- Esposito, Thomas M;
- Duchêne, Gaspard;
- Kalas, Paul;
- Rice, Malena;
- Choquet, Élodie;
- Ren, Bin;
- Perrin, Marshall D;
- Chen, Christine H;
- Arriaga, Pauline;
- Chiang, Eugene;
- Nielsen, Eric L;
- Graham, James R;
- Wang, Jason J;
- De Rosa, Robert J;
- Follette, Katherine B;
- Ammons, S Mark;
- Ansdell, Megan;
- Bailey, Vanessa P;
- Barman, Travis;
- Bruzzone, Juan Sebastián;
- Bulger, Joanna;
- Chilcote, Jeffrey;
- Cotten, Tara;
- Doyon, Rene;
- Fitzgerald, Michael P;
- Goodsell, Stephen J;
- Greenbaum, Alexandra Z;
- Hibon, Pascale;
- Hung, Li-Wei;
- Ingraham, Patrick;
- Konopacky, Quinn;
- Larkin, James E;
- Macintosh, Bruce;
- Maire, Jérôme;
- Marchis, Franck;
- Marois, Christian;
- Mazoyer, Johan;
- Metchev, Stanimir;
- Millar-Blanchaer, Maxwell A;
- Oppenheimer, Rebecca;
- Palmer, David;
- Patience, Jennifer;
- Poyneer, Lisa;
- Pueyo, Laurent;
- Rajan, Abhijith;
- Rameau, Julien;
- Rantakyrö, Fredrik T;
- Ryan, Dominic;
- Savransky, Dmitry;
- Schneider, Adam C;
- Sivaramakrishnan, Anand;
- Song, Inseok;
- Soummer, Rémi;
- Thomas, Sandrine;
- Wallace, J Kent;
- Ward-Duong, Kimberly;
- Wiktorowicz, Sloane;
- Wolff, Schuyler
We present new high resolution imaging of a light-scattering dust ring and halo around the young star HD 35841. Using spectroscopic and polarimetric data from the Gemini Planet Imager in H-band (1.6 μm), we detect the highly inclined (i = 85°) ring of debris down to a projected separation of ∼12 au (∼0.″12) for the first time. Optical imaging from HST/STIS shows a smooth dust halo extending outward from the ring to >140 au (>1.″4). We measure the ring's scattering phase function and polarization fraction over scattering angles of 22°-125°, showing a preference for forward scattering and a polarization fraction that peaks at ∼30% near the ansae. Modeling of the scattered-light disk indicates that the ring spans radii of ∼60-220 au, has a vertical thickness similar to that of other resolved dust rings, and contains grains as small as 1.5 μm in diameter. These models also suggest the grains have a low porosity, are more likely to consist of carbon than astrosilicates, and contain significant water ice. The halo has a surface brightness profile consistent with that expected from grains pushed by radiation pressure from the main ring onto highly eccentric but still bound orbits. We also briefly investigate arrangements of a possible inner disk component implied by our spectral energy distribution models, and speculate about the limitations of Mie theory for doing detailed analyses of debris disk dust populations.