Full Text

Turn on search term navigation

© 2021 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.

Abstract

A Three-Way Catalyst (TWC) contains a cordierite ceramic monolith coated with a layer of Al2O3, CexZr1−xO2 and platinoids mixture. Under standard operation, the platinoid concentration decreases, exposing the remaining washcoat structure. After that particle release stage, the sintering process follows where the crystalline CexZr1−xO2 solution is broken and begins to separate into ZrO2 and CeO2 phases. ZrO2 is released to the environment as micro and nanoparticles, while a small amount of CeO2 generates a new AlxCe1−xO2 composite. The main effect of Ce capture is the growth in the size of the polycrystal structure from 86.13 ± 16.58 nm to 225.35 ± 69.51 nm. Moreover, a transformation of cordierite to mullite was identified by XRD analysis. Raman spectra showed that the oxygen vacancies (Vö) concentration decreased as CexZr1−xO2 phases separation occurred. The SEM-EDS revealed the incorporation of new spurious elements and microfractures favouring the detachment of the TWC support structure. The release of ultrafine particles is a consequence of catalytic devices overusing. The emission of refractory micro to nanocrystals to the atmosphere may represent an emerging public health issue underlining the importance of implementing strict worldwide regulations on regular TWCs replacement.

Details

Title
Release of Nanoparticles in the Environment and Catalytic Converters Ageing
Author
Navarro-Espinoza, Sofía 1 ; Meza-Figueroa, Diana 2   VIAFID ORCID Logo  ; Guzmán, Roberto 3 ; Duarte-Moller, Alberto 4 ; Esparza-Ponce, Hilda 5   VIAFID ORCID Logo  ; Paz-Moreno, Francisco 2 ; González-Grijalva, Belem 2 ; Álvarez-Bajo, Osiris 6 ; Schiavo, Benedetto 7 ; Soto-Puebla, Diego 8   VIAFID ORCID Logo  ; Pedroza-Montero, Martín 8   VIAFID ORCID Logo 

 Departamento de Física, Posgrado en Nanotecnología, Universidad de Sonora, Hermosillo 83000, Sonora, Mexico; [email protected] 
 Departamento de Geología, Universidad de Sonora, Hermosillo 83000, Sonora, Mexico; [email protected] (F.P.-M.); [email protected] (B.G.-G.) 
 Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ 85721, USA; [email protected] 
 Facultad de Ingeniería Civil, Mecánica e Industrial, Universidad de La Salle Bajío, León 37150, Guanajuato, Mexico; [email protected] 
 Investigación en Materiales Avanzados, S. C., Complejo Industrial, Chihuahua 31136, Chihuahua, Mexico; [email protected] 
 Departamento de Investigación en Física, Universidad de Sonora, Hermosillo 83000, Sonora, Mexico; [email protected] (O.Á.-B.); [email protected] (D.S.-P.); Consejo Nacional de Ciencia y Tecnología CONACyT, Ciudad de México 03940, Mexico, Mexico 
 Instituto de Geofísica, Universidad Nacional Autónoma de México, Ciudad de México 04150, Mexico, Mexico; [email protected] 
 Departamento de Investigación en Física, Universidad de Sonora, Hermosillo 83000, Sonora, Mexico; [email protected] (O.Á.-B.); [email protected] (D.S.-P.) 
First page
3406
Publication year
2021
Publication date
2021
Publisher
MDPI AG
e-ISSN
20794991
Source type
Scholarly Journal
Language of publication
English
ProQuest document ID
2612828831
Copyright
© 2021 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.