Second Dissociation Constant of Succinic Acid from 0-Degrees to 50-Degrees-C
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Adsorption of Cd (II) and Pb (II) Using Physically Pretreated Camel Bone Biochar
Advanced Journal of Chemistry-Section A, 2019, 2(4), 347-364 http://ajchem-a.com Research Article Adsorption of Cd (II) and Pb (II) Using Physically Pretreated Camel Bone Biochar Mohamed Nageeb Rashed* , Allia Abd-Elmenaim Gad, Nada Magdy Fathy Faculty of Science, Aswan University, 81528 Aswan, Egypt A R T I C L E I N F O A B S T R A C T Received: 15 April 2019 In this study, low-cost biochar adsorbent originated from camel Revised: 06 May 2019 bone was prepared by physical treatment, and the prepared camel Accepted: 05 June bone biochar for the removal of Cd2+ and Pb2+ from aqueous Available online: 10 June solutions was examined. The characterization of the prepared biochar adsorbent before and after the treatment with the metal DOI: 10.33945/SAMI/AJCA.2019.4.8 solutions was done by using XRD, SEM, FT-IR, and BET surface isotherm. The bone sample was pyrolyzed at temperature 500, 600, 800, and 900 °C. Adsorption efficiency of Pb and Cd were optimized K E Y W O R D S by varying different parameters viz., pH, pHz, contact time, initial Wastewater metal concentration, adsorbent dosage, and temperature. Nature of Lead the adsorption process is predicted by using adsorption kinetic, Cadmium isotherms, and thermodynamic models. The results revealed that the Camel Bone effective pyrolysis of camel bone achieved at 800 °C which possess Biochar high removal capacity. The maximum adsorption removal percentage for Cd and Pb were 99.4 and 99.89%, respectively at contact time of 1 h, adsorbent dosage of 1 g, pH=5, and initial metal concentration 10 mg/L of both metal salts. -
Activated Carbon, Biochar and Charcoal: Linkages and Synergies Across Pyrogenic Carbon’S Abcs
water Review Activated Carbon, Biochar and Charcoal: Linkages and Synergies across Pyrogenic Carbon’s ABCs Nikolas Hagemann 1,* ID , Kurt Spokas 2 ID , Hans-Peter Schmidt 3 ID , Ralf Kägi 4, Marc Anton Böhler 5 and Thomas D. Bucheli 1 1 Agroscope, Environmental Analytics, Reckenholzstrasse 191, CH-8046 Zurich, Switzerland; [email protected] 2 United States Department of Agriculture, Agricultural Research Service, Soil and Water Management Unit, St. Paul, MN 55108, USA; [email protected] 3 Ithaka Institute, Ancienne Eglise 9, CH-1974 Arbaz, Switzerland; [email protected] 4 Eawag, Swiss Federal Institute of Aquatic Science and Technology, Department Process Engineering, Überlandstrasse 133, CH-8600 Dübendorf, Switzerland; [email protected] 5 Eawag, Swiss Federal Institute of Aquatic Science and Technology, Application and Development, Department Process Engineering, Überlandstrasse 133, CH-8600 Dübendorf, Switzerland; [email protected] * Correspondence: [email protected]; Tel.: +41-58-462-1074 Received: 11 January 2018; Accepted: 1 February 2018; Published: 9 February 2018 Abstract: Biochar and activated carbon, both carbonaceous pyrogenic materials, are important products for environmental technology and intensively studied for a multitude of purposes. A strict distinction between these materials is not always possible, and also a generally accepted terminology is lacking. However, research on both materials is increasingly overlapping: sorption and remediation are the domain of activated carbon, which nowadays is also addressed by studies on biochar. Thus, awareness of both fields of research and knowledge about the distinction of biochar and activated carbon is necessary for designing novel research on pyrogenic carbonaceous materials. Here, we describe the dividing ranges and common grounds of biochar, activated carbon and other pyrogenic carbonaceous materials such as charcoal based on their history, definition and production technologies. -
Gas Supersaturation Thresholds for Spontaneous Cavitation in Water with Gas Equilibration Pressures up to 570 Atm1 Wayne A
Gas Supersaturation Thresholds for Spontaneous Cavitation in Water with Gas Equilibration Pressures up to 570 atm1 Wayne A. Gerth and Edvard A. Hemmingsen * Physiological Research Laboratory Scripps Institution of Oceanography University of California, San Diego La Jolla, California 92093 (Z. Naturforsch. 31a, 1711-1716 [1976] ; received October 5, 1976) Supersaturations for the onset of cavitation in water were determined for various gases. At am- bient pressure, the threshold supersaturations (in atm) required for profuse cavitation to initiate both in bulk water and at the glass-water interface were CH4, 120; Ar, 160; N2, 190; He, 360. Exposure of the water and its containing surfaces to hydrostatic pressures up to 1100 atm prior to equilibration with gas had no detectable effect on these threshold values. This indicates that pre- formed gas nuclei are not significantly involved. Cavitation at the glass-water interface was investi- gated for CH4, Ar and N, saturations up to 570 atm. For 320 atm saturations, the threshold super- saturation was about one-half that for decompression directly to ambient pressure, and for 550 atm it was about one-third. These results indicate that the dissolved gas concentration is a critical factor limiting the spontaneous nucleation of bubbles in gas supersaturated liquids. Introduction thereby forcing the resolution of such dissolvable nuclei 4. Water that contains large gas supersaturations The results reported here bear directly upon the can remain stable with the absence of cavitation 2' 3. understanding of the gas supersaturated metastable However, as the gas supersaturation in the water is condition in pure liquids, the factors which limit it, increased, the system eventually fails to tolerate the and the characteristics of its degeneration via the supersaturation and bursts profusely with the for- nucleation and growth of bubbles. -
Chapter 1 the Fundamentals of Bubble Formation in Water Treatment
Chapter 1 The Fundamentals of Bubble Formation in Water Treatment Paolo Scardina and Marc Edwards1 Keywords: bubble, air binding, filters, nucleation, equilibrium, water treatment, headloss, filtration, gas transfer Abstract: Water utilities can experience problems from bubble formation during conventional treatment, including impaired particle settling, filter air binding, and measurement as false turbidity in filter effluent. Coagulation processes can cause supersaturation and bubble formation by converting bicarbonate alkalinity to carbon dioxide by acidification. A model was developed to predict the extent of bubble formation during coagulation which proved accurate, using an apparatus designed to physically measure the actual volume of bubble formation. Alum acted similar to hydrochloric acid for initializing bubble formation, and higher initial alkalinity, lower final solution pH, and increased mixing rate tended to increase bubble formation. Lastly, the protocol outlined in Standard Methods for predicting the degree of supersaturation was examined, and when compared to this work, the Standard Methods approach produces an error up to 16% for conditions found in water treatment. Introduction: Gas bubble formation is of established importance to divers and fish (i.e., the bends), carbonated beverages, solid liquid separation in mining, cavitation in pumps, gas transfer, stripping, and dissolved air flotation processes. Moreover, it is common knowledge that formation of gas bubbles in conventional sedimentation and filtration facilities is a significant nuisance at many utilities, because bubbles are believed to hinder sedimentation, cause headloss in filters through a phenomenon referred to as “air binding,” and measure as turbidity in effluents without posing a microbial hazard. Utilities have come to accept these problems, and to the knowledge of these authors there is currently no rigorous basis for predicting when such problems will occur or correcting them when they do. -
Cloud Microphysics
1. Microphysics of Clouds Changes in phase are basic to cloud microphysics. The possible changes are: vapor-liquid evaporation, condensation liquid-solid freezing, melting vapor-solid deposition, sublimation The changes from left to right correspond to increasing molecular order. These transitions don’t occur at thermodynamic equilibrium. There is a strong free en- ergy barrier that must be overcome for droplets to form. To form a droplet by condensation of vapor, surface tension must be overcome by a strong gradient of vapor pressure. This means that phase transitions don’t occur at es(1), or sat- uration over a plane surface of water. Even if a sample of moist air is cooled adiabatically to the equilibrium saturation point for bulk water, droplets should not be expected to form. In fact, water droplets do begin to condense in pure wa- ter vapor only when the relative humidity reaches several hundred percent! This is called Homogeneous Nucleation. The reason why cloud droplets are observed to form in the atmosphere when ascending air just reaches equilibrium saturation is because the atmosphere con- tains significant concentrations of particles of micron and sub-micron size which have an affinity for water. This is called Heterogeneous Nucleation. There are many types of condensation nuclei in the atmosphere. Some become wetted at RH less than 100% and account for haze. Larger condensation nuclei may grow to cloud droplet size. As moist air is cooled adiabatically and RH is close to 100 the hygroscopic CCN begin to serve as centers of condensation. If ascent con- tinues, there is supersaturation by cooling which is depleted by condensation on the nuclei. -
Carbonate Chemistry
CHAPTER 3 SOLUTION-MINERAL EQUILIBRIA PART 1: CARBONATES Carbonic acid and the carbonate minerals provide another good illustration of the use of equilibrium reasoning in geochemistry. Interactions among these compounds determine the conditions under which limestones and dolomites are fomied or dissolved, and likewise the conditions of formation of carbonate minerals as cements in soils and sandstones and as vein fillings. We start with some qualitative remarks about the most common of these substances, the carbonate of calcium, then go on to a more quantitative treatment and to the reactions of other common carbonate minerals. • 3-1 SOLUBILITY OF CALCITE Calcium carbonate occurs in nature as the two common minerals calcite and aragonite (Sec. 3-3). A third crystal form (vaterite) can be prepared artificially, and is known as a very rare mineral in nature. Under usual conditions near the Earth's surface calcite is the most stable and most abundant of the three forms, and for the discussion in this section and the next it will be the center of attention. Aragonite and vaterite may be assumed to show similar chemical behavior, but in general to react more rapidly and to have greater solubility. 61 62 INTRODUCTION TO GEOCHEMISTRY A strong acid dissolves calcite by the familiar reaction CaC03 + 2H+ ---+ Ca2+ + H20 + C02. (3-1 ) calcite At low acid concentrations a more accurate equation would be CaC03 + H+ - • Ca2+ + HCO) (3-2) calcite showing that W takes co~ - away from Ca2+ to form the very weak (little dissociated) acid HCO:J. (Still greater accuracy would require consideration of the complex ion CaHCOj , but under usual conditions its concentration is small and for the present can be neglected.) These reactions would take place in nature, for example, where acid solutions from the weathering of pyrite encounter limestone. -
Thesis Final
DEFLUORIDATION FROM AQUEOUS SOLUTION BY CATTLE BONE CHAR AND HYDROXYAPATITE by Dachuan Tang A thesis submitted to the Faculty of the University of Delaware in partial fulfillment of the requirements for the degree of Master of Civil Engineering 2019 Summer © 2019 Dachuan Tang All Rights Reserved DEFLUORIDATION FROM AQUEOUS SOLUTION BY CATTLE BONE CHAR AND HYDROXYAPATITE by Dachuan Tang Approved: __________________________________________________________ Chin-Pao Huang, Ph.D. Professor in charge of thesis on behalf of the Advisory Committee Approved: __________________________________________________________ Sue McNeil, Ph.D. Chair of the Department of Civil and Environmental Engineering Approved: __________________________________________________________ Levi T. Thompson, Ph.D. Dean of the College of Engineering Approved: __________________________________________________________ Douglas J. Doren, Ph.D. Interim Vice Provost for Graduate & Professional Education and Dean of the Graduate College ACKNOWLEDGMENTS First, I want to express my sincere appreciation to my advisor, Professor Chin- Pao Huang for his patient guidance, consistently encourage and valuable experience in research through all days in laboratory and class. I still remember the first day I came to the University of Delaware, when he told me that a person can be remembered because of his achievements rather than a rhetoric English name. I want to thank all members in our lab: Tommy Chen, Jenn Feng, Mary Fan, Jinghua, Thomas Lin, Sean, Daniel, Michael Huang, Yuchin Kao, Cuijuan, Wanze, and Kegang for their assistance during my graduate career. Especially, thanks to Tommy Chen, who taught me how to conduct experiments; and Thomas Lin, who helped me to calculate the complex formation model. Moreover, I will keep the memories of happy lunchtimes accompanied by all lab members in my mind forever. -
The Role of Evolving Surface Tension in the Formation of Cloud Droplets James F
Technical Note: The Role of Evolving Surface Tension in the Formation of Cloud Droplets James F. Davies1, Andreas Zuend2, Kevin R. Wilson3 1Department of Chemistry, University of California Riverside, CA USA 5 2Department of Atmospheric and Oceanic Sciences, McGill University, Montreal, Quebec, Canada 3Chemical Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA USA Correspondence to: James F. Davies ([email protected]) Abstract. The role of surface tension (σ) in cloud droplet activation has long been ambiguous. Recent studies have reported observations attributed to the effects of an evolving surface tension in the activation 10 process. However, adoption of a surface-mediated activation mechanism has been slow and many studies continue to neglect the composition-dependence of aerosol/droplet surface tension, using instead a value equal to the surface tension of pure water (σw). In this technical note, we clearly describe the fundamental role of surface tension in the activation of multicomponent aerosol particles into cloud droplets. It is demonstrated that the effects of surface tension in the activation process depend primarily on the evolution 15 of surface tension with droplet size, typically varying in the range 0.5σw ≲ σ ≤ σw due to the partitioning of organic species with a high surface affinity. We go on to report some recent laboratory observations that exhibit behavior that may be associated with surface tension effects, and propose a measurement coordinate that will allow surface tension effects to be better identified using standard atmospheric measurement techniques. Unfortunately, interpreting observations using theory based on surface film and liquid-liquid 20 phase separation models remains a challenge. -
Solid-Liquid Phase Equilibria and Crystallization of Disubstituted Benzene Derivatives
Royal Institute of Technology School of Chemical Science and Engineering Department of Chemical Engineering and Technology Division of Transport Phenomena Solid-Liquid Phase Equilibria and Crystallization of Disubstituted Benzene Derivatives Fredrik Nordström Doctoral Thesis Akademisk avhandling som med tillstånd av Kungliga Tekniska Högskolan i Stockholm framlägges till offentlig granskning för avläggande av teknologie doktorsexamen den 30:e Maj 2008, kl. 10:00 i sal D3, Lindstedtsvägen 5, Stockholm. Avhandlingen försvaras på engelska. i Cover picture: Crystals of o-hydroxybenzoic acid (salicylic acid) obtained through evaporation crystallization in solutions of ethyl acetate at around room temperature. Solid-Liquid Phase Equilibria and Crystallization of Disubstituted Benzene Derivatives Doctoral Thesis © Fredrik L. Nordström, 2008 TRITA-CHE Report 2008-32 ISSN 1654-1081 ISBN 978-91-7178-949-5 KTH, Royal Institute of Technology School of Chemical Science and Engineering Department of Chemical Engineering and Technology Division of Transport Phenomena SE-100 44 Stockholm Sweden Paper I: Copyright © 2006 by Wiley InterScience Paper II: Copyright © 2006 by Elsevier Science Paper III: Copyright © 2006 by the American Chemical Society Paper IV: Copyright © 2006 by the American Chemical Society ii In loving memory of my grandparents Aina & Vilmar Nordström iii i v Abstract The Ph.D. project compiled in this thesis has focused on the role of the solvent in solid-liquid phase equilibria and in nucleation kinetics. Six organic substances have been selected as model compounds, viz. ortho-, meta- and para-hydroxybenzoic acid, salicylamide, meta- and para-aminobenzoic acid. The different types of crystal phases of these compounds have been explored, and their respective solid-state properties have been determined experimentally. -
Microbubble Treatment of Gas Supersaturated Water
MICROBUBBLE TREATMENT OF GAS SUPERSATURATED WATER Contract No. GS-23F-0339K/01PE810319 Desalination and Water Purification R&D Program Report No. 70 December 2001 U.S. Department of Interior Bureau of Reclamation Denver Office Technical Service Center Environmental Resources Team Water Treatment Engineering and Research Group MICROBUBBLE TREATMENT OF GAS SUPERSATURATED WATER Mark A. Lichtwardt ARCADIS G&M, Inc. Highlands Ranch, Colorado Co-Author Andrew Murphy Bureau of Reclamation Denver, Colorado Contract No. GS-23F-0339K/01PE810319 Desalination and Water Purification R&D Program Report No. 70 December 2001 U.S. Department of Interior Bureau of Reclamation Denver Office Technical Service Center Environmental Resources Team Water Treatment Engineering and Research Group Mission Statements U.S. Department of the Interior The mission of the Department of the Interior is to protect and provide access to our Nation’s natural and cultural heritage and honor our trust responsibilities to tribes. Bureau of Reclamation The mission of the Bureau of Reclamation is to manage, develop, and protect water and related resources in an environmentally and economically sound manner in the interest of the American public. Disclaimer The information contained in this report regarding commercial products or firms may not be used for advertising or promotional purposes and is not to be construed as an endorsement of any product or firm by the Bureau of Reclamation. The information contained in this report was developed for the Bureau of Reclamation; no warranty as to the accuracy, usefulness, or completeness is expressed or implied. Acknowledgements This work was financially supported by the U.S. Department of Interior, Bureau of Reclamation under Contract No. -
Crystallisation Behaviour of Sunflower and Longan Honey with Glucose Addition by Absorbance Measurement
International Food Research Journal 27(4): 727 - 734 (August 2020) Journal homepage: http://www.ifrj.upm.edu.my Crystallisation behaviour of sunflower and longan honey with glucose addition by absorbance measurement Suriwong, V., *Jaturonglumlert, S., Varith, J., Narkprasom, K. and Nitatwichit, C. Graduate Program in Food Engineering, Faculty of Engineering and Agro-Industry, Maejo University, Chiang Mai 50290, Thailand Article history Abstract Received: 11 February 2020 The present work aimed to study the crystallisation behaviour of honey with glucose addition Received in revised form: by using the absorbance measurement at 660 nm. The Avrami model was used to explain the 7 May 2020 crystallisation kinetic. The effect of glucose addition on the colour and microstructure of Accepted: 4 June 2020 crystallised honey was also determined. Sunflower and longan honey were used in the present work. The biochemical compositions of honey samples were analysed before the addition of glucose powder at four concentrations (1.0, 1.5, 2.0, and 2.5%; w/w) and stored at 10 - 15°C. Keywords The absorbance at 660 nm, colour, and microstructure were measured until full crystallisation. crystallisation model, The results showed that different honey compositions exhibited different crystallisation glucose, behaviours, which could be monitored by the absorbance measurement at 660 nm as well. The longan honey, addition of glucose powder could stimulate the crystallisation time, thus affecting the crystal- sunflower honey lisation rate. The Avrami equation was found to be a good model for describing the crystallisa- tion behaviour from the intensity of absorbance values. The highest crystallisation rate was found at 2.0% (w/w) glucose addition at the rate constant (k) of 0.177 ± 0.038 and 0.083 ± 0.039 in sunflower and longan honey, respectively. -
The Influence of Polymers on the Supersaturation Potential of Poor and Good Glass Formers
pharmaceutics Article The Influence of Polymers on the Supersaturation Potential of Poor and Good Glass Formers Lasse I. Blaabjerg 1 , Holger Grohganz 1,* , Eleanor Lindenberg 2, Korbinian Löbmann 1 , Anette Müllertz 1 and Thomas Rades 1,3 1 Department of Pharmacy, University of Copenhagen, Universitetsparken 2, 2100 Copenhagen, Denmark; [email protected] (L.I.B.); [email protected] (K.L.); [email protected] (A.M.); [email protected] (T.R.) 2 Idorsia Pharmaceuticals Ltd., Hegenheimermwattweg 91, CH-4123 Allschwil, Switzerland; [email protected] 3 Faculty of Science and Engineering, Åbo Akademi University, Tykistökatu 6A, 20521 Turku, Finland * Correspondence: [email protected] Received: 16 August 2018; Accepted: 19 September 2018; Published: 21 September 2018 Abstract: The increasing number of poorly water-soluble drug candidates in pharmaceutical development is a major challenge. Enabling techniques such as amorphization of the crystalline drug can result in supersaturation with respect to the thermodynamically most stable form of the drug, thereby possibly increasing its bioavailability after oral administration. The ease with which such crystalline drugs can be amorphized is known as their glass forming ability (GFA) and is commonly described by the critical cooling rate. In this study, the supersaturation potential, i.e., the maximum apparent degree of supersaturation, of poor and good glass formers is investigated in the absence or presence of either hypromellose acetate succinate L-grade (HPMCAS-L) or vinylpyrrolidine-vinyl acetate copolymer (PVPVA64) in fasted state simulated intestinal fluid (FaSSIF). The GFA of cinnarizine, itraconazole, ketoconazole, naproxen, phenytoin, and probenecid was determined by melt quenching the crystalline drugs to determine their respective critical cooling rate.