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

Cite as:

Fagel, Natalie; Alleman, Laurent; Granina, L; Hatert, F; Thamo-Boszo, Edit; Cloots, R; André, Luc (2006): Composition of major oxide in bulk sediments from lake Baikal: ICP-AES data from P-rich samples. Deutsches GeoForschungsZentrum GFZ. https://doi.org/10.1594/GFZ.SDDB.1055

Status

I N R E V I E W : Fagel, Natalie; Alleman, Laurent; Granina, L; Hatert, F; Thamo-Boszo, Edit; Cloots, R; André, Luc (2006): Composition of major oxide in bulk sediments from lake Baikal: ICP-AES data from P-rich samples. Deutsches GeoForschungsZentrum GFZ. https://doi.org/10.1594/GFZ.SDDB.1055

Abstract

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).

Authors

Fagel, Natalie
Alleman, Laurent
Granina, L
Hatert, F
Thamo-Boszo, Edit
Cloots, R
André, Luc

Keywords

, Geology

GCMD Science Keywords

EARTH SCIENCE > Land Surface > Erosion/Sedimentation > Sediment Compositon

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