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Characteristics and impact of aged coal ash with slag emplaced in a karst cave: the case of Divaška jama, Slovenia
A mixture of coal bottom ash and slag, with a fraction of fly ash (CAFAS) from steam locomotives, was placed in the cave Divaška jama to delimit and level tourist trails. Emplacement began in 1914 and carried on for several decades. The CAFAS mixed with other cave material gradually changed its stru...
Autores principales: | , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2021
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8642485/ https://www.ncbi.nlm.nih.gov/pubmed/34862432 http://dx.doi.org/10.1038/s41598-021-02842-7 |
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author | Oarga-Mulec, Andreea Skok, Sara Simčič, Tatjana Mulec, Janez |
author_facet | Oarga-Mulec, Andreea Skok, Sara Simčič, Tatjana Mulec, Janez |
author_sort | Oarga-Mulec, Andreea |
collection | PubMed |
description | A mixture of coal bottom ash and slag, with a fraction of fly ash (CAFAS) from steam locomotives, was placed in the cave Divaška jama to delimit and level tourist trails. Emplacement began in 1914 and carried on for several decades. The CAFAS mixed with other cave material gradually changed its structure and appearance. Currently the concentration of some elements in the CAFAS (As, Cu, Hg, Ni, Pb, Zn), and also to a lesser extent in cave sediments (Cr, Cu, Ni), indicates a possibly harmful effect on sediment-associated biota based on ecotoxicological assays. Compared to the cave sediment, the CAFAS contains distinctly different mineral phases and presents a different source of radioactivity. Microbial metabolic activity of CAFAS is low, 0.22 μl O(2)/gDW h, but higher than that of cave sediment. The present environmental hazards from CAFAS are estimated to be low. Whereas the emplacement of CAFAS was seen initially a long-term solution for waste disposal and management of the cave, it turned out that CAFAS enriches the underground environment with inorganic and organic compounds and disperses pollution into the cave ecosystem. After its removal from the cave, the CAFAS should be investigated thoroughly due to its susceptibility to alteration. |
format | Online Article Text |
id | pubmed-8642485 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2021 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-86424852021-12-06 Characteristics and impact of aged coal ash with slag emplaced in a karst cave: the case of Divaška jama, Slovenia Oarga-Mulec, Andreea Skok, Sara Simčič, Tatjana Mulec, Janez Sci Rep Article A mixture of coal bottom ash and slag, with a fraction of fly ash (CAFAS) from steam locomotives, was placed in the cave Divaška jama to delimit and level tourist trails. Emplacement began in 1914 and carried on for several decades. The CAFAS mixed with other cave material gradually changed its structure and appearance. Currently the concentration of some elements in the CAFAS (As, Cu, Hg, Ni, Pb, Zn), and also to a lesser extent in cave sediments (Cr, Cu, Ni), indicates a possibly harmful effect on sediment-associated biota based on ecotoxicological assays. Compared to the cave sediment, the CAFAS contains distinctly different mineral phases and presents a different source of radioactivity. Microbial metabolic activity of CAFAS is low, 0.22 μl O(2)/gDW h, but higher than that of cave sediment. The present environmental hazards from CAFAS are estimated to be low. Whereas the emplacement of CAFAS was seen initially a long-term solution for waste disposal and management of the cave, it turned out that CAFAS enriches the underground environment with inorganic and organic compounds and disperses pollution into the cave ecosystem. After its removal from the cave, the CAFAS should be investigated thoroughly due to its susceptibility to alteration. Nature Publishing Group UK 2021-12-03 /pmc/articles/PMC8642485/ /pubmed/34862432 http://dx.doi.org/10.1038/s41598-021-02842-7 Text en © The Author(s) 2021 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . |
spellingShingle | Article Oarga-Mulec, Andreea Skok, Sara Simčič, Tatjana Mulec, Janez Characteristics and impact of aged coal ash with slag emplaced in a karst cave: the case of Divaška jama, Slovenia |
title | Characteristics and impact of aged coal ash with slag emplaced in a karst cave: the case of Divaška jama, Slovenia |
title_full | Characteristics and impact of aged coal ash with slag emplaced in a karst cave: the case of Divaška jama, Slovenia |
title_fullStr | Characteristics and impact of aged coal ash with slag emplaced in a karst cave: the case of Divaška jama, Slovenia |
title_full_unstemmed | Characteristics and impact of aged coal ash with slag emplaced in a karst cave: the case of Divaška jama, Slovenia |
title_short | Characteristics and impact of aged coal ash with slag emplaced in a karst cave: the case of Divaška jama, Slovenia |
title_sort | characteristics and impact of aged coal ash with slag emplaced in a karst cave: the case of divaška jama, slovenia |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8642485/ https://www.ncbi.nlm.nih.gov/pubmed/34862432 http://dx.doi.org/10.1038/s41598-021-02842-7 |
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