Pregled bibliografske jedinice broj: 1210923
Heat-induced changes in soil properties: fires as cause for remobilization of chemical elements
Heat-induced changes in soil properties: fires as cause for remobilization of chemical elements // Journal of hydrology and hydromechanics, 70 (2022), 4; 421-431 doi:10.2478/johh-2022-0024 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 1210923 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Heat-induced changes in soil properties: fires as
cause for remobilization of chemical elements
Autori
Fajković, Hana ; Ivanić, Maja ; Nemet, Ivan ; Rončević, Sanda ; Kampić, Štefica ; Leontić Vazdar, Dana
Izvornik
Journal of hydrology and hydromechanics (0042-790X) 70
(2022), 4;
421-431
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Heating ; soil ; trace metals ; physicochemical properties
Sažetak
Exposure of soil constituents to elevated temperatures during wildfire can significantly affect their properties and consequently, increase the mobility of the bound contaminants. To estimate the potential of wildfires to influence metal remobilization from the burned soil due to the changes in cation exchange capacity (CEC) after organic matter combustion and mineral alteration and degradation, changes in soil properties after exposure to different temperatures was investigated. This was accomplished through analysis of geochemical, mineralogical and surface physicochemical properties of a soil sample exposed to different temperatures in a laboratory. Heating the soil sample at 200°C, 500°C and 850°C resulted in an increase in pH (from 5.9 to 12.3), decrease in cation exchange capacity (from 47.2 to 7.3 cmol+kg-1) and changes in the specific surface area (observed only at 500°C), that are associated with structural modifications of clay minerals and ferromagnetic minerals. Extraction analysis showed the increase in the concentration of almost all analyzed elements (Al, Cd, Co, Cr, Fe, Mn and Zn) in soil eluats. The observed increase, following high–temperature heating (500°C and 850°C), was as much as 15 times higher (e.g., Al), compared to the native soil sample (25°C). This strongly indicates that wildfire can act as a trigger for remobilization of heavy metals.
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Kemija, Interdisciplinarne prirodne znanosti
POVEZANOST RADA
Ustanove:
Institut "Ruđer Bošković", Zagreb,
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Hana Fajković
(autor)
Sanda Rončević
(autor)
Ivan Nemet
(autor)
Maja Ivanić
(autor)
Štefica Kampić
(autor)
Poveznice na cjeloviti tekst rada:
Pristup cjelovitom tekstu rada doi sciendo.com doi.org fulir.irb.hrCitiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus