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Topic 2/3
15 Flashcards in this deck.
Ionization refers to the process by which atoms or molecules gain or lose electrons to form ions. In the context of water, ionization involves the separation of water molecules into hydrogen ions ($H^+$) and hydroxide ions ($OH^-$). This self-ionization is a natural and continuous process that occurs to a very small extent in pure water.
Pure water undergoes a reversible reaction known as self-ionization:
$$ 2H_2O(l) \leftrightarrow H_3O^+(aq) + OH^-(aq) $$Alternatively, it can be represented more simply as:
$$ H_2O(l) \leftrightarrow H^+(aq) + OH^-(aq) $$At 25°C, the concentration of both $H^+$ and $OH^-$ ions in pure water is $1.0 \times 10^{-7} \, M$.
The equilibrium constant for the ionization of water ($K_w$) is a crucial parameter:
$$ K_w = [H^+][OH^-] = 1.0 \times 10^{-14} \, (at \, 25^\circ C) $$This value indicates the product of the concentrations of hydrogen ions and hydroxide ions in water. $K_w$ varies with temperature, increasing as temperature rises.
pH and pOH are measures of the acidity and basicity of a solution, respectively. They are related to the concentrations of hydrogen and hydroxide ions:
$$ pH = -\log[H^+] $$ $$ pOH = -\log[OH^-] $$At 25°C, the sum of pH and pOH is always 14:
$$ pH + pOH = 14 $$To calculate pH or pOH, follow these steps:
Example: If $[H^+] = 1.0 \times 10^{-5} \, M$, then:
$$ pH = -\log(1.0 \times 10^{-5}) = 5 $$ $$ pOH = 14 - 5 = 9 $$The ion product ($K_w$) changes with temperature. For instance:
As temperature increases, water ionizes more, increasing the concentrations of $H^+$ and $OH^-$ ions.
Acid-base neutralization involves the reaction between $H^+$ ions and $OH^-$ ions to form water:
$$ H^+ + OH^- \rightarrow H_2O $$>This reaction is exothermic and helps maintain the pH balance in aqueous solutions.
The presence of a common ion can suppress the ionization of water. For example, adding a strong acid like HCl to water increases $[H^+]$, shifting the equilibrium to the left and decreasing water's ionization:
$$ HCl \rightarrow H^+ + Cl^- $$>This results in a lower $[OH^-]$ and thus a lower $K_w$.
Autoionization refers to water's self-ionization without any external influence. In contrast, ionization by external agents involves substances like acids or bases that increase $[H^+]$ or $[OH^-]$, respectively. Understanding the distinction is vital for accurate pH and pOH calculations.
The temperature dependence of $K_w$ can be expressed using the van 't Hoff equation. As temperature rises, the endothermic ionization of water leads to an increase in $K_w$, affecting the pH of pure water.
Knowledge of water ionization is essential in various fields:
Aspect | Self-Ionization of Water | Ionization by Acids/Bases |
Definition | Water molecules dissociate into $H^+$ and $OH^-$ ions spontaneously. | Addition of external agents like acids or bases increases $H^+$ or $OH^-$ concentrations. |
Equilibrium Constant ($K_w$) | Constant at a given temperature; $1.0 \times 10^{-14}$ at $25^\circ C$. | Varies based on the concentration of added ions, shifting the equilibrium. |
Effect on pH | Pure water has a neutral pH of 7. | Acids lower pH; bases raise pH. |
1. Remember the Balance: Always keep in mind that $pH + pOH = 14$ at 25°C. This relationship helps in quickly finding one value when you know the other.
2. Logarithm Mastery: Practice calculating $pH$ and $pOH$ using the negative logarithm of ion concentrations to enhance accuracy.
3. Temperature Awareness: Be aware that $K_w$ changes with temperature, so always consider the temperature when performing calculations.
4. Common Mnemonic: Use "pH and pOH are in Complete Relation" to remind yourself that their sum is constant.
1. The self-ionization of water is an endothermic process, meaning it absorbs heat. This property is essential in understanding how temperature changes affect water's pH levels in natural water bodies.
2. Heavy water (D₂O), used in certain nuclear reactors, ionizes less than regular water, affecting its acidity and basicity properties.
3. The concept of pH was developed by Danish chemist Søren Sørensen in 1909, revolutionizing how we measure and understand acidity and basicity in chemistry.
Mistake 1: Confusing the ion product of water ($K_w$) with the acid dissociation constant ($K_a$).
Incorrect: Using $K_w$ to calculate the pH of a strong acid.
Correct: Use $K_a$ for acid pH calculations and $K_w$ for pure water or neutral solutions.
Mistake 2: Forgetting that $pH + pOH = 14$ at 25°C.
Incorrect: Calculating pH and pOH independently without relation.
Correct: Use the relationship to find one value when the other is known.
Mistake 3: Miscalculating pH by not taking the negative logarithm of $[H^+]$.
Incorrect: Direct subtraction like $[H^+] - 1 = pH$.
Correct: Apply $pH = -\log[H^+]$ properly.