Such a dramatic change would indeed make it harder to reach space, in a precisely defined sense. The easiest measure of how 'hard' it is to get so space is the escape velocity, which is determined by the planet's mass $M$ and radius $R$ as
$$
v_\text{esc}=\sqrt{\frac{2GM}R}.
$$
For a planet like the one you mention, the escape velocity goes up by a factor of $\sqrt{17/2}\approx3$ with respect to the Earth's escape velocity $v_\text{E}$.
The reason this matters is that the total mass $M$ of a rocket that will send a payload of mass $m$ into space depends exponentially on the escape velocity. (More accurately, on the change in velocity required, $\Delta v$, which is of the order of $v_\text{esc}$.) This relation is known as the Tsiolkovsky rocket equation and it is one of the fundamental principles of rocket science; it states that
$$
M=m\exp\left(\frac{v_\text{esc}}{v_\text{exh}}\right),
$$
where $v_\text{exh}$ is the exhaust velocity.
Because of this exponential dependence, if $v_\text{esc}$ goes up from $v_\text{E}$ by a factor of three, the rocket mass will increase by a factor of
$$
\left(e^{v_\text{E}/v_\text{exh}}\right)^{3},
$$
which can be a lot more than three. To put some numbers in, $v_\text{E}\approx11.2 \,\text{km}/\text s$ whereas liquid propellants can get up to about $v_\text{exh}\approx 5 \,\text{km}/\text s$. When exponentials are involved the details do matter, but if you put this in you get an overall factor of the order of
$$
(e^2)^3\approx 400.
$$
This would mean, for example, that a behemoth like the 3,000-ton Saturn V would be able to transport about 100kg of payload - about the size of a 'minisatellite', instead of the 45 tons of a fully-fledged Apollo mission.
Now, there are a number of ways to get around this restriction, of which many are technological but some are physical. The most obvious one, to me, is that the size of the atmosphere will also change. This obviously depends on the amount and composition of the exoplanet's atmosphere, but with all other things equal, a more massive planet will compress its atmosphere into a thinner layer. This change on length scale is linear: as a first approximation, it is inversely proportional to the surface gravitational acceleration,
$$
g_0=\frac{GM}{R^2}
$$
which is about 4 times that of Earth for the exoplanet in question.
Thus, if all other things were equal - if the atmospheric composition and surface pressure were the same as Earth's - then you'd only have to go up, say, 40 km for low exoplanet orbit, instead of the ~160 km of low Earth orbit. This is important, because it radically reduces the $\Delta v$ required to get into orbit, and this goes again into the exponential dependence of the Tsiolkovsky equation. The $\Delta v$ to get to a height $h$ is roughly
$$
\Delta v=\sqrt{\frac{2GM}R-\frac{2GM}{R+h}}=\sqrt{\frac{2GMh}{R+h}},
$$
and this has now gone down, slightly, for Kepler-10c. (You still need to accelerate to stay in orbit, but that depends on the planet's rate of rotation which is yet another completely unknown variable.)
To summarize, then, it will indeed be harder to go to space from such a planet, but under certain circumstances it may be easier to get to orbit. The problem with all this, though, is that details - about the specifics of the planet and its atmosphere, and also about what you want to do - do matter, because of the exponential dependence, which is hard to understand until you run into a good number of walls like this one. As Phil Frost mentions, xkcd what-if is a good place to read about this, but in general, it pays to sit up and pay attention when a variable of interest is on the exponent.