Data Publications

Composition of major oxide in bulk sediments from lake Baikal: ICP-AES data from P-rich samples

hasData_Center_Short_Name
  • SDDB
hasDataset_Online_Resource
hasProject_Long_Name
  • Vereshchagin 98 Expedition
  • Vereshchagin Expedition 98
  • Vereshchagin Long Cores Expedition 2001
  • High-resolution CONTINENTal paleoclimate record in Lake Baikal
hasDataset_Release_Date
  • 2006-09-15
hasDataset_Title
  • Composition of major oxide in bulk sediments from lake Baikal: ICP-AES data from P-rich samples
hasEntry_ID
  • 10.1594/GFZ.SDDB.1055
hasKeyword
  • S
  • Al2O3
  • CaO
  • Fe2O3 total
  • K2O
  • MgO
  • MnO
  • Na2O
  • P2O5
  • PF
  • SiO2
  • SiO2 excess
  • TiO2
  • sample depth
  • total
hasReference
  • 10.1016/j.gloplacha.2004.09.022 http://dx.doi.org/10.1016/j.gloplacha.2004.09.022 N. Fagel, L.Y. Alleman, L. Granina, F. Hatert, E. Bozso, R. Cloots and L. André, Vivianite formation and distribution in Lake Baikal sediments, Glob. Planet. Change 46 (2005), pp. 315-336.
hasSummary
  • The sediment cores were sampled with a resolution of 10 cm, resulting in a total of 290 samples (Table 2). Around 250 mg of dried sediments was mechanically crushed through 100–200-μm mesh then processed by an alkaline digestion (Lithium meta-borate) in a Pt crucible at 1000 °C for 1 h. The residue was dissolved over night in a nitric acid matrix and then major and minor elements (Al, Ba, Ca, Fe, K, Mg, Mn, Na, P, S, Si, Sr, Ti) were analysed by Atomic Emission Spectrometry ICP-AES (Thermo Optek Iris Advantage, Royal Museum for Central Africa, Tervuren, Belgium). Y and Au internal standards were used to correct for instrumental drift. For both trace and major elements analyses, external calibrations were performed using artificial standard solutions and dissolved mineralised natural rock standard (e.g., BHVO-1, DWA, CCH-1 SGR-1, JGB-1).
GCMD Sciencekeywords describing the dataset. Click on Keyword to find similar datasets