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Effect of precipitation conditions on the magnetic and sorption ...

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<str<strong>on</strong>g>Effect</str<strong>on</strong>g> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>precipitati<strong>on</strong></str<strong>on</strong>g> <str<strong>on</strong>g>c<strong>on</strong>diti<strong>on</strong>s</str<strong>on</strong>g> <strong>on</strong> <strong>the</strong><strong>magnetic</strong> <strong>and</strong> sorpti<strong>on</strong> properties <str<strong>on</strong>g>of</str<strong>on</strong>g>zeolite-maghemite compositesMarek Matik 1 , Vladimir Sepelak 2 , Jiri Pechousek 1 , Radek Zboril 11Nanomaterial Research Centre, Palacky University, Svobody 26,771 46 Olomouc, Czech Republic.2Institute <str<strong>on</strong>g>of</str<strong>on</strong>g> Physical <strong>and</strong> Theoretical Chemistry, Technical University <str<strong>on</strong>g>of</str<strong>on</strong>g> Braunschweig,Hans-Sommer-Strasse 10, 381 06 Braunschweig, Germany.


MAGNETIC ZEOLITEWHY ZEOLITE ?good adsorbent <str<strong>on</strong>g>of</str<strong>on</strong>g> cati<strong>on</strong>scheap material (Nižný Hrabovec deposit)WHY MAGNETIC MODIFICATION ?<strong>magnetic</strong> separati<strong>on</strong>maghemite – adsorbent(cati<strong>on</strong>s <strong>and</strong> ani<strong>on</strong>s)


ZEOLITEGeneral formula <str<strong>on</strong>g>of</str<strong>on</strong>g> zeolite:Me2/m.Al2O3.nSiO2.pH2O,whereMe – cati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> alkali (m=1), <strong>and</strong>alkali earth metal (m=2)n - SiO 2/Al 2O 3molar ratiop – water moleculesClassificati<strong>on</strong>:NaturalModificated : cati<strong>on</strong> changes: ratio Al/Si changes: surface changesSyn<strong>the</strong>ticUsage: catalysis, adsorpti<strong>on</strong>


MODIFICATION WITH Fe PARTICLES• Modificati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> natural zeolite with magnetite <strong>and</strong> maghemite particles•Coverage <str<strong>on</strong>g>of</str<strong>on</strong>g> zeolite surface by <strong>magnetic</strong> metal nanoparticles (Fe, Co, Ni),•Incorporati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> Fe i<strong>on</strong>s into zeolite latticeSYNTHESISZEOLIT + Fe 2+ +Fe 3+ + OH - → ZEOLIT - γ-Fe 2 O 3


CONDITIONS OF SYNTHESISZeolite : Maghemite ratio :2:15:110:1Interacti<strong>on</strong> time after <str<strong>on</strong>g>precipitati<strong>on</strong></str<strong>on</strong>g>:0 min.30 min.90 min.24 hod.Temperature <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>precipitati<strong>on</strong></str<strong>on</strong>g> :20 °C50 °C85 °CIdentificati<strong>on</strong>: XRD, Mössbauer spectroscopy, SEM, TEM, VSM.


XRD-ANALYSIS250012002000NATURAL ZEOLITE1000MAGHEMITEINTENSITY15001000INTENSITY800600400500200020 30 40 50 60 70 802 THETA020 30 40 50 60 70 802 THETA3500INTENSITY30002500200015001000500°°°MODIFICATED ZEOLITE°MAGHEMITE°°°020 30 40 50 60 70 802 THETA


SEMElementO KAlKSiKK KCaKFeKWt %44.8405.0928.3701.3200.9219.46At %63.6004.2822.9200.7700.5207.91


MOSSBAUER100T = 10K, H ext. = 5TH ext.⊥γ-raysH obs(A) = H (A) + H extH obs[B] = H [B] - H extTRANSMISSION (%)989694-10 -5 0 5 10VELOCITY (mm/s)(Fe 3+ )[ Fe 3+ 5/3 [ ] 1/3 ]O 4 3 : 51: 3


MOSSBAUERWeight ratioZeolite/Fe2:1, 10:1TRANSMISSION (%)-8 -6 -4 -2 0 2 4 6 8VELOCITY (mm/s)


MOSSBAUERTemperature<str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>precipitati<strong>on</strong></str<strong>on</strong>g>20°C, 85°CTRANSMISSION (%)-8 -6 -4 -2 0 2 4 6 8VELOCITY (mm/s)


MOSSBAUERInteracti<strong>on</strong> timeafter <str<strong>on</strong>g>precipitati<strong>on</strong></str<strong>on</strong>g>0, 24 hours.TRANSMISSION (%)-8 -6 -4 -2 0 2 4 6 8VELOCITY (mm/s)


VSMZFC-FC10-240 K H=0.01 Tzero-field-cooling (ZFC)<strong>and</strong> field-cooling (FC) proceduresspin-glass systemscollective blocking <str<strong>on</strong>g>of</str<strong>on</strong>g> particle momentsMAGNETIZÁCIA (emu/g)2,01,81,61,41,21,0ZEO-MAG 850 50 100 150 200 250TEPLOTA (K)M.D. Mukadam et al., J. Magn. Magn.Mater. 272–276 (2004) 1401


SURFACE AND MAGNETISM•Indirect identificati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> maghemite c<strong>on</strong>tent with volume susceptibility•Comparis<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> surface area <strong>and</strong> pore volume with <strong>magnetic</strong> properties <str<strong>on</strong>g>of</str<strong>on</strong>g> modifiedzeolite


ADSORPTION <str<strong>on</strong>g>of</str<strong>on</strong>g> Pb10080pH test (Pb,Fe)10080Q (mg/g)6040200Q (mg/g)604020zeo-mag 85zeo-mag 20zeolite2 3 4 5 6pH00 100 200 300 400C (mg/L)Composite c<strong>on</strong>c. ............2 g/LStarting c<strong>on</strong>c. Pb 2+ .......20 – 400 mg/LAdsorpti<strong>on</strong> time.................... 24 hoursTemperature (c<strong>on</strong>st.) .......... 25°CI<strong>on</strong>ic strength.........................I = 0


ADSORPTION <str<strong>on</strong>g>of</str<strong>on</strong>g> As141210pH test (As,Fe)2015Q (mg/g)864Q (mg/g)102502 3 4 5 6 7 8pH00 100 200 300 400 500c (mg/l)Composite c<strong>on</strong>c. ............2 g/LStarting c<strong>on</strong>c. AsO 43-.....20 – 500 mg/LAdsorpti<strong>on</strong> time.................... 24 hoursTemperature (c<strong>on</strong>st.) .......... 25°CI<strong>on</strong>ic strength.........................I = 0


CONCLUSIONS‣Particle size dependence <strong>on</strong> reacti<strong>on</strong> <str<strong>on</strong>g>c<strong>on</strong>diti<strong>on</strong>s</str<strong>on</strong>g>‣Increasing <str<strong>on</strong>g>of</str<strong>on</strong>g> composite surface‣Ability <str<strong>on</strong>g>of</str<strong>on</strong>g> cati<strong>on</strong> <strong>and</strong> ani<strong>on</strong> adsorpti<strong>on</strong>‣Magnetic properties

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