Academic literature on the topic 'Allophagie'

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Journal articles on the topic "Allophagie"

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Parfitt, R. L. "Allophane and imogolite: role in soil biogeochemical processes." Clay Minerals 44, no. 1 (2009): 135–55. http://dx.doi.org/10.1180/claymin.2009.044.1.135.

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AbstractThe literature on the formation, structure and properties of allophane and imogolite is reviewed, with particular emphasis on the seminal contributions by Colin Farmer. Allophane and imogolite occur not only in volcanic-ash soils but also in other environments. The conditions required for the precipitation of allophane and imogolite are discussed. These include pH, availability of Al and Si, rainfall, leaching regime, and reactions with organic matter. Because of their excellent water storage and physical properties, allophanic soils can accumulate large amounts of biomass. In areas of
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Parfitt, R. L., A. Parshotam, and G. J. Salt. "Carbon turnover in two soils with contrasting mineralogy under long-term maize and pasture." Soil Research 40, no. 1 (2002): 127. http://dx.doi.org/10.1071/sr00105.

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Total organic carbon (C) and natural 13C abundance were measured in adjacent allophanic soils (Andisols) and non-allophanic soils (Inceptisols) under maize (Zea mays L.) and ryegrass pasture (Lolium perenne L.) to assess the C turnover rate in soils of contrasting mineralogy and specific surface area. The allophanic soil contained more total C than the non-allophanic soil (139 v. 101 t C/ha in the upper 0–35 cm) but neither soil showed a significant difference in C content between pasture and maize, provided maize residue was retained and incorporated. The gross annual inputs under mai
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Onodera, Yoshio, Takashi Iwasaki, Abhijit Chatterjee, et al. "Bactericidal allophanic materials prepared from allophane soil." Applied Clay Science 18, no. 3-4 (2001): 123–34. http://dx.doi.org/10.1016/s0169-1317(00)00038-7.

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Onodera, Yoshio, Shunji Sunayama, Abhijit Chatterjee, et al. "Bactericidal allophanic materials prepared from allophane soil." Applied Clay Science 18, no. 3-4 (2001): 135–44. http://dx.doi.org/10.1016/s0169-1317(00)00039-9.

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Perez del Villar, L., M. C. Moro, and M. L. Cembranos. "Allophane in weathered zones of barite ore deposits (Vide de Alba and San Blas, Zamora, Spain): mineralogy and genesis." Clay Minerals 27, no. 3 (1992): 309–23. http://dx.doi.org/10.1180/claymin.1992.027.3.04.

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AbstractThe allophane studied occurs in the weathered zones of the barite-sulphide-bearing dolomitic levels, interbedded in the barite ore deposits of Vide de Alba and San Bias (Province of Zamora). These ore deposits are interstratified in the Silurian-Devonian sulphide bearing volcano sedimentary materials of the Alcañices Synform. The allophanic samples have been studied by polarizing microscopy, SEM, XRD, DTA, TG, IRS, EMA and chemical analyses, the last after dissolving the samples by acid (HF + HNO3 + 3HCl + H3BO3) and alkaline digestion (0·5 m NaOH). It is suggested that allophane origi
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Moro, M. C., M. L. Cembranos, and A. Fernandez. "Allophane-like materials in the weathered zones of Silurian phosphate-rich veins from Santa Creu d'Olorda (Barcelona, Spain)." Clay Minerals 35, no. 2 (2000): 411–21. http://dx.doi.org/10.1180/000985500546873.

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AbstractAllophane-like materials occur in the weathered zones of the phosphate-rich veins hosted in Silurian metasediments of the Catalonian Coastal Ranges. These metasediments also host sulphide and phosphate sedimentary mineralizations. Mineralogical and geochemical investigations of the allophanic samples indicate that they comprise Si-rich allophane, with a molar SiO2/Al2O3 ratio ranging between 1.19 and 2.23, with amorphous Al-(Ca) phosphate and hydroxylapatite as major minerals, and minor goethite and quartz. It is assumed that allophane, amorphous Al-(Ca) phosphate and hydroxylapatite c
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Allbrook, RF. "Shrinkage of some New Zealand soils and its implications for soil physics." Soil Research 31, no. 2 (1993): 111. http://dx.doi.org/10.1071/sr9930111.

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Aggregates from three New Zealand soils were used to produce shrinkage curves. Each soil had a clay mineralogy dominated by a different mineral, namely allophane, halloysite and kaolinite.The curves showed marked differences. Only the allophanic soil showed structural shrinkage, and only the halloysitic soil showed residual shrinkage. When the slope of the normal shrinkage line is about unity, this indicates the soil is liable to crack- this was only shown by the allophanic soil. The implication for soil physics is that, since all soils with at least a moderate clay content shrink, bulk densit
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Gobin, Mukteshwar, Noriyuki Yasufuku, Midori Watanabe, Guojun Liu, and Ryohei Ishikura. "Influence of time on the small strain shear modulus of an allophanic volcanic ash." E3S Web of Conferences 544 (2024): 01005. http://dx.doi.org/10.1051/e3sconf/202454401005.

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The small strain shear modulus is an important parameter in the assessment of soil dynamics problems. Studies on the small strain shear stiffness of volcanic ash remain rare probably because globally they cover just under 1% of the land surface. However, on a regional scale, this figure may be consequential as in the case of Japan, where about one third of its total land surface is covered by andosols. In this research, we aimed at understanding the influence of confinement time, a non-negligible parameter, contingent on the soil type, which needs to be accounted for when assessing the shear m
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Chevallier, Tiphaine, Kenji Fujisaki, Olivier Roupsard, et al. "Short-range-order minerals as powerful factors explaining deep soil organic carbon stock distribution: the case of a coffee agroforestry plantation on Andosols in Costa Rica." SOIL 5, no. 2 (2019): 315–32. http://dx.doi.org/10.5194/soil-5-315-2019.

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Abstract. Soil organic carbon (SOC) constitutes the largest terrestrial C stock, particularly in the Andosols of volcanic areas. Quantitative information on distribution of SOC stocks is needed to construct a baseline for studying temporal changes in SOC. The spatial variation of soil short-range-order minerals such as allophane usually explains the variability of topsoil SOC contents, but SOC data for deeper soil layers are needed. We found that within a 1 km2 Costa Rican basin covered by coffee agroforestry, SOC stocks in the upper 200 cm of soil were highly variable (24 to 72 kg C m−2). Top
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Parfitt, RL. "Surface charge in some New Zealand soils measured at typical ionic strength." Soil Research 30, no. 3 (1992): 331. http://dx.doi.org/10.1071/sr9920331.

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The positive and negative surface charges of some New Zealand soils used for horticulture were measured at different pH values using 0.002 M CaCl2 solutions, Which have a similar ionic strength to soil solutions in New Zealand. The surface negative charge increased with pH for all soil samples including those containing mica and smectite. This behaviour was mainly due to the presence of organic matter and allophane both of which had an appreciable amount of variable negative charge. Allophanic soil B horizons had a higher positive charge than that of the Oxidic soils, which was less than 1 cmo
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Dissertations / Theses on the topic "Allophagie"

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Cailloce, Justine. "Identification des facteurs de reconnaissance des mitochondries spermatiques dans l’embryon de C. elegans, garants de l’hérédité mitochondriale uni-parentale maternelle." Electronic Thesis or Diss., Sorbonne université, 2023. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2023SORUS497.pdf.

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Les mitochondries sont des composants cellulaires essentiels, retrouvés dans le cytoplasme de la grande majorité des cellules des organismes eucaryotes. Elles interviennent dans plusieurs mécanismes garants du bon fonctionnement cellulaire comme l’apoptose ou le stockage du calcium. La principale fonction mitochondriale est portée par la membrane mitochondriale interne où sont situés des complexes protéiques permettant la production d’adénosine triphosphate ou ATP, source d’énergie pour nos cellules. Dans le règne animal les mitochondries sont les seuls autres organites, en plus du noyau, à po
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Casimir, Al-Mario. "From volcanic ash to allophanic dust : understanding phosphorous behaviour in Dominican soils." Thesis, Bangor University, 2015. https://research.bangor.ac.uk/portal/en/theses/from-volcanic-ash-to-allophanic-dust--understanding-phosphorous-behaviour-in-dominican-soils(cc56436e-015b-4489-b926-fd62dd25fb7c).html.

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The economy of the Commonwealth of Dominica is primarily agrarian based with banana production as one of the key export commodities, notwithstanding its preferential loss in the European Union market. However, banana productivity like most other crops has been severely impacted by a general low native soil nutrient status coupled with low application rates of phosphate (P) fertilizers in particular. The latter can be partly attributed to the low purchasing power on the international market as is evident in the long term trends of increaseprices for nitrogenous and phosphate fertilizers. The vo
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Bauer, McNeill John. "Multivariate Analysis of Factors Regulating the Formation of Synthetic Allophane and Imogolite Nanoparticles." Thesis, Virginia Tech, 2019. http://hdl.handle.net/10919/93330.

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Imogolite and allophane are nanosized aluminosilicates with high value in industrial and technological applications, however it remains unclear what factors control their formation and abundance in nature and in the lab. This work investigated the complex system of physical and chemical conditions that influence the formation of these nanominerals. Samples were synthesized and analyzed by powder x-ray diffraction, in situ and ex situ small angle x-ray scattering, and high-resolution transmission electron microscopy. Multivariate regression analysis combined with linear combination fitting of p
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Anderson, Donald Jared. "Understanding Soil Liquefaction of the 2016 Kumamoto Earthquake." BYU ScholarsArchive, 2019. https://scholarsarchive.byu.edu/etd/7135.

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The Kumamoto earthquake of April 2016 produced two foreshocks of moment magnitude 6.0 and 6.2 and a mainshock of 7.0, which should have been followed by widespread and intense soil liquefaction. A Geotechnical Extreme Events Reconnaissance team (GEER) led by Professor Rob Kayen of UC Berkley was dispatched to the Kumamoto Plain--which is in Kumamoto Prefecture, the southern main island of Japan--immediately following the earthquake. The Japanese and U.S. engineers in the GEER team observed mostly minor and sporadic liquefaction, which was unexpected as the local site geology, known soil strati
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Kolka-Jonsson, Pall Valdimar. "CarbBirch (Kolbjörk): Carbon sequestration and soil development under mountain birch (Betula pubescens) in rehabilitated areas in southern Iceland." The Ohio State University, 2011. http://rave.ohiolink.edu/etdc/view?acc_num=osu1302113068.

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Creton, Benoît. "Étude par dynamique moléculaire du comportement d'aluminosilicates tubulaires hydratés : structure et dynamique du sytème eau-imogolite." Lille 1, 2006. https://pepite-depot.univ-lille.fr/LIBRE/Th_Num/2006/50376-2006-Creton.pdf.

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La structure et la dynamique des molécules d'eau confinées dans des aluminosilicates de formes tubulaire (imogolite) et sphérique (allophane) ont été étudiées à l'échelle microscopique par la méthode de la dynamique moléculaire. Pour ce faire, des modèles structuraux de ces aluminosilicates ainsi que des modèles d'interactions ont été développés. La simulation de la dynamique vibrationnelle de l'imogolite fournit des résultats en accord avec ceux expérimentaux. Ainsi, certaines bandes des spectres infrarouge et Raman ont pu être attribuées. Les spectres Raman calculés pour ces structures montr
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Maillet, Perrine. "Structure et croissance de nanotubes de Ge-imogolite simple et double-paroi." Phd thesis, Université Pierre et Marie Curie - Paris VI, 2010. http://tel.archives-ouvertes.fr/tel-00584846.

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Les Imogolites (OH)3Al2O3Si(OH) sont des minéraux naturels découverts en 1962 dans des sols volcaniques japonais qui présentent une structure analogue à celle des nanotubes de carbone. Leur synthèse, décrite depuis 1977, permet l'obtention de tubes bien calibrés et monodisperses. La récente mise en évidence de la possibilité de synthétiser des analogues au germanium en grande quantité en a fait un matériau de choix dans le cadre de mon sujet de thèse visant à préparer des matériaux mésoporeux à base de nanoparticules anisotropes. Lors de la caractérisation de ces imogolites par diffusion de ra
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Creton, Benoît. "Étude par dynamique moléculaire du comportement d'aluminosilicates tubulaires hydratés : structure et dynamique du système eau-imogolite." Phd thesis, Université des Sciences et Technologie de Lille - Lille I, 2006. http://tel.archives-ouvertes.fr/tel-00270255.

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La structure et la dynamique des molécules d'eau confinées dans des aluminosilicates de formes tubulaire (imogolite) et sphérique (allophane) ont été étudiées à l'échelle microscopique par la méthode de la dynamique moléculaire. Pour ce faire, des modèles structuraux de ces aluminosilicates ainsi que des modèles d'interactions ont été développés. La simulation de la dynamique vibrationnelle de l'imogolite fournit des résultats en accord avec ceux expérimentaux. Ainsi, certaines bandes des spectres infrarouge et Raman ont pu être attribuées. Les spectres Raman calculés pour ces structures montr
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Levard, Clément. "Nanoparticules naturelles : imogolites et allophanes. Structure, mécanismes de croissance et capacité de rétention des éléments traces métalliques." Phd thesis, Université Paul Cézanne - Aix-Marseille III, 2008. http://tel.archives-ouvertes.fr/tel-00368753.

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Cette étude vise à déterminer le transfert et la mobilité d'éléments traces métalliques (ETM), dans des sols de la Réunion destinés à l'épandage de déchets urbains. En plus des fortes teneurs naturelles en ETM, ces sols ont la particularité d'avoir une minéralogie très spécifique avec la présence en abondance de nanoparticules naturelles, communément appelés "imogolites" (nanotubes) et "allophanes" (nanosphères, ovoïdes, amorphe ?). Ces aluminosilicates structurés à courte distance sont susceptibles de piéger les ETM pouvant ainsi limiter leur mobilité et leur biodisponibilité. <br /><br />Dan
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"The Effects of Chemical Weathering on Thermal-Infrared Spectral Data and Models: Implications for Aqueous Processes on the Martian Surface." Doctoral diss., 2011. http://hdl.handle.net/2286/R.I.9320.

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abstract: Chemical and mineralogical data from Mars shows that the surface has been chemically weathered on local to regional scales. Chemical trends and the types of chemical weathering products present on the surface and their abundances can elucidate information about past aqueous processes. Thermal-infrared (TIR) data and their respective models are essential for interpreting Martian mineralogy and geologic history. However, previous studies have shown that chemical weathering and the precipitation of fine-grained secondary silicates can adversely affect the accuracy of TIR spectral models
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Books on the topic "Allophagie"

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Su, Chunming. Surface charge characteristics and thermodynamic stability of imogolite and allophane. 1992.

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Book chapters on the topic "Allophagie"

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Hangay, George, Severiano F. Gayubo, Marjorie A. Hoy, et al. "Allophagic Speciation." In Encyclopedia of Entomology. Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-6359-6_160.

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Hewitt, Allan E., Megan R. Balks, and David J. Lowe. "Allophanic Soils." In The Soils of Aotearoa New Zealand. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-64763-6_2.

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Koji, Wada. "Allophane and Imogolite." In SSSA Book Series. Soil Science Society of America, 2018. http://dx.doi.org/10.2136/sssabookser1.2ed.c21.

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Harsh, James, Jon Chorover, and Egide Nizeyimana. "Allophane and Imogolite." In Soil Mineralogy with Environmental Applications. Soil Science Society of America, 2018. http://dx.doi.org/10.2136/sssabookser7.c9.

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Dahlgren, R. A. "Quantification of Allophane and Imogolite." In Quantitative Methods in Soil Mineralogy. Soil Science Society of America, 2015. http://dx.doi.org/10.2136/1994.quantitativemethods.c14.

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Huang, Yu-Tuan, David J. Lowe, G. Jock Churchman, Louis A. Schipper, Nicolas J. Rawlence, and Alan Cooper. "Carbon Storage and DNA Adsorption in Allophanic Soils and Paleosols." In Soil Carbon. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04084-4_17.

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Hiradate, S., and K. Inoue. "Interactions of Mugineic Acid with Allophane, Imogolite, Montmorillonite and Gibbsite." In Effect of Mineral-Organic-Microorganism Interactions on Soil and Freshwater Environments. Springer US, 1999. http://dx.doi.org/10.1007/978-1-4615-4683-2_9.

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Juo, Anthony S. R., and Kathrin Franzluebbers. "Properties and Management of Allophanic Soils." In Tropical Soils. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195115987.003.0017.

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Allophanic soils are dark-colored young soils derived mainly from volcanic ash. These soils typically have a low bulk density (&lt; 0.9 Mg/m3), a high water retention capacity (100% by weight at field capacity), and contain predominantly allophanes, imogolite, halloysite, and amorphous Al silicates in the clay fraction. These soils are found in small, restricted areas with volcanic activity. Worldwide, there are about 120 million ha of allophanic soils, which is about 1% of the Earth's ice-free land surface. In tropical regions, allophanic soils are among the most productive and intensively us
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"allophanic, adj.²." In Oxford English Dictionary, 3rd ed. Oxford University Press, 2023. http://dx.doi.org/10.1093/oed/7028187270.

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"allophanic, adj.¹." In Oxford English Dictionary, 3rd ed. Oxford University Press, 2023. http://dx.doi.org/10.1093/oed/3349524229.

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Conference papers on the topic "Allophagie"

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Tunega, Daniel, Maria Rechberger, Vivian Remlinger, et al. "Glyphosate adsorption on allophane and halloysite." In Goldschmidt2023. European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.20148.

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Sang, Hongji, Zhengcheng Gu, Zheng Cui, Ruoxue Zou, and Yan Wu. "Preparation and Properties of Ceramic Solidified Product Containing Cs and Sr." In 2022 29th International Conference on Nuclear Engineering. American Society of Mechanical Engineers, 2022. http://dx.doi.org/10.1115/icone29-92765.

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Abstract 137Cs and 90Sr in high level liquid waste, with high radioactivity, large heat-generating and relatively long half-life. In order to solve the problem of final disposal of 137Cs and 90Sr, natural mineral allophane was chosen as the base materials to synthesize the silicate ceramic solidified products with cold pressing/sintering method. The microstructure, phase composition and surface element distribution of the solidified products were analyzed. The solidification mechanism of the solidified products was also discussed. The surface of the solidified products appeared melting phenome
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Matsuura, Yoko, Fumitoshi Iyoda, Shuhei Hayashi, Shuichi Arakawa, Masami Okamoto, and Hidetomo Hayashi. "DNA adsorption characteristics of hollow spherical allophane nano-particles." In PROCEEDINGS OF PPS-29: The 29th International Conference of the Polymer Processing Society - Conference Papers. American Institute of Physics, 2014. http://dx.doi.org/10.1063/1.4873773.

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Jeute, Thomas J., Leslie L. Baker, Janice L. Bishop, Elizabeth B. Rampe, and Zaenal Abidin. "CHARACTERIZING NANOPHASE MATERIALS ON MARS: SPECTROSCOPIC STUDIES OF ALLOPHANE AND IMOGOLITE." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-303855.

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Castañeda Jaimes, A., J. Colmenares Montañez, and L. Viveros Rosero. "Influence of the Weathering Degree on the Dispersion Susceptibility of Allophanic Soils." In 7th International Conference on Geotechnical and Geophysical Site Characterization. CIMNE, 2024. http://dx.doi.org/10.23967/isc.2024.270.

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Pranoto, Santika Kunti Prabawani, and Nurul Fatimah. "Optimation of allophane clay and sugar palm fiber waste as Fe adsorbent." In THE 3RD INTERNATIONAL SEMINAR ON CHEMISTRY: Green Chemistry and its Role for Sustainability. Author(s), 2018. http://dx.doi.org/10.1063/1.5082444.

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Dharmawan, Christian Adi, Cari, Pranoto, and Prabang Setyono. "Effectiveness of combined activated allophane and effective microorganisms attached bioball to reduce phenol concentration in water." In THE 3RD INTERNATIONAL SEMINAR ON CHEMISTRY: Green Chemistry and its Role for Sustainability. Author(s), 2018. http://dx.doi.org/10.1063/1.5082449.

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