Mechanism of Na and K Substitutions in Bioapatite Within Salty Area  

Mechanism of Na and K Substitutions in Bioapatite Within Salty Area

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作  者:LI Zhen 

机构地区:[1]College of Resources and Environmental Science, Nanjing Agriculture University

出  处:《Acta Geologica Sinica(English Edition)》2014年第S1期86-86,共1页地质学报(英文版)

摘  要:Introduction Na and K are two most important cations in salty water,and also are two typical ions in animals’body fluids.The mineral,bioapatite,is a form of carbonated hydroxylapatite,which makes up over 50 wt.%of bonesIntroduction Na and K are two most important cations in salty water,and also are two typical ions in animals’body fluids.The mineral,bioapatite,is a form of carbonated hydroxylapatite,which makes up over 50 wt.%of bones

关 键 词:bone NA Mechanism of Na and K Substitutions in Bioapatite Within Salty Area 

分 类 号:P619.211[天文地球—矿床学]

 

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