The Chemical Analysis of Argonne Premium Coal Samples
Edited by Curtis A. Palmer
1997
U.S. Geological Survey Bulletin 2144
Determination of 62 Elements in 8 Argonne Premium Coal Ash Samples by Automated Semiquantitative Direct-Current Arc Atomic Emission Spectrography
By Carol J. Skeen, B.J. Libby, and W.B. Crandell
Table 3. Element concentrations determined by direct-current arc spectrographic anlayses of the Argonne Premium Coal samples -- continued.
Element | PITT PC-4-1 | PITT PC-4-2 | PITT PC-4-3 | POC PC-5-1 | POC PC-5-2 | POC PC-5-3 |
Si (%) | 26 | 29 | 32 | 18 | 17 | 19 |
Al | 24 | 21 | 24 | 12 | 14 | 14 |
Fe | 19 | 20 | 22 | 9.8 | 8.3 | 10 |
Mg | .71 | .70 | 97 | 1.9 | 2.0 | 2.0 |
Ca | 5.0 | 3.6 | 4.7 | 10 | 11 | 12 |
Na | .42 | .36 | .40 | 2.4 | 2.4 | 2.5 |
K | 1.4 | 1.3 | 1.5 | .65 | .63 | .73 |
Ti | .64 | .57 | .64 | .53 | .47 | .58 |
P | <.068 | <.068 | <.068 | <.068 | <.068 | <.068 |
Mn | .033 | .041 | .042 | .045 | .043 | .050 |
Ag (µg/g) | .95 | .94 | 1.0 | 1.8 | 1.8 | 2.0 |
As | 210 | 180 | 160 | 350 | 210 | 270 |
Au | <6.8 | <6.8 | <6.8 | <6.8 | <6.8 | <6.8 |
B | 530 | 580 | 570 | 320 | 310 | 360 |
Ba | 390 | 370 | 490 | 3,600 | 3,600 | 4,900 |
Be | 12 | 13 | 13 | 14 | 11 | 13 |
Bi | 22 | 17 | <10 | <10 | <10 | <10 |
Cd | <32 | <32 | <32 | <32 | <32 | <32 |
Ce | <200 | <200 | <200 | 220 | 190 | 270 |
Co | 31 | 25 | 30 | 45 | 44 | 56 |
Cr | 220 | 190 | 220 | 170 | 150 | 180 |
Cu | 58 | 89 | 66 | 420 | 290 | 380 |
Dy | <22 | <22 | <22 | <22 | <22 | <22 |
Er | <4.6 | <4.6 | <4.6 | <4.6 | <4.6 | <4.6 |
Eu | <2.2 | <2.2 | <2.2 | <2.2 | <4.2 | <2.2 |
Ga | 57 | 43 | 54 | 42 | 40 | 47 |
Gd | <32 | <32 | <32 | <32 | <32 | <32 |
Ge | 13 | 13 | 12 | 8.7 | 8.2 | 9.2 |
Hf | <150 | <150 | <150 | <15 | <15 | <15 |
Ho | <6.8 | <6.8 | <6.8 | <6.8 | <6.8 | <6.8 |
In | <10 | <10 | <10 | <10 | <10 | <10 |
Ir | <15 | <15 | <15 | <15 | <15 | <15 |
La | 60 | 66 | 62 | 130 | 130 | 150 |
Lu | <15 | <15 | <15 | <15 | <15 | <15 |
Mo | 9.4 | 7.4 | 9.0 | 37 | 41 | 46 |
Nb | 18 | 22 | 18 | 24 | 14 | 22 |
Nd | 47 | 46 | 35 | 100 | 130 | 110 |
Ni | 150 | 130 | 150 | 120 | 110 | 140 |
Os | <15 | <15 | <15 | <15 | <15 | <15 |
Pb | 79 | 75 | 84 | 220 | 160 | 220 |
Pd | <1.0 | <1.0 | <1.0 | <1.0 | <1.0 | <1.0 |
Pr | <100 | <100 | <100 | <100 | <100 | <100 |
Pt | <2.2 | <2.2 | <2.2 | <2.2 | <2.2 | <2.2 |
Re | <10 | <10 | <10 | <10 | <10 | <10 |
Rh | <2.2 | <2.2 | <2.2 | <2.2 | <2.2 | <2.2 |
Ru | <2.2 | <2.2 | <2.2 | <2.2 | <2.2 | <2.2 |
Sb | <68 | <68 | <68 | <68 | <68 | <68 |
Sc | 20 | 19 | 22 | 24 | 24 | 28 |
Sm | <10 | <10 | <10 | 14 | 13 | 16 |
Sn | 18 | 11 | 13 | 2,800 | 550 | 720 |
Sr | 960 | 900 | 1,100 | 2,000 | 1,900 | 2,300 |
Ta | <320 | <320 | <320 | <320 | <320 | <320 |
Tb | <32 | <32 | <32 | <32 | <32 | <32 |
Th | <46 | <46 | <46 | <46 | <46 | <46 |
Tl | <10 | <10 | <10 | <10 | <10 | <10 |
Tm | <4.6 | <4.6 | <4.6 | <4.6 | <4.6 | <4.6 |
U | <220 | <220 | <220 | <220 | <220 | <220 |
V | 130 | 130 | 150 | 130 | 120 | 150 |
W | <15 | <15 | <15 | <15 | <15 | <15 |
Y | 31 | 36 | 33 | 86 | 81 | 92 |
Yb | 6.9 | 5.5 | 5.2 | 8.7 | 8.8 | 7.9 |
Zr | 110 | 160 | 120 | 250 | 200 | 220 |
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