Arctic rivers transport 31-42 Tg organic carbon (OC) each year to the Arctic Ocean, which is equal to 10% of the global riverine OC discharge. Since the Arctic Ocean only holds approximately 1% of the global ocean volume, the influence of terrestrially derived organic carbon (OCter) in the Arctic Ocean is relatively high. Despite the global importance of this region the behavior of the, by far largest fraction of the OCter, the dissolved organic carbon (DOC) in Arctic and sub-arctic estuaries is still a matter of debate. This thesis describes data originating from field cruises in Arctic and sub-arctic estuaries and coastal areas with the aim to improve the understanding of the fate of OCter in these areas, with specific focus on DOC. All presented studies indicate that DOCter and terrestrially derived particulate organic carbon (POCter) are subjected to substantial degradation in high-latitude estuaries, as shown by the non-conservative behavior of DOC in the East Siberian Arctic Shelf Seas (ESAS) (paper I) and the even more rapid degradation of POC in the same region (paper II). The removals of OCter in Arctic shelf seas were further supported by multiple isotope studies (paper III and IV), which showed that a use of 13C/12C in both OC and DIC, together with 34S/32S is a powerful tool to describe the sources and fate of OCter in estuaries and coastal seas. High-latitude estuaries play a key role in the coupling between terrestrial and marine carbon pools. In contrast to the general perception, this thesis shows that they are not only transportation areas for DOCter from rivers to the ocean, but are also active sites for transformation, degradation and sedimentation of DOCter, as well as for POCter. In a rapidly changing climate, the importance of these areas for the coupling between inorganic and organic carbon pools cannot be underestimated. / <p>At the time of the doctoral defense, the following papers were unpublished and had a status as follows: Paper 1: In press. Paper 2: Submitted. Paper 4: Manuscript.</p>

Le TOC des sédiments du système Gange-Brahmapoutre croît linéairement avec la proportion de phylosilicates et de particules fines. La proportion de Corg fossile est ~ 20 % dans les MES et > 50 % dans les sédiments de fond. Plus de 50 % du Corg dérivé de l'Himalaya est oxydé et remplacé lors du transport dans la plaine du Gange. La charge en Corg est similaire dans les sédiments du Cône et dans les sédiments de rivière. L'abondance et le d13C des biomarqueurs indique que le Corg est dominé par les apports terrigènes. Par conséquent, l'efficacité d'enfouissement du Corg terrigène est proche de 100 %. Dans le système himalayen, nous estimons les flux d'enfouissement de Corg récent et fossile à respectivement 3.1±0.3 × 1011 mol/an et 0.9±0.4 × 1011 mol/an. L'enfouissement de Corg représente donc ~ 80 % de la consommation de CO2 engendrée par l'érosion de l'Himalaya. De manière générale, les orogènes actifs se caractérisent probablement par un enfouissement efficace de Corg / In the Ganga-Brahmaputra system, TOC linearly increases with the relative proportion of philosilicates and fine grain minerals. The proportion of fossil Corg in the suspended and bed sediments is respectively ~ 20 % and > 50 % of the TOC. During the Gangetic floodplain transit, more than 50 % of recent Corg derived from the Himalaya is oxidised and is replaced by Corg derived from the floodplain. The Corg loadings of river and recent Bengal Fan sediments are comparable. Biomarker abundance and ð13C show that Corg is dominated by terrestrial inputs. Consequently, the terrestrial Corg burial efficiency must be around 100 %. In the Himalayan basin, we estimate the burial fluxes or recent and fossil Corg to be respectively 3.1±0.3 × 1011 mol/yr and 0.9±0.4 × 1011 mol/yr. Corg burial therefore account for ~ 80 % of atmospheric CO2 consumption generated by Himalayan erosion. Efficient burial of Corg is likely a characteristic of high physical erosion typical of active orogenic systems

L'évolution de la législation en matière de valorisation des déchets organiques incite au développement de filières de valorisation, parmi lesquelles le compostage présente un intérêt d'amendement pour les sols, lié notamment à la présence de substances humiques. La matière organique (MO) est une composante importante du sol en raison de son rôle dans les équilibres physiques, chimiques et biologiques, ainsi que par son implication dans le comportement des métaux et métaux traces (MMT). Les objectifs de cette thèse étaient de développer une approche méthodologique afin de caractériser la MO du sol (MOS) et étudier son évolution spatio-temporelle suite à l’apport d’un compost sur une année et 2 profondeurs, et d'approcher son impact sur le comportement des MMT. Une procédure d’extraction séquentielle en 4 étapes (eau, acide, soude, pyrophosphate) a été réalisée afin de fractionner la MOS. Des analyses quantitatives et qualitatives, ont été effectuées sur les extraits. La procédure de fractionnent chimique a permis de distinguer plusieurs catégories de composés organiques (labiles, fulviques et humiques plus ou moins aromatiques). Les analyses quantitatives et les réponses spectrales sur les extraits ont révélé un effet compost essentiellement les trois premiers mois après l’épandage et en été, avec un impact des paramètres climatiques au cours de l'année, mais pas au-delà de 15 cm. Le compost peut apporter au sol une charge supplémentaire en MMT, notamment potentiellement mobilisables, avec un risque de contamination modéré, mais non négligeable lié aux effets potentiels d’accumulation et de concentration sur le long terme. / The evolution of the legislation regarding the valorization of biowaste (green manure) induces the development of valorization chains, among which amending soils with compost is of particular interest, due to the presence of humic substances. Organic matter (OM) is an important component of the soil due to its physical, chemical and biological participation, and its implication in the behaviour of metals and trace metals (MTM).The aims of this thesis were to develop a methodological approach to characterize OM of soil (SOM) and to study its spatiotemporal evolution over one year at two different depths following the addition of compost, and its impact on the behaviour of MTM. A 4-step sequential extraction procedure (water, acid, sodium hydroxide, pyrophosphate) was used to the SOM fractionation. Quantitative and qualitative analysis were applied on extracts. Solubilization kinetics of MTM was also carried out to refine the study of their mobility.The chemical fractionation procedure allowed distinguishing several classes of organic compounds (labile, fulvic and humic with various aromaticity). Quantitative analyzes and spectral responses of the extracts revealed an effect of the compost (organic carbon, metals, aromaticity and molecular weight compounds) essentially during the first three months after spreading and during the summer period, with a climate parameter effect during the year, but not beyond 15 cm of depth. Compost can bring to the soil an additional load of MTM, including potentially mobilized forms, with a moderate, but not negligible risk of contamination, due to the potential effects of accumulation and concentration over the long term.

The trophic state of lakes is commonly defined by the concentration of nutrients in the water column. High nutrient concentrations generate high phytoplankton production, and lakes with low nutrient concentrations are considered low-productive. This simplified view of lake productivity ignores the fact that benthic primary producers and heterotrophic bacteria can be important basal producers in lake ecosystems. In this thesis I have studied clear-water and brown-water lakes with respect to primary production, respiration and bacterial production based on allochthonous organic carbon. These processes were quantified in pelagic and benthic habitats on temporal and spatial scales. I also calculated the net ecosystem production of the lakes, defined as the difference between gross primary production (GPP) and respiration (R). The net ecosystem production indicates whether a lake is net heterotrophic (GPP &lt; R), net autotrophic (GPP &gt; R) or in metabolic balance (GPP = R). Net heterotrophic lakes are sources of carbon dioxide (CO2) to the atmosphere since respiration in these lakes, by definition, is subsidized by an external organic carbon source. External organic carbon is transported to lakes from the terrestrial environment via inlets, and can serve as a carbon source for bacteria but it also limits light availability for primary producers by absorbing light. On a seasonal scale, four of the clear-water lakes studied in this thesis were dominated by primary production in the soft-bottom benthic habitat and by respiration in the pelagic habitat. Concentrations of dissolved organic carbon (DOC) were low in the lakes, but still high enough to cause the lakes to be net heterotrophic. However, the lakes were not low-productive due to the high production in the benthic habitat. One of the clear-water lakes was studied also during the winter and much of the respiration under ice was supported by the benthic primary production from the previous summer. This is in contrast to brown-water lakes where winter respiration is suggested to be supported by allochthonous organic carbon. By studying lakes in a DOC gradient (i.e. from clear-water to brown-water lakes) I could draw two major conclusions. The lakes became less productive since benthic primary production decreased with increasing light extinction, and the lakes became larger sources of CO2 to the atmosphere since pelagic respiration was subsidized by allochthonous organic carbon. Thus, lake carbon metabolism can have an important role in the global carbon cycle due to their processing of terrestrial organic carbon and to their possible feedback effects on the climate system.

One of the modern times worst environmental problem are polluted water resources. An example of source of pollution to water resources are, heavy metal leached from acid sulfate soils (ASS). When these soils are stable, which they are if they are left underwater in an anoxic environment (for example below the water table), they are often sought after since they consist of high amount of nutrients which farmers use as farmlands. ASS is therefore created when farmers drain their land and the sulfide soil gets exposed to air, resulting in its oxidation and therefore formation of sulfuric acid. In a previous study performed by scientists from Linnaeus University, it was concluded that a natural reserve located in Vattenriket, Kristianstad was possibly damaged by the drainage discharge of an adjacent acid sulfate soil. For remediation of acid sulfate soil, notably removal of metals from drainage waters, grounded coffee has been suggested to be able to perform well as an adsorbent. This study was performed to investigate how well grounded coffee could be used as an adsorbent, for calcium (Ca) and zinc (Zn), from water samples collected in Vattenriket, Kristianstad. It was also studied to see if grounded coffee could be cleaned using a sodium hydroxide solution to increase its adsorption capacity. To be able to evaluate how well it could be used as an adsorbent, it went through two different cleaning procedures and total organic carbon and pH readings was performed. The used method for this paper was to clean the grounded coffee in two different stages. The first stage consisted of using distilled water and letting it run through the residues until the water came out as transparent. Cleaning using a NaOH solution consisted of suspending the residues in a NaOH solution for 45 minutes and swapping the solution 6-8 times. After the grounded coffee had dried in an oven at 30o for 48 hours, it was put into different fraction sizes, weighed and bagged. The water samples then had to be filtered using a pump and Filtropur S 0.45 filters. Lastly, 45 falcon tubes containing 15 different amounts of grounded coffee had 50 ml of filtered water sample added to them. For analysis, atomic absorption spectroscopy was used. The results showed that the maximum amount of adsorbed calcium was achieved at 1.5g of grounded coffee in a 50 ml water solution which managed to adsorb 99.53% of calcium. The maximum amount of adsorbed zinc was achieved at 1.25g of grounded coffee in a 50 ml solution which resulted in 99.16% of adsorbed zinc. The study also showed that when the total organic carbon-content was decreasing, due to excessive cleaning, the pH was increasing. This was further proof that the grounded coffee still had residues onto its surface that could inhibit its adsorption capabilities.

Orientador: Rafael Montanari / Resumo: A qualidade do solo não é algo que se pode medir diretamente, no entanto, pode ser avaliada pelos atributos que caracterizam seu estado físico, químico e biológico. A escolha de atributos mais relevantes e a interpretação das medidas obtidas não é algo simples, devido aos efeitos da mudança de uso da terra e as interações entre eles e as condições climáticas e serviços ecossistêmicos de cada região. O objetivo desse estudo foi fornecer uma visão geral de alguns indicadores de qualidade física e química do solo no contexto de restauração de pastagens do Cerrado Brasileiro. A tese é disposta em capítulos, compondo além das considerações gerais apresentadas no Capítulo 1, os Capítulos 2 e 3, que são estudos científicos de avaliação da qualidade física e química do solo. Os experimentos foram desenvolvidos no município de Selvíria – MS em duas áreas destinadas à pecuária extensiva de corte, subsidiadas pela planta forrageira Urochloa brizantha cv. Marandu. Malhas experimentais de 2,7 e 1,4 hectares, com 70 e 65 pontos, respectivamente, foram instaladas nas áreas e amostras de solo de estrutura deformada e indeformada foram tomadas para avaliação dos atributos físicos e químicos. Também se avaliou os estoques de carbono orgânico total, suas frações granulométricas e a emissão de CO2 nas áreas, visando enxergar os efeitos da reforma sob o aporte de carbono e as emissões de gases de efeito estufa. Em uma das áreas avaliou-se a curva de retenção de água do solo e índice S em todos os... (Resumo completo, clicar acesso eletrônico abaixo) / Abstract: Soil quality is not something that can be directly measured; however, it can be assessed by the attributes that characterize its physical, chemical and biological state. The choice of more relevant attributes and the interpretation of the measures obtained is not a simple matter, due to the effects of land use change and the interactions between them, the climatic conditions and ecosystem services of each region. The aim of this study was to provide an overview of some indicators of physical and chemical quality of the soil in the context of pasture restoration in the Brazilian Cerrado. The thesis is laid out in chapters, composing in addition to the general considerations presented in Chapter 1, Chapters 2 and 3, which are scientific studies to assess the physical and chemical quality of the soil. The experiments were carried out in the municipality of Selvíria – MS in two areas for extensive beef cattle, subsidized by the forage plant Urochloa brizantha cv. Marandu. Experimental meshes of 2.7 and 1.4 hectares, with 70 and 65 points, respectively, were installed in the areas and soil samples of deformed and undeformed structure were taken to assess the physical and chemical attributes. The total organic carbon stocks, their particle size fractions and the CO2 emission in the areas were also evaluated, aiming to see the effects of the reform under the carbon input and the greenhouse gas emissions. In one of the areas, the soil water retention curve and S index were evaluated ... (Complete abstract click electronic access below) / Doutor

The drive of the EU countries and most of the world towards a circular economy and togenerate zero waste raised a need to study more efficient and less costly treatment processes. The treatment of secondary and by-product fractions to convert them from what is considered waste to a resource will contribute to the movement towards zero waste and circular economy. The fines fraction of construction and demolition waste (CDW) contains high organic materials measured as total organic carbon TOC above the allowed landfilling levels that are allowed for landfilling in Sweden, yet lower organic matter than is required for energy recovery by incineration. The need for new processes to reuse and recycle materials have emphasized the work of thisstudy, this thesis research aims to develop viable, simple treatment methods and pathways ofrecycling systems to convert by-products that are considered waste to reusable and treatable fractions by reducing the total organic carbon TOC. Which have been defined in the researchquestion of this study “How can functional recycling become more effective through the development of innovative treatment pathways for by-products of the recycling system”? and its sub-questions. This study examined a fines fraction from the CDW sorting in Norway using mechanicalseparation methods including single and combined sequential processes of air classificationand float/sink density separation. Using single process batch separation of float/sink had produced a 73.80% weight of the original fines fraction, with reduced TOC from originally 35.54% DM to 4.09% DM which can be considered to be landfilled as non-hazardous provided that it meets all other leachateanalysis criterion, on the other hand, the process produced concentrated the organic carbon inthe float fraction giving a TOC of 40.14% DM to consider treating it with energy recovery. Using a single separation process of high air velocity with the zigzag air classification has lowered the TOC of 19.49% weight of the treated fraction to 1.8% DM from 35.54% DM of the original fines fraction, which can be considered to be landfilled as inert waste if it meetsall other leachate analysis criterion, or can be considered to be used in road base layers, and concentrated the organic carbon in the other fraction to TOC of 19.90% DM that which need further treatment. Using sequential air classification followed by float/sink sequentialseparation produced different low TOC fractions suitable for landfilling in the categoriesinert, non-hazardous, and hazardous waste in Sweden and concentrated the organic content toTOC levels of 20-48% DM TOC which can be considered for energy recovery recycling. The use of sequential density separation processes can lead to better results and can be controlled more to produced better fractions. The conclusion of this study, using float/sink and airclassification separation methods as single or combined sequential processes had successfully produced two fractions firstly the reduced the total organic carbon separated fraction to be suitable the landfilling requirements in Sweden at the same time concentrated the organicmaterial of the other fraction to be suitable for incineration.

No description available.

This thesis is focused on technological processes during drinking water treatment. The emphasis is put on monitoring indicators of organic substances present in water and indicators of the biological stability of treated water. The experimental part is focused on the comparison of separation efficiency of drinking water treatment technological processes by monitoring of chemical oxygen demand, absorbance measured at 254 nm, bioseston, culturable microorganisms and assimilable organic carbon.

Les prairies permanentes sont reconnues pour les nombreux services agronomiques et environnementaux qu’elles fournissent. Cependant, elles sont aujourd’hui encore retournées ou menacées de l’être au profit de productions plus rentables, ou abandonnées dans le cas des prairies humides où les conditions d’exploitation sont soumises à de nombreuses contraintes. Concilier objectifs de production et environnementaux afin de maintenir une activité agricole extensive au sein des prairies temporaires s’avère alors indispensable. Dans ce contexte, des études multi-services ont été réalisées au sein des prairies humides du Parc Naturel Régional (PNR) des marais du Cotentin et du Bessin (Normandie) ainsi que dans des prairies mésophilesaux conditions pédoclimatiques contrastées situées en Normandie, en Lorraine et en Auvergne. L’étude s’est focalisée sur 3 catégories de services écosystémiques (SE) telles que définis par le Millenium Ecosystem Assessment: la diversité floristique et fonctionnelle comme services de support, la qualité et la production du fourrage comme services d’approvisionnement et les stocks de carbone organique et les teneurs en carbone soluble du sol comme services de régulation. Afin de mettre en évidence la part du fonctionnement des communautés végétales dans le déterminisme des SE, la mesure de traits fonctionnels foliaires a été réalisée à l’échelle de l’espèce et/ou de la communauté végétale. Une partie de ces travaux se focalise sur les relations entre le fonctionnement des communautés végétales et la qualité du fourrage ainsi que l’impact des conditions hydriques du solsur les teneurs en micronutriments des espèces dans les prairies humides.Les résultats ont mis en évidence, qu’en fonction du groupe fonctionnel considéré, le SLA ou le LDMC étaient de bons proxies de la digestibilité des fourrages des prairieshumides. Les dicotylédones ont des teneurs en micronutriments plus élevées que les monocotylédones. Nos résultats montrent que l’inondation influence plus la composition élémentaire des espèces intolérantes aux inondations que les espèces adaptées et qu’elle n’a pas incidence sur la production de biomasse. De manière générale, le fonctionnement des communautés végétales n’explique pas à lui seul les relations entre les SE. La qualité du fourrage est liée au fonctionnement des communautés végétales ainsi qu’à la diversité floristique et fonctionnelle mais seulement en prairies humides. En prairies mésophiles, l’historique de la gestion ou la structure du paysage pourrait être déterminants. Par ailleurs, nos résultats montrent que les stocks de C organique dans le sol des prairies mésophiles et humides sont étroitement liés à sa nature.Les indicateurs des SE combinent les prairies humides en 4 groupes distincts en selon la nature du sol et la gestion (fauche ou pâturage). Globalement, les bouquets de services rendus par les prairies humides sont mieux équilibrés que ceux rendus par les prairies mésophiles, ces derniers ne se distinguant pas les uns des autres selon la localisation géographique des prairies mésophiles. Les prairies gérées de manière extensive fournissent de meilleurs services environnementaux que des prairies gérées de manière intensive et une qualité fourragère équivalente. / Permanent grasslands are recognized for the many agronomic and environmental services they provide. However, they are still plowed or threatened to be in favor of more productive cultures, or abandoned in the case of wet grasslands, where the conditions of exploitation are subjected to many constraints. Reconciling production and environmental objectives in order to maintain extensive agricultural activities is therefore essential in permanent grasslands. In this context, multi-service studies have been carried out in the wet grasslands of the Regional Natural Park (PNR) of the Cotentin and Bessin marshes (Normandy, France) as well as in a set of mesophilous grasslandsofcontrasting pedoclimatic conditions located in Normandy, Lorraine and Auvergne. The study focused on 3 categories of Ecosystem Services (ES) as defined by the Millennium Ecosystem Assessment: floristic and functional diversity as support services, quality and forage production as supply services and stocks of organic carbon and soluble carbon soil contents as regulatory services. In order to analyzethe role of plant community functioning in the ES determinism, the measurement of leaf functional traits was carried out at the species and/or the plant community scales. Part of this work focuses particularly on the relationships between plant communities functioning and forage quality, and soil moisture conditions impact on micronutrient contents of species in wet grasslands. The results showed that, depending on the functional group, SLA or LDMC were good proxies for the digestibility of wet grassland forages. Dicots have higher micronutrient contents than Monocots. Our results show that flooding influences the elemental composition of flood-intolerant species more than adapted species and does not affect biomass production. In general, the plant community functioning does not explain all the relationship between ESs. Forage quality is linked to the plant community functioning as well as thefloristic and functional diversity but only forwet grasslands. In mesophilic grasslands, the history of management or the landscape structure could be important drivers. In addition, our results show that organic C stocks in the soil of wet and mesophilic grasslands are closely related to soil nature. ESs indicators have brought together 4 distinct groups of wet grasslands according to soil nature and management practices (mowing or grazing). Overall, the ESs packages offered by wet grasslands are better balanced than those provided by mesophilic grasslands, the latter being indistinguishable from another according to the geographical location. Extensively managed grasslands provide better environmental services than intensively managed grasslands and equivalent forage quality.