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CONDITIONS OF SEDIMENTARY DEPOSITION.
509
ANALYSES—PARTS PER 1,000,000 OF WATER.
| Constituents. | Ottawa. | St. Lawrence. | Mississippi. | Missouri. | Missouri and Mississippi. | Missouri and Mississippi. |
|---|---|---|---|---|---|---|
| a | b | c | d | e | f | |
| Total Solids | — | — | 253.69 | 1207.66 | 1058.98 | 787.12 |
| Filtered sediment | 69.75 | 167.80 | 20.90 | 638.26 | 622.33 | 389.36 |
| K | 1.52[note 1] | 1.15[note 1] | not given | not given | not given | not given |
| Na | 2.39[note 1] | 5.03[note 1] | 3.37[note 1] | 12.76[note 1] | 9.16[note 1] | 10.37[note 1] |
| MgO | 2.36[note 1] | 12.08[note 1] | 28.26 | 41.96 | 37.51 | 39.40 |
| CaO | 13.88[note 1] | 44.92[note 1] | 52.93 | 110.15 | 109.63 | 94.90 |
| Cl | .76 | 2.42 | 5.31 | 19.53 | 14.22 | 15.93 |
| SO3 | 1.61 | 6.87 | 10.28 | 89.76 | 73.66 | 69.89 |
| SiO2 | 20.60 | 37.00 | not given | not given | not given | not given |
| 69.75 | 167.80 | 20.90 | 638.26 | 622.33 | 389.36 | |
| Iron and alumina | traces | traces | none | 55.84 | 20.90 | 26.80 |
According to Gooch[1] the combination in these analyses should be calculated in the order KCl, NaCl, K2SO4, Na2SO4, MgSO4, CaSO4, MgCO3, CaCO3, Na2CO3, etc.; and this is the order followed in the Canadian analyses. Hence the following is the hypothetical combination.
| a | b | c | d | e | f | |
|---|---|---|---|---|---|---|
| Total Solids | — | — | 253.69 | 1207.66 | 1058.98 | 787.12 |
| Filtered sediment | 69.75 | 167.80 | 20.90 | 638.26 | 622.33 | 389.36 |
| KCl | 1.60 | 2.20 | not given | not given | not given | not given |
| NaCl | — | 2.25 | 8.57 | 32.03 | 23.30 | 26.38 |
| K2SO4 | 1.22 | — | not given | not given | not given | not given |
| Na2SO4 | 1.88 | 12.29 | not given | not given | not given | not given |
| Mg SO4 | none | none | 15.41 | 125.90 | 118.49 | 104.83 |
| Ca SO4 | none | none | none | 9.93 | none | none |
| Mg CO3 | 6.96 | 25.37 | 19.63 | none | 1.37 | 4.28 |
| Ca CO3 | 24.80 | 80.83 | 94.56 | 189.35 | 195.79 | 169.47 |
| Na2CO3 | 4.10 | 0.61 | none | none | none | none |
| Fe2O3 + Al2O3 | traces | traces | none | 55.84 | 20.90 | 26.80 |
The chemical reactions which take place between substances dissolved in river waters and those contained in salt water are no doubt complex; but that which is most significant in relation to possible precipitation of carbonate of lime depends upon the fact that organic matter may decompose sulphate of lime. Ac-
- ↑ Analyses of Waters of the Yellowstone National Park,Bull. U. S. G. S., No. 47, p.24