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Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F03%3A00000119%21RIV%2F2004%2FMZP%2FN03004%2FN
rdf:type
n9:Vysledek skos:Concept
dcterms:description
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 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
dcterms:title
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 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
skos:prefLabel
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 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
skos:notation
RIV/00025798:_____/03:00000119!RIV/2004/MZP/N03004/N
n3:strany
765;779
n3:aktivita
n17:Z
n3:aktivity
Z(MZP:N03/98:00)
n3:cisloPeriodika
5
n3:dodaniDat
n12:2004
n3:domaciTvurceVysledku
n7:3685322
n3:druhVysledku
n15:J
n3:duvernostUdaju
n16:S
n3:entitaPredkladatele
n14:predkladatel
n3:idSjednocenehoVysledku
627005
n3:idVysledku
RIV/00025798:_____/03:00000119
n3:jazykVysledku
n11:eng
n3:klicovaSlova
stable isotopes;sulfur;nitrogen;carbon;atmospheric deposition;organic matter;sulfate reduction;ratios;catchment;soils;assimilation;mineralization
n3:klicoveSlovo
n5:organic%20matter n5:nitrogen n5:sulfate%20reduction n5:mineralization n5:soils n5:atmospheric%20deposition n5:ratios n5:carbon n5:catchment n5:assimilation n5:stable%20isotopes n5:sulfur
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[7AA912933660]
n3:nazevZdroje
Applied Geochemistry
n3:obor
n10:DD
n3:pocetDomacichTvurcuVysledku
5
n3:pocetTvurcuVysledku
6
n3:pocetUcastnikuAkce
0
n3:pocetZahranicnichUcastnikuAkce
0
n3:rokUplatneniVysledku
n12:2003
n3:svazekPeriodika
18
n3:tvurceVysledku
Novák, Martin
n3:zamer
n13:MZP%3AN03%2F98%3A00
s:issn
0883-2927
s:numberOfPages
14