Zeekoevlei / Rondevlei Rehabilitation Study ... - Southern Waters
Zeekoevlei / Rondevlei Rehabilitation Study ... - Southern Waters
Zeekoevlei / Rondevlei Rehabilitation Study ... - Southern Waters
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<strong>Southern</strong> <strong>Waters</strong> Ecological Research and Consulting<br />
2. Background to the <strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> <strong>Rehabilitation</strong><br />
<strong>Study</strong><br />
2.1 The Problems – History And Causes<br />
<strong>Zeekoevlei</strong> and <strong>Rondevlei</strong> exist as two adjacent shallow vleis (lacustrine wetlands) that are<br />
physically separate in terms of their surface characteristics, but linked via groundwater not<br />
only to each other, but to the pattern of sub-surface water movement across the Cape Flats in<br />
the general direction of False Bay. Despite their geographic proximity, the vleis are managed<br />
separately for the purposes of recreation (<strong>Zeekoevlei</strong>) and nature conservation (<strong>Rondevlei</strong>).<br />
For several decades (almost 80 years for <strong>Zeekoevlei</strong>), both vleis have been subject to water<br />
level controls and/or excessive loads of catchment-derived nutrient enrichment or deliberate<br />
waste disposal, with the effects thereof being evident particularly in <strong>Zeekoevlei</strong> as sustained<br />
blooms of blue-green algae and accelerated accumulation of organically-rich sediment. The<br />
non-limiting availability of phosphorus, in particular, has for many years been recognized as<br />
the cause of high levels of both plants and algae. The consequence of this sustained impact<br />
has been a loss of biodiversity and reduced ecosystem health. Both vleis exhibit the effects of<br />
eutrophication common in shallow, well-mixed lakes where natural cycles of flushing and<br />
water level variation have been tampered with.<br />
Eutrophication (from the Greek meaning well-nourished), refers to excessive enrichment of<br />
a waterbody by the plant nutrients nitrogen and phosphorus, usually the consequence of<br />
deliberate (“point source”) discharges, or the combined impact of polluted runoff (“diffuse<br />
pollution”) emanating from the catchment(s) draining into a river, lake or wetland. The effect<br />
may be sudden, i.e., the after effects of a single spill or discharge, or alternatively slow and<br />
insidious, with the receiving water changing progressively through increasing levels of<br />
enrichment from oligo- (poor) to hypereutophic (grossly enriched). The typical consequences<br />
of eutrophication are imbalanced algal and/or plant growth, reduced water clarity, reduced<br />
oxygen availability, blooms of toxic algae, fish kills and increased levels of (organic)<br />
sedimentation. The process is often accompanied by an increasing level of resistance to<br />
restoration or rehabilitation, i.e., the longer the impact is allowed to continue, the more<br />
difficult it is to remedy. While eutrophication is relatively easy to diagnose, it is exceedingly<br />
difficult to reverse.<br />
<strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> <strong>Rehabilitation</strong> <strong>Study</strong>: Action Plan<br />
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