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Dealing with salinity in Wheatbelt Valleys - Department of Water

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Scientists talk <strong>of</strong> up to 30% <strong>of</strong> the landscape<br />

generally be<strong>in</strong>g affected by <strong>sal<strong>in</strong>ity</strong>. Various figures<br />

are bandied around, but whatever figure is accurate,<br />

it means different th<strong>in</strong>gs to different people.<br />

Those fortunate enough to have land high <strong>in</strong> the<br />

catchment generally show little concern, as it is not<br />

their problem. They will never suffer much, if any,<br />

<strong>sal<strong>in</strong>ity</strong> on their properties. It is a problem <strong>of</strong> those<br />

neighbours lower <strong>in</strong> the landscape, not theirs.<br />

Landholders <strong>in</strong> the middle areas <strong>of</strong> the catchment are<br />

be<strong>in</strong>g forced to acknowledge that <strong>sal<strong>in</strong>ity</strong> may <strong>in</strong> fact<br />

be a problem for them, and not just those <strong>in</strong> the<br />

valley floors. This awaken<strong>in</strong>g is occurr<strong>in</strong>g due to<br />

"unexpla<strong>in</strong>ed" areas <strong>of</strong> salt affected land suddenly<br />

appear<strong>in</strong>g mid-slope, or runn<strong>in</strong>g up gullies, for no<br />

apparent reason. Unfortunately, there are also<br />

farmers who through no fault <strong>of</strong> their own have land<br />

low <strong>in</strong> the catchment <strong>in</strong> valley floors. These farmers<br />

face <strong>sal<strong>in</strong>ity</strong> on a daily basis. If 30% <strong>of</strong> each<br />

catchment becomes sal<strong>in</strong>e then the likely scenario<br />

for these farmers is almost total loss <strong>of</strong> their arable<br />

land. Farm<strong>in</strong>g, as they know it today, will disappear.<br />

This third sector <strong>of</strong> farmers is forced to accept the<br />

results caused not only by their excess water, but<br />

that <strong>of</strong> their upstream neighbours. This makes<br />

decision mak<strong>in</strong>g all the more difficult for them.<br />

The Lake Ch<strong>in</strong>ocup Catchment Committee began<br />

explor<strong>in</strong>g reasons for this <strong>in</strong>creased <strong>sal<strong>in</strong>ity</strong>.<br />

Frequently asked questions <strong>in</strong>cluded:<br />

• Is my <strong>sal<strong>in</strong>ity</strong> caused by my neighbour's water<br />

caus<strong>in</strong>g water table rises?<br />

• Is my <strong>sal<strong>in</strong>ity</strong> due to waterlogg<strong>in</strong>g?<br />

• Why is there suddenly an area <strong>of</strong> <strong>sal<strong>in</strong>ity</strong><br />

appear<strong>in</strong>g mid-slope?<br />

• Will plant<strong>in</strong>g trees solve my <strong>sal<strong>in</strong>ity</strong> problem?<br />

Morrell, Hatton and Curry<br />

Gett<strong>in</strong>g answers to our questions has always been<br />

difficult. When asked, <strong>of</strong>ten all we get is a lot <strong>of</strong> boot<br />

shuffl<strong>in</strong>g and evasive answers, as even the "experts"<br />

are not sure.<br />

The Lake Ch<strong>in</strong>ocup Catchment Resource<br />

Management Committee asked CSIRO Land and<br />

<strong>Water</strong>, plus the <strong>Department</strong> <strong>of</strong> Environmental<br />

Protection and Murdoch University, to assist <strong>in</strong><br />

answer<strong>in</strong>g some <strong>of</strong> these questions and give us a feel<br />

for what was happen<strong>in</strong>g <strong>with</strong><strong>in</strong> the catchment.<br />

SALINITY RISK ASSESSMENT OF LAKE<br />

CHINOCUP CATCHMENT<br />

In 2000, the Lake Ch<strong>in</strong>ocup Catchment<br />

commissioned an assessment <strong>of</strong> <strong>sal<strong>in</strong>ity</strong> risk under<br />

current and alternative land uses. The committee<br />

hoped to obta<strong>in</strong>:<br />

• A clearer awareness <strong>of</strong> the hydrological<br />

processes we are deal<strong>in</strong>g <strong>with</strong> <strong>in</strong> relation to our<br />

declared goal for manag<strong>in</strong>g ris<strong>in</strong>g water tables.<br />

• The best available <strong>in</strong>formation on options for<br />

future <strong>sal<strong>in</strong>ity</strong> management strategies.<br />

• A clearer <strong>in</strong>dication regard<strong>in</strong>g the timescale <strong>of</strong><br />

likely sal<strong>in</strong>isation and the w<strong>in</strong>dows <strong>of</strong><br />

opportunity for remedial action to reduce<br />

<strong>sal<strong>in</strong>ity</strong> risk <strong>in</strong> particular areas <strong>of</strong> the catchment.<br />

• A sounder basis on which to draw support for<br />

community plann<strong>in</strong>g and decision mak<strong>in</strong>g<br />

towards agreed sub-catchment scale<br />

environmental management goals which may be<br />

needed <strong>in</strong> relation to sav<strong>in</strong>g the natural diversity<br />

assets at risk <strong>in</strong> the Lake Ch<strong>in</strong>ocup Nature<br />

Reserve, and other reserves, remnant bush,<br />

listed wetlands and the many significant<br />

environmental values <strong>in</strong> the catchment, and<br />

downstream <strong>of</strong> it.<br />

• Why can't I dra<strong>in</strong> my groundwater <strong>of</strong>f my farm? • Advice on the extent and nature <strong>of</strong> any further<br />

• Are there farm<strong>in</strong>g systems currently available<br />

which will reverse my <strong>sal<strong>in</strong>ity</strong>?<br />

priorities for obta<strong>in</strong><strong>in</strong>g groundwater monitor<strong>in</strong>g<br />

data, or other l<strong>in</strong>es <strong>of</strong> monitor<strong>in</strong>g for<br />

environmental outcomes.<br />

• What can I do <strong>with</strong> my land that no longer<br />

susta<strong>in</strong>s a cereal crop? The report provided detailed descriptions <strong>of</strong> geology,<br />

• How can I rema<strong>in</strong> pr<strong>of</strong>itable?<br />

• What is a susta<strong>in</strong>able system <strong>of</strong> farm<strong>in</strong>g?<br />

• What percentage <strong>of</strong> my catchment, and my farm<br />

will go sal<strong>in</strong>e?<br />

• What needs to be done to save the vegetation<br />

found <strong>in</strong> the Lake Ch<strong>in</strong>ocup Reserve?<br />

– 7 –<br />

surface dra<strong>in</strong>age patterns, geomorphology and<br />

groundwater processes across the region. All<br />

available hydrological <strong>in</strong>formation was used to <strong>in</strong>fer<br />

groundwater levels and flow l<strong>in</strong>es. Due to the<br />

absence <strong>of</strong> adequate reduced water level data from<br />

exist<strong>in</strong>g bores, steady state water level maps were<br />

produced for the catchment us<strong>in</strong>g hydrogeomorphic<br />

pr<strong>in</strong>ciples (Salama et al. 1996b).

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