Bechtel, Achim

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  • Bechtel, Achim (1)
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Distribution of fatty acids and alcohols in lignites, from the Smederevsko Pomoravlje field, Kostolac Basin – biogeochemical approach

Đoković, Nataša; Mitrović, Danica; Bechtel, Achim; Vuković, Nikola; Medić, Ana; Vuković, Nikola; Životić, Dragana; Stojanović, Ksenija

(Beograd : Srpsko hemijsko društvo, 2015)

TY  - CONF
AU  - Đoković, Nataša
AU  - Mitrović, Danica
AU  - Bechtel, Achim
AU  - Vuković, Nikola
AU  - Medić, Ana
AU  - Vuković, Nikola
AU  - Životić, Dragana
AU  - Stojanović, Ksenija
PY  - 2015
UR  - https://ritnms.itnms.ac.rs/handle/123456789/915
AB  - In present study, both lipid classes, fatty acids and neutral lipids (e.g. alcohols) were
analysed in lignite samples in order to assess organic matter source and study biogeochemical and
diagenetic alteration processes.
The choice of polar compounds as useful biomarker indicators is based on several
considerations. As lipids, fatty acids are involved in energy storage, mobilization and in
membrane structure in all living organisms, while sterols have roles in membrane function and
hormonal regulation of metabolic processes primarily only in eucaryotes [1].
Pulverised lignites were extracted by an azeotrope mixture of dichloromethane and
methanol (88:12, v:v) using a Soxhlet’s apparatus. Extracts were dissolved in a mixture of nheptane:
dichloromethane (80:1, v:v) and asphaltenes were precipitated. The heptane-soluble
organic compounds (maltenes) were separated into saturated hydrocarbons, aromatic
hydrocarbons and NSO fraction (polar fraction, which contains nitrogen, sulphur, and oxygen
compounds) using column chromatography. Portions of NSO fractions were concentrated after
which the extracts were saponified with a mixture of 6% KOH in CH3OH and distilled water (3:1,
v:v) at 80°C (pH = 14). Fatty acids (FAs) and alcohols were analysed using a method modified
from Wakeham and Beier (1991) [1]. Alcohols and FAs were extracted 3 times with n-hexane at
pH 14 and pH 1, respectively using Na2SO4 for removal of the excess water. Prior to gas
chromatography-mass spectrometry analysis (GC-MS), the FAs and alcohol fractions were
derivatised with BSTFA (N,O-bis(trimethylsilyl)trifluoroacetamide, Fluka) for 1 h at 80°C to
form trimethylsilyl esters and ethers.
The obtained results are as follows: the fatty alcohols ranging from n-C12 to n-C28 alkanols
with a high abundance of long-chain fatty alcohols (n-C22 – C28) and only trace levels of shortchain
fatty alcohols (n-C12 – C18) indicating the main terrestrial input into the system. The
monounsaturated n-C18:1 fatty alcohol, which has been found in some species of diatoms,
Skeletonema costatum [2], was also present in samples. Steroidal alcohols, β-sitosterol (5-
cholesten-24β-ethyl-3β-ol), stigmastanol (24α-ethyl-5α-cholestan-3β-ol) and cholesterol, which
are the major sterols found in higher plants, are also found in small quantities. The presence of
kauran-13-ol is in accordance with the premise of terrestrial origin, given that abietane, pimarane,
kaurane and podocarpane skeletons are produced primarily by conifer vascular plants.
n-Alcanoic acids ranging from n-C6 – C30 with a notable predominance of even chainlenghts
are present in samples, having the maximum at hexadecanoic acid (C16:0). Saturated
compounds dominate in distribution but two unsaturated fatty acids were also found, 9-
octadecanoic (C18:1) and 9-hexadecanoic acid (C16:1). Apart from fatty acids, the polar fraction contains 4,8,12,16-tetramethylheptadecan-4-olide (a fragment of chlorophyll molecule with a side
phytol chain).
Typically high concentrations of long-chain (C22 –C30) n-alkanoic acids and n-alkanols (C12
– C28) with a sharp predominance of even homologues, certain hydroxyacids and dicarboxylic
acids, diterpenoid acids, long-chain saturated alkyl (wax) esters are characteristic components of
higher vascular plant cutin and suberin [3]. Biomarker analysis of aliphatic and aromatic fraction
of lignite coal is in concordance with the results obtained in the investigation of polar compounds,
confirming that in the case of Kostolac lignite, conifer terrestrial input was dominant source of
organic matter.
PB  - Beograd : Srpsko hemijsko društvo
C3  - 7. simpozijum „Hemija i zaštita životne sredine“ sa međunarodnim učešćem (EnviroChem 2015)
T1  - Distribution of fatty acids and alcohols in lignites, from the Smederevsko Pomoravlje field, Kostolac Basin – biogeochemical approach
EP  - 228
SP  - 227
ER  - 
@conference{
author = "Đoković, Nataša and Mitrović, Danica and Bechtel, Achim and Vuković, Nikola and Medić, Ana and Vuković, Nikola and Životić, Dragana and Stojanović, Ksenija",
year = "2015",
abstract = "In present study, both lipid classes, fatty acids and neutral lipids (e.g. alcohols) were
analysed in lignite samples in order to assess organic matter source and study biogeochemical and
diagenetic alteration processes.
The choice of polar compounds as useful biomarker indicators is based on several
considerations. As lipids, fatty acids are involved in energy storage, mobilization and in
membrane structure in all living organisms, while sterols have roles in membrane function and
hormonal regulation of metabolic processes primarily only in eucaryotes [1].
Pulverised lignites were extracted by an azeotrope mixture of dichloromethane and
methanol (88:12, v:v) using a Soxhlet’s apparatus. Extracts were dissolved in a mixture of nheptane:
dichloromethane (80:1, v:v) and asphaltenes were precipitated. The heptane-soluble
organic compounds (maltenes) were separated into saturated hydrocarbons, aromatic
hydrocarbons and NSO fraction (polar fraction, which contains nitrogen, sulphur, and oxygen
compounds) using column chromatography. Portions of NSO fractions were concentrated after
which the extracts were saponified with a mixture of 6% KOH in CH3OH and distilled water (3:1,
v:v) at 80°C (pH = 14). Fatty acids (FAs) and alcohols were analysed using a method modified
from Wakeham and Beier (1991) [1]. Alcohols and FAs were extracted 3 times with n-hexane at
pH 14 and pH 1, respectively using Na2SO4 for removal of the excess water. Prior to gas
chromatography-mass spectrometry analysis (GC-MS), the FAs and alcohol fractions were
derivatised with BSTFA (N,O-bis(trimethylsilyl)trifluoroacetamide, Fluka) for 1 h at 80°C to
form trimethylsilyl esters and ethers.
The obtained results are as follows: the fatty alcohols ranging from n-C12 to n-C28 alkanols
with a high abundance of long-chain fatty alcohols (n-C22 – C28) and only trace levels of shortchain
fatty alcohols (n-C12 – C18) indicating the main terrestrial input into the system. The
monounsaturated n-C18:1 fatty alcohol, which has been found in some species of diatoms,
Skeletonema costatum [2], was also present in samples. Steroidal alcohols, β-sitosterol (5-
cholesten-24β-ethyl-3β-ol), stigmastanol (24α-ethyl-5α-cholestan-3β-ol) and cholesterol, which
are the major sterols found in higher plants, are also found in small quantities. The presence of
kauran-13-ol is in accordance with the premise of terrestrial origin, given that abietane, pimarane,
kaurane and podocarpane skeletons are produced primarily by conifer vascular plants.
n-Alcanoic acids ranging from n-C6 – C30 with a notable predominance of even chainlenghts
are present in samples, having the maximum at hexadecanoic acid (C16:0). Saturated
compounds dominate in distribution but two unsaturated fatty acids were also found, 9-
octadecanoic (C18:1) and 9-hexadecanoic acid (C16:1). Apart from fatty acids, the polar fraction contains 4,8,12,16-tetramethylheptadecan-4-olide (a fragment of chlorophyll molecule with a side
phytol chain).
Typically high concentrations of long-chain (C22 –C30) n-alkanoic acids and n-alkanols (C12
– C28) with a sharp predominance of even homologues, certain hydroxyacids and dicarboxylic
acids, diterpenoid acids, long-chain saturated alkyl (wax) esters are characteristic components of
higher vascular plant cutin and suberin [3]. Biomarker analysis of aliphatic and aromatic fraction
of lignite coal is in concordance with the results obtained in the investigation of polar compounds,
confirming that in the case of Kostolac lignite, conifer terrestrial input was dominant source of
organic matter.",
publisher = "Beograd : Srpsko hemijsko društvo",
journal = "7. simpozijum „Hemija i zaštita životne sredine“ sa međunarodnim učešćem (EnviroChem 2015)",
title = "Distribution of fatty acids and alcohols in lignites, from the Smederevsko Pomoravlje field, Kostolac Basin – biogeochemical approach",
pages = "228-227"
}
Đoković, N., Mitrović, D., Bechtel, A., Vuković, N., Medić, A., Vuković, N., Životić, D.,& Stojanović, K.. (2015). Distribution of fatty acids and alcohols in lignites, from the Smederevsko Pomoravlje field, Kostolac Basin – biogeochemical approach. in 7. simpozijum „Hemija i zaštita životne sredine“ sa međunarodnim učešćem (EnviroChem 2015)
Beograd : Srpsko hemijsko društvo., 227-228.
Đoković N, Mitrović D, Bechtel A, Vuković N, Medić A, Vuković N, Životić D, Stojanović K. Distribution of fatty acids and alcohols in lignites, from the Smederevsko Pomoravlje field, Kostolac Basin – biogeochemical approach. in 7. simpozijum „Hemija i zaštita životne sredine“ sa međunarodnim učešćem (EnviroChem 2015). 2015;:227-228..
Đoković, Nataša, Mitrović, Danica, Bechtel, Achim, Vuković, Nikola, Medić, Ana, Vuković, Nikola, Životić, Dragana, Stojanović, Ksenija, "Distribution of fatty acids and alcohols in lignites, from the Smederevsko Pomoravlje field, Kostolac Basin – biogeochemical approach" in 7. simpozijum „Hemija i zaštita životne sredine“ sa međunarodnim učešćem (EnviroChem 2015) (2015):227-228.