Ra. Sutherland et Ad. Ziegler, A NEW APPROACH TO DETERMINING WATER-STABLE AGGREGATION, Communications in soil science and plant analysis, 28(19-20), 1997, pp. 1871-1887
A new method is introduced to measure water stability of soil aggregat
es. The wrist-action shaker is a simple, inexpensive tool that provide
s highly accurate data for the assessment of soil erodibility. Three s
oils from Hawaii (two Oxisols and one Vertisol) with different mineral
ogies, management histories, and potassium (K)-factors were examined i
n this study. Six indices of water stable aggregation were determined
after rapid immersion of air-dry aggregates, followed by gentle wet-si
eving. Single-sieve indices of percent water stable aggregates (WSA) <
0.063 mm, > 0.25 mm, and > 1.00 mm, were highly correlated. Additiona
lly, these indices were highly correlated with three multiple sieve in
dices, namely geometric mean aggregate diameter (GMAD), arithmetic mea
n aggregate mass diameter (MAMD), and the coarse-to-fine index (CFI =
% WSA > 1.00 mm / % WSA < 0.063 mm). Analysis of WSA data indicated th
at the relative soil erodibility ranking, from high to low, would be:
Lualualei Vertisol > Molokai Oxisol > Kaneloa Oxisol. Discriminant ana
lysis using GMAD and % WSA > 1.00 mm correctly classified 55 of 56 soi
l samples into their respective soil series.