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Cobalt-exchanged hydroxyapatite catalysts: Magnetic studies, spectroscopic investigations, performance in 2-butanol and ethane oxidative dehydrogenations

Identifieur interne : 000212 ( PascalFrancis/Checkpoint ); précédent : 000211; suivant : 000213

Cobalt-exchanged hydroxyapatite catalysts: Magnetic studies, spectroscopic investigations, performance in 2-butanol and ethane oxidative dehydrogenations

Auteurs : Kaoutar Elkabouss [Maroc, France] ; Mohamed Kacimi [Maroc] ; Mahfoud Ziyad [Maroc] ; Souad Ammar [France] ; Francois Bozon-Verduraz [France]

Source :

RBID : Pascal:04-0443422

Descripteurs français

English descriptors

Abstract

A series of exchanged cobalt/calcium (Co2+/Ca2+) hydroxyapatite Ca10-xCox (PO4)6(OH)2 was synthesized and characterized by XRD, UV-visible-near-infrared (NIR) and IR spectroscopy, magnetic measurements (SQUID), and X-ray photoemission spectroscopy (XPS). The level of Co2+/Ca2+ exchange was limited to 1.35 wt% Co. After calcination in air at 550°C, cobalt was still present as Co2+ and all samples were paramagnetic, showing that the apatite matrix impedes the oxidation of Co2+ and that the Co2+ ions are isolated, whatever the Co content. Magnetic measurements and UV-visible diffuse reflectance spectra show that the exchanged Co2+ ions are hosted by two types of sites (with octahedral and trigonal prismatic symmetries). XPS confirmed the surface cobalt enrichment and did not reveal Co3+ ions. Dehydrogenation of 2-butanol leads almost exclusively to the formation of hutanone. As the Co content increases, the ketone yield passes through a maximum. In the oxidative dehydrogenation of ethane, the ethylene yield also reaches a maximum (22 mol%) for 0.96 wt% Co at 550°C. These results are ascribed to (i) the partial compensation of the intrinsic dehydrogenating activity of cobalt by the decrease in basicity of apatite induced by the replacement of Ca2+ by Co2+, and (ii) the involvement of two types of sites.


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Pascal:04-0443422

Le document en format XML

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<term>Ethane</term>
<term>Hydroxyapatite</term>
<term>Magnetic susceptibility</term>
<term>Oxidation</term>
<term>Photoelectron spectrometry</term>
<term>Reflectance</term>
<term>X ray</term>
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<term>Cobalt</term>
<term>Apatite hydroxylée</term>
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<term>Ethane</term>
<term>Oxydation</term>
<term>Déshydrogénation</term>
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<div type="abstract" xml:lang="en">A series of exchanged cobalt/calcium (Co
<sup>2+</sup>
/Ca
<sup>2+</sup>
) hydroxyapatite Ca
<sub>10-x</sub>
Co
<sub>x</sub>
(PO
<sub>4</sub>
)
<sub>6</sub>
(OH)
<sub>2</sub>
was synthesized and characterized by XRD, UV-visible-near-infrared (NIR) and IR spectroscopy, magnetic measurements (SQUID), and X-ray photoemission spectroscopy (XPS). The level of Co
<sup>2+</sup>
/Ca
<sup>2+</sup>
exchange was limited to 1.35 wt% Co. After calcination in air at 550°C, cobalt was still present as Co
<sup>2+</sup>
and all samples were paramagnetic, showing that the apatite matrix impedes the oxidation of Co
<sup>2+</sup>
and that the Co
<sup>2+</sup>
ions are isolated, whatever the Co content. Magnetic measurements and UV-visible diffuse reflectance spectra show that the exchanged Co
<sup>2+</sup>
ions are hosted by two types of sites (with octahedral and trigonal prismatic symmetries). XPS confirmed the surface cobalt enrichment and did not reveal Co
<sup>3+</sup>
ions. Dehydrogenation of 2-butanol leads almost exclusively to the formation of hutanone. As the Co content increases, the ketone yield passes through a maximum. In the oxidative dehydrogenation of ethane, the ethylene yield also reaches a maximum (22 mol%) for 0.96 wt% Co at 550°C. These results are ascribed to (i) the partial compensation of the intrinsic dehydrogenating activity of cobalt by the decrease in basicity of apatite induced by the replacement of Ca
<sup>2+</sup>
by Co
<sup>2+</sup>
, and (ii) the involvement of two types of sites.</div>
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<s0>A series of exchanged cobalt/calcium (Co
<sup>2+</sup>
/Ca
<sup>2+</sup>
) hydroxyapatite Ca
<sub>10-x</sub>
Co
<sub>x</sub>
(PO
<sub>4</sub>
)
<sub>6</sub>
(OH)
<sub>2</sub>
was synthesized and characterized by XRD, UV-visible-near-infrared (NIR) and IR spectroscopy, magnetic measurements (SQUID), and X-ray photoemission spectroscopy (XPS). The level of Co
<sup>2+</sup>
/Ca
<sup>2+</sup>
exchange was limited to 1.35 wt% Co. After calcination in air at 550°C, cobalt was still present as Co
<sup>2+</sup>
and all samples were paramagnetic, showing that the apatite matrix impedes the oxidation of Co
<sup>2+</sup>
and that the Co
<sup>2+</sup>
ions are isolated, whatever the Co content. Magnetic measurements and UV-visible diffuse reflectance spectra show that the exchanged Co
<sup>2+</sup>
ions are hosted by two types of sites (with octahedral and trigonal prismatic symmetries). XPS confirmed the surface cobalt enrichment and did not reveal Co
<sup>3+</sup>
ions. Dehydrogenation of 2-butanol leads almost exclusively to the formation of hutanone. As the Co content increases, the ketone yield passes through a maximum. In the oxidative dehydrogenation of ethane, the ethylene yield also reaches a maximum (22 mol%) for 0.96 wt% Co at 550°C. These results are ascribed to (i) the partial compensation of the intrinsic dehydrogenating activity of cobalt by the decrease in basicity of apatite induced by the replacement of Ca
<sup>2+</sup>
by Co
<sup>2+</sup>
, and (ii) the involvement of two types of sites.</s0>
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<fC02 i1="01" i2="X">
<s0>001C01A03</s0>
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<s2>NC</s2>
<s5>01</s5>
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<s2>NC</s2>
<s5>01</s5>
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<s5>03</s5>
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<s2>NK</s2>
<s2>FX</s2>
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<s2>NK</s2>
<s2>FX</s2>
<s5>04</s5>
</fC03>
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<s0>Butanol</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE">
<s0>Ethane</s0>
<s2>NK</s2>
<s5>05</s5>
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<s0>Ethane</s0>
<s2>NK</s2>
<s5>05</s5>
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<s0>Etano</s0>
<s2>NK</s2>
<s5>05</s5>
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<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG">
<s0>Oxidation</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA">
<s0>Oxidación</s0>
<s5>06</s5>
</fC03>
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<s0>Déshydrogénation</s0>
<s5>07</s5>
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<s0>Dehydrogenation</s0>
<s5>07</s5>
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<s5>07</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE">
<s0>Facteur réflexion</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG">
<s0>Reflectance</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA">
<s0>Coeficiente reflexión</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE">
<s0>Susceptibilité magnétique</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG">
<s0>Magnetic susceptibility</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA">
<s0>Susceptibilidad magnética</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE">
<s0>Spectrométrie photoélectron</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG">
<s0>Photoelectron spectrometry</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA">
<s0>Espectrometría fotoelectrón</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE">
<s0>Rayon X</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG">
<s0>X ray</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA">
<s0>Rayos X</s0>
<s5>11</s5>
</fC03>
<fC07 i1="01" i2="X" l="FRE">
<s0>Métal transition</s0>
<s2>NC</s2>
<s5>12</s5>
</fC07>
<fC07 i1="01" i2="X" l="ENG">
<s0>Transition metal</s0>
<s2>NC</s2>
<s5>12</s5>
</fC07>
<fC07 i1="01" i2="X" l="SPA">
<s0>Metal transición</s0>
<s2>NC</s2>
<s5>12</s5>
</fC07>
<fC07 i1="02" i2="X" l="FRE">
<s0>Alcanol</s0>
<s5>13</s5>
</fC07>
<fC07 i1="02" i2="X" l="ENG">
<s0>Alkanol</s0>
<s5>13</s5>
</fC07>
<fC07 i1="02" i2="X" l="SPA">
<s0>Alcanol</s0>
<s5>13</s5>
</fC07>
<fC07 i1="03" i2="X" l="FRE">
<s0>Propriété magnétique</s0>
<s5>14</s5>
</fC07>
<fC07 i1="03" i2="X" l="ENG">
<s0>Magnetic properties</s0>
<s5>14</s5>
</fC07>
<fC07 i1="03" i2="X" l="SPA">
<s0>Propiedad magnética</s0>
<s5>14</s5>
</fC07>
<fC07 i1="04" i2="X" l="FRE">
<s0>Alcool</s0>
<s5>15</s5>
</fC07>
<fC07 i1="04" i2="X" l="ENG">
<s0>Alcohol</s0>
<s5>15</s5>
</fC07>
<fC07 i1="04" i2="X" l="SPA">
<s0>Alcohol</s0>
<s5>15</s5>
</fC07>
<fN21>
<s1>250</s1>
</fN21>
<fN44 i1="01">
<s1>OTO</s1>
</fN44>
<fN82>
<s1>OTO</s1>
</fN82>
</pA>
</standard>
</inist>
<affiliations>
<list>
<country>
<li>France</li>
<li>Maroc</li>
</country>
<region>
<li>Rabat-Salé-Kénitra</li>
<li>Île-de-France</li>
</region>
<settlement>
<li>Paris</li>
<li>Rabat</li>
</settlement>
</list>
<tree>
<country name="Maroc">
<region name="Rabat-Salé-Kénitra">
<name sortKey="Elkabouss, Kaoutar" sort="Elkabouss, Kaoutar" uniqKey="Elkabouss K" first="Kaoutar" last="Elkabouss">Kaoutar Elkabouss</name>
</region>
<name sortKey="Kacimi, Mohamed" sort="Kacimi, Mohamed" uniqKey="Kacimi M" first="Mohamed" last="Kacimi">Mohamed Kacimi</name>
<name sortKey="Ziyad, Mahfoud" sort="Ziyad, Mahfoud" uniqKey="Ziyad M" first="Mahfoud" last="Ziyad">Mahfoud Ziyad</name>
</country>
<country name="France">
<region name="Île-de-France">
<name sortKey="Elkabouss, Kaoutar" sort="Elkabouss, Kaoutar" uniqKey="Elkabouss K" first="Kaoutar" last="Elkabouss">Kaoutar Elkabouss</name>
</region>
<name sortKey="Ammar, Souad" sort="Ammar, Souad" uniqKey="Ammar S" first="Souad" last="Ammar">Souad Ammar</name>
<name sortKey="Bozon Verduraz, Francois" sort="Bozon Verduraz, Francois" uniqKey="Bozon Verduraz F" first="Francois" last="Bozon-Verduraz">Francois Bozon-Verduraz</name>
</country>
</tree>
</affiliations>
</record>

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