Erratum: “X‐Ray Ionization of Protoplanetary Disks” (ApJ, 480, 344 [1997])

1997 ◽  
Vol 485 (2) ◽  
pp. 920-920 ◽  
Author(s):  
A. E. Glassgold ◽  
J. Najita ◽  
J. Igea
Keyword(s):  
1997 ◽  
Vol 480 (1) ◽  
pp. 344-350 ◽  
Author(s):  
A. E. Glassgold ◽  
J. Najita ◽  
J. Igea
Keyword(s):  

2018 ◽  
Vol 865 (1) ◽  
pp. 75 ◽  
Author(s):  
Riouhei Nakatani ◽  
Takashi Hosokawa ◽  
Naoki Yoshida ◽  
Hideko Nomura ◽  
Rolf Kuiper

2009 ◽  
Vol 5 (H15) ◽  
pp. 727-728
Author(s):  
Jane Gregorio-Hetem ◽  
Silvia Alencar

In recent years our knowledge of star, brown dwarf and planet formation has progressed immensely due to new data in the IR domain (Spitzer telescope), new X-ray campaigns such as the Chandra Orion Ultradeep Project (COUP) and the X-ray Emission Survey of Taurus (XEST), with XMM-Newton, as well as adaptive optics results and synoptic studies of young stellar and substellar objects.


2012 ◽  
Vol 547 ◽  
pp. A69 ◽  
Author(s):  
G. Aresu ◽  
R. Meijerink ◽  
I. Kamp ◽  
M. Spaans ◽  
W.-F. Thi ◽  
...  

2011 ◽  
Vol 526 ◽  
pp. A163 ◽  
Author(s):  
G. Aresu ◽  
I. Kamp ◽  
R. Meijerink ◽  
P. Woitke ◽  
W.-F. Thi ◽  
...  

2019 ◽  
Vol 15 (S350) ◽  
pp. 408-409
Author(s):  
Stephen P. Thompson ◽  
Anna Herlihy ◽  
Claire A. Murray ◽  
Annabelle R. Baker ◽  
Sarah J. Day

AbstractAmorphous Mg-Fe silicates are produced from microwave-dried sol-gels and their thermal crystallisation is studied via in situ synchrotron X-ray powder diffraction. Mg-pyroxene crystallised to forsterite, enstatite and cristobalite. The inclusion of 10% Fe formed only forsterite at much higher temperature, while pure Mg-olivine crystallised at a lower temperature than Mg-pyroxene. Cristobalite is observed as a high-temperature crystallite in the pure-Mg compositions. Crystallisation activation energies are derived and discussed in relation to protoplanetary disks.


2007 ◽  
Vol 661 (1) ◽  
pp. 334-353 ◽  
Author(s):  
H. Nomura ◽  
Y. Aikawa ◽  
M. Tsujimoto ◽  
Y. Nakagawa ◽  
T. J. Millar

2009 ◽  
Vol 5 (H15) ◽  
pp. 744-744
Author(s):  
Eric D. Feigelson ◽  
Philip J. Armitage ◽  
Konstantin V. Getman

The physics of protoplanetary disks and the early stages of planet formation is strongly affected by the level of ionization of the largely-neutral gas (Armitage 2009; Balbus 2009). Where the ionization fraction is above some limit around ~ 10−12, the magnetorotational instability (MRI) will ensue and the gas will become turbulent. The presence or absence of disk turbulence at various locations and times has profound implications for viscosity, accretion, dust settling, protoplanet migration and other physical processes. The dominant source of ionization is very likely X-rays from the host star (Glassgold et al. 2000). X-ray emission is elevated in all pre-main sequence stars primarily due to the magnetic reconnection flares similar to, but much more powerful and frequent than, flares on the surface of the contemporary Sun (Feigelson et al. 2007).


2007 ◽  
Vol 656 (1) ◽  
pp. 515-523 ◽  
Author(s):  
Alfred E. Glassgold ◽  
Joan R. Najita ◽  
Javier Igea

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