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Title:Impact assessment of the Gajke and Brstje landfills on groundwater status using stable and radioactive isotopes
Authors:ID Cerar, Sonja (Author)
ID Serianz, Luka (Author)
ID Vreča, Polona (Author)
ID Štrok, Marko (Author)
ID Kanduč, Tjaša (Author)
Files:.pdf PDF - Presentation file, download (8,52 MB)
MD5: B00EC37CC730A96B3C839817B0FA732B
 
Language:English
Typology:1.01 - Original Scientific Article
Organization:Logo GeoZS - Geological Survey of Slovenia
Logo IJS - Jožef Stefan Institute
Abstract:Waste disposal in landfills represents a severe threat to aquatic environments on the local, regional, and global levels. In Slovenia, there are 69 registered landfills where groundwater is regularly monitored. However, isotope techniques are not regularly employed. Therefore, we employed isotope analysis of hydrogen, carbon, and oxygen in combination with total alkalinity to assess the impact of the selected landfill on groundwater and to evaluate the biogeochemical processes at work. The δ18O, δ2H, δ13CDIC, 3H activity and total alkalinity were determined in October 2020 at 12 sampling points from the surrounding area of the Gajke and Brstje landfills and leachate from the Gajke landfill. The δ18O (-9.24 ± 0.3 ‰) and δ2H (-64.9 ± 2.7 ‰) in groundwater indicate that the main water source consists in direct infiltration of precipitation, with no significant isotopic fractionation. Total alkalinity in the investigated area ranges from 5.45 to 73 mM and δ13CDIC from –14.9 to +6.1 ‰, respectively. Higher values of total alkalinity (up to 73 mM), δ13CDIC (up to +6.1 ‰), δ18O (-7.64 ‰) and 3H (209.8 TU) are detected in the leachate, indicating biogeochemical process related to CO2 reduction or methanogenesis. Methanogenesis could be present at locations GAP-10/13 (Brstje landfill) and G-2 (Gajke landfill) with δ13CDIC values ranging from –8.2 to –7.6 ‰ and with dissolved oxygen values around 0 % and elevated 3H values (from 16 to 18 TU). This study demonstrates the effectiveness of isotopic analysis as a valuable tool for monitoring landfills, revealing shifts in biogeochemical processes within the groundwater there.
Keywords:groundwater, monitoring, landfill, stable isotopes, tritium, Gajke, Brstje
Publication status:Published
Publication version:Version of Record
Publication date:21.12.2023
Year of publishing:2023
Number of pages:str. 275-283
Numbering:vol. 66, no. 2
PID:20.500.12556/DiRROS-17635 New window
UDC:556.3
ISSN on article:0016-7789
DOI:10.5474/geologija.2023.014 New window
COBISS.SI-ID:179274499 New window
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Publication date in DiRROS:16.01.2024
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Downloads:207
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Record is a part of a journal

Title:Geologija
Shortened title:Geologija
Publisher:Geološki zavod Slovenije
ISSN:0016-7789
COBISS.SI-ID:5636866 New window

Document is financed by a project

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:P1-0020-2020
Name:Podzemne vode in geokemija

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:P1-0143-2020
Name:Kroženje snovi v okolju, snovna bilanca in modeliranje okoljskih procesov ter ocena tveganja

Licences

License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.

Secondary language

Language:Slovenian
Title:Ocena vpliva odlagališč Gajke in Brstje na stanje podzemne vode z uporabo stabilnih in radioaktivnih izotopov
Abstract:Odlaganje odpadkov na odlagališčih predstavlja resno grožnjo za vodna okolja na lokalni, regionalni in globalni ravni. V Sloveniji je 69 registriranih odlagališč, kjer se redno izvajajo obratovalni monitoringi kemijskega stanja podzemne vode. Kljub temu izotopske tehnike niso rutinsko uporabljene. Zato smo uporabili analizo izotopov vodika, ogljika in kisika v kombinaciji s skupno alkalnostjo, da bi ocenili vpliv izbranega odlagališča na podzemno vodo in ovrednotili biogeokemične procese. δ18O, δ2H, δ13CDIC, aktivnost 3H in skupna alkalnost so bile določene v oktobru 2020 v 12 vodnjakih v okolici odlagališč Gajke in Brstje in v izcedni vodi iz odlagališča Gajke. Vrednosti δ18O (-9,24 ± 0,3 ‰) in δ2H (-64,9 ± 2,7 ‰) v podzemni vodi kažejo, da je glavni vir vode neposredna infiltracija padavin, brez bistvene izotopske frakcionacije. Totalna alkalnost na preiskanem območju se spreminja od 5.45 do 73 mM, δ13CDIC od –14.9 do +6.1 ‰. Višje vrednosti totalne alkalnosti (do 73 mM), δ 13CDIC (do +6.1 ‰), δ18O (-7.64 ‰) in 3H z 209.8 TU so zaznane v izcedni vodi CERO Gajke (kanal), kar kaže na biogeokemijski proces redukcije CO2 ali metanogeneze. Metanogeneza bi lahko bila prisotna tudi na lokacijah GAP-10/13 (odlagališče Brstje) in G-2 (odlagališče Gajke) z δ13CDIC vrednostima od -8.2 do -7.6 ‰ in z vrednostjo raztopljenega kisika okrog 0 % ter povišano vrednostjo 3H (od 16 do 18.2 TU). V tej raziskavi smo dokazali, da so izotopi koristna orodja v monitoring raziskavah odlagališč in kažejo na spremembe biogeokemičnih procesov v podzemni vodi.
Keywords:podzemna voda, monitoring, odlagališče odpadkov, stabilni izotopi, tritij, Gajke, Brstje


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