Rapid assessment of soil compaction damage II. Relationships between the SOILpak score, strength and aeration measurements, clod shrinkage parameters, and image analysis data on a Vertisol
D. C. McKenzie
Australian Journal of Soil Research 39(1) 127 - 141
Abstract
Compacted and well-structured sites, on a Vertisol used for irrigated cotton
production, were compared using a range of procedures for assessing soil
structural form. The techniques considered were: visual/ tactile
assessment using the SOILpak score, shear strength, penetration resistance,
core bulk density and air-filled porosity, clod shrinkage analysis, and image
analysis. All of the methods under consideration distinguished compacted soil
from well-structured soil, including core bulk density, which had previously
been thought of as a poor measure of soil structure in Vertisols. The simple
SOILpak scoring procedure was shown to have great potential as a tool for land
managers. Soil factors known to directly affect root growth, mechanical
impedance and aeration, correlated well with the indirect procedures. The
cheaper methods (SOILpak score and core bulk density determination) related
most strongly to shear strength at the reference water content (plastic
limit). The SOILpak score was more strongly related to air-filled porosity
than clod shrinkage analysis or image analysis; shear strength had the same
predictive power as the SOILpak score for estimating air-filled porosity.
However, an advantage of using resin-impregnated soil monoliths and the
SOLICON image analysis system is that the samples are big enough to represent
a large proportion of the root-zone. Staining of the soil with a Rhodamine dye
solution provided images that were too coarse for the routine determination of
SOLICON parameters, but it is a useful and rapid procedure for highlighting
those macropores that are connected with the soil surface. Clod shrinkage
parameters underestimated soil air-filled porosity where compacted aggregates
were interspersed with finely aggregated soil.
Keywords: soil structure, macropores, Vertosols, cotton, root growth, SOLICON.
Full text doi:10.1071/SR99117
© CSIRO 2001





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