dc.description.abstract |
Soil water repellency is a phenomenon that soils resist wetting when water is
applied on the surface. Water repellency can be assumed to improve aggregate
stability as it may reduce rapid wetting and slaking of aggregates. Soil organic
matter (SOM) affects both of these properties by increasing or inducing water
repellency, and improving aggregate stability of soils. The present study was
conducted to find the existence of soil water repellency, aggregate stability,
measured as the percentage of water stable aggregates, and any possible relationship
between aggregate stability and soil water repellency in soils under different lancf
uses in Matara District, Sri Lanka. The effects of other physical properties of soil
such as SOM, clay content, and sand content on aggregate stability and soil water
repellency was also observed. The soil samples were collected from different
locations under different land uses (pine forest, pine grown together with other tree
species, coconut plantation, and beach soil). Surface soils from 0 tolO cm depth
were taken for the experiment. Soil water repellency was measured using the Water
drop penetration time (WDPT) test. The wet aggregate stability was measured using
two techniques. First technique was immersing the soil aggregates in distilled water
overnight (Technique 1), and the second technique was oscillation of soil
aggregates placed in a sieve through a vertical distance of 3 cm at a rate of 20
oscillations per minute for 2 minutes (Technique 2). Measurements were taken with
three replicates. The other soil properties such as the amount of SOM, clay, and
sand were measured using standard methods.
All the soil samples studied were found to be non- repellent (WDPT < Is).
However, the WDPT was found to be negatively correlated with SOM content.*The
clay and sand content did not show any correlation with the WDPT. There were no
effect of SOM, clay or sand on aggregate stability observed using both technique 1
and 2. There was no clear relationship between the aggregate stability and WDPT. |
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