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On the chemistry and mineralogy of boron in pure and in mixed systems: A review1

 

作者: ClareM. Evans,   DonaldL. Sparks,  

 

期刊: Communications in Soil Science and Plant Analysis  （Taylor Available online 1983）
卷期: Volume 14, issue 9  

页码: 827-846

 

ISSN:0010-3624

 

年代: 1983

 

DOI:10.1080/00103628309367412

 

出版商: Taylor & Francis Group

 

关键词: B adsorption;B desorption;B kinetics

 

数据来源: Taylor

 

摘要:

Boron (B) is the third member of the third periodic group. It is a nonmetal with an atomic number of five and a constant valence of 3+. Boric acid [B(OH)3]and H2Bo3−are the most common geologic forms of B, with boric acid the predominant form of B in agricultural soils. Boron occurs mainly in silicate minerals. The 10 μg/g B concentration of the earth's crust is distributed among common rock types.

 

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