Biotechnological Applications of the Sepiolite Interactions with Bacteria
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Halloysite Nanotubes Coated by Chitosan for the Controlled Release of Khellin
polymers Article Halloysite Nanotubes Coated by Chitosan for the Controlled Release of Khellin Lorenzo Lisuzzo 1 , Giuseppe Cavallaro 1,2,* , Stefana Milioto 1,2 and Giuseppe Lazzara 1,2 1 Dipartimento di Fisica e Chimica, Università degli Studi di Palermo, Viale delle Scienze, pad. 17, 90128 Palermo, Italy; [email protected] (L.L.); [email protected] (S.M.); [email protected] (G.L.) 2 Consorzio Interuniversitario Nazionale per la Scienza e Tecnologia dei Materiali, INSTM, Via G. Giusti, 9, I-50121 Firenze, Italy * Correspondence: [email protected]; Tel.: +39-091-2389-7962 Received: 9 July 2020; Accepted: 5 August 2020; Published: 7 August 2020 Abstract: In this work, we have developed a novel strategy to prepare hybrid nanostructures with controlled release properties towards khellin by exploiting the electrostatic interactions between chitosan and halloysite nanotubes (HNT). Firstly, khellin was loaded into the HNT lumen by the vacuum-assisted procedure. The drug confinement within the halloysite cavity has been proved by water contact angle experiments on the HNT/khellin tablets. Therefore, the loaded nanotubes were coated with chitosan as a consequence of the attractions between the cationic biopolymer and the halloysite outer surface, which is negatively charged in a wide pH range. The effect of the ionic strength of the aqueous medium on the coating efficiency of the clay nanotubes was investigated. The surface charge properties of HNT/khellin and chitosan/HNT/khellin nanomaterials were determined by ζ potential experiments, while their morphology was explored through Scanning Electron Microscopy (SEM). Water contact angle experiments were conducted to explore the influence of the chitosan coating on the hydrophilic/hydrophobic character of halloysite external surface. -
HIGH TEMPERATURE PHASES in SEPIOLITB, ATTAPULGITE and SAPONITE Gnoncrs Kulnrcrr,* Departmentof Geology, Uniters'ityof Lllinois, Urbana,Illinois
THE AMERICAN MINERALOGIST, VOL 44, JULY_AUGUST, 1959 HIGH TEMPERATURE PHASES IN SEPIOLITB, ATTAPULGITE AND SAPONITE Gnoncrs Kulnrcrr,* Departmentof Geology, Uniters'ityof lllinois, Urbana,Illinois. AssrnA.cr The high temperature reactions of sepiolite, attapulgite and saponite were studied by continuous high temperatute rc-ray diffraction techniques. The easy formation of enstatite from the fibrous minerals is explained by structural analogy. The reactions of the well crystallized specimens of sepiolite and attapulgite difier somewhat from those of their massive sedimentary varieties. The difierences cannot be ex- plained with the chemical and structural data, suggesting possible variations in some inti- mate details of the framework of these two varieties. INrnooucuox The nature of the crystalline phases formed by firing the magnesian clay mineralshas beendescribed (2,3,7, I0, 12,15, 16),but only for the well crystallized chlorites (3) have the precise conditions of formation of these phases as well as their structural relationships with the starting material been clearly determined. The three minerals chosenfor this investigation provide difierent struc- tural arrangementsof the same type of lattice in a series of Al-Mg hydrous silicates.Saponite and sepiolite have the same bulk composi- tion but they difier in the mode of assemblage,i.e. layers or ribbons, of their structural units. Attapulgite has the same kind of framework as sepiolite, but a large proportion of magnesium has been replaced by aluminum or iron. It was thought that, by taking advantage of these features and by using a method of continuous high-tempetature x-ray diffraction analysis,a new contribution to the problem would be possible. -
Functional Biohybrid Materials Based on Halloysite, Sepiolite and Cellulose Nanofibers for Health Cite This: Dalton Trans., 2020, 49, 3830 Applications†
Dalton Transactions View Article Online PAPER View Journal | View Issue Functional biohybrid materials based on halloysite, sepiolite and cellulose nanofibers for health Cite this: Dalton Trans., 2020, 49, 3830 applications† Lorenzo Lisuzzo, a,b Bernd Wicklein, b Giulia Lo Dico, a Giuseppe Lazzara, a Gustavo del Real, c Pilar Aranda b and Eduardo Ruiz-Hitzky *b Biohybrid materials were prepared by co-assembling the three following components: nanotubular hal- loysite, microfibrous sepiolite, and cellulose nanofibers dispersed in water, in order to exploit the most salient features of each individual component and to render homogeneous, flexible, yet strong films. Indeed, the incorporation of halloysite improves the mechanical performance of the resulting hybrid nanopapers and the assembly of the three components modifies the surface features concerning wetting properties compared to pristine materials, so that the main characteristics of the resulting materials become tunable with regard to certain properties. Owing to their hierarchical porosity together with their Creative Commons Attribution-NonCommercial 3.0 Unported Licence. Received 25th September 2019, diverse surface characteristics, these hybrids can be used in diverse biomedical/pharmaceutical appli- Accepted 28th November 2019 cations. Herein, for instance, loading with two model drugs, salicylic acid and ibuprofen, allows controlled DOI: 10.1039/c9dt03804c and sustained release as deduced from antimicrobial assays, opening a versatile path for developing other rsc.li/dalton related -
Spring 1995 Gems & Gemology
TABLE CONTENTS FEATURE ARTICLES 2 Rubies from Mong Hsu Adolf Pelsetti, I(ar7 Schmetzer, Heinz-Jiirgen Bernhardt, and Fred Mouawad " 28 The Yogo Sapphire Deposit Keith A. ~~chaluk NOTES AND NEW TECHNIQUES 42 Meerschaum from Eskisehir Province, Turkey I<adir Sariiz and Islcender Isilc REGULAR FEATURES 52 Gem Trade Lab Notes Gem News Most Valuable Article Award Gems ed Gemology Challenge Book Reviews Gemological Abstracts Guidelines for Authors ABOUT THE COVER: One of the most important ruby localities of the 1990s cov- ers a broad orea near the town of Mong Hsu, in northeastern Myann~ar(B~lrrna). The distinctive gemological features of these rubies are detailed in this issue's lead article. The suite of fine jewelry illustraled here contains 36 Mong Hsu rubies with a total weigh1 of 65.90 ct; the two rubies in the ring total 5.23 ct. jewelry courtesy of Mouawad jewellers. Photo by Opass Sultsumboon-Opass Suksuniboon Studio, Bangltolz, Thailand. Typesetting for Gerrls eS Gemology is by Graphix Express, Santa Monica, CA. Color separations are by Effective Graphics, Compton, CA. Printing is by Cadmus lournal Services, Easton, MD. 0 1995 Gemological Institute of America All rights reserved ISSN 0016-626X - Editor-in-Chief Editor Editors, Gem Trade Lab Notes Richard T. Lidtlicoat Alicc S. I<cller Robcrt C. I<ammerling 1660 Stewart St. C. W. Fryer Associate Editors Smta Mon~ca,CA 90404 William E. Boyajian Editors, Gem News (800)421-7250 ~251 Robcrt C. Kamn~erling Rohcrt C. I<ammerling e-mail: altellcrBclass.org D. Vincent Manson John I. Koivula John Sinltanltas Sr~bscriptions Enirnanuel Fritsch Jln Ll~n Editors, Book llevielvs Technical Editor (800) 421-7250 x201 Susan B. -
INVESTMENT CLIMATE of ESKİŞEHİR
2017 INVESTMENT CLIMATE of ESKİŞEHİR INVESTMENT CLIMATE of ESKİŞEHİR 1 April 2017 INDEX 1. ABOUT BEBKA 4 2. FACTS AND FIGURES 5 3. LOCATION AND TRANSPORTATION 10 4. SOCIAL LIFE 11 5. ECONOMY 13 6. LABOR 15 7. FOREIGN TRADE 15 8. SECTORS 19 9. CLUSTERING 23 10. SPECIAL INVESTMENT ZONES 24 11. UNIVERSITIES 25 12. R&D AND INNOVATION 28 13. FOREIGN INVESTMENTS 28 14. INVESTMENT INCENTIVE SYSTEM 29 15. COSTS 32 16. WHY ESKİŞEHİR? 32 BIBLIOGRAPHY 33 INVESTMENT CLIMATE of ESKİŞEHİR 2017 2017 INVESTMENT CLIMATE of ESKİŞEHİR 1. ABOUT BEBKA Bursa Eskişehir Bilecik Development Agency (BEBKA) was established with the decision of the Council of Ministers dated July 14, 2009 and numbered 2009/15236 on the basis of Law No. 5449 on the Establishment, Coordination and Duties of Development Agencies dated 25.01.2006. BEBKA is an institution that provides solutions for local problems by providing coordination and cooperation between the public, private sector and non-governmental organizations, providing solutions locally and providing sustainable development by using resources in place and effectively in Bursa, Eskişehir and Bilecik provinces. BEBKA’s main goal is to reduce intra-regional development disparities by providing coordination and cooperation between the public sector, private sector, civil society and universities. In line with this objective, 2014-2023 Bursa Eskişehir Bilecik Regional Plan, which defines BEBKA’s regional priorities with scientific methods and participa- tory approach, has been prepared. Within the framework of this regional plan, a model has been developed to guide development of project finan- cing support, training needs, investment and promotion possibilities. -
Crystallochemical Characterization of the Palygorskite and Sepiolite from the Allou Kagne Deposit, Senegal
CRYSTALLOCHEMICAL CHARACTERIZATION OF THE PALYGORSKITE AND SEPIOLITE FROM THE ALLOU KAGNE DEPOSIT, SENEGAL 2 E. GARCÍA-RoMER01,*, M. SUÁREZ , J. SANTARÉN3 AND A. ALVAREZ3 1 Departamento de Cristalografía y Mineralogía, Universidad Complutense de Madrid, E-28040 Madrid, Spain 2 Departamento de Geología, Universidad de Salamanca, E-37008 Salamanca, Spain 3 TOLSA Ctra Vallecas-Mejorada del Campo, km 1600, 28031 Madrid, Spain Abstract-The Allou Kagne (Senegal) deposit consists of different proportions of palygorskite and sepiolite, and these are associated with small quantities of quartz and X-ray amorphous silica as impurities. No pure palygorskite or sepiolite has been recognized by X-ray diffraction. Textural and microtextural features indicate that fibrous clay minerals ofthe Allou Kagne deposit were formed by direct precipitation from solution. Crystal-chemistry data obtained by analyticalltransmission electron microscopy (AEMI TEM) analyses of isolated fibers show that the chemical composition of the particles varies over a wide range, from a composition corresponding to palygorskite to a composition intermediate between that of sepiolite and palygorskite, but particles with a composition corresponding to sepiolite have not been found. Taking mto account the results from selected area electron diffraction and AEM-TEM, fibers of pure palygorskite and sepiolite have been found but it cannot be confirmed that all of the particles analyzed correspond to pure palygorskite or pure sepiolite because both minerals can occur together at the crystallite scale. In addition, the presence ofMg-rich palygorskite and very Al-rich sepiolite can be deduced. It is infrequent in nature that palygorskite and sepiolite appear together because the conditions for simultaneous formation ofthe two minerals are very restricted. -
Microbial Interaction with Clay Minerals and Its Environmental and Biotechnological Implications
minerals Review Microbial Interaction with Clay Minerals and Its Environmental and Biotechnological Implications Marina Fomina * and Iryna Skorochod Zabolotny Institute of Microbiology and Virology of National Academy of Sciences of Ukraine, Zabolotny str., 154, 03143 Kyiv, Ukraine; [email protected] * Correspondence: [email protected] Received: 13 August 2020; Accepted: 24 September 2020; Published: 29 September 2020 Abstract: Clay minerals are very common in nature and highly reactive minerals which are typical products of the weathering of the most abundant silicate minerals on the planet. Over recent decades there has been growing appreciation that the prime involvement of clay minerals in the geochemical cycling of elements and pedosphere genesis should take into account the biogeochemical activity of microorganisms. Microbial intimate interaction with clay minerals, that has taken place on Earth’s surface in a geological time-scale, represents a complex co-evolving system which is challenging to comprehend because of fragmented information and requires coordinated efforts from both clay scientists and microbiologists. This review covers some important aspects of the interactions of clay minerals with microorganisms at the different levels of complexity, starting from organic molecules, individual and aggregated microbial cells, fungal and bacterial symbioses with photosynthetic organisms, pedosphere, up to environmental and biotechnological implications. The review attempts to systematize our current general understanding of the processes of biogeochemical transformation of clay minerals by microorganisms. This paper also highlights some microbiological and biotechnological perspectives of the practical application of clay minerals–microbes interactions not only in microbial bioremediation and biodegradation of pollutants but also in areas related to agronomy and human and animal health. -
Comparison of Phyllosilicates Observed on the Surface of Mars with Those Found in Martian Meteorites
80th Annual Meeting of the Meteoritical Society 2017 (LPI Contrib. No. 1987) 6115.pdf COMPARISON OF PHYLLOSILICATES OBSERVED ON THE SURFACE OF MARS WITH THOSE FOUND IN MARTIAN METEORITES. J. L. Bishop1, and M. A. Velbel2,3, 1SETI Institute & NASA-Ames (Mountain View, CA, USA; [email protected]), 2Michigan State University (East Lansing, MI); 3Smithsonian Institution (Washington, DC). Introduction: Phyllosilicates are an important indicator of aqueous processes on Mars and have been observed on the martian surface as well as inside martian meteorites. Here we survey the types of phyllosilicates detected at the surface of Mars and inside martian rocks in order to gain a better understanding of aqueous alteration processes taking place at Mars. Comparing the phyllosilicates observed on the surface today with those found in meteorites [1] may provide clues toward understanding which phyllosilicates formed in surface environments and which formed through subsurface processes. Martian Surface: Fe/Mg-phyllosilicates are present in numerous sites where the Noachian rocks are exposed [2]. These have been detected and characterized with the OMEGA [3] and CRISM [4] imaging spectrometers. Fe- rich smectite is the most abundant phyllosilicate on the surface of Mars [5], but a large variety of phyllosilicates and short-range-ordered (SRO) materials [6] have been observed. These include: nontronite, saponite, clinochlore, chamosite, serpentine, prehnite, talc, illite, beidelite, montmorillonite, kaolinite, halloysite, opal, hydrated silica, allophane, and imogolite. These are often observed together with iron oxides/hydroxides (FeOx), sulfates or car- bonates. Phyllosilicates and SROs have also been detected on Mars by CheMin on MSL [7]. Analyses of these data from several locations indicate the presence of trioctahedral and dioctahedral smectites and SRO phases [8, 9]. -
Suspension Polymerization of Methyl Methacrylate Stabilized Solely by Palygorskite Nano Fibers*
Chinese Journal of Polymer Science Vol. 32, No. 2, (2014), 123−129 Chinese Journal of Polymer Science © Chinese Chemical Society Institute of Chemistry, CAS Springer-Verlag Berlin Heidelberg 2014 Rapid Communication Suspension Polymerization of Methyl Methacrylate Stabilized Solely by Palygorskite Nano Fibers* Bai-yu Li**, Yin-ping Wang, Xiao-bin Niu and Zai-man Liu The School of Chemical & Biological Engineering, Lanzhou Jiaotong University, Lanzhou 730070, China Abstract A kind of fibrous clay, palygorskite (PAL), was used as the sole stabilizer in suspension polymerization without the using of any other stabilizer usually used, especially polymeric stabilizers. In order to improve the compatibility with the organic monomer, PAL nano fibers were organically modified with silane coupling agent methacryloxypropyltrimethoxysilane (MPS). Transmission electron microscopy (TEM) and Fourier-transform infrared (FTIR) spectroscopy results show that the hydrolyzed MPS was attached onto PAL surface through Si―O―Si bonds formation without morphology change of PAL. At a loading amount of PAL to monomer as low as 0.36 wt%, effective stabilization could be achieved. After suspension polymerization, spherical poly(methyl methacrylate) (PMMA) particles were obtained. Scanning electron microscopy (SEM) analysis on both the outer surface and the inner cracked surface of the spherical PMMA particles indicates that the PAL particles reside on the surface of the PMMA spheres. The densely stacked PAL together with attached silane coupling agent stabilized -
FIBROUS SEPIOLITE from YAVAPAI COUNTY, ARIZONA Ar-Nbnr J
FIBROUS SEPIOLITE FROM YAVAPAI COUNTY, ARIZONA Ar-nBnrJ. Knuuue.N, Jn.,* Columbia Uniaersit"t.Neut Yorh. eua"*o* Data yielded by chemical, optical, and r-ray methods of analysis identifies a hydrous magnesium silicate from Yavapai county, Arizona, as fibrous sepiolite. The study of this specimen is of interest because of the further information it yields concerning the nature of sepiolite. The literature may profit from more coordinated chemical, optical, and r-ray data on this mineral. The term'parasepiolite'is justified rather than sepiolite when refer- ring to the fibrous, highly crystalline variety of this material. A rather complete bibliog- raphy of sepiolite is included, in addition to the references cited. OccunnnNcn The hydrous magnesium silicate describedherein occurs in a contact zone situated about a half mile south of the Santa Maria River near the western boundary of Yavapai County and about 40 miles, by road, in a westerly direction from CongressJunction, Arizona. This locality, in southwestern Yavapai County, is in the ruggedly dissected basin of the Santa Maria River west of the Mccloud Moun- tains, a granite range that attains a height of 4900 feet. The region is composedmainly of granite, gneiss,and schist intruded by various dikes and stocks and overlain in places by mesa-forming lavas. This deposit was prospected thoroughly by the R. T. Vanderbilt Co., New York, but was found to be too limited in extent for commercial development. Puysrcar, Pnopenrrns In a hand specimen this material is white, massive, and compact with a foliated structure. The surfaceis smooth with a dull luster that assumes a polish with slight rubbing. -
Variability in Sepiolite: Diffraction Studies
American Mineralogist, Volume 96, pages 1443–1454, 2011 Variability in sepiolite: Diffraction studies MANUEL SÁNCHEZ DEL RÍO,1,* EMILIA GARCÍA-ROMERO,2,6 MERCEDES SUÁREZ,3 IVÁN DA SILVA,4 LUIS FUENTES-MONTERO,5 AND GEMA MARTÍNEZ-CRIADO1 1European Synchrotron Radiation Facility, 6 rue Jules Horowitz, 38000 Grenoble, France 2Departamento de Cristalografía y Mineralogía, Universidad Complutense de Madrid, 28040 Madrid, Spain 3Departamento de Geología. Universidad de Salamanca, Patio de Escuelas 1, 37008 Salamanca, Spain 4Spline Spanish CRG Beamline at the European Synchrotron Radiation Facility, 6 rue Jules Horowitz, 38000 Grenoble, France 5Institut Laue-Langevin, 6 rue Jules Horowitz, 38000 Grenoble, France 6Instituto de Geociencias (UCM-CSIC), 28040 Madrid, Spain ABSTRACT Twenty sepiolites of known composition from different origins were analyzed to quantify the variability in structural parameters and its possible relationships with composition and morphology. Morphology SEM analyses led to classify the sepiolites into several groups, beyond the two simple macroscopic or clay groups. X-ray powder diffraction with synchrotron light was used to discuss the variability of the a and b cell parameters with the nature of the cations and occupancy of the octahedral shell. Rietveld refinement using the ideal sepiolite model is performed on sepiolites at two tempera- tures: 225 °C (for zeolitically dehydrated sepiolite) and 25 °C (for hydrated ambient sepiolite). The latter permitted to locate ca. six molecules of the zeolitic H2O within the tunnels. A few samples were selected to evaluate the feasibility and potential of single-crystal diffraction methods: X-ray microdiffraction and electron diffraction. The macroscopic sepiolites gave well- structured and rich X-ray fiber diffraction patterns, in excellent agreement with ab initio simulations. -
Influence of Additives on Sepiolite
International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 07 Issue: 02 | Feb 2020 www.irjet.net p-ISSN: 2395-0072 INFLUENCE OF ADDITIVES ON SEPIOLITE Jiji Joseph1, Anila Angel P. R.2 1Student, Department of Civil Engineering, Marian Engineering College, Kerala, India 2 Assistant Professor, Department of Civil Engineering, Marian Engineering College, Kerala, India -------------------------------------------------------------------***--------------------------------------------------------------------- Abstract - The soil strength and its characteristics can be Materials can be viable alternatives to compacted clays, and can improved by mixing it with various additives. Sepiolite is a provide significant cost savings if the material is nearby cheap and transportation is not required. (Abichou et al. 2004). naturally occurring clay mineral. The additive is mixed with However, these alternative geomaterials may also exhibit some sepiolite at various percentages and properties such as specific characteristics that would not be desirable in landfill design. For gravity, pH, Atterberg limits, compaction characteristics, UCC, instance, bentonite-amended sands permeated with chemical and permeability are studied. In this study the sepiolite is mixed solutions and landfill leachate were reported to exhibit with two different additives, fly ash and kaolinite. The fly ash is significantly higher hydraulic conductivity than the hydraulic added to the sepiolite with 2%, 4% and 6% and the variation of conductivity of same mixtures permeated with water (Alther 1987). Mitchell and Madsen (1987) and Jo et al. (2001) reported properties are found out. 25% and 50% Kaolinite is mixed with that several factors, including valence of cation, concentration of sepiolite and variation of properties is studied. The the salt solution, and the pH of the medium, affect hydraulic improvement in the soil properties are reported with additives conductivity of bentonite.