Answer: E. 1.6ₓ10⁻¹⁰ M
Explanation:
The pH is a <u>measure of acidity or alkalinity of a solution.</u> The pH indicates the concentration of hydrogen ions present in certain solutions according to the following equation,
pH =
where ![a_{H^{+} } = y_{i} [H^{+}]](https://tex.z-dn.net/?f=a_%7BH%5E%7B%2B%7D%20%7D%20%3D%20y_%7Bi%7D%20%5BH%5E%7B%2B%7D%5D)
where
is the activity of hydrogen ions and
is the activity coefficient. The activity is a <u>measure of an "effective concentration" of a species</u>. It arises because the molecules in a non-ideal gas or solution interact with each other.
<u>The above equation is useful for solutions that do not have ideal behavior,</u> that is, <u>undiluted solutions</u>. However, <u>we can simplify the previous expression equalizing the activity with the concentration of hydrogen ions</u> without major loss of accuracy, since in general we work with diluted solutions in practice.
Then, if pH = 4.20,
pH = - log [H⁺] → [H⁺] =
→ [H⁺] = 
→ [H⁺] = 6.31ₓ10⁻⁵ M
Water self-ionization is the <u>chemical reaction in which water molecules react to produce an hydrogen ion (H⁺) and a hydroxide ion (OH⁻)</u>,
H₂O (l) ⇄ H⁺(ac) + OH⁻(ac)
The ionization equilibrium of water is described by the <em>ionic product of water</em> and is symbolized by Kw. Around 25ºC <u>Kw = 1.0ₓ10⁻¹⁴</u>, so
Kw = [H⁺] [OH⁻] → [OH⁻] = Kw / [H⁺] → [OH⁻] = 1.0ₓ10⁻¹⁴ / 6.31ₓ10⁻⁵ M
→ [OH⁻] = 1.59ₓ10⁻¹⁰ M ≈ 1.6ₓ10⁻¹⁰ M
So, when a solution has a pH of 4.20 the concentration of OH− is 1.6ₓ10⁻¹⁰ M