Dj. Eldridge et Pia. Kinnell, ASSESSMENT OF EROSION RATES FROM MICROPHYTE-DOMINATED CALCAREOUS SOILS UNDER RAIN-IMPACTED FLOW, Australian Journal of Soil Research, 35(3), 1997, pp. 475-489
Intact soil monoliths with surfaces of varying microphytic crust cover
were collected from a calcareous earth soil in a semi-arid belah-rose
wood woodland near Wentworth in south-western New South Wales. Monolit
hs were tested for their susceptibility to erosion by rain-impacted fl
ow using a laboratory rainfall simulator. The erosive stress applied t
o each surface was controlled by varying the flow depth between 4 and
8 mm whilst maintaining a flow velocity of 25 mm/s using 2.7 mm raindr
ops falling 11.2 m at average rainfall intensities of 65 mm/h. Increas
ing the cover of microphytic crusts on the surface resulted in a signi
ficant (P = 0.001) reduction in sediment concentration. A linear model
incorporating percentage cover and distribution of cover accounted fo
r 46% of the variance in soil erosion. A significant relationship was
also found between the coarse fraction (>0.053 mm) and crust cover (P
= 0.012) at the dmm depth. Management practices such as overgrazing, t
rampling, and fire, which reduce the cover of crusts in this landscape
, will lead to increased erosion hazard.