ALCHEMI finds a "shocking" carbon footprint in the starburst galaxy NGC~253

Centers of starburst galaxies may be characterized by a specific gas and ice chemistry due to their gas dynamics and the presence of various ice desorption mechanisms. This may result in a peculiar observable composition. We analyze abundances of \(CO_2\), a reliable tracer of ice chemistry, from data collected as part of the ALMA large program ALCHEMI, a wide-frequency spectral scan toward the starburst galaxy NGC~253 with an angular resolution of 1.6\(''\). We constrain the \(CO_2\) abundances in the gas phase using its protonated form \(HOCO^+\). The distribution of \(HOCO^+\) is similar to that of methanol, which suggests that \(HOCO^+\) is indeed produced from the protonation of \(CO_2\) sublimated from ice. The \(HOCO^+\) fractional abundances are found to be \((1-2)\times10^{-9}\) at the outer part of the central molecular zone (CMZ), while they are lower (\(\sim10^{-10}\)) near the kinematic center. This peak fractional abundance at the outer CMZ is comparable to that in the Milky Way CMZ, and orders of magnitude higher than that in Galactic disk star-forming regions. From the range of \(HOCO^+/CO_2\) ratios suggested from chemical models, the gas-phase \(CO_2\) fractional abundance is estimated to be \((1-20)\times10^{-7}\) at the outer CMZ, and orders of magnitude lower near the center. We estimate the \(CO_2\) ice fractional abundances at the outer CMZ to be \((2-5)\times10^{-6}\) from the literature. A comparison between the ice and gas \(CO_2\) abundances suggests an efficient sublimation mechanism. This sublimation is attributed to large-scale shocks at the orbital intersections of the bar and CMZ.