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Naslov:δ13C as a tool to determine the origin of soil organic carbon : Case study of a restored sloping orchard
Avtorji:ID Muršec, Mateja (Avtor)
ID Leveque, Jean (Avtor)
Datoteke:.pdf Mursec-2023-δ13C_as_a_tool_to_determine_the_or.pdf (287,07 KB)
MD5: 85657E3B69D77C2AA865426EFB172151
 
URL https://doi.org/10.17221/101/2022-SWR
 
Jezik:Angleški jezik
Vrsta gradiva:Znanstveno delo
Tipologija:1.01 - Izvirni znanstveni članek
Organizacija:FKBV - Fakulteta za kmetijstvo in biosistemske vede
Opis:The effect of drip irrigation on the origin and size fraction of soil organic carbon was studied in the soils of an apple orchard (Malus domestica Borkh.) on hilly (20%) terrain in northeastern Slovenia in three slope positions (upslope, midslope and downslope), comparing irrigated with non-irrigated soils. Physical fractionation of soil organic carbon was performed on three soil layers (0–0.05, 0.05–0.15 and 0.15–0.30 m) in three size fractions: fraction A (> 0.0002 m), fraction B (0.0002‒0.00005 m) and fraction C (< 0.00005 m). Fraction A was the richest in soil organic carbon (7.7%), but fraction C was the dominant fraction in the total soil volume (86‒92%), making it the largest source of soil organic carbon (73%). The δ13C signature was performed to determine the existence of two different types (origins) of soil organic carbon: fresh and sedimentary. Fresh organic carbon dominates in the A fraction, while sedimentary organic carbon dominates in the C fraction and may contribute to higher structural stability, besides higher carbonates in the finest fraction. Irrigation mainly contributes to the higher stock of soil organic carbon (predominantly fresh and less sedimentary) in the coarse A fraction (21.14 t/ha in irrigated and 14.17 t/ha in non-irrigated soils).
Ključne besede:CaCO3, carbon isotopes, drip irrigation, physical fractionation, soil organic matter
Status publikacije:Objavljeno
Verzija publikacije:Objavljena publikacija
Poslano v recenzijo:13.07.2022
Datum sprejetja članka:20.01.2023
Datum objave:22.02.2023
Založnik:Institute of Agricultural Economics and Information
Leto izida:2023
Št. strani:Str. 81-88
Številčenje:Letn. 18, Št. 2
PID:20.500.12556/DKUM-86980-fb9cf040-88b7-b53f-8947-5d9037ac4b49 Novo okno
UDK:631.4
COBISS.SI-ID:152677891 Novo okno
DOI:10.17221/101/2022-SWR Novo okno
ISSN pri članku:1801-5395
Datum objave v DKUM:02.02.2024
Število ogledov:558
Število prenosov:54
Metapodatki:XML DC-XML DC-RDF
Področja:Ostalo
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Vaša ocena:Ocenjevanje je dovoljeno samo prijavljenim uporabnikom.
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Gradivo je del revije

Naslov:Soil and Water Research
Skrajšan naslov:Soil Water Res.
Založnik:Czech Academy of Agricultural Sciences, Institute of Agricultural Economics and Information, Czech Academy of Agricultural Sciences - Institute of Agricultural and Food Information
ISSN:1801-5395
COBISS.SI-ID:152672515 Novo okno

Licence

Licenca:CC BY 4.0, Creative Commons Priznanje avtorstva 4.0 Mednarodna
Povezava:http://creativecommons.org/licenses/by/4.0/deed.sl
Opis:To je standardna licenca Creative Commons, ki daje uporabnikom največ možnosti za nadaljnjo uporabo dela, pri čemer morajo navesti avtorja.
Začetek licenciranja:22.02.2023

Sekundarni jezik

Jezik:Slovenski jezik
Ključne besede:ogljikovi izotopi, kapljično namakanje, fizikalna frakcionacija, organske snovi v tleh


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