Bibliografías temáticas / Water-clay interaction

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Literatura académica sobre el tema "Water-clay interaction"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 1 de febrero de 2022

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Artículos de revistas sobre el tema "Water-clay interaction"

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El-Sheikhy, Refat, and Mosleh Al-Shamrani. "Fast Laboratory Test for Mechanism of Natural Nanoclay-Water Interaction." Advanced Materials Research 214 (February 2011): 426–29. http://dx.doi.org/10.4028/www.scientific.net/amr.214.426.

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The relation between nanoclay and water effects is very complicated. Interactions of water and nano size type of silicate –aluminum is more complicated due to the special properties of nano material. A new simple technique is developed for studying the swelling phenomenon which represents the most important property of clay-water relation. The developed technique could find more aspects of water-clay behavior. The swelling property is not always only disadvantage with bad effects but sometimes has very important advantages. A comparison and differences with conventional clay-water are made. Th
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Sobolev, O., F. Favre Buivin, E. Kemner, et al. "Water–clay surface interaction: A neutron scattering study." Chemical Physics 374, no. 1-3 (2010): 55–61. http://dx.doi.org/10.1016/j.chemphys.2010.06.012.

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Iwata, S., F. Izumi, and A. Tsukamoto. "Differential heat of water adsorption for montmorillonite, kaolinite and allophane." Clay Minerals 24, no. 3 (1989): 505–12. http://dx.doi.org/10.1180/claymin.1989.024.3.04.

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AbstractDifferential heat of water vapour adsorption for Cs+-saturated montmorillonite, kaolinite and allophane was measured over a low relative humidity range from 10−4 to 10−1. Two interactions (clay surface atom-water and counterion-water) are mainly involved in the water vapour adsorption process. To assess the affinity of water to the clay surface, the amounts of adsorbed water and the differential heat due to Cs+ were estimated from equilibrium constants in the gas phase reactions. It is tentatively concluded that (i) a dominant role of water adsorption due to the Cs+-water interaction i
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4

Yang, Yu, Sanjeev Adhikari, and Guoyuan Xu. "Molecular Dynamics Simulation in the Interlayer of Mixed-Layer Clays Due to Hydration and Swelling Mechanism." Crystals 11, no. 6 (2021): 586. http://dx.doi.org/10.3390/cryst11060586.

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The swelling behavior of clay minerals is widely known for its importance in soil and environmental sciences and its detrimental effects in engineering fields. Although more than 70 percent of all clays are of mixed-layer types, the vast majority of the previous experiments and simulations are focused on pure clays, which cause the swelling mechanism of the widespread mixed-layer clay (MLC) and its role in soils are little understood, especially the most common illite-montmorillonite (I-M) mixed-layer clay (MLC). This paper reports on a molecular dynamics (MD) study of the differences in swell
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5

Sun, He-mei, Wei Yang, Ren-peng Chen, and Xin Kang. "A coarse-grained water model for mesoscale simulation of clay-water interaction." Journal of Molecular Liquids 318 (November 2020): 114085. http://dx.doi.org/10.1016/j.molliq.2020.114085.

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Lin, Yuan, Huaitao Qin, Jin Guo, and Jiawang Chen. "Study on the Rheological Behavior of a Model Clay Sediment." Journal of Marine Science and Engineering 9, no. 1 (2021): 81. http://dx.doi.org/10.3390/jmse9010081.

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Clay sediments are the main component of seabed sediment. Interactions between the nano-sized, disk-shaped and charged clay particles are complicated, as they control the sediment’s rheology. In this study, we studied the rheological behavior of the clay sediment modeled by laponite and bentonite suspensions experimentally using a rotational rheometer. The yield stress decreased when water content increased. Meanwhile, the yield stress of the laponite suspension first increased and then decreased with increasing salinity. It is considered that the face-to-face repulsive electrostatic interacti
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7

Díaz-Pérez, A., I. Cortés-Monroy, and J. C. Roegiers. "The role of water/clay interaction in the shale characterization." Journal of Petroleum Science and Engineering 58, no. 1-2 (2007): 83–98. http://dx.doi.org/10.1016/j.petrol.2006.11.011.

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Sun, Y., H. Lin, and P. F. Low. "The nonspecific interaction of water with the surfaces of clay minerals." Journal of Colloid and Interface Science 112, no. 2 (1986): 556–64. http://dx.doi.org/10.1016/0021-9797(86)90126-8.

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Katti, Dinesh R., Lakshmikanth Srinivasamurthy, and Kalpana S. Katti. "Molecular modeling of initiation of interlayer swelling in Na–montmorillonite expansive clay." Canadian Geotechnical Journal 52, no. 9 (2015): 1385–95. http://dx.doi.org/10.1139/cgj-2014-0309.

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Expansive soils are found in many parts of the world. A major constituent of these clays is the mineral montmorillonite. Molecular interactions between clay, cations, and water play an important role in swelling. Molecular models of Na–montmorillonite clay are constructed, and solvation studies are conducted using molecular dynamics. Analysis of molecular trajectories, conformations, and interaction energies reveal key mechanisms that initiate interlayer swelling. In the initially dry interlayer, the interlayer collapses due to strong attractive interactions between Na ions and clay sheets. Th
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Primanti, Ima Sandra, and Oteng Haridjaja. "Phonska Fertilizer Leaching and Its Effect on Spinach Growth and Productivity (Amaranthus tricolor. L) on Latosol with Different Clay Content." Jurnal Ilmu Tanah dan Lingkungan 7, no. 1 (2005): 22–26. http://dx.doi.org/10.29244/jitl.7.1.22-26.

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Sufficient available water in soil is very essential for plant growth, not only as a nutrient solvent but also to maintainoptimal turgor pressure. Occasionally, additional water supply from irrigation is necessary to achieve optimal soil water,:ondition. The aim of this research was to study leaching of several nutrients correlated to the growth and productivity ofspinach. PHONSKA fertilizer as a source of nutrients was applied to Latosols Darmaga having different clay content. Thetreatments were subjected to different level of water supply resulting in different soil moisture regime. Factoria
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Tesis sobre el tema "Water-clay interaction"

1

Song, Weikang. "Experimental investigation of water evaporation from sand and clay using an environmental chamber." Thesis, Paris Est, 2014. http://www.theses.fr/2014PEST1047/document.

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Il est bien connu que l'évaporation d'eau joue un rôle essentiel dans l'interaction entre le sol et l'atmosphère. Pendant le processus d'évaporation, le comportement thermo-hydro-mécanique des sols change, engendrant ainsi des problèmes préoccupants. Ceci peut concerner différents domaines comme l'agronomie, l'hydrologie, la science des sols, la géotechnique, etc. Par conséquent, il est essentiel d'étudier les mécanismes d'évaporation de façon approfondie. Cette étude porte sur les mécanismes d'évaporation dans des conditions atmosphériques contrôlées. Le sable de Fontainebleau et l'argile d'H
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2

Vidal, Emanuella Layne Ferreira. "Avalia??o do comportamento de argila ativada na presen?a de ?gua destilada, solu??es salinas e inibidores de hidrata??o cati?nicos." Universidade Federal do Rio Grande do Norte, 2009. http://repositorio.ufrn.br:8080/jspui/handle/123456789/17603.

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Made available in DSpace on 2014-12-17T15:41:44Z (GMT). No. of bitstreams: 1 EmanuellaLFV.pdf: 2331935 bytes, checksum: 3f4df9b602349e41bf8ab4d2c561b59d (MD5) Previous issue date: 2009-01-14<br>Coordena??o de Aperfei?oamento de Pessoal de N?vel Superior<br>The clay swelling is today one of the major problems during the well drilling. Nearly 50% of clays that constitute shale expand easily in the presence of water molecules. During the drilling of a geological formation containing swelling clays, when is feasible the use of water base fluids, it is necessary to apply clay inhibitors. This av
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3

Shewring, Nigel Ivor Edward. "Interactions at the clay/polymer/water interface." Thesis, Sheffield Hallam University, 1998. http://shura.shu.ac.uk/20358/.

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The thesis investigates the behaviour of aqueous montmorillonite suspensions and also the interactions between montmorillonite as a free standing film and in highly dispersed aqueous suspension with water soluble polymers used as additives in water based drilling fluids. FTIR microscopy and FTIR ATR spectroscopy have been employed to study in-situ dehydration of fully dispersed aqueous montmorillonite suspensions. The IR spectrum of the dispersed bentonite shows significant differences from that of a dry bentonite powder, which have been attributed to the hydration of the exchangeable cation.
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Libros sobre el tema "Water-clay interaction"

1

Velde, B. The origin of clay minerals in soils and weathered rocks. Springer, 2008.

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Velde, B. The origin of clay minerals in soils and weathered rocks. Springer, 2008.

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3

Alain, Meunier, ed. The origin of clay minerals in soils and weathered rocks. Springer, 2008.

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4

Merritt, Michael L. Simulation of the interaction of karstic lakes Magnolia and Brooklyn with the upper Floridan Aquifer, southwestern Clay County, Florida. U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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5

Netzer, Falko P., and Claudine Noguera. Oxide Thin Films and Nanostructures. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780198834618.001.0001.

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Nanostructured oxide materials ultra-thin films, nanoparticles and other nanometer-scale objects play prominent roles in many aspects of our every-day life, in nature and in technological applications, among which is the all-oxide electronics of tomorrow. Due to their reduced dimensions and dimensionality, they strongly interact with their environment gaseous atmosphere, water or support. Their novel physical and chemical properties are the subject of this book from both a fundamental and an applied perspective. It reviews and illustrates the various methodologies for their growth, fabrication
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Capítulos de libros sobre el tema "Water-clay interaction"

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Velde, Bruce, and Alain Meunier. "Clay Mineral Formation in Weathered Rocks: Water/Rock Interaction." In The Origin of Clay Minerals in Soils and Weathered Rocks. Springer Berlin Heidelberg, 2008. http://dx.doi.org/10.1007/978-3-540-75634-7_4.

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Donnert, D., S. H. Eberle, and J. Horst. "Kinetic Studies on the Interaction of Metals between Water and Clay Mineral." In Metal Speciation in the Environment. Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-74206-4_8.

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Green, R. E. "Pesticide-Clay-Water Interactions." In Pesticides in Soil and Water. Soil Science Society of America, 2015. http://dx.doi.org/10.2136/1974.pesticides.c2.

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Geptner, A. R., V. V. Petrova, and H. Kristmannsdottir. "On biochemical genesis of clay minerals in basalts, Iceland." In Water-Rock Interaction. Routledge, 2021. http://dx.doi.org/10.1201/9780203734049-61.

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Huaiyan, Lei, Fu Wanjun, and Shi Yuxin. "Enhanced gas generation by clay mineral catalysis of source rocks." In Water-Rock Interaction. Routledge, 2021. http://dx.doi.org/10.1201/9780203734049-64.

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Beaucaire, C., P. Toulhoat, and H. Pitsch. "Chemical characterisation and modelling of the interstitial fluid in the Boom clay formation." In Water-Rock Interaction. Routledge, 2021. http://dx.doi.org/10.1201/9780203734049-194.

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Sanyal, Saheli, Harsh Anjirwala, Meet Bhatia, et al. "Interaction of Clay–Crude Oil–Injection Brine: An Experimental Approach for Understanding the Effectiveness of Low Saline Water (LSW) During Enhanced Oil Recovery (EOR)." In Macromolecular Characterization of Hydrocarbons for Sustainable Future. Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-33-6133-1_4.

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Chen, Chi-Wei, Vincent Gaudefroy, Myriam Duc, Yannick Descantes, Ferhat Hammoum, and Jean-Pierre Magnan. "A Mineralogical Approach of the Interactions Between Bitumen, Clay and Water in Hot Mix Asphalt (HMA)." In RILEM Bookseries. Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-7342-3_6.

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Netzer, Falko P., and Claudine Noguera. "Clay mineral layers and nanoparticles." In Oxide Thin Films and Nanostructures. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780198834618.003.0007.

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This chapter provides an introduction to the properties of naturally occurring oxide ultra-thin films and nanoparticles of complex composition, namely clay minerals. Clays represent a wide family of nanomaterials, formed from the weathering of primary rocks at the Earth surface. Their layered structure is responsible for their extreme anisotropy and their extremely high specific surface area which is at the origin of their unique properties and of their strong interaction with their surrounding. The focus of this chapter is on their structural and composition characteristics, the conditions of their formation, their interaction with water and their chemical properties. A mention is given of their uses in human cultural activities, in dwelling constructions and statuary, in porcelain fabrication, in retention of metal contaminants in the environment, in the pharmaceutical and cosmetic industries, and as lubricants, catalysts, therapeuthic agents, among others.
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Minear, Roger A., and Mark A. Nanny. "Solution and Condensed Phase Characterization." In Nuclear Magnetic Resonance Spectroscopy in Environment Chemistry. Oxford University Press, 1997. http://dx.doi.org/10.1093/oso/9780195097511.003.0012.

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Improvements in nuclear magnetic resonance (NMR) instrumentation, magnetic field strength, pulse sequences, and computer technology and software have increased the range of applications and specific elements available for study by NMR. The five chapters in this Part clearly indicate the benefits of these advances, especially regarding studies of aquatic, environmental significance. Each of the studies focuses on environmentally significant issues. For example, chlorination is widely used to disinfect drinking waters, a method that can produce undesirable disinfection by-products. This was first recognized in 1974 with the discovery of trihalomethanes in most finished drinking waters where hypochlorite was used for disinfection. Chapter 7 examines the chlorination of alanine and relates it to the chlorination reactions of acetaldehyde and ammonia, a topic of importance with respect to drinking water disinfection. Aluminum is also widely used in drinking water treatment, and understanding its hydrolysis chemistry and complexation behavior is of great importance to aquatic chemistry. In addition, the aquatic chemistry of aluminum is important because acid rain can release soluble aluminum ions from clay into soil water, possibly damaging terrestrial plant life. Aluminum may eventually reach and accumulate in hydrological systems where it can be toxic to aquatic life. Chapters 8 and 9 focus on 27Al NMR in defining aqueous aluminum speciation in a mildly acidic solution or in the presence of complexing organic compounds. Furthermore, aluminum is of environmental and geochemical significance since it is an integral component of clays, another ubiquitous constituent of natural waters (surface and ground). Interaction between clays, cations, and internal water molecules can be significant in understanding the fate and transport of chemicals through the environment. Since colloidal suspensions of clay materials frequently represent challenges to water and wastewater treatment, understanding of physical and chemical processes are of tantamount importance to the environmental scientist and engineer. Chapter 10 explores cation behavior in clay matrices by using “uncommon” nuclei such as 7Li, 23Na, and 133Cs as probes. This is unique in that many NMR studies of complexation in clay have focused primarily upon the nuclei 27A1 and 29Si.
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Actas de conferencias sobre el tema "Water-clay interaction"

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Mese, Ali I. "Clay‐water interaction, intermolecular forces and acoustic velocity." In SEG Technical Program Expanded Abstracts 2008. Society of Exploration Geophysicists, 2008. http://dx.doi.org/10.1190/1.3059218.

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Letertre, T., M. W. Ben Ayoub, E. Georgin, A. L. Neves, P. Pouliguen, and P. Sabouroux. "Influence of the Temperature in a Water/Clay Mixture." In 2018 12th International Conference on Electromagnetic Wave Interaction with Water and Moist Substances (ISEMA). IEEE, 2018. http://dx.doi.org/10.1109/isema.2018.8442294.

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Schmidt, D. D., A. J. Roos, and J. T. Cline. "Interaction of Water With Organophilic Clay in Base Oils To Build Viscosity." In SPE Annual Technical Conference and Exhibition. Society of Petroleum Engineers, 1987. http://dx.doi.org/10.2118/16683-ms.

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Bore, Thierry, Norman Wagner, Antoine Coperey, Markus Loewer, Andre Revil, and Alexander Scheuermann. "Analysis of Interfacial Water in Clay by High Frequency Dielectric Relaxation Spectroscopy." In 2021 13th International Conference on Electromagnetic Wave Interaction with Water and Moist Substances (ISEMA). IEEE, 2021. http://dx.doi.org/10.1109/isema49699.2021.9508278.

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Zhao, Rixin, Shuangfang Lu, and Haitao Xue. "Wettability Alteration and Oil-Water-Rock Interaction at Hydrated Kaolinite Clay Mineral Surfaces." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.3168.

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Al-Heed, Mohammed, Mobeen Murtaza, Sayed Hussain, and Rahul Gajbhiye. "A New Cationic Shale Inhibitor and Water Blocking Agent for Water-Based Drilling Fluid." In IADC/SPE Asia Pacific Drilling Technology Conference. SPE, 2021. http://dx.doi.org/10.2118/201055-ms.

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Abstract Drilling a shale formation is one of the challenges faced by the petroleum industry. Designing the drilling fluid, that reduces the interaction with shale, is important for safe and efficient drilling. This study investigates the new cationic surfactant as a shale inhibitor for the drilling fluid. The main objective of this study is to block the water penetration into the clay layers using the new shale inhibitor and evaluate its performance with commercial shale inhibitors. To assess the performance of new cationic surfactant two reliable clay sources were considered. The first sourc
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Fagundes, Diego F., Khader I. Rammah, Marcio S. S. Almeida, Julio Pequeno, Jose Renato M. S. Oliveira, and Ricardo Garske Borges. "Strength Behaviour Analysis of an Offshore Brazilian Marine Clay." In ASME 2012 31st International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/omae2012-83008.

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The main purpose of this paper is to describe the geotechnical behaviour of a deep water marine clay obtained from Campos basin oil field located offshore the state of Rio de Janeiro in Brazil. The soil samples were obtained at a depth of about 1500 m using a Kullenberg piston corer. Characterization tests were undertaken on the clay samples, including water content, Atterberg limits, particle size distribution and specific density. Isotropic and anisotropic undrained triaxial tests were also carried out on both normal and over-consolidated samples to assess both the conventional strength and
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8

Fouzder, Anup, Arash Zakeri, and Bipul Hawlader. "Steel Catenary Risers at Touchdown Zone: A Fluid Dynamics Approach to Understanding the Water-Riser-Soil Interaction." In 2012 9th International Pipeline Conference. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/ipc2012-90283.

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The critical location for fatigue damage in Steel Catenary Riser’s (SCR’s) often occurs within the Touchdown Zone (TDZ), where cyclic interaction of the riser with the seabed takes place. Riser-fluid-soil interaction at the TDZ is a complex phenomenon. In this study, Computational Fluid Dynamics (CFD) technique is used to investigate the velocity field and suction forces during riser-fluid-soil interaction for a two-dimensional cross section of 0.10 m diameter SCR at TDZ. Numerical simulation shows that the suction forces at the bottom of the riser are high enough to pull the clay upward when
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Pasic, Borivoje, Nediljka Gaurina-Medjimurec, and Bojan Moslavac. "Application of Artificial Clay Samples (Pellets) in Laboratory Testing of Shale/Drilling Fluid Interaction." In ASME 2013 32nd International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2013. http://dx.doi.org/10.1115/omae2013-10211.

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Wellbore instability was and is one of the most frequent problems in petroleum industry, especially in the drilling operations. It is mainly caused by the shale formations which represent 75% of all drilled formations. The wellbore instability problems involve tight hole spots, wellbore diameter enlargement, the appearance of cavings, the inability of carrying out wireline operations, poor hole cleaning, unsuccessful wellbore cementing operations and other. The wellbore instability is the result of mechanical and physico-chemical causes mostly acting concurrently. The shale instability basical
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Emami Azadi, M. R. "Influence of Spud-Can-Soil Interaction Modeling and Parameters on the Reliability Index of Neka Drilling Jack-Up Platform." In ASME 2008 International Mechanical Engineering Congress and Exposition. ASMEDC, 2008. http://dx.doi.org/10.1115/imece2008-66092.

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In the present study, the influence of spud-can-soil modeling and parameters on the reliability index of jack-up platform is investigated. Neka platform is studied as a case which is a 3-leg drilling jack-up type platform located in water depth of about 91m in Caspian Sea region. Various spud-can-soil interaction models such as pinned, fixed-base, hyper-elastic and non-linear elasto-plastic spud-can models are applied. The soil type is varied from loose to dense sand and also from soft NC-clay to very stiff OC-Clay. The effects of bias and COV of the spud-can-soil interaction modeling and also
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Informes sobre el tema "Water-clay interaction"

1

Cushman, J. H. Supercomputer simulation of clay-water-chemical interactions, Phase 3. Office of Scientific and Technical Information (OSTI), 1991. http://dx.doi.org/10.2172/5746634.

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Cushman, J., D. Diestler, P. Low, and C. Roth. Supercomputer simulation of clay-organic-water interactions: Phase 2. Office of Scientific and Technical Information (OSTI), 1989. http://dx.doi.org/10.2172/6907081.

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Cushman, J. H. Supercomputer simulation of clay-water-chemical interactions, Phase 3. Progress report, 15 April 1991--30 December 1991. Office of Scientific and Technical Information (OSTI), 1991. http://dx.doi.org/10.2172/10130322.

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