04 COMPLEXATION AND CHELATION
Complexation and Chelation
Definition: Complexation refers to the process in which metal ions form complexes with ligands, whereas chelation is a specific type of complexation where a ligand bonds to a metal ion at two or more coordination sites.
Chemical and Biochemical Phenomena in Stratified Water Bodies
Gas Exchange:
Gases such as CO2 and O2 exchanged with the atmosphere.
Chemical equations indicate processes like photosynthesis and acid-base reactions:
For example: HCO3 + OH- <-> Ca2+ + CO3(2-)
Microbial Action:
Microbial processes lead to leaching and uptake of nutrients (e.g., CH2O). Against a background of sediment groundwater interactions.
Metals Dissolved in Water
Properties depend on the species of metals dissolved in bodies of water.
Speciation:
Crucial for environmental chemistry in waters.
Chemical Speciation
Definition: Determining individual concentrations of different chemical forms that make up the total concentration of an element.
Trace Metal Speciation
Involves determining:
Free ions
Complexes (labile and non-labile)
Colloids
Total dissolved concentrations
Ligands and Complexes
Hydrated Metal Ion Complexation:
Example: Cyanide can form complexes with iron, Fe(CN)2-, Fe(CN)3-, etc.
Coordination Compounds:
Comprised of complex ions and counter ions.
Ligands:
Entities that bond with metal ions and donate electrons.
Donor Atom and Coordination Number
Donor Atom: Atom in ligand attached to the metal (e.g., in complex [Ag(NH3)2]+, N serves as donor).
Coordination Number: Number of donor atoms around metal ion.
Classification of Ligands
Monodentate Ligands:
Have one donor atom (e.g., ammonia, water, cyanide).
Bidentate Ligands:
Have two donor atoms (e.g., ethylenediamine, oxalate).
Polydentate Ligands:
Have multiple donor atoms (e.g., EDTA).
Chelation
Chelating Agents:
Can bind to metal ions at multiple sites, forming stable ring structures.
Stability:
Chelates are more stable than complexes composed of unidentate ligands.
Stability increases with the number of chelating sites.
Humic Substances as Complexing Agents
Humic substances are important natural complexing agents formed from vegetation decay.
Classification:
Humic acid
Fulvic acid
Humin
They strongly affect water properties via acid-base reactions and solubility effects.
Binding of Metal Ions by Humic Substances
Binding types include:
Chelation (e.g., between carboxyl and phenolic groups).
They notably bind iron and other metals, influencing their bioavailability and mobility.
Redox Chemistry in Natural Waters
Oxidation-Reduction Reactions:
Organic matter oxidation is a significant process (e.g., decomposition reactions).
Microbial activity can significantly alter oxygen and nutrient cycles.
Oxygen Demand:
Biochemical Oxygen Demand (BOD) and Chemical Oxygen Demand (COD) are metrics of organic matter and contaminants.
Sediment Formation and Characteristics
Formed through physical, chemical, and biological processes.
Contain various organisms and pollutants that interact with the water column.
Pore Water:
Water found in spaces between sediment particles, crucial for nutrient processing.
Microbial Activities in Aquatic Systems
Microorganisms (bacteria, fungi, protozoa) are vital for nutrient cycles:
They decompose organic matter, influence gas exchange, and manage nutrient availability.
Types of Microorganisms:
Algae: Involved in photosynthesis and biomass production.
Fungi: Decompose organic matter and have a role in nutrient cycling.
Protozoa: Participate in food webs and can impact water quality.
Importance of Microbial Processes
Microbial metabolism plays a key role in carbon cycling:
Methanogenesis occurs in anoxic conditions, yielding methane as a byproduct.
Microbial decomposition of organic matter is crucial for nutrient release and energy production in aquatic ecosystems.