In Versuch 1 wurde bei der Rohrzuckervariante der größte Teil an C4-C innerhalb der ersten 5 Tage mineralisiert, in der Cellulosevariante konnte dagegen eine geringere, aber länger anhaltende Mineralisation bis Tag 33 beobachtet werden. Dies sowie die Entwicklung des C4-C der mikrobiellen Biomasse deuten darauf hin, dass die Cellulose erst zu diesem Zeitpunkt vollständig umgesetzt war, der Rohrzucker dagegen aber schon nach 5 Inkubationstagen. Der Anteil an C4-C in den mikrobiellen Residuen lag an Tag 33 bei 28 % (Cellulosevariante) bzw. 22 % (Rohrzuckervariante) des zugegebenen C4-Kohlenstoffs. Dagegen lag im zweiten Versuch der Anteil an C4-Kohlenstoff in den mikrobiellen Residuen bei 40 %. In Versuch 1 führte die Zugabe der C3-Cellulose an Tag 33 nicht zu einem Verbrauch von mikrobiellen Residuen, im Versuch 2 hingegen zu einer signifikanten Abnahme. Der zugegebene Stickstoff wurde in beiden Versuchen durch die Zugabe des Rohrzuckers in hohen Anteilen immobilisiert, aber nur in geringem Umfang in die mikrobielle Biomasse inkorporiert. An Tag 33 lag der Anteil Stickstoff in den mikrobiellen Residuen bei 52 % (Versuch 1) bzw. 84 % (Versuch 2) des zugegebenen Stickstoffs. In Versuch 1 setzte nach 33 Tagen eine Remineralisation des immobilisierten Stickstoffs ein, unabhängig von der Zugabe der C3-Cellulose. In Versuch 2 wurde der immobilisierte Stickstoff zu keinem Zeitpunkt remineralisiert. Die Zugabe der C3-Cellulose führte hier nicht zu einer Remineralisation des immobilisierten Stickstoffs. Es bestätigte sich die Annahme, dass durch die Zugabe von leicht umsetzbaren Kohlstoffsubstraten die Bildung von mikrobiellen Residuen gesteigert werden kann. Die zweite Annahme, dass durch die Zugabe von N-freiem Substrat, hier C3-Cellulose, die mikrobiellen Residuen bevorzugt abgebaut werden, konnte nicht bestätigt werden.

Salinity-induced changes in the microbial use of sugarcane filter cake added to soil

Five laboratory incubation experiments were carried out to assess the salinity-induced changes in the microbial use of sugarcane filter cake added to soil. The first laboratory experiment was carried out to prove the hypothesis that the lower content of fungal biomass in a saline soil reduces the decomposition of a complex organic substrate in comparison to a non-saline soil under acidic conditions. Three different rates (0.5, 1.0, and 2.0%) of sugarcane filter cake were added to both soils and incubated for 63 days at 30°C. In the saline control soil without amendment, cumulative CO2 production was 70% greater than in the corresponding non-saline control soil, but the formation of inorganic N did not differ between these two soils. However, nitrification was inhibited in the saline soil. The increase in cumulative CO2 production by adding filter cake was similar in both soils, corresponding to 29% of the filter cake C at all three addition rates. Also the increases in microbial biomass C and biomass N were linearly related to the amount of filter cake added, but this increase was slightly higher for both properties in the saline soil. In contrast to microbial biomass, the absolute increase in ergosterol content in the saline soil was on average only half that in the non-saline soil and it showed also strong temporal changes during the incubation: A strong initial increase after adding the filter cake was followed by a rapid decline. The addition of filter cake led to immobilisation of inorganic N in both soils. This immobilisation was not expected, because the total C-to-total N ratio of the filter cake was below 13 and the organic C-to-organic N ratio in the 0.5 M K2SO4 extract of this material was even lower at 9.2. The immobilisation was considerably higher in the saline soil than in the non-saline soil. The N immobilisation capacity of sugarcane filter cake should be considered when this material is applied to arable sites at high rations. The second incubation experiment was carried out to examine the N immobilizing effect of sugarcane filter cake (C/N ratio of 12.4) and to investigate whether mixing it with compost (C/N ratio of 10.5) has any synergistic effects on C and N mineralization after incorporation into the soil. Approximately 19% of the compost C added and 37% of the filter cake C were evolved as CO2, assuming that the amendments had no effects on the decomposition of soil organic C. However, only 28% of the added filter cake was lost according to the total C and d13C values. Filter cake and compost contained initially significant concentrations of inorganic N, which was nearly completely immobilized between day 7 and 14 of the incubation in most cases. After day 14, N re-mineralization occurred at an average rate of 0.73 µg N g-1 soil d-1 in most amendment treatments, paralleling the N mineralization rate of the non-amended control without significant difference. No significant net N mineralization from the amendment N occurred in any of the amendment treatments in comparison to the control. The addition of compost and filter cake resulted in a linear increase in microbial biomass C with increasing amounts of C added. This increase was not affected by differences in substrate quality, especially the three times larger content of K2SO4 extractable organic C in the sugarcane filter cake. In most amendment treatments, microbial biomass C and biomass N increased until the end of the incubation. No synergistic effects could be observed in the mixture treatments of compost and sugarcane filter cake. The third 42-day incubation experiment was conducted to answer the questions whether the decomposition of sugarcane filter cake also result in immobilization of nitrogen in a saline alkaline soil and whether the mixing of sugarcane filter cake with glucose (adjusted to a C/N ratio of 12.5 with (NH4)2SO4) change its decomposition. The relative percentage CO2 evolved increased from 35% of the added C in the pure 0.5% filter cake treatment to 41% in the 0.5% filter cake +0.25% glucose treatment to 48% in the 0.5% filter cake +0.5% glucose treatment. The three different amendment treatments led to immediate increases in microbial biomass C and biomass N within 6 h that persisted only in the pure filter cake treatment until the end of the incubation. The fungal cell-membrane component ergosterol showed initially an over-proportionate increase in relation to microbial biomass C that fully disappeared at the end of the incubation. The cellulase activity showed a 5-fold increase after filter cake addition, which was not further increased by the additional glucose amendment. The cellulase activity showed an exponential decline to values around 4% of the initial value in all treatments. The amount of inorganic N immobilized from day 0 to day 14 increased with increasing amount of C added in comparison to the control treatment. Since day 14, the immobilized N was re-mineralized at rates between 1.31 and 1.51 µg N g-1 soil d-1 in the amendment treatments and was thus more than doubled in comparison with the control treatment. This means that the re-mineralization rate is independent from the actual size of the microbial residues pool and also independent from the size of the soil microbial biomass. Other unknown soil properties seem to form a soil-specific gate for the release of inorganic N. The fourth incubation experiment was carried out with the objective of assessing the effects of salt additions containing different anions (Cl-, SO42-, HCO3-) on the microbial use of sugarcane filter cake and dhancha leaves amended to inoculated sterile quartz sand. In the subsequent fifth experiment, the objective was to assess the effects of inoculum and temperature on the decomposition of sugar cane filter cake. In the fourth experiment, sugarcane filter cake led to significantly lower respiration rates, lower contents of extractable C and N, and lower contents of microbial biomass C and N than dhancha leaves, but to a higher respiratory quotient RQ and to a higher content of the fungal biomarker ergosterol. The RQ was significantly increased after salt addition, when comparing the average of all salinity treatments with the control. Differences in anion composition had no clear effects on the RQ values. In experiment 2, the rise in temperature from 20 to 40°C increased the CO2 production rate by a factor of 1.6, the O2 consumption rate by a factor of 1.9 and the ergosterol content by 60%. In contrast, the contents of microbial biomass N decreased by 60% and the RQ by 13%. The effects of the inoculation with a saline soil were in most cases negative and did not indicate a better adaptation of these organisms to salinity. The general effects of anion composition on microbial biomass and activity indices were small and inconsistent. Only the fraction of 0.5 M K2SO4 extractable C and N in non-fumigated soil was consistently increased in the 1.2 M NaHCO3 treatment of both experiments. In contrast to the small salinity effects, the quality of the substrate has overwhelming effects on microbial biomass and activity indices, especially on the fungal part of the microbial community.

Management approaches in organic potato and tomato production

The presented thesis considered three different system approach topics to ensure yield and plant health in organically grown potatoes and tomatoes. The first topic describes interactions between late blight (Phytophthora infestans) incidence and soil nitrogen supply on yield in organic potato farming focussing in detail on the yield loss relationship of late blight based on results of several field trials. The interactive effects of soil N-supply, climatic conditions and late blight on the yield were studied in the presence and absence of copper fungicides from 2002-2004 for the potato cultivar Nicola. Under conditions of central Germany the use of copper significantly reduced late blight in almost all cases (15-30 %). However, the reductions in disease through copper application did not result in statistically significant yield increases (+0 – +10 %). Subsequently, only 30 % of the variation in yield could be attributed to disease reductions. A multiple regression model (R²Max), however, including disease reduction, growth duration and temperature sum from planting until 60 % disease severity was reached and soil mineral N contents 10 days after emergence could explain 75 % of the observed variations in yield. The second topic describes the effect of some selected organic fertilisers and biostimulant products on nitrogen-mineralization and efficiency, yield and diseases in organic potato and tomato trials. The organic fertilisers Biofeed Basis (BFB, plant derived, AgroBioProducts, Wageningen, Netherlands) and BioIlsa 12,5 Export (physically hydrolysed leather shavings, hair and skin of animals; ILSA, Arizignano, Italy) and two biostimulant products BioFeed Quality (BFQ, multi-compound seaweed extract, AgroBioProducts) and AUSMA (aqueous pine and spruce needle extract, A/S BIOLAT, Latvia), were tested. Both fertilisers supplied considerable amounts of nitrogen during the main uptake phases of the crops and reached yields as high or higher as compared to the control with horn meal fertilisation. The N-efficiency of the tested fertilisers in potatoes ranged from 90 to 159 kg yield*kg-1 N – input. Most effective with tomatoes were the combined treatments of fertiliser BFB and the biostimulants AUSMA and BFQ. Both biostimulants significantly increased the share of healthy fruit and/or the number of fruits. BFQ significantly increased potato yields (+6 %) in one out of two years and reduced R. solani-infestation in the potatoes. This suggests that the biostimulants had effects on plant metabolism and resistance properties. However, no effects of biostimulants on potato late blight could be observed in the fields. The third topic focused on the effect of suppressive composts and seed tuber health on the saprophytic pathogen Rhizoctonia solani in organic potato systems. In the present study 5t ha-1 DM of a yard and bio-waste (60/40) compost produced in a 5 month composting process and a 15 month old 100 % yard waste compost were used to assess the effects on potato infection with R. solani when applying composts within the limits allowed. Across the differences in initial seed tuber infestation and 12 cultivars 5t DM ha-1 of high quality composts, applied in the seed tuber area, reduced the infestation of harvested potatoes with black scurf, tuber malformations and dry core tubers by 20 to 84 %, 20 to 49 % and 38 to 54 %, respectively, while marketable yields were increased by 5 to 25 % due to lower rates of wastes after sorting (marketable yield is gross yield minus malformed tubers, tubers with dry core, tubers with black scurf > 15% infested skin). The rate of initial black scurf infection of the seed tubers also affected tuber number, health and quality significantly. Compared to healthy seed tubers initial black scurf sclerotia infestation of 2-5 and >10 % of tuber surface led in untreated plots to a decrease in marketable yields by 14-19 and 44-66 %, a increase of black scurf severity by 8-40 and 34-86 % and also increased the amount of malformed and dry core tubers by 32-57 and 109-214 %.

Effects of fertilizer type and rate on partitioning of soil organic matter into pools of different stability

Type and rate of fertilizers influence the level of soil organic carbon (Corg) and total nitrogen (Nt) markedly, but the effect on C and N partitioning into different pools is open to question. The objectives of the present work were to: (i) quantify the impact of fertilizer type and rate on labile, intermediate and passive C and N pools by using a combination of biological, chemical and mathematical methods; (ii) explain previously reported differences in the soil organic matter (SOM) levels between soils receiving farmyard manure with or without biodynamic preparations by using Corg time series and information on SOM partitioning; and (iii) quantify the long-term and short-term dynamics of SOM in density fractions and microbial biomass as affected by fertilizer type and rate and determine the incorporation of crop residues into labile SOM fractions. Samples were taken from a sandy Cambisol from the long-term fertilization trial in Darmstadt, Germany, founded in 1980. The nine treatments (four field replicates) were: straw incorporation plus application of mineral fertilizer (MSI) and application of rotted farmyard manure with (DYN) or without (FYM) addition of biodynamic preparations, each at high (140 – 150 kg N ha-1 year-1; MSIH, DYNH, FYMH), medium (100 kg N ha-1 year-1; MSIM, DYNM, FYMM) and low (50 – 60 kg N ha-1 year-1; MSIL, DYNL, FYML) rates. The main findings were: (i) The stocks of Corg (t ha-1) were affected by fertilizer type and rate and increased in the order MSIL (23.6), MSIM (23.7), MSIH (24.2) < FYML (25.3) < FYMM (28.1), FYMH (28.1). Stocks of Nt were affected in the same way (C/N ratio: 11). Storage of C and N in the modelled labile pools (turnover times: 462 and 153 days for C and N, respectively) were not influenced by the type of fertilizer (FYM and MSI) but depended significantly (p ≤ 0.05) on the application rate and ranged from 1.8 to 3.2 t C ha 1 (7 – 13% of Corg) and from 90 to 140 kg N ha-1 (4-5% of Nt). In the calculated intermediate pool (C/N ratio 7), stocks of C were markedly higher in FYM treatments (15-18 t ha-1) compared to MSI treatments (12-14 t ha-1). This showed that differences in SOM stocks in the sandy Cambisol induced by fertilizer rate may be short-lived in case of changing management, but differences induced by fertilizer type may persist for decades. (ii) Crop yields, estimated C inputs (1.5 t ha-1 year-1) with crop residue, microbial bio¬mass C (Cmic, 118 – 150 mg kg-1), microbial biomass N (17 – 20 mg kg-1) and labile C and N pools did not differ significantly between FYM and DYN treatments. However, labile C increased linearly with application rate (R2 = 0.53) from 7 to 11% of Corg. This also applied for labile N (3.5 to 4.9% of Nt). The higher contents of Corg in DYN treatments existed since 1982, when the first sampling was conducted for all individual treatments. Contents of Corg between DYN and FYM treatments con-verged slightly since then. Furthermore, at least 30% of the difference in Corg was located in the passive pool where a treatment effect could be excluded. Therefore, the reported differences in Corg contents existed most likely since the beginning of the experiment and, as a single factor of biodynamic agriculture, application of bio-dynamic preparations had no effect on SOM stocks. (iii) Stocks of SOM, light fraction organic C (LFOC, ρ ≤ 2.0 g cm-3), light fraction organic N and Cmic decreased in the order FYMH > FYML > MSIH, MSIL for all sampling dates in 2008 (March, May, September, December). However, statistical significance of treatment effects differed between the dates, probably due to dif-ferences in the spatial variation throughout the year. The high proportion of LFOC on total Corg stocks (45 – 55%) highlighted the importance of selective preservation of OM as a stabilization mechanism in this sandy Cambisol. The apparent turnover time of LFOC was between 21 and 32 years, which agreed very well with studies with substantially longer vegetation change compared to our study. Overall, both approaches; (I) the combination of incubation, chemical fractionation and simple modelling and (II) the density fractionation; provided complementary information on the partitioning of SOM into pools of different stability. The density fractionation showed that differences in Corg stocks between FYM and MSI treatments were mainly located in the light fraction, i.e. induced by higher recalcitrance of the organic input in the FYM treatments. Moreover, the use of the combination of biological, chemical and mathematical methods indicated that effects of fertilizer rate on total Corg and Nt stocks may be short-lived, but that the effect of fertilizer type may persist for longer time spans in the sandy Cambisol.

Effects of tillage on processes of organic matter sequestration

To increase the organic matter (OM) content in the soil is one main goal in arable soil management. The adoption of tillage systems with reduced tillage depth and/or frequency (reduced tillage) or of no-tillage was found to increase the concentration of soil OM compared to conventional tillage (CT; ploughing to 20-30 cm). However, the underlying processes are not yet clear and are discussed contradictorily. So far, few investigations were conducted on tillage systems with a shallow tillage depth (minimum tillage = MT; maximum tillage depth of 10 cm). A better understanding of the interactions between MT implementation and changes in OM transformation in soils is essential in order to evaluate the possible contribution of MT to a sustainable management of arable soils. The objectives of the present thesis were (i) to compare OM concentrations, microbial biomass, water-stable aggregates, and particulate OM (POM) between CT and MT soils, (ii) to estimate the temporal variability of water-stable aggregate size classes occurring in the field and the dynamics of macroaggregate (>250 µm) formation and disruption under controlled conditions, (iii) to investigate whether a lower disruption or a higher formation rate accounts for a higher occurrence of macroaggregates under MT compared to CT, (iv) to determine which fraction is the major agent for storing the surplus of OM found under MT compared to CT, and (v) to observe the early OM transformation after residue incorporation in different tillage systems simulated. Two experimental sites (Garte-Süd and Hohes Feld) near Göttingen, Germany, were investigated. Soil type of both sites was a Haplic Luvisol. Since about 40 years, both sites receive MT by a rotary harrow (to 5-8 cm depth) and CT by a plough (to 25 cm depth). Surface soils (0-5 cm) and subsoils (10-20 cm) of two sampling dates (after fallow and directly after tillage) were investigated for concentrations of organic C (Corg) and total N (N), different water-stable aggregate size classes, different density fractions (for the sampling date after fallow only), microbial biomass, and for biochemically stabilized Corg and N (by acid hydrolysis; for the sampling date after tillage only). In addition, two laboratory incubations were performed under controlled conditions: Firstly, MT and CT soils were incubated (28 days at 22°C) as bulk soil and with destroyed macroaggregates in order to estimate the importance of macroaggregates for the physical protection of the very labile OM against mineralization. Secondly, in a microcosm experiment simulating MT and CT systems with soil <250 µm and with 15N and 13C labelled maize straw incorporated to different depths, the mineralization, the formation of new macroaggregates, and the partitioning of the recently added C and N were followed (28 days at 15°C). Forty years of MT regime led to higher concentrations of microbial biomass and of Corg and N compared to CT, especially in the surface soil. After fallow and directly after tillage, a higher proportion of water-stable macroaggregates rich in OM was found in the MT (36% and 66%, respectively) than in the CT (19% and 47%, respectively) surface soils of both sites (data shown are of the site Garte-Süd only). The subsoils followed the same trend. For the sampling date after fallow, no differences in the POM fractions were found but there was more OM associated to the mineral fraction detected in the MT soils. A large temporal variability was observed for the abundance of macroaggregates. In the field and in the microcosm simulations, macroaggregates were found to have a higher formation rate after the incorporation of residues under MT than under CT. Thus, the lower occurrence of macroaggregates in CT soils cannot be attributed to a higher disruption but to a lower formation rate. A higher rate of macroaggregate formation in MT soils may be due to (i) the higher concentrated input of residues in the surface soil and/or (ii) a higher abundance of fungal biomass in contrast to CT soils. Overall, as a location of storage of the surplus of OM detected under MT compared to CT, water-stable macroaggregates were found to play a key role. In the incubation experiment, macroaggregates were not found to protect the very labile OM against mineralization. Anyway, the surplus of OM detected after tillage in the MT soil was biochemically degradable. MT simulations in the microcosm experiment showed a lower specific respiration and a less efficient translocation of recently added residues than the CT simulations. Differences in the early processes of OM translocation between CT and MT simulations were attributed to a higher residue to soil ratio and to a higher proportion of fungal biomass in the MT simulations. Overall, MT was found to have several beneficial effects on the soil structure and on the storage of OM, especially in the surface soil. Furthermore, it was concluded that the high concentration of residues in the surface soil of MT may alter the processes of storage and decomposition of OM. In further investigations, especially analysis of the residue-soil-interface and of effects of the depth of residue incorporation should be emphasised. Moreover, further evidence is needed on differences in the microbial community between CT and MT soils.

Effects of Different Feeding Regimes on the Digestibility and Faecal Excretion of Nitrogen, Soluble Carbohydrates and Fibre Fractions in Water Buffaloes kept under Subtropical Conditions

In the course of the ‘Livestock Revolution’, extension and intensification of, among others, ruminant livestock production systems are current phenomena, with all their positive and negative side effects. Manure, one of the inevitable secondary products of livestock rearing, is a valuable source of plant nutrients and its skillful recycling to the soil-plant interface is essential for soil fertility, nutrient - and especially phosphorus - uses efficiency and the preservation or re-establishment of environmentally sustainable farming systems, for which organic farming systems are exemplarily. Against this background, the PhD research project presented here, which was embedded in the DFG-funded Research Training Group 1397 ‘Regulation of soil organic matter and nutrient turnover in organic agriculture ’ investigated possibilities to manipulate the diets of water buffalo (Bubalus bubalis L.) so as to produce manure of desired quality for organic vegetable production, without affecting the productivity of the animals used. Consisting of two major parts, the first study (chapter 2) tested the effects of diets differing in their ratios of carbon (C) to nitrogen (N) and of structural to non-structural carbohydrates on the quality of buffalo manure under subtropical conditions in Sohar, Sultanate of Oman. To this end, two trials were conducted with twelve water buffalo heifers each, using a full Latin Square design. One control and four tests diets were examined during three subsequent 7 day experimental periods preceded each by 21 days adaptation. Diets consisted of varying proportions of Rhodes grass hay, soybean meal, wheat bran, maize, dates, and a commercial concentrate to achieve a (1) high C/N and high NDF (neutral detergent fibre)/SC (soluble carbohydrate) ratio (HH), (2) low C/N and low NDF/SC ratio (LL); (3) high C/N and low NDF/SC ratio (HL) and (4) low C/N and high NDF/SC (LH) ratio. Effects of these diets, which were offered at 1.45 times maintenance requirements of metabolizable energy, and of individual diet characteristics, respectively, on the amount and quality of faeces excreted were determined and statistically analysed. The faeces produced from diets HH and LL were further tested in a companion PhD study (Mr. K. Siegfried) concerning their nutrient release in field experiments with radish and cabbage. The second study (chapter 3) focused on the effects of the above-described experimental diets on the rate of passage of feed particles through the gastrointestinal tract of four randomly chosen animals per treatment. To this end, an oral pulse dose of 683 mg fibre particles per kg live weight marked with Ytterbium (Yb; 14.5 mg Yb g-1 organic matter) was dosed at the start of the 7 day experimental period which followed 21 days of adaptation. During the first two days a sample for Yb determination was kept from each faecal excretion, during days 3 – 7 faecal samples were kept from the first morning and the first evening defecation only. Particle passage was modelled using a one-compartment age-dependent Gamma-2 model. In both studies individual feed intake and faecal excretion were quantified throughout the experimental periods and representative samples of feeds and faeces were subjected to proximate analysis following standard protocols. In the first study the organic matter (OM) intake and excretion of LL and LH buffaloes were significantly lower than of HH and HL animals, respectively. Digestibility of N was highest in LH (88%) and lowest in HH (74%). While NDF digestibility was also highest in LH (85%) it was lowest in LL (78%). Faecal N concentration was positively correlated (P≤0.001) with N intake, and was significantly higher in faeces excreted by LL than by HH animals. Concentrations of fibre and starch in faecal OM were positively affected by the respective dietary concentrations, with NDF being highest in HH (77%) and lowest in LL (63%). The faecal C/N ratio was positively related (P≤0.001) to NDF intake; C/N ratios were 12 and 7 for HH and LL (P≤0.001), while values for HL and LH were 11.5 and 10.6 (P>0.05). The results from the second study showed that dietary N concentration was positively affecting faecal N concentration (P≤0.001), while there was a negative correlation with the faecal concentration of NDF (P≤0.05) and the faecal ratios of NDF/N and C/N (P≤0.001). Particle passage through the mixing compartment was lower (P≤0.05) for HL (0.033 h-1) than for LL (0.043 h-1) animals, while values of 0.034 h-1 and 0.038 h-1 were obtained for groups LH and HH. At 55.4 h, total tract mean retention time was significantly (P≤0.05) lower in group LL that in all other groups where these values varied between 71 h (HH) and 79 h (HL); this was probably due to the high dietary N concentration of diet LL which was negatively correlated with time of first marker appearance in faeces (r= 0.84, P≤0.001), while the dietary C concentration was negatively correlated with particle passage through the mixing compartment (r= 0.57, P≤0.05). The results suggest that manure quality of river buffalo heifers can be considerably influenced by diet composition. Despite the reportedly high fibre digestion capacity of buffalo, digestive processes did not suppress the expression of diet characteristics in the faeces. This is important when aiming at producing a specific manure quality for fertilization purposes in (organic) crop cultivation. Although there was a strong correlation between the ingestion and the faecal excretion of nitrogen, the correlation between diet and faecal C/N ratio was weak. To impact on manure mineralization, the dietary NDF and N concentrations seem to be the key control points, but modulating effects are achieved by the inclusion of starch into the diet. Within the boundaries defined by the animals’ metabolic and (re)productive requirements for energy and nutrients, diet formulation may thus take into account the abiotically and biotically determined manure turnover processes in the soil and the nutrient requirements of the crops to which the manure is applied, so as to increase nutrient use efficiency along the continuum of the feed, the animal, the soil and the crop in (organic) farming systems.