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and 27% of the soil surface at 80 m 3 /ha. Ammonia emissions were equivalent to a<br />

mean of 10% of the total N applied (range 7–14%) from the broadc<strong>as</strong>t application<br />

and a mean of 12% of the total N applied (range 7–20%) from the trailing shoe<br />

application (Figure 2).<br />

NH 3 loss (% N applied)<br />

30<br />

20<br />

10<br />

0<br />

20 35 50 65 80<br />

Application rate (m 3 /ha)<br />

Broadc<strong>as</strong>t<br />

Shallow injection<br />

Figure 1: Ammonia losses after shallow injection and broadc<strong>as</strong>t slurry<br />

applications to gr<strong>as</strong>sland in November 2003<br />

The higher hydraulic loading from the trailing shoe slurry application (11–30 mm per<br />

unit of surface area occupied by the slurry) compared with the surface broadc<strong>as</strong>t<br />

application (2–8 mm), meant that while the slurry stayed in a band, infiltration into<br />

the moist clay soil w<strong>as</strong> restricted (Table 1). Hence, the NH 3<br />

emission patterns and<br />

rates were similar from the two techniques, even though the emitting surface of the<br />

trailing shoe application w<strong>as</strong> only 18–30% that of the surface broadc<strong>as</strong>t application.<br />

Again, there w<strong>as</strong> no relationship (P > 0.05) between broadc<strong>as</strong>t or trailing shoe slurry<br />

application rates and NH 3<br />

emissions in March 2004.<br />

NH 3 loss (% N applied)<br />

30<br />

20<br />

10<br />

0<br />

Broadc<strong>as</strong>t<br />

Trailing shoe<br />

20 35 50 65 80<br />

Application rate (m 3 /ha)<br />

Figure 2: Ammonia losses after bandspread and broadc<strong>as</strong>t slurry applications<br />

to gr<strong>as</strong>sland in March 2004<br />

242

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