  Pebble accretion is a promising process for decreasing growth timescales of
planetary cores, allowing gas giants to form at wide orbital separations.
However, nebular turbulence can reduce the efficiency of this gas-assisted
growth. We present an order of magnitude model of pebble accretion, which
calculates the impact of turbulence on the average velocity of small bodies,
the radius for binary capture, and the sizes of the small bodies that can be
accreted. We also include the effect of turbulence on the particle scale
height, which has been studied in previous works. We find that turbulence does
not prevent rapid growth in the high-mass regime: the last doubling time to the
critical mass to trigger runaway gas accretion ($M \sim 10 \, M_\oplus$) is
well within the disk lifetime even for strong ($\alpha \gtrsim 10^{-2}$)
turbulence. We find that while the growth timescale is quite sensitive to the
local properties of the protoplanetary disk, over large regimes of parameter
space large cores grow in less than the disk lifetime if appropriately-sized
small bodies are present. Instead, the effects of turbulence are most
pronounced for low planetary masses. For strong turbulence the growth timescale
is longer than the gas disk lifetime until the core reaches masses $\gtrsim
10^{-2}-10^{-1} M_\oplus$. A "Flow Isolation Mass", at which binary capture
ceases, emerges naturally from our model framework. We comment that the
dependence of this mass on orbital separation is similar to the semi-major axis
distribution of solar-system cores.
