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Isotopic evidence (δ¹³C, δ³⁷Cl, δ²H) for distinct transformation mechanisms of chloroform: Catalyzed H₂-water system vs. zero-valent iron (ZVI)

Asfaw, Berhane Abrha ; Sakaguchi-Söder, Kaori ; Schiedek, Thomas ; Michelsen, Nils ; Bernstein, Anat ; Siebner, Hagar ; Schüth, Christoph (2024)
Isotopic evidence (δ¹³C, δ³⁷Cl, δ²H) for distinct transformation mechanisms of chloroform: Catalyzed H₂-water system vs. zero-valent iron (ZVI).
In: Journal of Environmental Chemical Engineering, 2023, 11 (3)
doi: 10.26083/tuprints-00027722
Artikel, Zweitveröffentlichung, Verlagsversion

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Kurzbeschreibung (Abstract)

Catalytic hydrodechlorination is an efficient technology for degrading organochlorinated compounds, such as chloroform (CF), into harmless products. Compound-specific stable isotope analysis (CSIA) of multiple elements is widely used for the investigation of degradation mechanisms. Yet, its application in the study of catalytic hydrodechlorination is still limited. We have applied CSIA to derive chlorine, carbon, and hydrogen isotope enrichment factors (ε) during the degradation of CF over Pd/Al₂O₃ and over Rh/Al₂O₃. In addition, the enrichment factors for the same isotopes were derived for the reaction of CF with zero-valent iron (ZVI) for comparison. For the reactions of CF over Pd/Al₂O₃ and Rh/Al₂O₃, εC values (−21.9±0.25 ‰ and −23.4±2.3 ‰) and εCl values (−12.1±1.7 ‰ and −10.3±0.6 ‰) were determined, respectively. The corresponding εC and εCl values, for the dechlorination of CF with ZVI were −22.2±2.8 ‰ and −4.7±0.45 ‰, respectively. The apparent kinetic isotope effects (AKIE) of Cl suggest that the transformation mechanism in the catalyzed hydrogen-water system is a non-concerted reaction, unlike the known reductive dechlorination of CF with ZVI. Moreover, dual-isotope slopes (ΛC/Cl) for both catalyzed reactions (ΛPd = 1.8±0.13 and ΛRh = 2.1±0.14) are markedly different than for the ZVI (ΛZVI = 5.8±0.41), reflecting that the reactions proceed in different mechanisms. For hydrogen isotopes, while there was no clear trend for the catalyzed reactions, an inverse secondary hydrogen isotope effect was observed for the reaction of CF with ZVI.

Typ des Eintrags: Artikel
Erschienen: 2024
Autor(en): Asfaw, Berhane Abrha ; Sakaguchi-Söder, Kaori ; Schiedek, Thomas ; Michelsen, Nils ; Bernstein, Anat ; Siebner, Hagar ; Schüth, Christoph
Art des Eintrags: Zweitveröffentlichung
Titel: Isotopic evidence (δ¹³C, δ³⁷Cl, δ²H) for distinct transformation mechanisms of chloroform: Catalyzed H₂-water system vs. zero-valent iron (ZVI)
Sprache: Englisch
Publikationsjahr: 29 Juli 2024
Ort: Darmstadt
Publikationsdatum der Erstveröffentlichung: 2023
Ort der Erstveröffentlichung: Amsterdam [u.a.]
Verlag: Elsevier
Titel der Zeitschrift, Zeitung oder Schriftenreihe: Journal of Environmental Chemical Engineering
Jahrgang/Volume einer Zeitschrift: 11
(Heft-)Nummer: 3
Kollation: 9 Seiten
DOI: 10.26083/tuprints-00027722
URL / URN: https://tuprints.ulb.tu-darmstadt.de/27722
Zugehörige Links:
Herkunft: Zweitveröffentlichungsservice
Kurzbeschreibung (Abstract):

Catalytic hydrodechlorination is an efficient technology for degrading organochlorinated compounds, such as chloroform (CF), into harmless products. Compound-specific stable isotope analysis (CSIA) of multiple elements is widely used for the investigation of degradation mechanisms. Yet, its application in the study of catalytic hydrodechlorination is still limited. We have applied CSIA to derive chlorine, carbon, and hydrogen isotope enrichment factors (ε) during the degradation of CF over Pd/Al₂O₃ and over Rh/Al₂O₃. In addition, the enrichment factors for the same isotopes were derived for the reaction of CF with zero-valent iron (ZVI) for comparison. For the reactions of CF over Pd/Al₂O₃ and Rh/Al₂O₃, εC values (−21.9±0.25 ‰ and −23.4±2.3 ‰) and εCl values (−12.1±1.7 ‰ and −10.3±0.6 ‰) were determined, respectively. The corresponding εC and εCl values, for the dechlorination of CF with ZVI were −22.2±2.8 ‰ and −4.7±0.45 ‰, respectively. The apparent kinetic isotope effects (AKIE) of Cl suggest that the transformation mechanism in the catalyzed hydrogen-water system is a non-concerted reaction, unlike the known reductive dechlorination of CF with ZVI. Moreover, dual-isotope slopes (ΛC/Cl) for both catalyzed reactions (ΛPd = 1.8±0.13 and ΛRh = 2.1±0.14) are markedly different than for the ZVI (ΛZVI = 5.8±0.41), reflecting that the reactions proceed in different mechanisms. For hydrogen isotopes, while there was no clear trend for the catalyzed reactions, an inverse secondary hydrogen isotope effect was observed for the reaction of CF with ZVI.

Freie Schlagworte: CSIA, Chloroform, Catalytic hydrodechlorination, Pd/Al2O3, Rh/Al2O3, ZVI
ID-Nummer: Artikel-ID: 110005
Status: Verlagsversion
URN: urn:nbn:de:tuda-tuprints-277223
Sachgruppe der Dewey Dezimalklassifikatin (DDC): 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften
600 Technik, Medizin, angewandte Wissenschaften > 624 Ingenieurbau und Umwelttechnik
Fachbereich(e)/-gebiet(e): 11 Fachbereich Material- und Geowissenschaften
11 Fachbereich Material- und Geowissenschaften > Geowissenschaften
11 Fachbereich Material- und Geowissenschaften > Geowissenschaften > Fachgebiet Bodenmineralogie und Bodenchemie
13 Fachbereich Bau- und Umweltingenieurwissenschaften
13 Fachbereich Bau- und Umweltingenieurwissenschaften > Institut IWAR - Wasser- und Abfalltechnik, Umwelt- und Raumplanung
13 Fachbereich Bau- und Umweltingenieurwissenschaften > Institut IWAR - Wasser- und Abfalltechnik, Umwelt- und Raumplanung > Fachgebiet Stoffstrommanagement und Ressourcenwirtschaft
Hinterlegungsdatum: 29 Jul 2024 14:17
Letzte Änderung: 30 Jul 2024 06:02
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