Occurrence of carbon nanotubes and implication for the siting of elements in selected anthracites

Petrographic, geochemical, and electron microbeam investigations of selected anthracites and anthracite-rank coaly shales were conducted. The Pennsylvania, Rhode Island, and KwaZu-Natal anthracites show an enrichment in the middle to heavy rare earths (REE) while the Virginia semi-anthracite exhibit...

Descripción completa

Detalles Bibliográficos
Autores: Silva, Luis F. O., Crissien, Tito J., Hoffmann Sampaio, Carlos|||0000-0001-5840-1614, Howe, James C., Dai, Shifeng
Tipo de recurso: artículo
Fecha de publicación:2020
País:España
Institución:Universitat Politècnica de Catalunya (UPC)
Repositorio:UPCommons. Portal del coneixement obert de la UPC
Idioma:inglés
OAI Identifier:oai:upcommons.upc.edu:2117/175413
Acceso en línea:https://hdl.handle.net/2117/175413
https://dx.doi.org/10.1016/j.fuel.2019.116740
Access Level:acceso abierto
Palabra clave:Carbon nanotubes
Rare earth metals
Mercury
Anthracite coal
Rare earth elements
Coal rank
Nanotubs de carboni
Metalls de terres rares
Mercuri
Antracita
Àrees temàtiques de la UPC::Energies::Recursos energètics no renovables::Carbó
Descripción
Sumario:Petrographic, geochemical, and electron microbeam investigations of selected anthracites and anthracite-rank coaly shales were conducted. The Pennsylvania, Rhode Island, and KwaZu-Natal anthracites show an enrichment in the middle to heavy rare earths (REE) while the Virginia semi-anthracite exhibited a decreasing trend through the light REE, a peak in Gd, and a depletion in the heavy REE. Substitution of As, Hg, and Se in pyrite was most apparent in the Virginia coal. The Pennsylvania, Rhode Island, and KwaZu-Natal anthracites contained spherical carbon nanotube (CNT) structures. The CNTs contained several elements, including Hg, Cd, F, Cl, and Br. While CNTs are known to be produced from coals of varying ranks, this seems to be the first report of naturallyoccurring CNTs.