User:Praseodymium-141/Boron compounds
![](http://upload.wikimedia.org/wikipedia/commons/thumb/4/4c/Boron-trifluoride-pi-bonding-2D.png/110px-Boron-trifluoride-pi-bonding-2D.png)
Boron compounds are compounds containing the element boron. In the most familiar compounds, boron has the formal oxidation state +3. These include oxides, sulfides, nitrides, and halides.[1]
Halides
The trihalides adopt a planar trigonal structure. These compounds are
It is found in nature on Earth almost entirely as various oxides of B(III), often associated with other elements. More than one hundred borate minerals contain boron in oxidation state +3. These minerals resemble silicates in some respect, although it is often found not only in a tetrahedral coordination with oxygen, but also in a trigonal planar configuration. Unlike silicates, boron minerals never contain it with coordination number greater than four. A typical motif is exemplified by the tetraborate anions of the common mineral borax, shown at left. The formal negative charge of the tetrahedral borate center is balanced by metal cations in the minerals, such as the sodium (Na+) in borax.[1] The tourmaline group of borate-silicates is also a very important boron-bearing mineral group, and a number of borosilicates are also known to exist naturally.[2]
Boranes
Boranes are chemical compounds of boron and hydrogen, with the generic formula of BxHy. These compounds do not occur in nature. Many of the boranes readily oxidise on contact with air, some violently. The parent member BH3 is called borane, but it is known only in the gaseous state, and dimerises to form diborane, B2H6. The larger boranes all consist of boron clusters that are polyhedral, some of which exist as isomers. For example, isomers of B20H26 are based on the fusion of two 10-atom clusters.
The most important boranes are diborane B2H6 and two of its pyrolysis products, pentaborane B5H9 and decaborane B10H14. A large number of anionic boron hydrides are known, e.g. [B12H12]2−.
The formal
Nitrides
The
Organoboron chemistry
A large number of organoboron compounds are known and many are useful in organic synthesis. Many are produced from hydroboration, which employs diborane, B2H6, a simple borane chemical. Organoboron(III) compounds are usually tetrahedral or trigonal planar, for example, tetraphenylborate, [B(C6H5)4]− vs. triphenylborane, B(C6H5)3. However, multiple boron atoms reacting with each other have a tendency to form novel dodecahedral (12-sided) and icosahedral (20-sided) structures composed completely of boron atoms, or with varying numbers of carbon heteroatoms.
Organoboron chemicals have been employed in uses as diverse as
Compounds of B(I) and B(II)
As anticipated by its
![](http://upload.wikimedia.org/wikipedia/commons/thumb/d/d2/Magnesium-diboride-3D-balls.png/220px-Magnesium-diboride-3D-balls.png)
Binary metal-boron compounds, the metal borides, contain boron in negative oxidation states. Illustrative is
Certain other metal borides find specialized applications as hard materials for cutting tools.[10] Often the boron in borides has fractional oxidation states, such as −1/3 in calcium hexaboride (CaB6).
From the structural perspective, the most distinctive chemical compounds of boron are the hydrides. Included in this series are the cluster compounds dodecaborate (B
12H2−
12), decaborane (B10H14), and the carboranes such as C2B10H12. Characteristically such compounds contain boron with coordination numbers greater than four.[1]
References
- ^ ISBN 978-3-11-007511-3.
- ^ "Mindat.org - Mines, Minerals and More". mindat.org. Archived from the original on 22 April 2011. Retrieved 4 August 2019.
- PMID 23535980.
- (PDF) from the original on 13 June 2013. Retrieved 8 January 2012.
- ISBN 978-3527306732.
- ISBN 978-0-08-037941-8.
- .
- (PDF) from the original on 26 February 2012. Retrieved 8 January 2012.
- ^ "Category "News+Articles" not found - CERN Document Server". cds.cern.ch. Archived from the original on 20 February 2022. Retrieved 9 October 2020.
- ISBN 978-1-84628-668-1. Archivedfrom the original on 8 January 2017. Retrieved 5 January 2016.