Colloidal Dispersion: 1.Basing on Charge- (+), (-) 2.Basing on State of Matter – Solid, Liquid, Gas
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Effect of Electrolyte Addition on the Colloidal Stability of Aqueous Zeolite Sols
First published in: 2550 Helvetica Chimica Acta ± Vol. 84 (2001) Effect of Electrolyte Addition on the Colloidal Stability of Aqueous Zeolite Sols by Torsten Mäurer and Bettina Kraushaar-Czarnetzki*1) Institute of Chemical Process Engineering CVT, University of Karlsruhe (TH), D-76128 Karlsruhe Dedicated to Professor Andre M. Braun on the occasion of his 60th birthday Recovery of zeolites from aqueous media can be a very difficult operation, when the crystals have colloidal dimensions. The solid-liquid separation can be facilitated by processing at the respective isoelectric point (IEP) where the sol is unstable and the crystals form aggregates. The addition of salts results in a further improvement, because the zeolite agglomerates become larger, and the pH range of flocculation is broadened. This wider operational window, in particular, is of importance for the recovery of zeolites that would dealuminate or collapse at their respective IEP. Introduction. ± Handling of aqueous sols or suspensions of zeolite crystals is a frequently recurring operation in the manufacturing of zeolite-based catalysts or adsorbents. Starting with the zeolite synthesis in aqueous medium, the typical workup comprises repeated ion exchange in aqueous solutions and, finally, a wet shaping process during which bodies of suitable size, shape, strength, pore texture, and site distribution must be formed. Large agglomerates of crystals are beneficial, when zeolites must be recovered from their mother liquor or from ion-exchange solutions, whereas isolated zeolite single crystals, dispersed in the porous matrix of a shaped particle, are highly desirable when catalytic properties are to be optimized. These opposing require- ments for efficient solid-liquid separations, on one hand, and optimum product quality, on the other hand, demand for means to control the particle size in a reversible manner. -
Mechanical Dispersion of Clay from Soil Into Water: Readily-Dispersed and Spontaneously-Dispersed Clay Ewa A
Int. Agrophys., 2015, 29, 31-37 doi: 10.1515/intag-2015-0007 Mechanical dispersion of clay from soil into water: readily-dispersed and spontaneously-dispersed clay Ewa A. Czyż1,2* and Anthony R. Dexter2 1Department of Soil Science, Environmental Chemistry and Hydrology, University of Rzeszów, Zelwerowicza 8b, 35-601 Rzeszów, Poland 2Institute of Soil Science and Plant Cultivation (IUNG-PIB), Czartoryskich 8, 24-100 Puławy, Poland Received July 1, 2014; accepted October 10, 2014 A b s t r a c t. A method for the experimental determination of Clay particles can either flocculate or disperse in aque- the amount of clay dispersed from soil into water is described. The ous solution. When flocculation occurs, the particles com- method was evaluated using soil samples from agricultural fields bine to form larger, compound particles such as soil in 18 locations in Poland. Soil particle size distributions, contents microaggregates. When dispersion occurs, the particles of organic matter and exchangeable cations were measured by separate in suspension due to their electrical charge. Clay standard methods. Sub-samples were placed in distilled water flocculation leads to soils that are considered to be stable in wa- and were subjected to four different energy inputs obtained by ter whereas dispersion is associated with soils that are consi- different numbers of inversions (end-over-end movements). The dered to be unstable in water. We may note that this termi- amounts of clay that dispersed into suspension were measured by light scattering (turbidimetry). An empirical equation was devel- nology is the opposite of that used in colloid science where oped that provided an approximate fit to the experimental data for the terms ‘stable’ and ‘unstable’ are used in relation to the turbidity as a function of number of inversions. -
Colloidal Suspensions
Chapter 9 Colloidal suspensions 9.1 Introduction So far we have discussed the motion of one single Brownian particle in a surrounding fluid and eventually in an extaernal potential. There are many practical applications of colloidal suspensions where several interacting Brownian particles are dissolved in a fluid. Colloid science has a long history startying with the observations by Robert Brown in 1828. The colloidal state was identified by Thomas Graham in 1861. In the first decade of last century studies of colloids played a central role in the development of statistical physics. The experiments of Perrin 1910, combined with Einstein's theory of Brownian motion from 1905, not only provided a determination of Avogadro's number but also laid to rest remaining doubts about the molecular composition of matter. An important event in the development of a quantitative description of colloidal systems was the derivation of effective pair potentials of charged colloidal particles. Much subsequent work, largely in the domain of chemistry, dealt with the stability of charged colloids and their aggregation under the influence of van der Waals attractions when the Coulombic repulsion is screened strongly by the addition of electrolyte. Synthetic colloidal spheres were first made in the 1940's. In the last twenty years the availability of several such reasonably well characterised "model" colloidal systems has attracted physicists to the field once more. The study, both theoretical and experimental, of the structure and dynamics of colloidal suspensions is now a vigorous and growing subject which spans chemistry, chemical engineering and physics. A colloidal dispersion is a heterogeneous system in which particles of solid or droplets of liquid are dispersed in a liquid medium. -
Known As the Dispersed Phase), Distributed Throughout a Continuous Phase (Known As Dispersion Medium)
COLLOIDAL DISPERSIONS Dispersed systems consist of particulate matter (known as the dispersed phase), distributed throughout a continuous phase (known as dispersion medium). CLASSIFICATION OF DISPERSED SYSTEMS On the basis of mean particle diameter of the dispersed material, three types of dispersed systems are generally considered: a) Molecular dispersions b) Colloidal dispersions, and c) Coarse dispersions Molecular dispersions are the true solutions of a solute phase in a solvent. The solute is in the form of separate molecules homogeneously distributed throughout the solvent. Example: aqueous solution of salts, glucose Colloidal dispersions are micro-heterogeneous dispersed systems. The dispersed phases cannot be separated under gravity or centrifugal or other forces. The particles do not mix or settle down. Example: aqueous dispersion of natural polymer, colloidal silver sols, jelly Coarse dispersions are heterogeneous dispersed systems in which the dispersed phase particles are larger than 0.5µm. The concentration of dispersed phase may exceed 20%. Example: pharmaceutical emulsions and suspensions COMPARISON OF CHARACTERISTICS THREE DISPERSED SYSTEMS Molecular dispersions Colloidal dispersions Coarse dispersions 1. Particle size <1 nm 1 nm to 0.5 µm >0.5 µm 2. Appearance Clear, transparent Opalescent Frequently opaque 3. Visibility Invisible in electron Visible in electron Visible under optical microscope microscope microscope or naked eye 4. Separation Pass through semipermeable Pass through filter paper but Do not pass through -
CHAPTER 3 Transport and Dispersion of Air Pollution
CHAPTER 3 Transport and Dispersion of Air Pollution Lesson Goal Demonstrate an understanding of the meteorological factors that influence wind and turbulence, the relationship of air current stability, and the effect of each of these factors on air pollution transport and dispersion; understand the role of topography and its influence on air pollution, by successfully completing the review questions at the end of the chapter. Lesson Objectives 1. Describe the various methods of air pollution transport and dispersion. 2. Explain how dispersion modeling is used in Air Quality Management (AQM). 3. Identify the four major meteorological factors that affect pollution dispersion. 4. Identify three types of atmospheric stability. 5. Distinguish between two types of turbulence and indicate the cause of each. 6. Identify the four types of topographical features that commonly affect pollutant dispersion. Recommended Reading: Godish, Thad, “The Atmosphere,” “Atmospheric Pollutants,” “Dispersion,” and “Atmospheric Effects,” Air Quality, 3rd Edition, New York: Lewis, 1997, pp. 1-22, 23-70, 71-92, and 93-136. Transport and Dispersion of Air Pollution References Bowne, N.E., “Atmospheric Dispersion,” S. Calvert and H. Englund (Eds.), Handbook of Air Pollution Technology, New York: John Wiley & Sons, Inc., 1984, pp. 859-893. Briggs, G.A. Plume Rise, Washington, D.C.: AEC Critical Review Series, 1969. Byers, H.R., General Meteorology, New York: McGraw-Hill Publishers, 1956. Dobbins, R.A., Atmospheric Motion and Air Pollution, New York: John Wiley & Sons, 1979. Donn, W.L., Meteorology, New York: McGraw-Hill Publishers, 1975. Godish, Thad, Air Quality, New York: Academic Press, 1997, p. 72. Hewson, E. Wendell, “Meteorological Measurements,” A.C. -
Colloid Stability 3 Kinetics of Coagulation Lyophobic Dispersions Are Never Stable in the Thermodynamic Sense, but Exhibit Some Degree of Instability
1 المحاضرة الثالثة – ثالثة علوم كيمياء Colloid stability 3 Kinetics of coagulation Lyophobic dispersions are never stable in the thermodynamic sense, but exhibit some degree of instability. From a practical point of view, the word 'stable' is often loosely used to describe a dispersion in which the coagulation rate is slow in relation to its required 'shelf life'. The rate at which a sol coagulates depends on the frequency with which the particles encounter one another and the probability that their thermal energy is sufficient to overcome the repulsive potential energy barrier to coagulation when these encounters take place. The rate at which particles aggregate is given by dn k n2 dt 2 Where n is the number of particles per unit volume of sol at time t, and k2 is a second-order rate constant, Integrating, and putting n - no at t = 0, 1 1 gives kt (16) n no During the course of coagulation k2 usually decreases, and sometimes an equilibrium state is reached with the sol only partially coagulated. This may be a consequence of the height of the repulsion energy barrier increasing with increasing particle size. In experimental tests of stability theories it is usual to restrict measurements to the early stages of coagulation (where the aggregating mechanism is most straightforward), using moderately dilute sols. The particle concentration during early stages of coagulation can be determined directly, by visual particle counting, or indirectly, from turbidity (spectrophotometric or light scattering) measurements. If necessary, coagulation in an aliquot of sol can be halted prior to 2 examination by the addition of a small amount of a stabilizing agent, such as gelatin. -
Eco-Friendly Colloidal Aqueous Sol-Gel Process for Tio2 Synthesis: the Peptization Method to Obtain Crystalline and Photoactive Materials at Low Temperature
catalysts Review Eco-Friendly Colloidal Aqueous Sol-Gel Process for TiO2 Synthesis: The Peptization Method to Obtain Crystalline and Photoactive Materials at Low Temperature Julien G. Mahy 1,* , Louise Lejeune 1, Tommy Haynes 1 , Stéphanie D. Lambert 2 , Raphael Henrique Marques Marcilli 3, Charles-André Fustin 3 and Sophie Hermans 1,* 1 Molecular Chemistry, Materials and Catalysis (MOST), Institute of Condensed Matter and Nanosciences (IMCN), Université Catholique de Louvain, Place Louis Pasteur 1, B-1348 Louvain-la-Neuve, Belgium; [email protected] (L.L.); [email protected] (T.H.) 2 Department of Chemical Engineering—Nanomaterials, Catalysis, Electrochemistry, B6a, University of Liège, B-4000 Liège, Belgium; [email protected] 3 Bio and Soft Matter Division (BSMA), Institute of Condensed Matter and Nanosciences (IMCN), Université Catholique de Louvain, Place Louis Pasteur 1, B-1348 Louvain-la-Neuve, Belgium; [email protected] (R.H.M.M.); [email protected] (C.-A.F.) * Correspondence: [email protected] (J.G.M.); [email protected] (S.H.); Tel.: +32-10-47-28-10 (S.H.) Abstract: This work reviews an eco-friendly process for producing TiO via colloidal aqueous sol– 2 gel synthesis, resulting in crystalline materials without a calcination step. Three types of colloidal Citation: Mahy, J.G.; Lejeune, L.; aqueous TiO2 are reviewed: the as-synthesized type obtained directly after synthesis, without any Haynes, T.; Lambert, S.D.; specific treatment; the calcined, obtained after a subsequent calcination step; and the hydrothermal, Marcilli, R.H.M.; Fustin, C.-A.; obtained after a specific autoclave treatment. This eco-friendly process is based on the hydrolysis of a Hermans, S. -
Gravimetric Analysis – Skoog Book • Page 179-198 Do Problems: 1,2,4,9,10,11,14,16,21,27,30,33
Gravimetric Methods of Analysis • Chapter 8 Gravimetric Analysis – Skoog Book • Page 179-198 Do Problems: 1,2,4,9,10,11,14,16,21,27,30,33 • Chapter 9 Electrolyte Effects Activities – effective concentration and equilibrium • Chapter 10 Complex Equilibria – similar but a few steps we have not looked at Gravimetric Analysis • Gravimetric Analysis--quantitative technique based on the determination of the mass of a precipitated or volatized compound which the analyte is stoichiometrically related • Analyte: the substance determined in the procedure. – converted to an insoluble form, collected and massed on an analytical balance. • Reaction: aA + rR ===> AaRr (s) Analyte Precipitating Precipitate that we will dry, Agent mass and relate to analyte Gravimetry Vacuum Filteration Set Up Aspirator Buchner Funnel Filter Filter Paper Adaptor Rubber tubing Filter Flask Mother Liquor Mechanicism of Precipitation • Two Competing Processes – Nucleation vs Particle Growth Representative Gravimetry Representative Gravimetry Mechanicism of Precipitation • Two Competing Processes – Nucleation vs Particle Growth Desirable! Creating “Ideal” Precipitates • Now let’s learn more about precipitate formation in particular colloids and crystalline precipitates precipitating agent AgNO (aq) + NaCl(aq) AgCl(s) + NaNO (aq) 3 ←−→ 3 Colloidal Double Layer Model - - • If we add Cl we run out of Cl and NO3 “fills” in Precipitates Vary And Complicate ! Particle Size of the precipitate is determined by a number of factors, such as ! Relative supersaturation (RSS) ! Mechanism of formation: nucleation vs particle growth ! Experimental control: pH, temperature, mixing, ! Supersaturation occurs when precip. agent is added to analyte. • System reacts to reach equilibrium (Q > Ksp). It does this by “nucleation”. • Nucleation is not desirable as the particles are small. -
Cationic Surfactant Templated Synthesis of Magnetic Mesoporous Nanocomposites for Efficient Removal of Light Green
Korean J. Chem. Eng., 38(7), 1425-1437 (2021) pISSN: 0256-1115 DOI: 10.1007/s11814-021-0829-x eISSN: 1975-7220 INVITED REVIEW PAPER INVITED REVIEW PAPER Cationic surfactant templated synthesis of magnetic mesoporous nanocomposites for efficient removal of Light Green Beyhan Erdem*,†, Sezer Erdem**, and Nalan Tekin*** *Department of Chemistry, Faculty of Science and Arts, Bursa Uludag University, 16059, Bursa, Turkey **Department of Physics, Faculty of Science and Arts, Bursa Uludag University, 16059, Bursa, Turkey ***Department of Chemistry, Faculty of Science and Arts, Kocaeli University, 41380, Kocaeli, Turkey (Received 25 December 2020 • Revised 26 April 2021 • Accepted 29 April 2021) Abstract Fe3O4-SiO2-NH2, Fe3O4-CTABSiO2-NH2 and Fe3O4-SiO2-CTABSiO2-NH2 magnetic adsorbents were suc- cessfully prepared and could be used effectively for the adsorption of Light Green from aqueous solutions. Unlike the first sample, mesoporous silica coatings were created using cetyltrimethylammoniumbromide micelles as molecular templates on superparamagnetic iron oxide in one sample, and on silica-coated iron oxide in the other sample to improve the adsorptive properties of the nanocomposites. The characterization by FT-IR, SEM/EDX, Zeta-potential, XRD, VSM, and N2-adsorption/desorption confirmed the production of mesoporous silica layer. Although coating pro- cesses with both silica and mesoporous silica layers led to a vaguely decrease in saturation magnetization of the Fe3O4- SiO2-CTABSiO2-NH2, the nanoparticles were protected with silica coatings -
Control of the Textural Properties of Nanocrystalline Boehmite (-Alooh
Control of the textural properties of nanocrystalline boehmite (γ-AlOOH) regarding its peptization ability Fouad Karouia, Malika Boualleg, Mathieu Digne, Pierre Alphonse To cite this version: Fouad Karouia, Malika Boualleg, Mathieu Digne, Pierre Alphonse. Control of the textural properties of nanocrystalline boehmite (γ-AlOOH) regarding its peptization ability. Powder Technology, Elsevier, 2013, vol. 237, pp. 602-609. 10.1016/j.powtec.2012.12.054. hal-01167383 HAL Id: hal-01167383 https://hal.archives-ouvertes.fr/hal-01167383 Submitted on 24 Jun 2015 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Open Archive TOULOUSE Archive Ouverte ( OATAO ) OATAO is an o pen access repository that collects the work of Toulouse researchers and makes it freely available over the web where possible. This is an author-deposited version published in : http://oatao.univ-toulouse.fr/ Eprints ID : 13997 To link to this article : doi: 10.1016/j.powtec.2012.12.054 URL : http://dx.doi.org/10.1016/j.powtec.2012.12.054 To cite this version : Karouia, Fouad and Boualleg, Malika and Digne, Mathieu and Alphonse, Pierre Control of the textural properties of nanocrystalline boehmite ( γ-AlOOH) regarding its peptization ability . -
Food Dispersion Systems Process Stabilization. a Review
───Food Technology ─── Food dispersion systems process stabilization. A review. Andrii Goralchuk, Olga Grinchenko, Olga Riabets, Оleg Kotlyar Kharkiv State University of Food Technology and Trade, Kharkiv, Ukraine Abstract Keywords: Introduction. The overview is given to systematize Emulsion information on the indicators, affecting the production and Foam stabilization of foams and emulsions, for applying the Stabilization existing regularities for more complex dispersed Rheology (polyphase) systems. Layers Materials and methods. Analytical studies of the production and stabilization of foams and polyphase dispersed systems published over the past 20 years. The research focuses on the foams, emulsions, foam emulsion systems and the systems, being simultaneously foam, Article history: emulsion and suspension. Results and discussion. Though foams and Received 28.11.2018 emulsions have similarities and their production differs in Received in revised form 15.08.2019 the dispersion rate, determined by the rate of surfactants Accepted 28.11.2019 adsorption. Emulsifying is faster than foaming, therefore, the production of foam emulsions can be sequential only. Coalescence, as a destruction indicator, is typical of foams and emulsions alike, and it is determined by the properties Corresponding author: of surfactants. Other indicators are determined by the features of the dispersion medium. The study systematized Andrii Goralchuk the factors, ensuring the stability of dispersion systems. The E-mail: structural mechanical factor is effective in -
Characterization of Salt- and Surfactant-Containing Sandy Soil Extracts by Laser Light Methods Szilvia Joó1,2, Judit Tóth3, and Rita Földényi1*
Int. Agrophys., 2015, 29, 291-298 doi: 10.1515/intag-2015-0034 Characterization of salt- and surfactant-containing sandy soil extracts by laser light methods Szilvia Joó1,2, Judit Tóth3, and Rita Földényi1* 1Department of Earth and Environmental Sciences, University of Pannonia, Egyetem str. 10, H-8200 Veszprém, Hungary 2Agricultural Institute, Centre for Agricultural Research, Hungarian Academy of Sciences, Brunszvik str. 2, H-2462 Martonvásár, Hungary 3Institute of Materials and Environmental Chemistry, Research Centre for Natural Sciences, Hungarian Academy of Sciences, Magyar tudósok blv. 2, H-1117 Budapest, Hungary Received November 7, 2014; accepted June 15, 2015 A b s t r a c t. The aim of this work was to study how dif- and clay. There is no standard procedure for determination ferent salt and surfactant solutions influence the particle size of soil PSD by the LD method (Arriaga et al., 2006); distribution and colloidal stability of sandy soil extracts. Particle therefore, data are given in volume percentage. Commonly size distribution was investigated by the laser diffraction method. used methods for determination of PSD (pipette, aerometer Extracts were made from the soil – before and after removing etc.) are based on Stokes law and results are expressed in its organic content – with solutions of NaCl or CaCl2 and one cationic and two anionic surfactants. The surfactants influence the mass percentage. LD has the advantage that small samples particle size distribution of the soil. Due to the use of the NaCl can be analyzed accurately, which cannot be carried out by and surfactant mixtures after removal of organic content, the par- the pipette method (Cooper et al., 1984).