(Table 2) Concentrations and composition of aliphatic hydrocarbons in bottom sediments of the Sakhalin shelf

Aliphatic and polycyclic aromatic hydrocarbons were examined in the surface layer of bottom sediments from the eastern part of the Sakhalin Island shelf (materials were sampled in summer 2002). Concentrations of hydrocarbons were determined to know changed since beginning of development of oil field...

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Bibliographic Details
Main Author: Nemirovskaya, Inna A
Format: Dataset
Language:English
Published: PANGAEA 2008
Subjects:
Aliphatic hydrocarbons
Archive of Ocean Data
ARCOD
Calculated
Carbon
organic
total
Carbon analyser AN-7529
7560
Carbon Preference Index
Depth
bottom/max
sediment/rock
top/min
Event label
Grab
Infrared spectrometry
Latitude of event
Longitude of event
n-Alkane sum
NES02-14
NES02-29
NES02-5
NES02-60
NES02-66
NES02-67
NES02-69
NES02-72
NES02-79
NES02-80
NES02-81
NES02-82
NES02-85
NES02-86
NES02-87
NES02-94
NES02-95
NES02-96
NES02-99
Percentage
Ratio
Sea of Okhotsk
Sakhalin Shelf
Okhotsk
Sakhalin
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.745953
https://doi.org/10.1594/PANGAEA.745953
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.745953
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.745953 2023-05-15T18:08:52+02:00 (Table 2) Concentrations and composition of aliphatic hydrocarbons in bottom sediments of the Sakhalin shelf Nemirovskaya, Inna A MEDIAN LATITUDE: 52.077142 * MEDIAN LONGITUDE: 143.547279 * SOUTH-BOUND LATITUDE: 48.194000 * WEST-BOUND LONGITUDE: 142.824100 * NORTH-BOUND LATITUDE: 54.522600 * EAST-BOUND LONGITUDE: 144.390100 * MINIMUM DEPTH, sediment/rock: 0.005 m * MAXIMUM DEPTH, sediment/rock: 0.005 m 2008-10-06 text/tab-separated-values, 190 data points https://doi.pangaea.de/10.1594/PANGAEA.745953 https://doi.org/10.1594/PANGAEA.745953 en eng PANGAEA Nemirovskaya, Inna A (2008): Concentrations and composition of hydrocarbons in bottom sediments of the Sakhalin shelf. Geokhimiya (Geochemistry), Geochemistry International, 56(4), 375-385, https://doi.org/10.1134/S001670290804006X https://doi.pangaea.de/10.1594/PANGAEA.745953 https://doi.org/10.1594/PANGAEA.745953 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow Aliphatic hydrocarbons Archive of Ocean Data ARCOD Calculated Carbon organic total Carbon analyser AN-7529 7560 Carbon Preference Index Depth bottom/max sediment/rock top/min Event label Grab Infrared spectrometry Latitude of event Longitude of event n-Alkane sum NES02-14 NES02-29 NES02-5 NES02-60 NES02-66 NES02-67 NES02-69 NES02-72 NES02-79 NES02-80 NES02-81 NES02-82 NES02-85 NES02-86 NES02-87 NES02-94 NES02-95 NES02-96 NES02-99 Percentage Ratio Sea of Okhotsk Sakhalin Shelf Dataset 2008 ftpangaea https://doi.org/10.1594/PANGAEA.745953 https://doi.org/10.1134/S001670290804006X 2023-01-20T08:51:30Z Aliphatic and polycyclic aromatic hydrocarbons were examined in the surface layer of bottom sediments from the eastern part of the Sakhalin Island shelf (materials were sampled in summer 2002). Concentrations of hydrocarbons were determined to know changed since beginning of development of oil fields (compared with earlier years). According to distribution of markers in hydrocarbon compositions, bottom sediments are dominated by allochthonous (terrigenous) hydrocarbons that are the most stable compounds. Occurrence of transformed anthropogenic oil alkanes that have never been found before may be indicative of increasing pollution in the region. Dataset Sakhalin PANGAEA - Data Publisher for Earth & Environmental Science Okhotsk ENVELOPE(142.824100,144.390100,54.522600,48.194000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Aliphatic hydrocarbons
Archive of Ocean Data
ARCOD
Calculated
Carbon
organic
total
Carbon analyser AN-7529
7560
Carbon Preference Index
Depth
bottom/max
sediment/rock
top/min
Event label
Grab
Infrared spectrometry
Latitude of event
Longitude of event
n-Alkane sum
NES02-14
NES02-29
NES02-5
NES02-60
NES02-66
NES02-67
NES02-69
NES02-72
NES02-79
NES02-80
NES02-81
NES02-82
NES02-85
NES02-86
NES02-87
NES02-94
NES02-95
NES02-96
NES02-99
Percentage
Ratio
Sea of Okhotsk
Sakhalin Shelf
spellingShingle Aliphatic hydrocarbons
Archive of Ocean Data
ARCOD
Calculated
Carbon
organic
total
Carbon analyser AN-7529
7560
Carbon Preference Index
Depth
bottom/max
sediment/rock
top/min
Event label
Grab
Infrared spectrometry
Latitude of event
Longitude of event
n-Alkane sum
NES02-14
NES02-29
NES02-5
NES02-60
NES02-66
NES02-67
NES02-69
NES02-72
NES02-79
NES02-80
NES02-81
NES02-82
NES02-85
NES02-86
NES02-87
NES02-94
NES02-95
NES02-96
NES02-99
Percentage
Ratio
Sea of Okhotsk
Sakhalin Shelf
Nemirovskaya, Inna A
(Table 2) Concentrations and composition of aliphatic hydrocarbons in bottom sediments of the Sakhalin shelf
topic_facet Aliphatic hydrocarbons
Archive of Ocean Data
ARCOD
Calculated
Carbon
organic
total
Carbon analyser AN-7529
7560
Carbon Preference Index
Depth
bottom/max
sediment/rock
top/min
Event label
Grab
Infrared spectrometry
Latitude of event
Longitude of event
n-Alkane sum
NES02-14
NES02-29
NES02-5
NES02-60
NES02-66
NES02-67
NES02-69
NES02-72
NES02-79
NES02-80
NES02-81
NES02-82
NES02-85
NES02-86
NES02-87
NES02-94
NES02-95
NES02-96
NES02-99
Percentage
Ratio
Sea of Okhotsk
Sakhalin Shelf
description Aliphatic and polycyclic aromatic hydrocarbons were examined in the surface layer of bottom sediments from the eastern part of the Sakhalin Island shelf (materials were sampled in summer 2002). Concentrations of hydrocarbons were determined to know changed since beginning of development of oil fields (compared with earlier years). According to distribution of markers in hydrocarbon compositions, bottom sediments are dominated by allochthonous (terrigenous) hydrocarbons that are the most stable compounds. Occurrence of transformed anthropogenic oil alkanes that have never been found before may be indicative of increasing pollution in the region.
format Dataset
author Nemirovskaya, Inna A
author_facet Nemirovskaya, Inna A
author_sort Nemirovskaya, Inna A
title (Table 2) Concentrations and composition of aliphatic hydrocarbons in bottom sediments of the Sakhalin shelf
title_short (Table 2) Concentrations and composition of aliphatic hydrocarbons in bottom sediments of the Sakhalin shelf
title_full (Table 2) Concentrations and composition of aliphatic hydrocarbons in bottom sediments of the Sakhalin shelf
title_fullStr (Table 2) Concentrations and composition of aliphatic hydrocarbons in bottom sediments of the Sakhalin shelf
title_full_unstemmed (Table 2) Concentrations and composition of aliphatic hydrocarbons in bottom sediments of the Sakhalin shelf
title_sort (table 2) concentrations and composition of aliphatic hydrocarbons in bottom sediments of the sakhalin shelf
publisher PANGAEA
publishDate 2008
url https://doi.pangaea.de/10.1594/PANGAEA.745953
https://doi.org/10.1594/PANGAEA.745953
op_coverage MEDIAN LATITUDE: 52.077142 * MEDIAN LONGITUDE: 143.547279 * SOUTH-BOUND LATITUDE: 48.194000 * WEST-BOUND LONGITUDE: 142.824100 * NORTH-BOUND LATITUDE: 54.522600 * EAST-BOUND LONGITUDE: 144.390100 * MINIMUM DEPTH, sediment/rock: 0.005 m * MAXIMUM DEPTH, sediment/rock: 0.005 m
long_lat ENVELOPE(142.824100,144.390100,54.522600,48.194000)
geographic Okhotsk
geographic_facet Okhotsk
genre Sakhalin
genre_facet Sakhalin
op_source P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
op_relation Nemirovskaya, Inna A (2008): Concentrations and composition of hydrocarbons in bottom sediments of the Sakhalin shelf. Geokhimiya (Geochemistry), Geochemistry International, 56(4), 375-385, https://doi.org/10.1134/S001670290804006X
https://doi.pangaea.de/10.1594/PANGAEA.745953
https://doi.org/10.1594/PANGAEA.745953
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.745953
https://doi.org/10.1134/S001670290804006X
_version_ 1766181218045394944

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