Grain surface

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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.

Table: Surface, volume and specific surface
for different grain diameters at a density of 2.6 g / cm³
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

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