@article{oai:u-ryukyu.repo.nii.ac.jp:02004845,
 author = {Oomori, Tamotsu and Nakasone, Moritoshi and Kaneshima, Kiyoshi and Kitano, Yasushi and 大森, 保},
 issue = {39},
 journal = {琉球大学理学部紀要, Bulletin of the College of Science. University of the Ryukyus},
 month = {Mar},
 note = {The incorporation of Na^+ into calcium carbonate and protodolomite was studied by precipitating carbonates from Ca (HCO_3)_2 + NaCl(or NaHCO_3) + MgCl_2 solution. Relationship between sodium content of carbonate and Na^+ concentration in solution is obtained as: log[Na]_<carbonate> = n log[Na^+]_<solution> + k (n and k are constants). The addition of NaHCO_3 and/or MgCl_2 to Ca(HCO_3)_2 solution increases the incorporation of Na^+ into aragonite. Incorporation of Na^+ into protodolomite precipitated from brine solution is much higher than that into Mg-poor calcite precipitated from solution having the same Na^+  concentration as that in the brine solution., 紀要論文},
 pages = {51--56},
 title = {Incorporation of Sodium into Calcium Carbonate and Protodolomite},
 year = {1985}
}