Inorganic Chemicals Table


Inorganic ChemicalClassFormula/CompositionImmediate roleUpstream inputsDownstream outputs
WaterPolar moleculeH2OUniversal solvent, reactant, temperature bufferPrecipitation, metabolic waterHydration shells, hydrolysis reactions
Oxygen gasDiatomic moleculeO2Terminal electron acceptor in aerobic respiration, photosynthetic productPhotosynthesis, atmospheric mixingH2O via respiration, ROS
Carbon dioxideLinear moleculeCO2Carbon source for photosynthesis, product of respirationRespiration, combustionCarbohydrates via Calvin cycle
Nitrogen gasDiatomic moleculeN2Atmospheric N source for fixationAtmospheric reservoirNH3, organic N via nitrogen fixation
AmmoniaInorganic baseNH3 / NH4+Nitrogen nutrient for plants/microbesNitrogen fixation, organic N mineralizationNitrate via nitrification, amino acids
Nitrite ionInorganic anionNO2-Intermediate in nitrogen cycleNitrification, denitrificationNitrate, N2 gas
Nitrate ionInorganic anionNO3-Plant/microbial nitrogen sourceNitrificationOrganic N, N2 gas via denitrification
Phosphate ionInorganic oxyanionPO4^3- / H2PO4- / HPO4^2-Essential nutrient (ATP, nucleic acids)Mineral weathering, OM mineralizationBiomass P, precipitated minerals
Sulfate ionInorganic oxyanionSO4^2-Sulfur nutrient, electron acceptorWeathering of sulfates, OM mineralizationSulfide via microbial reduction
Sulfide ionInorganic anionS^2- / HS-Reduced S form, microbial electron donorSulfate reductionElemental S, SO4^2-
Chloride ionInorganic anionCl-Osmotic balance, enzyme cofactorHalite dissolution, atmospheric depositionBiomass Cl, leaching
Sodium ionInorganic cationNa+Osmotic balance, some enzyme cofactor rolesMineral dissolution (halite)Sodium salts, ion gradients
Potassium ionInorganic cationK+Essential plant/microbial nutrientMineral dissolution (feldspar, mica)Biomass K, ion gradients
Calcium ionInorganic cationCa2+Structural role in cell walls, signalingCalcite/dolomite weatheringCa salts, cell wall crosslinks
Magnesium ionInorganic cationMg2+Chlorophyll central atom, enzyme cofactorDolomite/olivine weatheringBiomass Mg, Mg salts
Iron (ferrous) ionInorganic cationFe2+Electron donor, enzyme cofactorMineral dissolution under reducing conditionsFe3+ via oxidation
Iron (ferric) ionInorganic cationFe3+Electron acceptor, enzyme cofactorOxidation of Fe2+, mineral weatheringFe2+ via reduction, Fe oxides
Manganese ionInorganic cationMn2+Enzyme cofactor, photosystem II water-splittingMineral weatheringMn oxides via oxidation
Zinc ionInorganic cationZn2+Enzyme cofactor, structural role in proteinsMineral weatheringBiomass Zn, Zn salts
Copper ionInorganic cationCu+/Cu2+Electron transfer in respiration/photosynthesisMineral weatheringBiomass Cu, Cu salts
Cobalt ionInorganic cationCo2+Cofactor in vitamin B12Mineral weatheringBiomass Co, corrinoids
Hydrogen ion (proton)Inorganic ionH+pH control, proton motive forceAcid dissociation, water autoprotolysisWater, metabolic proton gradients
Hydroxide ionInorganic ionOH-pH control, base catalysisWater autoprotolysis, base additionWater, metal hydroxides

Integration notes:

  • These inorganic chemicals are the free ionic and molecular forms — the “mobile” inorganic currency — that link the Inorganic Minerals pool to the Organic Chemicals and biological systems.
  • Many entries directly tie to your Organic Minerals list via chelation or precipitation (e.g., Ca2+ ↔ calcium oxalate, Mg2+ ↔ chlorophyll-Mg complex).
  • They also serve as nodes in major biogeochemical cycles (C, N, P, S, Fe, etc.) that are relevant across soil, algae, mycelium, and genetic code contexts.

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