CHARACTERISTICS OF MACROPOROSITY IN A REDUCED TILLAGE AGROECOSYSTEM WITH MANIPULATED EARTHWORM POPULATIONS - IMPLICATIONS FOR INFILTRATION AND NUTRIENT TRANSPORT
Sl. Lachnicht et al., CHARACTERISTICS OF MACROPOROSITY IN A REDUCED TILLAGE AGROECOSYSTEM WITH MANIPULATED EARTHWORM POPULATIONS - IMPLICATIONS FOR INFILTRATION AND NUTRIENT TRANSPORT, Soil biology & biochemistry, 29(3-4), 1997, pp. 493-498
The effects of macroporosity on the potential for nutrient transport h
as been extensively studied for no-tillage agroecosystems. The present
study was undertaken to quantify macroporosity and to demonstrate the
potential for nutrient transport in reduced-tillage systems. Soil mac
ropore area and numbers were quantified by image analysis into three s
ize classes (1-8, 8-16 and >16 mm(2)) at three depths (10, 20 and 30 c
m) at two locations (between-row, within-row) in corn agroecosystem en
closures with manipulated earthworm populations (reduction, not manipu
lated, addition). A dilute solution of latex paint was surface-applied
to determine pathways for water infiltration. All macropore sizes con
tributed to infiltration. Earthworm-treatments had no significant effe
cts on infiltration rates, but rates were significantly faster within
crop rows than between rows. In the earthworm-addition plots the area
of macropores was significantly greater in the surface soil (10 cm dep
th) then in the other treatments, indicating re-formation of continuou
s flow pathways destroyed by tillage practices. The majority of the >1
6 mm(2) size pores were recognized as Lumbricus terrestris (L.) burrow
s, which represented the greatest per cent area of all size classes at
the 10 cm depth. The area of these large macropores was significantly
greater in addition-treatments than in the other plots at all depths
and locations except for 30 cm-deep between-row locations. The absence
of an earthworm effect at this location is attributed to the existenc
e of pre-existing burrows that were not disrupted by tillage or root a
ctivity and is due to earthworms concentrating their activity in the r
oot-zone, in the within-row location. By increasing soil macroporosity
and creating transport pathways of preferential flow, earthworms pote
ntially affect the nutrient transport in leachate and nutrient loss fr
om the agroecosystem. (C) 1997 Elsevier Science Ltd.