Long-term X-ray Variability of the Symbiotic System RT Cru based on Chandra Spectroscopy

TL;DR

This study analyzes long-term X-ray variability of RT Cru using Chandra spectroscopy, revealing changes in plasma temperature, obscuration, and reflection features, suggesting complex accretion and possible jet activity in this rare symbiotic system.

Contribution

First detailed spectral comparison of RT Cru across different epochs, highlighting variability in plasma temperature, absorption, and reflection components, advancing understanding of its X-ray emission mechanisms.

Findings

Higher plasma temperature in low/hard states.

Presence of a fluorescent iron line at 6.4 keV.

Soft thermal component may indicate jet activity.

Abstract

RT Cru belongs to the rare class of hard X-ray emitting symbiotics, whose origin is not yet fully understood. In this work, we have conducted a detailed spectroscopic analysis of X-ray emission from RT Cru based on observations taken by the Chandra Observatory using the Low Energy Transmission Grating (LETG) on the High-Resolution Camera Spectrometer (HRC-S) in 2015 and the High Energy Transmission Grating (HETG) on the Advanced CCD Imaging Spectrometer S-array (ACIS-S) in 2005. Our thermal plasma modeling of the time-averaged HRC-S/LETG spectrum suggests a mean temperature of $kT \sim 1.3$ keV, whereas $kT \sim 9.6$ keV according to the time-averaged ACIS-S/HETG. The soft thermal plasma emission component ($\sim1.3$ keV) found in the HRC-S is heavily obscured by dense materials ($> 5 \times 10^{23}$ cm$^{-2}$). The aperiodic variability seen in its light curves could be due to changes in either absorbing material covering the hard X-ray source or intrinsic emission mechanism in the inner layers of the accretion disk. To understand the variability, we extracted the spectra in the "low/hard" and "high/soft" spectral states, which indicated higher plasma temperatures in the low/hard states of both the ACIS-S and HRC-S. The source also has a fluorescent iron emission line at 6.4 keV, likely emitted from reflection off an accretion disk or dense absorber, which was twice as bright in the HRC-S epoch compared to the ACIS-S. The soft thermal component identified in the HRC-S might be an indication of a jet that deserves further evaluations using high-resolution imaging observations.