%0 Journal Article
%T Influence of Mg<sup>2+</sup>, Fe<sup>2+</sup> and Zn<sup>2+</sup> Cations on <sup>13</sup>C-<sup>18</sup>O Bonds in Precipitated Aragonite,  Calcite and Dolomite: An <i>ab Initio</i> Study
%A Jie Yuan
%J Open Journal of Geology
%P 254-267
%@ 2161-7589
%D 2015
%I Scientific Research Publishing
%R 10.4236/ojg.2015.55023
%X The influence of metal
cations on<span class=\"apple-converted-space\" style=\"font-size:12px;font-family:Verdana;\"> </span><sup><span style=\"font-size:12px;font-family:Verdana;\">13</span></sup><span style=\"font-size:12px;font-family:Verdana;\">C-</span><sup><span style=\"font-size:12px;font-family:Verdana;\">18</span></sup><span style=\"font-size:12px;font-family:Verdana;\">O
bonds in carbonates is still under debate. This paper used</span><span class=\"apple-converted-space\" style=\"font-size:12px;font-family:Verdana;\"> </span><i><span style=\"font-size:12px;font-family:Verdana;\">ab initio</span></i><span class=\"apple-converted-space\" style=\"font-size:12px;font-family:Verdana;\"> </span><span style=\"font-size:12px;font-family:Verdana;\">method</span><span class=\"apple-converted-space\" style=\"font-size:12px;font-family:Verdana;\"> </span><span style=\"font-size:12px;font-family:Verdana;\">to investigate this kind of influence
of Mg</span><sup><span style=\"font-size:12px;font-family:Verdana;\">2+</span></sup><span style=\"font-size:12px;font-family:Verdana;\">, Fe</span><sup><span style=\"font-size:12px;font-family:Verdana;\">2+</span></sup><span class=\"apple-converted-space\" style=\"font-size:12px;font-family:Verdana;\"> </span><span style=\"font-size:12px;font-family:Verdana;\">and
Zn</span><sup><span style=\"font-size:12px;font-family:Verdana;\">2+</span></sup><span class=\"apple-converted-space\" style=\"font-size:12px;font-family:Verdana;\"> </span><span style=\"font-size:12px;font-family:Verdana;\">cations on</span><span class=\"apple-converted-space\" style=\"font-size:12px;font-family:Verdana;\"> </span><sup><span style=\"font-size:12px;font-family:Verdana;\">13</span></sup><span style=\"font-size:12px;font-family:Verdana;\">C-</span><sup><span style=\"font-size:12px;font-family:Verdana;\">18</span></sup><span style=\"font-size:12px;font-family:Verdana;\">O bonds in
precipitated aragonite, calcite and dolomite. The polynomials of <span style=\"white-space:nowrap;\">жд</span></span><sub><span style=\"font-size:12px;font-family:Verdana;\">47</span></sub><span class=\"apple-converted-space\" style=\"font-size:12px;font-family:Verdana;\"> </span><span style=\"font-size:12px;font-family:Verdana;\">and reduced partition function ratios
(RPFRs) for</span><span class=\"apple-converted-space\" style=\"font-size:12px;font-family:Verdana;\"> </span><sup><span style=\"font-size:12px;font-family:Verdana;\">13/12</span></sup><span style=\"font-size:12px;font-family:Verdana;\">C,</span><span class=\"apple-converted-space\"
%K Metal Cation
%K &lt
%K sup&gt
%K 13&lt
%K /sup&gt
%K C-&lt
%K sup&gt
%K 18&lt
%K /sup&gt
%K O Bond
%K жд47
%K Phosphoric Acid
%K &lt
%K i&gt
%K ab Initio&lt
%K /i&gt
%K Calculation
%U http://www.scirp.org/journal/PaperInformation.aspx?PaperID=56211