Grain surface
The grain surface or specific surface (= surface area per unit weight) increases very sharply in batches of grain with decreasing mean grain diameter. In soil science and sedimentology , the grain size distribution plays an important role, because many properties of soils (more precisely the soil type ) and sediments depend on this composition; The grain surface is a measure of the expected water binding or ion exchange.
Because the grain diameter ranges are very large, they are measured at intervals of powers of ten with the factors 2 and 6.3, with 6.3 dividing the range between 2 and 20 on the logarithmic scale into equal sections.
The table gives the surface and the volume of the spherical individual grains as well as the number of these individual grains, which have a total volume of 1 cm³, for the limits of grain diameter ranges that are customary in soil science and sedimentology. Assuming a uniform density of 2.6 g / cm³, the number of grains per gram and the specific surface area are listed in m² / g.
Diameter mm |
Surface mm² |
Volume mm³ |
Number per cm³ 1 / cm³ |
Number per g 1 / g |
Surface area per g m² / g |
---|---|---|---|---|---|
2.0000 | 12,566371 | 4.1887902048 | 239 | 92 | 0.00116 |
0.6300 | 1.246898 | 0.1309243030 | 7638 | 2938 | 0.00366 |
0.2000 | 0.125664 | 0.0041887902 | 238732 | 91820 | 0.01154 |
0.0630 | 0.012469 | 0.0001309243 | 7638001 | 2937693 | 0.03663 |
0.0200 | 0.001257 | 0.0000041888 | 238732415 | 91820160 | 0.11542 |
0.0063 | 0.000125 | 0.0000001309 | 7638001324 | 2937692817 | 0.36721 |
0.0020 | 0.000013 | 0.0000000042 | 238732414638 | 91820159476 | 1.19366 |
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See also
swell
- Winfried EH Blum: Soil science in brief . Bornträger, Berlin, Stuttgart, 2007, ISBN 3-443-03117-X
- Karl Heinrich Hartge: Introduction to Soil Physics . Schweizerbart'sche Verlagbuchhandlung, 1999, ISBN 3-510-65223-1