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Trace element composition of concretions, ICP–MS measurements

Description: In order to get a complete geochemical signature, 14 P-rich concretions, chosen among the different cores, were acid digested (Table 3a and Table 3b). In a clean laboratory, 1.7 to 36 mg of concretions were digested overnight in a concentrated mixture of Suprapur acid (3 ml HCl/2 ml HNO3/1 ml HF) at 90 °C in sealed Teflon beakers. After evaporation to dryness, the residue was dissolved in 2.5 ml of 2% HNO3 Suprapur and diluted to 12 ml with Milli-Q water. During the same procedure, we have also dissolved and analysed, for comparison, a pure vivianite from Anlua, Cameroon (tubular crystals, MRAC collection).

Global identifier:

Doi(
    "10.1594/GFZ.SDDB.1059",
)

Types:

Origins: /Wissenschaft/Helmholtz-Gemeinschaft/GFZ

Tags: Ytterbium ? Barium ? Cerium ? Kobalt ? Dysprosium ? Hafnium ? Niob ? Rubidium ? Strontium ? Tantal ? Zirkonium ? Blei ? Kupfer ? Gadolinium ? Erbium ? Europium ? Holmium ? Lutetium ? Neodym ? Praseodym ? Samarium ? Thorium ? Salpetersäure ? Lanthan ? Uran ? Yttrium ? Zink ? Verdunstung ? Vergleichsanalyse ? R/V Vereshchagin ? sample depth ? type of main lithological unit ? Vereshchagin 98 Expedition ? ICP-MS ? Vereshchagin Long Cores Expedition 2001 ?

License: unbekannt

Language: Englisch/English

Organisations

Issued: 2006-01-01

Time ranges: 2006-01-01 - 2006-01-01

Status

Quality score

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