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Dissertations / Theses on the topic 'Mineral associated organic carbon'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

Heyes, Andrew. "Mineral weathering by dissolved organic carbon in subarctic fens." Thesis, McGill University, 1990. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=59647.

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The contribution of dissolved organic carbon (DOC) to mineral weathering was investigated under the changing Eh and pH conditions in three subarctic fens, near Schefferville, Quebec. No evidence of increased weathering rates nor different weathering patterns were found in the fen basal sediment despite DOC-rich and low Eh (0 to +200 mV) conditions.<br>Solutions containing 50 mg DOC/L derived from subarctic fen peat, and of 50 and 300 mg DOC/L, derived from deciduous leaf litter were used as weathering agents. Clinochlore, microcline and the Fe-rich basal till from the Schefferville fens were u

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2

Robertson, David R. K. "Organo-mineral interactions : implications for carbon burial and preservation." Thesis, University of Newcastle Upon Tyne, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.273518.

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3

Yeasmin, Sabina. "An Assessment of Mineral–Organic Matter Associations in Soils." Thesis, The University of Sydney, 2016. http://hdl.handle.net/2123/15543.

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This study aimed to obtain a better understanding on the mechanisms and controls of mineral–organic matter (OM) interactions across a range of soil types and land uses. Batch adsorption experiments were conducted to evaluate sorption capacity of different organic carbon (OC) compounds on pure minerals and their interaction mechanisms were determined by infrared spectroscopy. Role of mineralogy on the dynamics of soil OM pools was assessed in four cropped soils with contrasting mineralogy by sequential density fractionation and chemical treatments. Effect of land use change on soil OM pools als

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4

Bynoe, Kisandra Nicole Natasha. "Factors controlling the retention and release of dissolved organic carbon in upland organo-mineral soils." Thesis, University of Leeds, 2016. http://etheses.whiterose.ac.uk/16119/.

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Soils play a significant role in the movement of Dissolved Organic Carbon (DOC) within a catchment and are a major source of DOC to surface waters. Recent DOC increases in some surface waters in Europe and North America could be indicative of changes in soils leading to greater export of DOC. Organo-mineral soils have the ability to act as both sources and sinks for DOC due to the presence of a large organic layer as well as mineral horizon(s). However, the role of these soils in the movement of DOC within catchments requires further research. This study investigated the factors controlling th

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5

Zhou, Zhe. "Fe(II)-catalyzed transformation of ferrihydrite associated with natural organic matter." Diss., University of Iowa, 2018. https://ir.uiowa.edu/etd/6670.

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The association between natural organic matter (NOM) and iron (Fe) minerals was widely found in soil and sediments and has been shown to impact the fate of Fe minerals and NOM. Ferrihydrite, a ubiquitous Fe mineral, serves as important sink for NOM and rapidly transforms to secondary Fe minerals in the presence of Fe(II). The associated NOM has been found to influence the Fe(II)-catalyzed ferrihydrite transformation pathway, but it remains unclear how various NOM affects this transformation and the implication. This study specifically investigates how different species of NOM affect Fe(II)-cat

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6

Simonetti, Gianluca. "Mechanisms of soil organic matter protection and sequestration." Doctoral thesis, Università degli studi di Padova, 2010. http://hdl.handle.net/11577/3422238.

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Soil organic carbon (SOC) protection processes have received much interest recently due to the possibility to enhance the carbon sink in agricultural soils with atmospheric CO2 reduction purposes. Further knowledge of these mechanisms is thus fundamental to promote effective C sequestration practices in terrestrial sinks, as recognized by Article 3.4 of the Kyoto Protocol. In a long-term experiment established in the early 1960s in north-eastern Italy, we used a combination of physical fractionation and chemical extraction techniques aiming to isolate homogeneous pools of SOC. In particular we

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7

Thomalla, S. J. "Particulate organic carbon and mineral export from the North and South Atlantic gyres : the 234Th/238U disequilibrium approach." Doctoral thesis, University of Cape Town, 2007. http://hdl.handle.net/11427/6452.

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Includes bibliographical references (leaves 228-270).<br>Subtropical ocean gyres are typically characterised by low carbon export into the deep ocean. However, due to their large area, even relatively small average carbon export may be globally significant. Strong correlations observed between deep-sea organic carbon, calcite and opal suggest that mineral phases may enhance the export and survival of organic matter as it sinks (the 'ballast effect'). However, the processes underlying these correlations are not well understood and remain key uncertainties in models that predict global carbon cy

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8

Lyu, Han. "EFFECTS OF CLIMATE AND GEOCHEMISTRY ON SECONDARY MINERAL DISTRIBUTION AND SOIL ORGANIC CARBON POOLS IN TROPICAL VOLCANIC REGIONS." Doctoral thesis, Kyoto University, 2021. http://hdl.handle.net/2433/263813.

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9

Heckman, Katherine Ann. "Pedogenesis & Carbon Dynamics Across a Lithosequence Under Ponderosa Pine." Diss., The University of Arizona, 2010. http://hdl.handle.net/10150/196016.

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Three studies were completed to investigate the influence of mineral assemblage on soil organic carbon (SOC) cycling and pedogenesis in forest soils. Two studies utilized a lithosequence of four parent materials (rhyolite, granite, basalt, limestone/volcanic cinders) under Pinus ponderosa, to explicitly quantify the contribution of parent material mineral assemblage to the character of the resulting soil. The first study explored variation in pedogenesis and elemental mass loss as a product of parent material through a combination of quantitative X-ray diffraction and elemental mass balance. R

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10

Burant, Aniela S. "Fate of Organic Compounds in High Salinity Waters and Supercritical CO2 Associated with Carbon Storage Environments." Research Showcase @ CMU, 2015. http://repository.cmu.edu/dissertations/602.

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Carbon capture, utilization, and storage (CCUS), including enhanced oil recovery (EOR), is one of the most promising mitigation strategies for climate change. CCUS involves the capture of CO2 from point sources and the subsequent injection of that CO2 into geologic storage formations. Depleted oil reservoirs will be the first targets of CCUS due to the economic benefits associated with EOR. EOR operations are expected to produce large volumes of wastewater brines with the crude oil. Brines, which can have high concentrations of salts and dissolved organic compounds; and CO2, which can have dis

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11

Kothawala, Dolly N. "Controls on the soil solution partitioning of dissolved organic carbon and nitrogen in the mineral horizons of forested soils." Thesis, McGill University, 2009. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=115565.

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Note:<br>The soil-solution partitioning of dissolved organic carbon (DOC) withinmineral soil horizons is primarily controlled by processes of adsorption and desorption. These abiotic processes largely occur within a short equilibration time of seconds to minutes, which generally occur faster than microbial processes. To characterise the adsorption of DOC to mineral soils, I used the Langmuir adsorption isotherm, which holds several advantages to the commonly used linear initial mass (IM) isotherm. One advantage to using the Langmuir isotherm is anestimation of the maximum DOC adsorption capaci

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12

Kothawala, Dolly N. 1972. "Controls on the soil solution partitioning of dissolved organic carbon and nitrogen in the mineral horizons of forested soils." Thesis, McGill University, 2009. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=115858.

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The soil-solution partitioning of dissolved organic carbon (DOC) within mineral soil horizons is primarily controlled by processes of adsorption and desorption. These abiotic processes largely occur within a short equilibration time of seconds to minutes, which generally occur faster than microbial processes. To characterise the adsorption of DOC to mineral soils, I used the Langmuir adsorption isotherm, which holds several advantages to the commonly used linear initial mass (IM) isotherm. One advantage to using the Langmuir isotherm is an estimation of the maximum DOC adsorption capacity (Qma

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13

Dorji, Tshering. "Soil organic carbon variability under montane ecosystems: assessing the influence of landscape attributes." Thesis, The University of Sydney, 2015. http://hdl.handle.net/2123/14811.

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Soil organic carbon (SOC) is integral to soil functioning and serves as a common indicator for soil security, water security, food security, energy security, climate change abatement, biodiversity protection, and ecosystem service. Since SOC varies in space and time, its quantification is essential to better understand the carbon (C) dynamics at various scales. As a gamut of montane ecosystems, the Himalayan region serves as one of the major C storage pools in the world due to its rich biodiversity and good forest cover. However, much of the Himalayan region is environmentally vulnerable becau

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14

Chen, Yujuan. "The Influence of Urban Soil Rehabilitation on Soil Carbon Dynamics, Greenhouse Gas Emission, and Stormwater Mitigation." Diss., Virginia Tech, 2013. http://hdl.handle.net/10919/51240.

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Global urbanization has resulted in rapidly increased urban land. Soils are the foundation that supports plant growth and human activities in urban areas. Furthermore, urban soils have potential to provide a carbon sink to mitigate greenhouse gas emission and climate change. However, typical urban land development practices including vegetation clearing, topsoil removal, stockpiling, compaction, grading and building result in degraded soils. In this work, we evaluated an urban soil rehabilitation technique that includes compost incorporation to a 60-cm depth via deep tillage followed by more t

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15

Weiglein, Tyler Lorenz. "A Continental-Scale Investigation of Factors Controlling the Vulnerability of Soil Organic Matter in Mineral Horizons to Decomposition." Thesis, Virginia Tech, 2019. http://hdl.handle.net/10919/101987.

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Soil organic matter (SOM) is the largest terrestrial pool of organic carbon (C), and potential carbon-climate feedbacks involving SOM decomposition could exacerbate anthropogenic climate change. Despite the importance of SOM in the global C cycle, our understanding of the controls on SOM stabilization and decomposition is still developing, and as such, SOM dynamics are a source of major uncertainty in current Earth system models (ESMs), which reduces the effectiveness of these models in predicting the efficacy of climate change mitigation strategies. To improve our understanding of controls on

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16

Koren, Lindsey Michelle. "Influence of Salinity Variations on the Desorption and Lability of Soil Organic Carbon Associated with Tidal Freshwater Marshes." VCU Scholars Compass, 2009. http://hdl.handle.net/10156/2465.

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17

Njeru, Sarah Kangai. "Tillage effects on the aggregate-associated organic carbon and bulk density in some South African soils with different texture." Thesis, University of Fort Hare, 2015. http://hdl.handle.net/10353/2512.

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Tillage operations disrupt the soil structure resulting in aggregates of various sizes and altered bulk density. Moreover, tillage influences soil carbon pools and many other soil physical properties. The objectives of this study were to determine, in various South African soils under different tillage systems, the following. (1) Amount of aggregate-associated soil organic carbon (SOC), (2) soil compressibility, and (3) relationship between compressibility, texture and the aggregate-associated SOC. The soil samples used in this study were collected from six different sites in Eastern Cape Prov

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18

Zakharova, Anna. "Soil organic matter dynamics: influence of soil disturbance on labile pools." Thesis, University of Canterbury. School of Biological Sciences, 2014. http://hdl.handle.net/10092/9944.

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Soils are the largest pool of carbon (C) in terrestrial ecosystems and store 1500 Gt of C in their soil organic matter (SOM). SOM is a dynamic, complex and heterogeneous mixture, which influences soil quality through a wide range of soil properties. Labile SOM comprises a small fraction of total SOM (approximately 5%), but due to its rapid turnover has been suggested to be most vulnerable to loss following soil disturbance. This research was undertaken to examine the consequences of soil disturbance on labile SOM, its availability and protection in soils using the isotopic analysis of soil-res

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19

Kanari, Eva. "Understand and use the estimation of soil organic carbon persistence by Rock-Eval® thermal analysis." Electronic Thesis or Diss., Sorbonne université, 2022. http://www.theses.fr/2022SORUS037.

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A la croisée de la terre solide et de l'atmosphère, les sols forment le plus grand réservoir terrestre de carbone organique, contenant deux fois plus de carbone que l'atmosphère et la végétation réunies, et constituant un contrôle majeur sur le flux des gaz à effet de serre. En outre, le carbone organique des sols (COS) est essentiel pour leur santé et fertilité, ainsi que pour la qualité de l'eau. La précision de l'outil le plus précieux dont nous disposons pour prédire l'évolution de ce réservoir, les modèles de dynamique du COS, est limitée par notre capacité à estimer la proportion du COS

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20

Kyulavski, Vladislav Dimitrov. "Greenhouse gas emissions and soil carbon stocks associated with crop residues and organic fertilizers mixtures in sugar cane cropping systems." Thesis, La Réunion, 2019. https://elgebar.univ-reunion.fr/login?url=http://thesesenligne.univ.run/19_27_VDKyulav.pdf.

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Dans le contexte environnemental actuel il est nécessaire d’optimiser l’utilisation des ressources pour réduire les déchets et les émissions de gaz à effet de serre (GES). L’utilisation de ressources renouvelables et le recyclage sont au cœur du modèle d’économie circulaire, selon lequel le déchet est une ressource mobilisable, transformable, réutilisable et par conséquent non limitée. En agriculture, le cercle vertueux de l’économie circulaire peut être mis en place à travers le recyclage des matières organiques en tant que fertilisants et l’adoption d’une approche agroécologique qui privilég

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21

Wissing, Livia Verfasser], Ingrid [Akademischer Betreuer] [Kögel-Knabner, and Wulf [Akademischer Betreuer] Amelung. "Evolution of mineral-associated organic matter in paddy soils – a chronosequence study / Livia Wissing. Gutachter: Ingrid Kögel-Knabner ; Wulf Amelung. Betreuer: Ingrid Kögel-Knabner." München : Universitätsbibliothek der TU München, 2013. http://d-nb.info/1032693274/34.

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22

Franks, Matthew James. "The Role of Soil Organic Matter and Fe- and Mn-(Oxy)Hydroxide Minerals in Agriculture: Implications on Nutrient Dynamics." Bowling Green State University / OhioLINK, 2020. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1594151828787397.

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23

Ma, Li. "Soil Organic Nitrogen - Investigation of Soil Amino Acids and Proteinaceous Compounds." Diss., Virginia Tech, 2015. http://hdl.handle.net/10919/51960.

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Soil carbon (C) and nitrogen (N) are predominantly in organic form. Proteins/ peptides, as an important organic form of N, constitute a substantial part of soil organic matter. On one hand, proteins/peptides are an important N source for plants and microorganisms, particularly in soils where inorganic N is limited. On the other hand, their stabilization in soils by forming organo-mineral associates or macromolecule complex reduces the C loss as CO2 into the atmosphere. Therefore, studies on the turnover, abundance, composition, and stability of proteins/peptides are of crucial importance to ag

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24

Biau, Aresté Anna. "Stover management, organic and mineral nitrogen fertilization effects on maize production and soil quality under irrigated Mediterranean conditions." Doctoral thesis, Universitat de Lleida, 2013. http://hdl.handle.net/10803/123965.

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El rostoll dels cultius te un paper molt important en el manteniment de la fertilitat del sòl. L’incorporació del rostoll al sòl afecta favorablement els nivells de matèria orgànica (MO) i per tant l'estructura del sòl, l'emmagatzematge i el moviment d'aigua i aire, i altres determinants de la productivitat del sòl. Retornar el rostoll de blat de moro al sòl també contribueix al segrest de carboni (C) afavorint la reducció de l'emissió de gasos d'efecte hivernacle. La interacció entre la gestió del rostoll i la fertilització nitrogenada (N) pot ajudar a millorar l'eficiència d'ús de N, alhora

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25

Moon, Jinyoung. "Selective accrual and dynamics of proteinaceous compounds during pedogenesis: testing source and sink selection hypotheses." Diss., Virginia Tech, 2015. http://hdl.handle.net/10919/77030.

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The emerging evidence of preferential accumulation and long residence time of proteinaceous compounds in soil are counter to the traditional view that their structure is readily broken down through microbial activity. The shift in thinking of their residence time is, however, heavily influenced by physical and chemical protections in soil, representing an important change for understanding global biogeochemical carbon and nitrogen cycling. We investigated the accumulation patterns of proteinogenic amino acids for a long term (thousands of years) related to their sources and sinks. We found cle

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26

Vogel, Cordula Verfasser], Ingrid [Akademischer Betreuer] [Kögel-Knabner, Markus Akademischer Betreuer] Kleber, and Georg [Akademischer Betreuer] [Guggenberger. "Micro-structures generated by the mineral phase determine the fate of organic carbon and nitrogen in soil / Cordula Vogel. Gutachter: Markus Kleber ; Ingrid Kögel-Knabner ; Georg Guggenberger. Betreuer: Ingrid Kögel-Knabner." München : Universitätsbibliothek der TU München, 2015. http://d-nb.info/1075317177/34.

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27

Piccoli, Ilaria. "CHALLENGES OF CONSERVATION AGRICULTURE ON SILTY SOILS. DISENTANGLING THE EFFECTS OF CONSERVATION PRACTICES ON SOIL ORGANIC CARBON CYCLE AND SOIL PORE NETWORK IN NORTH-EASTERN ITALY." Doctoral thesis, Università degli studi di Padova, 2017. http://hdl.handle.net/11577/3424845.

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Soil organic matter loss is a widely recognized European soil threat and intensive and repeated tillage operations are known to negatively affect numerous soil properties and ecosystem services. In this view, the study on more sustainable agronomic managements is a pressing need for research community. Between sustainable techniques, conservation agriculture (CA) is nowadays a spread technique based on three main pivotal points: 1) minimum soil disturbance, 2) permanent soil covering and 3) crop diversification. CA is often associated with numerous soil functions such as increasing of soil bio

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28

Torres, Bocero Irene Florentina. "Dynamics of carbon in degraded semiarid soils : effects of organic amendments and associated soil microbial communities= Dinámica del carbono en suelos degradados de zonas semiáridas: implicación de enmiendas orgánicas y comunidades microbianas asociadas." Doctoral thesis, Universidad de Murcia, 2015. http://hdl.handle.net/10803/313226.

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El suelo desempeña funciones de gran importancia para el sustento de la vida en este planeta pero la desertificación producida en el mismo, en las zonas áridas o semiáridas, repercute notoriamente en una abundante pérdida de materia orgánica, y por tanto de carbono orgánico, la cual afecta negativamente a la calidad y la sostenibilidad del suelo. La recuperación del carbono orgánico del suelo hacia unos valores umbrales suficientes para poder gestionar sus funciones básicas es de vital importancia. Por este motivo, la presente Tesis Doctoral tiene como Objetivo entender el ciclo del carbono en

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29

Noirot-Cosson, Paul-Emile. "Optimisation de l'insertion des Produits Résiduaires Organiques dans les systèmes de cultures d'un territoire francilien : évolution des stocks de carbone organique et substitution des engrais minéraux." Thesis, Paris, AgroParisTech, 2016. http://www.theses.fr/2016AGPT0011/document.

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L’utilisation des Produits Résiduaires Organiques (PRO) par l’agriculture peut permettre de substituer une partie des engrais minéraux et augmenter les niveaux de matière organique des sols. Elle peut également générer des pollutions azotées via la lixiviation de nitrate ou des émissions gazeuses. Mieux connaitre le devenir du carbone (C) et de l’azote (N) après applications de PRO sur les sols agricoles contribue à améliorer les bénéfices de cette pratique et à en limiter les impacts environnementaux. Cette thèse a pour objectif: (i) de prédire les dynamiques du C et du N en cas d’application

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30

Lamotte, Jean. "Etude par spectroscopie infrarouge des proprietes superficielles de la thorine et des especes adsorbees resultant de l'interaction co + h : :(2)." Caen, 1987. http://www.theses.fr/1987CAEN2047.

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31

Yaacoubi, Abdelrani. "Etude de l'influence d'ions metalliques et de composes organiques sur l'adsorption du dodecyl sulfate de sodium sur charbon actif." Poitiers, 1988. http://www.theses.fr/1988POIT2286.

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Les resultats experimentaux (cinetique rapide d'adsorption, parametre d'equilibre des isothermes d'adsorption et variation du potentiel zeta des particules de charbon) montrent une augmentation de la capacite d'adsorption du dodecylsulfate de sodium en presence d'ions metalliques et une inhibition mutuelle de l'adsorption en presence d'alcools aliphatiques et de composes organiques

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32

ABDALLAH, KHODR. "Contribution experimentale a l'etude de la cinetique d'adsorption de gaz." Paris, ENSAM, 1989. http://www.theses.fr/1989ENAM0003.

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Une nouvelle technique experimentale a ete mise au point pour etudier la cinetique d'adsorption due aux transferts de masse et de chaleur. Application a l'adsorption du methanol sur la zeolite x et le charbon actif

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33

Masri, Ahlam El. "Influence de la modification de la surface des électrodes sur la réduction du monoxyde de carbone et l'oxydation de dialdéhydes et de dialcools." Grenoble INPG, 1986. http://www.theses.fr/1986INPG0003.

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Sur Pt et Pt platine, la reduction de Co en milieu organique contenant de l'eau, conduit a la formation de methanol avec un rendement de 47% : co+4h**(+)+4e**(-)->ch::(3)oh. Le potentiel auquel a lieu cette reaction (-2,5 vvsag/ag**(+)10**(-2)m, est en accord aec une reduction simultanee de co et de h**(+) et une reaction entre les especes adsorbees sur l'electrode d'influence des adatomes sur les produits issus de l'oxydation du glyoxal et de l'ethylene glycol a ete etudiee en milieu hclo::(4) hclo::(4),n, h::(2)so::(4)2m et kno::(3)m de concentration de certaines especes, comme l'acide glyox

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34

Allali-Hassani, Mohamed. "Etude de l'adsorption de tensioactifs non ioniques sur charbon actif : influence de coadsorbats, essai de modelisation." Poitiers, 1988. http://www.theses.fr/1988POIT2284.

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L'adsorption de l'alkylphenolpolyethoxyle sur une poudre de charbon actif a ete etudiee seule, puis en presence de nacl et cacl::(2), d'alcool (ethanol a pentanol, tertiobutanol) et d'agents de surface anioniques

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35

Souabi, Salah. "Etude de l'adsorption de tensioactifs cationiques sur charbon actif influence de coadsorbats /." Grenoble 2 : ANRT, 1988. http://catalogue.bnf.fr/ark:/12148/cb376186543.

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36

Chgoura, Mohammed. "Adsorption par des charbons actifs de molécules organiques à partir de solutions aqueuses." Aix-Marseille 1, 1987. http://www.theses.fr/1987AIX11082.

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37

Ayed, Othman. "Etude des interactions entre atomes alcalins (li, na, k) et monoxyde de carbone en matrices de gaz rares : analyse en spectroscopie vibrationnelle et calcul quantiques de quelques complexes." Paris 6, 1987. http://www.theses.fr/1987PA066117.

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Dans le cas de li(le plus reactif), identification de li(co)::(n), ou n = 1,2,3,4,(ou 6), avec des frequences de vibration de valence de co plus perturbees que pour les metaux de transition carbonyle,et de li::(m) co, ou m = 2,3, avec frequences nu (co) abaissees. Pour na et k, observation d'especes de haute stoechiometrie (c::(n)o::(n))**(2-) (m**(+))::(2) ou n = 2,3,4, formees apres irradiation uv-visible et correspondant a des transformations chimiques. Essai d'interpretation de ces differences de reactivite par une description quantique des agregats de plus basse stoechiometrie : dans le c

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38

Brodbeck, Claude. "Transitions doubles induites par collisions dans des melanges gazeux comprimes." Paris 6, 1987. http://www.theses.fr/1987PA066285.

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Etude des transitions doubles (simultanees) correspondant a l'absorption d'un seul photon par deux molecules en interaction pour les systemes gazeux comprimes : h::(2) + cf::(4) ou sf::(6), o::(2) ou n::(2) + sf::(6), n::(2) + co::(2). Determination de coefficients d'absorption binaire integres et des profils normalises que l'on compare aux valeurs theoriques calculees en utilisant le moment dipolaire induit et l'intensite de la transition induite en fonction des regles de selection sur les nombres quantiques. Choix des differents parametres caracterisant les deux molecules et leur potentiel d

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39

Pyle, Lacey Ann. "Isolating the effect of mineral-organic interactions on the decomposition of recalcitrant organic soil carbon." Thesis, 2012. http://hdl.handle.net/2152/ETD-UT-2012-08-6341.

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Recalcitrant soil carbon is a poorly understood component of total soil organic carbon (SOC). Although the turnover rate of the recalcitrant fraction is slow, warming temperatures are expected to speed the decomposition of recalcitrant SOC resulting in an increase of atmospheric CO₂ in the future. Several studies show that the oldest SOC is associated with the smallest mineral particles (clays), making direct spectroscopic analysis of old carbon difficult. To overcome the difficulty of analyzing natural samples, we created synthetic soils to examine the association between clay surfaces and sp

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40

Howard, Matthew T. "Modeling of particulate organic carbon fluxes in the ocean with mineral ballasting." 2004. http://catalog.hathitrust.org/api/volumes/oclc/58481605.html.

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Thesis (M.S.)--University of Wisconsin--Madison, 2004.<br>Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (p. 39-43).

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41

Russo, Fabio. "Interaction of recombinant and disease-associated prion proteins with organic and mineral soil colloids." Tesi di dottorato, 2008. http://www.fedoa.unina.it/1697/1/Russo_Agrobiologia_e_Agrochimica.pdf.

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42

LaCroix, Rachelle. "Mineral and Redox Controls on Soil Carbon Cycling in Seasonally Flooded Soils." 2018. https://scholarworks.umass.edu/masters_theses_2/725.

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Soils contain nearly three times the amount of carbon (C) than the atmosphere, with C turnover times ranging from centuries to millennia. Although wetland soils represent a relatively small portion of the terrestrial landscape, they account for an estimated 20-30% of the global C reservoir. Seasonally flooded soils are likely the most vulnerable wetlands to climate change, as changing temperature and precipitation patterns are expected to alter the timing and duration of flooding. Seasonal variations in soil moisture are recognized as a critical control on soil C stocks and CO2emissions. Howev

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Kumari, Poonam. "Study of soil carbon sequestration due to land use changes and associated soil modification." Thesis, 2018. http://localhost:8080/iit/handle/2074/7762.

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44

"Seasonal storage of fine-grained sediment in the lowermost Mississippi and Atchafalaya Rivers and an analysis of associated terrestrial organic carbon." Tulane University, 2005.

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Abstract:

Geophysical and geological data collected during cruises conducted on the lowermost Mississippi and Atchafalaya Rivers from 1999 through 2004 investigated the seasonal storage patterns of fine-grained sediment and the associated terrestrial organic carbon (TOC). We found that in the estuarine section of the Mississippi River, storage was dominated by estuarine trapping associated with salt-water wedge intrusion, with rapid rates of accumulation (mm-cm/day), whereas the Atchafalaya showed little wedge intrusion or storage due to the presence of un-dredged river-mouth bars. Above the estuarine r

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