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Flashcards covering biogeochemical reactions, microbial processes, bioleaching, and mineral transformations from ERTH 3222 lecture notes.
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What is the name and ionic charge of Fe2+?
Ferrous ion, charge of +2.
What is the name and ionic charge of Fe3+?
Ferric ion, charge of +3.
What is the name and ionic charge of SO42−?
Sulfate ion, charge of −2.
What is the name and ionic charge of NO3−?
Nitrate ion, charge of −1.
What is the name and ionic charge of HCO3−?
Bicarbonate ion, charge of −1.
What is the name and ionic charge of UO22+?
Uranyl ion, charge of +2.
What is the name and ionic charge of TcO4−?
Pertechnetate ion, charge of −1.
What is the name and ionic charge of S2O32−?
Thiosulfate ion, charge of −2.
What are the chemical formulas and charges for native gold vs the ionic gold species in the document?
Native gold is Au0 (charge 0). Ionic gold species are aurous Au+ (charge +1) and auric Au3+ (charge +3).
Identify the reaction process: 6CO2+6H2O+photons→C6H12O6+6O2
Oxygenic Photosynthesis (standard reaction)
Identify the reaction process: 2NO3−+5H2→N2(g)+2OH−+4H2O
Denitrification
Identify the reaction process: UO22++H2→UO2(s)+2H+
Uranium Reduction
Identify the reaction process: TcO4−+121H2→TcO2(s)+OH−+H2O
Technetium Reduction
Identify the reaction process: H2S+2Au+→2H++Au0
Effect of SRB on Ionic Gold
Write the complete balanced equation for Oxygenic Photosynthesis (standard reaction).
6CO2+6H2O+photons→C6H12O6+6O2
Write the complete balanced equation for Oxygenic Photosynthesis (bicarbonate reaction).
6HCO3−+6H2O+photons→C6H12O6+6O2+6OH−
Write the complete balanced equation for Mineral Carbonation.
Ca2++HCO3−+OH−→CaCO3(s)+H2O
Write the complete balanced equation for Aerobic Heterotroph Respiration.
C6H12O6+6O2→6CO2+6H2O
Write the complete balanced equation for Methane Oxidation.
CH4+2O2→CO2+2H2O
Write the complete balanced equation for Decane Oxidation.
C10H22+1521O2→10CO2+11H2O
Write the complete balanced equation for Biological Iron Oxidation.
4Fe2++O2+4H+→4Fe3++2H2O
Write the complete balanced equation for Ferric Iron Hydrolysis.
Fe3++3H2O→Fe(OH)3(s)+3H+
Write the complete balanced equation for Sulfur Oxidation by Bacteria.
S0+121O2+H2O→SO42−+2H+
Write the complete balanced equation for Denitrification.
2NO3−+5H2→N2(g)+2OH−+4H2O
Write the complete balanced equation for Sulfate Reduction using Acetate (Desulforudis audaxviator).
CH3COOH+SO42−→H2S+2HCO3−
Write the complete balanced equation for Sulfate Reduction using Hydrogen (Desulforudis audaxviator).
4H2+SO42−→H2S+2OH−+2H2O
Write the complete balanced equation for Black Precipitate Reaction in a Winogradsky Column.
H2S+Fe2+→FeS(s)+2H+
Write the complete balanced equation for Uranium Reduction.
UO22++H2→UO2(s)+2H+
Write the complete balanced equation for Technetium Reduction.
TcO4−+121H2→TcO2(s)+OH−+H2O
Write the complete balanced equation for Hydrogenotrophic Methanogenesis.
4H2+CO2→CH4(g)+2H2O
Write the complete balanced equation for Acetoclastic Methanogenesis.
CH3COOH→CH4(g)+CO2(g)
Write the complete balanced equation for Serpentinised Olivine.
9Mg2(Ni)SiO4+3Fe2(Ni)SiO4+14H2O→6Mg3Si2O5(OH)4+2Fe3O4+2H2
Write the complete balanced equation for Manganese Oxidation.
Mn2++H2O+21O2→MnO2+2H+
Write the complete balanced equation for Complete Pyrite Oxidation by Ferric Iron.
FeS2+14Fe3++8H2O→15Fe2++2SO42−+16H+
Write the complete balanced equation for Partial Pyrite Oxidation by Ferric Iron (forming elemental sulfur).
FeS2+2Fe3+→3Fe(aq)2++2S0
Write the complete balanced equations for Supergene Enrichment of Copper via Disproportionation and Precipitation.
2S0+H2O→S2−+SO+2H+
Cu2++S2−→CuS(s)
Write the complete balanced equation for Chalcocite Leaching.
Cu2S(s)+8Fe3++4H2O→2Cu++8Fe2++SO42−+8H+
Write the complete balanced equation for Covellite Leaching.
CuS(s)+8Fe3++4H2O→Cu2++8Fe2++SO42−+8H+
Write the complete balanced equation for Chalcopyrite Leaching.
CuFeS2(s)+16Fe3++8H2O→Cu2++17Fe2++2SO42−+16H+
Write the complete balanced equation for Carbonate Buffering.
CaCO3(s)+2H+→Ca2++H2O+CO2(g)
Write the complete balanced equation for Slow Anaerobic Pyrite Formation.
FeS(s)+H2S→FeS2(s)+H2
Write the complete balanced equations for Fast Microaerophilic Pyrite Formation (Step 1 and Step 2).
Step 1: H2S+21O2→S0+H2O
Step 2: FeS(s)+S0→FeS2(s)
Write the complete balanced equations for the Biogeochemistry of Gold (Dissolution, Disproportionation, Chloride Complex, Thiosulfate Complex).
Dissolution: 2Au0+H2O2→2Au++2OH−
Disproportionation: 3Au+→2Au0+Au3+
Chloride Complex: Au3++4Cl−→AuCl4−
Thiosulfate Complex: Au++2S2O32−→Au(S2O3)23−
Write the complete balanced equations for the Effect of Sulfur (Thiosulfate) Oxidising Bacteria on Gold.
Thiosulfate Oxidation: S2O32−+2O2+H2O→2SO42−+2H+
Gold Complex Breakdown: Au(S2O3)23−+4O2+2H2O→Au++4SO42−+4H+
Write the complete balanced equations for the Effect of Ferric Iron (Iron Oxidising Bacteria) on Gold Thiosulfate.
Iron Oxidation of Thiosulfate: 8Fe3++S2O32−+5H2O→8Fe2++2SO42−+10H+
Iron Release of Gold: 16Fe3++Au(S2O3)23−+10H2O→16Fe2++Au++4SO42−+2OH+
Write the complete balanced equation for
What is the name and ionic charge of Fe2+?
Ferrous ion, charge of +2.
What is the name and ionic charge of Fe3+?
Ferric ion, charge of +3.
What is the name and ionic charge of SO42−?
Sulfate ion, charge of −2.
What is the name and ionic charge of NO3−?
Nitrate ion, charge of −1.
What is the name and ionic charge of HCO3−?
Bicarbonate ion, charge of −1.
What is the name and ionic charge of UO22+?
Uranyl ion, charge of +2.
What is the name and ionic charge of TcO4−?
Pertechnetate ion, charge of −1.
What is the name and ionic charge of S2O32−?
Thiosulfate ion, charge of −2.
What are the chemical formulas and charges for native gold vs the ionic gold species?
Native gold is Au0 (charge 0). Ionic gold species are aurous Au+ (charge +1) and auric Au3+ (charge +3).
What are six major biogeochemical forms/species of nitrogen?
Dinitrogen gas (N2)
Nitrate (NO3−)
Nitrite (NO2−)
Ammonium (NH4+)
Ammonia (NH3)
Nitrous oxide (N2O) or organic nitrogen (amino acids/proteins).
Why is water (H2O) essential for life and biogeochemical reactions?
Water acts as a universal polar solvent, a transport medium for ions, a reactant/electron donor in photosynthesis, a source of H+ and OH− for acid-base reactions, and a key agent in mineral hydrolysis and serpentinization.
What is the core pathway of the biogeochemical Carbon Cycle?
Carbon cycles between inorganic oxidized forms (CO2, HCO3−) and organic reduced forms (C6H12O6) or reduced gases (CH4) via photosynthesis, respiration, methanogenesis, methane oxidation, and mineral precipitation/dissolution (CaCO3).
What is the core pathway of the Methane Cycle?
Methane (CH4) is produced in anaerobic environments by methanogens (via hydrogenotrophic or acetoclastic pathways) and oxidized back to CO2 by aerobic or anaerobic methane-oxidizing bacteria.
What is the chemical theory behind Oxygenic Photosynthesis?
Autotrophic organisms use light energy (photons) to fix inorganic carbon (CO2 or HCO3−) into organic matter (C6H12O6), splitting water and releasing oxygen (O2) as a byproduct.
What is the chemical theory behind Mineral Carbonation?
In aqueous environments, calcium ions (Ca2+) react with bicarbonate (HCO3−) under alkaline conditions (OH−) to permanently sequester carbon into solid calcium carbonate (CaCO3).
What is the chemical theory behind Aerobic Respiration and Hydrocarbon Degradation?
Heterotrophic organisms and hydrocarbon-degrading bacteria oxidize organic molecules (C6H12O6) or hydrocarbons (CH4, C10H22) using oxygen (O2) as the terminal electron acceptor, producing CO2 and H2O.
What is the chemical theory behind Biological Iron Oxidation and Hydrolysis?
Iron-oxidizing bacteria oxidize soluble ferrous iron (Fe2+) to ferric iron (Fe3+) using oxygen. Ferric iron subsequently hydrolyzes in water to form insoluble ferric hydroxide (Fe(OH)3) precipitate and release protons (H+).
What is the chemical theory behind Bacterial Sulfur Oxidation?
Sulfur-oxidizing bacteria use oxygen to oxidize elemental sulfur (S0) to sulfate (SO42−), generating sulfuric acid (H+) which drives acid mine drainage and rock weathering.
What is the chemical theory behind Denitrification?
Anaerobic bacteria use nitrate (NO3−) as a terminal electron acceptor and hydrogen gas (H2) as an electron donor, reducing nitrate to inert dinitrogen gas (N2(g)) and generating alkalinity (OH−).
What is the chemical theory behind Sulfate Reduction by Desulforudis audaxviator?
Obligate anaerobes reduce sulfate (SO42−) using electron donors like acetate (CH3COOH) or molecular hydrogen (H2) to generate hydrogen sulfide (H2S).
What is the chemical theory behind Anaerobic Metal Reduction (Uranium and Technetium)?
Anaerobic bacteria reduce soluble, toxic radionuclides—uranyl (UO22+) and pertechnetate (TcO4−)—using H2 to convert them into insoluble oxide precipitates (UO2(s), TcO2(s)).
What is the chemical theory behind Methanogenesis?
Strict anaerobic archaea reduce CO2 using H2 (hydrogenotrophic) or split acetate (CH3COOH) (acetoclastic) to generate methane (CH4(g)) in oxygen-depleted subsurface environment.
What is the chemical theory behind Olivine Serpentinization?
Anorganic hydrothermal reaction where water oxidizes ferrous iron in olivine minerals (Mg2SiO4, Fe2SiO4), forming serpentine minerals, magnetite (Fe3O4), and abiotic hydrogen gas (H2).
What is the chemical theory behind Manganese Oxidation?
Dissolved manganese (Mn2+) is oxidized by oxygen in the presence of water to precipitate solid manganese dioxide (MnO2) and release protons.
What is the chemical theory behind Pyrite Oxidation by Ferric Iron?
Ferric iron (Fe3+) acts as a powerful oxidant that attacks pyrite (FeS2). Complete oxidation yields sulfate (SO42−) and acidity, whereas partial oxidation generates elemental sulfur (S0).
What is the chemical theory behind Pyrite Formation pathways?
Iron monosulfide (FeS) transforms into pyrite (FeS2) slowly under anaerobic conditions via reaction with H2S, or rapidly under microaerophilic conditions where trace oxygen generates elemental sulfur (S0) to react with FeS.
What is the chemical theory behind Supergene Copper Enrichment and Leaching?
Supergene processes involve elemental sulfur disproportionation to produce sulfide (S2−) that precipitates copper as covellite (CuS). Acidic ferric iron leaches copper sulfide minerals (chalcocite, covellite, chalcopyrite) to release soluble copper ions.
What is the chemical theory behind Carbonate Buffering?
Calcium carbonate (CaCO3) reacts with excess acidity (H+) to produce dissolved Ca2+, water, and carbon dioxide gas (CO2), regulating pH in natural waters.
What is the chemical theory behind Gold Biogeochemistry?
Gold (Au0) is solubilized by oxidative peroxide or complexes with chloride (Cl−) and thiosulfate (S2O32−). Bacteria or ferric/sulfur oxidizers break down these complexes, while sulfate-reducing bacteria (H2S) reduce ionic gold back to native gold (Au0) precipitates.
Write the complete balanced equation for Oxygenic Photosynthesis (standard reaction).
6CO2+6H2O+photons→C6H12O6+6O2
Write the complete balanced equation for Oxygenic Photosynthesis (bicarbonate reaction).
6HCO3−+6H2O+photons→C6H12O6+6O2+6OH−
Write the complete balanced equation for Mineral Carbonation.
Ca2++HCO3−+OH−→CaCO3(s)+H2O
Write the complete balanced equation for Aerobic Heterotroph Respiration.
C6H12O6+6O2→6CO2+6H2O
Write the complete balanced equation for Methane Oxidation.
CH4+2O2→CO2+2H2O
Write the complete balanced equation for Decane Oxidation.
C10H22+1521O2→10CO2+11H2O
Write the complete balanced equation for Biological Iron Oxidation.
4Fe2++O2+4H+→4Fe3++2H2O
Write the complete balanced equation for Ferric Iron Hydrolysis.
Fe3++3H2O→Fe(OH)3(s)+3H+
Write the complete balanced equation for Sulfur Oxidation by Bacteria.
S0+121O2+H2O→SO42−+2H+
Write the complete balanced equation for Denitrification.
2NO3−+5H2→N2(g)+2OH−+4H2O
Write the complete balanced equation for Sulfate Reduction using Acetate (Desulforudis audaxviator).
CH3COOH+SO42−→H2S+2HCO3−
Write the complete balanced equation for Sulfate Reduction using Hydrogen (Desulforudis audaxviator).
4H2+SO42−→H2S+2OH−+2H2O
Write the complete balanced equation for Black Precipitate Reaction in a Winogradsky Column.
H2S+Fe2+→FeS(s)+2H+
Write the complete balanced equation for Uranium Reduction.
UO22++H2→UO2(s)+2H+
Write the complete balanced equation for Technetium Reduction.
TcO4−+121H2→TcO2(s)+OH−+H2O
Write the complete balanced equation for Hydrogenotrophic Methanogenesis.
4H2+CO2→CH4(g)+2H2O
Write the complete balanced equation for Acetoclastic Methanogenesis.
CH3COOH→CH4(g)+CO2(g)
Write the complete balanced equation for Serpentinised Olivine.
9Mg2(Ni)SiO4+3Fe2(Ni)SiO4+14H2O→6Mg3Si2O5(OH)4+2Fe3O4+2H2
Write the complete balanced equation for Manganese Oxidation.
Mn2++H2O+21O2→MnO2+2H+
Write the complete balanced equation for Complete Pyrite Oxidation by Ferric Iron.
FeS2+14Fe3++8H2O→15Fe2++2SO42−+16H+
Write the complete balanced equation for Partial Pyrite Oxidation by Ferric Iron (forming elemental sulfur).
FeS2+2Fe3+→3Fe(aq)2++2S0
Write the complete balanced equations for Supergene Enrichment of Copper via Disproportionation and Precipitation.
2S0+H2O→S2−+SO+2H+
Cu2++S2−→CuS(s)
Write the complete balanced equation for Chalcocite Leaching.
Cu2S(s)+8Fe3++4H2O→2Cu++8Fe2++SO42−+8H+
Write the complete balanced equation for Covellite Leaching.
CuS(s)+8Fe3++4H2O→Cu2++8Fe2++SO42−+8H+
Write the complete balanced equation for Chalcopyrite Leaching.
CuFeS2(s)+16Fe3++8H2O→Cu2++17Fe2++2SO42−+16H+