Gauteng Smallholder June 2017 | Page 19

From page 15 aquifer. In addition, in developed areas, rainwater ends up in storm water drains and does not reach the aquifers in the area. The number, proximity and depth of other boreholes in your area will also affect your hole, especially if they are drawing on the same aquifer. Pumping too much water out of your borehole without adequate rainwater to recharge the aquifer will result in your borehole delivering less water. The dynamic becomes quite simple: no Graph showing borehole yields over four years rain plus high abstraction (removal) rates equals a diminishing (or vanishing) resource. If you are lucky, after a few weeks of good rains your borehole may return to its former strong output. Experience with numerous commercial installations have show n how quickly water levels in boreholes can recover after a few good downpours. But is this always the case? For, what happens if a borehole is being over pumped? The accompanying graph shows data that was collected from a borehole over a period of 30 months. The top graph shows how much water was taken out of the borehole. An installed totalising water meter will give you this reading. The red trend line shows that the rate of abstraction increased slightly over the 30 months that the hole was monitored. 17 www.sasmallholder.co.za WATER The bottom graph shows that the rainfall was erratic but the trend was constant. The middle graph, however, shows that even though rain had fallen in the area, the water level in the borehole dropped from about 25m below ground to 46m. That's a drop of 21m in the water content in the aquifer. The good rainfall in December of Year 2 did not have a significant influence on the overall situation. The owner of this borehole was clearly taking out more than what Continued on page 18