Lecture 10 Flashcards
1
Q
Ilmenite reduction with H2
A
- product: Oxygen
- feedstock: Ilmenite (FeTiO3) from high-Ti mare basalts
- Reduction (step 1, at 700-1000°C) -> FeTiO3 + H2 -> Fe + TiO2 + H2O
- Electrolysis (step 2) -> H2O -> H2 + 1/2 O2
- mildly endothermic
- mole fraction of water needs to remain < 10% to maintain the reaction
- shrinking core type process
2
Q
Ilmenite reduction with H2 - Pro/Con
A
- Pro
- single reaction step already yields water
- Mild reaction T
- Ilmenite is an abundant resource in Mare regions
- Con
- Beneficiation of ilmenite is recommended & greatly affects process efficiency
- only low oxygen yield is possible (5wt%)
3
Q
Shrinking core type process
A
- Diffusion of the reactant through product TiO2 layer
- Reaction with the ilmenite core -> core shrinks
- Diffusion of iron out of the TiO2 pores (more porous material after reaction)
- Formation of metallic iron outside the ilmenite grains
4
Q
Glass reduction with H2
A
- product: O2
- Feedstock: Glass (w. up to 20wt% FeO)
- from mare basalts, either produced by impacts or volcanic activity
- faster reaction kinetics compared to silicates
- Reduction: FeO + H2 -> Fe + H20
- Electrolysis: H2O -> H2 + 1/2 O2
- Glass found in agglutinates abundant but mixed with silicates -> beneficiation required
- Glass found in pyroclastic deposits is comparably pure, but not as abundant
5
Q
Glass reduction with H2 - Pro/Con
A
- Pro
- Single reaction step already yields water
- Mild reaction temperatures
- Glass is an abundant resource across the lunar surface
- Con
- Beneficiation of glass is required of not taken from a pyroclastic deposit
- Process has not yet been demonstrated on a plant scale
6
Q
Ilmenite reduction with CO
A
- product: oxygen
- feedstock: Ilmenite from high-Ti mare basalts
- Step: Reduction: FeTiO3 + CO -> Fe + TiO2 + CO2
- Step: CO2 cracking: CO2 -> Co + 1/2 O2
- similar to reduction with H2 but slower (higher activation energy)
- follows the shrinking core model
- CO2 cracking is highly endothermic
7
Q
Ilmenite reduction with CO - Pro/Con
A
- Pro
- Mild reaction T
- Ilmenite is an abundant resource in Mare regions
- Con
- Beneficiation of ilmenite is recommended & greatly affects process efficiency
- Cracking of CO2 requires much energy
- Reduction rate is slower c compared to using hydrogen
8
Q
Ilmenite Reduction with CH4
A
- product: O2
- feedstock: Ilmenite from high-Ti mare basalts
- Step 1: Reduction: FeTiO3 + CH4 -> Fe + TiO2 + CO + H2
- Step 2: Hydrogenation: CO + 3 H2 -> CH4 + H2O
- Step 3: Electrolysis: H2O -> H2 + 1/2 O2
- similar process as for reduction with hydrogen
- reaction T starts around 1000°C & involves decomposition of CH4 into C & H2
- SW implanted H2/C could be used to replenish
9
Q
Ilmenite reduction with CH4 - Pro/Con
A
- Pro
- Medium reaction T
- Ilmenite is an abundant resource in Mare
- Con
- Beneficiation of ilmenite is recommended & greatly affects process efficiency
- Hydrogenation as additional process step
- Additional reactant needed (H2)
10
Q
Carbothermal reduction
A
- product: oxygen
- feedstock: any kind of silicate or oxide minerals
- Step 1:
- Reduction (v1): Mg2SiO4 + 2CH4 -> 2MgO + Si + 4H2 + 2CO
- Reduction (v2): FeTiO3 + C -> Fe + TiO2 + CO
- Step 2: Hydrogenation: CO + 3H2 -> CH4 + H2O
- Step 3: Electrolysis: H2O -> H2 + 1/2 O2
- Carbothermal includes all processes involving molten reactant & carbon in some form
- as CH4 decomposes prior to reacting C/CO/CO2 can be used
- melt required for highest efficiency
- No beneficiation
- process was demonstrated with simulants
11
Q
Carbothermal reaction - Pro/Con
A
- Pro
- Higher oxygen yield possible ( ~10wt%)
- No beneficiation required & applicable to various minerals
- Con
- High reaction T
- Added system complexity & material handling challenges
- Considerable reactant makeup requires resupply or compensation from SWIP
12
Q
Extraction with Fluorine
A
- product: O2
- Feedstock: all minerals
- MxyOy + y F2 -> xy MF(2/x) + y/2 O2
- large variety of feedstock
- Fluorine is a strong oxidiser
- Silicates combine with fluorine to build fluorides, oxygen is liberated
- has been demonstrated in the 90s
13
Q
Extraction with Fluorine - Pro/Con
A
- Pro
- About 80% of the total oxygen can be released
- Moderate T required
- Con
- Experiments have only been done with small sample quantities
- Fluorine needs to be recycled to a high degree or imported
- Fluorine is toxic to humans
14
Q
Sabatier process
A
- product: oxygen
- Feedstock: CO2 in the atmosphere (96% on Mars)
- Step 1: Reaction: CO2 + H2 -> CH4 + 2 H2O
- Step 2: Electrolysis: H2O -> H2 + 1/2 O2
- T = 300-400°C; ~30 bar
- Nickel or ideally ruthenium acts as catalyst
- residual H2 is fed back into reaction
- process is used on the ISS to support recovery of oxygen
- CH4 & O2 can be used as fuel -> Methalox engine
15
Q
Sabatier process - Pro/Con
A
- Pro
- Well-known process, part of Life Support System (LSS) on the ISS
- Exothermic reaction, excess heat can be used to drive reactor
- Con
- H2 needs to be imported from Earth
- Excess heat might require radiators or heat sinks