• Title/Summary/Keyword: Dissolution-precipitation

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Recovery of Sn from Copper Alloy Dross by a Selective Dissolution and Its Heat-treatment for the Synthesis of SnO2 (선택적 용해에 의한 동합금 부산물에서의 Sn 회수 및 열처리에 의한 SnO2 합성)

  • Ryu, Jeong Ho;Kong, Man-Sik;Lee, Jung-Il
    • Journal of the Korean Society for Heat Treatment
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    • v.26 no.4
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    • pp.173-177
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    • 2013
  • Separation and recovery of valuable metals such as zinc, nickel or tin from copper alloy dross has recently attracted from the viewpoints of environmental protection and resource recycling. In this report, preliminary study on concentration and separation of tin from copper alloy dross using selective dissolution method was performed. The tin in the copper alloy dross did not dissolve in the nitric acid solution which could allow the concentration and separation of the tin from the copper alloy dross. Precipitation of tin as $H_2SnO_3$ (metastannic acid) occurred in the solution and transformed to tin dioxide ($SnO_2$) after drying process. The dried sample was heat-treated at low temperature and its phase characteristics, surface morphology and chemical composition were investigated.

Studies on the Bioavailability of Berberine Preparations(II) : Antibacterial Activity and Bioavailability of Coprecipitate of Coptidis Rhizoma and Glycyrrhizae Radix (베르베린 제제의 생체이용율에 관한 연구(II): 황련과 감초 공침물의 항균효과 및 생체이용율)

  • Yang, Jae-Heon;Eun, Jae-Soon;Lee, Nam-Hee
    • Journal of Pharmaceutical Investigation
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    • v.25 no.3
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    • pp.185-192
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    • 1995
  • Precipitation reaction occured between berberine in Coptidis Rhizoma and glycyrrhizin in Glycyrrhizae Radix when they were boiled together in aqueous solution and the supernatant solution thus obtained did not show any antibacterial activity which was derived from berberine. The content of berberine in BG and CGP by HPLC analysis were 41.1%, 8.3% respectively. BG was occured mostly at pH 5.0. The solubility of berberine was 0.15%, while that of BG and CGP was 0.07%, 0.12%, respectively. CGP shown more increased antibacterial activity to gram positive bacteria, S. dysenteriae and K. pneumoniae than berberine. The absorption rates of CGP in stomach, duodenum and jejunum of rats were compared with those of Coptidis Rhizoma water extracts (CR), which were increased more than CR. The time required for the maximum serum concentration of berberine from CGP in mice was 90 minutes after oral administration. The maximum serum concentration of berberine from CGP was higher than that from CR. The dissolution of CGP was increased more than berberine and BG in both artificial gastric and intestinal fluids. The dissolution of CGP pill made from gelatin was 63.4% in artificial gastric fluids and that made from CMC was 76.0% in artificial intestinal fluids.

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Enhanced Dissolution and Duodenal Permeation of Atorvastatin Calcium Using Bile Salt and 2-Hydroxypropyl-${\beta}$-Cyclodextrin (담즙산염과 2-히드록시프로필-${\beta}$-시클로덱스트린을 이용한 아토르바스타틴칼슘의 용출 및 십이지장 점막 투과 증진)

  • Choi, Ji-Won;Chun, In-Koo
    • YAKHAK HOEJI
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    • v.56 no.3
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    • pp.164-172
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    • 2012
  • This study was aimed to increase the solubility, dissolution and permeation rates of atorvastatin calcium (ATC) using bile salt and/or 2-hydroxypropyl-${\beta}$-cyclodextrin ($HP{\beta}CD$). From solubility studies, sodium deoxycholate (SDC) among bile salts studied was found to have the highest solubilizing effect on ATC ($4.4{\pm}0.4$ mg/ml), and the order of increasing solubility was SDC>sod. cholate>sod. glycocholate>sod. taurodeoxycholate>sod. taurocholate>conjugated bile acid. ATC solid dispersions were prepared at various ratios of drug to SDC and/or $HP{\beta}CD$, and evaluated by differential scanning calorimetry (DSC), dissolution studies and dissolution-permeation studies. DSC curves showed amorphous state of ATC in the physical mixture and solid dispersion. Dissolution rates of ATC-SDC solid dispersions and physical mixture were markedly increased at pH 6.8, but decreased at pH 1.2 with greater proportions of SDC due to the precipitation of SDC, compared with that of drug alone. On the other hand, dissolution rates of ATC-$HP{\beta}CD$ solid dispersion and physical mixture at pH 1.2 were varied with the ratio of drug to carriers. From duodenal permeation studies, it was found that fluxes of ATC (donor dose: 0.5 mg/3.5 ml) in the presence of 25 mM sodium glycocholate, SDC, sod. cholate and sod. taurocholate $(5.7{\pm}0.9$, $5.6{\pm}0.9$, $4.8{\pm}0.7$ and $4.6{\pm}0.9\;{\mu}g/cm^2/hr$, respectively) were enhanced, compared with drug alone ($3.4{\pm}0.9\;{\mu}g/cm^2/hr$). In the dissolution-permeation studies, 1 : 9 : 10 (w/w) ATC-SDC-$HP{\beta}CD$ solid dispersion increased the flux 2.2 times, compared with 1 : 5 : 4 (w/w) ATC-lactose-corn starch mixture as control. In conclusion, solid dispersions with bile salt and $HP{\beta}CD$ were found to be an effective means for increasing the dissolution and permeation rates of ATC.

A Study on the Ion Exchange and th Chemical Stability of Na-fluor-tetrasilicic Mica by $H^+$ions (나트륨형불소 4 규소운모의 $H^+$ 이온교환 및 화학적인 안정성에 관한 연구)

  • 송종택
    • Journal of the Korean Ceramic Society
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    • v.22 no.1
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    • pp.35-39
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    • 1985
  • Synthetic mica $NaMg_{2.5}(Si_4O_{10})F_2 (Na-TSM)$ was treated with HCl solution and H-type exchange resin to investigate the chemical stability and the ion exchange by measuring the dissolution of chemical components and the exchanged $H^+$ ion. The replacement of $Na^+$ ion occurred in contact with HCl solution and H-type ion exchange resin at the surface of Na-TSM particles reached $Na^+$ ions at maximum value of 70~80%. $Mg^{2+}$ ion of octahedral layer became to dissolve from the pH2 solution and th amount of it dissolved in-creased almost proportional to $H^+$ ion concentration from around 0.02N $H^+$ ion equilibrium concentration. The crystalline structure of Na-TSM was destructed by dissolution of Mg2+ ion in cncentrated hydrochloric acid solution and resulted silica gel precipitation.

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$\beta$-SiC Formation Mechanisms in Si Melt-C-SiC System (용융 Si-C-SiC계에서 $\beta$-SiC 생성기구)

  • 서기식;박상환;송휴섭
    • Journal of the Korean Ceramic Society
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    • v.36 no.6
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    • pp.655-661
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    • 1999
  • ${\beta}$-SiC formation mechanism in Si melt-C-SiC system with varying in size of carbon source was investigated. A continuous reaction sintering process using Si melt infiltration method was adopted to control the reaction sintering time effectively. It was found that ${\beta}$-SiC formation mechanism in Si melt-C-SiC system was directly affected by the size of carbon source. In the Si melt-C-SiC system with large carbon source ${\beta}$-SiC formation mechanism could be divided into two stages depending on the reaction sintering time: in early stage of reaction sintering carbon dissolution in Si melt and precipitation of ${\beta}$-SiC was occurred preferentially and then SIC nucleation and growth was controlled by diffusion of carbon throughy the ${\beta}$-SiC layer formed on graphite particle. Furthmore a dissolution rate of graphite particles in Si melt could be accelerated by the infiltration of Si melt through basal plane of graphite crystalline.

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Water chemistry controlled by drainage basin: Case study in the Han River, South Korea

  • Ryu Jong-Sik;Lee Gwang-Sik;Sin Hyeong-Seon;An Gyu-Hong;Jang Ho-Wan
    • Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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    • 2005.04a
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    • pp.405-407
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    • 2005
  • To evaluate the main hydrogeochemical characteristics, river waters are investigated using element리 and isotopic compositions in South Korea. In this area, the chemical compositions are mostly classified into three groups; $Ca^{2+}-{HCO_3}^-$ type, $Ca^{2+}-Cl^{-}-{NO_3}^-$ type and $Ca^{2+}-{HCO_3}^{-}-Cl^{-}-{NO_3}^-$ type. These types are affected by two major factors: water-rock interaction and anthropogenic inputs such as sewage and fertilizers. Based on the values of ${\delta}^{18}O$ and ${\delta}D$, most of waters are originated from precipitation except two samples contaminated. The lithology and geography of basins mainly control the water chemistry. Elemental and isotopic compositions show that water chemistry are mainly controlled by three end members, especially by carbonate dissolution, and suggest that anthropogenic input affect the water chemistry. Also, three weathering sources are identified: silicates, dolomite and limestone.

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Experimental Study on the Geochemical and Mineralogical Alterations in a Supercritical CO2-Groundwater-Zeolite Sample Reaction System (초임계 이산화탄소-지하수-제올라이트 시료 반응계에서의 지화학적 및 광물학적 변화에 관한 실험적 연구)

  • Park, Eundoo;Wang, Sookyun;Lee, Minhee
    • Economic and Environmental Geology
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    • v.47 no.4
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    • pp.421-430
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    • 2014
  • In this study, a series of autoclave experiments were conducted in order to investigate the geochemical and mineralogical effects of carbon dioxide on deep subsurface environments. High pressure and temperature conditions of $50^{\circ}C$ and 100 bar, which are representative environments for geological $CO_2$ sequestration, were created in stainless-steel autoclaves for simulating the interactions in the $scCO_2$-groundwater-mineral reaction system. Zeolite, a widespread mineral in Pohang Basin where many researches have been focused as a candidate for geological $CO_2$ sequestration, and groundwater sampled from an 800 m depth aquifer were applied in the experiments. Geochemical and mineralogical alterations after 30 days of $scCO_2$-groundwater-zeolite sample reactions were quantitatively examined by XRD, XRF, and ICP-OES investigations. The results suggested that dissolution of zeolite sample was enhanced under the acidic condition induced by dissolution of $scCO_2$. As the cation concentrations released from zeolite sample increase, $H^+$ in groundwater was consumed and pH increases up to 10.35 after 10 days of reaction. While cation concentrations showed increasing trends in groundwater due to dissolution of the zeolite sample, Si concentrations decreased due to precipitation of amorphous silicate, and Ca concentrations decreased due to cation exchange and re-precipitation of calcite. Through the reaction experiments, it was observed that introduction of $CO_2$ could make alterations in dissolution characteristics of minerals, chemical compositions and properties of groundwater, and mineral compositions of aquifer materials. Results also showed that geochemical reactions such as cation exchange or dissolution/precipitation of minerals could play an important role to affect physical and chemical characteristics of geologic formations and groundwater.

Effects of Niobium Microalloying on Microstructure and Properties of Hot-Dip Galvanized Sheet

  • Mohrbacher, Hardy
    • Corrosion Science and Technology
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    • v.9 no.2
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    • pp.67-73
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    • 2010
  • Niobium microalloying is effective in hot-rolled and cold-rolled steels by providing a fine-grained microstructure resulting in increased strength. To optimize the strengthening effect, alloy design and hot-rolling conditions have to be adapted. As a key issue the dissolution and precipitation characteristics of Nb are discussed in particular with regard to the run-out table conditions. It is then considered how the hot-rolled microstructure and the solute state of Nb interact with the hot-dip galvanizing cycle. The adjusted conditions allow controlling the morphology and distribution of phases in the cold-rolled annealed material. Additional precipitation hardening can be achieved as well. The derived options can be readily applied to produce conventional HSLA and IF high strength steels as well as to modern multiphase steels. It will be explained how important application properties such as strength, elongation, bendability, weldability and delayed cracking resistance can be influenced in a controlled and favorable way. Examples of practical relevance and experience are given.

Precipitation of Magnesium Sulfate from Concentrated Magnesium Solution for Recovery of Magnesium in Seawater (해수 중 마그네슘 회수를 위한 마그네슘 농축액으로부터 황산마그네슘의 석출)

  • Cho, Taeyeon;Kim, Myoung-Jin
    • Resources Recycling
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    • v.25 no.4
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    • pp.32-41
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    • 2016
  • The precipitation test, which is the last step of magnesium recovery process consisting of three processes (pre-precipitation, selective dissolution of magnesium, precipitation) is performed to obtain magnesium sulfate powder from seawater. In the study, we succeed in precipitating the magnesium sulfate by adding acetone into the solution of magnesium over 4 times concentrated from seawater. The yield efficiency of magnesium sulfate increases with increasing pH and the ratio of added acetone. More than 99% of magnesium is obtained as magnesium sulfate hydrate ($MgSO_4{\cdot}6H_2O$) under the following conditions; pH 1.0 ~ 1.5, and the ratio of solution and acetone 1 : 1.5 (v:v). The acetone used in the precipitation process is recovered by the fractional distillation.

BIOGEOCHEMICAL ACTIVITIES OF MICROORGANISMS IN MINERAL TRANSFORMATIONS: CONSEQUENCES FOR METAL AND NUTRIENT MOBILITY

  • Gadd, Geoffrey M.
    • Proceedings of the Korean Society for Applied Microbiology Conference
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    • 2002.10a
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    • pp.39-61
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    • 2002
  • Bacteria and fungi are fundamental biotic components of natural biogeochemical cycles for metals and metalloids and play important roles in dissolution, precipitation, oxidation and reduction processes. Some processes catalyzed by microorganisms also have important applications in environmental biotechnology in the areas of ore leaching and bioremediation.

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