Heldervue – Clearing their “vue” to ensure sustainable water resource management 

Written by Marige Carstens (GEOSS South Africa (Pty) Ltd) 

“There is a real and urgent need to deal with water losses due to invasive alien trees in our catchments in a consistent and long-term manner.” – Richard Bugan,  Hydrogeologist for The Nature Conservancy in South Africa. 

A case study on the effect of Alien Clearing & Groundwater Recharge

The Fruit Farm Group  

The Fruit Farm Group (TFFG), established at the end of 2014, has farms distributed over four countries and three continents. Its farmers produce a variety of sought-after fruits by implementing sustainable and regenerative agriculture practices. They strive towards healthy soils, saving water, and vibrant ecosystems. In doing so, their plants receive the nutrients they require to produce healthy fruit. The company is especially well known for producing, packaging, distributing, and marketing fruit in Southern  Africa.  


Heldervue is one of five South African farms part of TFFG. The farm is located on top of the Piketberg Mountain in the Western Cape, an area well known for cultivating deciduous fruits including apples and pears.

This region has a typical Mediterranean climate, with warm, dry summers and cold, wet winters.  During summer, they rely on boreholes and storage dams for irrigation. The area forms part of the  Breede-Olifants Water Management Area (WMA), according to the 2023 classification.

Previously, Heldervue was situated on the border between the Berg and Olifants-Doorn WMA’s. In 2010, the Berg and Olifants-Doorn WMA’s were classified by the Department of Water and Sanitation as those having the lowest volume of available groundwater per year (DWS, 2010).  

The Geohydrology of Heldervue 

There are 17 boreholes located on the Heldervue farm, of which  9 have been monitored since  2017. These boreholes are drilled into the quartzitic Peninsula Formation of the Table Mountain Group, which is a fractured super-aquifer (Blake  et al., 2010).

Considering that the farm is situated on top of a mountain, the geology is complex (Figure 1). 

Figure 1 The Geology of Heldervue on the Piketberg Mountain

The locations of the boreholes are plotted with yellow dots in Figure  1 and the locations of the monitoring boreholes are displayed in Figure 2. The boreholes are fairly deep (80+  meters) and low-yielding (2- 5 L/s).  

Figure 2 Monitoring Borehole Locations on the Heldervue Farm

The Hydrology of Heldervue 

There are 9 dams located on the main farm portion of Heldervue, spread across six catchment areas  (Grobler & Barrow, 2021). Only 54.35% of the total surface area of the farm drains into the dams  (Grobler & Barrow, 2021). Additionally, groundwater is used to fill the dams.

A drought hit the Western  Cape of South Africa from 2016-2018. Rainfall was low and the draw down of the borehole water levels were as low as the pump inlet. In Table 1, the effect of the drought is clear in 2017, when the farm only received 61% of the 10-year average yearly rainfall. 

Table 1 Heldervue Rainfall Data (2013–2023) 

Month 2013 2014 2015 2016 2017 2018 2019 2020 2021 2022 2023 Average
Jan 10 42.2 6.7 30.4 13 12 37 6 7 0 5 15
Feb 33.4 3.6 4.8 10 3 14 11 12 9 5 45 14
Mar 14.4 20 2.9 43.1 5 38 14 18 117 37 97 37
Apr 133.6 7.4 4.9 75.5 23 64 18 55 23 14 74 45
May 45.8 12.6 31.9 22.3 6 101 58 69 191 54 107 64
Jun 199 214.8 150.4 153.2 167 159 160 149 170 182 471 198
Jul 98.8 155.2 125.3 139.4 48 86 169 170 124 69 96 116
Aug 211 126.8 50.1 70.3 70 89 55 149 129 128 112 108
Sep 5.8 28.2 31.4 75.7 33 117 22 61 27 30 121 50
Oct 17 8.8 10.2 20.9 43 41 58 9 88 0 10 28
Nov 23.8 59.4 27.8 7.4 33 21 11 58 65 30 0 31
Dec 0.4 0.6 11.9 9.3 0 49 35 5 53 75 2 22
Total 793 679.6 458.3 657.5 444 791 648 761 1003 624 1140 727.2

*Data is displayed in millimeters and collected from a rain gauge at Heldervue (32°48’47.14”S, 18°43’18.83”E). 

The Drought and Invasive Plant Species 

Groundwater’s resilience to drought is well-known and many would respond by drilling more boreholes  (DWS, 2010). However, TFFG had a different approach to the multi-year drought. In South Africa,  invasive plant species pose a serious threat to the ecosystem because they increase evapotranspiration  and above-ground biomass, which reduce surface water runoff and groundwater recharge (Chamier et  al., 2012). About 5% of our priceless water resources are consumed by invasive plant species, which  also lowers the carrying capacity of our natural rangelands (Bonthuys, 2021).

According to CapeFarmMapper 3 (2023), the potential evapotranspiration loss on Piketberg Mountain is 1 100– 1 200 mm/year. Increases in evapotranspiration brought on by invasive plants result in lower dilution and higher concentrations of nutrients, contaminants, and suspended particles in water as well as reductions in streamflow and groundwater recharge rates (Chamier et al., 2012). Where evapotranspiration exceeds rainfall, irrigation is needed to ensure a healthy crop. 

Heldervue’s Adaptation Strategy 

The farm’s alien plant species lowered the amount of water that drained into the storage dams on the property and lessened the potential discharge from the watershed. To assure continuity in irrigation water supplies and to alleviate water stress, TFFG partnered with BlueScience to evaluate the costs of removing and controlling the invasive species, as well as the potential benefits.

BlueScience identified  Black Wattle, Eucalyptus, and Port Jackson as the most common alien species found on the Heldervue farm (Grobler & Barrow, 2021). Densely infested areas covered 14.93 ha and moderately infested areas  covered 11.06 ha (Grobler & Barrow, 2021). Under a moderate rainfall scenario, an 8.11% increase in surface runoff was predicted upon the completion of the alien vegetation clearing (Grobler & Barrow,  2021).  

The Outcomes 

Heldervue started the alien-clearing process in August 2021, and by August 2022 most of the aliens were cleared. They started from the northern farm boundary and worked to the south. In Figure 3, the  area where the alien clearing took place is indicated in yellow. During January 2024, the shallowest  (best recovered) groundwater levels were measured since monitoring commenced in 2017. Significant groundwater recharge was observed at all of the monitoring boreholes and can be attributed to the alien  clearing. Surface runoff increased and resulted in increased groundwater recharge and drainage into  storage dams. The triple La Niña of the past three years (2021-2023) also resulted in reduced  abstraction from the boreholes. The Eikevlei boreholes are located at the southern border of the farm. Eikevlei BH3 (Figure 4) and Eikevlei BH2 (Figure 5) were used as case studies. 

Figure 3 Alien Clearing Area on Heldervue

Case Studies  

In Figure 4, the consequence of the drought can be observed from 2018 to 2021, when pumped water levels were running at the pump inlet. This poses a risk of burning out the pump and dewatering the aquifer and is a result of insufficient recharge and increased abstraction due to below-average rainfall.  Eikevlei BH3 is one of the main production boreholes on the farm and could not be left to rest. The period when alien clearing occurred is marked with a red band on the graph in Figure 4. It is evident that since alien clearing started in August 2021, water levels have begun to rise. The recharge potential on the farm increased and the good rainfall of 2023 resulted in reduced abstraction. Before alien clearing, the static water level was 80 meters below ground level (mbgl). After the good rainfall of 2023, and the completion of the alien clearing in August 2022, static water levels were 20 mbgl. The static  groundwater level recovered by an astonishing 60 meters. The water level has since dropped during the 2023-2024 summer period, as abstraction increased and rainfall reduced but still demonstrates significant improvement.


Figure 4 Eikevlei BH3 Water Level and Monthly Rainfall (2017 – 2024 YTD)


In Figure 5, a decommissioned borehole, Eikevlei BH2, is shown. This borehole can be considered a proper monitoring borehole, as no abstraction has been taking place since the end of 2021 when water levels dropped below the pump inlet. The period when alien clearing occurred (August 2021 – August  2022) is also marked with a red band on the graph in Figure 5. Since abstraction ceased, and the alien vegetation cleared, water levels continued to rise. Static water levels were 70 mbgl before 2022. Manual water level measurements obtained in January 2024 showed that the static water level was ~10 mbgl, indicating a 60 m rise in the groundwater levels. During May 2024, the water level was still at  ~20 mbgl, according to manual measurements.  


Figure 5 Eikevlei BH2 Water Level and Monthly Abstraction (2018 – 2023)


Discussion and Conclusion 

Maclear already identified the significance of saving water in South Africa in 1995 due to rising demands on limited water resources (Maclear, 1995). With a sustainability mindset, Heldervue placed itself in a very good situation. The early implementation of a groundwater monitoring and management plan helped them understand their drought resilience.

Due to its value in the agricultural sector, groundwater is directly related to food security and must be treated as a limited resource in land-use planning (DWS,  2010). All essential precautions must be taken to protect the resource and its recharge processes  (DWS, 2010) and even though very few studies have quantified the impacts of invasive alien plants on stream flow, runoff, or groundwater recharge (Chamier et al., 2012)

Heldervue took a leap of faith and is now “picking the fruit”. The conjunctive use of surface water and groundwater, in addition to removing alien vegetation, will ensure long-term water security on the farm. 


I would like to express my gratitude to Mr Trevor Dukes and The Fruit Farm Group for allowing me the  opportunity to write about their success. A special thanks go out to Mr Jaco Botma for sharing all the required information. Additionally, I would like to thank Mr Dana Grobler, who shared his knowledge. 


Blake D., Mlisa A. and Hartnady C., 2010. Large scale quantification of aquifer storage and volumes  from the Peninsula and Skurweberg Formations in the southwestern Cape. Water SA, 36(2):  177-184. 

Bonthuys J., 2021. Assessing groundwater reclamation benefits of clearing invasive alien trees – insights from the Atlantis aquifer. The Water Wheel: 34-37. 

CapeFarmMapper 3, 2023. Western Cape Government Department of Agriculture. Available online:  https://gis.elsenburg.com/apps/cfm/ [Accessed: 03 June 2024]. 

Chamier J., Schachtschneider K., Maitre D.C.L., Ashton P.J. and Van Wilgen B.W., 2012. Impacts of  invasive alien plants on water quality, with particular emphasis on South Africa. Water SA,  38(2): 345-356. 

DWS, 2010. Groundwater Strategy 2010. Available online:  https://www.dws.gov.za/Groundwater/gs.aspx [Accessed: 03 June 2024].  

Grobler D. and Barrow S., 2021. The Potential Runoff Reduction on the Heldervue Farm Piketberg due  to Alien Invasive Vegetation. BlueScience, Somerset West.  

Maclear L.G.A., 1995. Cape Town Needs Groundwater – A Note on the Potential of the Cape Flats  Aquifer Unit to Supply Groundwater for Domestic Use in the Cape Town Metropolitan Area.  Geohydrology Directorate, Department of Water Affairs and Forestry, Cape Town.  

Download the full Heldervue study PDF:

For more information or if you need assistance with sustainable groundwater resource management – get in touch with Marige Carstens: mcarstens@geoss.co.za

Client Testimonial

Just a quick thanks to all of you from our side for your amazing service and support. Dealing with all the parties involved in getting our borehole’s functionality back has been nothing short of a pleasure. A special word of thanks to you, Cameron, for your kindness and for coordinating everything. In the end, you’ve helped us to take the set-back of the copper theft and turn it into a hugely improved borehole. Very grateful indeed!

— Werner Cloete – Calling Education Principal

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