Bibliografías temáticas / Salt formation

Literatura académica sobre el tema "Salt formation"

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Publicado: 11 de marzo de 2023

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Artículos de revistas sobre el tema "Salt formation"

1

Makary, Patrick. "Principles of Salt Formation". UK Journal of Pharmaceutical Biosciences 2, n.º 4 (1 de agosto de 2014): 1. http://dx.doi.org/10.20510/ukjpb/2/i4/91101.

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Guadarrama-Cetina, J., A. Mongruel, W. González-Viñas y D. Beysens. "Frost formation with salt". EPL (Europhysics Letters) 110, n.º 5 (1 de junio de 2015): 56002. http://dx.doi.org/10.1209/0295-5075/110/56002.

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Clegg, Nicola A. y Ralf Toumi. "Non-sea-salt-sulphate formation in sea-salt aerosol". Journal of Geophysical Research: Atmospheres 103, n.º D23 (1 de diciembre de 1998): 31095–102. http://dx.doi.org/10.1029/98jd02595.

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Escapa, Mauricio, Gerardo M. E. Perillo y Oscar Iribarne. "Biogeomorphically driven salt pan formation in Sarcocornia-dominated salt-marshes". Geomorphology 228 (enero de 2015): 147–57. http://dx.doi.org/10.1016/j.geomorph.2014.08.032.

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Lewis, Andrew L. y Howard C. K. Stokes. "Formation of a Stabilised Phospholane Salt". Journal of Chemical Research 23, n.º 10 (octubre de 1999): 612–13. http://dx.doi.org/10.1177/174751989902301013.

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N,N′-Substituted amines (as illustrated using TMEDA) will react with a short chain 2-alkoxy-2-oxo-1,3,2-dioxaphospholane, to form a stabilised phospholane salt and not the corresponding phosphobetaine as anticipated.
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Dongyan, WEI, DENG Xiaolin, LIU Zhenmin y YANG Gengsheng. "On Biochemical Formation of Salt Deposits". Acta Geologica Sinica - English Edition 74, n.º 3 (7 de septiembre de 2010): 613–17. http://dx.doi.org/10.1111/j.1755-6724.2000.tb00032.x.

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Lewis, Andrew L. y Howard C. K. Stokes. "Formation of a Stabilised Phospholane Salt". Journal of Chemical Research, n.º 10 (1999): 612–13. http://dx.doi.org/10.1039/a904940a.

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Serajuddin, Abu T. M. "Salt formation to improve drug solubility". Advanced Drug Delivery Reviews 59, n.º 7 (julio de 2007): 603–16. http://dx.doi.org/10.1016/j.addr.2007.05.010.

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Hussain, Syed Asim, Feng-Qing Han, Jibin Han, Hawas Khan y David Widory. "Chlorine isotopes unravel conditions of formation of the Neoproterozoic rock salts from the Salt Range Formation, Pakistan". Canadian Journal of Earth Sciences 57, n.º 6 (junio de 2020): 698–708. http://dx.doi.org/10.1139/cjes-2019-0149.

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During the late Neoproterozoic, the Salt Range in Pakistan was one of the regions where the Tethys truncated and marine strata developed. The numerous transgressions and regressions that occurred during that period provided enough initial material for the development of marine evaporites. The geology of the Salt Range is characterized by the presence of dense salt layers and the existence of four regional and local scale unconformities. These thick salt deposits geologically favor potash formation. Here we coupled chloride isotope geochemistry and classical chemistry of local halite samples to assess the extent of brine evaporation that ultimately formed the salt deposits. Our results indicate that evaporites in the Salt Range area are Br-rich and precipitated from seawater under arid climate conditions. The corresponding δ37Cl values vary from –1.04‰ to 1.07‰, with an average of –0.25‰ ± 0.52‰, consistent with the isotope range values reported for other evaporites worldwide. The positive δ37Cl values we obtained indicate the addition of nonmarine Cl, possibly from reworking of older evaporites, the influx of dilute seawater, the mixing of meteoric and seawater, and the influence of gypsum-dehydration water. The negative Cl isotope compositions (δ37Cl < –1‰) indicate that brines reached the last stages of salt deposition during the late Neoproterozoic. We conclude that the Salt Range Formation could be promising for K-Mg salts.
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Sigfridsson, Kalle, Lena Nilsson, Matti Ahlqvist, Thomas Andersson y Anna-Karin Granath. "Preformulation investigation and challenges; salt formation, salt disproportionation and hepatic recirculation". European Journal of Pharmaceutical Sciences 104 (junio de 2017): 262–72. http://dx.doi.org/10.1016/j.ejps.2017.03.041.

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Tesis sobre el tema "Salt formation"

1

Lam, Ka Wing. "Pharmaceutical salt formation guided by phase diagrams /". View abstract or full-text, 2009. http://library.ust.hk/cgi/db/thesis.pl?CBME%202009%20LAM.

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Cropper, Paul Edward. "A kinetic template effect in arylphosphonium salt formation". Thesis, Sheffield Hallam University, 1988. http://shura.shu.ac.uk/19513/.

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This thesis describes studies of a "kinetic template effect" which assists the formation of arylphosphonium salts from aryl halides and tertiary phosphines in the presence of a transition metal halide catalyst in refluxing ethanol. The "kinetic template effect" arises from the presence in the aryl halide of a limited range of orthosubstituents capable of intramolecular coordination with the metal at a critical stage of the reaction. In Chapter One, the "kinetic template effect" is compared with the better known "thermodynamic template effect". Earlier work on related "kinetic template effects" in the formation of aryl-phosphorus bonds is reviewed. The evidence for the possible involvement of aryl-metal intermediates in such reactions is also discussed. Chapter Two is concerned with the design and synthesis of potential template molecules. A model is proposed for the features necessary in the template substituent in terms of the nature and position of the donor atom or group essential for the replacement of the ortho-halogen under mild conditions. Chapter Three describes a kinetic study of the nickel (II) catalysed reactions of ortho-haloaryl Schiff's base and ortho-haloarylazo-dyestuff templates with tertiary phosphines. A rate law is deduced which indicates a first order dependence in each reactant, i.e. rate a [template] [phosphine] [catalyst], an overall third order expression. Rate studies also indicate that the nature of the orthohalogen is important, the order of replacement being I > Br > Cl. The effects of substituents remote from the ortho-haloaryl template are also considered. A mechanistic scheme consistent with the rate data is proposed. The X-ray crystal structures of two arylphosphonium salts derived from template aryl halides are discussed in Chapter Four, providing unequivocal proof that the position of replacement of halogen in substrates bearing more than one replaceable halogen, in different positions, is ortho with respect to the template donor group.
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Konishi, Hirokazu. "Formation of Dy Alloy Films by Molten Salt Electrochemical Process". Kyoto University, 2003. http://hdl.handle.net/2433/149313.

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Kyoto University (京都大学)
0048
新制・課程博士
博士(エネルギー科学)
甲第9870号
エネ博第58号
新制||エネ||18(附属図書館)
UT51-2003-C638
京都大学大学院エネルギー科学研究科エネルギー基礎科学専攻
(主査)教授 伊藤 靖彦, 教授 八尾 健, 教授 尾形 幸生
学位規則第4条第1項該当
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4

Ren, Lirong. "Inorganic salt nanofibers as templates for the formation of oxide nanotubes". [S.l. : s.n.], 2004. http://deposit.ddb.de/cgi-bin/dokserv?idn=974105651.

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Chou, Tai-Li. "Kinetics of salt formation using terephthalic acid and N-methyl-2-pyrrolidinone". Thesis, Montana State University, 2004. http://etd.lib.montana.edu/etd/2004/chou/ChouT04.pdf.

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Terephthalic acid (TA) is used as a raw material for producing polyesters. As the global demand for polyesters increases at a rate of 7% per year on average for the last few years and next 10-year forecast, the demand of TA also increases. The global production exceeded 27 million tons for the year 2003, and will be in excess of 30 million tons for the year 2004. Therefore improving the production or purification process for terephthalic acid becomes more and more important. A new purification method using N-methyl-2-pyrrolidinone (NMP) as solvent was recently developed. In this process, the salt complex consisting of TA and NMP was formed to exclude the impurities. The research topic of this thesis was to characterize the salt formation rate and develop possible explanations for salt formation kinetics. Gas Chromatography was used to determine the percentage of salt in the salt formation samples as prepared by varying mixing times, temperatures and loadings. The TA-salt transition (salt formation) was found to behave as first-order solid-solid phase transition with a temperature range where both phases coexist. The salt formation rate was explained using the combination of reaction rate and salt formation possibility.
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6

Elder, David. "Physicochemical and crystallographic investigations into the salt formation of two heterocyclic drugs". Thesis, University of Edinburgh, 1992. http://hdl.handle.net/1842/8721.

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Salt formation provides a means of altering the physicochemical and resultant biological characteristics of a drug entity without modifying its molecular structure. Many published reviews have indicated the importance of the selection of the most appropriate salt form. This work is an investigation into the salt formation of two heterocyclic drugs. This is done by the physicochemical and the crystallographic studies of 19 high resolution single crystal diffraction studies. The particular targets of the work are the selection of the most appropriate salt forms, investigations into the tautomerism and polymorphism (or pseudopolymorphism) and an understanding of the interactions most likely between these heterocyclic drugs and their specific receptor sites. Section 1 describes the effect of protonation on the absorption of drugs, the rationale for using various salt forms and the resultant effect this has on a number of physicochemical properties of the parent compound. Section 2 is a description of the experimental techniques used in the physicochemical investigations and in crystal structure determination. In Sections 3 and 7, the preparation and characterisation of the salts and modifications of the two heterocyclic drugs, GU and IM is described. In Sections 4 and 8, the physicochemical investigations into the hygroscopicity and solid-state stabilities of the salts of GU and IM is described. Van't Hoff solubility studies are used to determine the enthalpies of solution and where appropriate the relative thermodynamic stabilities of the various phases produced. The structures of 19 of the salts or modifications of GU and IM, together with their packing and hydrogen bonding interactions is described in Sections 5 and 9. Sections 6 and 10 describe the ionisation properties of these molecules. Both the guanidine and imidazole moieties of GU and IM, respectively, are tautomeric, the particular form(s) found in these investigations and the effect of protonation is discussed. The conformations of these structures are discussed and the effect of protonation, especially on the puckering of the piperazine ring, is described.
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7

Iida, Takahisa. "Formation of Sm and Yb Alloy Films by Molten Salt Electrochemical Process". Kyoto University, 2003. http://hdl.handle.net/2433/148653.

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Kyoto University (京都大学)
0048
新制・課程博士
博士(エネルギー科学)
甲第10335号
エネ博第71号
新制||エネ||21(附属図書館)
UT51-2003-H756
京都大学大学院エネルギー科学研究科エネルギー基礎科学専攻
(主査)教授 伊藤 靖彦, 教授 八尾 健, 教授 吉田 起國
学位規則第4条第1項該当
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8

Rödner, Sandra. "Interfacial colloidal particle films and their structure formation". Licentiate thesis, KTH, Chemistry, 2002. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-1505.

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Abstract to“Interfacial colloidal particle films andtheir structure formation”; a licentiate thesis, whichwill be presented by Sandra Rödner in Q2, 29 November 2002at 13.00.

Colloidal particles can be made to organise themselves intoordered arrays. These colloidal structures acquire interestingand useful properties, not only from their constituentmaterials but also from the spontaneous emergence of mesoscopicorder that characterises their internal structure. Orderedarrays of colloidal particles, with lattice constants rangingfrom a few nanometers to a few microns, have potentialapplications as optical computing elements and chemicalsensors, and also has an important influence on the mechanicalproperties and optical appearance of paint films and papercoatings.

The control of colloidal structure formation starts with theparticle interactions (attractive or repulsive) and colloidaldynamics, which is the topic of this thesis. To enable adetailed understanding of the different factors that controlthe formation of dense 2D colloidal films, a method forstructural characterisation was developed. The degree of orderin the hexagonal close-packed structure, displayed by thecolloidal films, was characterised by the size of ordereddomains and by the distribution of pore sizes. The size ofordered domains was obtained from the pair distributionfunction, and the distribution of pores from a Delaunaytriangulation procedure. These methods are based on theparticle positions in the film, which were determined by lightmicroscopy and processed digital images.

The two methods were used to study the effect of particleinteractions on the structure of colloidal monoparticulatefilms, formed at the air-liquid interface. The size of theordered domains decreased exponentially with increasing bondstrength, while the pore density increased. The transfer andsubsequent drying of the formed film on a solid substrateinduced structural changes; the capillary forces transformedsmall pores into triangular order while some of the largervoids and cracks increased in size.

The structural features of colloidal monolayers, formed bydrying a dilute silica suspension on a substrate, wereinvestigated. Addition of small amounts of salt resulted indrastic changes of the particle film structure. The size of theordered domains decreased exponentially with increasing amountsof added salt (0-2.9% NaCl/Silica ratio), with a simultaneousincrease of the concentration of large defects. This suggeststhat loss of colloidal stability and onset of particle adhesionto the substrate inhibit rearrangement and ordering. Theevaporation rate was controlled by varying the relativehumidity during drying. Colloidal monolayers with the largestordered domains and the lowest concentration of stacking faultswere formed at an intermediate humidity (55% RH).

The rearrangement process during drying of dilute silicasuspensions was followed in detail by studying the changes inthe structural features during growth of colloidal monolayers.Low crystal growth rate promoted the transition of squarelattice domains to a hexagonal close-packed structure. Additionof salt to the electrostatically stabilised dispersionincreased the formation of square structured regions at thecrystal-suspension interface, due to increasing adhesion to thesubstrate. The loss of colloidal stability inhibited therearrangement process, resulting in higher concentrations ofsquare lattice domains at large distances from the crystal edgecompared to systems without added salt.

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Ziga, Jeffrey Michael. "The Moroni formation in Salt Creek Canyon Central, Utah: implications for paleogene topography". Connect to resource, 2006. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1149600004.

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Robbins, Michael. "Sedimentology and sedimentary tectonics of the Salt Wash Member, Morrison Formation, Western Colorado". Thesis, Boston College, 2009. http://hdl.handle.net/2345/658.

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Thesis advisor: Kenneth G. Galli
Thesis advisor: Noah P. Snyder
The Brushy Basin Member of the Morrison Formation records a time of increased volcanic activity in the North American Cordillera during the Late Jurassic. Sedimentological and petrographic observations in the Brushy Basin, in conjunction with findings of widespread plutonic intrusion in the source areas, point to a volcanic pulse within the Cordilleran magmatic arc. This study investigated the subjacent Salt Wash Member, for the purpose of better constraining the timing of the volcanic pulse. Petrographic and statistical analyses of the Salt Wash sandstone identified statistically significant upsection trends in volcanic rock fragment and plagioclase feldspar at one of the four study areas. The remaining three study areas showed no upsection trends in sandstone composition that would reflect a pulse in volcanism during Salt Wash Member time. It is more likely that the Salt Wash was deposited during a time of volcanic quiescence leading up to the post-Nevadan Orogeny volcanic reactivation. Sedimentology and cementation patterns of the Salt Wash Member were also studied. Cathodoluminescence indicates that the member was well-flushed with shallow formation waters, thus preventing any calcite optical zoning. Luminescence intensity suggests that the Salt Wash Member sediments were cemented at varying depths and within differing Eh-pH regimes. Field-based sedimentological observations support a model of braided stream channel deposition across a semi-arid landscape with streamflow entering the basin from both the south and west
Thesis (MS) — Boston College, 2009
Submitted to: Boston College. Graduate School of Arts and Sciences
Discipline: Geology and Geophysics
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Libros sobre el tema "Salt formation"

1

United States. Dept. of Energy. Albuquerque Operations Office. y Geological Survey (U.S.), eds. Dissolution of halite and gypsum, and hydration of anhydrite to gypsum, Rustler Formation, in the vicinity of the waste isolation pilot plant, southeastern New Mexico. Denver, Colo: U.S. Dept. of the Interior, Geological Survey, 1985.

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Hazel, Joseph E. Sedimentary response to intrabasinal salt tectonism in the Upper Triassic Chinle Formation, Paradox Basin, Utah. Washington: U.S. G.P.O., 1994.

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Tōkyō Daigaku. Kikō Shisutemu Kenkyū Sentā, ed. Role of freshwater forcing and salt transport in the formation of the Atlantic deep circulation. Tokyo]: University of Tokyo, Center for Climate System Research, 2003.

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Pérez, Xosé Luis Otero y Felipe Macías Vazquez. Biogeochemistry and pedogenetic process in saltmarsh and mangrove systems. New York: Nova Science Publishers, 2010.

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Hoffman, Gretchen K. Quality assessment of strippable coals in northwestern New Mexico: Fruitland, Menefee, and Crevasse Canyon Formation coals in San Juan Basin, and Moreno Hill Formation coals in Salt Lake field. Socorro: New Mexico Bureau of Mines & Mineral Resources, 1993.

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Cornell, Vaun. South Africa today: How do we characterise the social formation? : papers from the 2011 ILRIG April Conference, Community House, Salt River, Cape Town, 29 and 30 April 2011. [Cape Town?]: International Labour Research and Information Group (ILRIG), 2011.

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L, Fisher James y Geological Survey (U.S.), eds. Variations in the abundance of occluded light hydrocarbons (Cb1s-Cb5s) and their relation to diagenetic changes, in the Salt Wash Member, Late Jurassic Morrison Formation, Slick Rock district, San Miguel County, Colorado. Denver, CO: U.S. Dept. of the Interior, Geological Survey, 1988.

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International Congress on Toxic Combustion By-products: Formation and Control. Incineration of hazardous waste 2: Toxic combustion by-products : based on the proceedings of the Second International Congress on Toxic Combustion By-products--Formation and Control, University of Utah, Salt Lake City, 26-29 March, 1991. Langhorne, Pa: Gordon and Breach Science Publishers, 1994.

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K, Hoffman Gretchen, Barker James M. 1945- y New Mexico Research and Development Institute., eds. Quality assessment of strippable coals in New Mexico, year III, phase II, Menefee and Crevasse Canyon, and Moreno Hill formation coals in the San Juan Basin of northwestern New Mexico and the Salt Lake coal field, west-central New Mexico. Santa Fe, N.M: New Mexico Research and Development Institute, 1989.

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T, Hussnain, Geological Survey (U.S.) y Geological Survey of Pakistan, eds. Measured stratigraphic sections of the Lower Permian Nilawahan Group, Salt Range, Punjab Province, Pakistan. Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1989.

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Capítulos de libros sobre el tema "Salt formation"

1

Minkley, W., C. Lüdeling y A. Taghichian. "Mechanism for the formation of sinkholes above deep salt caverns". En The Mechanical Behavior of Salt X, 590–603. London: CRC Press, 2022. http://dx.doi.org/10.1201/9781003295808-54.

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Raith, Alexander, Sven Wille, Birgit Horváth y Dirk Zander-Schiebenhöfer. "Integrity of the geological formation barrier - A comprehensive approach for the assessment of salt caverns". En The Mechanical Behavior of Salt X, 545–52. London: CRC Press, 2022. http://dx.doi.org/10.1201/9781003295808-50.

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Bui, T. A., G. Cammarata, V. C. Kancharla y S. Brasile. "Modeling the behavior of underground structures in a rock salt formation: A coupled Finite Element approach". En The Mechanical Behavior of Salt X, 395–406. London: CRC Press, 2022. http://dx.doi.org/10.1201/9781003295808-37.

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Ginzberg, Idit, Yoram Kapulnik y Aviah Zilberstein. "Transcription of Δ1-Pyrroline-5-Carboxylate Synthase in Alfalfa Roots During Salt Stress". En Biology of Root Formation and Development, 279. Boston, MA: Springer US, 1997. http://dx.doi.org/10.1007/978-1-4615-5403-5_59.

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Molemaker, M. Jeroen y Henk A. Dijkstra. "Layer Formation in a Salt Stratified Liquid Cooled from Above". En Geophysical Monograph Series, 97–104. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm094p0097.

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Mianping, Zheng. "Material Sources and Model of Salt Formation of Saline Lakes". En An Introduction to Saline Lakes on the Qinghai—Tibet Plateau, 123–46. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5458-1_7.

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Arai, Tohru y Hatsuhiko Oikawa. "Nitride and Carbide Formation onto Ceramics by Molten Salt Dipping Method". En Sintering ’87, 1385–90. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-1373-8_233.

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Rao, P. N., E. B. Faraghar, A. Buxton, V. Prendiville y N. J. Blacklock. "Is Salt Restriction Necessary to Reduce the Risk of Stone Formation?" En Urolithiasis and Related Clinical Research, 429–32. Boston, MA: Springer US, 1985. http://dx.doi.org/10.1007/978-1-4684-7272-1_91.

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Feigin, Alexander M., Joseph G. Brand, Yuzo Ninomiya, Bruce P. Bryant, Sergey M. Bezrukov, Paul A. Moore, Igor Vodyanoy y John H. Teeter. "Effect of Novobiocin on Cation Channel Formation and Enhancement of Salt Taste". En Olfaction and Taste XI, 104–7. Tokyo: Springer Japan, 1994. http://dx.doi.org/10.1007/978-4-431-68355-1_42.

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Mikkanen, P., E. I. Kauppinen, J. Pyykönen, J. K. Jokiniemi y M. Mäkinen. "Alkali Salt Ash Formation During Black Liquor Combustion at Kraft Recovery Boilers". En Applications of Advanced Technology to Ash-Related Problems in Boilers, 409–23. Boston, MA: Springer US, 1996. http://dx.doi.org/10.1007/978-1-4757-9223-2_27.

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Actas de conferencias sobre el tema "Salt formation"

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Vaghmare, Kaustubh, Sudhanshu Barway, Petri Vaisanen y Ajit Kembhavi. "Star Formation Histories of S0 Galaxies". En SALT Science Conference 2015. Trieste, Italy: Sissa Medialab, 2016. http://dx.doi.org/10.22323/1.250.0012.

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Van Dorp, Quirinius Teunis, Maarten Slijkhuis y Pacelli Lidio Jose Zitha. "Salt Precipitation in Gas Reservoirs". En 8th European Formation Damage Conference. Society of Petroleum Engineers, 2009. http://dx.doi.org/10.2118/122140-ms.

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Loubser, Ilani. "Fuelling (and quenching) star formation in Brightest Cluster Galaxies". En SALT Science Conference 2015. Trieste, Italy: Sissa Medialab, 2016. http://dx.doi.org/10.22323/1.250.0015.

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Kleinitz, W., M. Koehler y G. Dietzsch. "The Precipitation of Salt in Gas Producing Wells". En SPE European Formation Damage Conference. Society of Petroleum Engineers, 2001. http://dx.doi.org/10.2118/68953-ms.

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Zhang, Yuping y Elisabeta Isaj. "Halite Envelope for Downhole Salt Deposition Prediction and Management". En SPE European Formation Damage Conference and Exhibition. Society of Petroleum Engineers, 2015. http://dx.doi.org/10.2118/174206-ms.

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Samuel, Robello y HanYi Wang. "Optimized Centralizer Placement for Pre-Salt Formation". En OTC Brasil. Offshore Technology Conference, 2015. http://dx.doi.org/10.4043/26092-ms.

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Fukuyama, David, Hugh Daigle, Michael Nole y Jennifer Frederick. "Convection initiated by hydrate formation and salt exclusion." En Proposed for presentation at the UT-Austin Academic Alliance LDRD Poster Session held April 08, 2021 in , . US DOE, 2021. http://dx.doi.org/10.2172/1888391.

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Toledo, S., M. Basso, G. Chinelatto, L. De Carvalho Mendes y A. Campane Vidal. "Insights into the Morphology and Seismic Facies of the Barra Velha Formation, Santos Basin Brazil." En Third EAGE Conference on Pre Salt Reservoirs. European Association of Geoscientists & Engineers, 2022. http://dx.doi.org/10.3997/2214-4609.202288038.

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Powers, Michael, Daria Nikitina, Martin F. Helmke, Cameron Knight y Magnus Payzine. "RELATIONSHIP BETWEEN GROUNDWATER FLOW, TIDES, AND SALT POND FORMATION AT THE DELAWARE SALT MARSH". En GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-356816.

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Martins, M., I. Neves, L. Longhi, T. Santos, Y. Camargo, A. Monlevade, K. Conte et al. "Seismic, Well Logs and Cycles Patterns From Pre-Salt Carbonate Reservoir, Macabu Formation, Campos Basin, Brazil." En Third EAGE Conference on Pre Salt Reservoirs. European Association of Geoscientists & Engineers, 2022. http://dx.doi.org/10.3997/2214-4609.202288035.

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Informes sobre el tema "Salt formation"

1

Stormont, J. C. Discontinuous behavior near excavations in a bedded salt formation. Office of Scientific and Technical Information (OSTI), octubre de 1990. http://dx.doi.org/10.2172/6461949.

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Howard, Clifford L. Mechanical and hydrological characterization of the near-field surrounding excavations in a geologic salt formation. Office of Scientific and Technical Information (OSTI), septiembre de 2014. http://dx.doi.org/10.2172/1167522.

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Bigl, Matthew, Sandra LeGrand, Samuel Beal, Ariana Sopher y David Ringelberg. Macroscale salt-crust formation on indoor playa-like test plots for dust-emission research applications : methodology assessment. Engineer Research and Development Center (U.S.), agosto de 2019. http://dx.doi.org/10.21079/11681/33723.

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Chidsey, Thomas C., David E. Eby, Michael D. Vanden Berg y Douglas A. Sprinkel. Microbial Carbonate Reservoirs and Analogs from Utah. Utah Geological Survey, julio de 2021. http://dx.doi.org/10.34191/ss-168.

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Multiple oil discoveries reveal the global scale and economic importance of a distinctive reservoir type composed of possible microbial lacustrine carbonates like the Lower Cretaceous pre-salt reservoirs in deepwater offshore Brazil and Angola. Marine microbialite reservoirs are also important in the Neoproterozoic to lowest Cambrian starta of the South Oman Salt Basin as well as large Paleozoic deposits including those in the Caspian Basin of Kazakhstan (e.g., Tengiz field), and the Cedar Creek Anticline fields and Ordovician Red River “B” horizontal play of the Williston Basin in Montana and North Dakota, respectively. Evaluation of the various microbial fabrics and facies, associated petrophysical properties, diagenesis, and bounding surfaces are critical to understanding these reservoirs. Utah contains unique analogs of microbial hydrocarbon reservoirs in the modern Great Salt Lake and the lacustrine Tertiary (Eocene) Green River Formation (cores and outcrop) within the Uinta Basin of northeastern Utah. Comparable characteristics of both lake environments include shallowwater ramp margins that are susceptible to rapid widespread shoreline changes, as well as compatible water chemistry and temperature ranges that were ideal for microbial growth and formation/deposition of associated carbonate grains. Thus, microbialites in Great Salt Lake and from the Green River Formation exhibit similarities in terms of the variety of microbial textures and fabrics. In addition, Utah has numerous examples of marine microbial carbonates and associated facies that are present in subsurface analog oil field cores.
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Ernest Mancini. Basin Analysis of Mississippi Interior Salt Basin and Petroleum System Modeling of the Jurassic Smackover Formation, Eastern Gulf Coastal Plain. Office of Scientific and Technical Information (OSTI), marzo de 2001. http://dx.doi.org/10.2172/1036744.

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Berkowitz, Jacob, Christine VanZomeren y Nicole Fresard. Rapid formation of iron sulfides alters soil morphology and chemistry following simulated marsh restoration. Engineer Research and Development Center (U.S.), septiembre de 2021. http://dx.doi.org/10.21079/11681/42155.

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Many marshes show signs of degradation due to fragmentation, lack of sediment inputs, and erosion which may be exacerbated by sea level rise and increasing storm frequency/intensity. As a result, resource managers seek to restore marshes via introduction of sediment to increase elevation and stabilize the marsh platform. Recent field observations suggest the rapid formation of iron sulfide (FeS) materials following restoration in several marshes. To investigate, a laboratory microcosm study evaluated the formation of FeS following simulated restoration activities under continually inundated, simulated drought, and simulated tidal conditions. Results indicate that FeS horizon development initiated within 16 days, expanding to encompass > 30% of the soil profile after 120 days under continuously inundated and simulated tidal conditions. Continuously inundated conditions supported higher FeS content compared to other treatments. Dissolved and total Fe and S measurements suggest the movement and diffusion of chemical constituents from native marsh soil upwards into the overlying sediments, driving FeS precipitation. The study highlights the need to consider biogeochemical factors resulting in FeS formation during salt marsh restoration activities. Additional field research is required to link laboratory studies, which may represent a worst-case scenario, with in-situ conditions.
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Mancini, Ernest A. Basin Analysis of the Mississippi Interior Salt Basin and Petroleum System Modeling of the Jurassic Smackover Formation, Eastern Gulf Coastal Plain. Office of Scientific and Technical Information (OSTI), febrero de 2003. http://dx.doi.org/10.2172/807526.

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Ernest A, Mancini. BASIN ANALYSIS OF THE MISSISSIPPI INTERIOR SALT BASIN AND PETROLEUM SYSTEM MODELING OF THE JURASSIC SMACKOVER FORMATION, EASTERN GULF COASTAL PLAIN. Office of Scientific and Technical Information (OSTI), abril de 1999. http://dx.doi.org/10.2172/811896.

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Ernest A. Mancini. Basin Analysis of the Mississippi Interior Salt Basin and Petroleum System Modeling of the Jurassic Smackover Formation, Eastern Gulf Coastal Plain. Office of Scientific and Technical Information (OSTI), diciembre de 1997. http://dx.doi.org/10.2172/1566.

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Ernest A. Mancini. Basin Analysis of the Mississippi Interior Salt Basin and Petroleum System Modeling of the Jurassic Smackover Formation, Eastern Gulf Coastal Plain. Office of Scientific and Technical Information (OSTI), abril de 1998. http://dx.doi.org/10.2172/1567.

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