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Distribution of as within magnetic and non-magnetic fractions of fluidized-bed coal combustion ash

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27360%2F21%3A10248478" target="_blank" >RIV/61989100:27360/21:10248478 - isvavai.cz</a>

  • Result on the web

    <a href="https://www.mdpi.com/2075-163X/11/12/1411" target="_blank" >https://www.mdpi.com/2075-163X/11/12/1411</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.3390/min11121411" target="_blank" >10.3390/min11121411</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Distribution of as within magnetic and non-magnetic fractions of fluidized-bed coal combustion ash

  • Original language description

    Separation of coal ash into magnetic and non-magnetic fractions facilitates their utilization when processed separately. Due to desulphurization additives added to coal during the fluidisedbed combustion, non-magnetic fractions often contain elevated CaO levels (while magnetic concentrates are typically rich in Fe2O3). Both CaO and Fe2O3 are known for their ability to bind As during the combustion, whose distribution is a crucial parameter in terms of proper utilization of these fractions. Therefore, the study deals with the As partitioning within magnetic and non-magnetic fractions of fluidized-bed coal combustion ashes. Two different (successive) procedures of dry magnetic separation were used to separate each ash into strongly magnetic, less magnetic, and a nonmagnetic fraction. Due to their optimal utilization, the concentrations of As and other target elements in these fractions were evaluated and compared. Magnetic concentrates from the first separation step (in vibrofluidized state) contained 60-70% Fe2O3, magnetic concentrates separated manually out of the residues after the first separation contained 26-41% Fe2O3, and the non-magnetic residues contained 2.4-3.5% Fe2O3. Arsenic levels were the highest in the non-magnetic residues and gradually decreased with the increasing Fe2O3 content in the magnetic fractions. The dominant As association in the studied samples was to CaO (r = +0.909) and with SO3 (r = +0.906) whereas its joint occurrence with Fe2O3 was improbable (r = MINUS SIGN 0.834). (C) 2021 by the authors. Licensee MDPI, Basel, Switzerland.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    20402 - Chemical process engineering

Result continuities

  • Project

    <a href="/en/project/EF17_049%2F0008426" target="_blank" >EF17_049/0008426: Research on the management of waste, materials and other products of metallurgy and related sectors</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2021

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Minerals

  • ISSN

    2075-163X

  • e-ISSN

  • Volume of the periodical

    11

  • Issue of the periodical within the volume

    12

  • Country of publishing house

    CH - SWITZERLAND

  • Number of pages

    1411

  • Pages from-to

  • UT code for WoS article

    000736881700001

  • EID of the result in the Scopus database

    2-s2.0-85121032951