Table 4 Summary table: slope (m), regression coefficient (b), and the determination coefficient (r2). (a) experiment 1. (b) experiment 2.
From: Quantitative determination of the mineral content of settleable particulate matter samples
Standard Corundum (d = 1,737Å) | m | b | r2 |
|---|---|---|---|
(a) | |||
Quartz (d = 4,238Å) | 0.582 | − 0.062 | 0.977 |
Calcite (d = 3,029Å) | 0.043 | 0.003 | 0.983 |
Dolomite (d = 2,8786Å) | 0.040 | − 0.006 | 0.948 |
Kaolinite (d = 7,152Å) | 0.237 | 0.057 | 0.988 |
Illite-Mus. (d = 9,861Å) | 0.863 | 0.004 | 0.988 |
(b) | |||
Quartz (d = 4,238Å) | 0.614 | − 0.019 | 0.989 |
Calcite (d = 3,029Å) | 0.134 | 0.006 | 0.985 |
Dolomite (d = 2,8786Å) | 0.169 | − 0.013 | 0.986 |
Kaolinite (d = 7,152Å) | 0.378 | 0.049 | 0.986 |
Illite-Mus. (d = 9,861Å) | 1.103 | 0.015 | 0.995 |
