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Resolving a Clumpy Disk Wind in 4U 1957+115 with XRISM

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Abstract

We present a high-resolution XRISM/Resolve observation of the persistent black hole candidate 4U 1957+115, revealing the first detection of an intrinsic disk wind in this source. The absorption is dominated by highly ionized Fe XXV and Fe XXVI and varies substantially throughout the observation, becoming prominent during the final ∼40\sim40 ks despite a modest decrease of only ∼5\sim5–10%10\% in source flux. The observed evolution of the absorption cannot be explained solely by ionization changes driven by the modest continuum variability, favoring an inhomogeneous outflow with evolving line-of-sight properties. Time-resolved spectroscopy reveals substantially narrower absorption features in shorter intervals, with the inferred turbulent velocity decreasing from ∼350 km/s\sim350~{\rm km/s} in the longer integration to ≲70 km/s\lesssim70~{\rm km/s} in the shortest selections. This suggests that the broader absorption profiles measured over longer integrations may result, at least in part, from averaging over an evolving wind rather than from intrinsically larger turbulent velocities. Such time averaging can therefore affect the inferred physical properties of the wind and complicate efforts to identify its launching mechanism. Even though the wind carries only a small fraction of the radiative luminosity in kinetic form, its mass-loss rate may remain dynamically relevant. These results highlight the importance of time-resolved, high-resolution X-ray spectroscopy for characterizing the structure and variability of accretion disk winds.

Introduction

Accretion disk winds are a common feature of luminous black hole (BH) X-ray binaries (XRBs) and provide a direct view of the interaction between the accretion flow and its surrounding environment. In the X-ray band, these outflows are identified as narrow absorption features from highly ionized species, often blueshifted by hundreds to thousands of km/s ([3, 4]). Their preferential detection in systems viewed at high inclination indicates that the highly ionized phase of the wind has a predominantly equatorial geometry ([4]). Additionally, winds are strongly connected to the BH XRB accretion state, with prominent ionized absorption being most commonly observed during bright, disk-dominated soft states, while the features generally weaken or disappear as sources transition toward harder states ([5, 4]). The inferred mass-loss rates can be comparable to, or even exceed, the mass accretion rate reaching the inner disk, implying that winds may influence the evolution of the accretion flow itself and potentially participate in the observed coupling between accretion states and relativistic jets ([5, 4]).

Despite their ubiquity, the physical mechanism responsible for launching these winds remains uncertain. Irradiation of the outer disk naturally produces a Compton-heated atmosphere that can become unbound at sufficiently large radii, while radiation pressure can further increase the density and velocity of such thermally driven winds ([6, 7, 8]). Thermal-radiative calculations can reproduce many of the observed properties of winds in BH XRBs, including their characteristic velocities and their strong dependence on spectral state ([8]). In contrast, the high densities and small inferred launching radii measured in some systems, most notably GRO J1655-40 and GRS 1915+105, have motivated models in which magnetic pressure or magnetocentrifugal forces play an important role ([9, 10]). The absorbing medium can also be highly dynamic, with changes in line strength, ionization, and velocity being observed from seconds to much longer timescales, reflecting both the response of the plasma to variations in the illuminating continuum and possible changes in the density or geometry of the outflow ([11, 12]). Resolving this variability is therefore essential to distinguish changes in ionization from genuine structural evolution of the wind and to determine whether the outflow is smooth, stratified, or composed of transient inhomogeneities.

High-resolution X-ray spectroscopy is essential for resolving the narrow absorption features produced by highly ionized disk winds and for measuring their velocity structure, line broadening, and ionization state. The Resolve instrument ([14]) aboard the X-Ray Imaging and Spectroscopy Mission (XRISM; [13]) provides non-dispersive microcalorimeter spectroscopy with an energy resolution of ≲5\lesssim 5 eV near the Fe K band, enabling velocity and line-profile measurements that are impossible to obtain with conventional CCD spectroscopy. This capability is particularly valuable for BH XRB winds, where Fe XXV and Fe XXVI absorption can be intrinsically narrow and variable, and recent XRISM observations have demonstrated the ability of Resolve to detect and characterize weak absorption features at Fe K energies ([15]). XRISM therefore provides a new opportunity to follow the evolution of highly ionized outflows on timescales short enough to probe changes in the structure and physical conditions of the wind.

4U 1957+115 is a persistent low-mass X-ray binary (LMXB) and BH candidate that has remained in a disk-dominated soft state throughout its observed history, displaying only weak rapid X-ray variability and a weak hard spectral component ([16, 18, 19]). Within the irradiated disk-instability model, such persistent behavior is expected when the mass-transfer rate is sufficiently high to keep the accretion disk in the hot, ionized state, and 4U 1957+115 has previously been discussed in this context ([30, 31]). The fundamental properties of the binary remain uncertain, largely because the donor star has not been directly detected and therefore no dynamical black hole mass or robust distance measurement is available. Spectral modeling generally favors a rapidly spinning black hole and a relatively high disk inclination ([18, 19, 21, 20]). Despite this combination of a persistently soft spectrum and potentially high inclination, previous high-resolution Chandra and XMM-Newton observations have not revealed a clear intrinsic disk wind, with prior detections of narrow absorption toward the source, including Ne IX and O VII, being attributed to hot gas in the Galactic interstellar medium ([17, 18]). As a result, prior to the XRISM observation presented here, there was no compelling spectroscopic evidence for a highly ionized outflow intrinsic to 4U 1957+115.

In this work, we present a high-resolution XRISM/Resolve observation of 4U 1957+115 and investigate the properties and variability of its highly ionized absorbing material. The paper is structured as follows. In § 2, we present the observation and the details of the spectral extraction pipeline used. In § 3 we present the analysis of the Resolve spectra. In particular, in § 3.1 we offer a view of the time-averaged spectrum, in § 3.2 we create a spectrogram using the observation, in § 3.3 we apply a line-search algorithm to the data, and in § 3.4 we present a time-resolved analysis of the spectra. Lastly, in § 4 we summarize our results and put them in context with the current view of the field.

Figure 1

Figure 1. Resolve and Xtend light curves of 4U 1957+115 across multiple energy bands, binned at 1 ks time resolution. The horizontal dashed lines represent the median value of each light curve, calculated over the first 40 ks of the observation (not accounting for dead time). The axes on the right show the ratio between the individual light curves and their corresponding medians.

Data

XRISM observed 4U 1957+115 on Nov 24, 2025 under ObsID 202036010 for an effective exposure of 62 ks. The data were analyzed using the standard calibration procedures1 with the tools available in Heasoft v6.36 and using CALDB version 20260315. The Resolve observation was conducted with the filter wheel open and the Xtend observation was conducted using the 1/8 window mode. The spectral analysis in this work was performed using XSPEC v12.15.1. Figure 1 shows the Resolve 2-10 keV, 7-15 keV, and Xtend 0.4-2 keV, 2-10 keV, 7-15 keV, and 0.4-15 keV light curves obtained during the observation, extracted using 1 ks time bins. The horizontal dashed lines represent the medians of the respective light curves during the first 40 ks of spacecraft time, duration chosen arbitrarily to better highlight changes in observed rates. Across data from both instruments and across different energy bands, the source flux decayed by ∼5−10%\sim5-10\% throughout the observation.

The Resolve spectra were extracted from the entire detector, with the exception of pixels 12 (calibration) and 27 (known stability issues), using only high-resolution primary (Hp) events. Throughout the analysis, we used large (L) rmf files, generated using the rslmkrmf command, after excluding low-resolution secondary (Ls) events. For each spectrum extracted throughout the analysis, we generated exposure maps using the xaexpmap command, which were subsequently used to generate arf files through the xaarfgen command. Unless otherwise noted in the text, spectra presented were rebinned using the “optimal" binning scheme in ftgrouppha ([1]). Given the brightness of the source, we did not extract background spectra for Resolve. In the Resolve 2-10 keV band, the source had an average count rate of 7 c/s. The analysis of the Xtend spectra is reserved for a follow-up publication.

Analysis

Time-averaged analysis

We extracted a time-averaged Resolve spectrum of the source, together with the L rmf file and the associated arf file. The spectrum is shown in the top panel of Figure 2, in units of keV2×(ct/s/cm2/keV)\rm keV^2\times(ct/s/cm^2/keV). An initial fit using the model TBabs×\timesdiskbb produces a good fit, with Cstat/ν=3037/2879\rm Cstat/\nu=3037/2879. The diskbb component accounts for the thermal emission originating from the accretion disk, while the TBabs component models the galactic absorption along the line of sight. However, the residuals of this fit indicate that the model does not fully capture the complexity of the spectrum. Fitting the spectrum with the model TBabs×\times(diskbb+powerlaw) produces a significantly improved fit to the continuum, with Cstat/ν=2889/2877\rm Cstat/\nu=2889/2877. The powerlaw component accounts for non-thermal emission from a compact corona. This best-fit continuum model is shown through the red line in Figure 2, and the bottom panel in Figure 2 shows the residuals of the fit in terms of Cstat. The fit measured the disk temperature to be kTin≃1.46  keVkT_{\rm in}\simeq1.46\;\rm keV, and the power-law index to be Γ≤4.9\Gamma\leq4.9. The column density along the line of sight NHN_{\rm H} was unconstrained in the fit, taking the lowest allowed value. This is likely due to a combination of limited low-energy coverage and an intrinsically small column along the line of sight, estimated around 1021  cm−210^{21}\;\rm cm^{-2} using the HEASARC Column Density tool2.

Figure 2

Figure 2. Time-averaged Resolve spectrum of 4U 1957+115. The top panel shows the spectrum (black) and the best-fit continuum model described in § 3.1, not accounting for absorption. The bottom panel shows the residuals in terms of Cstat. The vertical dashed lines show the rest energies of Fe XXV and Fe XXVI transitions.

The most striking feature when visually inspecting the residuals in Figure 2 is an absorption line around 7 keV, consistent with the rest-energy of Fe XXVI. Figure 3 shows a zoom-in version, focused around the Fe band (6.25-7.25 keV). Notably, while the absorption structure around 6.97 keV is present, no absorption features are evident around lower-ionization states of Fe. In particular, this time-averaged spectrum shows no evident absorption feature around 6.7 keV (Fe XXV). Furthermore, the spectra show no evidence of narrow Fe Kα\alpha (at 6.4 keV) or Fe Kβ\beta (at 7.06 keV) emission. Lastly, no strong Fe K edge is present in the spectra (around 7.1 keV), consistent with expectations based on the low galactic column density in the direction of the source.

Figure 3

Figure 3. Zoom in on the Fe band of the time-averaged Resolve spectrum of 4U 1957+115. The colors used are the same as in Figure 2. The absorption feature around 6.97 keV stands out in both the raw data panel and the panel showing the residuals.

Interestingly, the line which we tentatively attribute to Fe XXVI appears to be broadened. To understand whether this apparent broadening is an intrinsic effect or an artifact caused by averaging the spectrum from the entire duration of the observation, we further extracted spectra from fine time slices. This analysis is presented in the following section.

Spectrogram

To investigate the temporal evolution of spectral features, particularly the Fe-band absorption, we constructed a spectrogram of the Resolve observation. Based on the 2-10 keV light curve, we split the exposure in finely sliced time intervals according to multiple schemes. First, we set an arbitrary duration of 2ks for the spectra. Second, we split the light curve so that each good time interval (GTI) contains 10,000 Hp counts in the 2-10 keV band. Lastly, we performed the same experiment with each spectrum containing 25,000 counts. For clarity, we only present the results of the last of the three experiments, but note that all treatments produce consistent results.

Splitting the observation into intervals containing 25,000 counts produced 19 GTIs. For each interval, we extracted a spectrum and rebinned it at 3eV resolution. For simplicity, as we did not attempt to measure any fit parameters through this experiment, we used the time-averaged rmf and arf files for analyzing these spectra. We fit all 19 spectra with the same model, TBabs×\times(diskbb+powerlaw) in the 2-10 keV band and plotted the residuals, normalized by the statistical uncertainty in each spectral bin, as a function of the time elapsed during the observation and the orbital phase of the binary system. The orbital phase was computed according to the ephemeris of [2]: P=0.388879  days=9.3331  hrP=0.388879\;\rm days=9.3331\;\rm hr and T0=MJD  54621.329T_0=\mathrm{MJD}\;54621.329, with phase zero corresponding to the peak of the optical flux. The XRISM observation spans roughly three binary orbits. Figure 4 shows this spectrogram in the entire 2-10 keV band, with a 2D Gaussian smoothing applied (σ=1.3\sigma =1.3 bins in the temporal direction, and σ=2\sigma =2 in the spectral direction), for visual clarity.

Figure 4

Figure 4. Spectrogram showing contributions to Cstat in the Resolve observation of 4U 1957+115, across the 2-10 keV band. The x-axis represents photon energy, and the y-axis represents time during the observation. The y-axis on the right side of the figure shows the corresponding orbital phase of the system. The residuals are computed with respect to the TBabs*(diskbb+powerlaw) model, with bluer color indicating negative residuals and red colors indicating positive contributions. The duration of each individual time slice was selected to encompass a total of 25,000 Hp counts. The arrows at the top indicate the rest-frame energies of Fe XXV and Fe XXVI. The solid horizontal line shows the point at which the observation was split to extract the “Part 1" (before) and “Part 2" (after) spectra (see below). The horizontal dotted lines indicate the interval used for the “Narrow" spectrum. The spectrogram was smoothened, for visual clarity.

The first noticeable element in the spectrogram is an overall excess above 8.5 keV in all fits. This is likely due to the powerlaw component not fully capturing the spectral curvature, and may indicate that a more physically motivated continuum model, including relativistic reflection, could better describe this part of the spectrum. We note, however, that the dynamic range in ΔC\Delta C-stat in Figure 4 is small, and the corresponding positive residuals are not statistically significant enough to warrant the addition of a reflection component for the analysis presented here. We discuss this effect further in § 3.4.

A second feature to note is narrow, double-peaked absorption between 6.2-6.5 keV in the first ∼15\sim15 ks of the observation. The proximity of the energies at which these features appear to the neutral Fe Kα\alpha line at 6.4 keV makes it appealing for further investigation. We extracted a spectrum using only that first segment of the observation to probe this. In the unsmoothed spectra, the features appear as a series of narrow (1-2 spectral bins), low-significance absorption features at 6.27, 6.33, and 6.37 keV. Given how all these are low-significance features, and how in order for the energies they appear at to be caused by redshifted Fe Kα\alpha their velocities would need to be significantly higher than what could be inferred from their widths, we attribute these to noise in the spectra and do not further investigate their origin.

Figure 5

Figure 5. Left: spectrogram of 4U 1957+115, similar to that in Figure 4, but focused on the 6.6-7.1 keV band, with residuals calculated using a local powerlaw model. Center: Spectrogram showing the number of counts per spectral bin as a function of energy and time during the observation. Both spectrograms were smoothened for visual clarity. Right: Resolve light curves in the 2-10 keV (red) and 7-15 keV (blue) bands, with axes offset to bring the two to the same scale. The vertical dashed lines indicate the median values of the respective light curves. Across the three panels, the horizontal lines have the same meaning as in Figure 4.

The third noticeable effect is that absorption in the Fe band is not persistent, becoming most prominent only ∼70\sim70 ks after the beginning of the observation. To further assess the temporal structure of absorption in the spectra, we re-fit the 19 segments in the 6.6-7.1 keV band using a simple powerlaw model, under the assumption that locally, the spectrum is relatively flat. The left and central panels in Figure 5 show the spectrogram in the 6.6-7.1 keV band, focusing on the Fe region. The left panel shows the contribution to Cstat, similarly to Figure 4. The central panel shows the number of counts per 3 eV spectral bin. The right panel shows the Resolve light curve of the source during the observation, in the 2-10 keV band (red) and 7-15 keV band (blue). The vertical dashed lines show the median value of the light curves in the respective bands.

Figure 6

Figure 6. Top: Time-averaged (black), Part 1 (blue) and Part 2 (red) Resolve spectra, offset for visual clarity. Bottom: Local line significance resulting from the line-search algorithm using a velocity width of 500 km/s. The vertical lines show the positions of the Fe XXV and Fe XXVI resonance transitions, and the horizontal dashed lines in the bottom panel show the ±3σ\pm3\sigma significance thresholds.

Figure 5 further demonstrates the transient nature of absorption during the XRISM observation of 4U 1957+115. Therefore, moving forward, we extracted Resolve spectra from the first 69 ks of the observation (corresponding to 39 ks of effective exposure, hereafter “Part 1," shown in blue), and the remaining 39 ks segment (23 ks of effective exposure, hereafter “Part 2," shown in red), after the onset of the absorption features. We identify the time where the two segments were separated by the solid horizontal lines in Figure 4 and Figure 5. To further investigate the temporal evolution of the absorption features, we also considered shorter, 15 ks intervals throughout the observation. The strongest Fe-band absorption was identified between 75 and 90 ks, corresponding to 8.4 ks of effective exposure (indicated by the horizontal dotted lines in Figure 4 and Figure 5). We refer to the spectrum extracted from this interval as the “Narrow” spectrum and analyze its properties in § 3.4. For reference, the entire observation spanned 108 ks, with 62 ks of effective exposure. These spectra were also rebinned using the “optimal" binning scheme in ftgrouppha. The top panel of Figure 6 shows the time-averaged spectrum (black) and the two parts of the observation, displaced vertically for visual clarity.

To identify narrow absorption and emission features in the spectra, we ran a line-search algorithm on the time-averaged spectrum and on the two segments (first 69ks and last 39ks). The line search works as follows. We first fit the continuum of the spectra using the model presented above, TBabs×\times(diskbb+powerlaw). After fixing the parameters of the continuum model, we added a gaussian component to the model at fixed energies, with fixed width, and fit for the normalization of the component. The normalization was allowed to take both negative and positive values, to explore the presence of narrow absorption and emission features. After fitting and assessing the change in fit statistic, the algorithm changes the energy of the line, and repeats the process. For each spectrum, we ran the scan using four different line widths, corresponding to velocities of 50 km/s, 200 km/s, 500 km/s, and 1000 km/s. The search was performed with a resolution of 2 eV (the size of the step in energy) between 2-10 keV.

Table 2 in Appendix § 5 shows the resulting significance in terms of σ\sigma of any absorption or emission features detected in any of the three spectra. The bottom panel in Figure 6 shows the local significance derived by the search using a width of 500 km/s. Note that this significance is only local, it does not account for the look-elsewhere effect, and assumes a single free parameter (line normalization). There are few instances of significant (≥3  σ\geq3\;\sigma) detections, most appearing as absorption lines. The most significant detection (at >4.5σ>4.5\sigma) is the absorption feature at 6.974 keV in the last segment of the observation, that is consistent with Fe XXVI, as identified in § 3.1.

Additionally, an emission feature is detected across most of the velocity scans at 6.746 keV in the time-averaged spectrum and in the first segment of the observation. While this feature can be interpreted as mildly blue-shifted Fe XXV emission, it can also be interpreted as a local mischaracterization of the continuum, with the spectrogram in Figure 5 showing a mild reduction in counts (and fit statistic) around 6.7 keV, followed by an increase in flux around 6.75 keV. This effect is noticeable in the bottom panel of Figure 6, where the general significance trend (i.e., underlying residuals of the continuum) indicates a broad deviation from the zero line. This trend resembles the residuals expected to be produced by unaccounted relativistic reflection. We tested whether introducing a reflection model to our continuum impacts the overall fit and the inferred line properties by replacing the powerlaw component in our best-fit model with the relxilllp variant of the relxill family of models ([35, 36]). For the Part 2 spectrum, where the detection of the wind component was strongest, replacing the powerlaw component (Cstat/ν=2362.6/2471\rm Cstat/\nu=2362.6/2471) with relxilllp (Cstat/ν=2346.3/2464\rm Cstat/\nu=2346.3/2464) decreases the fit statistic by ΔCstat=16.3\Delta \rm Cstat=16.3 for 7 extra free parameters, representing a 2σ2\sigma improvement. However, this improvement corresponds to a decrease of 2.3 in the Akaike Information Criterion (AIC; [37]) and an increase of 38.6 in the Bayesian Information Criterion (BIC; [38]). The negligible decrease in AIC and the increase in BIC suggest that a reflection component is not statistically significant for this dataset. Nevertheless, we further tested the impact of including relativistic reflection to the model on the properties of the absorption component (see § 3.4). We found that all inferred properties of the absorption component are fully consistent, regardless of the choice of the continuum model. Therefore, we continue our analysis using the powerlaw component in our continuum model, but acknowledge that the significance levels of the narrow features reported in this section may be slightly impacted by a different continuum choice.

At lower energies, the most significant tentative detections are an absorption feature only in the first part of the observation at 2.538 keV (at 4σ\sigma for broadening under 200 km/s) and an emission feature at 2.930 keV, again identified only in the first part of the observation, favoring broadening ≥200\geq200 km/s. It is important to note that these significance calculations do not account for the look-elsewhere effect. Given the weak significance of these detections, we do not investigate the low-energy lines further, but note their tentative detection.

While scanning for a single narrow feature in the spectra can provide initial insights into possibly interesting detections, in the case of such low-significance measurements, a more physically-motivated approach could strengthen the inference. We performed a second scan of the spectra, focusing on identifying features that resemble the Fe XXV and Fe XXVI complex. The choice to focus on the two most highly ionized ions of Fe was made based on the presence of Fe XXVI absorption in the spectra, but the lack of clear signs of lower-ionization states. In this updated search, on top of the continuum, we added three zgauss components with energies fixed at the rest energies of the Fe XXV Heα\alpha and the Fe XXVI Lyα\alpha1 and Lyα\alpha2 resonance lines, and linked redshift parameter. Additionally, we linked the widths of the three lines, and set the normalization of the Lyα\alpha1 line (at 6.973 keV) to be twice that of the Lyα\alpha2 line (at 6.952 keV), while the normalization of the Fe XXV line was allowed to vary independently. We tested the same 4 broadening velocities, and varied the redshift of the entire complex of 3 lines to scan the 6-8 keV band in increments of 2 eV.

Table 3 in Appendix § 5 shows all trials that produced an improvement in fit statistic of ≥1.5  σ\geq1.5\;\sigma. The only significant detections ≥3  σ\geq3\;\sigma were obtained at z=−8.9×10−4z=-8.9\times10^{-4} (∼−270  km/s\sim-270\;\rm km/s) and z=−0.039z=-0.039 (∼−12000  km/s\sim-12000\;\rm km/s). However, the second solution is highly unlikely, with the fit identifying the 6.97 keV Fe XXVI lines as a blue-shifted version of the 6.7 keV Fe XXV line, and adjusting the normalization of its corresponding Fe XXVI lines to vanish. This experiment suggests that the spectra favor a single, slightly blue-shifted absorption layer as opposed to multiple absorption layers with different speeds and broadening.

Time- and phase-resolved analysis

Following the results of the line search, particularly the three-line experiment, we fit the Resolve spectra using the self-consistent photoionization model pion ([22, 23]). As pion is currently only available within SPEX, we used the “SPEX-to-XSPEC" 3 package ([24, 25]) to generate xspec-compatible multiplicative tables. We first fit the continuum of the source in SPEX and used it to compute pion models using an array of 10 linearly-spaced points in ionization between log⁡ξ=3−7\log\xi=3-7, 10 logarithmically-spaced points in column density between N=1021  cm−2\rm N=10^{21}\;cm^{-2} and N=1025  cm−2\rm N=10^{25}\;cm^{-2}, and 10 logarithmically-spaced points in turbulent velocity between vturb=1−104  km/sv_{\rm turb}=1-10^4\;\rm km/s. The ranges of the parameters were chosen based on preliminary fits using broader ranges and coarser spacing. We note that the use of precomputed pion tables in xspec does not allow the ionizing spectral energy distribution to respond self-consistently to changes in the fitted continuum parameters, as would be possible when fitting the continuum and photoionized absorber simultaneously in SPEX. Consequently, the inferred absorber properties depend on the assumed ionizing continuum, introducing an additional source of systematic uncertainty, particularly for the column density and ionization parameter.

We modified the previously obtained best-fit models to include the multiplicative pion component, producing the following model: TBabs ×\times pion ×\times (diskbb + powerlaw). First, we fit the Part 2 spectrum, obtaining a good fit, with Cstat/ν=2362.68/2471\rm Cstat/\nu=2362.68/2471. This represents a 4σ4\sigma detection when compared to the Cstat/ν=2387.41/2475\rm Cstat/\nu=2387.41/2475 obtained without the pion component. The pion component measures a high ionization log⁡ξ=5.8−0.5+0.3\log\xi=5.8_{-0.5}^{+0.3}, a column density NH,  PION=4.8−3.7+1.7×1023  cm−2N_{\rm H,\; PION}=4.8_{-3.7}^{+1.7}\times10^{23}\;\rm cm^{-2}, a turbulent velocity vturb=350−170+290  km/sv_{\rm turb}=350_{-170}^{+290}\;\rm km/s, and a blueshift of z=1.4−0.6+0.4×10−3z=1.4_{-0.6}^{+0.4}\times10^{-3} (420−190+150  km/s420_{-190}^{+150}\;\rm km/s), when fixing the covering fraction to 1. The uncertainties on the parameters were assessed through an MCMC analysis on the best-fit model for the Part 2 spectrum. The corner plot resulting from the analysis is shown in Figure 10 in Appendix § 7. However, it is extremely important to note that the MCMC analysis reveals a strong, nonlinear correlation between the ionization parameter and the column density of the absorbing material. At higher ionization, a broad range of column densities can reproduce the observed absorption, while lower-ionization solutions occupy a much narrower region of parameter space. Indeed, we identify an alternative solution with lower ionization (log⁡ξ=4.8\log\xi=4.8) and column density (NH=4×1022 cm−2N_{\rm H}=4\times10^{22}~{\rm cm^{-2}}), comparable to those measured in the shorter integrations (see below), that provides a virtually identical fit statistic (ΔCstat=0.05\Delta C_{\rm stat}=0.05). The relative density of MCMC samples across these regions may be influenced by the geometry of the parameter space and the efficiency with which it is explored, and should not be interpreted as evidence that the higher-ionization solution is uniquely preferred. Importantly, the turbulent and bulk outflow velocities inferred from this alternative solution remain consistent with those obtained from the original fit. Consequently, while the large column density inferred for Part 2 is not uniquely required by the data, the inferred kinematic properties appear less sensitive to this degeneracy, and physical quantities derived from the ionization and column density should be interpreted with caution.

The 6.6-7.1 keV band of the spectrum and the resulting model are shown in red in Figure 7. Figure 8 in Appendix § 6 shows the full 2-10 keV spectra for both parts of the observation. Additionally, Figure 9 in Appendix § 6 shows the 6.4-10 keV bands, and the rest-energies of strong transitions of Fe XXV, Fe XXVI, Ni XXVII, and Ni XXVIII.

Figure 7

Figure 7. Time-resolved spectra obtained from the Resolve observation of 4U 1957+115, focusing on the Fe band (6.6-7.1 keV). The “Part 1" and “Part 2" spectra (blue and red) were obtained from the first 69 ks (39 ks of effective exposure) and last 39 ks (23 ks of effective exposure), respectively. The “Narrow" spectrum (brown) was obtained from the 75-90 ks interval during the observation (8.4 ks of effective exposure). The “Phase 0" spectrum (purple) was obtained by phase-folding the observation and extracting the spectrum from a phase bin of width of 0.125 centered at 0 (effective exposure of 8.5 ks). The numbers on the y axis correspond to the Part 2 spectrum, with the other 3 spectra being offset for visual clarity. The vertical green lines indicate the rest energies of the Fe XXV and Fe XXVI transitions. The solid curves represent the best-fit models described in the paper.

To highlight the change in absorption structure, we used the best-fit model for Part 2 of the observation to fit Part 1 (shown in blue in Figure 7). Note that the addition of the pion component to the Part 1 spectrum only improves the fit at ∼0.7σ\sim0.7\sigma level, and cannot be regarded as a statistically significant detection. Nevertheless, we tested four scenarios. First, we tested whether the change in absorption features was caused by a change in ionization of the material. We fixed all the parameters in the pion component to the ones obtained using the spectrum from Part 2, but allowed the ionization to vary freely, measuring log⁡ξ≥6.4\log\xi\geq6.4 (at 1σ1\sigma confidence assessed through the xspec error function). Given the apparent lack of absorption in the Part 1 spectrum, this value would translate to an over-ionization of the obscuring material. However, comparing the lower limit of log⁡ξ≥6.4\log\xi\geq6.4 in Part 1 with the upper limit of the 1σ1\sigma confidence limit on the ionization for Part 2 of 5.8+0.3=6.1, the difference in ionization parameter for equal column density translates to a required decrease in ionizing luminosity by a factor of greater than 2 when assuming a constant density. This scenario is excluded because of the small reduction in observed flux between the two parts of the observation, on the order of 5%\% (see Figure 1).

Second, we tested whether the change can be attributed to an increase in covering fraction of the obscurer as the time in the observation progresses. Fixing all parameters in the model to the value obtained when fitting the spectrum from Part 2 except for the covering fraction (assumed to be 1 in the fit to the Part 2 spectrum) measures a covering fraction of ≤0.4\leq0.4 for the first part of the observation. Third, we tested whether the change in absorption can be attributed to a change in column density of the obscurer. Applying the same treatment but allowing only the column density to vary, we measure NH≤1.3×1022  cm−2N_{\rm H}\leq1.3\times10^{22}\;\rm cm^{-2} (≤1×1022  cm−2\leq1\times10^{22}\;\rm cm^{-2} for the alternative Part 2 solution). Lastly, we allowed all parameters of the pion model to vary. However, the weak absorption lines did not allow a significant improvement in fit statistic over any of the three fits described above. The first three scenarios produced Cstat/ν≃2690/2653\rm Cstat/\nu\simeq2690/2653, with the fourth one producing Cstat/ν≃2688/2650\rm Cstat/\nu\simeq2688/2650. All four scenarios provide statistically comparable fits, indicating that the weak or absent absorption in Part 1 can be explained by changes in ionization, covering fraction, or column density, or by a combination of these effects. However, because the absorption features are not significantly detected in Part 1, the data only constrain the range of parameter values consistent with their absence, rather than providing robust measurements of the absorber properties.

We next considered the “Narrow” spectrum introduced in § 3.2, extracted from the 75–90 ks interval. This spectrum is shown in Figure 7 and Figure 9 in brown (indicated by the label “Narrow"). Interestingly, focusing on the Fe band in Figure 7 shows that the Fe XXV and Fe XXVI lines are narrower compared to the Part 2 spectrum, and still moderately blueshifted. Notably, the Fe XXV line around 6.7 keV stands out more significantly from the continuum compared to the Part 2 spectrum. It is important to acknowledge that the “Narrow" spectrum represents a temporal subset of the “Part 2" spectrum.

Applying the same model described previously to this “Narrow" spectrum measures a significantly lower ionization log⁡ξ=4.5−0.3+0.4\log\xi=4.5_{-0.3}^{+0.4}, which, in turn, leads to a lower column density NH=4−2+7×1022  cm−2N_{\rm H}=4_{-2}^{+7}\times10^{22}\;\rm cm^{-2} through the correlation between the two parameters highlighted in the corner plot in Figure 10. As visually suggested by the widths of the lines in Figure 7, the measured turbulent velocity of the pion component is lower, but still consistent within 1σ1\sigma, compared to that of Part 2: vturb=120−80+120  km/sv_{\rm turb}=120_{-80}^{+120}\;\rm km/s. Lastly, the measured blueshift of the component is z=4±2×10−4z=4\pm2\times10^{-4} (120−60+70  km/s120_{-60}^{+70}\;\rm km/s), significantly lower compared to that measured in the Part 2 spectrum (420−190+150  km/s420_{-190}^{+150}\;\rm km/s). The lower bulk velocity of the absorption component and the reduced width compared to the one inferred from the Part 2 spectrum may suggest that, in addition to a change in column density and potentially ionization, the obscurer is experiencing significant acceleration throughout the duration of the observation, either in a linear or radial direction (i.e. orbital motion).

We also extracted spectra from the intervals immediately preceding (69–75 ks) and following (90–105 ks) the Narrow interval to investigate the evolution of the absorption. However, the addition of the wind component improves the fits at only ∼1σ\sim1\sigma and ≲2σ\lesssim2\sigma, respectively. These spectra therefore do not provide sufficient constraints to establish whether the outflow velocity evolves continuously or whether the observed differences arise from distinct absorbing structures.

To further test this hypothesis, despite the lack of clear evidence for orbital modulation in the spectrograms in Figure 4 and Figure 5, we folded the light curve of the observation on the known 9.3331 hr orbital period and extracted spectra from 8 phase bins, with each spectrum covering a phase interval of Δϕ=0.125\Delta\phi=0.125. Of the 8 phase bins, a pion component was only statistically required for the spectrum corresponding to a phase width of ±0.062\pm0.062 around phase 0 (superior conjunction - BH closer to the observer). The resulting spectrum from this phase bin (hereafter “Phase 0") is shown in purple in Figure 7 and Figure 9. For this spectrum, adding the pion component to the model improves the fit statistic by ΔCstat=41\Delta \rm Cstat=41 for 4 additional free parameters, corresponding to a detection at the 5.6σ5.6\sigma level. Notably, when focusing on this narrow band in orbital phase, despite the short 8.5 ks effective exposure within the spectrum, both the Fe XXV and the Fe XXVI doublet appear even narrower compared to either of the previous approaches at dividing the observation. For this spectrum, the pion model measures an ionization consistent with that in the “Narrow" spectrum, log⁡ξ=4.5±0.3\log\xi=4.5\pm0.3, column density NH=6−3+12×1022  cm−2N_{\rm H}=6_{-3}^{+12}\times10^{22}\;\rm cm^{-2}, and blueshift, z=4.6−0.8+1.1×10−4z=4.6_{-0.8}^{+1.1}\times10^{-4} (140−20+30  km/s140_{-20}^{+30}\;\rm km/s). However, the inferred turbulent velocity of the pion component is even lower than that of the Narrow spectrum, vturb≤70  km/sv_{\rm turb}\leq70\;\rm km/s, but still formally within 1σ1 \sigma.

The best-fit photoionization parameters obtained from the Part 2, Narrow, and Phase 0 spectra are summarized in Table 1.

ParameterPart 2NarrowPhase 0
Exposure (ks)23238.48.48.58.5
log⁡ξ\log\xi5.8−0.5+0.35.8^{+0.3}_{-0.5}4.5−0.3+0.44.5^{+0.4}_{-0.3}4.5±0.34.5\pm0.3
NH  (1022 cm−2)N_{\rm H}\;(10^{22}\,{\rm cm^{-2}})48−37+1748^{+17}_{-37}4−2+74^{+7}_{-2}6−3+126^{+12}_{-3}
vturb  (km/s)v_{\rm turb}\;({\rm km/s})350−170+290350^{+290}_{-170}120−80+120120^{+120}_{-80}<70<70
vout  (km/s)v_{\rm out}\;({\rm km/s})420−190+150420^{+150}_{-190}120−60+70120^{+70}_{-60}140−20+30140^{+30}_{-20}

Table 1. Photoionization parameters measured from the time- and phase-resolved spectra.

Results and Discussion

The main results of the XRISM/Resolve observation of 4U 1957+115 can be summarized as follows:

  • We detect the first compelling spectroscopic evidence for an intrinsic disk wind in 4U 1957+115. During the latter part of the observation, photoionization modeling measures a highly ionized absorber with log⁡ξ=5.8−0.5+0.3\log\xi=5.8^{+0.3}_{-0.5}, NH=4.8−3.7+1.7×1023 cm−2N_{\rm H}=4.8^{+1.7}_{-3.7}\times10^{23}~{\rm cm^{-2}}, and an outflow velocity of 420−190+150 km/s420^{+150}_{-190}~{\rm km/s}.

  • The wind is strongly variable. Fe-band absorption is weak or absent during the first part of the observation and becomes prominent only after ∼70\sim70 ks. The small contemporaneous change in continuum flux cannot account for this behavior through ionization alone, favoring changes in the amount or geometry of absorbing material and therefore an inhomogeneous, likely clumpy wind.

  • The absorption features become narrower in shorter integrations, indicating that unresolved variability in the wind’s velocity structure likely contributes to the apparent line broadening measured in longer integrations, rather than this broadening arising entirely from intrinsic turbulence.

  • Phase-resolved spectroscopy shows the strongest and narrowest absorption near orbital phase zero, where the pion component is detected at 5.6σ5.6\sigma and vturb≲70 km/sv_{\rm turb}\lesssim70~{\rm km/s}. However, because the observation samples only approximately three binary orbits, we do not interpret this as evidence for a strictly phase-locked wind.

The detection of a disk wind in 4U 1957+115 is notable given that previous high-resolution observations of the source found narrow absorption associated with the Galactic interstellar medium but no compelling evidence for an intrinsic outflow ([17, 18]). The highly ionized Fe XXV and Fe XXVI absorption detected with Resolve, together with its measurable blueshift and strong temporal variability, instead clearly associates the absorbing material with the binary. The absorption component is detected at 4σ4\sigma level for the “Part 2" spectrum, 4.9σ4.9\sigma for the “Narrow" spectrum, and 5.6σ5.6\sigma for the “Phase 0" spectrum. These levels of significance were estimated using an asymptotic likelihood-ratio approximation, treating the improvement in Cstat\rm Cstat as following a χ2\chi^2 distribution with 4 degrees of freedom. Because the absorber parameters are not fully identifiable under the null hypothesis of no absorption, this significance should be interpreted with caution.

The rapid appearance and disappearance of the Fe-band absorption provides important information about the structure of the wind. Similar short-timescale variability has been observed in other BH XRB disk winds. In H1743–322, Fe XXV absorption was found to vary on timescales of a few hundred seconds, with the observed changes requiring a combination of ionization and geometric effects and allowing for an interpretation in terms of a clumpy outflow ([26]). Conversely, flux-resolved spectroscopy of GRS 1915+105 demonstrated that sufficiently large changes in the illuminating continuum can produce substantial wind variability through progressive over-ionization ([27]). We tested whether the variability could be explained by changes in ionization driven solely by the observed continuum evolution. Suppressing the absorption in Part 1 requires log⁡ξ≳6.4\log\xi\gtrsim6.4, compared with log⁡ξ=5.8−0.5+0.3\log\xi=5.8^{+0.3}_{-0.5} in Part 2, implying a change in ionizing luminosity substantially larger than observed if the density and location of the absorber remain unchanged. However, because ξ=Lion/nr2\xi=L_{\rm ion}/nr^2, variations in the density or location of the absorbing material could also change its ionization state without requiring substantial continuum variability. The rapid appearance of strong Fe-band absorption therefore favors an inhomogeneous wind with evolving line-of-sight properties, potentially involving discrete clumps or a more continuously stratified outflow ([26, 10]). The present observations do not uniquely distinguish between these geometries.

The inclination of 4U 1957+115 provides an additional constraint on the geometry of the wind. Highly ionized Fe-band absorption is detected preferentially in high-inclination BH XRBs, which has motivated a predominantly equatorial wind geometry ([4]). Although the inclination of 4U 1957+115 remains uncertain, recent spectral and polarimetric studies generally favor a moderate to high inclination (50∘≲θ≲80∘50^\circ\lesssim\theta\lesssim80^\circ; [18, 19, 21, 20]). The XRISM detection is therefore broadly consistent with an equatorial wind geometry. At the same time, if the true inclination lies toward the lower end of the allowed range (≳50∘\gtrsim50^\circ), the detection would imply that the highly ionized wind has an appreciable vertical extent, or that clumpy structures can extend above the densest equatorial layers and intermittently cross the line of sight.

The progressive narrowing of the absorption features as the integration time is reduced also has implications for how line widths measured in BH XRB winds should be interpreted. During the 75–90 ks “Narrow” interval, the inferred turbulent velocity decreases to vturb=120−80+120 km/sv_{\rm turb}=120^{+120}_{-80}~{\rm km/s}, compared with 350−170+290 km/s350^{+290}_{-170}~{\rm km/s} in the longer Part 2 spectrum, while the measured bulk outflow velocity also decreases from 420−190+150420^{+150}_{-190} to 120−60+70 km/s120^{+70}_{-60}~{\rm km/s}. This suggests that at least part of the apparent broadening measured in longer integrations may arise from unresolved temporal evolution of the absorber velocity, rather than from intrinsic turbulence alone. High-resolution studies of other BH XRB winds have similarly shown multiple velocity components and time-dependent line centroids that can blend into broader features when averaged over longer intervals ([10, 3]). The Resolve spectra of 4U 1957+115 therefore highlight how time-averaged line widths may encode both microscopic broadening and macroscopic variability in the outflow.

For comparison, the expected thermal broadening of Fe ions at T=107T=10^7 K corresponds to a Gaussian velocity dispersion of σth≃39 km/s\sigma_{\rm th}\simeq39~{\rm km/s}, or a full width at half maximum of approximately 90 km/s90~{\rm km/s}. The upper limit of vturb≲70 km/sv_{\rm turb}\lesssim70~{\rm km/s} measured in the Phase 0 spectrum therefore allows only relatively modest additional turbulent broadening. This suggests that the narrowest absorption features may be close to the thermal broadening regime, while the larger widths measured in longer integrations may partly reflect unresolved bulk velocity variations rather than intrinsic turbulence.

To investigate whether orbital geometry contributes to this kinematic variability, we examined the spectra as a function of binary phase. The absorber is statistically required only in the Δϕ=0.125\Delta\phi=0.125 interval centered on phase 0, which corresponds approximately to superior conjunction of the donor star, with the compact object between the donor and the observer ([2]). In this phase interval, the pion component is detected at 5.6σ5.6\sigma and the absorption features are especially narrow, with vturb≲70 km/sv_{\rm turb}\lesssim70~{\rm km/s} and vout=140−20+30 km/sv_{\rm out}=140^{+30}_{-20}~{\rm km/s}. If this concentration of absorption at a particular orbital phase is persistent, it would imply that the absorbing material is not azimuthally symmetric around the disk, but instead occupies a preferred region in the binary frame. Such a geometry could arise from a vertically extended structure associated with the stream–disk interaction, or from an azimuthally structured disk wind in which enhanced-density material reaches the line of sight only over a limited range of orbital phase ([32, 7]). Phase-dependent velocity shifts of order ∼100 km/s\sim100~{\rm km/s} have also been reported in the disk wind of GRO J1655–40, demonstrating that orbital motion can imprint measurable Doppler shifts on wind absorption lines ([28]). However, the XRISM observation of 4U 1957+115 samples only approximately three binary orbits, and the spectrogram does not reveal an obvious repeating pattern. We therefore regard the concentration of narrow absorption near phase 0 as suggestive of orbital or azimuthal structure, rather than as evidence for a strictly phase-locked absorber.

The measured ionization and column density also constrain the characteristic location of the absorbing material. Combining ξ=Lion/nr2\xi=L_{\rm ion}/nr^2 with NH=nΔrN_{\rm H}=n\Delta r, and requiring Δr≤r\Delta r\leq r, gives rmax=Lion/(ξNH)r_{\rm max}=L_{\rm ion}/(\xi N_{\rm H}). Using the measured 0.01–100 keV ionizing flux, Fion=1.0081×10−9 erg s−1 cm−2F_{\rm ion}=1.0081\times10^{-9}~{\rm erg\,s^{-1}\,cm^{-2}}, for which

Lion=1.21×1037(d10 kpc)2erg s−1,\begin{equation} L_{\rm ion}=1.21\times10^{37}\left(\frac{d}{10~{\rm kpc}}\right)^2{\rm erg\,s^{-1}}, \tag*{(1)} \end{equation}

we obtain rmax=0.4−0.3+4.9×108  (d10)2r_{\rm max}=0.4^{+4.9}_{-0.3}\times10^{8}\; (d_{10})^2 cm for Part 2, 7−5+33×109(d10)27^{+33}_{-5}\times10^{9}(d_{10})^2 cm for the Narrow spectrum, and 8−6+16×109(d10)28^{+16}_{-6}\times10^{9}(d_{10})^2 cm for Phase 0 (where d10d_{10} represents the distance in units of 10 kpc10~\rm kpc). We caution that the particularly small radius inferred for Part 2 is sensitive to the strong degeneracy between the ionization parameter and column density discussed in § 3.4. The alternative, lower-ionization and lower-column solution, which provides a virtually identical fit statistic, yields rmax⁡≃4.7×109(d/10  kpc)2 cmr_{\max}\simeq4.7\times10^9(d/10\;{\rm kpc})^2~{\rm cm}, approximately two orders of magnitude larger than the nominal estimate and comparable to the radii inferred from the shorter integrations. Although this alternative radius remains below the characteristic thermal-launching regime for the assumed parameters, the difference illustrates the substantial model dependence of the inferred absorber location.

These values can be compared with the Compton radius, RIC=GMBHμmp/(kBTIC)R_{\rm IC}=GM_{\rm BH}\mu m_p/(k_{\rm B}T_{\rm IC}), which sets the characteristic scale for thermally driven outflows. Thermal winds can typically be launched at radii ≳0.1RIC\gtrsim0.1R_{\rm IC}, although the precise threshold depends on the illuminating spectrum, luminosity, and contribution of radiation pressure ([6, 7]). For MBH=5±1 M⊙M_{\rm BH}=5\pm1\,M_\odot ([29]) and a Compton temperature of TIC=9.3×106  KT_{\rm IC}=9.3\times10^6\;\rm K, we estimate RIC=(5±1)×1011R_{\rm IC}=(5\pm1)\times10^{11} cm. At an assumed distance of 10 kpc, the inferred upper limits on the absorber radius correspond to approximately 8×10−5  RIC8\times10^{-5}\;R_{\rm IC}, 0.014  RIC0.014\;R_{\rm IC}, and 0.016  RIC0.016\;R_{\rm IC} for Part 2, Narrow, and Phase 0, respectively. Although the nominal radius estimates remain below the characteristic thermal-launching regime, their interpretation is limited by the uncertainties in the absorber properties, particularly the degeneracy between ionization and column density in Part 2. These radius constraints, however, remain sensitive to the uncertain distance, absorber geometry, and photoionization parameters.

Several mechanisms may contribute to launching the outflow detected in 4U 1957+115. Thermal driving is one possible mechanism, since sustained X-ray irradiation can heat the disk atmosphere and launch an outflow at sufficiently large radii ([6, 7]). However, the efficiency of this process depends on the irradiating spectrum, luminosity, and location of the absorbing material. The relatively low velocities measured in the Narrow and Phase 0 spectra are also broadly consistent with predictions from thermal-wind simulations ([39]), although such velocities are not unique to thermally driven outflows. However, the inferred upper limits on absorber radius remain below the characteristic thermal-launching regime, even for these shorter intervals. Radiation pressure may contribute to the acceleration, although the high ionization of the absorbing gas makes UV line driving unlikely to be efficient, while the importance of electron-scattering radiation pressure depends on the uncertain Eddington ratio. Alternatively, magnetic pressure or magnetocentrifugal forces could accelerate material from the relatively small radii implied by our fits, as proposed for other BH XRB winds ([9, 40]). The rapid appearance of absorption despite the nearly constant continuum does not, by itself, distinguish between these mechanisms, since a persistent outflow could exhibit substantial variability in its density, ionization structure, or line-of-sight covering fraction. Thus, although the nominal radius estimates present a challenge for purely thermal driving, the uncertain geometry and physical structure of the absorber prevent us from establishing a unique launching mechanism.

An additional possibility is that the absorbing material does not constitute a freely escaping wind, but instead represents a bound disk atmosphere or a partially accelerated, potentially failed outflow. Under the adopted single-zone radius estimates, the measured line-of-sight velocities of 120−420  km/s120-420\;\rm km/s are substantially smaller than the corresponding local escape velocities. A similar discrepancy between compact inferred absorber locations and relatively slow outflows has been identified in other BH XRBs, including recent XRISM observations of 4U 1630–472, where some absorption components have been interpreted as failed winds ([41, 42]). However, the observed blueshifts measure only the line-of-sight velocity, and the absorbing material may still be accelerating or moving along trajectories substantially inclined to our viewing direction. Furthermore, the radius estimates depend on the assumed geometry and thickness of the absorbing layer, which may not adequately describe an extended or stratified wind. We therefore regard a failed wind as a plausible interpretation, rather than a necessary consequence of the measured velocities.

The inferred wind properties also allow us to estimate its mass outflow rate and kinetic power. These estimates assume a steady, radially outflowing wind; if some of the absorbing material instead forms a bound or failed outflow, the inferred mass flux would not necessarily represent net mass loss from the system. For a photoionized outflow, the mass-loss rate can be written as

M˙wind=4πCΩCVμmpLionξvout,\begin{equation} \dot{M}_{\rm wind} = 4\pi C_{\Omega} C_{\rm V}\mu m_{\rm p} \frac{L_{\rm ion}}{\xi}v_{\rm out}, \tag*{(2)} \end{equation}

where CΩ=Ω/4πC_{\Omega}=\Omega/4\pi is the global covering factor and CVC_{\rm V} is the volume filling factor. The corresponding kinetic luminosity is

Lkin=12M˙windvout2.\begin{equation} L_{\rm kin} = \frac{1}{2}\dot{M}_{\rm wind}v_{\rm out}^{2}. \tag*{(3)} \end{equation}

Using the posterior distributions of ξ\xi and voutv_{\rm out}, we infer Lkin/Lion=1.0−0.8+7.5×10−6CΩCVL_{\rm kin}/L_{\rm ion} =1.0^{+7.5}_{-0.8}\times10^{-6} C_{\Omega}C_{\rm V} for Part 2, 4.1−3.3+28.7×10−7CΩCV4.1^{+28.7}_{-3.3}\times10^{-7} C_{\Omega}C_{\rm V} for the Narrow interval, and 1.1−1.0+23.7×10−8CΩCV1.1^{+23.7}_{-1.0}\times10^{-8} C_{\Omega}C_{\rm V} for Phase 0. Thus, despite the substantial column densities inferred for the absorber, the relatively low outflow velocities imply that the wind carries only a small fraction of the radiative luminosity in kinetic form. The corresponding absolute kinetic luminosity therefore inherits the same d2d^2 dependence as LionL_{\rm ion}. If we further assume that Lbol≃LionL_{\rm bol}\simeq L_{\rm ion}, the ratio of the wind mass-loss rate to the accretion rate becomes independent of distance:

M˙windM˙acc=M˙windLionηc2.\begin{equation} \frac{\dot{M}_{\rm wind}}{\dot{M}_{\rm acc}} = \frac{\dot{M}_{\rm wind}}{L_{\rm ion}}\eta c^2. \tag*{(4)} \end{equation}

These estimates also inherit the uncertainties associated with the photoionization modeling, particularly the strong correlation between ionization and column density in Part 2. Because the mass outflow rate scales inversely with ξ\xi, alternative solutions with comparable fit statistics may yield substantially different wind energetics.

For η=0.1\eta=0.1, this gives M˙wind/M˙acc=0.10−0.06+0.22CΩCV\dot{M}_{\rm wind}/\dot{M}_{\rm acc} =0.10^{+0.22}_{-0.06}C_{\Omega}C_V, 0.41−0.25+0.69CΩCV0.41^{+0.69}_{-0.25}C_{\Omega}C_V, and 0.22−0.17+0.27CΩCV0.22^{+0.27}_{-0.17}C_{\Omega}C_V for Part 2, Narrow, and Phase 0, respectively. Since neither the global covering factor CΩC_{\Omega} nor the volume filling factor CVC_V can be independently constrained by the present observations, these estimates remain strongly dependent on the assumed wind geometry. Although the inferred clumpiness may suggest a small volume filling factor, it does not necessarily imply a small global covering factor. For the nominal spectral solutions, the inferred mass-loss rates remain below the accretion rate even when CΩCV=1C_\Omega C_V=1. However, the alternative Part 2 solution permits a substantially larger mass-loss rate, while the unknown wind geometry introduces additional uncertainty. We therefore cannot robustly determine the fraction of accreting material removed by the outflow.

This may be particularly interesting in the context of the persistent nature of 4U 1957+115. Within the irradiated disk-instability model, the source is expected to remain persistent if its mass-transfer rate is sufficiently high to keep the outer disk hot and ionized, preventing the thermal-viscous instability that drives transient outbursts ([30]). Strong wind mass loss can instead deplete the disk and shorten X-ray binary outbursts, whereas scattering of the central X-ray emission in an extended wind can enhance irradiation of the outer disk and promote its thermal stability ([33, 34]). The influence of the wind on the persistent accretion state of 4U 1957+115 therefore depends on the balance between mass loss and the additional irradiation provided by scattering in the outflow. However, neither the global wind geometry nor its scattering efficiency is constrained by the present observations, preventing us from determining whether the wind plays a significant role in maintaining the source’s persistent soft state.

Taken together, the XRISM observation reveals a disk wind in 4U 1957+115 that is highly structured in both time and velocity space. The absorber changes substantially over the course of the observation, while the shortest time- and phase-resolved spectra reveal considerably narrower Fe XXV and Fe XXVI features than those inferred from longer integrations. In particular, the turbulent velocity decreases from vturb=350−170+290 km/sv_{\rm turb}=350^{+290}_{-170}~{\rm km/s} in Part 2 to 120−80+120 km/s120^{+120}_{-80}~{\rm km/s} during the Narrow interval and to vturb≲70 km/sv_{\rm turb}\lesssim70~{\rm km/s} around phase 0. This evolution suggests that line broadening measured in time-averaged spectra may contain a contribution from unresolved changes in the velocity and structure of the absorbing material, rather than tracing intrinsic turbulence alone. The spectra also contain hints of asymmetric absorption and P-Cygni-like profiles, although neither is statistically significant when tested with additional spectral components. The combination of the spectral resolution of XRISM/Resolve with time-resolved spectroscopy therefore provides a powerful means of investigating the relative contributions of intrinsic line broadening and macroscopic wind variability. Future observations that sample multiple binary orbits with higher signal-to-noise ratios will be particularly valuable for determining whether the changes observed here arise from accelerating clumps, persistent azimuthal structure, or orbital modulation of the wind, and for searching for more subtle signatures of wind geometry and acceleration.

Acknowledgments

P.D. thanks Yerong Xu and Ciro Pinto for their help with the SPEX-to-XSPEC package. E.B. is supported by The Israel Science Foundation (Grant No. 2617/25). V.B. is supported by the National Science Foundation Graduate Research Fellowship Program (Grant No. 2141064).

The authors declare the use of generative AI in the research and writing process. According to the GAIDeT taxonomy (2026), the following tasks were delegated to GAI tools under full human supervision: Code optimization, Process automation, Visualization, Proofreading and editing the text for clarity.

The GAI tool used was ChatGPT GPT-6 Astra. Responsibility for the final manuscript lies entirely with the authors. GAI tools are not listed as authors and do not bear responsibility for the final outcomes. Declaration submitted by Paul Draghis

Line search results

Table 2 displays all energies returned through our line-search algorithm for a single gaussian feature. We are only displaying the energies for which at least one of either the time averaged, the Part 1, or the Part 2 spectra return at least one significant (≥3σ\geq 3\sigma) detection at either line width. For an in-depth explanation of the algorithm and the interpretation of the findings, see § 3.3.

Table 3 shows all redshift values of our three-line search, together with the corresponding velocity and observed energy of the Fe XXV line, for which the local significance was above 1.5σ1.5\sigma. The bold entries represent 3σ3\sigma detections. Only two values of the redshift (blueshift) produce significant detections. However, one of the two solutions is unphysical, as described in § 3.3.

Spectra

Figure 8 shows the full Part 1 and Part 2 spectra, in the entire 2-10 keV Resolve band. Other than the Fe XXVI line in the Part 2 spectrum, no other narrow emission or absorption features are immediately noticeable. This is corroborated by the result of the line-search algorithm (§ 3.3 and Appendix § 5).

Figure 8

Figure 8. Part 1 (blue, left) and Part 2 (red, right) Resolve spectra of 4U 1957+115 in the 2-4, 4-6, 6-8, and 8-10 keV, respectively. The solid lines indicate the respective best-fit models for the two spectra. Other than the Fe XXVI line around 7 keV, no narrow absorption or emission features stand out.

Figure 9 shows the spectra presented in Figure 7, but in the 6.4-10 keV band, using the same coloring and naming conventions.

Figure 9

Figure 9. 6.4-10 keV Resolve spectra, generated as splitting the observation in the same way as the one described in Figure 7. The color scheme follows that in Figure 7. The colored lines at the top show the expected positions of strong transitions of Fe XXV, Fe XXVI, Ni XXVII, and Ni XXVIII. The spectra were rebinned for visual clarity.

Corner plots

Figure 10 shows the corner plot resulting from the MCMC analysis of the Part 2, Narrow, and Phase 0 spectra. All the parameters in the TBabs ×\times pion ×\times (diskbb+powerlaw) model are shown. A strong correlation is noticeable between the ionization log⁡ξ\log\xi and the column density of the pion component NH,PIONN_{\rm H, PION}.

Figure 10

Figure 10. Corner plot resulting from the MCMC analysis of the Part 2, Narrow, and Phase 0 spectra. The color convention was maintained as in Figure 7 and Figure 9.

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