Limiting molar conductivity refers to the maximum molar conductivity that a solution of an electrolyte can achieve as the concentration approaches infinity (in the limit of infinite dilution). In other words, it's the molar conductivity of an electrolyte solution when it is so dilute that further dilution doesn't significantly affect its conductivity.

At infinite dilution, the ions in the solution are effectively isolated from each other, minimizing the influence of ion-ion interactions. Thus, the limiting molar conductivity provides a measure of the inherent conductivity of the ions themselves, independent of the specific conditions of the solution.

Mathematically, the limiting molar conductivity (Λ0Λ0) of an electrolyte can be determined using the Kohlrausch's Law of independent migration of ions:

Λ0=lim⁡c→0κcΛ0=limc→0cκ

where:

• Λ0Λ0 is the limiting molar conductivity,
• κκ is the conductivity of the solution, and
• cc is the concentration of the electrolyte (which approaches zero as it tends towards infinite dilution).

Limiting molar conductivity values are often used to compare the conductivities of different electrolytes and to understand their behavior at low concentrations.

The relation between conductivity (κκ) and molar conductivity (ΛmΛm) of a solution held in a cell is given by the equation:

κ=Λm×Cκ=Λm×C

where:

• κκ is the conductivity of the solution (measured in siemens per meter, S/m),
• ΛmΛm is the molar conductivity of the solution (measured in siemens per meter squared per mole, S·m²/mol),
• CC is the concentration of the solution (measured in moles per cubic meter, mol/m³).

This equation demonstrates that conductivity (κκ) is directly proportional to the molar conductivity (ΛmΛm) and the concentration of the solution (CC). Therefore, an increase in molar conductivity or concentration will result in an increase in conductivity.

The cell constant, resistance of the solution in the cell, and conductivity of the solution are related through the equation:

Conductivity(κ)=1Cell Constant(Λ)×1Resistance of solution in cell(R)Conductivity(κ)=Cell Constant(Λ)1×Resistance of solution in cell(R)1

Where:

• Conductivity (κκ) is measured in siemens per meter (S/m).
• Cell Constant (ΛΛ) is measured in reciprocal meters (m−1m−1).
• Resistance of the solution in the cell (R) is measured in ohms (ΩΩ).

This equation indicates that conductivity is inversely proportional to the product of the cell constant and the resistance of the solution in the cell. Essentially, as conductivity increases, resistance decreases, and vice versa. The cell constant is a property of the conductivity cell used in the measurement, and it relates the geometry of the cell to the conductivity of the solution being measured.

The conductivity of a solution (κκ) is related to its molar conductivity (ΛmΛm) through the equation:

κ=Λm×Cκ=Λm×C

Where:

• Molar conductivity (ΛmΛm) is measured in siemens per meter per mole (S⋅m2⋅mol−1S⋅m2⋅mol−1).
• CC is the concentration of the solution in moles per liter (mol/L).

This equation shows that the conductivity of a solution is directly proportional to its molar conductivity and concentration. Molar conductivity is a measure of the conductivity of a solution containing one mole of solute per liter, and it accounts for the contribution of each ion to the solution's conductivity.

The reducing power of a metal is related to its ability to lose electrons and undergo oxidation. Metals with lower standard electrode potentials (E°) have a greater tendency to lose electrons and therefore are stronger reducing agents.

Here are the metals arranged in increasing order of their reducing power based on their standard electrode potentials:

1. K (Potassium) with E° = -2.93 V
2. Mg (Magnesium) with E° = -2.37 V
3. Cr (Chromium) with E° = -0.74 V
4. Fe (Iron) with E° = -0.44 V
5. Cu (Copper) with E° = 0.34 V
6. Ag (Silver) with E° = 0.80 V

So, the order of reducing power is: K < Mg < Cr < Fe < Cu < Ag.

The corrosion of iron in the atmosphere primarily involves the following electrochemical reactions:

1. Formation of Iron Oxide (Rusting): When iron is exposed to atmospheric oxygen and moisture, it undergoes oxidation to form iron oxide, commonly known as rust. The overall reaction is:

   4Fe+3O2+6H2O→4Fe(OH)34Fe+3O2+6H2O→4Fe(OH)3

   This reaction occurs in the presence of water and oxygen. Iron atoms lose electrons to oxygen molecules, forming iron ions (Fe²⁺) and hydroxide ions (OH⁻). These ions then react with water molecules to form rust (Fe(OH)₃).

2. Electron Transfer (Oxidation Reaction): The oxidation of iron can be represented as:

   Fe→Fe2++2e−Fe→Fe2++2e−

   Iron atoms lose electrons to form ferrous ions (Fe²⁺). This process is known as oxidation. These electrons released during oxidation are involved in the reduction half-reaction.

3. Reduction Reaction (Oxygen Reduction): Atmospheric oxygen reacts with water and electrons to form hydroxide ions. This reaction is represented as:

   O2+2H2O+4e−→4OH−O2+2H2O+4e−→4OH−

   Oxygen molecules gain electrons and react with water molecules to form hydroxide ions (OH⁻). This process is called reduction.

4. Overall Reaction: Combining the oxidation and reduction half-reactions, we get the overall reaction for the corrosion of iron in the atmosphere:

   4Fe+3O2+6H2O→4Fe(OH)34Fe+3O2+6H2O→4Fe(OH)3

   This reaction shows the formation of rust (iron hydroxide) from iron, oxygen, and water.

In summary, the corrosion of iron in the atmosphere is an electrochemical process involving the oxidation of iron and reduction of oxygen. Moisture and oxygen from the atmosphere facilitate the formation of rust, leading to the degradation of iron structures over time.