# Probing CO and N$_2$ Snow Surfaces in Protoplanetary Disks with   N$_2$H$^+$ Emission

**Authors:** Chunhua Qi, Karin I. \"Oberg, Catherine C. Espaillat, Connor E., Robinson, Sean M. Andrews, David J. Wilner, Geoffrey A. Blake, Edwin A., Bergin, L. Ilsedore Cleeves

arXiv: 1907.10647 · 2019-09-25

## TL;DR

This study uses ALMA observations of N$_2$H$^+$ to probe the snow surfaces of CO and N$_2$ in protoplanetary disks, revealing diverse temperature structures and snowline locations crucial for understanding planet formation.

## Contribution

It provides the first empirical measurements of CO and N$_2$ snowline pairs in multiple disks, linking emission morphologies to vertical temperature structures.

## Key findings

- N$_2$H$^+$ emission shows two distinct morphologies linked to disk temperature structures.
- Snowline radii vary significantly among disks of similar spectral types.
- Empirical snowline data inform models of disk chemistry and planet formation.

## Abstract

Snowlines of major volatiles regulate the gas and solid C/N/O ratios in the planet-forming midplanes of protoplanetary disks. Snow surfaces are the 2D extensions of snowlines in the outer disk regions, where radiative heating results in a decreasing temperature with disk height. CO and N$_2$ are two of the most abundant carriers of C, N and O. N$_2$H$^+$ can be used to probe the snow surfaces of both molecules, because it is destroyed by CO and formed from N$_2$. Here we present Atacama Large Millimeter/submillimeter Array (ALMA) observations of N$_2$H$^+$ at 0.2$''$-0.4$''$ resolution in the disks around LkCa 15, GM Aur, DM Tau, V4046 Sgr, AS 209, and IM Lup. We find two distinctive emission morphologies: N$_2$H$^+$ is either present in a bright, narrow ring surrounded by extended tenuous emission, or in a broad ring. These emission patterns can be explained by two different kinds of vertical temperature structures. Bright, narrow N$_2$H$^+$ rings are expected in disks with a thick Vertically Isothermal Region above the Midplane (VIRaM) layer (LkCa 15, GM Aur, DM Tau) where the N$_2$H$^+$ emission peaks between the CO and N$_2$ snowlines. Broad N$_2$H$^+$ rings come from disks with a thin VIRaM layer (V4046 Sgr, AS 209, IM Lup). We use a simple model to extract the first sets of CO and N$_2$ snowline pairs and corresponding freeze-out temperatures towards the disks with a thick VIRaM layer. The results reveal a range of N$_2$ and CO snowline radii towards stars of similar spectral type, demonstrating the need for empirically determined snowlines in disks.

## Full text

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## Figures

32 figures with captions in the complete paper: https://tomesphere.com/paper/1907.10647/full.md

## References

69 references — full list in the complete paper: https://tomesphere.com/paper/1907.10647/full.md

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Source: https://tomesphere.com/paper/1907.10647