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. 2017 Mar 1;13:393–404. doi: 10.3762/bjoc.13.42

Table 1.

Adsorption of RNA on synthetic minerals formed by double-decomposition reactions.a

MgCl2 CaCl2 SrCl2 BaCl2 MnCl2

Na2B4O7 no PPT 86% 87% 95% 87%
Na2CO3 magnesite
77%
calcite
86%
strontianite
90%
witherite
95%
rhodochrosite
89%
Na2PO4b 64% apatite
93%
strontium apatite
84%
barium apatite
32%
metaswitzerite
86%
Na2SO4 no PPT gypsum
2%
celestine
71%
baryte
88%
no PPT
Na3VO4 magnesium coulsonite
78%
cavoite
92%
73% 85% ansermetite
38%
Na2HAsO4 6% johnbaumite
73%
4% gurimite
30%
61%
NaF no PPT fluorite
no PPT
72% 15% no PPT

FeCl2 FeCl3 CoCl2 NiCl2 CuCl2 ZnCl2

Na2B4O7 88% no PPT 87% 94% 96% 93%
Na2CO3 siderite
65%
no PPT cobalite
95%
94% malachite
73%
smithsonite
93%
Na2PO4b vivianite
68%
30% pakhomovskyte
80%
75% libethenite
84%
hopeite
6%
Na2SO4 22% no PPT no PPT no PPT no PPT no PPT
Na3VO4 fervanite
2%
46% 2% 12% 73% 17%
Na2HAsO4 75% 10% erythrite
12%
49% lammerite
79%
adamite
62%
NaF 24% 29% no PPT no PPT 43% no PPT

aNo PPT: no precipitate observed. For some minerals, the name of the natural species is reported. bNa3PO4 + NaHPO4.