Lec5&6 Flashcards

1
Q

Between the oil leg and water leg

A

Oil-water transition zone (OWTZ)

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2
Q

Below oil leg, 100% of pore space is saturated with water and various salts at low PH (3-7).
This is called?

A

Water leg

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3
Q

Oil saturated part of the reservoir.

A

Oil leg.

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4
Q

Time of reservoir charging depends on?

A
  1. Migration rate
  2. Generation of petroleum in the source rocks
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5
Q

Why there are non-biodegraded oil reservoirs?

A

Due to the killing of the degrading M.O
And the reservoir is pasteuized/sterilized because of the temperature is more than 80°C

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6
Q

Petroleum biodegradation in the reservoirs and refineries can be demonstrated by?

A
  1. Compositional modification of the petroleum components.
  2. Detection of microbial metabolic products in petroleum fluids
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7
Q

Quantity of acidic substance in 1 g of a sample of the oil.

A

Total acid number ( TAN value )

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8
Q

Reaction of methane formation:
H2 is ……. , CO2 is …….

A

H2 is electron donor (oxidized), CO2 is electron acceptor (reduced)

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9
Q

Is a unique biochemical process (mehanogenesis) that starts at beginning of life on earth by autotrophs

A

Biogenic methane formation

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10
Q

petroleum fluds are found in?

A

In permeable rocks, such as sandstone and limestone.

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11
Q

Factors affecting the biodegradation process
عددي

A
  1. Effect of temperature and pressure
  2. Effect of salinity
  3. Effect of oil migration
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12
Q

High salinities increase the level of biodegradation at
any reservoir temperature.
T/F

A

F , High salinities reduce

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13
Q

petroleum biodegradation in the reservoirs and refineries can be demonstrated by?

A
  1. compositional modification of the petroleum components.
  2. The detection of microbial metabolic products
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14
Q

quantity of acidic substances in 1g of a sample of the OIL

A

Total Acid Number (TAN)

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15
Q

methanogens characters

A
  • mesophilic or thermophilic.
  • Strict anaerobes found in diverse anaerobic habitats
  • great morphologic diversity
  • All methane-forming M.Os
  • Most are obligate or facultative autotrophs.
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16
Q

Methanospirillum
Methanomicrobium
Methanosarcina
Methanogenium
Methanococcus

A

genera of methanogens

17
Q

anaerobically oxidized by some microbes e.g SRB in the anoxic zone of the marine environments.

A

Anaerobic Methanotrophy

18
Q

used as the sole source of carbon and energy by a number of aerobic bacteria.

A

Aerobic Methanotrophy

19
Q

Is a unique biochemical process (methanogenesis) that starts at the beginning of life on Earth by autotrophs to obtain energy from simple organic gases CO2 and H2.

A

biogenic methane formation

20
Q

Why Methane cannot escape in the form of gaseous bubbles?

A

because it is accumulated in the sediments in the form of methane hydrates.

21
Q

General characters of methanogens:

A
  1. All methane-forming M.Os (methanogens) are members of the domain Archaea
  2. great morphologic diversity
  3. Strict anaerobes found in diverse anaerobic habitats
  4. May be mesophilic or thermophilic.
  5. Most are obligate or facultative autotrophs.