ERTH 3222 Bio-Geo-Chemical Reactions Flashcards

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Flashcards covering biogeochemical reactions, microbial processes, bioleaching, and mineral transformations from ERTH 3222 lecture notes.

Last updated 6:23 AM on 10/5/26
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107 Terms

1
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What is the name and ionic charge of Fe2+Fe^{2+}?

Ferrous ion, charge of +2+2.

2
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What is the name and ionic charge of Fe3+Fe^{3+}?

Ferric ion, charge of +3+3.

3
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What is the name and ionic charge of SO42−SO_4^{2-}?

Sulfate ion, charge of −2-2.

4
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What is the name and ionic charge of NO3−NO_3^-?

Nitrate ion, charge of −1-1.

5
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What is the name and ionic charge of HCO3−HCO_3^-?

Bicarbonate ion, charge of −1-1.

6
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What is the name and ionic charge of UO22+UO_2^{2+}?

Uranyl ion, charge of +2+2.

7
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What is the name and ionic charge of TcO4−TcO_4^-?

Pertechnetate ion, charge of −1-1.

8
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What is the name and ionic charge of S2O32−S_2O_3^{2-}?

Thiosulfate ion, charge of −2-2.

9
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What are the chemical formulas and charges for native gold vs the ionic gold species in the document?

Native gold is Au0Au^0 (charge 00). Ionic gold species are aurous Au+Au^+ (charge +1+1) and auric Au3+Au^{3+} (charge +3+3).

10
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Identify the reaction process: 6CO2+6H2O+photons→C6H12O6+6O26CO_2 + 6H_2O + \text{photons} \rightarrow C_6H_{12}O_6 + 6O_2

Oxygenic Photosynthesis (standard reaction)

11
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Identify the reaction process: 2NO3−+5H2→N2(g)+2OH−+4H2O2NO_3^- + 5H_2 \rightarrow N_{2(g)} + 2OH^- + 4H_2O

Denitrification

12
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Identify the reaction process: UO22++H2→UO2(s)+2H+UO_2^{2+} + H_2 \rightarrow UO_{2(s)} + 2H^+

Uranium Reduction

13
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Identify the reaction process: TcO4−+112H2→TcO2(s)+OH−+H2OTcO_4^- + 1\frac{1}{2}H_2 \rightarrow TcO_{2(s)} + OH^- + H_2O

Technetium Reduction

14
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Identify the reaction process: H2S+2Au+→2H++Au0H_2S + 2Au^+ \rightarrow 2H^+ + Au^0

Effect of SRB on Ionic Gold

15
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Write the complete balanced equation for Oxygenic Photosynthesis (standard reaction).

6CO2+6H2O+photons→C6H12O6+6O26CO_2 + 6H_2O + \text{photons} \rightarrow C_6H_{12}O_6 + 6O_2

16
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Write the complete balanced equation for Oxygenic Photosynthesis (bicarbonate reaction).

6HCO3−+6H2O+photons→C6H12O6+6O2+6OH−6HCO_3^- + 6H_2O + \text{photons} \rightarrow C_6H_{12}O_6 + 6O_2 + 6OH^-

17
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Write the complete balanced equation for Mineral Carbonation.

Ca2++HCO3−+OH−→CaCO3(s)+H2OCa^{2+} + HCO_3^- + OH^- \rightarrow CaCO_{3(s)} + H_2O

18
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Write the complete balanced equation for Aerobic Heterotroph Respiration.

C6H12O6+6O2→6CO2+6H2OC_6H_{12}O_6 + 6O_2 \rightarrow 6CO_2 + 6H_2O

19
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Write the complete balanced equation for Methane Oxidation.

CH4+2O2→CO2+2H2OCH_4 + 2O_2 \rightarrow CO_2 + 2H_2O

20
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Write the complete balanced equation for Decane Oxidation.

C10H22+1512O2→10CO2+11H2OC_{10}H_{22} + 15\frac{1}{2}O_2 \rightarrow 10CO_2 + 11H_2O

21
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Write the complete balanced equation for Biological Iron Oxidation.

4Fe2++O2+4H+→4Fe3++2H2O4Fe^{2+} + O_2 + 4H^+ \rightarrow 4Fe^{3+} + 2H_2O

22
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Write the complete balanced equation for Ferric Iron Hydrolysis.

Fe3++3H2O→Fe(OH)3(s)+3H+Fe^{3+} + 3H_2O \rightarrow Fe(OH)_{3(s)} + 3H^+

23
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Write the complete balanced equation for Sulfur Oxidation by Bacteria.

S0+112O2+H2O→SO42−+2H+S^0 + 1\frac{1}{2}O_2 + H_2O \rightarrow SO_4^{2-} + 2H^+

24
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Write the complete balanced equation for Denitrification.

2NO3−+5H2→N2(g)+2OH−+4H2O2NO_3^- + 5H_2 \rightarrow N_{2(g)} + 2OH^- + 4H_2O

25
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Write the complete balanced equation for Sulfate Reduction using Acetate (Desulforudis audaxviator).

CH3COOH+SO42−→H2S+2HCO3−CH_3COOH + SO_4^{2-} \rightarrow H_2S + 2HCO_3^-

26
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Write the complete balanced equation for Sulfate Reduction using Hydrogen (Desulforudis audaxviator).

4H2+SO42−→H2S+2OH−+2H2O4H_2 + SO_4^{2-} \rightarrow H_2S + 2OH^- + 2H_2O

27
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Write the complete balanced equation for Black Precipitate Reaction in a Winogradsky Column.

H2S+Fe2+→FeS(s)+2H+H_2S + Fe^{2+} \rightarrow FeS_{(s)} + 2H^+

28
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Write the complete balanced equation for Uranium Reduction.

UO22++H2→UO2(s)+2H+UO_2^{2+} + H_2 \rightarrow UO_{2(s)} + 2H^+

29
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Write the complete balanced equation for Technetium Reduction.

TcO4−+112H2→TcO2(s)+OH−+H2OTcO_4^- + 1\frac{1}{2}H_2 \rightarrow TcO_{2(s)} + OH^- + H_2O

30
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Write the complete balanced equation for Hydrogenotrophic Methanogenesis.

4H2+CO2→CH4(g)+2H2O4H_2 + CO_2 \rightarrow CH_{4(g)} + 2H_2O

31
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Write the complete balanced equation for Acetoclastic Methanogenesis.

CH3COOH→CH4(g)+CO2(g)CH_3COOH \rightarrow CH_{4(g)} + CO_{2(g)}

32
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Write the complete balanced equation for Serpentinised Olivine.

9Mg2(Ni)SiO4+3Fe2(Ni)SiO4+14H2O→6Mg3Si2O5(OH)4+2Fe3O4+2H29Mg_2(\text{Ni})SiO_4 + 3Fe_2(\text{Ni})SiO_4 + 14H_2O \rightarrow 6Mg_3Si_2O_5(OH)_4 + 2Fe_3O_4 + 2H_2

33
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Write the complete balanced equation for Manganese Oxidation.

Mn2++H2O+12O2→MnO2+2H+Mn^{2+} + H_2O + \frac{1}{2}O_2 \rightarrow MnO_2 + 2H^+

34
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Write the complete balanced equation for Complete Pyrite Oxidation by Ferric Iron.

FeS2+14Fe3++8H2O→15Fe2++2SO42−+16H+FeS_2 + 14Fe^{3+} + 8H_2O \rightarrow 15Fe^{2+} + 2SO_4^{2-} + 16H^+

35
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Write the complete balanced equation for Partial Pyrite Oxidation by Ferric Iron (forming elemental sulfur).

FeS2+2Fe3+→3Fe(aq)2++2S0FeS_2 + 2Fe^{3+} \rightarrow 3Fe^{2+}_{(aq)} + 2S^0

36
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Write the complete balanced equations for Supergene Enrichment of Copper via Disproportionation and Precipitation.

2S0+H2O→S2−+SO+2H+2S^0 + H_2O \rightarrow S^{2-} + SO + 2H^+

Cu2++S2−→CuS(s)Cu^{2+} + S^{2-} \rightarrow CuS_{(s)}

37
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Write the complete balanced equation for Chalcocite Leaching.

Cu2S(s)+8Fe3++4H2O→2Cu++8Fe2++SO42−+8H+Cu_2S_{(s)} + 8Fe^{3+} + 4H_2O \rightarrow 2Cu^+ + 8Fe^{2+} + SO_4^{2-} + 8H^+

38
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Write the complete balanced equation for Covellite Leaching.

CuS(s)+8Fe3++4H2O→Cu2++8Fe2++SO42−+8H+CuS_{(s)} + 8Fe^{3+} + 4H_2O \rightarrow Cu^{2+} + 8Fe^{2+} + SO_4^{2-} + 8H^+

39
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Write the complete balanced equation for Chalcopyrite Leaching.

CuFeS2(s)+16Fe3++8H2O→Cu2++17Fe2++2SO42−+16H+CuFeS_{2(s)} + 16Fe^{3+} + 8H_2O \rightarrow Cu^{2+} + 17Fe^{2+} + 2SO_4^{2-} + 16H^+

40
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Write the complete balanced equation for Carbonate Buffering.

CaCO3(s)+2H+→Ca2++H2O+CO2(g)CaCO_{3(s)} + 2H^+ \rightarrow Ca^{2+} + H_2O + CO_{2(g)}

41
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Write the complete balanced equation for Slow Anaerobic Pyrite Formation.

FeS(s)+H2S→FeS2(s)+H2FeS_{(s)} + H_2S \rightarrow FeS_{2(s)} + H_2

42
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Write the complete balanced equations for Fast Microaerophilic Pyrite Formation (Step 1 and Step 2).

Step 1: H2S+12O2→S0+H2OH_2S + \frac{1}{2}O_2 \rightarrow S^0 + H_2O

Step 2: FeS(s)+S0→FeS2(s)FeS_{(s)} + S^0 \rightarrow FeS_{2(s)}

43
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Write the complete balanced equations for the Biogeochemistry of Gold (Dissolution, Disproportionation, Chloride Complex, Thiosulfate Complex).

Dissolution: 2Au0+H2O2→2Au++2OH−2Au^0 + H_2O_2 \rightarrow 2Au^+ + 2OH^-

Disproportionation: 3Au+→2Au0+Au3+3Au^+ \rightarrow 2Au^0 + Au^{3+}

Chloride Complex: Au3++4Cl−→AuCl4−Au^{3+} + 4Cl^- \rightarrow AuCl_4^-

Thiosulfate Complex: Au++2S2O32−→Au(S2O3)23−Au^+ + 2S_2O_3^{2-} \rightarrow Au(S_2O_3)_2^{3-}

44
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Write the complete balanced equations for the Effect of Sulfur (Thiosulfate) Oxidising Bacteria on Gold.

Thiosulfate Oxidation: S2O32−+2O2+H2O→2SO42−+2H+S_2O_3^{2-} + 2O_2 + H_2O \rightarrow 2SO_4^{2-} + 2H^+

Gold Complex Breakdown: Au(S2O3)23−+4O2+2H2O→Au++4SO42−+4H+Au(S_2O_3)_2^{3-} + 4O_2 + 2H_2O \rightarrow Au^+ + 4SO_4^{2-} + 4H^+

45
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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+8Fe^{3+} + S_2O_3^{2-} + 5H_2O \rightarrow 8Fe^{2+} + 2SO_4^{2-} + 10H^+

Iron Release of Gold: 16Fe3++Au(S2O3)23−+10H2O→16Fe2++Au++4SO42−+2OH+16Fe^{3+} + Au(S_2O_3)_2^{3-} + 10H_2O \rightarrow 16Fe^{2+} + Au^+ + 4SO_4^{2-} + 2OH^+

46
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Write the complete balanced equation for

47
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What is the name and ionic charge of Fe2+Fe^{2+}?

Ferrous ion, charge of +2+2.

48
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What is the name and ionic charge of Fe3+Fe^{3+}?

Ferric ion, charge of +3+3.

49
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What is the name and ionic charge of SO42−SO_4^{2-}?

Sulfate ion, charge of −2-2.

50
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What is the name and ionic charge of NO3−NO_3^-?

Nitrate ion, charge of −1-1.

51
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What is the name and ionic charge of HCO3−HCO_3^-?

Bicarbonate ion, charge of −1-1.

52
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What is the name and ionic charge of UO22+UO_2^{2+}?

Uranyl ion, charge of +2+2.

53
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What is the name and ionic charge of TcO4−TcO_4^-?

Pertechnetate ion, charge of −1-1.

54
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What is the name and ionic charge of S2O32−S_2O_3^{2-}?

Thiosulfate ion, charge of −2-2.

55
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What are the chemical formulas and charges for native gold vs the ionic gold species?

Native gold is Au0Au^0 (charge 00). Ionic gold species are aurous Au+Au^+ (charge +1+1) and auric Au3+Au^{3+} (charge +3+3).

56
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What are six major biogeochemical forms/species of nitrogen?

  1. Dinitrogen gas (N2N_2)

  2. Nitrate (NO3−NO_3^-)

  3. Nitrite (NO2−NO_2^-)

  4. Ammonium (NH4+NH_4^+)

  5. Ammonia (NH3NH_3)

  6. Nitrous oxide (N2ON_2O) or organic nitrogen (amino acids/proteins).


57
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Why is water (H2OH_2O) 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+H^+ and OH−OH^- for acid-base reactions, and a key agent in mineral hydrolysis and serpentinization.

58
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What is the core pathway of the biogeochemical Carbon Cycle?

Carbon cycles between inorganic oxidized forms (CO2CO_2, HCO3−HCO_3^-) and organic reduced forms (C6H12O6C_6H_{12}O_6) or reduced gases (CH4CH_4) via photosynthesis, respiration, methanogenesis, methane oxidation, and mineral precipitation/dissolution (CaCO3CaCO_3).

59
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What is the core pathway of the Methane Cycle?

Methane (CH4CH_4) is produced in anaerobic environments by methanogens (via hydrogenotrophic or acetoclastic pathways) and oxidized back to CO2CO_2 by aerobic or anaerobic methane-oxidizing bacteria.

60
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What is the chemical theory behind Oxygenic Photosynthesis?

Autotrophic organisms use light energy (photons) to fix inorganic carbon (CO2CO_2 or HCO3−HCO_3^-) into organic matter (C6H12O6C_6H_{12}O_6), splitting water and releasing oxygen (O2O_2) as a byproduct.

61
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What is the chemical theory behind Mineral Carbonation?

In aqueous environments, calcium ions (Ca2+Ca^{2+}) react with bicarbonate (HCO3−HCO_3^-) under alkaline conditions (OH−OH^-) to permanently sequester carbon into solid calcium carbonate (CaCO3CaCO_3).

62
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What is the chemical theory behind Aerobic Respiration and Hydrocarbon Degradation?

Heterotrophic organisms and hydrocarbon-degrading bacteria oxidize organic molecules (C6H12O6C_6H_{12}O_6) or hydrocarbons (CH4CH_4, C10H22C_{10}H_{22}) using oxygen (O2O_2) as the terminal electron acceptor, producing CO2CO_2 and H2OH_2O.

63
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What is the chemical theory behind Biological Iron Oxidation and Hydrolysis?

Iron-oxidizing bacteria oxidize soluble ferrous iron (Fe2+Fe^{2+}) to ferric iron (Fe3+Fe^{3+}) using oxygen. Ferric iron subsequently hydrolyzes in water to form insoluble ferric hydroxide (Fe(OH)3Fe(OH)_3) precipitate and release protons (H+H^+).

64
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What is the chemical theory behind Bacterial Sulfur Oxidation?

Sulfur-oxidizing bacteria use oxygen to oxidize elemental sulfur (S0S^0) to sulfate (SO42−SO_4^{2-}), generating sulfuric acid (H+H^+) which drives acid mine drainage and rock weathering.

65
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What is the chemical theory behind Denitrification?

Anaerobic bacteria use nitrate (NO3−NO_3^-) as a terminal electron acceptor and hydrogen gas (H2H_2) as an electron donor, reducing nitrate to inert dinitrogen gas (N2(g)N_{2(g)}) and generating alkalinity (OH−OH^-).

66
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What is the chemical theory behind Sulfate Reduction by Desulforudis audaxviator?

Obligate anaerobes reduce sulfate (SO42−SO_4^{2-}) using electron donors like acetate (CH3COOHCH_3COOH) or molecular hydrogen (H2H_2) to generate hydrogen sulfide (H2SH_2S).

67
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What is the chemical theory behind Anaerobic Metal Reduction (Uranium and Technetium)?

Anaerobic bacteria reduce soluble, toxic radionuclides—uranyl (UO22+UO_2^{2+}) and pertechnetate (TcO4−TcO_4^-)—using H2H_2 to convert them into insoluble oxide precipitates (UO2(s)UO_{2(s)}, TcO2(s)TcO_{2(s)}).

68
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What is the chemical theory behind Methanogenesis?

Strict anaerobic archaea reduce CO2CO_2 using H2H_2 (hydrogenotrophic) or split acetate (CH3COOHCH_3COOH) (acetoclastic) to generate methane (CH4(g)CH_{4(g)}) in oxygen-depleted subsurface environment.

69
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What is the chemical theory behind Olivine Serpentinization?

Anorganic hydrothermal reaction where water oxidizes ferrous iron in olivine minerals (Mg2SiO4Mg_2SiO_4, Fe2SiO4Fe_2SiO_4), forming serpentine minerals, magnetite (Fe3O4Fe_3O_4), and abiotic hydrogen gas (H2H_2).

70
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What is the chemical theory behind Manganese Oxidation?

Dissolved manganese (Mn2+Mn^{2+}) is oxidized by oxygen in the presence of water to precipitate solid manganese dioxide (MnO2MnO_2) and release protons.

71
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What is the chemical theory behind Pyrite Oxidation by Ferric Iron?

Ferric iron (Fe3+Fe^{3+}) acts as a powerful oxidant that attacks pyrite (FeS2FeS_2). Complete oxidation yields sulfate (SO42−SO_4^{2-}) and acidity, whereas partial oxidation generates elemental sulfur (S0S^0).

72
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What is the chemical theory behind Pyrite Formation pathways?

Iron monosulfide (FeSFeS) transforms into pyrite (FeS2FeS_2) slowly under anaerobic conditions via reaction with H2SH_2S, or rapidly under microaerophilic conditions where trace oxygen generates elemental sulfur (S0S^0) to react with FeSFeS.

73
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What is the chemical theory behind Supergene Copper Enrichment and Leaching?

Supergene processes involve elemental sulfur disproportionation to produce sulfide (S2−S^{2-}) that precipitates copper as covellite (CuSCuS). Acidic ferric iron leaches copper sulfide minerals (chalcocite, covellite, chalcopyrite) to release soluble copper ions.

74
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What is the chemical theory behind Carbonate Buffering?

Calcium carbonate (CaCO3CaCO_3) reacts with excess acidity (H+H^+) to produce dissolved Ca2+Ca^{2+}, water, and carbon dioxide gas (CO2CO_2), regulating pH in natural waters.

75
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What is the chemical theory behind Gold Biogeochemistry?

Gold (Au0Au^0) is solubilized by oxidative peroxide or complexes with chloride (Cl−Cl^-) and thiosulfate (S2O32−S_2O_3^{2-}). Bacteria or ferric/sulfur oxidizers break down these complexes, while sulfate-reducing bacteria (H2SH_2S) reduce ionic gold back to native gold (Au0Au^0) precipitates.

76
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Write the complete balanced equation for Oxygenic Photosynthesis (standard reaction).

6CO2+6H2O+photons→C6H12O6+6O26CO_2 + 6H_2O + \text{photons} \rightarrow C_6H_{12}O_6 + 6O_2

77
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Write the complete balanced equation for Oxygenic Photosynthesis (bicarbonate reaction).

6HCO3−+6H2O+photons→C6H12O6+6O2+6OH−6HCO_3^- + 6H_2O + \text{photons} \rightarrow C_6H_{12}O_6 + 6O_2 + 6OH^-

78
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Write the complete balanced equation for Mineral Carbonation.

Ca2++HCO3−+OH−→CaCO3(s)+H2OCa^{2+} + HCO_3^- + OH^- \rightarrow CaCO_{3(s)} + H_2O

79
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Write the complete balanced equation for Aerobic Heterotroph Respiration.

C6H12O6+6O2→6CO2+6H2OC_6H_{12}O_6 + 6O_2 \rightarrow 6CO_2 + 6H_2O

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Write the complete balanced equation for Methane Oxidation.

CH4+2O2→CO2+2H2OCH_4 + 2O_2 \rightarrow CO_2 + 2H_2O

81
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Write the complete balanced equation for Decane Oxidation.

C10H22+1512O2→10CO2+11H2OC_{10}H_{22} + 15\frac{1}{2}O_2 \rightarrow 10CO_2 + 11H_2O

82
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Write the complete balanced equation for Biological Iron Oxidation.

4Fe2++O2+4H+→4Fe3++2H2O4Fe^{2+} + O_2 + 4H^+ \rightarrow 4Fe^{3+} + 2H_2O

83
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Write the complete balanced equation for Ferric Iron Hydrolysis.

Fe3++3H2O→Fe(OH)3(s)+3H+Fe^{3+} + 3H_2O \rightarrow Fe(OH)_{3(s)} + 3H^+

84
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Write the complete balanced equation for Sulfur Oxidation by Bacteria.

S0+112O2+H2O→SO42−+2H+S^0 + 1\frac{1}{2}O_2 + H_2O \rightarrow SO_4^{2-} + 2H^+

85
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Write the complete balanced equation for Denitrification.

2NO3−+5H2→N2(g)+2OH−+4H2O2NO_3^- + 5H_2 \rightarrow N_{2(g)} + 2OH^- + 4H_2O

86
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Write the complete balanced equation for Sulfate Reduction using Acetate (Desulforudis audaxviator).

CH3COOH+SO42−→H2S+2HCO3−CH_3COOH + SO_4^{2-} \rightarrow H_2S + 2HCO_3^-

87
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Write the complete balanced equation for Sulfate Reduction using Hydrogen (Desulforudis audaxviator).

4H2+SO42−→H2S+2OH−+2H2O4H_2 + SO_4^{2-} \rightarrow H_2S + 2OH^- + 2H_2O

88
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Write the complete balanced equation for Black Precipitate Reaction in a Winogradsky Column.

H2S+Fe2+→FeS(s)+2H+H_2S + Fe^{2+} \rightarrow FeS_{(s)} + 2H^+

89
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Write the complete balanced equation for Uranium Reduction.

UO22++H2→UO2(s)+2H+UO_2^{2+} + H_2 \rightarrow UO_{2(s)} + 2H^+

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Write the complete balanced equation for Technetium Reduction.

TcO4−+112H2→TcO2(s)+OH−+H2OTcO_4^- + 1\frac{1}{2}H_2 \rightarrow TcO_{2(s)} + OH^- + H_2O

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Write the complete balanced equation for Hydrogenotrophic Methanogenesis.

4H2+CO2→CH4(g)+2H2O4H_2 + CO_2 \rightarrow CH_{4(g)} + 2H_2O

92
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Write the complete balanced equation for Acetoclastic Methanogenesis.

CH3COOH→CH4(g)+CO2(g)CH_3COOH \rightarrow CH_{4(g)} + CO_{2(g)}

93
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Write the complete balanced equation for Serpentinised Olivine.

9Mg2(Ni)SiO4+3Fe2(Ni)SiO4+14H2O→6Mg3Si2O5(OH)4+2Fe3O4+2H29Mg_2(\text{Ni})SiO_4 + 3Fe_2(\text{Ni})SiO_4 + 14H_2O \rightarrow 6Mg_3Si_2O_5(OH)_4 + 2Fe_3O_4 + 2H_2

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Write the complete balanced equation for Manganese Oxidation.

Mn2++H2O+12O2→MnO2+2H+Mn^{2+} + H_2O + \frac{1}{2}O_2 \rightarrow MnO_2 + 2H^+

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Write the complete balanced equation for Complete Pyrite Oxidation by Ferric Iron.

FeS2+14Fe3++8H2O→15Fe2++2SO42−+16H+FeS_2 + 14Fe^{3+} + 8H_2O \rightarrow 15Fe^{2+} + 2SO_4^{2-} + 16H^+

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Write the complete balanced equation for Partial Pyrite Oxidation by Ferric Iron (forming elemental sulfur).

FeS2+2Fe3+→3Fe(aq)2++2S0FeS_2 + 2Fe^{3+} \rightarrow 3Fe^{2+}_{(aq)} + 2S^0

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Write the complete balanced equations for Supergene Enrichment of Copper via Disproportionation and Precipitation.

2S0+H2O→S2−+SO+2H+2S^0 + H_2O \rightarrow S^{2-} + SO + 2H^+

Cu2++S2−→CuS(s)Cu^{2+} + S^{2-} \rightarrow CuS_{(s)}

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Write the complete balanced equation for Chalcocite Leaching.

Cu2S(s)+8Fe3++4H2O→2Cu++8Fe2++SO42−+8H+Cu_2S_{(s)} + 8Fe^{3+} + 4H_2O \rightarrow 2Cu^+ + 8Fe^{2+} + SO_4^{2-} + 8H^+

99
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Write the complete balanced equation for Covellite Leaching.

CuS(s)+8Fe3++4H2O→Cu2++8Fe2++SO42−+8H+CuS_{(s)} + 8Fe^{3+} + 4H_2O \rightarrow Cu^{2+} + 8Fe^{2+} + SO_4^{2-} + 8H^+

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Write the complete balanced equation for Chalcopyrite Leaching.

CuFeS2(s)+16Fe3++8H2O→Cu2++17Fe2++2SO42−+16H+CuFeS_{2(s)} + 16Fe^{3+} + 8H_2O \rightarrow Cu^{2+} + 17Fe^{2+} + 2SO_4^{2-} + 16H^+