The density of particle aggregates

1997 ◽  
Vol 36 (4) ◽  
pp. 1-13 ◽  
Author(s):  
John Gregory

Aggregates of particles formed in coagulation/flocculation processes very often have a fractal, self-similar structure, with the very important practical consequence that the effective density of aggregates decreases as their size increases. This has very significant effects on separation processes such as sedimentation, flotation and filtration. The fundamental factors which influence the density of aggregates (flocs) are reviewed, with a discussion of the effects on aggregate size distribution, the rate of formation of flocs and their capture by collectors. Several experimental methods for determining floc density are critically examined.

2021 ◽  
Vol 211 ◽  
pp. 105023
Author(s):  
C. Polakowski ◽  
A. Sochan ◽  
M. Ryżak ◽  
M. Beczek ◽  
R. Mazur ◽  
...  

Soil Research ◽  
1995 ◽  
Vol 33 (1) ◽  
pp. 153 ◽  
Author(s):  
AJ Gijsman ◽  
RJ Thomas

This study evaluated soil aggregate size distribution and stability of an Oxisol under improved grass-only or grass-legume pastures, established in previously native savanna. Three grass-legume combinations were included at various stocking rates. In all treatments and soil layers, soils were well aggregated, having more than 90% of their weight in macroaggregates (>250 �m). The addition of legumes to pastures did not affect the soil aggregate size distribution, although aggregates showed somewhat more stability against slaking. An increase in stocking rate negatively affected both average aggregate size and aggregate stability. Aggregates showed little or no dispersion of clay particles in any treatment. A positive correlation was found between wet aggregate stability and hot-water extractable carbohydrate concentration, supporting the hypothesis that these carbohydrates equate with plant-derived or microbial polysaccharides which glue soil aggregates together. It is suggested that determination of hot-water extractable carbohydrates may serve as a useful indicator of small differences in aggregate stability, even when these differences are not evident in the stability measurement itself.


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