B-type asteroid

{{short description|Asteroid spectral class; uncommon type of carbonaceous asteroid}}

File:Bennu mosaic OSIRIS-REx (square).png from a range of {{convert|24|km|mi|abbr=on}}]]

B-type asteroids are a relatively uncommon type of carbonaceous asteroid, falling into the wider C-group; the 'B' indicates these objects are spectrally blue. In the asteroid population, B-class objects can be found in the outer asteroid belt, and also dominate the high-inclination Pallas family which includes the third-largest asteroid 2 Pallas. They are thought to be primitive, volatile-rich remnants from the early Solar System. There are 65 known B-type asteroids in the SMASS classification, and 9 in the Tholen classification as of March 2015.

Characteristics

Generally similar to the C-type objects, but differing in that the ultraviolet absorption below 0.5 μm is small or absent, and the spectrum is rather slightly bluish than reddish. The albedo also tends to be greater than in the generally very dark C type. Spectroscopy of B-class objects suggests major surface constituents of anhydrous silicates, hydrated clay minerals, organic polymers, magnetite, and sulfides. The closest matches to B-class asteroids have been obtained on carbonaceous chondrite meteorites that have been gently heated in the laboratory.

The majority of asteroids that have been observed to display cometary-like activity are B-types.{{cite journal |last1=Licandro |first1=J |last2=Hargrove |first2=K |last3=Kelley |first3=M |last4=Campins |first4=H |title=5–14 μm Spitzer spectra of Themis family asteroids |journal=Astronomy & Astrophysics |date=Jan 2012 |volume=537 |page=A73 |doi=10.1051/0004-6361/201118142|bibcode=2012A&A...537A..73L |doi-access=free }}{{cite journal |last1=Alí-Lagoa |first1=V |last2=De León |first2=J |last3=Licandro |first3=J |last4=Delbo |first4=M |last5=Campins |first5=H |last6=Pinilla-Alonso |first6=N |last7=Kelley |first7=M |title=Physical properties of B-type asteroids from WISE data |journal=Astronomy & Astrophysics |date=Mar 2013 |volume=554 |page=A71 |doi=10.1051/0004-6361/201220680|arxiv=1303.5487 |bibcode=2013A&A...554A..71A |doi-access=free }} 1. Introduction: "the majority of asteroids

that have been observed to display cometary-like activity are B-types" Some of these objects display indications of aqueous alteration in the past, and they may have incorporated significant amounts of water ice.

Well studied B-type asteroids

See also

References

{{reflist

| refs =

{{cite web

|title = JPL Small-Body Database Search Engine: spec. type = B (SMASSII)

|publisher = JPL Solar System Dynamics

|url = http://ssd.jpl.nasa.gov/sbdb_query.cgi?obj_group=all;obj_kind=all;obj_numbered=all;OBJ_field=0;ORB_field=0;c1_group=OBJ;c1_item=Ax;c1_op=%3D;c1_value=B;table_format=HTML;max_rows=100;format_option=comp;c_fields=AcBhBgBjBiBnBsAiApAyAx;.cgifields=format_option;.cgifields=obj_kind;.cgifields=obj_group;.cgifields=obj_numbered;.cgifields=ast_orbit_class;.cgifields=table_format;.cgifields=com_orbit_class&query=1&c_sort=AxA |access-date = 2015-06-17}}

{{cite journal

| title=Identification of Magnetite in B-type Asteroids

| last1=Yang | first1=Bin | last2=Jewitt | first2=David

| journal=The Astronomical Journal

| volume=140 | issue=3 | pages=692–698 | date=September 2010

| arxiv=1006.5110 | bibcode=2010AJ....140..692Y

| doi=10.1088/0004-6256/140/3/692 | s2cid=724871 }}

}}

{{Asteroids}}

{{Small Solar System bodies}}

Category:Asteroid spectral classes