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25th International Meeting on Organic Geochemistry IMOG 2011

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P-074<br />

Discussi<strong>on</strong> <strong>on</strong> appliance of 25-norhopanoids compounds in<br />

organic geochemical research<br />

Chunhua Ni 1,2<br />

1 Sinopec Research Institute of Petroleum Explorati<strong>on</strong> and Producti<strong>on</strong>, Beijing, China, 2 Wuxi Institute of<br />

Petroleum Geology, Sinopec Research Institute of Petroleum Explorati<strong>on</strong> and Producti<strong>on</strong>, Wuxi, China<br />

(corresp<strong>on</strong>ding author:nichunhua.syky@sinopec.com)<br />

Abundant of crude oil which suffers from different<br />

biodegradati<strong>on</strong> degrees occurs widely in the world. At<br />

present, the biodegradati<strong>on</strong> degrees of crude oil are<br />

mainly under qualitative identificati<strong>on</strong> based <strong>on</strong> some<br />

biomarkers detected in the crude oil which stand for<br />

different antibiodegradati<strong>on</strong> abilities.<br />

19 oil samples collected from the primary oil and gas<br />

structures of Bohai Bay Basin, North China have been<br />

investigated for their physical properties, molecular<br />

geochemistry and carb<strong>on</strong> stable isotope. According to<br />

the comparis<strong>on</strong> of geochemical parameters, 4 oil<br />

samples from the same oil and gas structure show the<br />

similar characteristics which prove they have the<br />

same genetic type, although there are some<br />

differences in their physical properties. The theory<br />

research indicates that there is a relative positive<br />

relati<strong>on</strong>ship between the abundance or c<strong>on</strong>centrati<strong>on</strong><br />

of 25-norhopnoids and the biodegradati<strong>on</strong> degree of<br />

crude oil. Therefore, the two ratios which are C29nor(25-norhopane)/C30-17<br />

α -hopane ratio and C28nor(25-norhopane)/C29-17<br />

α -norhopane ratio<br />

respectively are applied to semi-quantitatively<br />

evaluate the biodegradati<strong>on</strong> degree of the four crude<br />

oil. They distribute obviously in the different areas<br />

from the figure which reveals there are four<br />

biodegradati<strong>on</strong> degrees. The results of our study<br />

coincide well with the c<strong>on</strong>venti<strong>on</strong>al knowledge, the<br />

higher the biodegradati<strong>on</strong> degree of crude oil is, the<br />

heavier its density is, that is to say, the oil sample with<br />

the highest biodegradati<strong>on</strong> degree has the heaviest<br />

density. In additi<strong>on</strong>, the crude oil with lower burial<br />

depth is more likely to suffer from biodegradati<strong>on</strong>, so<br />

the No. 4 oil sample whose burial depth is <strong>on</strong>ly 1131.6<br />

meters encounters the highest biodegradati<strong>on</strong> degree<br />

am<strong>on</strong>g them.<br />

In c<strong>on</strong>trast with foreign petroliferous basins, Chinese<br />

basins are famous for their more complex evoluti<strong>on</strong><br />

history of tect<strong>on</strong>ic movements and most of them have<br />

two or more phases of hydrocarb<strong>on</strong> generati<strong>on</strong>,<br />

migrati<strong>on</strong> and accumulati<strong>on</strong>.<br />

Geochemical characteristics of the crude oil from Well<br />

B1 with underproductive oil flows in Southern North<br />

China Basin are studied and they show the crude oil<br />

is characterized by higher abundance of C16<br />

homodrimane, C23 tricyclic terpanes, pentacyclic<br />

terpanes, C31 homohopane and C27 sterane. Oilsource<br />

correlati<strong>on</strong> shows it is from the source rock of<br />

the Lower Cretaceous, which bel<strong>on</strong>gs to an<br />

indigenously generating and accumulating oil<br />

reservoir. According to the biodegradati<strong>on</strong> sequences<br />

of different biomarkers, normal alkanes are prior to be<br />

destroyed by the bacteria and 25-norhopanoids series<br />

usually appear when the crude oil undergoes severe<br />

biodegradati<strong>on</strong>. Interestingly, normal alkanes and 25norhopanoids<br />

series coexist in the oil sample from<br />

Well B1. How to explain this strange phenomen<strong>on</strong>?<br />

With the rapid development of numerical simulati<strong>on</strong><br />

technology, more and more professi<strong>on</strong>al software are<br />

used to complete the inversi<strong>on</strong> of the evoluti<strong>on</strong> history<br />

of the petroliferous basins, including thermal history,<br />

hydrocarb<strong>on</strong> generating history and hydrocarb<strong>on</strong><br />

charging history. Corresp<strong>on</strong>dence with the analysis of<br />

burial-thermal evoluti<strong>on</strong> history, there were at least<br />

two phrases of hydrocarb<strong>on</strong> charging of the crude oil<br />

from Lower Cretaceous of Well B1, the first charging<br />

phrase was the Early Cretaceous when it was<br />

dominated by low-matured oil with 0.50% Ro and<br />

suffered from biodegradati<strong>on</strong>, the sec<strong>on</strong>d charging<br />

phrase was from late Tertiary to Quaternary<br />

predominant with high-matured oil with 0.70-1.30%<br />

Ro. So the crude oil from Well B1 in Southern North<br />

China Basin is the mixture of the two-phase charging.<br />

It has been noticed that different biomarkers have<br />

their specific prerequisite and they should be<br />

comprehensively analyzed in combinati<strong>on</strong> with other<br />

research methods to promote their effectiveness. 25norhopanoids<br />

compounds is no excepti<strong>on</strong>.<br />

218

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