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Dealing with salinity in Wheatbelt Valleys - Department of Water

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George and Coleman<br />

for example <strong>in</strong> the Central and Eastern <strong>Wheatbelt</strong><br />

from Tamm<strong>in</strong> (9.26%) to Merred<strong>in</strong> (2.3%) (George<br />

1990). These were considered to be an underestimate<br />

<strong>of</strong> the real extent <strong>of</strong> salt-affected land.<br />

In 1988, regional hydrologists <strong>of</strong> the WA <strong>Department</strong><br />

<strong>of</strong> Agriculture estimated areas <strong>of</strong> <strong>sal<strong>in</strong>ity</strong> and trends<br />

across the state. Anon (1988) describes that <strong>in</strong> the<br />

Eastern <strong>Wheatbelt</strong>, where at that time no substantive<br />

evidence <strong>of</strong> groundwater rise existed (bores drilled<br />

<strong>in</strong> 1985 onwards had too short a record), <strong>sal<strong>in</strong>ity</strong><br />

affected only 1.64% (based on ABS 1984 data) <strong>of</strong> the<br />

area and that potentially 10–20% was at risk. In<br />

1994, <strong>with</strong> better catchment mapp<strong>in</strong>g and longer<br />

groundwater records, Ferdowsian et al. (1996)<br />

<strong>in</strong>dicated as much as 9% <strong>of</strong> farmland was 'affected'<br />

by <strong>sal<strong>in</strong>ity</strong> to some degree (greater than 50% yield<br />

reduction). They concluded that <strong>sal<strong>in</strong>ity</strong> could<br />

potentially double and then double aga<strong>in</strong> (33%)<br />

before com<strong>in</strong>g to equilibrium <strong>in</strong> approximately 50 to<br />

200 years.<br />

At the time <strong>of</strong> writ<strong>in</strong>g, Land Monitor data from the<br />

Kellerberr<strong>in</strong>, Perth, Newdegate and Bencubb<strong>in</strong><br />

scenes are available for the central and Eastern<br />

<strong>Wheatbelt</strong>. Each scene represents over 1 M ha, and<br />

covers the area from Toodyay <strong>in</strong> the west, to<br />

Bullf<strong>in</strong>ch (north-east), Ravensthorpe (south-east),<br />

<strong>in</strong>clud<strong>in</strong>g a southern boundary near Lake Grace,<br />

Kond<strong>in</strong><strong>in</strong>, Quairad<strong>in</strong>g and P<strong>in</strong>gelly (Table 2). In this<br />

area, '<strong>sal<strong>in</strong>ity</strong>' has been def<strong>in</strong>ed and mapped as land<br />

hav<strong>in</strong>g 'consistent and low productivity due to<br />

shallow watertables'. It also <strong>in</strong>cludes many areas <strong>of</strong><br />

primary <strong>sal<strong>in</strong>ity</strong>, but usually excludes heavy barley<br />

grass pastures, sal<strong>in</strong>e remnants and lakes (water)<br />

which have been identified by field check<strong>in</strong>g. Field<br />

verified 'commission errors' (overestimates that<br />

<strong>in</strong>clude non-sal<strong>in</strong>e land) and 'omission errors'<br />

(underestimates <strong>of</strong> actual sal<strong>in</strong>e areas such as thick<br />

stands <strong>of</strong> barley grass and saltbush) are typically<br />

about 5% and 20% respectively. The process <strong>of</strong><br />

ground truth<strong>in</strong>g and statistical analysis has been<br />

described <strong>in</strong> more detail <strong>in</strong> each scene report which<br />

is available on the Land Monitor website<br />

(www.landmonitor.wa.gov.au/ – see Caccetta et al.<br />

2000; Caccetta et al. 2000b; Caccetta & Beetson<br />

2000; Dunne & Beetson 2000; Furby 2000).<br />

Table 2: Land Monitor statistics <strong>of</strong> the area <strong>of</strong> land classified as hav<strong>in</strong>g a low productivity attributed to <strong>sal<strong>in</strong>ity</strong><br />

(<strong>in</strong>cludes primary <strong>sal<strong>in</strong>ity</strong>; excludes most barley grass, saltbush, and lakes).<br />

Each scene is based on statistics from different set <strong>of</strong> satellite data.<br />

Scene/Shire<br />

Shire Area<br />

Ha<br />

Sal<strong>in</strong>e 1987–1991<br />

Ha (%)<br />

Sal<strong>in</strong>e 1995–1996<br />

Ha (%)<br />

Difference<br />

Ha (%)<br />

Kellerberr<strong>in</strong><br />

Merred<strong>in</strong> 329393 7537 (2.3)* 9138 (2.8) 1601 (0.5)<br />

Bruce Rock 272516 11517 (4.2) 12608 (4.6) 1091 0.4)<br />

Trayn<strong>in</strong>g 165196 6750 (4.1) 7577 (4.6) 827 (0.5)<br />

Kellerberr<strong>in</strong> 191554 11580 (6.0) 11964 (6.2) 384 (0.2)<br />

Tamm<strong>in</strong> 110246 7492 (6.8) 84176 (7.6) 925 (0.8)<br />

Bencubb<strong>in</strong><br />

Koorda 283197 41255 (14.56) 42619(15.05) 1346 (0.47)<br />

Dalwal<strong>in</strong>u 722135 83381 (11.5) 84412(11.69) 1031 (0.14)<br />

Wongan-Ballidu 336518 34232 (10.17) 36587(10.87) 2355 (0.7)<br />

Perth<br />

Cunderd<strong>in</strong> 186234 13032 (7.0) 13395 (7.2) 363 (0.2)<br />

Northam 143127 2606 (1.8) 2732 (1.9) 126 (0.08)<br />

York 213080 4537 (2.1) 4736 (2.2) 199 (0.09)<br />

Beverly 237118 6296 (2.7) 6663 (2.8) 367 (0.15)<br />

Chitter<strong>in</strong>g 121874 538 (0.4) 702 (0.6) 164 (0.13)<br />

Toodyay 169285 832 (0.5) 917 (0.5) 85 (0.05)<br />

Newdegate 1022162 63693 (6.2) 69507 (6.8) 5814 (0.57)<br />

* Percentage <strong>of</strong> Shire area as def<strong>in</strong>ed by Land Monitor.<br />

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