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Magnetically Aligned Striations in the L914 Filamentary Cloud

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Published 2024 March 26 © 2024. The Author(s). Published by the American Astronomical Society.
, , Citation Li Sun et al 2024 AJ 167 176 DOI 10.3847/1538-3881/ad2ea3

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Abstract

We present CO(J = 1–0) multiline observations toward the L914 dark cloud in the vicinity of the Cygnus X region, using the 13.7 m millimeter telescope of the Purple Mountain Observatory. The CO observations reveal in the L914 cloud a long filament with an angular length of ∼3fdg6, corresponding to approximately 50 pc at the measured distance of ∼ 760 pc. Furthermore, a group of hair-like striations are discovered in two subregions of the L914 cloud, which are connected with the dense ridge of the filament. These striations display quasiperiodic characteristics in both the CO intensity images and position–velocity diagrams. Two of the striations also show increasing velocity gradients and dispersions toward the dense ridge, which could be fitted by accretion flows under gravity. Based on the Planck 353 GHz dust polarization data, we find that the striations are well aligned with the magnetic fields. Moreover, both the striations and magnetic fields are perpendicular to the dense ridge, constructing a bimodal configuration. Using the classic method, we estimate the strength of the magnetic field and further evaluate the relative importance of gravity, turbulence, and the magnetic field, finding that the L914 cloud is strongly magnetized. Our results suggest that magnetic fields play an important role in the formation of filamentary structures by channeling the material along the striations toward the dense ridge. The comparison between the observations and simulations suggests that striations could be a product of the magnetohydrodynamic process.

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1. Introduction

The universality of filamentary structures in molecular clouds has been revealed by multiwavelength surveys (see, e.g., Schneider & Elmegreen 1979; Molinari et al. 2010; Schuller et al. 2017; Yuan et al. 2021). Herschel observations suggest that filaments play an important role in connecting molecular clouds to star formation (André et al. 2014). Nevertheless, the physical mechanisms relevant to the formation and evolution of filaments are complex. The interactions of gravity, turbulence, thermal pressure, and magnetic field and their relative importances remain a subject of debate (see, e.g., Inutsuka & Miyama 1992; Padoan et al. 2001; Hennebelle 2013; Gómez & Vázquez-Semadeni 2014).

Large-scale ordered striations may help us to understand the physical processes leading to the formation of filamentary structures (see the reviews in Hacar et al. 2023 and Pineda et al. 2023). Striations were first identified by Goldsmith et al. (2008), who discovered a string of hair-like structures with a large dynamic range of CO mapping in the Taurus region. The polarization measurements reveal that these striations are well aligned with the projected magnetic field. The subsequent Herschel observations at the same region found the perpendicular striations connecting to the crest of the B211 filament and led to the view that the filament is accreting material through the striations (Palmeirim et al. 2013; Shimajiri et al. 2019). The molecular striations were also discovered in the Musca (Cox et al. 2016), L1642 (Malinen et al. 2014, 2016), and Polaris (Panopoulou et al. 2016) clouds, etc.

In addition to molecular clouds, striations are also observed in the diffuse atomic medium (e.g., McClure-Griffiths et al. 2006; Tritsis et al. 2019). These structures are observed to be ordered, quasiperiodic, and well aligned with the plane-of-sky (POS) magnetic field (e.g., Heyer et al. 2008, 2016; Panopoulou et al. 2016; Soler 2019). With these striking features, it is natural to conjecture that the striation structures are the result of material flowing along magnetic field lines (Goldsmith et al. 2008; Palmeirim et al. 2013). The analysis of velocity fields and line excitation in Taurus suggests either Kelvin–Helmholtz instability or magnetohydrodynamic (MHD) waves as the origins of Taurus striations (Heyer et al. 2016). Alternatively, Chen et al. (2017) proposed that the striations are the corrugations of sheets caused by the thin-shell instability. Nevertheless, due to the extremely small sample of the observed striations, it is still difficult to set strong constraints on the theoretical models and simulations. Therefore, it is of importance to search for more filaments associated with striations, in order to better understand the formation mechanism of filaments.

The L914 cloud is a dark nebula first listed in Lynds (1962). It was covered by the 13CO survey with the two 4 m millimeter telescopes at Nagoya University (Dobashi et al. 1994). In the 13CO observations, the L914 cloud showed an elongated structure overall. In this work, we present higher-resolution CO observations toward the L914 cloud, as part of the Milky Way Imaging Scroll Painting (MWISP) project, 4 which is an unbiased CO (J = 1 − 0) multiline survey toward the northern Galactic plane using the 13.7 m millimeter telescope of the Purple Mountain Observatory (PMO; Su et al. 2019; Sun et al. 2021). Additionally, complementary dust polarization data from Planck are also used. The observations and data reduction are introduced in Section 2. In Section 3, we present the observational results and report the discovery of a long filament associated with magnetically aligned striations. In Section 4, we evaluate the balance between the magnetic field, turbulence, and gravity in the L914 cloud and discuss the potential mechanisms involved in the formation of the filamentary structures, as well as diffuse striations. The main conclusions are summarized in Section 5.

2. Observations

2.1. PMO 13.7 m CO observations

The CO observations toward the L914 cloud covered a region within 81° ≤ l ≤ 84° and −3° ≤ b ≤ −1°. The observations were conducted with the PMO 13.7 m millimeter telescope located in Delingha, China, from 2012 March to 2018 May. The nine-beam Superconducting Spectroscopic Array Receiver (Shan et al. 2012) was used as the front end, and the 12CO, 13CO, and C18O J = 1 − 0 emission lines were simultaneously observed in the sideband separation mode. The upper sideband (USB) contains the 12CO line and the lower sideband (LSB) contains the 13CO and C18O lines. The half-power beamwidth was ∼55'' at 110 GHz and ∼52'' at 115 GHz. The typical system temperature was ∼275 K for 12CO and ∼155 K for 13CO and C18O. A fast Fourier-transform spectrometer was used as the back end, which has a total bandwidth of 1 GHz and contains 16,384 channels. The corresponding velocity resolution is 0.16 km s−1 for the 12CO line and 0.17 km s−1 for the 13CO and C18O lines, respectively. The observed area is divided into individual $30^{\prime} \times 30^{\prime} $ cells. Each cell was observed in the on-the-fly mode with a scanning rate of 50'' per second and a dump time of 0.3 s. The scanning interval was 15'' (50'' s−1 × 0.3 s). To reduce the scanning effects, each cell was mapped along both the Galactic longitude and latitude.

We calibrated the antenna temperature (TA) with the standard chopper wheel method (Ulich & Haas 1976). The main-beam temperature (Tmb) was derived from the antenna temperature (TA) using the equation of Tmb = TA/Beff, where the main-beam efficiencies (Beff) were approximately 44% for the USB and 48% for the LSB during the observations. The calibration errors were estimated to be within 10%.

The raw data were reduced by the MWISP working group with the GILDAS software 5 and self-developed pipelines. After eliminating the abnormal data, we mosaicked the data cubes ($30^{\prime} \times 30^{\prime} $ FITS) of cloud regions and regridded the maps into 30'' × 30''. The typical rms noise level was below ∼0.5 K for 12CO at a channel width of 0.16 km s−1 and below ∼0.3 K for 13CO and C18O at a channel width of 0.17 km s−1. All velocities given in this work are relative to the local standard of rest (LSR).

2.2. Planck 353 GHz Observation

To investigate the magnetic field of the L914 cloud, we retrieved dust polarization data from the Planck Legacy Archive. 6 The Planck all-sky survey (Planck Collaboration et al. 2011) observed the linear polarization in seven bands from 30 to 353 GHz, of which the 353 GHz band was the most sensitive for detecting dust polarization (Planck Collaboration et al. 2015). Additionally, the cosmic microwave background does not significantly contribute to polarized emission in this band when observing molecular clouds (Soler 2019). Therefore, Planck 353 GHz submillimeter polarization data were used in this work to trace magnetic fields. The original maps have a resolution of $4\buildrel{\,\prime}\over{.} 8$ in the HEALPIX 7 format, with a pixelization at Nside = 2048, which corresponds to a pixel size of $1\buildrel{\,\prime}\over{.} 7$. We smoothed the maps into $10^{\prime} $ to increase the signal-to-noise ratio of the extended regions, as suggested by Planck Collaboration et al. (2016). The polarization position angle (PA) is calculated with

Equation (1)

where θPA is given in the IAU convention, i.e., θPA = 0° points to the north and θPA increases counterclockwise. The orientation of the magnetic field is perpendicular to the PA, ${\theta }_{{\rm{B}}}={\theta }_{\mathrm{PA}}-\tfrac{\pi }{2}$.

3. Results

3.1. L914: A Filamentary Molecular Cloud with Striations

Figure 1 presents an overview of the Cygnus X region in the MWISP 13CO observations. The integral velocity interval is [−100, 40] km s−1. Around the center of the Cygnus X region (the Cyg OB2 cluster), there are many bright filamentary molecular clouds, and a lot of research has focused on these molecular clouds over the past few decades (e.g., Schneider et al. 2010; Cao et al. 2022; Gong et al. 2023; Li et al. 2023). However, the relatively isolated L914 molecular cloud located at the periphery of this region has received little attention. The 13CO J = 1 − 0 survey from the Nagoya 4 m millimeter telescope ($\sim 2\buildrel{\,\prime}\over{.} 7$ in angular resolution) showed an elongated structure of the L914 cloud at the velocity range of ∼[1, 6] km s−1 (Dobashi et al. 1994). The enlarged view in Figure 1 displays the three-color image of the MWISP CO data toward the L914 cloud, with 12CO emission shown in blue, 13CO in green, and C18O in red. Based on the higher-angular-resolution MWISP CO data, we reveal a long filamentary structure in the L914 cloud.

Figure 1.

Figure 1. Top: overview of the Cygnus X region in the MWISP 13CO observations (Zhang et al. 2024), which is integrated over the velocity range of [−100, 40] km s−1. Bottom: three-color image of the 12CO (blue), 13CO (green), and C18O (red) emission toward the L914 cloud. The integral velocity intervals for the individual lines are the same as in Figure 3.

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Figure 2 shows the velocity channel maps of the MWISP CO emission toward the L914 cloud. The grayscale background represents the 12CO emission, with the overlapped green and magenta contours showing the 13CO and C18O emission, respectively. As shown in this image, the L914 cloud is detected in the velocity range from ∼0 to 7 km s−1. The two ends of the filament appear in the velocity channel ranging from roughly 1 to 4 km s−1, whereas the central part is predominantly observed in about [3, 6] km s−1. The integrated intensity maps of 12CO, 13CO, and C18O are shown in Figure 3, where the three molecular lines are integrated over the velocity ranges of [0, 7], [0, 6], and [0.5, 5.5] km s−1, respectively. Compared with 12CO and 13CO, the C18O line traces much denser regions. Figure 3(c) shows that the L914 cloud has strong C18O emission along the filament. We adopt the Discrete Persistent Structure Extractor (DisPerSE; Sousbie 2011) algorithm on the C18O data for the dense ridge extraction. As the DisPerSE algorithm extracts persistent structures by connecting topological critical points (e.g., maximum, minimum, and saddle points), it is susceptible to local extrema. We thus smooth the C18O data to 75'' before extraction. In DisPerSE, the persistence and robustness thresholds are set to be 2 and 0.8 K km s−1 (σ ∼ 0.25 K km s−1; see the DisPerSE 8 website for more details). The results obtained from DisPerSE are further visually inspected in the integrated intensity map and minor adjustments have been applied according to the 3σ contour. The resulting ridge is depicted in Figure 3 with the solid cyan lines. Figure 4 presents the position–velocity (PV) map along the ridge from left to right. The structure extends more than 3fdg6 in length (i.e., ∼50 pc at a distance of 760 pc; see below), showing continuous and strong emission in both the 12CO and 13CO lines.

Figure 2.

Figure 2. Velocity-integrated channel maps of the 12CO (grayscale background), 13CO (lime contours), and C18O (magenta contours) line emission. The integrated velocity range is marked in the bottom right corner of each panel in units of km s−1. The 13CO contours start at 1 K km s−1 and increase with a step of 1 K km s−1 (σ ∼ 0.15 K km s−1). The C18O contours start at 0.5 K km s−1 and increase by 0.5 K km s−1 (σ ∼ 0.15 K km s−1).

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Figure 3.

Figure 3. Velocity-integrated intensity maps of 12CO, 13CO, and C18O (from top to bottom) toward the L914 cloud. The integral interval is labeled at the top right corner of each panel. The cyan line in each panel represents the ridge of the L914 filamentary cloud identified by the DisPerSE algorithm using the C18O data.

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Figure 4.

Figure 4. CO PV image along the ridge of the L914 filamentary cloud (from east to west). The grayscale background represents the 12CO emission. The lime and pink contours represent the 13CO (levels = 0.75, 1.75, 2.75 K; σ ∼ 0.15 K) and C18O (levels = 0.5, 1.0, 1.5 K; σ ∼ 0.15 K) emission, respectively.

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Interestingly, as seen in Figure 2, distinct 12CO and 13CO hair-like structures are discovered in the velocity channels of [4, 5] and [1, 2] km s−1, located in the central and right parts of the L914 cloud, respectively. We zoom in on these two parts and carefully choose the velocity ranges that could clearly detect the structures for integration. The 12CO narrow velocity-integrated intensity maps are shown in Figure 5, with the integrated velocity ranges of [4, 6] and [0, 2] km s−1, respectively. As seen below, these hair-like structures display quasiperiodic characteristics and also parallel the magnetic lines derived from the Planck dust polarization (see Section 3.3.1), and therefore are identified as striations in this work (see the definition suggested by Hacar et al. 2023).

Figure 5.

Figure 5.  12CO striations revealed in different velocity channels. The striations found in the [4, 6] km s−1 velocity range are located in the central part of the L914 cloud, while the striations in [0, 2] km s−1 are situated in the western region. The blue solid line shows part of the dense ridge related to the striations, which is identified with the DisPerSE algorithm. The green rectangle demonstrates the slice used for intensity profile plotting (see Figure 6). The magenta arrow line shows the path used for the PV map (see Figure 7).

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To investigate the periodicity of the striations, we present profiles of the averaged integrated intensity along the directions (the arrow lines in Figure 5) perpendicular to the striations in Figure 6. The blue solid lines are the original averaged intensity and the dotted orange lines show the profiles after smoothing. We mark the local peaks of the smoothed intensity as the positions of the 12CO striations. In the central part, four 12CO striations are observed and it is evident that the spacing between the striations gradually decreases from left to right, ranging from about 1.4 to 0.6 pc, with a mean value of ∼1.1 pc. In the right part, six 12CO striations are found to show a quasiperiodic pattern with a period T of about 1.4 pc. Given that the striations are likely in a plane inclined to the POS by an angle of θ, the actual period is determined as $T/\cos (\theta $). Here, we only set a lower limit for the oscillation period. Additionally, in the right part, quasiperiodic oscillation is also observed in the velocity dispersions of both the 12CO and 13CO spectra (see Figure 7). The red dashed lines in Figure 7 show the sinusoidal function with a period of ∼1.4 pc. We assign the 12CO striations S1–S10 from left to right. The contrast between the striation and its surroundings can be estimated with $\tfrac{{I}_{\max }-{I}_{\min }}{{I}_{\max }}$, where ${I}_{\max }$ and ${I}_{\min }$ represent the local maximum and minimum of the integral intensity, respectively. The mean contrasts in these two parts are ∼12% and 28%, respectively. Since the 12CO emission is relatively diffuse, it is difficult to obtain the path of the striation skeleton. We thus choose the striations with prominent 13CO emission to do the ridge extraction. We present the 13CO narrow velocity-integrated intensity maps of these two regions in Figure 8. The integrated velocity ranges are [4.5, 5.1] and [1.5, 2.4] km s−1, respectively. According to the morphology of 3σ contours, we identify the ridges for the striations S1–S6 in the 13CO images.

Figure 6.

Figure 6. Profiles (blue solid lines) of averaged intensity along the directions perpendicular to the striations (magenta arrow lines in Figure 5). The orange dotted line shows the profile after applying a low-pass noise filter. The green and red dots represent the local maxima and minima, respectively.

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Figure 7.

Figure 7. PV maps along the arrow line shown in Figure 5(b). The top two panels depict the 12CO emission, while the bottom two panels display the 13CO emission. The 12CO contours start at 1 K and increase in steps of 1 K (σ ∼ 0.3 K). The 13CO contours start at 0.3 K with an increasing step of 0.6 K (σ ∼ 0.1 K). The blue dashed lines in the first and third panels indicate the velocity ranges, which are magnified in the second and fourth panels, respectively. The red dashed line shows the "by-eye" fitting of sine waves to the oscillating velocity dispersion, with an oscillation period of T ∼ 1.4 pc. The vertical arrow lines mark the positions of striations according to the local peaks of the 12CO emission (see Figure 6).

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Figure 8.

Figure 8.  13CO narrow velocity-integrated integral maps of the striations. The grayscale backgrounds represent the integrated intensity of the 13CO emission with integrated velocity ranges of [4.5, 5.1] and [1.5, 2.4] km s−1, respectively. The contour levels are at 0.75, 1.5, and 2.25 K km s−1 (σ ∼ 0.25 K km s−1). Striations S1–S6 (see Section 3.1) are shown with red dotted lines. The blue solid line represents the dense ridge (the same as Figure 5).

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3.2. Properties of Filamentary Structures

The distance of the L914 cloud listed in previous work is about 800 pc (Dobashi et al. 1994), which is estimated through the spectrophotometry of the nearby stars. In this work, we measure the distance of the cloud based on the MWISP CO data and Gaia Data Release 3 (DR3) data (Gaia Collaboration et al. 2023), using the same method as described in Yan et al. (2019). The details of the distance measurement are presented in the Appendix and a distance of 760 pc is obtained to the L914 cloud.

The optical depth of the 12CO J = 1 − 0 line is estimated with the MWISP 12CO and 13CO data. Assuming that 12CO and 13CO have the same excitation temperature and beam-filling factor, we calculate the optical depth of 12CO as follows:

Equation (2)

where T(12CO), T(13CO), and τ are the peak intensity of the 12CO and 13CO spectra and the optical depth of 12CO, respectively. Ri represents the isotopic ratio of 12CO/13CO, derived from the relation [12C/13C] = 4.08DGC + 18.8 (Sun et al. 2024). In this equation, DGC denotes the Galactocentric distance and the isotopic ratio is estimated to be Ri ∼ 52 for the L914 cloud. The calculated optical depth (τ) varies from approximately 15 in the outskirts of the cloud to around 60 at the densest positions. The mean value of τ, approximately 32, suggests that the 12CO emission is optically thick in the L914 cloud.

We further convert the main-beam brightness temperature TMB of 12CO to the excitation temperature Tex under the assumption of local thermodynamic equilibrium (LTE) with the following formula:

Equation (3)

where Tbg = 2.7 K is the background temperature, J is the radiation temperature, and ${J}_{\nu }(T)={T}_{0}/[{e}^{(h\nu /{k}_{{\rm{B}}}T)}-1]$, where T0 is the intrinsic temperature of 12CO and T0 = h ν/kB, kB and h are the Boltzmann constant and Planck constant, respectively. We analyze the pixels with an integrated intensity of 13CO larger than 1 K km s−1 ( ∼ 3σ) and find that the Tex in L914 ranges from 6 to 15 K, with a mean value of ∼10 K. We further assume a uniform Tex of CO and its isotopologues. The optical depth and column density of 13CO can be calculated as follows (Bourke et al. 1997):

Equation (4)

Equation (5)

The abundance ratios of H2/12CO ≈ 1.1 × 104 (Frerking et al. 1982) and 12C/13C ≈ 52 (Sun et al. 2024) are used to calculate the H2 column density. The column density map is displayed in Figure 9. The column densities of the dense ridge and diffuse striations are N(H2) ∼ 5–7 × 1021cm−2 and N(H2) ∼ 1–3 × 1021cm−2, respectively. As seen in Figure 9, the striations appear to be connected with the densest parts of the skeleton.

Figure 9.

Figure 9. H2 column density map calculated with the 13CO emission. The blue contours show the density levels of 1, 3, 5, and 7 × 1021 cm−2. The cyan contours show the C18O integrated intensity with levels at 0.3, 0.9, 1.5, and and 2.1 K km s−1. The purple, orange, and lime lines represent the segments in Section 3.3.1.

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We employ the Gaussian model in the Python package RadFil (Zucker & Chen 2018) to fit the column density profiles of the L914 filament and estimate the deconvolved width (${\mathrm{FWHM}}_{\mathrm{dec}}\,=\,\sqrt{{\mathrm{FWHM}}^{2}-{\mathrm{HPBW}}^{2}}$) of the filament. Assuming that the filamentary structure is a long cylinder, the line mass, volume density, and average column density can be calculated with the equations of Mline = μmHN(r)dr, $n=\tfrac{{M}_{\mathrm{line}}}{\pi {r}^{2}}$, and $\overline{N}=\tfrac{{M}_{\mathrm{line}}}{2\times r}$, where μ, mH, and r are the mean molecular mass, the hydrogen atom mass, and the radius of the filament, respectively. With the same method, we also calculate the properties of the six striations (S1–S6) identified in Section 3.1. All properties of the filamentary structures are listed in Table 1. The estimated width, line mass, and volume density of the L914 filament are ∼1 pc, 80 M pc−1, and 1300 cm−3, respectively. The L914 filament is thermally supercritical, with the line mass much larger than the critical equilibrium value for an isothermal cylinder (Mline, crit ∼ 17 M pc−1 at a gas temperature of 10 K, derived from ${M}_{\mathrm{line},\ \mathrm{crit}}=2{c}_{{\rm{s}}}^{2}/{\rm{G}}$; Ostriker 1964). The mean width of the striations is about 0.5 pc, which is half that of the L914 filament. The line masses of the striations range from 3 to 12 M pc−1, with a mean value of ∼8 M pc−1. All the striations are thermally subcritical. Unless additional pressure is supplied (such as magnetic compression), these striations are expected to disperse. Considering that striations can be so tenuous that they can easily be affected by surrounding material, large uncertainties will inevitably be introduced into the calculations.

Table 1. Properties of Filamentary Structures

Name Npeak WidthLength Mline n $\overline{N}$ Mtot Orientation
 (1021 cm−2)(pc)(pc)(M pc−1)(cm−3)(1021 cm−2)(M)(degrees)
Fil3.94 ± 0.31.06 ± 0.248.5 ± 0.177 ± 161300 ± 3003.20 ± 1.03700 ± 800
S10.76 ± 0.10.44 ± 0.14.6 ± 0.16 ± 2560 ± 2000.60 ± 0.128 ± 9–120 ± 12
S21.34 ± 0.10.50 ± 0.23.7 ± 0.112 ± 5870 ± 3601.06 ± 0.144 ± 19–138 ± 22
S30.47 ± 0.10.33 ± 0.24.7 ± 0.13 ± 2500 ± 3600.40 ± 0.114 ± 9–129 ± 18
S40.80 ± 0.20.38 ± 0.24.6 ± 0.16 ± 4760 ± 4000.70 ± 0.228 ± 19–129 ± 23
S50.99 ± 0.10.68 ± 0.26.6 ± 0.112 ± 4500 ± 2200.78 ± 0.179 ± 26–138 ± 12
S60.83 ± 0.20.46 ± 0.25.8 ± 0.17 ± 4600 ± 3600.67 ± 0.240 ± 24–141 ± 4

Note. Properties of the filamentary structures. Column (1): the names of the L914 filament and striations. Columns (2) and (3): the peak column density and width obtained from the Gaussian fitting. Column (4): the length of the structure. Columns (5)–(8): the line mass, volume density, averaged column density, and total mass. Column (9): the orientation angle of the filamentary structure, measured counterclockwise from Galactic north in degrees.

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3.3. Magnetic Field Traced by Planck Dust Polarization

3.3.1. Field-structure Orientation

The POS magnetic field can be derived with the Planck data based on the assumption that the short axis of the dust grains is well aligned with the local direction of the magnetic field (Andersson et al. 2015). Figure 10 shows the inferred magnetic field overlaid on the MWISP 13CO zeroth-moment image. In the left part of L914, the magnetic field aligns well with the dense skeleton. However, in the central and right parts, the magnetic field appears to display a sharp turn, becoming perpendicular to the dense skeleton and parallel to the diffuse striation structures. In order to quantify the relative orientation between the magnetic field and the filamentary structures, we first present the distribution of the polarization PAs in Figure 11, from which the PAs can be visually divided into three groups. We perform a multicomponent Gaussian function fitting on the PA distribution and obtain mean values of ∼29fdg6, −44fdg2, and −63fdg9, with 1σ dispersions of ∼5fdg03, 7fdg56, and 4fdg23, for the three components C1, C2, and C3, respectively. The first component C1 (the purple shadow in Figure 11) covers a range of PAs from ∼9° to 50° and corresponds to the marked region "R1" in Figure 10. The second component (C2; orange shadow) ranges from ∼ −52° to −14° and the corresponding area is "R2." The third component (C3; green shadow) spans from ∼ − 81° to −52° and is located to the right of L914, i.e., region "R3." The global B-field orientation, denoted as θB , can be derived from the PA, using the formula ${\theta }_{B}={\overline{\theta }}_{\mathrm{PA}}-\tfrac{\pi }{2}$.

Figure 10.

Figure 10. POS magnetic field overlaid on the MWISP 13CO integrated intensity map. The colorful background shows the 13CO emission, integrated over the velocity range of 0–6 km s−1. The "drapery" pattern, produced with the line integral convolution method (Cabral & Leedom 1993), indicates the orientation of magnetic field lines derived from Planck dust polarization data. The colorful contours show three subregions with different polarization PAs (see Figure 11).

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Figure 11.

Figure 11. Statistics of polarization PAs (red step line). The blue dashed line shows the fitting result with a multicomponent Gaussian function. The green, orange, and blue shadow areas represent the angle ranges of the three components, respectively.

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As for the structure orientation, we first roughly break the L914 filament into three segments (Seg1–Seg3 in Figure 9) according to the distribution of dust polarization PAs illustrated in Figures 10 and 11. We then employ cubic polynomial fitting to smooth the path of each filamentary structure (segments and striations) and compute the derivative at each point along the trajectory. The mean tangential angle along each path is adopted as the structure orientation. The structure orientations of Seg1–Seg3 also adhere to the IAU convention (see Section 2.2), with orientation angles of −88° ± 18°, −77° ± 23°, and −66° ± 12° for Seg1, Seg2, and Seg3, respectively. Figure 12 presents the relative orientations of the projected magnetic fields Bpos with respect to the dense segments and diffuse striations. As seen in this image, the magnetic fields in R2 and R3 are indeed parallel to the hair-like structures, which is consistent with the definition of striations (see Section 3.1). Moreover, a bimodal configuration is shown in subregions R2 and R3.

Figure 12.

Figure 12. Relative angles between B-fields and filamentary structures. The colorful dots show the relative orientations of segments and large-scale B-fields, while the distribution of striations is represented by the colorful squares. The blue and orange shadow areas represent the regions that are within 30° from parallelism and perpendicularity, respectively.

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3.3.2. Strength of Magnetic Field

The strength of the magnetic field projected onto the POS (Bpos) can be estimated with the Davis–Chandrasekhar–Fermi (DCF; Davis 1951; Chandrasekhar & Fermi 1953) method. Under the assumption that the observed dispersion of the polarization PAs is purely caused by incompressible and isotropic turbulence, the magnetic field strength is estimated as

Equation (6)

where ρ is the volume density (ρ ∼ 1300 cm−3; see Section 3.2), σturb is the one-dimensional nonthermal velocity dispersion, σθ is the dispersion in polarization PA, and Q is the correction factor. The three-dimensional numerical MHD simulations in Ostriker et al. (2001) suggest that the correction factor of Q = 0.5 should be applied to the DCF formula when the dispersion of PAs is less than ∼25°, which is applicable for our samples (see Figure 11). The uncertainty of the Q factor is 30% (Crutcher et al. 2004).

The PA dispersion has been derived in Section 3.3.1. We further evaluate the nonthermal velocity dispersion (σturb) with 13CO data by eliminating the thermal portion (σth) from the observed velocity dispersion (σobs):

Equation (7)

where the thermal velocity dispersion is determined by ${\sigma }_{\mathrm{th}}\,=\sqrt{\tfrac{{k}_{{\rm{B}}}{T}_{\mathrm{kin}}}{{m}_{\mathrm{obs}}}}$, where mobs is the mass of the 13CO molecule (mobs = 29 amu) and Tkin is the gas kinematic temperature, for which we adopt the excitation temperature estimated from the 12CO emission, under the assumption of LTE (see Section 3.2). The estimated median of σth is ∼0.05 ± 0.01 km s−1 for all three regions, which is too small and therefore negligible compared to σobs. The effect of opacity (τ) broadening on the velocity dispersion can be estimated by referring to (see, e.g., Phillips et al. 1979; Hacar et al. 2016)

Equation (8)

where σobs and σint are the observed and intrinsic velocity dispersions, respectively. As the opacity reaches 0.6, the contribution of opacity broadening can reach up to 10%. According to Equation (4), we find that more than 30% of the pixels in the L914 cloud have 13CO optical depth greater than 0.6. Therefore, the optical depth correction is necessary. In Equation (8), we adopt the intensity-weighted velocity dispersion σobs to calculate σint. Figure 13 presents the distributions of σint, with mean values of ∼0.6, 0.5, and 0.4 km s−1 for subregions R1, R2, and R3, respectively.

Figure 13.

Figure 13. Distribution of the one-dimensional velocity dispersion in the three subregions.

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With Equation (6) and all the parameters obtained above, the magnetic field strengths are estimated to be ∼101 ± 71, 54 ± 27, and 75 ± 45 μG for regions R1, R2, and R3, respectively (see Table 2). Since the angular resolution of Planck data is $\sim 10^{\prime} $, any disordered structures smaller than the beam size will be smoothed and result in an overestimate of Bpos. Also, if we use the critical density of CO J = 1 − 0 (∼1000 cm−3; see Yang et al. 2010) at the kinematic temperature of 10 K to calculate Bpos, the estimated strength will be 88, 47, and 66 μG, respectively. Additionally, we attempt to estimate the magnetic field strength using the modified DCF method (the ST method: ${B}_{\mathrm{pos}}=\sqrt{2\pi \rho }\tfrac{{\sigma }_{{\rm{v}}}}{\sqrt{{\sigma }_{\theta }}}$; see Skalidis & Tassis 2021; Skalidis et al. 2021), which takes into account both the anisotropy and compressibility of turbulence. The estimated strengths of the magnetic field are 42, 28, and 29 μG in the three subregions, nearly half of the DCF results. However, as mentioned in Skalidis & Tassis (2021), the ST method will underestimate the magnetic field strength for regions where self-gravitation is non-negligible. We thus consider the results from the ST method as a lower limit of Bpos.

Table 2. Properties of Subregions

Region δ V δ θ Bpos (DCF) Bpos (ST) λobs (DCF) λobs (ST) ${V}_{{\rm{A}},3{\rm{D}}}^{\mathrm{DCF}}$ ${V}_{{\rm{A}},3{\rm{D}}}^{\mathrm{ST}}$ ${M}_{{\rm{A}}}^{\mathrm{DCF}}$ ${M}_{{\rm{A}}}^{\mathrm{ST}}$
 (km s−1)(degree)(μG)(μG)  (km s−1)(km s−1)  
R10.64 ± 0.45.03101 ± 7142 ± 270.24 ± 0.190.58 ± 0.424.62 ± 3.31.92 ± 1.30.24 ± 0.230.58 ± 0.54
R20.51 ± 0.27.5754 ± 2728 ± 120.45 ± 0.270.87 ± 0.462.47 ± 1.31.28 ± 0.60.36 ± 0.240.69 ± 0.42
R30.40 ± 0.24.2375 ± 4529 ± 150.32 ± 0.220.84 ± 0.513.43 ± 2.11.33 ± 0.70.20 ± 0.160.52 ± 0.38

Note. Properties of the three subregions R1, R2, and R3. Columns (2) and (3): the velocity dispersion and the dispersion of the polarization PAs. Columns (4) and (5): the magnetic field strengths derived from the DCF and ST methods, respectively. Columns (6), (8), and (10): the mass-to-flux ratio, the three-dimensional $\mathrm{Alfv}\acute{{\rm{e}}}{\rm{n}}$ velocity, and the Mach number calculated with the Bpos obtained from the DCF method. Columns (7), (9), and (11): the corresponding values computed based on the Bpos derived from the ST method.

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4. Discussion

4.1. Comparison with the Taurus and Musca Filamentary Clouds

The combined MWISP CO and Planck dust observations show a filamentary structure in the L914 cloud, with a string of magnetically aligned striations perpendicular to the dense ridge (see, e.g., Figure 10). Similar striation structures are also observed in the Taurus B211 (e.g., Palmeirim et al. 2013) and Musca filaments (e.g., Cox et al. 2016; Bonne et al. 2020). In comparison to the L914 cloud, these two objects are located at relatively higher Galactic latitudes and are much closer (140 pc for Taurus; 200 pc for Musca), so there is very low line-of-sight (LOS) contamination. The main filament of L914 spans ∼50 pc in length, which is roughly five times longer than that of B211 and Musca (∼10 pc). Besides, the line mass of the L914 filament (∼80 M pc−1) is also much larger than that of the Musca and Taurus B211 filaments (∼20 M pc−1 and 50 M pc−1, respectively). It must be noted that the properties of filaments can vary significantly due to different tracers, sensitivities, and spatial resolutions. 9 Furthermore, we reveal the quasiperiodic arrangements in both the CO intensity (see Figure 6) and velocity dispersion (see Figure 7), which are not observed in the cases of B211 and Musca. These newly discovered characteristics may help us to better understand the nature of the striations associated with filaments and provide new observational constraints on the theoretical models. The morphology of the B-field, revealed by polarization measurements from either starlight or dust emission, demonstrates a large-scale ordered field parallel to the striations in all three clouds. The estimated B-field strengths in the Musca, Taurus, and L914 clouds are ∼12 μG (Planck Collaboration et al. 2016), 25 μG (Chapman et al. 2011), and 80 μG (this work), respectively.

André et al. (2014) proposed that filaments gain mass through magnetized accretion. In this scenario, the B-field is dynamically dominant in the formation of filaments, by channeling the material along the substructures onto the dense ridge. So far, there have been several cases of accretion activity identified by velocity gradients, such as the OMC-1 (Hacar et al. 2017), OMC-3 (Ren et al. 2021), DR21 (Cao et al. 2022), M120.1 + 3.0 (Sun et al. 2023), California (Guo et al. 2021), and Serpens (Gong et al. 2018, 2021) regions. In these cases, accretion flows converge toward the gravity center, either along the main filament or the substructures in the hub–filament system. In the Musca and B211 clouds, large-scale velocity gradients perpendicular to the main filaments are observed and are considered as evidence that the main filament is accreting material from its surroundings via striations (see Palmeirim et al. 2013; Shimajiri et al. 2019; Bonne et al. 2020). For L914, we check the PV profiles along the striations and find increasing velocity gradients and dispersions along the striations S5 and S6 toward the dense ridge. The PV maps are exhibited in Figure 14. If gravity is responsible for the velocity gradients, we can quantitatively delineate the motion of material in the potential well. We assume that the main filament is an infinite cylinder and then use the observed line mass to estimate the freefall velocity vff at a radius r (Palmeirim et al. 2013):

Equation (9)

where D is the distance from the tail end of the striation to the dense ridge. Since we can only derive the LOS velocity VLSR and the projected position p, Equation (9) can be rewritten as ${v}_{\mathrm{LSR}}={v}_{\mathrm{sys}}+2\sqrt{{{GM}}_{\mathrm{line}}\cdot {ln}(\tfrac{D}{p/\sin \theta })}\cdot \cos \theta $, where vsys is the system velocity and θ is the inclination angle of the striation against the LOS. In Figure 14, we display the fitted velocity profiles under the line masses of 60, 80, and 100 M pc−1, respectively. The derived systematic velocities are ∼1.37 and 1.52 km s−1, respectively. The velocity reaching the surface of the dense ridge is estimated to be 2.7–3.1 km s−1, resulting in an estimated freefall velocity of ∼1.3–1.7 km s−1. With the estimated freefall velocity, we further calculate the current mass accretion rate with the equation of ${\dot{M}}_{\mathrm{line}}=\rho (R)\,\times {v}_{\mathrm{ff}}\times 2\pi R$, where ρ(R) ∼ 600cm−3 is the density at the radius of the dense ridge R ∼ 0.5 pc. This results in an accretion rate of ∼170–230 M pc−1 Myr−1. It means that the main filament of L914 would be formed in roughly 0.3–0.5 Myr. Using a similar method, the timescales in the B211 and Musca systems are estimated to be 1–2 Myr (Palmeirim et al. 2013) and 1 Myr (Bonne et al. 2020), respectively. Our results suggest that the L914 cloud is in an earlier stage of evolution compared to the B211 and Musca filaments.

Figure 14.

Figure 14. PV maps along striations S5 and S6. The grayscale background shows the 12CO emission, and the blue contours are at 0.5 and 1.5 K (σ12 ∼ 0.2 K). The overlapped lime and magenta contours show the 13CO and C18O emission, respectively. The lime contours start at 0.5 K and increase with steps of 1 K (σ13 ∼ 0.15 K). The magenta contours start at 0.5 K and increase with steps of 0.5 K (σ18 ∼ 0.15 K). The orange solid line represents the dense ridge and the blue shadow region shows its width. The red solid curve is the fitted velocity profile for a free-falling particle under the gravity of a cylinder with a line mass of 80 M pc−1 (see Section 4.1 for more details). The two dashed lines display the expected velocity profiles by changing the line masses to 60 (yellow) and 100 M pc−1 (orange). The scaling is shown with the vertical arrow line and the resolution is marked with the pink rectangle.

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To date, numerous filamentary molecular clouds have been observed in various environments (see, e.g., the review by Hacar et al. 2023). However, the striation-associated samples have only been discovered in a few of them, such as B211 (Palmeirim et al. 2013), Musca (Cox et al. 2016), and L914 in this work. Based on a comparison of the striations in B211, Musca, and L914, we consider the following reasons for the limited number of observed striations: (1) striations may be transient, short-lived structures and only appear at the early formation stage of filamentary molecular clouds; and (2) striations are more diffuse and slender than the main filament. Consequently, in observations, the striations will drown in backgrounds due to a lack of strong contrast with the surrounding emission or because of their small beam-filling factors (Heyer et al. 2016). Therefore, large-scale surveys with both high sensitivity and spatial resolution are needed to search for more striation samples.

4.2. Comparison between the Observations and Simulations

Similar to the field structure orientations in R2 and R3 (see Figure 12), the bimodal configurations have been revealed in multiple studies. For example, Planck Collaboration et al. (2016) statistically measured the relative orientations between gas structures and magnetic fields within 10 nearby Gould belt molecular clouds, using the Histogram of Relative Orientations (HRO; Soler et al. 2013) technique, and found that the relative orientation changes systematically with column density NH, transitioning from being parallel in the lowest-density regions to perpendicular in the highest-density regions. With the same method, other molecular clouds, such as Vela C (Soler et al. 2017) and Serpens Main (Kwon et al. 2022), have also been studied and yielded the same conclusion. The HRO method calculated the relative orientation pixel by pixel and the Planck results focused on the high- and low-density medium, while Li et al. (2013) defined the global cloud orientation and demonstrated that the bimodal configuration exists in the 2 < Av < 5 medium as well (see also Gu & Li 2019). Such strong coupling of B-fields and filamentary structures indicates the important role that magnetic fields play in shaping the morphology of molecular clouds. In addition, we note that subregion R1 has a column density comparable to the dense ridges of R2 and R3, while the magnetic field in R1 is parallel to the gas structure. We consider that the sharp turn in the relative orientation may be caused by the stellar feedback, which compresses and reshapes both the arc-like gas and magnetic field in subregion R1 (see, e.g., Chapman et al. 2011; Chen et al. 2022). Alternatively, the parallel configuration observed in R1 may result from projection effects. For instance, if the magnetic field is primarily oriented along the LOS but slightly tilted toward the longitudinal direction, we would observe a projected magnetic field (Bpos) parallel to the filamentary structure on the POS. However, the verification of these hypotheses is beyond the scope of this work. In this work, we focus on the subregions exhibiting striations (i.e., subregions R2 and R3).

The bimodality in the orientation between the B-field and filamentary structures is also seen in synthetic polarization maps of numerical simulations (e.g., Hennebelle 2013; Soler et al. 2013; Chen et al. 2016; Li & Klein 2019). Soler et al. (2013) conducted a series of three-dimensional MHD simulations with varying initial magnetic field strengths threading molecular clouds and demonstrated that the bimodal configurations are observed exclusively in the strongly magnetized clouds (β = 0.1, where β is the squared ratio of the sound speed to the $\mathrm{Alfv}\acute{{\rm{e}}}{\rm{n}}$ speed).

In order to evaluate whether the subregions in L914 are gravity-bound or magnetically supported, we calculate the mass-to-flux ratio in units of the critical value via

Equation (10)

where the observed mass-to-flux ratio is ${(M/{\rm{\Phi }})}_{\mathrm{obs}}=\tfrac{\mu {m}_{{\rm{H}}}N({{\rm{H}}}_{2})}{B}$, and the critical value is ${(M/{\rm{\Phi }})}_{\mathrm{cri}}=\tfrac{1}{2\pi \sqrt{G}}$ (Nakano & Nakamura 1978). Then, Equation (10) can be simplified as described in Crutcher et al. (2004):

Equation (11)

where N(H2) is the mean column density in units of cm−2, and Bobs is the projected B-field strength in μG. The cloud region with the ratio λ > 1 is in a supercritical state and will collapse under gravity. On the contrary, the region with λ < 1 is magnetically supported. We adopt the magnetic field strengths derived from both the DCF and ST methods to calculate the ratios (see Table 2) and find that all the subregions are subcritical. According to the velocity profile fitting in Section 4.1, the inclination angles of the striations (S5 and S6) against the LOS are estimated to be θ ∼ 45°. Thus, the corrected mass-to-flux ratio should be ${\lambda }_{\mathrm{obs}}\cdot \cos \theta $. This correction reinforces our conclusion that the L914 cloud is in a magnetically subcritical state.

As a key parameter to describe the relative importance of turbulence and the magnetic field, the $\mathrm{Alfv}\acute{{\rm{e}}}\mathrm{nic}$ Mach number is also calculated with the following formula:

Equation (12)

where ${V}_{{\rm{A}},3{\rm{D}}}=\tfrac{B}{\sqrt{{\mu }_{0}\rho }}$ is the three-dimensional $\mathrm{Alfv}\acute{{\rm{e}}}{\rm{n}}$ velocity, μ0 is the permeability of the vacuum, and $B=\tfrac{4}{\pi }{B}_{\mathrm{pos}}$ (Crutcher et al. 2004) is the total magnetic field strength. The $\mathrm{Alfv}\acute{{\rm{e}}}\mathrm{nic}$ Mach numbers of the three subregions are all less than 1 (see Table 2), indicating that the L914 cloud is sub-$\mathrm{Alfv}\acute{{\rm{e}}}\mathrm{nic}$.

These results demonstrate the significant dominance of the magnetic field over gravity or turbulence in the L914 cloud. In this case, the magnetic field introduces anisotropies into the cloud, assisting in the formation of filamentary structures, since motions perpendicular to the field lines are restricted by the Lorentz force (Soler et al. 2017). Conversely, in the case of super-$\mathrm{Alfv}\acute{{\rm{e}}}\mathrm{nic}$ turbulence (MA > 1), motions are expected to be more random. The MHD and hydrodynamical simulations presented in Hennebelle (2013) also suggest that the magnetic field could increase the ellipticity of the clumps, making them more filamentary.

Tritsis & Tassis (2016) conducted Kelvin–Helmholtz instability and MHD simulations to reproduce the Taurus striations 10 (Goldsmith et al. 2008). The contrast of the intensity on and off the Taurus striations is ∼25% and Tritsis & Tassis (2016) suggested that only the nonlinear coupling of MHD waves can reproduce the density contrast. The contrasts in the subregions R2 and R3 of the L914 cloud are roughly 12% and 28%, respectively (see Section 3.1). We further estimate the magnetic Jeans length (λJ,mag) of the L914 filament using the following equation (Krumholz & Federrath 2019):

Equation (13)

where ρ and λJ represent the mass density and the standard Jeans length including only thermal pressure, respectively. The plasma beta (β) is calculated as $\beta =\tfrac{{c}_{{\rm{s}}}^{2}}{{V}_{{\rm{A}},\ 3{\rm{D}}}^{2}}$. Using the parameters obtained above, we estimate the magnetic Jeans length to be in the range of ∼2–10 pc. However, the H2 number densities of the striations tend to be much lower than those in the filaments (i.e., R1, R2, and R3). According to the relation that magnetic field strengths are proportional to the H2 number densities (Crutcher & Kemball 2019), the magnetic field strengths of the striations are estimated to be much weaker. For instance, if we take B = 11 μG, the plasma parameter β becomes 0.1, a value commonly adopted in the high-magnetization model (Soler et al. 2013). Consequently, the estimated magnetic Jeans length is approximately 1.4–1.8 pc, which is consistent with the period of the striations observed in this work (see Section 3.1). Our results suggest that the striations are likely produced by MHD processes. If the striations are created by fast magnetosonic waves, Tritsis et al. (2018) predict that the power spectra of column density cuts perpendicular to striations have peaks at roughly the same wavenumbers as the velocity centroid power spectra, proposing a new method to calculate the magnetic field strength,

Equation (14)

where Γn is the square root of the ratio of the power in the velocity power spectrum and the power in the column density power spectrum, ${{\rm{\Gamma }}}_{n}=\sqrt{\tfrac{| {P}_{v1}{| }^{2}}{| {P}_{{N}_{{{\rm{H}}}_{2}}^{1}}{| }^{2}}}$. The mean column densities ${N}_{{{\rm{H}}}_{2}}$ and the mean density ρ can be computed from the $\overline{N}$ and n of the striations listed in Table 1. We present the power spectra in subregions R2 and R3 in Figure 15 and the left panel of Figure 16, respectively. The correlation of the periodicity of the velocity and the density exists only in subregion R3 (not in subregion R2). Based on this correlation, we calculate a magnetic field strength of 47 ± 12 μG, which falls within the range of the results obtained by the DCF and ST methods.

Figure 15.

Figure 15. Power spectra of column density cuts (blue lines) perpendicular to striations in subregion R2 and velocity centroid power spectra (red dashed lines). The column density is derived from the 12CO emission with the equation of ${N}_{{{\rm{H}}}_{2}}=X\int {T}_{\mathrm{MB},{\ }^{12}\mathrm{CO}}{dV}$, where X = 2.0 × 1020 cm−2 K−1 km−1 s (Bolatto et al. 2013).

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Figure 16.

Figure 16. Left: the same as Figure 15, but for subregion R3. Right: the distribution of the parameter Γ as a function of wavenumber for the peaks in the power spectra shown in the left panel. The red dashed line shows the fitting result obtained with the orthogonal distance regression method, and the shaded region shows the 1σ error of the fit.

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Combining the identified accretion activities in Section 4.1, we suggest a simple scenario where, at the early stage, a sheet-like cloud with the magnetic field parallel to it fragments into filaments under the Jeans instability. The self-gravitating filaments, perpendicular to the magnetic field, continuously accrete material from their surroundings along the magnetic field lines (through striations observed in the sensitive observations). When the filaments gain sufficient material, axial fragmentation then occurs in the MHD process, with a characteristic scale corresponding to the magnetically Jeans length (i.e., the period observed in this work).

5. Summary

We present the MWISP CO (J = 1 − 0) multiline observations toward the L914 cloud, using the PMO 13.7 m millimeter telescope. We reveal filamentary structures (a dense skeleton and diffuse striations) in the L914 cloud and derive their properties from the CO data. Combined with the dust polarization data from the Planck survey, we further investigate the relationship between the B-field and filamentary structures, aiming to understand the formation mechanism of filaments and the role of B-fields in this process. The main results are summarized below.

  • 1.  
    L914 is a filamentary molecular cloud located at a distance of ∼760 pc. Based on the C18O data, we identify the dense ridge of the L914 filament using the DisPerSE algorithm. The length, width, and line mass of the L914 filament are ∼50 pc, 1 pc, and ∼80 M pc−1, respectively. The L914 filament is thermally supercritical, with the line mass much larger than the critical line mass (Mline,crit ∼ 17 M pc−1).
  • 2.  
    A group of hair-like striations are discovered in two subregions of the L914 filamentary cloud. These striations are connected to the dense ridge of the filament and display quasiperiodic characteristics, with an oscillation period of about 1.1–1.4 pc. For the striations with prominent 13CO emission (S1–S6), we estimate their basic physical properties. The mean width and line mass of these striations are ∼0.5 pc and 8 M pc−1, respectively. All striations are in a thermally subcritical state.
  • 3.  
    The PV diagrams along two of the striations (S5 and S6) present increasing velocity gradients and velocity dispersions toward the dense ridge, which could be well fitted by freefall motions, suggesting that material flows along the striations toward the dense ridge under gravity.
  • 4.  
    The magnetic field inferred from the Planck 353 GHz observation presents a bimodal configuration. The large-scale ordered B-field is well aligned with the diffuse striations, but perpendicular to the dense ridge. We estimate the strength of the B-field and evaluate the relative importance between the gravity, turbulence, and B-field, then suggest that B-fields play an important role in the formation of filaments by channeling the material along the striations onto the dense ridge.

Acknowledgments

We thank the anonymous referee for providing insightful suggestions and comments, which helped us to improve this work. This work is supported by the National Natural Science Foundation of China (grant No. 12041305). This research made use of the data from the Milky Way Imaging Scroll Painting (MWISP) project, which is a multiline survey in 12CO/13CO/C18O along the northern Galactic plane with the PMO 13.7 m telescope. We are grateful to all the members of the MWISP working group, particularly the staff members at the PMO 13.7 m telescope, for their long-term support. MWISP was sponsored by the National Key R&D Program of China with grants 2023YFA1608000, 2017YFA0402701, and the CAS Key Research Program of Frontier Sciences with grant QYZDJ-SSW-SLH047. X. Chen acknowledges the support by the CAS International Cooperation Program (grant No. 114332KYSB20190009).

Appendix: Distance of L914 Cloud

In principle, because of the existence of molecular clouds along the LOS, the extinction value AG of on-cloud stars will produce a jump point, which can be used to deduce the distance of the cloud by using a Bayesian analysis. In this work, we adopt the same prior distribution and likelihood function as described in Yan et al. (2019) and then use the Python package emcee 11 (Foreman-Mackey et al. 2013) to compute the posterior probability distribution of the cloud distance (D). The sampling result is shown in Figure 17 and the mean value of ∼760 pc is adopted as the distance of the cloud.

Figure 17.

Figure 17. Measured distance of L914. The middle panel shows the selected region used for distance estimation. The colorful background represents the MWISP 12CO emission, and the gray contour shows the edge of the cloud (∼3σ ). The cyan and pink dots represent the on- and off-cloud Gaia DR3 stars, respectively. The corner plots of the Markov Chain Monte Carlo sampling (distance and the extinction values and uncertainties of foreground and background stars) are shown in the left panel, where the mean values of the samples are shown with solid vertical lines. In the right panels, the dots show the Gaia stars as illustrated in the legend of each panel. The orange solid line in the upper right panel represents the result of monotonic regression fitting, while the dashed green lines in the bottom right panel are the modeled extinction AG.

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Footnotes

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10.3847/1538-3881/ad2ea3