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Figure 92. Oblique air pho<strong>to</strong>s of Horseshoe Lagoon looking East.<br />

4.3 Water quality<br />

Section 4.1 discussed human and animal activity and distribution, and Section 4.2 foc<strong>used</strong><br />

on processes affecting water volume and sediment load in key lagoons. Both of these issues<br />

are potentially significant <strong>to</strong> station water quality in general, and <strong>to</strong> water quality in those key<br />

lagoons in particular. Information in Section 2.2.5 and elsewhere suggests that water quality<br />

is impacted by a range of fac<strong>to</strong>rs including:<br />

Increased sediment loads in water ca<strong>used</strong> by landscape processes (erosion, fire,<br />

grazing, etc.)<br />

Turbidity ca<strong>used</strong> by animal activity directly in or adjacent <strong>to</strong> water (including large<br />

terrestrial animals like pigs and cattle, as well as naturally occurring turbidity ca<strong>used</strong><br />

by aquatics);<br />

Larger dead animals in or adjacent <strong>to</strong> the water (either naturally occurring or<br />

deli<strong>be</strong>rately shot);<br />

Sediment or chemical inputs from human activities (most significant for the<br />

homestead, cattle yards, roads close <strong>to</strong> lagoon banks or inlet or outlet channels, etc.);<br />

Oriners cattlemen referred <strong>to</strong> Oriners Lagoon water <strong>be</strong>ing „milky‟ in the past, particularly in<br />

the late dry season (but that floodwater ran clear in the wet). Clearly there is a natural<br />

sediment load in the system, but seasonal increases in this load do <strong>not</strong> render lagoon water<br />

undrinkable (or pose immediate risks <strong>to</strong> aquatic species). This „milky‟ appearance late in the<br />

dry season is likely a result of the suspension of small clay particles (colloidal clays <strong>with</strong><br />

electric charge) that do <strong>not</strong> readily settle out. This is largely a natural phenomenon, but could<br />

<strong>be</strong> enhanced by excess clay sediment delivered <strong>to</strong> the lagoon from land-use impacts. More<br />

significant water quality risks <strong>to</strong> the major lagoons lie from inputs by humans and larger<br />

animals. More frequent and extended residence at Oriners increases the need for adequate<br />

water quality, but also increases the chance that the immediate risks <strong>to</strong> quality can <strong>be</strong> <strong>be</strong>tter<br />

managed. A model for water quality will <strong>not</strong> <strong>be</strong> produced here, but it remains a relevant issue<br />

in a synthesis foc<strong>used</strong> on the implications of greater human residence and on the volume<br />

and status of key permanent lagoons.<br />

Working Knowledge at Oriners Station, Cape York<br />

196

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