Understanding pH is essential in chemistry, as it represents the negative logarithm of the hydrogen ion concentration, expressed as pH = -\log[H^+] or pH = -\log[H_3O^+]. At elevated temperatures, such as 50 degrees Celsius, the ionization constant of water, denoted as K_w, changes. For pure water at this temperature, K_w is given as 7.94 \times 10^{-14}.
In a neutral solution, the concentrations of hydrogen ions [H^+] and hydroxide ions [OH^-] are equal. We can denote both concentrations as x. The relationship between these ions is defined by the equation:
[H^+][OH^-] = K_w
Substituting x for both concentrations gives us:
x^2 = 7.94 \times 10^{-14}
To find x, we take the square root of both sides:
x = \sqrt{7.94 \times 10^{-14}} \approx 2.8178 \times 10^{-7} \, \text{M}
This value represents both the hydrogen ion concentration and the hydroxide ion concentration in the neutral solution. To calculate the pH, we focus on the hydrogen ion concentration:
pH = -\log(2.8178 \times 10^{-7}) \approx 6.55
This result indicates that the pH of pure water at 50 degrees Celsius is approximately 6.55, which is slightly acidic compared to the neutral pH of 7 at 25 degrees Celsius.
When considering pure water with additional free-floating ions, it is important to account for the ionic strength and the activity coefficients, as these factors can influence the pH. The presence of ions alters the behavior of the solution, affecting both the concentration of hydrogen ions and the overall pH. Understanding these concepts is crucial for accurately determining pH in various chemical contexts.