Similarity between C,N and S stable isotope profiles in European spruce forest soils: Implications for the use of delta S-34 as a tracer

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F03%3A00000119" target="_blank" >RIV/00025798:_____/03:00000119 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Similarity between C,N and S stable isotope profiles in European spruce forest soils: Implications for the use of delta S-34 as a tracer

Popis výsledku v původním jazyce

Stable isotope systematics of C, N and S were studied in soils of 5 European forest ecosystems. In Picea stands, the behavior of C, N and S isotopes was similar in 3 aspects: (1) assimilation favored the lighter isotopes C-12, N-14 and S-32; (2) mineralization in the soil profile left in situ residues enriched in the heavier isotopes C-13, N-15 and S-34; and (3) NO3-N as well as SO4-S in soil solution was isotopically lighter compared to the same species in the atmospheric input. Stable sotope systematics of Jezeri soil S (mean of 2.5parts per thousand in the O + A horizon, 4.8parts per thousand in the B horizon, and 5.8parts per thousand in the bedrock) suggests that most of the soil-derived S in discharge must come from the

Název v anglickém jazyce

Similarity between C,N and S stable isotope profiles in European spruce forest soils: Implications for the use of delta S-34 as a tracer

Popis výsledku anglicky

Stable isotope systematics of C, N and S were studied in soils of 5 European forest ecosystems. In Picea stands, the behavior of C, N and S isotopes was similar in 3 aspects: (1) assimilation favored the lighter isotopes C-12, N-14 and S-32; (2) mineralization in the soil profile left in situ residues enriched in the heavier isotopes C-13, N-15 and S-34; and (3) NO3-N as well as SO4-S in soil solution was isotopically lighter compared to the same species in the atmospheric input. Stable sotope systematics of Jezeri soil S (mean of 2.5parts per thousand in the O + A horizon, 4.8parts per thousand in the B horizon, and 5.8parts per thousand in the bedrock) suggests that most of the soil-derived S in discharge must come from the

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DD - Geochemie

OECD FORD obor

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Projekt

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2003

Kód důvěrnosti údajů

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

Název periodika

Applied Geochemistry

ISSN

0883-2927

e-ISSN

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Svazek periodika

18

Číslo periodika v rámci svazku

5

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

14

Strana od-do

765-779

Kód UT WoS článku

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EID výsledku v databázi Scopus

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