Abstract:
The major reason for the top soil erosion linked with the disruption of aggregates is
identified as the rapid wetting rates of surface soils. Hydrophobicity (water repellency)
is a property of soils that reduces their affinity for water and their infiltration capacity,
which may help impeding the pressure buildup within aggregates, and reduces aggregate
disruption. A relationship would be helpful to interpret aggregate stability considering
the hydrophobicity and initial wetting rates, which will be represented with contact angle
and water drop penetration time (WDPT), respectively. The purpose of this study was
to develop a relationship to identify the most suited initial wetting rates to achieve the
most durable stability for aggregates while preventing the floating of dry aggregates using
a Japanese surface Andisol. Soil was hydrophobized using stearic acid into different
hydrophobicities and the contact angle was measured using the sessile drop method. To
determine the water stability of aggregates (%WSA), model aggregates were placed in a 0.5
mm sieve, immersed in water and kept overnight. The total floating time of each aggregate,
was recorded. The %WSA increased as the contact angle increased with increasing stearic
acid content. Aggregate floating started when the contact angle exceeds ioo° and a similar
trend was observed with WDPT. As the wetting rate decreased, the 96WSA increased.
Floating appeared when WDPT exceeded 2 s. Considering the 1 s floating as the critical
point, the hydrophobicity level and the wetting rate which provide maximum %WSA was
decided to be around ioo° and ~2 s, respectively. Although the %WSA increased with
increasing contact angle and WDPT above this level, those levels were considered not
suitable considering the risk of undesirable effects of water repellency. The results revealed
the most suited initial wetting rates to achieve the most durable stability for aggregates
while preventing the floating of dry aggregates for the examined Japanese Andisol. This
further indicates that the contact angle and wetting rate, as measured by WDPT, are
closely related with the water stability of aggregates. The results further confirm that high
levels of hydrophobicities would induce aggregate floating and further loss of top soil.
