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25th International Meeting on Organic Geochemistry IMOG 2011

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P-283<br />

Correlati<strong>on</strong> between compositi<strong>on</strong> of naphthenoarenes and their<br />

saturated analogues in oils from different geological age<br />

deposits<br />

Natalya Vor<strong>on</strong>etskaya, Galina Pevneva, Anatoly Golovko<br />

Institute of Petroleum Chemistry SB RAS, Tomsk, Russian Federati<strong>on</strong> (corresp<strong>on</strong>ding<br />

author:vor<strong>on</strong>etskaya@ipc.tsc.ru)<br />

Now hydrocarb<strong>on</strong>s of hybrid structure c<strong>on</strong>taining<br />

simultaneously aromatic and naphthenic cycles –<br />

naphthenoarenes are the least studied class of oil<br />

compounds. The structure of naphthenearene<br />

molecules determined in oils is similar to that of<br />

saturated cyclic compounds (cyclanes). The aim of<br />

the present work was to study compositi<strong>on</strong>s and<br />

distributi<strong>on</strong>s of naphthenoarenes and cyclanes in oils<br />

of multihoriz<strong>on</strong> fields. The oils recovered from<br />

multihoriz<strong>on</strong> oil fields Sirakovo (5 samples) and<br />

Bradarac-Maljurevac (3 samples) (Serbia) occurring<br />

in Cainozoic deposits, as well as oils from Usinskoye<br />

oil field (5 samples), Paleozoic deposits (Russia) were<br />

used as the objects of investigati<strong>on</strong>.<br />

The oils in Sirakovo oil field occur in the depths<br />

ranging from 1400 to 1800 m and oils in Bradarac-<br />

Maljurevac oil field - from 1800 to 2200 m. The depth<br />

of occurrence of Paleozoic oils in Usinskoye oil field<br />

ranges from 1190 to 1400 m.<br />

C<strong>on</strong>centrates of saturated, m<strong>on</strong>o-, bi- and<br />

triaromatic hydrocarb<strong>on</strong>s were isolated by a column<br />

liquid-adsorpti<strong>on</strong> chromatography. The c<strong>on</strong>centrates<br />

of arenes were divided into fracti<strong>on</strong>s of alkyl- and<br />

naphthenoarenes by extracti<strong>on</strong> with methanol.<br />

Carbamide dewaxing was used to separate cyclanes<br />

from acyclic alkanes.<br />

Compositi<strong>on</strong>s of cyclanes, naphthenobenzenes,<br />

naphthen<strong>on</strong>aphthalenes and<br />

naphthenophenanthrenes were determined by a<br />

mass-spectrometry method via direct introducti<strong>on</strong> of<br />

the sample into an i<strong>on</strong>izati<strong>on</strong> chamber. The energy of<br />

i<strong>on</strong>izing electr<strong>on</strong>s was 12 eV.<br />

Cyclanes c<strong>on</strong>tain from 1 to 5 saturated cycles in<br />

a molecule. Naphthenoarenes are presented by the<br />

compounds with a number of aromatic cycles from 1<br />

(naphthenobenzenes) to 3<br />

(naphthenophenanthrenes). Total number of cycles in<br />

a molecule of naphthenoarenes does not exceed five.<br />

The c<strong>on</strong>tent of compounds with two cycles in a<br />

molecule – m<strong>on</strong><strong>on</strong>aphthenobenzenes and their<br />

saturated analogues bicyclanes – symbately<br />

decreases with the depth of oil occurrence.<br />

Tricyclic compounds are presented by<br />

naphthenobenzenes, m<strong>on</strong><strong>on</strong>aphthen<strong>on</strong>aphthalenes<br />

and their saturated analogues – tricyclanes. The<br />

c<strong>on</strong>tent of dinaphthenobenzenes decreases with the<br />

depth of oil occurrence. The c<strong>on</strong>tent of<br />

naphthen<strong>on</strong>aphthalenes increases in oils from<br />

Cainozoic deposits with the depth of occurrence and<br />

decreases in Paleozoic oils. The c<strong>on</strong>centrati<strong>on</strong> of<br />

tricyclanes in oils from Cainozoic deposits decreases<br />

with the depth of occurrence, while in Paleozoic oils it<br />

increases.<br />

Am<strong>on</strong>g tetracyclic compounds we have studied<br />

distributi<strong>on</strong>s of trinaphthenobenzenes,<br />

dinaphthen<strong>on</strong>aphthalenes,<br />

m<strong>on</strong><strong>on</strong>aphthenophenanthrenes and their saturated<br />

analogues – tetracyclanes. The c<strong>on</strong>tent of<br />

trinaphthenobenzenes decreases with the depth of oil<br />

occurrence. The c<strong>on</strong>tents of<br />

dinaphthen<strong>on</strong>aphthalenes and<br />

m<strong>on</strong><strong>on</strong>aphthenophenanthrenes increase in Cainozoic<br />

oils with the depth of occurrence and decrease in<br />

Paleozoic oils. The c<strong>on</strong>tent of tetracyclanes increases<br />

in deeper occurring oils both from Cainozoic and<br />

Paleozoic deposits.<br />

Pentacyclic compounds are presented by<br />

tetranaphthenobenzenes, trinaphthen<strong>on</strong>aphthalenes,<br />

dinaphthenophenanthrenes and their saturated<br />

analogues – pentacyclanes. The c<strong>on</strong>tents of both<br />

naphthenoarenes and their saturated analogues –<br />

pentacyclanes increase in Cainozoic and Paleozoic<br />

oil with the depth of occurrence. One observes slope<br />

oppositi<strong>on</strong> in the changes of<br />

trinaphthen<strong>on</strong>aphthalenes and pentacyclanes<br />

c<strong>on</strong>centrati<strong>on</strong>s with the depth.<br />

Based <strong>on</strong> the investigati<strong>on</strong>s it was shown that the<br />

c<strong>on</strong>tent of naphthen<strong>on</strong>aphthalenes and<br />

naphthenophenanthrenes with total number of cycles<br />

3-4 increases in Cainozoic oils with the depth of<br />

occurrence, whereas in Paleozoic oils it decreases.<br />

In spite of the age of deposits the c<strong>on</strong>tent of<br />

cyclanes (4-5 cycles) and naphthenoarenes with total<br />

number of cycles in a molecule 5 increases with the<br />

depth of occurrence, whereas the c<strong>on</strong>tent of<br />

naphthenobenzens with a number of cycles in a<br />

molecule from 2 to 4 decreases.<br />

416

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