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. 2019 Mar 18;9:4726. doi: 10.1038/s41598-019-41265-3

Table 1.

Bulk compositions of pre-experimental pseudo-ash samples measured with X-ray fluorescence.

Bulk oxide abundance (wt %) LW-NINW LW-ONW R-1 K38-PC2 SHV347-B OBS1 ECF2LAP*
Basic samples Intermediate samples Acidic samples
SiO2 48.78 49.12 53.56 53.43 58.11 76.19 72.75
TiO2 1.96 1.90 0.78 0.61 0.64 0.14 0.32
Al2O3 17.13 17.14 17.98 19.39 18.21 12.71 14.19
Fe2O3 11.29 11.36 9.21 8.79 7.34 1.32 2.10
MnO 0.18 0.18 0.16 0.23 0.19 0.05 0.05
MgO 5.90 5.73 6.06 4.37 2.95 0.15 0.68
CaO 8.27 8.46 7.80 9.74 7.70 0.44 1.66
Na2O 3.49 3.22 2.40 2.83 3.61 4.40 3.81
K2O 1.82 1.73 0.99 0.56 0.79 4.59 4.35
P2O5 1.19 1.16 0.12 0.13 0.14 0.02 0.09
Total 100 100 99 100 100 100 100
Rb/a 0.45 0.44 0.37 0.36 0.29 0.12 0.14

Each value is an average of five individual measurements. Based upon these values, the two basic samples (LW-NINW and LW-ONW) are classified as trachybasalts, the three intermediate samples (R-1, K38-PC2, and SHV347-B) are considered basaltic andesites/andesites, and the acidic samples (OBS1 and ECF2LAP) are classified as rhyolites. Rb/a is the ratio of basic to acidic oxides and is calculated as Rb/a = (CaO + Fe2O3 + MgO + K2O + Na2O + MnO)/(SiO2 + Al2O3 + TiO2 + P2O5) following previous methods32. *Values for ECF2LAP are not those of the exact sample used in the experiments, but for a different pyroclast derived from the same eruptive sequence.