Academic literature on the topic 'Organo-Minerals'

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Journal articles on the topic "Organo-Minerals"

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Kovacević, Dragana, Jovan Lemić, Milan Damjanović, Radivoj Petronijević, Đorđe Janaćković, and Tanja Stanić. "Fenitrothion adsorption – desorption on organo – minerals." Applied Clay Science 52, no. 1-2 (2011): 109–14. http://dx.doi.org/10.1016/j.clay.2011.02.006.

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Noh, Hye-Ji, Hyang-Hyun Cho, Chul-Kyu Lee, and Hee-Kyong Kim. ""Development of Chemical Fertilizer Substitute Type Organo-Minerals Fertilizer Field effectiveness Evaluation of Organo-Minerals Fertilizers Produced Based on Vitamin for Lettuce (Lactuca sativa L.)." Journal of Chitin and Chitosan 21, no. 3 (2016): 149–57. http://dx.doi.org/10.17642/jcc.21.3.1.

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Siébou Palé, Djibril Yonli, Albert Barro, et al. "Assessing the effect of tillage and fertilization on the accumulation of minerals in pearl millet stover." World Journal of Advanced Research and Reviews 15, no. 2 (2022): 606–15. http://dx.doi.org/10.30574/wjarr.2022.15.2.0826.

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Pearl millet [Pennisetum glaucum (L.) R. Br.] constitutes the third most important cultivated cereal and source of nutrients in Burkina Faso. The study carried out in 2018 and 2019 at the Saria Environment and Agricultural Researches Station aimed to assess the effects of tillage and organo-mineral fertilization on the quantities of minerals accumulated in pearl millet stover that could be used in animal diets as nutritional supplements. The experimental design was a completely randomized block with a split-plot arrangement of treatments, three replications with four tillage methods assigned t
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Siébou, Palé, Yonli Djibril, Barro Albert, et al. "Assessing the effect of tillage and fertilization on the accumulation of minerals in pearl millet stover." World Journal of Advanced Research and Reviews 15, no. 2 (2022): 606–15. https://doi.org/10.5281/zenodo.7759444.

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Pearl millet [<em>Pennisetum glaucum</em>&nbsp;(L.) R. Br.] constitutes the third most important cultivated cereal and source of nutrients in Burkina Faso. The study carried out in 2018 and 2019 at the Saria Environment and Agricultural Researches Station aimed to assess the effects of tillage and organo-mineral fertilization on the quantities of minerals accumulated in pearl millet stover that could be used in animal diets as nutritional supplements. The experimental design was a completely randomized block with a split-plot arrangement of treatments, three replications with four tillage meth
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Vujakovic, Aleksandra, Aleksandra Dakovic, Jovan Lemic, Ana Radosavljevic-Mihajlovic, and Magdalena Tomasevic-Canovic. "Adsorption of inorganic anionic contaminants on surfactant modified minerals." Journal of the Serbian Chemical Society 68, no. 11 (2003): 833–41. http://dx.doi.org/10.2298/jsc0311833v.

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Organo-mineral complexes were obtained by treatment of aluminosilicate minerals (zeolite, bentonite and diatomaceous earth) with a primary amine (oleylamine) and an alkyl ammonium salt (stearyldimethylbenzyl ammonium chloride). The modification of the zeolite surface was carried out in two steps. The first step was treatment of the zeolite with 2M HCl. This acid treatment of the zeolite increased its affinity for neutral molecules such as surface-active amines. The second step of the modification was the adsorption of oleylamine on the acid treated zeolite. Four types of organo-mineral complex
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Tuchowska, Magdalena, Magdalena Wołowiec, Agnieszka Solińska, Anita Kościelniak, and Tomasz Bajda. "Organo-Modified Vermiculite: Preparation, Characterization, and Sorption of Arsenic Compounds." Minerals 9, no. 8 (2019): 483. http://dx.doi.org/10.3390/min9080483.

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Among the various technologies tested for removing the anionic species resulting from arsenic contamination, sorption methods have received unflagging interest. Being potential sorbent materials, clay minerals modified by cationic surfactants are often examined for this purpose. Among the clay minerals tested, information regarding sorption properties of expanded vermiculite modified with surfactants is scarce. Therefore, the present study aims to prepare organo-vermiculites modified with hexadecyltrimethylammonium (HDTMA) and benzyldimethylhexadecylammonium (HDBA) at surfactant concentrations
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Daab, Matthias, Natalie J. Eichstaedt, Andreas Edenharter, Sabine Rosenfeldt, and Josef Breu. "Layer charge robust delamination of organo-clays." RSC Advances 8, no. 50 (2018): 28797–803. http://dx.doi.org/10.1039/c8ra05318a.

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Weng, Yi-Tse, Chun-Chieh Wang, Cheng-Cheng Chiang, et al. "In situ evidence of mineral physical protection and carbon stabilization revealed by nanoscale 3-D tomography." Biogeosciences 15, no. 10 (2018): 3133–42. http://dx.doi.org/10.5194/bg-15-3133-2018.

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Abstract. An approach for nanoscale 3-D tomography of organic carbon (OC) and associated mineral nanoparticles was developed to illustrate their spatial distribution and boundary interplay, using synchrotron-based transmission X-ray microscopy (TXM). The proposed 3-D tomography technique was first applied to in situ observation of a laboratory-made consortium of black carbon (BC) and nanomineral (TiO2, 15 nm), and its performance was evaluated using dual-scan (absorption contrast and phase contrast) modes. This novel tool was then successfully applied to a natural OC–mineral consortium from mo
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Philippine Journal of Crop Science, Rubigilda Paraguison-Alili, Ma Angeline M. Donato, Aldrin M. Corpuz, and Emelie C. Ablaza. "Assessing the Impact of Organo-Minerals on Water Quality Parameters and Pathogen Reduction in Irrigation Water." Philippine Journal of Crop Science 49, no. 3 (2024): 50–58. https://doi.org/10.63568/vol49iss3pp50-58.

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This study addresses the pressing need for effective, in-situ bioremediation of irrigation water contaminated with microbial pathogens. Contaminated water can introduce pathogens to crops, impacting both agricultural productivity and public health. Using organo-minerals as a treatment method, we specifically focused on microbial reduction by measuring the presence of Escherichia coli and Salmonella spp. before and after treatment. Quantitative analysis showed a significant decrease in microbial contaminants post-treatment, with microbial levels reduced by an average of 70% across sampling site
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Riebe, Beate, Stefan Dultz, and Claus Bunnenberg. "Temperature effects on iodine adsorption on organo-clay minerals." Applied Clay Science 28, no. 1-4 (2005): 9–16. http://dx.doi.org/10.1016/j.clay.2004.01.004.

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Dissertations / Theses on the topic "Organo-Minerals"

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Henry, Erwin. "Synthèse d’agrégats organo-minéraux : analogues des particules en suspension de rivières." Electronic Thesis or Diss., Université de Lorraine, 2021. http://www.theses.fr/2021LORR0209.

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Les matières en suspension (MES) participent au transfert de matière des continents vers les océans. Les MES sont quantitativement issues de plusieurs sources : de l'érosion des surfaces continentales, de la remobilisation des sédiments, de l'activité biologique aquatique, et de l’activité anthropique introduisant directement des particules dans le milieu aquatique. Leur composition, leur distribution en taille et leur nature va dépendre de l’ensemble des processus qui contrôlent l’érosion, l’activité biologique ainsi que l’ensemble des activités humaines au sein d’un bassin versant. L’objecti
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Garcia, Arredondo Mariela. "Root-Driven Weathering Impacts on Mineral-Organic Associations Over Pedogenic Time Scales." 2019. https://scholarworks.umass.edu/masters_theses_2/739.

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Plant roots are critical weathering agents in deep soils, yet the impact of resulting mineral transformations on the vast deep soil carbon (C) reservoir are largely unknown. Root-driven weathering of primary minerals may cause the formation of reactive secondary minerals, which protect mineral-organic associations (MOAs) for centuries or millennia. Conversely, root-driven weathering may also transform secondary minerals, potentially enhancing the bioavailability of C previously protected in MOAs. Here we examined the impact of root-driven weathering on MOAs and their capacity to store C over p
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Yoo, Hye-Dong. "Photodechlorination of pentachlorobenzene in organo-clay." Thesis, 1994. http://hdl.handle.net/1957/35547.

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Books on the topic "Organo-Minerals"

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1934-, Yariv Shmuel, and Cross H. 1930-, eds. Organo-clay complexes and interactions. Marcel Dekker, 2002.

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(Editor), Shmuel Yariv, and Harold Cross (Editor), eds. Organo-Clay Complexes & Interactions. CRC, 2001.

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Yoo, Hye-Dong. Photodechlorination of pentachlorobenzene in organo-clay. 1994.

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Book chapters on the topic "Organo-Minerals"

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Alekseeva, Tatiana Victorovna. "Clay Minerals and Organo-Mineral Associates." In Encyclopedia of Agrophysics. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-3585-1_27.

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"Organo-Minerals and Organo-Clay Interactions and the Origin of Life on Earth." In Organo-Clay Complexes and Interactions. CRC Press, 2001. http://dx.doi.org/10.1201/9781482270945-16.

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Zhang, X. N., and A. Z. Zhao. "Surface Charge." In Chemistry of Variable Charge Soils. Oxford University Press, 1997. http://dx.doi.org/10.1093/oso/9780195097450.003.0005.

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The surface of soil colloids carries electric charges, and these surface charges are the basic cause for soil to possess a series of surface properties. Soil surface charges affect the chemical properties of the soil through varying the quantity of electric charge and the surface charge density. For example, adsorptions of cations and anions are caused by negative and positive surface charges of the soil, respectively. The amount of ions adsorbed is determined by the quantity of surface charge, whereas the tightness of adsorption is related to charge density. In addition, the migration of ions
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Kuang, W., and C. Detellier. "Structuration of organo-minerals: nanohybrid materials resulting from the incorporation of alcohols in the tunnels of palygorskite." In Nanoporous Materials IV, Proceedings of the 4th International Symposium on Nanoporous Materials. Elsevier, 2005. http://dx.doi.org/10.1016/s0167-2991(05)80242-3.

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"Structure and Surface Acidity of Clay Minerals." In Organo-Clay Complexes and Interactions. CRC Press, 2001. http://dx.doi.org/10.1201/9781482270945-6.

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"Staining of Clay Minerals and Visible Absorption Spectroscopy of Dye-Clay Complexes." In Organo-Clay Complexes and Interactions. CRC Press, 2001. http://dx.doi.org/10.1201/9781482270945-14.

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Conference papers on the topic "Organo-Minerals"

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Bolotin, Oleg, Cristina Mogorici, Oleg Petuhov, and Natalia Costriucova. "Preparation of an organo-montmorillonite complex based on bentonite clays from Moldova." In Conferința științifică națională cu participare internațională "Integrare prin cercetare și inovare", dedicată Zilei Internaționale a Științei pentru Pace și Dezvoltare. Moldova State University, 2025. https://doi.org/10.59295/spd2024n.68.

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The article provides data on the interaction of clay minerals with organic substances. With an increase in the amount of organic cations adsorbed in the interlayer space of monmorillonite, an increase in its interplanar distance is observed according to the X-ray analysis data. Oxidation of organic matter of organobentonites occurs stepwise, which is confirmed by the results of thermal analysis of the studied samples.
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Reports on the topic "Organo-Minerals"

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Liseroudi, M. H., O. H. Ardakani, P. K. Pedersen, R. A. Stern, J M Wood, and H. Sanei. Diagenetic and geochemical controls on H2S distribution in the Montney Formation, Peace River region, western Canada. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329785.

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The Lower Triassic Montney Formation is a major siltstone dominated unconventional tight gas play in the Western Canadian Sedimentary Basin (WCSB). In the Peace River region, the Montney Formation contains a regionally variable amount of hydrogen sulfide (H2S) in gas-producing wells with western Alberta's wells having the highest concentrations. Previous studies on the source and distribution of H2S in the Montney Formation mainly focused on variations of H2S concentration and its relationship with other hydrocarbon and non-hydrocarbon gases, sulfur isotope composition of H2S, as well as organ
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