"Applied Geochemistry" . "5" . "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"@en . "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" . . "Z(MZP:N03/98:00)" . "Nov\u00E1k, Martin" . "0883-2927" . "GB - Spojen\u00E9 kr\u00E1lovstv\u00ED Velk\u00E9 Brit\u00E1nie a Severn\u00EDho Irska" . . . . "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"@en . . . "18" . . . . . "6"^^ . "[7AA912933660]" . . . "RIV/00025798:_____/03:00000119" . . "14"^^ . "5"^^ . . . "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" . "RIV/00025798:_____/03:00000119!RIV/2004/MZP/N03004/N" . . . "stable isotopes;sulfur;nitrogen;carbon;atmospheric deposition;organic matter;sulfate reduction;ratios;catchment;soils;assimilation;mineralization"@en . . "765;779" . . . . "0"^^ . . "627005" . "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"@en . . "0"^^ . . "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" .