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 />
<strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> <strong>Rehabilitation</strong> <strong>Study</strong><br />
Executive Summary<br />
<strong>Zeekoevlei</strong> and <strong>Rondevlei</strong> are adjacent, shallow lacustrine wetlands that, over a period of<br />
many decades, have acted as receiving waters for runoff and pollution from a combined<br />
catchment area of some 100 km 2 . The level of impact is such that restoration to natural<br />
condition is not possible and, given the hydraulic modifications to each vlei, impractical.<br />
However, rehabilitation to a vastly improved ecological condition in keeping with the<br />
ecological importance of these vleis remains a very real option. While the rehabilitation of<br />
these two vleis will be a costly and time-consuming process, the results are likely to be<br />
significant and economically- and ecologically-sustainable in the long term. Both vleis are<br />
eco-recreational resources of local and regional importance.<br />
The recommendations made in this report range from catchment level assessments of the<br />
efficacy of Best Management Practices, to gross rehabilitation activities required for<br />
<strong>Zeekoevlei</strong>. Some of the recommendations are not new, but their consideration in holistic<br />
terms has served to highlight their importance. It is apparent that, for <strong>Zeekoevlei</strong>, anything<br />
less than large scale and concerted effort will not achieve the desired aims and objectives.<br />
The report includes a detailed assessment of the possible management and rehabilitation<br />
options, and condenses those deemed workable into an Action Plan. The recommended<br />
actions are bolstered by a comprehensive assessment of monitoring and audit needs.<br />
The most difficult step in the rehabilitation of <strong>Zeekoevlei</strong>, and to a lesser extent <strong>Rondevlei</strong>,<br />
will be the implementation of the recommendations. These will require commitment from<br />
both the metropolitan and local authorities, as well as buy-in from all involved stakeholders.<br />
The present highly-impacted condition of these vleis is the product of years of abuse.<br />
Progress along the road to recovery will be slow and costly, but is achievable. It is estimated<br />
that implementation of the initial rehabilitation options will cost R17.5 million (at 2000 Rand<br />
values) over a period of 5 years, and with the lion’s share of this expenditure required for the<br />
gross rehabilitation of <strong>Zeekoevlei</strong>. It should be noted, however, that a major portion of the<br />
total cost (c. R8 million) is for the acquisition of dredging plant that is likely to also be needed<br />
at Princess Vlei, Zandvlei and several other vleis and rivers within the CMA. Accordingly,<br />
the initial cost could be spread over several rehabilitation programmes, thus reducing the<br />
burden on the <strong>Zeekoevlei</strong> project.<br />
<strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> <strong>Rehabilitation</strong> <strong>Study</strong>: Action Plan<br />
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Five Point <strong>Rehabilitation</strong> Action Plan Summary<br />
1. Reduce total annual loading of phosphorus to <strong>Zeekoevlei</strong> by 60% through:<br />
• dredging of 1.1 million m 3 of accumulated sediments;<br />
• attenuating the seepage of phosphorus-rich water from the adjacent<br />
wastewater treatment plant.<br />
Core programme cost over five years: R 13 000 000.<br />
(parallel reduction of pollution within the <strong>Zeekoevlei</strong> catchment is being<br />
investigated and costed by a separate study)<br />
2. Reduce total annual loading of phosphorus to <strong>Rondevlei</strong> by 45% through:<br />
• rehabilitation of the Princess Vlei ecosystem and, in particular, internal<br />
nutrient generation from the sediments and catchment management (30%<br />
total reduction);<br />
• implementation of Best Management Practices within the <strong>Rondevlei</strong><br />
catchment (10% total reduction);<br />
• wetland treatment of low flows during the dry season (5 % total reduction).<br />
Core programme cost over five years: R 3 500 000.<br />
3. Implement landuse planning and management policies to reduce the<br />
generation of nutrients at the catchment level, by:<br />
• imposition of non-structural Best Management Practices including<br />
legislation to reverse, modify or relocate identified polluting activities;<br />
• adopt and/or develop Best Management Practices to reduce nutrient<br />
generation by current landuse, or prevent same occurring from planned use;<br />
• apply economic benefit and regulatory mechanisms to encourage catchment<br />
and wetland management directed towards nutrient reduction.<br />
Core programme cost over five years: R 500 000.<br />
4. Monitor and audit water chemistry and biotic response of both vleis to the<br />
implemented rehabilitation (years 3-5).<br />
Core programme cost over five years: R 500 000.<br />
5. Reassess ecosystem health and functioning in terms of:<br />
• Post- vs pre-rehabilitation condition;<br />
• Attainment of water quality targets<br />
• Ecosystem structure, composition, functioning and direction of change,<br />
and determine second phase (year 5+) management needs, inclusive of a<br />
reassessment of the diversion option.<br />
Core programme cost over five years: R 600 000<br />
<strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> <strong>Rehabilitation</strong> <strong>Study</strong>: Executive Summary<br />
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Table of Contents<br />
Executive Summary<br />
i<br />
Action Plan<br />
1. Introduction 1<br />
1.1 How to Use this Document 1<br />
1.2 Contents of the Action Plan 1<br />
2. Background to the <strong>Study</strong><br />
2.1 The Problems: History and Causes 3<br />
2.2 Approach Adopted for this <strong>Study</strong> 4<br />
2.3 <strong>Rehabilitation</strong> vs Restoration 5<br />
3. The <strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> Environment and Ecology<br />
3.1 Geology and Climate 6<br />
3.2 Vlei morphology 6<br />
3.3 Ecology 7<br />
3.4 Wetland importance 7<br />
4. Issues, Options and Actions Required<br />
4.1 Major Issues 9<br />
4.1.2 The Key Role of Groundwater 9<br />
4.1.3 Other key findings related to groundwater 10<br />
4.2 Eutrophication and Phosphorus Loading 11<br />
4.2.1 Sources of Phosphorus Loading in <strong>Zeekoevlei</strong> 13<br />
4.2.2 Phosphorus Reduction Scenarios for <strong>Zeekoevlei</strong> 15<br />
4.2.2.1 Sediment Removal 15<br />
4.2.2.2 Seepage Curtailment 15<br />
4.3 Sources of Phosphorus Loading in <strong>Rondevlei</strong> 17<br />
4.3.1 Phosphorus Reduction Scenarios for <strong>Rondevlei</strong> 18<br />
4.4 Water Level Regulation and Drawdowns<br />
4.4.1 Response of <strong>Zeekoevlei</strong> to drawdowns 20<br />
4.4.2 Why drawdowns benefit <strong>Zeekoevlei</strong> 20<br />
4.4.3 Negative impacts of the drawdowns – midges 21<br />
4.4.4 Need for deep water areas and sediment removal 21<br />
4.4.5 Modification of drawdown rate and timing 22<br />
4.4.6 Impact on bird populations 23<br />
5. Secondary Issues<br />
5.1 Issues pertaining to fish populations 24<br />
5.2 Issues pertaining to midges 26<br />
5.3 Issues pertaining to faecal pollution and water quality 26<br />
Section A<br />
1. Background and Terms of Reference<br />
1.1 Background 1<br />
1.2 Terms of Reference 2<br />
1.3 Other Relevant Studies and Guidelines 3<br />
2. Approach and <strong>Study</strong> Team 7<br />
3. Historical Review<br />
3.1 Perspective of the Cape Flats vleis 13<br />
3.2 <strong>Zeekoevlei</strong> 14<br />
3.3 <strong>Rondevlei</strong> 24<br />
3.4 Concluding Remarks 29<br />
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4. Public Consultation Process<br />
4.1 Introduction 33<br />
4.2 Terms of Reference 33<br />
4.3 EIA Regulations 33<br />
4.4 Public Consultation Process 34<br />
4.5 Key Issues Raised 39<br />
Appendix A: Interested and Affected Parties 51<br />
Appendix B: Background Information Document 55<br />
Appendix C: Announcement of <strong>Study</strong> 61<br />
Appendix D: Notes of Meeting held 22 March 2000 63<br />
Appendix E: Notes of Meeting held 5 April 2000 73<br />
Appendix F: Copies of IAAP Submissions 77<br />
Section B: Specialist Reports<br />
1. Morphology and Bathymetry 1<br />
1.1 <strong>Zeekoevlei</strong> 2<br />
1.2 <strong>Rondevlei</strong> 4<br />
2. Geohydrology<br />
2.1 Introduction 7<br />
2.2 Background 11<br />
2.3 Geohydrological Description 23<br />
2.4 Vlei – Groundwater Interaction 39<br />
2.5 Management Measures 50<br />
2.6 Monitoring 57<br />
2.7 Conclusions and Recommendations 61<br />
Appendix A: Groundwater Fluxes through Unit Widths 71<br />
Appendix B: Wellpoint Data 73<br />
Appendix C: EC Depth Profiling Data 75<br />
Appendix D: Chemical Data 77<br />
Appendix E: Hydrocensus Data 79<br />
Appendix F: Groundwater Level Data 81<br />
3. Aquatic Ecosystem Assessments<br />
3.1 <strong>Zeekoevlei</strong><br />
3.1.1 Biotic and abiotic characteristics 83<br />
3.1.2 Management Issues 95<br />
3.1.3 <strong>Zeekoevlei</strong> and Trophic State Concepts 95<br />
3.1.4 Information Gaps 97<br />
3.1.5 Assessment Terms of Reference and Approach 97<br />
3.1.6 Phosphorus Load and Effect Modelling 98<br />
3.1.7 Wetland Assessment 113<br />
3.1.8 Summary and Recommendations 118<br />
3.2 <strong>Rondevlei</strong><br />
3.2.1 Biotic and abiotic characteristics 125<br />
3.2.2 Management Issues 128<br />
3.2.3 <strong>Rondevlei</strong> and Trophic State Concepts 128<br />
3.2.4 Information Gaps 130<br />
3.2.5 Assessment Terms of Reference and Approach 130<br />
3.2.6 Phosphorus Load and Effect Modelling 131<br />
3.2.7 Wetland Assessment 144<br />
3.2.8 Recommendations 155<br />
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3.3 Sediments<br />
3.3.1 Introduction 159<br />
3.3.2 Sediment Characteristics 159<br />
3.4 Issues pertaining to swarming insects (midges)<br />
3.4.1 Characteristics of non-biting midges 161<br />
3.4.2 Recent Incidence of midge problems 169<br />
3.4.3 Previous Studies 169<br />
3.4.4 Emergence Patterns and Control Mechanisms 170<br />
3.4.5 Possible cause for increased swarms 171<br />
3.4.6 Summary and Recommendations 171<br />
3.5 Management of Fish Populations<br />
3.5.1 Introduction 175<br />
3.5.2 Approach and Methodology 176<br />
3.5.3 Present Populations and Historic Changes 176<br />
3.5.4 Barriers to Fish Movement 180<br />
3.5.5 Facilitating Fish Movement 182<br />
3.5.6 Artificial Fish Introductions 185<br />
3.5.7 Effects of Drawdowns 186<br />
3.6 Effect of Drawdowns on Bird Populations<br />
3.6.1 Introduction 191<br />
3.6.2 Response to Drawdowns at <strong>Rondevlei</strong> 192<br />
3.6.3 Response to Drawdowns at <strong>Zeekoevlei</strong> 199<br />
3.7 <strong>Zeekoevlei</strong> Bacteriology (Faecal indicator bacteria)<br />
3.7.1 Introduction 203<br />
3.7.2 Data utilization and Approach 203<br />
3.7.3 Updated Assessment 204<br />
3.7.4 Conclusions 206<br />
3.8 Summarized Spatial Information<br />
3.8.1 Introduction 207<br />
3.8.2 Construction of Spatial Covers 207<br />
3.8.3 Description of Information per Cover 208<br />
Section C: Management Synthesis<br />
1. Concepts of Restoration, <strong>Rehabilitation</strong> and Remediation 1<br />
1.1 The Concept of Phosphorus as Limiting Nutrient 2<br />
2. Identification of Management Needs for <strong>Zeekoevlei</strong> 3<br />
2.1 The Case for Dredging 3<br />
2.2 Management Options 4<br />
2.3 Proposed Sequence of Rehabilitatory Options 5<br />
Schedule of Management Options for <strong>Zeekoevlei</strong> 6<br />
3. Identification of Management Needs for <strong>Rondevlei</strong> 10<br />
3.1 Management Options 10<br />
3.2` Proposed Timing of Rehabilitatory Options<br />
Schedule of Management Options for <strong>Rondevlei</strong> 12<br />
4. Matrices for watershed level BMP audit (<strong>Rondevlei</strong>) 15<br />
5. Monitoring Needs<br />
5.1 Introduction 23<br />
5.2 Data Management 23<br />
5.3 Surface Water Monitoring Requirements 24<br />
5.4 Monitoring Frequency: Determination of Loads 28<br />
5.5 Groundwater Monitoring Requirements 28<br />
5.6 Recommended Monitoring Protocol 30<br />
<strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> <strong>Rehabilitation</strong> <strong>Study</strong>: Action Plan<br />
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<strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> <strong>Rehabilitation</strong> <strong>Study</strong><br />
Action Plan<br />
1. Introduction<br />
1.1 How To Use This Document<br />
This section of the report on the <strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> <strong>Rehabilitation</strong> <strong>Study</strong> summarizes the<br />
identified core ecological problems prevailing in <strong>Zeekoevlei</strong> and <strong>Rondevlei</strong>, the associated<br />
key issues, and those options and actions deemed most likely to succeed in rehabilitating the<br />
vlei ecosystems.<br />
1.2 Contents of the Action Plan<br />
The <strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> <strong>Rehabilitation</strong> <strong>Study</strong> Report is comprised of four sections and<br />
supportive appendices, namely:<br />
• The Action Plan – this section should be read together with Section C;<br />
• Section A: Background to the study and details of the stakeholder involvement<br />
process;<br />
• Section B: Reports of the Specialist Studies;<br />
• Section C: Synthesis of rehabilitation options and monitoring requirements (for<br />
an initial period of five years following completion of this<br />
assessment).<br />
The Action Plan integrates the key findings of the study, and suggests actions recommended<br />
for the rehabilitation of the two vleis. The basis for the recommendations is provided in<br />
Sections B and C.<br />
<strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> <strong>Rehabilitation</strong> <strong>Study</strong>: Action Plan<br />
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The Action Plan ranks those actions that are deemed necessary to:<br />
• reduce the identified bulk sources of phosphorus reaching the vleis;<br />
• address those problematical issues that stem from the eutrophication of either system;<br />
• monitor the change in condition of the vleis in response to applied rehabilitatory<br />
procedures;<br />
• implement other ameliorative monitoring and management procedures that are<br />
required to ensure the future dynamic functioning of these wetland systems.<br />
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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 />
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Phosphorus as a limiting nutrient. “Life can multiply until all the phosphorus has gone and<br />
then there is an inexorable halt which nothing can prevent” (Isaac Asimov). Phosphorus is a<br />
key component of the molecule commonly known as ATP (adenosine triphosphate) – the<br />
molecule that provides the requisite energy for cell life. Accordingly, phosphorus is the<br />
limiting factor to life, both in water and on land. Phosphorus does not exist in nature in its<br />
elemental (P) form, but rather as one or other form of phosphate. Phosphorus cycles and<br />
recycles through organic (living) and inorganic (non-living) matter. The deleterious impacts<br />
of the disposal of phosphate-rich sewage effluent and/or detergent-rich grey water to lakes<br />
and rivers first became evident during the 1950s, and is now recognized as a global threat to<br />
water quality, ecosystem health and the recreational use of rivers and lakes. Phosphorus is<br />
not a pollutant or a toxicant, but a naturally scarce and life-supporting element that, when<br />
present in oversupply, frequently results in biological overgrowth. Its effective management<br />
and control, especially in shallow lakes and vleis, can reverse or prevent this process.<br />
2.2 Approach Adopted For This <strong>Study</strong><br />
A considerable and informative base of well-researched data exists for <strong>Zeekoevlei</strong>, and to a<br />
lesser extent for <strong>Rondevlei</strong>. As its fundamental points of departure, the <strong>Zeekoevlei</strong> /<br />
<strong>Rondevlei</strong> <strong>Rehabilitation</strong> <strong>Study</strong> encompassed the following key elements in its approach:<br />
• to not undertake or initiate any new collections of primary data other than to determine<br />
the role played by groundwater in the hydrological cycling and nutrient loading of these<br />
two vleis (an understanding of the role of groundwater in the hydrological and ecological<br />
functioning of the Cape Flats vleis has, for too long, been neglected;<br />
• to model the cause and effect linkages between the identified phosphorus loads, and the<br />
resultant in-lake condition;<br />
• to develop rehabilitation scenarios based on phosphorus reduction which, in conjunction<br />
with other management and/or biomanipulatory practices, would serve to reverse the<br />
extant extreme levels of eutrophication in each vlei.<br />
The primary focus of the study was to convert the existing knowledge and information into<br />
guidelines for rehabilitation.<br />
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2.3 The Concept Of <strong>Rehabilitation</strong> vs Restoration And Remediation<br />
In terms of formulating management needs and recommendations for <strong>Zeekoevlei</strong> and<br />
<strong>Rondevlei</strong>, it is important that the concepts of restoration, rehabilitation and remediation be<br />
defined. The concept of restoration implies an inherent degree of naturalness, viz. that<br />
whatever efforts are undertaken will strive to restore aspects such as vegetation, hydraulic<br />
and/or hydrological patterns, water quality or faunal composition to their natural condition.<br />
By contrast, rehabilitation recognizes that restoration may be neither pragmatic nor possible.<br />
However, the enhancement of core aspects of ecological functioning and processes, in order<br />
to resemble a semi-natural condition, is attainable. Remediation procedures are common for<br />
systems that have been grossly abused (e.g. mine tailing wetlands), and any semblance of<br />
original condition is no longer possible. Here the goal would be to improve the ecological<br />
condition, to an endpoint that is unlikely to mirror any previous natural state.<br />
The specialist investigations conducted for this study indicate that, for <strong>Zeekoevlei</strong>, any<br />
management approach should encompass a blend of rehabilitation and remediation options.<br />
In the case of <strong>Rondevlei</strong>, future management should be rehabilitation-focussed.<br />
<strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> <strong>Rehabilitation</strong> <strong>Study</strong>: Action Plan<br />
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3. The <strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> Environment and Ecology<br />
3.1 Geology and Climate<br />
<strong>Zeekoevlei</strong> and <strong>Rondevlei</strong> are situated in the winter-rainfall region of South Africa. Annual<br />
rainfalls average between 550 and 600 mm, with in excess of 80% of the total falling between<br />
April and September. Air temperatures range from minima of 11°C during July to 21°C<br />
during January and February, while water temperatures for these shallow vleis vary between<br />
12 and 23°C. The mean annual day length is 8 hours, with 3000 hours of bright sunshine<br />
measured during a typical year. The vleis experience a particularly windy climate, and with<br />
an almost total absence of calm conditions – measured as windspeeds of less than 6 m s -1 .<br />
Mean annual windspeeds exceed 6 m s -1 . The greater surface area of <strong>Zeekoevlei</strong> is<br />
completely mixed on a daily basis. Annual evaporation totals 1.4 m, i.e., a nett loss of 0.85m.<br />
3.2 Vlei morphology<br />
Morphological details for the two vleis are summarized in the following table:<br />
Summarized morphological and hydrological data for <strong>Zeekoevlei</strong> and<br />
<strong>Rondevlei</strong><br />
Hydrologic /<br />
morphometric variable<br />
<strong>Zeekoevlei</strong><br />
<strong>Rondevlei</strong><br />
Catchment drainage area 8.01 x 10 7 m 2 1.23 x 10 7 m 2<br />
Annual runoff volume (estimated) 2.01 x 10 7 m 3 4.26 x 10 6 m 3<br />
Lake surface area 2.56x 10 6 m 2 4.49 x 10 5 m 2<br />
Lake volume 5.0 x 10 6 m 3 6.8 x 10 5 m 3<br />
Lake mean depth 1.91 m 1.43 m<br />
Precipitation – evaporation -0.85 m -0.85 m<br />
Hydraulic loading 1.79 x 10 7 m 3 y -1 3.87 x 10 6 m 3 y -1<br />
Areal water load 7.0 m y -1 8.62 m y -1<br />
Lake flushing rate 0.28 y 0.18 y<br />
Sediment volume 1.1 x 10 6 m3 Not determined<br />
Area covered by sediment 60 ha Not determined<br />
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3.3 Ecology<br />
The hydraulic regimes of both vleis are attenuated by weirs that were constructed during the<br />
1940s. Both vleis are hypertrophic (see below), but with the degree of anthropogenic nutrient<br />
enrichment in <strong>Zeekoevlei</strong> equivalent to 3-fold that for <strong>Rondevlei</strong> (see below). Both vleis<br />
exhibit the microphyte (phytoplankton) dominance typical of shallow, regulated lakes, but<br />
with this dominance considerably more sustained and ingrained in <strong>Zeekoevlei</strong>. Prior to the<br />
recent implementation of water level drawdowns, <strong>Zeekoevlei</strong> was characterized by nearpermanent<br />
algal blooms, an impoverished population of small-bodied cladoceran<br />
zooplankton, and a large population of coarse fish. The drawdowns served to release the topdown<br />
pressure on the zooplankton community, resulting in a considerable reduction in the<br />
algal population. Algal dominance in <strong>Rondevlei</strong> followed a more distinct periodicity prior to<br />
drawdowns being applied. Given a preceding greater level of ecological balance and stability<br />
in this smaller vlei, the benefits that may have accrued from the drawdown procedure have<br />
not been visibly apparent, and have not been subject to scientific investigation.<br />
Macro-hydrophyte dominance in both vleis is limited to dense stands of emergent reeds. In<br />
<strong>Zeekoevlei</strong> Typha capensis predominates, with a lesser contribution by Scirpus nodosus in the<br />
deeper water. <strong>Rondevlei</strong> reflects an apposite situation with S. nododus as the dominant genus,<br />
but with Typha encroachment. <strong>Rondevlei</strong> supports some 18 species of endangered or<br />
vulnerable flora, and with one endemic species.<br />
Avifaunal composition is much more diverse in <strong>Rondevlei</strong> than in <strong>Zeekoevlei</strong>, but the recent<br />
drawdown-facilitated improvement in water clarity has allowed a return of greater numbers of<br />
piscivorous birds to <strong>Zeekoevlei</strong>. The low human disturbance levels of the <strong>Rondevlei</strong> Nature<br />
Reserve environment, together with a greater seasonal availability of shallow wading habitat<br />
(that <strong>Zeekoevlei</strong> lacks), makes the smaller vlei more attractive to bird life. <strong>Rondevlei</strong><br />
provides habitat for 10 species of birds that are of rare or indeterminate importance.<br />
3.4 Wetland importance<br />
Both vleis have been provisionally assessed in terms of their present condition, and their<br />
ecological importance and sensitivity. Ecological importance implies the value of a wetland<br />
environment to maintain ecological diversity and functioning on local and wider scales, while<br />
sensitivity relates to the capacity of the wetland to resist disturbance, and its ability to recover<br />
once an impact has been endured (resilience). The level of variation between the present<br />
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condition, and the predicted ecological importance and sensitivity provides an indication of<br />
the scope, if any, and need for rehabilitation.<br />
<strong>Zeekoevlei</strong>: The present condition of <strong>Zeekoevlei</strong> is considered to be seriously impaired<br />
(modified), and found to be a Class E condition, which is regarded as being unacceptable.<br />
However, the vlei rates a Class C in terms of its importance and sensitivity. This implies that,<br />
at the very least, efforts should be made to raise the present condition to a Class C – i.e.,<br />
moderately modified.<br />
<strong>Rondevlei</strong>: The present condition of <strong>Rondevlei</strong> was deemed to be moderately modified<br />
(Class C). This was expected given the protected nature of the vlei, and the considerably<br />
lower overall level of impact. The ecological importance was rated two classes higher, i.e.<br />
Class A, again indicating scope and need for rehabilitation in order to improve the present<br />
state.<br />
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4. Issues, Options and Actions Required<br />
4.1 Major Issues<br />
Three major rehabilitation issues were identified, namely:<br />
• the role played by groundwater, and particularly regarding the nutrient enrichment of<br />
<strong>Zeekoevlei</strong> as a consequence of polluted seepages;<br />
• phosphorus enrichment of the vleis, and the sources of said enrichment, including that<br />
from the aforementioned seepage;<br />
• the ecosystem processes that derive benefit from the drawdown process.<br />
Several other issues, classified here as secondary in that they are components of greater<br />
rehabilitation needs, were also identified and are dealt with later in this Action Plan (see<br />
Section 5).<br />
Together, all of the identified issues encompass and address those ecological aspects<br />
identified by the Public Participation component of the <strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> <strong>Rehabilitation</strong><br />
<strong>Study</strong>.<br />
4.1.2 The Key Role of Groundwater<br />
The geohydrological study conducted as part of this investigation revealed that groundwater<br />
intrusion to both <strong>Zeekoevlei</strong> and <strong>Rondevlei</strong> forms a crucial component of the annual water<br />
balance of these wetlands. This finding provided the last pieces of the puzzle of “ghost”<br />
sources of phosphorus identified using mass balance modelling. The geohydrological<br />
investigation encompassed the creation of a field of some 40 wellpoints around <strong>Zeekoevlei</strong><br />
and <strong>Rondevlei</strong>. This provides an established physical infrastructure for the continued<br />
monitoring of groundwater patterns and quality in the groundwater control zone of these vleis.<br />
The geohydrological investigation clearly illustrated the role of groundwater in the<br />
functioning of the vleis, as well as inter-vlei sub-surface linkages across the Cape Flats. It<br />
was determined that groundwater inflows contribute approximately 15% of the total annual<br />
inflow into the two vleis, and play a critical role during summer when groundwater becomes<br />
the sole source of supply. A key finding was that the inflow from groundwater approximates<br />
between 4 and 5 mm per day, throughout the year. The study highlighted the importance of<br />
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the primary aquifer in the vicinity of <strong>Zeekoevlei</strong> and <strong>Rondevlei</strong>, and recommended that it be<br />
afforded protection as a special aquifer system.<br />
The investigation also showed that <strong>Rondevlei</strong> and <strong>Zeekoevlei</strong> function as a single<br />
hydrological unit. In terms of linkage to the groundwater regime of the greater Cape Flats<br />
area, the vleis play an important role as groundwater flows towards them discharge through<br />
them as evaporation.<br />
A most significant finding was that seepage (= leakage) from the wastewater treatment plant<br />
to the south of <strong>Zeekoevlei</strong> accounted for 34% of the total annual load of phosphorus in the<br />
vlei. Decades of impact of sewage management in the immediate area had resulted in the<br />
collapse of the phosphorus retention barriers typical of coastal plain soils. A further finding<br />
that dispelled earlier speculation was that the groundwater to the east of <strong>Zeekoevlei</strong> was not<br />
contaminated by agricultural practices.<br />
In the case of <strong>Rondevlei</strong>, groundwater was estimated to contribute less than 2% of the total<br />
annual phosphorus load, a background and insignificant portion of the total.<br />
4.1.3 Other key findings relating to groundwater<br />
• Monitoring of water levels around both <strong>Zeekoevlei</strong> and <strong>Rondevlei</strong> showed that the<br />
drawdown procedure exerted a limited impact on the geohydrological regime. The<br />
impact of the drawdown procedure was highly localized, with a 0.2 m drop in water<br />
levels, concurrent with the drawdown, measured 500 m from the edge of the vlei.<br />
• The shallow water table in the area was found to have resulted in some minimal<br />
interference with the operation of septic tanks systems, but no abnormal contamination of<br />
the groundwater from this source was detected.<br />
Recommendation 1:<br />
1.1 Strengthen the conceptual understanding of the role of groundwater in<br />
the ecological functioning of <strong>Zeekoevlei</strong> and <strong>Rondevlei</strong> through the<br />
continued monitoring of the established wellpoint field, and associated<br />
surface water characteristics (see Monitoring Protocol).<br />
1.2 Make application for protection of the primary aquifer system in terms<br />
of the Water Act of 1998.<br />
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4.2 Eutrophication and Phosphorus Loading<br />
Nutrient concentrations in waterbodies can range from very low to very high. Such<br />
concentrations are normally characterized in terms of the trophic state or condition of the<br />
system, and ranked as oligotrophic (= poorly nutrient enriched) through meso- (= moderately<br />
enriched) to eutrophic or even hypertrophic (highly to grossly-high in-lake levels of<br />
phosphorus availability). For both <strong>Zeekoevlei</strong> and <strong>Rondevlei</strong>, restriction of the natural cycles<br />
of filling, flushing and drying (through the construction of weirs), and their use as detention<br />
ponds for effluent and urban runoff, has resulted in their being classified as highly eutrophic,<br />
with impaired ecosystem functioning and biodiversity. While some relief of water level<br />
regulation has been possible through the implementation of drawdowns, the greater problem<br />
of excessive nutrient enrichment continues unabated.<br />
Total phosphorus<br />
(mg/l)<br />
1<br />
0.8<br />
0.6<br />
0.4<br />
0.2<br />
0<br />
400<br />
350<br />
300<br />
250<br />
200<br />
150<br />
100<br />
50<br />
0<br />
90/91<br />
91/92<br />
92/93<br />
93/94<br />
Chlorophyll-a (ug/l)<br />
94/95<br />
95/96<br />
96/97<br />
97/98<br />
98/99<br />
Growing season (GS)<br />
Total phosphorus<br />
Chlorophyll-a<br />
Graph showing the change in growing season phosphorus concentration and chlorophyll-a in<br />
<strong>Zeekoevlei</strong> during the 1990s. Note, despite the continuing year-to-year increase in the<br />
ambient concentration of phosphorus, the marked decrease in chlorophyll-a as a consequence<br />
of the applied drawdowns.<br />
Appropriate management philosophy for eutrophication encompasses two broad options,<br />
either: (a) minimizing the causes or (b) learning to live with the symptoms. The process, once<br />
ingrained in an aquatic ecosystem, often adopts a high level of resilience to rehabilitation, and<br />
the “live with it” option is a common choice, unwillingly made by many, in the face of the<br />
extremely high costs associated with reversing the process.<br />
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The findings of this report clearly indicate that, despite the high levels of eutrophication<br />
present in both vleis (see Table below), meaningful rehabilitation is possible, although at a<br />
relatively high initial cost. The cost implications should, however, be weighed against the<br />
period of time that the vleis have been abused. Also, the eco-recreational value of having the<br />
wetlands in a significantly better condition than at present, is likely to render the cost of<br />
rehabilitation relatively small when viewed long-term.<br />
Comparison Of <strong>Zeekoevlei</strong> And <strong>Rondevlei</strong> With The Trophic State Classification System For<br />
African Lakes And Lacustrine Wetlands<br />
Indicator<br />
Upper limit of<br />
<strong>Zeekoevlei</strong><br />
<strong>Rondevlei</strong><br />
mesotrophy<br />
(median)<br />
(median)<br />
Phosphorus<br />
concentration<br />
0.05-0.06 0.70 0.24<br />
mg l -1<br />
Chlorophyll-a<br />
concentration<br />
10-15 200 125<br />
mg m -3<br />
Nitrogen concentration<br />
mg l -1 0.2-1.0 2.0 2.8<br />
Primary production<br />
level<br />
g C m -2 d -1 2-3 1.2 – 4.4 Not determined<br />
Dominant algal family Cyanophyta Cyanophytes<br />
Cyanophytes<br />
Chlorophytes<br />
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4.2.1 Sources of phosphorus loading in <strong>Zeekoevlei</strong><br />
On average an estimated 34 000 kg of phosphorus enters <strong>Zeekoevlei</strong> per year. This exceeds<br />
the guideline annual loading for a vlei of this area and depth by two orders of magnitude<br />
(100x). The largest single contribution, 35%, originates from seepage from the adjacent<br />
WWTP; the second-largest contribution, from the catchment of the Big Lotus River (28%);<br />
and the third-largest contribution as internal loading generated from the considerable volume<br />
of organically-rich sediments (25%).<br />
The various phosphorus loadings for <strong>Zeekoevlei</strong> are summarized in the following diagram:<br />
Groundwater<br />
3.8%<br />
Lake surface<br />
0.1%<br />
Septic tanks<br />
1.5%<br />
Big Lotus catchment<br />
28.4%<br />
Seepage<br />
34.6%<br />
Little Lotus catchment<br />
4.7%<br />
Reed beds<br />
1.1%<br />
Internal loading<br />
25.1%<br />
Local catchment<br />
0.6%<br />
Diagrammatic representation of the identified annual phosphorus loads, by source and<br />
percentage of the total, for <strong>Zeekoevlei</strong>.<br />
This study concluded that reducing the total phosphorus loading to an in-lake growing season<br />
median concentration of between 0.1 and 0.2 mg l -1 , in conjunction with continued<br />
drawdowns and other management options (see elsewhere in this summary) would:<br />
• reduce algal growth and sedimentation;<br />
• restore clear water lake conditions;<br />
• allow sufficient light penetration to support the re-establishment of desired rooted<br />
aquatic plants;<br />
• lead to increased levels of biodiversity;<br />
• reduce the rate of reed encroachment.<br />
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Attaining the desired in-lake phosphorus level would require a load reduction in excess of<br />
70% of the total (see diagram below). However, attenuation of the two well-defined sources<br />
of phosphorus, namely seepage from the WWTP, and the sediments accumulated in the vlei<br />
(combined 60% reduction), together with continued drawdowns (see Section 4.4), is<br />
anticipated to result in the above-mentioned improvements in lake water quality and<br />
attributes.<br />
TP or chlorophyll-a (ug/l)<br />
800<br />
700<br />
600<br />
500<br />
400<br />
300<br />
200<br />
100<br />
0<br />
691<br />
634<br />
576<br />
516<br />
455<br />
392<br />
326<br />
258<br />
225 208 189 170 185<br />
151<br />
131 109<br />
87 105<br />
63<br />
37<br />
0 10 20 30 40 50 60 70 80 90<br />
% reduction in P load<br />
In-lake total P<br />
In-lake chlorophyll-a<br />
Graph showing the predicted change (reduction) in the concentration of phosphorus during<br />
the algal growth season in response to reduction of the gross annual load of this nutrient to<br />
<strong>Zeekoevlei</strong>.<br />
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4.2.2 Phosphorus reduction scenarios for <strong>Zeekoevlei</strong><br />
Note: The brief for this study did not encompass close examination of, or derivation of Best<br />
Management Practices for, the <strong>Zeekoevlei</strong> catchment. This aspect is receiving attention<br />
through a study funded by the Water Research Commission. Diversion of riverine flows<br />
around <strong>Zeekoevlei</strong> is not recommended until all other possible watershed-level management<br />
control options have been implemented.<br />
4.2.2.1 Sediment removal<br />
The removal of the accumulated sediments in <strong>Zeekoevlei</strong> will:<br />
• reduce the annual phosphorus load by 25% of the present total value;<br />
• restore presently inaccessible deep water habitat (21% of the volume of the vlei, and some<br />
40% of the surface area).<br />
These benefits would be best achieved through removal by dredging. Sediment analyses have<br />
shown that the composition of the sediments does not preclude their reuse as admixture for<br />
fertilizers or soil stabilizers.<br />
As part of this project, a specialist dredging engineer from Australia visited <strong>Zeekoevlei</strong>, and<br />
advised on appropriate procedures and costs. It was apparent from this investigation that the<br />
commissioning of this level of expertise could result in cost savings of as much as 3x over<br />
alternative commercial offers to dredge the system. Scenario case studies support the value<br />
and potential success of dredging as a rehabilitatory option for <strong>Zeekoevlei</strong>.<br />
4.2.2.2 Seepage curtailment<br />
Curtailment of the seepage flows will:<br />
• Reduce the annual phosphorus load by 35% of the present total value.<br />
A suite of options for attenuating the seepage flows, ranging from the unlikely and<br />
impractical cessation of WWTP operations and closure of the works, to the creation of<br />
physical and/or hydraulic barriers between the WWTP and the vlei were identified.<br />
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This report considers the removal of sediments from <strong>Zeekoevlei</strong>, and curtailment of the<br />
seepages to be achievable short term objectives. It is predicted that the successful mitigation<br />
of nutrient loading from these two sources will result in a reduction in algal growth of<br />
between 2.5 and 5x the present level (as measured using chlorophyll-a). Any further<br />
reductions in nutrient attenuation achieved in the catchment (a medium to long term process),<br />
will further enhance the level of water quality improvement.<br />
Recommendation 2:<br />
2.1 Remove the estimated 1.1 million m 3 of sediment from <strong>Zeekoevlei</strong> by<br />
dredging. This process will amount to an annual load reduction of<br />
25% of the present total. The estimated cost of the dredging<br />
procedure is 1 million US dollars, plus a further 0.5 million USD for<br />
the processing of the dredge spoils (the cost of the latter operation<br />
may be offset against resale of the product). Between nine and fifteen<br />
months will be required to complete the operation.<br />
2.2 Concurrent with the dredging operation, implement those measures<br />
deemed most appropriate for the attenuation of the phosphorus-rich<br />
seepage flows from the Strandfontein WWTP to <strong>Zeekoevlei</strong>. This<br />
will reduce the annual phosphorus loading of the vlei by up to 35%.<br />
The cost of this mitigation is estimated at between ZAR 2.5 and 5<br />
million (2000 prices).<br />
2.3 That watershed-directed Best Management Practices be identified and<br />
implemented as part of the envisaged Catchment Management Plans<br />
for the Big and Little Lotus River catchments.<br />
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4.3 Sources of phosphorus loading in <strong>Rondevlei</strong><br />
Phosphorus loading to <strong>Rondevlei</strong> stems from diffuse catchment sources, and from sediment<br />
loading of the upstream Princess Vlei (see diagram). In contrast to <strong>Zeekoevlei</strong>, internal<br />
sediment loading in <strong>Rondevlei</strong> was not deemed to be a significant (13%) source of nutrients.<br />
Reed beds<br />
5.4%<br />
Internal loading<br />
13.2%<br />
Local catchment<br />
1.1%<br />
Groundwater<br />
0.7%<br />
Lake surface<br />
0.3%<br />
<strong>Rondevlei</strong><br />
catchment<br />
23.0%<br />
Princess Vlei<br />
catchment<br />
56.3%<br />
Diagrammatic representation of the identified annual phosphorus loads, by source and<br />
percentage of the total, for <strong>Rondevlei</strong>.<br />
A total annual load of some 2300 kg of phosphorus per annum was estimated for <strong>Rondevlei</strong>.<br />
The bulk (56%) of this loading stems from the upstream Princess Vlei (a vlei for which a<br />
separate rehabilitation study is currently underway), with the urban catchment draining<br />
directly to <strong>Rondevlei</strong> contributing a further 23% of the estimated total. Given the surface area<br />
to volume proportions of <strong>Rondevlei</strong>, this amounts to a loading of approximately 40x the<br />
guideline value for a shallow lake.<br />
Notwithstanding the level of phosphorus loading, the ecological functioning of <strong>Rondevlei</strong> is<br />
impaired to a much lesser degree compared with <strong>Zeekoevlei</strong>. This is probably because the<br />
vlei has been impacted at a lower level and for a shorter period of time; has a lower<br />
dominance by bloom-forming algae; a greater degree of natural depth and water level<br />
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variability and possesses a greater flushing rate (0.18 vs 0.28 year). Accordingly, relatively<br />
less (compared with <strong>Zeekoevlei</strong>) rehabilitation effort is anticipated for <strong>Rondevlei</strong>.<br />
TP or chlorophyll-a<br />
(ug/l))<br />
250<br />
200<br />
150<br />
100<br />
50<br />
0<br />
220<br />
200<br />
182<br />
163<br />
144<br />
124<br />
103<br />
82<br />
130 120 59<br />
109 98 34<br />
87<br />
76<br />
63<br />
51<br />
37<br />
22<br />
0 10 20 30 40 50 60 70 80 90<br />
% reduction in P-load<br />
In-lake total P<br />
In-lake chlorophyll-a<br />
Graph showing the predicted change (reduction) in the concentration of phosphorus during<br />
the algal growth season in response to reduction of the gross annual load of this nutrient to<br />
<strong>Rondevlei</strong>.<br />
4.3.1 Nutrient enrichment attenuation options for <strong>Rondevlei</strong>.<br />
The following options were identified, by this and previous studies, for reducing nutrient<br />
pollution of <strong>Rondevlei</strong>:<br />
• rehabilitation of Princess Vlei, including implementation of watershed-directed measures<br />
within the Princess Vlei catchment;<br />
• watershed-directed Best Management Practices;<br />
• treatment wetlands – this option has already been implemented for low flows discharging<br />
to <strong>Rondevlei</strong>;<br />
• drawdowns (discussed later in this section);<br />
• diversion of flows around <strong>Rondevlei</strong>.<br />
Outflow from Princess Vlei discharges directly to <strong>Rondevlei</strong>, thus it is logical for effort to be<br />
concentrated on improving the water quality of the former as close to source as is possible,<br />
and thereafter implementing such measures as may be feasible and possible to deal with the<br />
balance. The situation in Princess Vlei is somewhat similar to that in <strong>Zeekoevlei</strong> in that the<br />
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vlei contains a large accumulation of nutrient rich sediments spread over much of the floor of<br />
the vlei. Unless this nutrient source is effectively managed, Princess Vlei will continue to<br />
generate nutrients that flow to <strong>Rondevlei</strong>. Given the linkage of the Princess Vlei catchment to<br />
<strong>Rondevlei</strong>, it would be beneficial to link the catchment management resources for these two<br />
vleis.<br />
In addition, an assessment needs to be made as to whether catchment-based Best Management<br />
Practices within the <strong>Rondevlei</strong> catchment area are likely to be effective, or indeed<br />
implementable, given space and existing infrastructure limitations. Nutrient loads generated<br />
by this catchment may be at “background” levels, i.e. levels that are high enough to generate<br />
problematical loads for small waterbodies, but so low as to preclude effective mitigation using<br />
conventional BMPs.<br />
Recommendation 3:<br />
3.1 Integrate the management needs of <strong>Rondevlei</strong> with those for Princess<br />
Vlei, and manage these vleis as interlinked components of the same<br />
system;<br />
3.2 Implement whatever identified catchment level BMPs are deemed likely<br />
to reduce pollution with the <strong>Rondevlei</strong> catchment;<br />
3.3 Should the rehabilitation of Princess Vlei not achieve the desired<br />
improvement in the quality of water draining to <strong>Rondevlei</strong>, investigate<br />
options for the introduction of a low-flow bypass system to the Zeekoe<br />
Canal, and the creation of a non-hydraulically-occlusive treatment<br />
wetland in the latter.<br />
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4.4 Water level regulation and drawdowns<br />
4.4.1 Response of <strong>Zeekoevlei</strong> to the drawdown procedure<br />
The use of drawdowns as a management technique was instituted at <strong>Zeekoevlei</strong> during 1997,<br />
and at <strong>Rondevlei</strong> the following year. The original purpose of lowering the water levels was to<br />
enable physical access to the shoreline areas of the vlei for the purposes of litter and reed<br />
removal. The 1997 event was subjected to detailed scientific evaluation of changes to the<br />
biota of the vlei, and in particular the phyto- and zooplankton populations. The findings were<br />
profound. The receding water levels isolating the reed beds, and the absence of deep water<br />
refugia, resulted in a high level of fish predation by piscivorous birds. This reduction in<br />
pressure on the zooplankton enhanced phytoplankton grazing pressure, and with a sustained<br />
clear-water phase being the result. This characteristic was reconfirmed during the second<br />
(1998) drawdown. The improved water clarity also resulted in the reappearance of pondweed<br />
(Potamogeton pectinatus) in the shallow northern and north-western bays of the vlei.<br />
Subsequent drawdowns (post-1998) have not been subject to detailed investigation, and no<br />
comparative studies have been conducted for <strong>Rondevlei</strong>. Notwithstanding this, aggregate<br />
measurement of the level of algal pigments (chlorophyll-a) in <strong>Zeekoevlei</strong> has revealed that,<br />
despite no change in the ambient level of nutrient availability, phytoplankton populations<br />
have remained at approximately 50% of the level measured prior to implementation of the<br />
drawdown procedure.<br />
4.4.2 Why the drawdowns benefit <strong>Zeekoevlei</strong><br />
The drawdowns have resulted in improved ecological functioning for the following reasons:<br />
1. At a gross level, the procedure served to relieve top-down pressure on the vlei food<br />
chain by reducing grazing by fish on the organisms that feed on algae. This cause<br />
and effect response is both predictable, and relatively easy to measure.<br />
2. At a more subtle but no less important level, the procedure has released pressure on a<br />
mechanism common to shallow lakes, viz. that water level regulation forces the<br />
system towards dominance by phytoplankton rather than by more desirable rooted<br />
plant species such as pondweeds – i.e. plant communities that support a wide range of<br />
valued ecosystem services. Shallow lakes are known to exist in one of two<br />
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predominant conditions, namely a clear water condition dominated by rooted plants,<br />
or a turbid state in which algae are the major form of aquatic plant life. The<br />
implication here is that the response will be directly proportional to the release on<br />
water level regulation. This benefit will, however, be limited by other prevailing<br />
factors such as the presence of sediment in the vlei (see below).<br />
4.4.3 Negative impacts of the drawdowns - midges<br />
A negative consequence of the drawdown procedure is a disturbance of the fish – aquatic<br />
insect (midge) dynamic. The absence of deep water refugia during the drawdowns resulted in<br />
a high level of fish predation by birds, as the fish had no means of escaping this impact.<br />
Annual re-implementation of the drawdowns under the same conditions has allowed the<br />
impact to be sustained.<br />
The predominant fish species in <strong>Zeekoevlei</strong> is the common carp (Cyprinus carpio), a species<br />
known to be an excellent biological control for the development of chironomid midge larvae<br />
in shallow lakes. Immediately following the 1997 winter drawdown of <strong>Zeekoevlei</strong>, as well as<br />
during the subsequent years, midge emergence reached plague proportions. This is now<br />
considered to be a direct consequence of the reduction in the fish population, and the<br />
consequent reduction in control on the midge population. However, as midge emergence on<br />
the Cape Flats varies widely on inter-annual basis, and no emergence trapping trials have<br />
been conducted after the drawdowns, other natural forcing functions may also be in effect.<br />
4.4.4 The need for deep water areas and sediment removal<br />
Apart from generating an enormous internal nutrient load (see above), the sediments<br />
accumulated in <strong>Zeekoevlei</strong> occupy in toto the deep water areas (> 1.9 m) of the vlei. During<br />
the drawdowns, average water levels are reduced to 0.5 and < 1m, a time when, should the<br />
sediment basins that cover an area of some 60 ha (= 40% of the vlei area), be open water, they<br />
would provide an additional water depth of up to 3 m.<br />
The sediments currently present in the vlei have accumulated over a period of approximately<br />
70 years, i.e., from the time of establishment of the first wastewater treatment facility on the<br />
south-eastern shoreline. <strong>Rehabilitation</strong> of the vlei, as is envisaged and recommended in this<br />
report, would reduce algal sedimentation rates to very low levels. Thus the benefits for the<br />
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future aquatic health of the vlei would not only be immediately profound, but likely to be<br />
sustainable for a very long period of time.<br />
4.4.5 Options for modifying the timing and rate of the drawdown<br />
procedure<br />
The present timing of the drawdowns at <strong>Zeekoevlei</strong> corresponds with the time of year when<br />
the water levels would naturally have receded. However, the current drawdown procedure<br />
suddenly exaggerates this cycle, but at a point towards the natural end of the low water<br />
period. This is not an ideal ecological scenario.<br />
<strong>Zeekoevlei</strong>, and to a lesser degree <strong>Rondevlei</strong>, provide very little in the way of shallow,<br />
exposed shorelines for migrant waders. By the time that the drawdowns are implemented,<br />
usually late-April, it is too late for wading birds to benefit. Furthermore, the shorelines of<br />
<strong>Zeekoevlei</strong> are rather abrupt, either bordered by reed beds extending into relatively deep<br />
water, or by houses and lawns extending to the water’s edge. These features also reduce the<br />
availability of suitable habitat for wading birds. A benefit of increasing wading bird<br />
populations would be additional predation on midge larvae and other aquatic invertebrates, a<br />
dynamic that is currently precluded by the present policy of water level management.<br />
The earlier implementation of a gradual drawdown process, i.e. by progressively reducing<br />
water levels by increments of approx 100 mm between November and April, such that the vlei<br />
is fully drawn down (1 m ) by the end of the process, would be a more representative<br />
simulation of natural events, and provide a greater range of habitat for birds. This process<br />
would further benefit from compositional restructuring of the certain of the reed bed areas to<br />
provide exposed or sparsely-reeded areas away from high recreational usage zones. In the<br />
case of <strong>Rondevlei</strong>, drawdowns should be timed so as to not connect islands to the mainland<br />
too early in the breeding cycles of birds.<br />
4.4.6 Impact of the drawdowns on bird populations<br />
The drawdowns have invoked certain predictable responses in terms of the effect on bird<br />
populations. These have largely centred on increases in counts due to habitat provision<br />
(flamingoes) and food availability (pelicans). Other changes or influences have not been<br />
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discernible as a consequence of the absence of count data (<strong>Zeekoevlei</strong>), or the short study<br />
period (<strong>Rondevlei</strong>). It is, however, deemed likely that, should the proposed phased<br />
drawdowns be implemented, positive benefits will accrue to both vleis insofar as their bird<br />
populations are concerned.<br />
Recommendation 4:<br />
4.1 Create or re-create deep water habitat areas in <strong>Zeekoevlei</strong> (existing<br />
basins) and <strong>Rondevlei</strong> (as desired) – see also Recommendation 2.1.<br />
4.2 Continue to implement the annual drawdowns in a gradual and phased<br />
manner over a period of six months, and at an incremental rate of 100<br />
mm per interval of 10% of the total drawdown period.<br />
4.3 In conjunction with 4.2, restructure the vegetation of reeded areas of<br />
shoreline so as to enhance the quality of habitat for migrant wading<br />
birds.<br />
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5. Secondary Issues<br />
The following secondary issues were identified as part of this study. Please note that use of<br />
the term secondary does not imply lesser overall importance of the topics, but rather a lower<br />
tier of linkage to one or more of the above major issues.<br />
5.1 Issues Pertaining to Fish Populations<br />
The following aspects pertaining to the management of fish populations were identified by<br />
this study.<br />
• The merits of trying to facilitate the movement of marine fish into the vleis;<br />
• The merits of installing fish ladders;<br />
• Stocking of the vleis with additional fish species;<br />
• The impact of drawdowns on fish populations and midge control (addressed above).<br />
The specialist fish study drew the following conclusions:<br />
• The fish fauna of both vleis comprised only exotic species introduced for angling, or<br />
possibly for midge control. Of those species identified, common carp and banded tilapia<br />
were dominant.<br />
• In addition to the exotics identified for the vleis, the lower (seaward) 500 m of the Zeekoe<br />
Canal also contained mullet.<br />
• Several major barriers preclude fish movement between the lower Zeekoe Canal and the<br />
vleis, these barriers being:<br />
• the gabion weir and bridge supporting the Muizenberg sewage rising main (no<br />
fish other than possibly eel, would be able to negotiate this obstruction);<br />
• the outlet weirs of each vlei;<br />
• the outlet sluices. No fish would be able to move into the vleis against the force<br />
of flow during the drawdowns, or thereafter;<br />
• the <strong>Rondevlei</strong> fish ladder. The fish ladder that has been constructed at <strong>Rondevlei</strong>,<br />
while suitable for large strong swimmers such as trout and salmon, is wholly<br />
unsuitable for the <strong>Rondevlei</strong> flow regime and the type of fish that would be in a<br />
position to attempt use of it.<br />
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• aquatic plant growth, including water hyacinth, that predominates in the Zeekoe<br />
Canal from time to time, reduces oxygen levels, rendering the canal unsuitable<br />
for the movement of fish.<br />
• It is doubtful whether the benefits, if any, of facilitating the movement of marine fish<br />
species into <strong>Zeekoevlei</strong> and <strong>Rondevlei</strong> would outweigh the considerable cost and effort<br />
that would be required for this purpose.<br />
• If marine fish did attempt to move up the Zeekoe Canal, only southern mullet Liza<br />
richardsonii and flathead mullet Mugil cephalus are likely to do this. Both species could<br />
be artificially introduced into the vleis quite cheaply. As they would not breed in the<br />
vleis, reintroductions would be required from time to time.<br />
• Both vleis and the canal essentially contain the same assemblage species, and there exists<br />
little motivation exists for undertaking a costly interconnection of the two systems.<br />
The fish study concurred with the concomitant specialist findings regarding the dynamic<br />
relationship between birds, fish and midges, and the need to create deepwater habitat to offset<br />
attrition of the fish population during the drawdown period.<br />
This study has recommended (see above) that <strong>Rondevlei</strong> and Princess Vlei be managed as<br />
linked components of the same system. In this regard, the fish population of Princess Vlei is<br />
important as it is known to contain a population of introduced barbel Clarias gariepinus. This<br />
fish, in small enclosed environments, can be utterly devasting for not only other species of<br />
fish, but for populations of aquatic organisms, including birds, in general. Accordingly, the<br />
population characteristics of barbel in relation to other fish and aquatic organisms, requires<br />
close monitoring.<br />
It is unlikely that a natural fishway, other than an intermittent connection via flooded lagoons<br />
and pans, ever existed between the <strong>Zeekoevlei</strong> / <strong>Rondevlei</strong> complex and the sea. The<br />
deliberate creation of such a fishway has no obvious merit, and would necessitate costly<br />
financial outlay for little or no benefit. Augmentation of the fish communities of these vleis<br />
through re-stocking is deemed the most sensible option, provided that this is undertaken after<br />
the vleis have been rehabilitated to an improved ecological condition. Given the<br />
demonstrated effect of the top-down control exerted by fish on the zooplankton, and hence<br />
phytoplankton populations of <strong>Zeekoevlei</strong>, considerable benefit is likely to be derived from the<br />
deliberate management of the fish community of this vlei.<br />
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Actions required<br />
• Annual fish population surveys of <strong>Zeekoevlei</strong> and <strong>Rondevlei</strong>, as well as Princess Vlei and<br />
the upper and lower reaches of the Zeekoe Canal, and integration of the findings with the<br />
results of catch-and-return angling activities.<br />
Recommendation 5:<br />
5.1 Artificial stocking of <strong>Rondevlei</strong> with mullet and/or other desirable<br />
fish species may be undertaken.<br />
5.2 Introductions of a wider spectrum of fish species to <strong>Zeekoevlei</strong><br />
should be undertaken after implementation of the rehabilitation<br />
recommended above.<br />
5.3 Catch-and-return fishing activities should be managed through<br />
compulsory fish tagging.<br />
5.2 Issues Pertaining to Midges<br />
This aspect has been dealt with under the section dealing with drawdowns (Section 4.4.3).<br />
5.3 Issues Pertaining to Faecal Pollution and Bacteriological Water<br />
Quality<br />
Although the bacteriological water quality, as measured using faecal indicator bacteria, of the<br />
rivers draining to <strong>Zeekoevlei</strong> is exceedingly poor, rapid attrition of the high counts occurs in<br />
the vlei itself. This results in the vlei complying, on a seasonal basis, with the guidelines for<br />
contact recreation. No appreciable change in the trend of faecal pollution discernible for the<br />
past 20 years.<br />
Notwithstanding the above, the high counts present in the rivers and the indirect use of<br />
<strong>Zeekoevlei</strong> as a treatment pond for this pollution, is undesirable. Every effort should be made<br />
to contain faecal pollution within the catchment to acceptable background levels.<br />
Actions required<br />
• Catchment level identification and control of all sources of faecal pollution over and<br />
above the reasonable background levels deemed acceptable for the landuse type.<br />
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