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Journal articles on the topic 'Organo-Minerals'

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1

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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2

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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3

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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4

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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5

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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6

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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7

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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8

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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9

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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10

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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11

Dultz, Stefan, Beate Riebe, and Claus Bunnenberg. "Temperature effects on iodine adsorption on organo-clay minerals." Applied Clay Science 28, no. 1-4 (2005): 17–30. http://dx.doi.org/10.1016/j.clay.2004.01.005.

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12

Seliem, Moaaz K., Sridhar Komarneni, Yunchul Cho, et al. "Organosilicas and organo-clay minerals as sorbents for toluene." Applied Clay Science 52, no. 1-2 (2011): 184–89. http://dx.doi.org/10.1016/j.clay.2011.02.024.

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13

Egwunatum, Anselm Enwelem, Patience Ndidi Emilimor, Nneka Sophia Emma-Otum, and Alukwe Doreen. "Evaluation of organo-mineral qualities of combusted compost floor litters in Achalla forest reserve on early growth responses of Dacryodes edulis H. J. Lam." International Journal of Agricultural Research, Innovation and Technology 13, no. 1 (2023): 31–37. http://dx.doi.org/10.3329/ijarit.v13i1.67953.

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This study evaluated the potential of compost-combusted forest litters as alternative sources of ex-situ organo-mineral products to the direct use of controlled fire for enhanced soil nutrients in forest stands. Floor litters from six (6) delineated standing forest patches of Pterocarpus erinaceus, Gmelina arborea, Tectona grandis, Bambusa vulgaris, Ceiba pentandra and Mangifera indica were characterized for N, K, P, Ca and Mg; composted for 3, 6, 9 and 12 days and then uniformly combusted to produce organo-minerals for early growth response of Dacryodes edulis in a 6 x 4 split-plot factorial
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14

Anselm, Enwelem Egwunatum, Ndidi Emilimor Patience, Sophia Emma-Otum Nneka, and Doreen Alukwe. "Evaluation of organo-mineral qualities of combusted compost floor litters in Achalla forest reserve on early growth responses of Dacryodes edulis H. J. Lam." International Journal of Agricultural Research, Innovation and Technology 13, no. 1 (2023): 31–37. https://doi.org/10.3329/ijarit.v13i1.67953.

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This study evaluated the potential of compost-combusted forest litters as alternative sources of&nbsp;<em>ex-situ&nbsp;</em>organo-mineral products to the direct use of controlled fire for enhanced soil nutrients in forest stands. Floor litters from six (6) delineated standing forest patches of&nbsp;<em>Pterocarpus erinaceus</em>,&nbsp;<em>Gmelina</em><em>&nbsp;arborea</em>,&nbsp;<em>Tectona grandis</em>,&nbsp;<em>Bambusa vulgaris</em>,&nbsp;<em>Ceiba pentandra</em>&nbsp;and&nbsp;<em>Mangifera indica</em>&nbsp;were characterized for N, K, P, Ca and Mg;&nbsp; composted for 3, 6, 9 and 12 days a
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15

Gu, B., and L. E. Lowe. "Observations on the effect of a soil polysaccharide fraction on boron adsorption by clay minerals." Canadian Journal of Soil Science 72, no. 4 (1992): 623–26. http://dx.doi.org/10.4141/cjss92-053.

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Complexes formed by coating a soil polysaccharide fraction on illite, montmorillonite and kaolinite, substantially reduced boron adsorption by the clay minerals at approximately neutral pH. This suggests that boron retention in soils is influenced by the occurrence of stable polysaccharide-clay complexes. Key words: boron adsorption, organo-clay complex, soil polysaccharide
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16

Lao, Hongbai, Sylvie Latieule, and Christian Detellier. "Molecular recognition in microporous organo-minerals. Shape-specific interactions of carbon dioxide in functionalized organo-montmorillonite microcavities." Chemistry of Materials 3, no. 6 (1991): 1009–11. http://dx.doi.org/10.1021/cm00018a011.

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17

Albanis, T. A., T. G. Danis, and P. J. Pomonis. "Separation of chlorophenols using columns of hydroxyaluminium interlayered clays." Clay Minerals 32, no. 1 (1997): 143–47. http://dx.doi.org/10.1180/claymin.1997.032.1.15.

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Clay minerals play an important role in the retention, transport and chemistry of organic micropollutants in soils. There has been considerable recent interest in modelling and designing modified clays as adsorbents and catalysts for the removal of contaminants from waste waters (McBride et al., 1977; Mortland et al., 1986; Boyd et al., 1988). Organo-clays have been used as chromatographic stationary phases over the past three decades. White (1957) and Barrer &amp; Hampton (1957) used alkylammonium montmorillonites as stationary phases and determined the selective retention of aromatic hydroca
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18

Torqueti, Sabrina Thereza dos Santos, Karina Volpi Furtini Boldrin, Ângela Maria Pereira do Nascimento, Patrícia Duarte de Oliveira Paiva, Antônio Eduardo Furtini Neto, and Iracema Clara Alves Luz. "Alternative potassium source for the cultivation of ornamental sunflower." Ciência e Agrotecnologia 40, no. 3 (2016): 257–64. http://dx.doi.org/10.1590/1413-70542016403036115.

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ABSTRACT Brazil is dependent on importation of fertilizers, especially the potassics. Rocks and minerals that contain nutrients have a potential for use in agriculture as fertilizer, especially those of slow solubilization and that exhibit residual effect. In this context, the objective was to assess the feasibility of glauconite rock as potassium source for the cultivation of ornamental sunflower. The experiment was conducted under controlled conditions arranged in an entirely randomized design, in a 4x4 + 4 factorial scheme, with four replicates and one plant per plot. Four glauconite-based
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19

Volzone, Cristina, Norma Gallegos, Carlos Cantera, and Alberto Greco. "Uptake of acid black 210 dye by organo-montmorillonite clay minerals." European Journal of Chemistry 4, no. 4 (2013): 366–69. http://dx.doi.org/10.5155/eurjchem.4.4.366-369.862.

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20

Kim, Joo Young, Sridhar Komarneni, Robert Parette, Fred Cannon, and Hiroaki Katsuki. "Perchlorate uptake by synthetic layered double hydroxides and organo-clay minerals." Applied Clay Science 51, no. 1-2 (2011): 158–64. http://dx.doi.org/10.1016/j.clay.2010.11.025.

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21

Wójcik-Bania, Monika, and Jakub Matusik. "The Effect of Surfactant-Modified Montmorillonite on the Cross-Linking Efficiency of Polysiloxanes." Materials 14, no. 10 (2021): 2623. http://dx.doi.org/10.3390/ma14102623.

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Polymer–clay mineral composites are an important class of materials with various applications in the industry. Despite interesting properties of polysiloxanes, such matrices were rarely used in combination with clay minerals. Thus, for the first time, a systematic study was designed to investigate the cross-linking efficiency of polysiloxane networks in the presence of 2 wt % of organo-montmorillonite. Montmorillonite (Mt) was intercalated with six quaternary ammonium salts of the cation structure [(CH3)2R’NR]+, where R = C12, C14, C16, and R’ = methyl or benzyl substituent. The intercalation
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22

Danilin, Igor V., Yulia G. Izosimova, Ruslan A. Aimaletdinov, and Inna I. Tolpeshta. "Thermodynamic Stability of Clay Minerals in Boreal Forest Soil and Its Relationship to the Properties of Soil Organic Matter." Minerals 15, no. 4 (2025): 430. https://doi.org/10.3390/min15040430.

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This paper assesses the thermodynamic stability of clay minerals in the upper organo-mineral horizon of podzolic soil, as well as in the rhizosphere of Norway spruce (Picea abies (L.) H. Karst.) and Norway maple (Acer platanoides L.). Moreover, it determines the impact of soil organic matter on the thermodynamic stability of clay minerals. Calculations of ΔGf and the saturation index (SI) for clay minerals in laboratory experiments simulating soil conditions without soil moisture outflow allowed us to find out that the thermodynamic stability of clay minerals decreased in the series kaolinite
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23

Galan, E. "Properties and applications of palygorskite-sepiolite clays." Clay Minerals 31, no. 4 (1996): 443–53. http://dx.doi.org/10.1180/claymin.1996.031.4.01.

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AbstractThe palygorskite-sepiolite group of clay minerals has a wide range of industrial applications derived mainly from its sorptive, rheological and catalytic properties which are based on the fabric, surface area, porosity, crystal morphology, structure and composition of these minerals. For assessing potential industrial uses, the mineralogical and chemical composition of the clay and its basic physical and physico-chemical parameters must be determined. Then some particular properties of commercial interest can be modified and improved by appropriate thermal, mechanical and acid treatmen
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24

Wei, Chao Xian, and Ni Liang. "Sorption of Phenanthrene by Dissolved Organic Matters and their Complex with Iron Oxide Nanoparticles." Advanced Materials Research 1073-1076 (December 2014): 489–94. http://dx.doi.org/10.4028/www.scientific.net/amr.1073-1076.489.

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The environmental behavior of polycyclic aromatic hydrocarbons (PAHs) has attracted great research attention. However, their sorption mechanisms in organo-mineral complexes are still not specific enough. Batch sorption experiments with humic acid (HA) were carried out with iron oxide and their complexes adsorption phenanthrene (PHE) to determine the adsorption characteristics and mechanisms in this study. These results showed that the weakly polar and aromatic fractions of DOM preferentially adsorbed on the surface of iron oxide minerals. The organic matter (OM) binding on the surface of iron
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25

Ingrassia, Michela, Aida Maria Conte, Cristina Perinelli, et al. "Experimental vs. Natural Mineral Precipitation in Modern Microbialites: The Case Study of the Alkaline Bagno Dell’acqua Lake (Pantelleria Island, Italy)." Minerals 14, no. 10 (2024): 1013. http://dx.doi.org/10.3390/min14101013.

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Microbial activity has been documented in various lacustrine environments, suggesting its fundamental role in mineral precipitation and, therefore, in the formation of organo-deposits such as microbialites. Many studies are currently focused on documenting how the association of microbes and extracellular polymeric substances (EPSs) may influence the authigenesis of Mg-rich clay minerals and the subsequent carbonate precipitation in growing microbialites in lacustrine environments. In this study, we investigate the present-day microbialites of the alkaline Bagno dell’Acqua lake (Pantelleria Is
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26

Ymeti, Irena, Dhruba Pikha Shrestha, and Freek van der Meer. "Monitoring Soil Surface Mineralogy at Different Moisture Conditions Using Visible Near-Infrared Spectroscopy Data." Remote Sensing 11, no. 21 (2019): 2526. http://dx.doi.org/10.3390/rs11212526.

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The soil minerals determine essential soil properties such as the cation exchange capacity, texture, structure, and their capacity to form bonds with organic matter. Any alteration of these organo-mineral interactions due to the soil moisture variations needs attention. Visible near-infrared imaging spectroscopy is capable of assessing spectral soil constituents that are responsible for the organo-mineral interactions. In this study, we hypothesized that the alterations of the surface soil mineralogy occur due to the moisture variations. For eight weeks, under laboratory conditions, imaging sp
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27

Gürses, Ahmet, and Elif Şahin. "Preparation of Melamine Formaldehyde Foam and a Melamine-Formaldehyde-Organo-Clay Nanocomposite and Hybrid Composites." Minerals 13, no. 11 (2023): 1407. http://dx.doi.org/10.3390/min13111407.

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Mineral fillers can be added to thermoset polymers to improve thermal conductivity and deformation behavior, shrinkage, impact strength, dimensional stability and molding cycle time. This study aims to prepare various hybrid composites (MFHCs) using melamine formaldehyde foam (MF), a melamine formaldehyde organo-clay nanocomposite (MFNC) and also pumice as primary filler, and gypsum, kaolinite and a hollow glass sphere as secondary filler. It also focuses on the study of some mechanical properties and thermal conductivities, as well as their microscopic and spectroscopic characterization. For
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28

Yu, Xin Yang, Liu Yin Xia, Shuai Wang, and Hong Zhong. "The Synthesis of Novel Organosilicon Collector QAS222 and its Flotation Performance on Aluminosilicate Minerals." Advanced Materials Research 233-235 (May 2011): 2113–18. http://dx.doi.org/10.4028/www.scientific.net/amr.233-235.2113.

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In the article the organosilicon Quaternary Ammonium surfactant QAS222 was synthesized by one step reaction from silicane coupling agent and dodecyl amine, and its collecting ability to aluminosilicate minerals was investigated. The results showed that the percent conversion of dodecyl amine was more than 95% and the content of novel organosilicon in the production was about 96.53% when reaction was conducted at 80°C for 37 hours, with silicane coupling agent: N, N-Dimethyl dodecyl amine: KI=1.1:1:0.01 by the molar ratio, using anhydrous ethanol as solvent, protecting the reacting system with
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29

Koh, Sang-Mo, and Joe Boris Dixon. "Preparation and application of organo-minerals as sorbents of phenol, benzene and toluene." Applied Clay Science 18, no. 3-4 (2001): 111–22. http://dx.doi.org/10.1016/s0169-1317(00)00040-5.

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30

Kumari, Neeraj, Chandra Mohan, and Arvind Negi. "An Investigative Study on the Structural, Thermal and Mechanical Properties of Clay-Based PVC Polymer Composite Films." Polymers 15, no. 8 (2023): 1922. http://dx.doi.org/10.3390/polym15081922.

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The present study aims to explore the impact of pristine and surfactant-modified clays (montmorillonite, bentonite and vermiculite) on the thermomechanical properties of a poly (vinyl chloride) (PVC) polymer film. Initially, clay was modified by employing the ion exchange method. The modification of clay minerals was confirmed by the XRD pattern and thermogravimetric analysis. Pristine PVC polymer film and clay (montmorillonite, bentonite and vermiculite)-based PVC polymer composite films were fabricated using solution casting. The ideal dispersion of surfactant-modified organo-clays was obser
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31

Chiper (Petrea), Bianca-Mihaela, Mădălina Olaru, Crina-Loredana Turcu (Leonte), et al. "Long-Term Experiences with Fertilizers on Wheat and Maize Crops in the Pedoclimatic Conditions of the Bârlad Plateau." Romanian Agricultural Research 41 (2024): 445–56. http://dx.doi.org/10.59665/rar4143.

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A large number of long-term field experiments demonstrate that optimal application of nitrogen fertilizers to crops did not result in loss of organic matter, nor did it adversely affect soil microbial activity. Optimal use of fertilizers on agricultural crops reduces soil erosion, but repeated application of high doses of nitrogen fertilizer can lead to soil acidification, a negative trait of soil health. The main objective of this paper is to study the particular effect, interaction and complementarity of NP, NPK and organo-mineral fertilizers on the production of agricultural crops. This pap
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32

Kyryliuk, V. P. "Formation of the weed component of seads after the effect of long-term cultivation of soil." Interdepartmental thematic scientific collection "Agriculture" 1, no. 94 (2018): 32–37. http://dx.doi.org/10.31073/zem.94.32-37.

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The results of investigations of the influence of the long application of systems of main soil and fertilizer treatment on the quantitative indices of the weed component of soybean agrocenosis are described. The research was conducted in the four-field crop rotation of stationary experience in 2009-2016.&#x0D; It was found that the unploded system of main treatment compared with the plow, led to an increase in the number of weeds by 89% in mineral fertilizers and 104% in the organo-mineral. Vegetative crude mass of weeds on unplugged systems increased, comparatively with plow, on the backgroun
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33

Li, Huan, Zhenmin Hu, Qing Wan, Bing Mu, Guifei Li, and Yiyang Yang. "Integrated Application of Inorganic and Organic Fertilizer Enhances Soil Organo-Mineral Associations and Nutrients in Tea Garden Soil." Agronomy 12, no. 6 (2022): 1330. http://dx.doi.org/10.3390/agronomy12061330.

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Soil quality is one of the main factors that affect the growth and quality of tea (Camellia sinensis L.) plantations. The formation of the organo-mineral complex is one of the critical factors that influence the evolution of soil fertility. This study used chemical analyses and spectroscopy to study the effects of inorganic and organic fertilizer on the soil nutrients and organo-mineral complex in tea garden soil. SR-FTIR analysis revealed that clay minerals were connected as nuclei with the capacity to bind carbon, and that this interaction was aided by organic fertilization. Specifically, th
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34

Yang, Fan, Zibo Xu, Yuandong Huang, et al. "Stabilization of dissolvable biochar by soil minerals: Release reduction and organo-mineral complexes formation." Journal of Hazardous Materials 412 (June 2021): 125213. http://dx.doi.org/10.1016/j.jhazmat.2021.125213.

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35

Chen, Chunmei, and Donald L. Sparks. "Multi-elemental scanning transmission X-ray microscopy–near edge X-ray absorption fine structure spectroscopy assessment of organo–mineral associations in soils from reduced environments." Environmental Chemistry 12, no. 1 (2015): 64. http://dx.doi.org/10.1071/en14042.

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Environmental context Organo–mineral associations represent a fundamental process for stabilising organic carbon in soils. In this study, we employed scanning transmission X-ray microscopy–near edge X-ray absorption fine structure (STXM-NEXAFS) spectroscopy at C, Al and Si K-edges as well as Ca and Fe L-edges to conduct submicrometre-level investigations of the associations of C with mineral components in soils from reduced environments. This study provides the first insights into organo–mineral associations in reduced environments and shows progress towards examining, at the submicrometre lev
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36

Yang, Xuemei, Jie Zhang, Khan M. G. Mostofa, et al. "Solubility characteristics of soil humic substances as a function of pH: mechanisms and biogeochemical perspectives." Biogeosciences 22, no. 7 (2025): 1745–65. https://doi.org/10.5194/bg-22-1745-2025.

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Abstract. Soil humic substances (HSs) typically alter their electrochemical behaviours in the pH range of 1–12, which simultaneously regulates the stability of organo-minerals by modifying the HS functionalities. This process facilitates both biotic and abiotic transformations, which consequently leads to the export of degradative byproducts (e.g. HS components, nutrients) from soils into surrounding aquatic environments through water and/or rainwater discharges. However, the solubility features, environmental consequences, and mechanisms of HSs, including humic acids (HAs), fulvic acids (FAs)
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37

Liang, Ni, Di Zhang, and Min Wu. "Adsorption of Phenanthrene and Bisphenol A on Organo-Nano Iron Oxide Complexes." Advanced Materials Research 864-867 (December 2013): 1793–97. http://dx.doi.org/10.4028/www.scientific.net/amr.864-867.1793.

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Organo-mineral complexes are important in regulating the transport and retention of hydrophobic organic contaminants in soils/sediments. Humic acid will be fractionated during adsorption on mineral. This study examined the sorption of model compounds with different properties (tannin acid, gallic acid, fumaric acid sodium and sodium oleate) on nanoiron oxide minerals and determined the sorption of phenanthrene and Bisphenol A on these organooxide complexes. The results showed that the sorption of model compounds on nanoFe2O3 followed the order of O &gt; T &gt; G&gt; F. The higher adsorption of
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38

Seliem, Moaaz K., S. Komarneni, R. Parette, et al. "Perchlorate uptake by organosilicas, organo-clay minerals and composites of rice husk with MCM-48." Applied Clay Science 53, no. 4 (2011): 621–26. http://dx.doi.org/10.1016/j.clay.2011.05.012.

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39

Poirier, Vincent, Isabelle Basile-Doelsch, Jérôme Balesdent, Daniel Borschneck, Joann K. Whalen, and Denis A. Angers. "Organo-Mineral Interactions Are More Important for Organic Matter Retention in Subsoil Than Topsoil." Soil Systems 4, no. 1 (2020): 4. http://dx.doi.org/10.3390/soilsystems4010004.

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Decomposing crop residues contribute to soil organic matter (SOM) accrual; however, the factors driving the fate of carbon (C) and nitrogen (N) in soil fractions are still largely unknown, especially the influence of soil mineralogy and autochthonous organic matter concentration. The objectives of this work were (1) to evaluate the retention of C and N from crop residue in the form of occluded and mineral-associated SOM in topsoil (0–20 cm) and subsoil (30–70 cm) previously incubated for 51 days with 13C-15N-labelled corn residues, and (2) to explore if specific minerals preferentially control
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YLI-HALLA, M., D. L. MOKMA, and L. P. WILDING. "Formation of a cultivated spodosol in east-central Finland." Agricultural and Food Science 15, no. 1 (2008): 12. http://dx.doi.org/10.2137/145960606777245560.

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The processes involved in Spodosol (Podzol) formation are still being debated. The pedogenic processes in a Spodosol, 10,700 years-old, at Sotkamo that has been cultivated for about 50 years were studied by characterizing the morphology and analyzing the major chemical properties, texture and mineralogy. Before cultivation, organic acids produced by decomposition of organic matter from pine litter in O and A horizons had weathered primary minerals in A and E horizons releasing Al and Fe. Percolating waters moved the organo-metallic complexes from A and E horizons to Bhsm and Bs horizons where
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Phothitontimongkol, Theeradit, Nina Siebers, Nipaka Sukpirom, and Fuangfa Unob. "Preparation and characterization of novel organo-clay minerals for Hg(II) ions adsorption from aqueous solution." Applied Clay Science 43, no. 3-4 (2009): 343–49. http://dx.doi.org/10.1016/j.clay.2008.09.016.

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Pan, Yun Feng, Ya Qing Jiang, and Si Jia Zhang. "Study on the Effect of Condensate-Type and Copolymer-Type Combined Superplasticizers on Hydration of Cement." Key Engineering Materials 703 (August 2016): 360–64. http://dx.doi.org/10.4028/www.scientific.net/kem.703.360.

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For the limitation of single-component superplasticizer, condensate-type and copolymer-type combined superplasticizers were prepared. The adsorption of compound superplasticizers on cement paste was tested by Total Organic Carbon (TOC) measurement. Influences of superplasticizers on early hydration process of cement and Organo-mineral phase formation were studied by X-Ray Diffraction Analysis (XRD), Scanning Electron Microscope analysis (SEM) and so on. The results show that owing to the electrostatic repulsion and steric effect cooperative mechanism, condensate-type and copolymer-type combine
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Galicia-Andrés, Edgar, Chris Oostenbrink, Martin H. Gerzabek, and Daniel Tunega. "On the Adsorption Mechanism of Humic Substances on Kaolinite and Their Microscopic Structure." Minerals 11, no. 10 (2021): 1138. http://dx.doi.org/10.3390/min11101138.

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Soil organic matter (SOM) and various inorganic minerals represent key components of soils. During pedogenesis and due to biological activity these species interact, having a crucial impact on the formation of an aggregated soil structure with a hierarchical arrangement from nano to macro scale. In this process, the formation of organo–mineral microaggregates represents a dominant factor affecting soil functions and properties. This study focuses on the interactions between humic substances (HSs) and the mineral kaolinite as typical representatives of SOM and soil minerals. By performing class
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Rosendo-González, Verónica, Javier Illescas, María del Carmen Díaz-Nava, Yolanda Alvarado-Pérez, and José Juan García-Sánchez. "Synthesis and characterization of clay nanocomposites based on starch." MRS Advances 4, no. 59-60 (2019): 3243–49. http://dx.doi.org/10.1557/adv.2019.403.

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ABSTRACTIn this work, the synthesis of starch-clay nanocomposites was carried out. For this purpose, natural starch was extracted from rice grains and it was characterized by structural and spectrophotometric techniques. Afterwards, it was used as the polymer matrix for the synthesis of nanocomposites crosslinked with different agents: glycerol, citric acid (CA) and sodium trimetaphosphate (STMP). As a reinforcement phase, a natural Mexican clay from the Montmorillonite-type (Mt), was employed, which was modified with a cationic surfactant, hexadecyltrimethylammonium bromide (HDTMA-Br), in ord
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Wang, Yongzhuang, Joann K. Whalen, Xin Chen, et al. "Mechanisms for altering phosphorus sorption characteristics induced by low-molecular-weight organic acids." Canadian Journal of Soil Science 96, no. 3 (2016): 289–98. http://dx.doi.org/10.1139/cjss-2015-0068.

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Exudation of low-molecular-weight organic acids (LMWOAs) from plant roots enhances phosphorus (P) acquisition from soil, either by dissolving P fixed in secondary minerals or by reducing P sorption to organo-minerals. How LMWOAs may modify P sorption in soils with contrasting pH is not well understood, much less the mechanisms involved. The effects of three common LMWOAs (oxalic, citric, and malic acids) on P sorption in calcareous, neutral, and acidic soils were studied in batch experiments, followed by sequential P fractionation to elucidate the mechanisms whereby LMWOAs alter P sorption. Th
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Nwite, J., B. Eneruvie, and S. Nwafor. "Impact of Organo Minerals and Their Integrated Forms on Soil Fertility and Maize Productivity in Southeastern Nigeria." Journal of Agriculture and Ecology Research International 5, no. 3 (2016): 1–8. http://dx.doi.org/10.9734/jaeri/2016/15192.

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Lo, Irene Man-Chi. "Optimization in thickness of a liner composed of claymax® and organo-clay." Water Science and Technology 34, no. 7-8 (1996): 421–27. http://dx.doi.org/10.2166/wst.1996.0650.

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Present design philosophy reflects the uncertainty about the long-term effectiveness of liner systems by incorporating redundancy in the barrier layers through the concurrent use of both geosynthetic and clay minerals. A possible reason may be the lack of an engineering based design procedure for liners and a lack of a suitable optimization model which can be used to predict liner performance. In this study, Claymax® and Organo-Clay are chosen to be the liner materials because of their low hydraulic conductivity and high sorption capacity, respectively. The simulation model “Pollute 3.3” is co
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Polyakov, Vyacheslav, Alexey Petrov, and Evgeny Abakumov. "Micromorphological Characteristics of Fallow, Pyrogenic, Arable Soils of Central Part of Yakutia." Soil Systems 6, no. 3 (2022): 68. http://dx.doi.org/10.3390/soilsystems6030068.

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The assessment of the micromorphological characteristics of soils is a powerful tool for studying the transformation of soils under the influence of various weathering mechanisms (physical, biogenic). The central part of Yakutia is characterized by a large area of agricultural lands, some of which has become fallow land and is subject to cryogenic processes, fires and anthropogenic impact. Under the conditions of climate change, the fallow soils of Yakutia can be re-involved in the agricultural complex. To study their state, a method of micromorphological investigation of thin soil sections is
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Undabeytia, Tomas, Uri Shuali, Shlomo Nir, and Baruch Rubin. "Applications of Chemically Modified Clay Minerals and Clays to Water Purification and Slow Release Formulations of Herbicides." Minerals 11, no. 1 (2020): 9. http://dx.doi.org/10.3390/min11010009.

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This review deals with modification of montmorillonite and other clay-minerals and clays by interacting them with organic cations, for producing slow release formulations of herbicides, and efficient removal of pollutants from water by filtration. Elaboration is on incorporating initially the organic cations in micelles and liposomes, then producing complexes denoted micelle- or liposome-clay nano-particles. The material characteristics (XRD, Freeze-fracture electron microscopy, adsorption) of the micelle– or liposome–clay complexes are different from those of a complex of the same composition
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Litvinovich, A. V., O. Yu Pavlova, A. V. Lavrishchev, and A. A. Belimov. "Composition of organic-mineral complexes (OMC) migrating in the reclaimed sod-podzolic soils (Umbric Albeluvisol Abruptic)." E3S Web of Conferences 224 (2020): 04012. http://dx.doi.org/10.1051/e3sconf/202022404012.

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The composition of organo-mineral complexes (OMC) migrating from the arable horizon limed by Umbric Albeluvisol Abruptic was studied. The carbon content in organic-mineral complexes (OMC) ranged from 5.5 to 5.7%. The optical density index (Esmg/ml) varied in the range of values from 2.7 to 3.1, characteristic for fulvic acids (FA). It was established that FAs averaged with bases retain the ability to exert a destructive effect on soil minerals, transferring a significant amount of Al, Mn, and Fe into solution. According to their ability to migrate as part of OMC, the elements studied in the ex
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