Age Dating Of Groundwater In Perched Aquifers Okongo Area, Ohangwena Region

Abstract

Knowledge of groundwater age / residence time in Okongo perched aquifer is important in understanding key issues in the evolution of groundwater, recharge rates, recharge mechanisms, resource renewability, flow rate and distribution of recharge areas. The build-up in the atmosphere of trace gases such as sulfur hexafluoride (SF6) and tritium (3H) from over a centenary ago offers a convenient way of dating groundwater up to the age of 60 years. These gases are well mixed in the atmosphere; therefore, their input functions help to provide information about groundwater age, distribution and recharge patterns. In this study, sulfur hexafluoride and tritium were used as an age dating tracer for shallow groundwater.

The focus of the study was to understand how age dating of groundwater in a perched aquifer system can help to determine recharge dynamics, e.g. recharge rates, processes, and vulnerability of these aquifers to pollution. The study consequently contributes to the knowledge on shallow groundwater in respect to the effectiveness of age dating methods to determine age / residence time of groundwater in perched aquifers.

The study’s objective was to determine the residence time, investigate the distribution of recharge and examine the origins of recharge to the perched aquifer using sulfur hexafluoride, tritium and hydrochemistry, stable isotopes (2H and 18O) methods. A total number of 26 groundwater samples were collected during two separate sampling seasons / campaigns namely in October 2016 (for tritium and stable isotopes testing) and April 2017 (sulfur hexafluoride, hydro-chemistry and stable isotope). Samples were then grouped into sub-sets of six samples (18O and 2H) and five sample sets (SF6,3H) by method of analysis and by the six (6) sampling sites namely Omboloka 1 and 2, Ohameva, Okamanya, Oshanashiwa and Epumbalondjaba.

The results on concentration of SF6 in the groundwater samples indicate that recharge to the perched aquifer happened in 2000 for Omboloka 2, with a groundwater age of 17 years; Ohameva in 2010 with an age of 7 years; Okamanya in 2012 with an age of 5 years; and Omboloka 1 and Oshanashiwa in 2016 with an age of 1 year. Epumbalondjaba borehole was not sampled during the sampling campaign due to the site being flooded. Applying a conservative mixing ratio model, the samples were observed to have a higher proportion of young water compared to old water. This proves that the groundwater in the perched aquifer is young with a short residence time. Furthermore, the tritium method used to calculate theoretic/hypothetic activities suggests that groundwaterat Ohameva, Okamanya, Omboloka 1 and Oshanashiwa, is sub-modern. While results for Epumbalondjaba and Omboloka 2 portray a mix of both sub-modern and modern water.

The ionic composition of groundwater in the perched aquifer presents three groups of water types characterised by mixed zone water, Na+-K+-HCO3 and Ca2+-Mg2+-HCO3. The perched aquifer system is dominated by the Ca2+-Mg2+-HCO3 water type which is a result of the dissolution of calcrete and the formation of carbonate-rich rocks derived from recent recharge with short residence times. Stable isotopes show that groundwater in perched aquifer systems is enriched in heavy isotopes and has been subjected to evaporation, which is caused by the prevailing climatic and hydrological conditions in the area. This shows that groundwater recharge to the perched aquifer originate from the local catchment systems. Therefore, it is recommended that thetrace gases (sulfur hexafluoride and tritium) methods should be applied to a wide range of groundwater in the perched aquifers of the Okongo area in order to understand recharge areas better. It is necessary to further investigate the groundwater chemistry and isotopic composition of perched groundwater aquifer in more detail. It is further recommended that a long-term monitoring programme consisting of sampling stations for water levels, water quality and stable isotopes is established.