What powers the wind from the black hole accretion disc in GRO J1655-40?

TL;DR

This study reanalyzed data from the black hole GRO J1655-40, showing that thermal-radiative winds can explain observed features without invoking magnetic driving, challenging previous magnetic wind models and their application to quasars.

Contribution

The paper demonstrates that thermal-radiative wind models can fit the data as well as magnetic models, revising the understanding of wind launching mechanisms in black hole systems.

Findings

Cascade effects reduce inferred wind density by over an order of magnitude.

A thermal-radiative wind model matches the observational data.

Magnetic wind models struggle to reproduce the ion population at required densities.

Abstract

Black hole accretion discs can produce powerful outflowing plasma (disc winds), seen as blue-shifted absorption lines in stellar and supermassive systems. These winds in Quasars have an essential role in controlling galaxy formation across cosmic time, but there is no consensus on how these are physically launched. A single unique observation of a stellar-mass black hole GRO J1655-40 was used to argue that magnetic driving was the only viable mechanism and motivated unified models of magnetic winds in both binaries and Quasars. The alternative, X-ray heating (thermal-radiative wind), was ruled out for the low observed luminosity by the high wind density estimated from an absorption line of a metastable level of Fe xxii. Here we reanalyse these data using a photoionisation code that includes cascades from radiative excitation as well as collisions in populating the metastable level. The cascade reduces the inferred wind density by more than an order of magnitude. The derived column is also optically thick, so the source is intrinsically more luminous than observed. We show that a thermal-radiative wind model calculated from a radiation hydrodynamic simulation matches well with the data. We revisit the previous magnetic wind solution and show that this is also optically thick, leading to a larger source luminosity. However, unlike the thermal-radiative wind, it struggles to reproduce the overall ion population at the required density. These results remove the requirement for a magnetic wind in these data and remove the basis of the self-similar unified magnetic wind models extrapolated to Quasar outflows