The average bond enthalpies of the \(\mathrm{C}-\mathrm{C}\) and \(\mathrm{C}-\mathrm{H}\) bonds are \(348 \mathrm{~kJ} / \mathrm{mol}\) and $413 \mathrm{~kJ} / \mathrm{mol}$, respectively. (a) What is the maximum wavelength that a photon can possess and still have sufficient energy to break the \(\mathrm{C}-\mathrm{H}\) and \(\mathrm{C}-\mathrm{C}\) bonds, respectively? (b) Given the fact that \(\mathrm{O}_{2}, \mathrm{~N}_{2},\) and \(\mathrm{O}\) in the upper atmosphere absorb most of the light with wavelengths shorter than $240 \mathrm{nm}$, would you expect the photodissociation of \(\mathrm{C}-\mathrm{C}\) and \(\mathrm{C}-\mathrm{H}\) bonds to be significant in the lower atmosphere?

Short Answer

Expert verified
The maximum wavelength for C-C and C-H bonds are 343 nm and 289 nm, respectively. Since these values are greater than 240 nm, photodissociation of C-C and C-H bonds can be significant in the lower atmosphere.

Step by step solution

01

Planck's Equation

Planck's equation is given by: \[E = h \nu\] Where E is the energy of the photon, h is Planck's constant (6.626 x 10^(-34) J.s), and ν is the frequency of the photon. The frequency of a photon is related to its wavelength (λ) by the speed of light (c): \[\nu = \frac{c}{\lambda}\] Where c = 3 x 10^8 m/s. Substituting this equation into Planck's equation, we get: \[E = \frac{hc}{\lambda}\]
02

Calculate wavelength for C-C bond

Given the bond enthalpy of the C-C bond is 348 kJ/mol, we first need to convert this to energy per photon: \[\frac{348\,\text{kJ}}{\text{mol}} \times \frac{1000\,\text{J}}{1\,\text{kJ}} \times \frac{1 \text{mol}}{6.022 \times 10^{23}\,\text{atoms}} = 5.78 \times 10^{-19}\,\text{J}\] Now we can use Planck's equation to find the maximum wavelength: \[\lambda_{\mathrm{C-C}} = \frac{hc}{E_{\mathrm{C-C}}} = \frac{(6.626 \times 10^{-34}\,\text{J.s})(3 \times 10^8\,\text{m/s})}{5.78 \times 10^{-19}\,\text{J}} = 343\,\text{nm}\]
03

Calculate wavelength for C-H bond

Similarly, do the same for the C-H bond with a bond enthalpy of 413 kJ/mol: \[\frac{413\,\text{kJ}}{\text{mol}} \times \frac{1000\,\text{J}}{1\,\text{kJ}} \times \frac{1 \text{mol}}{6.022 \times 10^{23}\,\text{atoms}} = 6.86 \times 10^{-19}\,\text{J}\] And find the maximum wavelength: \[\lambda_{\mathrm{C-H}} = \frac{hc}{E_{\mathrm{C-H}}} = \frac{(6.626 \times 10^{-34}\,\text{J.s})(3 \times 10^8\,\text{m/s})}{6.86 \times 10^{-19}\,\text{J}} = 289\,\text{nm}\]
04

Compare the wavelengths to atmospheric absorption

We are given that wavelengths shorter than 240 nm are absorbed in the upper atmosphere. The calculated wavelengths for the C-C and C-H bonds were 343 nm and 289 nm, respectively. Both of these values are greater than 240 nm.
05

Determine the significance of photodissociation

Since the maximum wavelengths required to break C-C and C-H bonds are greater than 240 nm, the photons with these wavelengths can pass through the upper atmosphere without being absorbed. This means that photodissociation of C-C and C-H bonds can be significant in the lower atmosphere.

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Most popular questions from this chapter

In the lime soda process once used in large scale municipal water softening, calcium hydroxide prepared from lime and sodium carbonate are added to precipitate \(\mathrm{Ca}^{2+}\) as \(\mathrm{CaCO}_{3}(s)\) and \(\mathrm{Mg}^{2+}\) as \(\mathrm{Mg}(\mathrm{OH})_{2}(s);\) $$ \begin{aligned} \mathrm{Ca}^{2+}(a q)+\mathrm{CO}_{3}^{2-}(a q) & \longrightarrow \mathrm{CaCO}_{3}(s) \\ \mathrm{Mg}^{2+}(a q)+2 \mathrm{OH}^{-}(a q) & \longrightarrow \mathrm{Mg}(\mathrm{OH})_{2}(s) \end{aligned} $$ How many moles of \(\mathrm{Ca}(\mathrm{OH})_{2}\) and $\mathrm{Na}_{2} \mathrm{CO}_{3}\( should be added to soften (remove the \)\mathrm{Ca}^{2+}$ and \(\mathrm{Mg}^{2+}\) ) 1000 L of water in which $$ \begin{array}{l} {\left[\mathrm{Ca}^{2+}\right]=3.5 \times 10^{-4} \mathrm{M}} \\ {\left[\mathrm{Mg}^{2+}\right]=7.5 \times 10^{-4} \mathrm{M}} \end{array} $$

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