– 4 –
SMA observations at 0.87 mm revealed more complex magnetic field structures which are
likely the reason for the depolarization in the larger BIMA beam. The finer B-field structures
in e2 and e8 showing hourglass-like topologies with clearly bent field lines were interpreted
as gravitational collapse imprinted onto the B-field morphology (Tang et al. 2009b). The
first ALMA observations at 1.3 mm (Koch et al. 2018), again improving the resolution by a
factor of 10 in area, revealed striking new features. In particular, they clearly resolved the
satellite core e2-NW with bow-shock shaped B-field structures that are hinting infall of this
smaller core towards the dominating mass center e2-E. Additionally, areas with centrally
converging symmetrical B-field structures (convergence zones) and possibly streamlined B-
field morphologies were detected. A generic feature seen in many of the resolved cores inside
e2, e8, North, and also on larger scale between e2 and e8, is B-field structures resembling
gravitational pull towards the core’s center on one side with the other side showing B-
field lines appearing to be dragged away towards the next more massive neighboring core.
This imprint in the B-field morphology was interpreted as a scenario where local collapse
is ongoing while a locally collapsing core, as an entity, is pulled to the next more massive
gravitational center which itself is also collapsing (Koch et al. 2018). Recent numerical work
by V´azquez-Semadeni et al. (2019) is exactly presenting such a scenario as a result of a global
hierarchical collapse where a flow regime leads to collapses within collapses.
While the successively higher-resolution observations in W51 keep revealing new mag-
netic field features from imprints of dynamical processes, the W51 region has, at the same
time, served as a mine of information for our developments of new analysis techniques. The
SMA observations (Tang et al. 2009b) served as a testbed for the polarization–intensity gra-
dient technique (Koch et al. 2012a,b). This technique uses the measurable angle δbetween
a magnetic field orientation and an intensity gradient as a key observable which, in combi-
nation with a second angle between intensity gradient and local gravity, makes it possible
to derive a magnetic field strength. The technique gives a local magnetic field strength – at
every position where a magnetic field orientation is detected – and therefore, leads to maps
of field strengths. At the same time, the technique puts forward a magnetic field-to-gravity
force ratio, ΣB, based solely on measurable angles which allows for a completely indepen-
dent estimate of a mass-to-flux ratio (Koch et al. 2012b). The establishment of δas a prime
observable as well as an approximation for ΣBis presented in Koch et al. (2013) with an
application to a 50-source sample of low- and high-mass star-forming sources in Koch et al.
(2014). A main result from this series of papers is the recognition of a spatially varying role
of the magnetic field, e.g., mass-to-flux ratios can transition from outer sub-critical to inner
super-critical areas in a star-forming region, and force ratios ΣBare clearly varying from
zones where collapse and infall are slowed down or prohibited by the magnetic field to other
zones, within the same source, where collapse is possible. With the first ALMA data in Koch