Sedimentary 3 Carbonate minerals and rocks Flashcards

1
Q

What canCO2 be injected into to capture and store it?

A

Depleted oil and gas reservoirs, coal seams that cannot be mined, saline aquifers

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2
Q

Why is CO2 injected as a supercritical fluid?

A

It moves through pores better than a gas or a liquid

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3
Q

How is CO2 trapped? (three ways)

A

Structural trapping - held in rock pores
Solubility trapping - dissolved in saline water
Mineral trapping - precipitates as minerals, e.g. calcite

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4
Q

What is meant by mineral carbonation?

A

Fixing of CO2 in minerals such as calcite, magnesite, siderite and dolomite

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5
Q

What is in situ mineral carbonation?

A

The injection of CO2 rich solutions into rocks rich in divalent cations

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6
Q

What are the best rocks for in situ carbonation and why?

A

Peridotite and basalt

  1. Contain high concentrations of Mg, Ca and Fe
  2. Elements hosted in soluble material e.g. olivine, anorthite
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7
Q

What promotes precipitation of calcite and aragonite in a saturated solution?

A

Evaporation and degassing of CO2

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8
Q

Name four ways that CO2 can be lost

A

Photosynthesis
Temp increase (solubility of CO2 in seawater decreases as temp increases)
Turbulence
Movement of a volume of water from areas of high to low pCO2 (e.g. submarine caves)

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9
Q

What three varities of CaCO3 precipitate in sea water?

A

Low magnesium calcite,
High magnesium calcite (both low in strontium)
Aragonite (high in strontium)

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10
Q

Today most marine carbonates are formed organically, by weak and strong biogenic effects. What do these entail?

A

Weak biogenic effect = photosynthetic marine organisms (algae) induce biomineralisation by removal of CO2 from seawater
Strong biogenic effect = Metabolic activity of an organism to form skeletal carbonates (bivalves, gastropods)

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11
Q

Why are carbonates good palaeoclimate indicators?

A
  1. Aragonite and calcite form at or close to surface so similar to conditions in air.
  2. Carbonate minerals undergo little transportation so represent environment where they were formed
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12
Q

In what three ways has carbonate rock deposition changed in the last 600 million years?

A

Skeletal constituents are different
Volume of limestones formed
Original, mineralogy, chemical and isotopic composition have all changed.

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13
Q

What are marine algae shells composed of?

A

Aragonite

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14
Q

What do organisms with a strong control on mineralisation compose their shell of?

A

LMC e.g. brachiopods or LMC + aragonite e.g. bivalves

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15
Q

How did Sandberg (1983) first know that the mineralogy of the sea had changed over the last 600 million years?

A

Examined fabrics of ooids and early marine sediments and sometimes composed of LMC and sometimes of HMC/aragonite

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16
Q

Over what time periods did the aragonite and calcite seas occur?

A

Aragonite seas = Carboniferous to Triassic and Cenozoic

Calcite seas = Cambrian to Devonian and Jurassic to Cretaceous

17
Q

Explain what happens to aragonite if isolated in water?

A

Aragonite replaced by calcite during diagenesis. If isolated from water will last indefinitely.

18
Q

What forms from the recrystallisation of high magnesium calcite?

A

LMC, Dolomite and Celestite

19
Q

What affect to changes in sea composition have on the Sr/Ca ratios in the sea according to Steuber and Veizer (2002) ?

A

More Sr was removed during aragonite+HMC seas than the LMC

20
Q

What three theories have been proposed by Sandberg (1993), Morse et al. (1997) and HArdie (1997) to explain the change in inorganic composition and mineralogy?

A

Sandberg (1993) - Changes in atmospheric CO2, linked to tectonics resulted in ice house (low CO2) for aragonite seas and green house (high CO2) for calcite seas
Morse et al. (1997) - Ionic strength and temperature
Hardie (1997) - Seawater Ca2+ cncentrations and Mg/Ca

21
Q

Can temperature explain aragonite vs calcite seas?

A

With present day Mg/Ca, LMC precipitating shallow shelf seas will be cold. This disagrees with palaeoenvironmental evidence

22
Q

What controls seawater Mg + Ca concentrations?

A

Rivers (e.g. terrestrial chemical weathering)
Hydrothermal brines from Mid-ocean ridges
- Hydrothermal alteration of basalt takes in Mg2+ and releases Ca2+