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Understanding River Landscapes

Naturally Forested Headwaters

Headwater streams across much of humid Australia are the common, small narrow streams that collect much of the runoff and feed it into the larger creeks and rivers. They are found throughout catchments, in the uplands around the edges of a catchment and along the lowlands, plains, and coast. They are naturally forested and wooded, but in cases where the vegetation has been cleared, they tend be highly degraded. The impact of agriculture and pastoral activities on headwater streams is significant, with only a few examples of these streams remaining intact in National Parks and other State Reserves. In situations where vegetation is cleared, the form of the river is fundamentally changed (bed and banks), as is the wildlife it supports and the balance of the processes controlling it. The diagram below explains some of the key processes at work in these streams and how the removal of vegetation significantly impacts upon river functioning:

<table border='0' cellspacing='0' cellpadding='0'> <tr valign='top'><td><img height="249" width="400" src="graphics/map3_lib.gif" alt="Naturally Forested Headwaters" border="0"> <ul> <li><a href="#shade">shade</a> <li><a href="#buffering">buffering</a>, and <li><a href="#floodcontrol">flood control</a> </ul> <p>Other significant processes are:</p> <ul> <li>supply of <a href="#woodydebris">woody debris</a>, and <li><a href="#erosioncontrol">erosion control</a> </ul> <p><a name="shade">&nbsp;</a></p> <h3>Shade</h3> <p>The provision of shade is a crucial process because headwater streams are small enough that the canopy of the tress can completely cover the stream. This modifies light and temperature, contributing in turn to water quality, <a class='glossaryitem' href="glossary.htm#Aquatic%20Habitat" onMouseover='showTerm(event,"Physical environment of streams.")' onmouseOut='hideTerm();'>aquatic habitat</a>, and control of weeds. When designed well, shade can also enhance agricultural productivity.</p> <p><a href="shading.htm">Click for other benefits of shading.</a></p> <p><a name="buffering">&nbsp;</a></p> <h3>Buffering</h3> <p>Most of the runoff comes first into headwater streams before it reaches the main river. Relatively little runoff enters the main river directly from the land. Thus the ability of riparian lands in headwater streams to buffer the contaminants coming from the land is a crucial control on water quality throughout the river.</p> <p><a href="buffering.htm">Click for other benefits of buffering.</a></p> <p><a name="floodcontrol">&nbsp;</a></p> <h3>Flood control</h3> <p>Flooding along rivers causes concern because of the impact it can have on <a href="agriculture.htm#flooding">agricultural production</a> and other land uses. When large rivers flood, the scale of the flows is large relative to the influence of vegetation and woody debris. In contrast, vegetation and <a class='glossaryitem' href="glossary.htm#Large%20Woody%20Debris" onMouseover='showTerm(event,"The sticks, branches, trunks and whole trees that fall into rivers and streams.")' onmouseOut='hideTerm();'>woody debris</a> in small headwater streams have a strong local influence and can retard flows and dampen flood peaks.</p> <p><a href="floodcontrol.htm">Click for more info</a></p> <p><a name="woodydebris">&nbsp;</a></p> <h3>Woody debris</h3> <p><a class='glossaryitem' href="glossary.htm#Large%20Woody%20Debris" onMouseover='showTerm(event,"The sticks, branches, trunks and whole trees that fall into rivers and streams.")' onmouseOut='hideTerm();'>Woody debris</a> accumulates easily in headwater streams, as the flows have insufficient power to sweep the fallen trees away. Many trees actually span the streams. This debris is most important as physical habitat in headwater streams, and for flood and erosion control.</p> <p><a href="woodydebris.htm">Click for more info</a></p> <p><a name="erosioncontrol">&nbsp;</a></p> <h3>Erosion Control</h3> <p>In headwater streams, there is only limited power of flows to erode stream banks. Thus vegetation alone can be a very effective stabiliser of the banks. Accelerated erosion of headwater streams can cause problems of water quality and habitat degradation far downstream, and local problems of weed invasion. Headwater streams do not erode very far so that damage of agricultural land is only an issue when there is rapid headward migration of <a class='glossaryitem' href="glossary.htm#Gully" onMouseover='showTerm(event,"A deeply eroded channel or small stream that has cut into the land where a stream would not usually be found; in a paddock for example.")' onmouseOut='hideTerm();'>gullies</a> and <a class='glossaryitem' href="glossary.htm#Incised%20Channel" onMouseover='showTerm(event,"A stream that has eroded its bed and banks to several metres depth so that floods no longer flow onto the floodplain. In other words, the channel is obviously much larger for its catchment area than would be found naturally.")' onmouseOut='hideTerm();'>incised channels</a>. In many headwater streams it is the loosening of sediment from the banks that is the main erosion process. Vegetation can protect the banks from extremes of temperature, wetting and drying, and rainfall impact, which accelerate these processes.</p> <p><a href="erosioncontrol.htm">Click for more info</a></p> </td><td>&nbsp;&nbsp;&nbsp;</td><td><p class='photocaption'>You are seeing the non-interactive version of this page.</p> <p class='photocaption'>This maybe because your browser settings prevent you from viewing Macromedia Flash, or you may not have the Macromedia Flash player installed.</p> <p class='photocaption'>The Macromedia Flash player is <a class='photocaption' href="../../www.macromedia.com/go/getflashplayer/index.htm">available from the Macromedia site</a>.</p> </td></tr></table>
Shading | Buffering | Flood control

 

See also Rivers as Ecological Systems Chapter 2.