Page 235 - Geochemistry of Oil Field Waters

Potassium
-
Copper
~
Chromium
md q75 md q25 q75 md q75 q75 ~ ~ 400 300 180 75p lop <lop ND ND 3P 400 300 160 <25p <25p <25p ND < 2P 300 <50 ND <1 <1 ND*~ ND*~ <5P < 1P 2P 1,000 300 ND 450p 150p ND ND 25P 35P 500 350 120 ND ND ND 10P 1P 4P 750 400 160 ND ND ND 10P 2P 4P 400 300 200 ND ND ND 5P < 1P 4P 450 300 170 ND ND 15~ 4~ < 1P 4P 650 400 200 ND 15~ 4~ 3P
~
Cobalt ND ND ND*~ ND ND ND ND ND ND ND ND ND <5P ND ND ND
- 119 131 116 1 24 173 215 168 72 128 203 88 296 11 11 15 30 quartile (4)
Dissolved solids (gll) md - q75 98 70 69 30 66 27 222 173 111 61 143 70 115 80 55 42 67 53 137 51 59 9 173 115 5 3 5 4 5 3 18 5 35 -

Number of samples 22 79 88 24 148 74 34 15 21 118 25 55 22 28 18 116 - - Rittenhouse et al., 1969)and data, less sensitive methods of analysis used.

(continued)*' .-. *3 Includes Oklahoma Platform and Ardmore Basin.

TABLE 7.XIV Illinois Basin Louisiana and Texas Gulf Coast East Texas North Texas West Texas and New Mexico Permian only Pennsylvanian only Silurian and Devonian only Ordovician and Cambrian only Anadarko Basin*3 Williston Basin, post- Paleozoic Williston Basin, Paleozoic Powder River Basin Other Wyoming Colorado California Sea water Estimated detection limit - __ *' Medium (md - No *'