Redistribution of Slurry Components as Influenced by Injection Method, Soil, and Slurry Properties
Søren O. Petersen*,a,
Henrik H. Nissenb,
Ivar Lundc and
Per Ambusd
a Dep. of Agroecology, Danish Inst. of Agric. Sci., P.O. Box 50, DK-8830 Tjele
b Aalborg Univ., Dep. of Civil Engineering, Sohngaardsholmsvej 57, DK-9000 Aalborg
c Dep. Automation and System Engineering, Danish Inst. of Agric. Sci., P.O. Box 536, DK-8700 Horsens
d Risø National Lab., Dep. of Plant Res., P.O. Box 49, DK-4000 Roskilde, Denmark

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Fig. 1. A map of Denmark in northern Europe, showing the locations of the two experimental sites at 55°52' N, 9°49' E (Bygholm) and 56°29' N, 9°34' E (Foulum).
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Fig. 2. An example of the time course of water loss from slurry due to a water potential gradient. The slurry was enclosed in a dialysis membrane and submerged in a solution of polyethylene glycol (see text).
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Fig. 3. The experimental setup used for quantifying the air permeability of soil cores sampled from the wall of simulated injection slits. A constant head pressure of 1 kPa was used for the field measurements.
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Fig. 4. Soil moisture and apparent electrical conductivity in and around the injection slit was measured with a small printed circuit-board time-domain-reflectometry probe. (A) Design of the probe, with dimensions in mm. (B) Positions AD of the four probes installed in each profile; probes were positioned relative to the bottom of the injection slit.
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Fig. 5. Injection slits amended with labeled pig and cattle slurry were sampled after 24 h with a rectangular corer (14 x 4 x 8 cm, l x w x h). The blocks were sectioned as indicated.
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Fig. 6. The water loss from 22 cattle (white), pig (black), and anaerobically digested (gray) slurries as a function of slurry organic matter content for three selected water potentials. Water was extracted by dialysis with solutions of polyethylene glycol (30, 60, and 90 g L-1). Except for two outliers (square symbols), all measurements accommodated the relationship relative water loss = 1/(1 + aVS); VS = volatile solids, values of a (a function of water potential) (± SE) are inserted in the three plots.
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Fig. 7. Relationships between air flow and head pressure for soil (gravimetric soil moisture, 18.6%) compacted by pressures of 6, 12, and 18 kN m-2 (n = 6). The curvilinearity was caused by turbulent flow.
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Fig. 10. Ratios of atom % 13N to atom % 15N in each of the eight sections sampled in the field experiment with application of labeled slurry to slits prepared by simulated injection.
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Copyright © 2003 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.