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Dealing with salinity in Wheatbelt Valleys - Department of Water

Dealing with salinity in Wheatbelt Valleys - Department of Water

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In summary the picture is one <strong>of</strong> an agriculture that<br />

does not have the capacity to f<strong>in</strong>ance large-scale<br />

change. However there are also <strong>in</strong>dications that<br />

some past downward trends <strong>in</strong> the <strong>Wheatbelt</strong><br />

economy may be stabilis<strong>in</strong>g, re<strong>in</strong>forc<strong>in</strong>g the region’s<br />

ongo<strong>in</strong>g role as a major contributor to the economy<br />

and community <strong>of</strong> Western Australia.<br />

WHY PERENNIALS?<br />

Perennial plants <strong>in</strong>vest a large proportion <strong>of</strong> their<br />

resources to develop deep root systems and so get<br />

access to deeply <strong>in</strong>filtrat<strong>in</strong>g water. Access to deep<br />

moisture permits a longer active grow<strong>in</strong>g season and<br />

greater water use than can be achieved by annual<br />

plants. Sal<strong>in</strong>ity researchers agree that perennials will<br />

elim<strong>in</strong>ate recharge over the area on which they stand<br />

where annual ra<strong>in</strong>fall is less than 600 mm. There is<br />

however debate about whether relatively small areas<br />

<strong>of</strong> perennial plants might <strong>in</strong>tercept significant surface<br />

and subsurface flows <strong>of</strong> water from adjacent annual<br />

crops or pastures. Hatton & George (2001) review<br />

the circumstances where this will occur. The extent<br />

to which water will move to trees is favoured by<br />

slop<strong>in</strong>g land, less sal<strong>in</strong>e groundwater, th<strong>in</strong>ner regolith<br />

(

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