A rate constant almost always increases as temperature rises — because more molecules cross the energy barrier, not because the mechanism changes. For most reactions, raising the temperature does not change the reaction pathway; it changes how many collisions happen with enough energy to react.
The physical picture. At any temperature, molecular kinetic energies follow a spread (the Maxwell–Boltzmann distribution) — most molecules have energy near the average, and only a small fraction has energy equal to or above the activation energy \(\displaystyle E_a \) (the minimum energy a collision needs to react). Raising the temperature shifts this distribution so a larger fraction of molecules clears the \(\displaystyle E_a \) barrier. It is this growing fraction of "energetic enough" collisions — not a change in collision frequency alone — that makes the rate constant \(\displaystyle k \) rise sharply with \(\displaystyle T \).
A rough empirical rule (valid over the ordinary lab temperature range) is that
the rate constant of a reaction nearly doubles for every \(\displaystyle 10\ \text{K} \) (or \(\displaystyle 10\,^\circ\text{C} \)) rise in temperature. This is captured by the temperature coefficient,
\[\text{Temperature coefficient} = \frac{k_{T+10}}{k_{T}} \approx 2 \text{ to } 3
\]
where \(\displaystyle k_T \) and \(\displaystyle k_{T+10} \) are the rate constants at temperature \(\displaystyle T \) and \(\displaystyle T+10\,\text{K} \). This is only a rule of thumb — the exact relationship is quantitative and exponential, not linear.
The quantitative relationship: the Arrhenius equation.
\[k = A\, e^{-E_a/RT}
\]
Here:
\(\displaystyle k \) is the rate constant of the reaction,
\(\displaystyle A \) is the pre-exponential factor (also called the frequency factor) — it accounts for the frequency of collisions and the fraction of collisions with the correct orientation; \(\displaystyle A \) has the same units as \(\displaystyle k \),
\(\displaystyle E_a \) is the activation energy in \(\displaystyle \text{J mol}^{-1} \) (or \(\displaystyle \text{kJ mol}^{-1} \)),
\(\displaystyle R \) is the gas constant, \(\displaystyle 8.314\ \text{J K}^{-1}\text{mol}^{-1} \),
\(\displaystyle T \) is the absolute temperature in kelvin.
A step people get wrong here: \(\displaystyle T \) in this equation must be the
absolute (kelvin) temperature, never degrees Celsius — the exponential blows up any Celsius value used by mistake.
Why \(\displaystyle k \) rises with \(\displaystyle T \) follows directly from this equation. As \(\displaystyle T \) increases, the exponent \(\displaystyle -E_a/RT \) becomes less negative, so \(\displaystyle e^{-E_a/RT} \) increases, and hence \(\displaystyle k \) increases. The larger \(\displaystyle E_a \) is, the more sensitive \(\displaystyle k \) is to a change in \(\displaystyle T \) — reactions with high activation energy speed up much more sharply on heating than those with low activation energy.
A more convenient (linear) form. Taking the natural logarithm of both sides:
\[\ln k = \ln A - \frac{E_a}{RT}
\]
or, in base-$\displaystyle 10$ form (more common for graphical work),
\[\log k = \log A - \frac{E_a}{2.303\,RT}
\]
Since this last equation has the form \(\displaystyle y = c + mx \), a plot of \(\displaystyle \log k \) (y-axis) against \(\displaystyle 1/T \) (x-axis) gives a
straight line with
slope \(\displaystyle = -\dfrac{E_a}{2.303\,R} \), so \(\displaystyle E_a = -2.303\,R \times \text{slope} \), and
intercept \(\displaystyle = \log A \).
This is how \(\displaystyle E_a \) and \(\displaystyle A \) are actually determined experimentally: measure \(\displaystyle k \) at several temperatures, plot \(\displaystyle \log k \) vs. \(\displaystyle 1/T \), and read off the slope and intercept.
The two-temperature form. If the rate constants \(\displaystyle k_1 \) and \(\displaystyle k_2 \) are known at two temperatures \(\displaystyle T_1 \) and \(\displaystyle T_2 \), subtracting the log form of the Arrhenius equation at \(\displaystyle T_2 \) from that at \(\displaystyle T_1 \) eliminates \(\displaystyle A \):
\[\log k_1 = \log A - \frac{E_a}{2.303\,R\,T_1}, \qquad \log k_2 = \log A - \frac{E_a}{2.303\,R\,T_2}
\]
\[\log k_2 - \log k_1 = \frac{E_a}{2.303\,R}\left(\frac{1}{T_1} - \frac{1}{T_2}\right)
\]
\[\log\frac{k_2}{k_1} = \frac{E_a}{2.303\,R}\left(\frac{1}{T_1} - \frac{1}{T_2}\right)
\]
This form is the one most often used in numerical problems: given \(\displaystyle E_a \) and \(\displaystyle k \) at one temperature, it gives \(\displaystyle k \) at another temperature (or, given \(\displaystyle k \) at two temperatures, it gives \(\displaystyle E_a \)) without needing to know \(\displaystyle A \) separately.
Answer: For most reactions, the rate constant \(\displaystyle k \) increases with rising temperature (roughly doubling for every \(\displaystyle 10\,\text{K}/10\,^\circ\text{C}\) rise), because a larger fraction of molecules then possesses energy at or above the activation energy \(\displaystyle E_a \). This is represented quantitatively by the Arrhenius equation \(\displaystyle k = A e^{-E_a/RT} \), or in logarithmic form \(\displaystyle \log k = \log A - \dfrac{E_a}{2.303\,RT} \), whose two-temperature version is \(\displaystyle \log\dfrac{k_2}{k_1} = \dfrac{E_a}{2.303\,R}\left(\dfrac{1}{T_1}-\dfrac{1}{T_2}\right) \).