_version_ 1867169038766964736
author Shulga, N A
Peresypkin, Valery I
Revelskii, I A
author_facet Shulga, N A
Peresypkin, Valery I
Revelskii, I A
collection Datos científicos de ciencias marinas y ambientales
contents Optimum conditions were selected for chromatographic separation of model mixtures of C12-C40 n-alkanes. For one of samples of hydrothermal deposits extraction conditions of hydrocarbons were studied and a sample preparation procedure was selected. The procedure was proposed to determine n-alkanes in samples of hydrothermal deposits by means of gas chromatography - mass spectrometry (GC-MS). Detection limit for n-alkanes was 3x10**-9 to 10**-8% depending on components. On the basis of the proposed procedure composition of n-alkanes was studied in samples of hydrothermal deposits collected at the Mid-Atlantic Ridge (Broken Spur, Lost City, and Rainbow hydrothermal fields). Analyses showed that samples contained C14-C35 n-alkanes. Concentrations of the n-alkanes were rather low and varied from 0.002 to 0.038 µg/g. Hypotheses concerning genesis of identified n-alkanes were offered.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_770016
institution PANGAEA
language en
publishDate 2010
publisher PANGAEA
record_format pangaea
spellingShingle (Table 3) Relative content of n-alkane groups in samples from hydrothermal fields of the Mid-Atlantic Ridge
Shulga, N A
Peresypkin, Valery I
Revelskii, I A
Akademik Mstislav Keldysh; AMK50; AMK50-4793-1; AMK50-4796-3; AMK50-4797-8; AMK50-4800-2; AMK50-4800-7; AMK50-4806-3; AMK50-4815-6; AMK50-4816-1; AMK50-4816-5; Archive of Ocean Data; ARCOD; Area/locality; Broken Srur Hydrothermal Field, K point mound; Broken Srur Hydrothermal Field, Spire mound; Broken Srur Hydrothermal Field, Triple Chimney mound; Calculated; Carbon Preference Index; Elevation of event; Event label; Gas chromatography - Mass spectrometry (GC-MS); i-C19/i-C20 ratio; Latitude of event; Longitude of event; Lost City; Lost Village Field, Mid-Atlantic Ridge; MIR; MIR deep-sea manned submersible; n-alkanes, total, per unit sediment mass; Rainbow; Sample type; Sum(C14-C22)/sum(C23-C35) n-alkanes ratio; Sum n-alkanes C14-C17; Sum n-alkanes C18-C22; Sum n-alkanes C20-C24; Sum n-alkanes C23-C35
Optimum conditions were selected for chromatographic separation of model mixtures of C12-C40 n-alkanes. For one of samples of hydrothermal deposits extraction conditions of hydrocarbons were studied and a sample preparation procedure was selected. The procedure was proposed to determine n-alkanes in samples of hydrothermal deposits by means of gas chromatography - mass spectrometry (GC-MS). Detection limit for n-alkanes was 3x10**-9 to 10**-8% depending on components. On the basis of the proposed procedure composition of n-alkanes was studied in samples of hydrothermal deposits collected at the Mid-Atlantic Ridge (Broken Spur, Lost City, and Rainbow hydrothermal fields). Analyses showed that samples contained C14-C35 n-alkanes. Concentrations of the n-alkanes were rather low and varied from 0.002 to 0.038 µg/g. Hypotheses concerning genesis of identified n-alkanes were offered.
title (Table 3) Relative content of n-alkane groups in samples from hydrothermal fields of the Mid-Atlantic Ridge
topic Akademik Mstislav Keldysh; AMK50; AMK50-4793-1; AMK50-4796-3; AMK50-4797-8; AMK50-4800-2; AMK50-4800-7; AMK50-4806-3; AMK50-4815-6; AMK50-4816-1; AMK50-4816-5; Archive of Ocean Data; ARCOD; Area/locality; Broken Srur Hydrothermal Field, K point mound; Broken Srur Hydrothermal Field, Spire mound; Broken Srur Hydrothermal Field, Triple Chimney mound; Calculated; Carbon Preference Index; Elevation of event; Event label; Gas chromatography - Mass spectrometry (GC-MS); i-C19/i-C20 ratio; Latitude of event; Longitude of event; Lost City; Lost Village Field, Mid-Atlantic Ridge; MIR; MIR deep-sea manned submersible; n-alkanes, total, per unit sediment mass; Rainbow; Sample type; Sum(C14-C22)/sum(C23-C35) n-alkanes ratio; Sum n-alkanes C14-C17; Sum n-alkanes C18-C22; Sum n-alkanes C20-C24; Sum n-alkanes C23-C35
url https://doi.org/10.1594/PANGAEA.770016