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20<br />

Wilson’s work is particularly <strong>in</strong>terest<strong>in</strong>g <strong>in</strong> its implications. It suggests that by <strong>in</strong>creas<strong>in</strong>g break width<br />

from merely 3 m to 4 m, the <strong>in</strong>tensity <strong>of</strong> a <strong>fire</strong> that can just be prevented from cross<strong>in</strong>g the break,<br />

rises from 6.3 MW m-1 to 11.3 MW m-1 – a substantial rise. A <strong>fire</strong> <strong>in</strong>tensity <strong>of</strong> 9 MW m-1 could arise<br />

from a fuel load <strong>of</strong> 5 t ha-1 (0.5 kg m-2 ) and a rate <strong>of</strong> <strong>for</strong>ward <strong>fire</strong> spread <strong>of</strong> 1 m sec-1 (3.6 km hr-1 ), if<br />

the same heat yield as used by Wilson (18,000 kJ kg-1 ) was adopted. Wilson’s model suggests that<br />

with a modest <strong>in</strong>crease <strong>in</strong> the width <strong>of</strong> a break, there is a large <strong>in</strong>crease <strong>in</strong> the <strong>in</strong>tensity <strong>of</strong> <strong>fire</strong> that can<br />

be passively controlled. This only applies <strong>in</strong> grasslands where no spot <strong>fire</strong> is likely.<br />

The model discussed above is the simpler <strong>of</strong> the two that Wilson (1988) produced. The other much<br />

more complicated model gives the probability <strong>of</strong> spann<strong>in</strong>g a break <strong>for</strong> <strong>fire</strong>s <strong>of</strong> various <strong>in</strong>tensities<br />

burn<strong>in</strong>g <strong>in</strong> grassland fuels with trees at various distances from the break. This model predicts that<br />

the approximate probability <strong>of</strong> bridg<strong>in</strong>g a 3 m wide break is 29% <strong>for</strong> a 2 MW m-1 (2,000 kW m-1 )<br />

<strong>fire</strong>. Trees near a break can markedly reduce the value <strong>of</strong> a break <strong>in</strong> stopp<strong>in</strong>g <strong>fire</strong>s because <strong>of</strong> their<br />

propensity to produce l<strong>of</strong>ted <strong>fire</strong> brands. Thus the effectiveness <strong>of</strong> a fuel break <strong>in</strong> <strong>for</strong>ests is markedly<br />

reduced, compared with that <strong>in</strong> grasslands.<br />

Flame length is harder to measure than break width: flames pulsate so length varies all the time,<br />

thereby mak<strong>in</strong>g objective measurement difficult. What is actually taken as flame length is probably<br />

the average length <strong>of</strong> the longer flames, rather than the maximum lengths <strong>of</strong> flames (e.g. flares). If a<br />

photograph is taken, the variation can be observed. The measurement <strong>of</strong> flame height was discussed<br />

<strong>in</strong> detail by Gill et al. (1987a). The same pr<strong>in</strong>ciples apply to length. On the CSIRO Grassland Fire<br />

Spread Meter (CSIRO 1997) there is the comment that ‘flashes <strong>of</strong> flame may extend to twice [given]<br />

values’, the maximum height (not length) given there be<strong>in</strong>g 4.4 m <strong>in</strong> natural pasture with the very<br />

rapid spread rate <strong>of</strong> 20 km hr-1 (5.6 m sec-1 ).<br />

Although there is no published data on the matter <strong>of</strong> flame height or length as a function <strong>of</strong> grass<br />

height and density, the CSIRO Grassland Fire Spread Meter notes that a shift from natural pasture<br />

(generally more than 50 cm tall) to grazed pasture (generally less than 10 cm tall) will halve, or more<br />

than halve, flame height <strong>for</strong> <strong>fire</strong>s travell<strong>in</strong>g up to 20 km hr-1 (5.6 m sec-1 ). Flame height is a curvil<strong>in</strong>ear<br />

function <strong>of</strong> rate <strong>of</strong> spread <strong>of</strong> the <strong>fire</strong> (Cheney and Sullivan 1997, p. 25). Rate <strong>of</strong> spread drops<br />

approximately 20% <strong>for</strong> <strong>fire</strong>s <strong>in</strong> natural pastures, compared to those under normal graz<strong>in</strong>g, but much<br />

more <strong>in</strong> eaten out pastures (ibid, p. 39). Note that the values on the meter are considered to be a<br />

guide only (CSIRO 1997).<br />

A logical consequence <strong>of</strong> Wilson’s research is that attention needs to be given to the details <strong>of</strong> break<br />

construction and ma<strong>in</strong>tenance. If the width changes even a little, the consequences can be large. If<br />

the break is poorly ma<strong>in</strong>ta<strong>in</strong>ed so that fuel cover is present to some extent, although slight, then the<br />

effective width <strong>of</strong> the break is reduced. A steep but relatively narrow grassy batter on the downhill side<br />

<strong>of</strong> a break can support quite a long flame, which may be well beyond that expected. Debris swept to<br />

the side <strong>of</strong> the break may be a weak l<strong>in</strong>k <strong>in</strong> terms <strong>of</strong> the effectiveness <strong>of</strong> the break when it is alight.<br />

While Wilson’s work rema<strong>in</strong>s valid <strong>for</strong> the conditions under which he worked, the person apply<strong>in</strong>g<br />

these f<strong>in</strong>d<strong>in</strong>gs to other situations may need to adapt them to local conditions. Indeed, Wilson himself<br />

po<strong>in</strong>ted out that ‘In southern Australia, <strong>fire</strong>breaks [i.e. fuel breaks] even wider than 10 m can be<br />

breached when w<strong>in</strong>ds are strong enough to transport surface debris such as smoulder<strong>in</strong>g animal<br />

manure’ (Wilson 1988). The composition <strong>of</strong> the particular grassland and other fuels <strong>of</strong> concern can<br />

be important. Luke and McArthur (1978, p. 107) note that spot <strong>fire</strong>s can be common up to 100 m<br />

ahead <strong>of</strong> the flame front <strong>in</strong> grassland <strong>fire</strong>s, due to carriage <strong>of</strong> burn<strong>in</strong>g seed heads <strong>of</strong> thistles, Phalaris<br />

(a pasture grass) or wheat, <strong>for</strong> example. While this suggests that <strong>in</strong> such circumstances an effective<br />

break would need to be 100 m wide, verge treatments, such as slash<strong>in</strong>g, may reduce the problem.<br />

Even so, Noble’s (1991) case history <strong>of</strong> an extremely fast and <strong>in</strong>tense grass<strong>fire</strong> <strong>in</strong> the River<strong>in</strong>a <strong>of</strong><br />

southern Australia is a cautionary one – the <strong>fire</strong> jumped a 54 m wide break. In northern Queensland<br />

woodlands, where grassy fuels predom<strong>in</strong>ate but trees are common, it is recommended that fuel<br />

breaks (see Plate 2.4) need to exceed one kilometre <strong>in</strong> width if they are to be effective <strong>in</strong> the late dry<br />

season when <strong>fire</strong>s are at their most <strong>in</strong>tense (Crowley et al. 2003).<br />

Fire and adaptive <strong>management</strong> <strong>Underp<strong>in</strong>n<strong>in</strong>gs</strong> <strong>of</strong> <strong>fire</strong> <strong>management</strong> <strong>for</strong> <strong>biodiversity</strong> <strong>conservation</strong> <strong>in</strong> reserves

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