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Articles

Origin and chemical and isotopic evolution of dissolved inorganic carbon (DIC) in groundwater of the Okavango Delta, Botswana

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Pages 105-120 | Received 24 Apr 2018, Accepted 03 Nov 2018, Published online: 05 Feb 2019

Figures & data

Figure 1. Map of the Okavango Delta, Botswana, showing selected sample locations (●: shallow groundwater, ■: deep groundwater, ♦: island groundwater and ▲: surface water). Map modified from McCarthy et al. (Citation2012).

Figure 1. Map of the Okavango Delta, Botswana, showing selected sample locations (●: shallow groundwater, ■: deep groundwater, ♦: island groundwater and ▲: surface water). Map modified from McCarthy et al. (Citation2012).

Table 1. Statistical summary of data for selected parameters for shallow groundwater, deep groundwater, island groundwater and surface water from the Okavango Delta, Botswana. Min.: minimum; Max.: maximum; SD: standard deviation. DIC: dissolved inorganic carbon; TDS: total dissolved solids.

Figure 2. Plot of dissolved inorganic carbon (DIC) vs the stable carbon isotope composition of DIC (δ13CDIC) for shallow groundwater, deep groundwater, island groundwater and surface water.

Figure 2. Plot of dissolved inorganic carbon (DIC) vs the stable carbon isotope composition of DIC (δ13CDIC) for shallow groundwater, deep groundwater, island groundwater and surface water.

Figure 3. Conceptual model showing the pathways and processes that affect dissolved inorganic carbon (DIC) in the river water, island groundwater and the unsaturated zone prior to recharge of groundwater in the Okavango Delta, Botswana.

Figure 3. Conceptual model showing the pathways and processes that affect dissolved inorganic carbon (DIC) in the river water, island groundwater and the unsaturated zone prior to recharge of groundwater in the Okavango Delta, Botswana.

Figure 4. Plot of the stable oxygen (δ18O) vs stable hydrogen (δD) isotopic composition for shallow groundwater, deep groundwater, island groundwater and surface water. Also shown is the Local Meteoric Water Line (LMWL) constructed from Maun rain, the Global Meteoric Water Line (GMWL; Craig and Gordon, 1965) and the Okavango Delta evaporation line (ODEL; Atekwana et al. Citation2016).

Figure 4. Plot of the stable oxygen (δ18O) vs stable hydrogen (δD) isotopic composition for shallow groundwater, deep groundwater, island groundwater and surface water. Also shown is the Local Meteoric Water Line (LMWL) constructed from Maun rain, the Global Meteoric Water Line (GMWL; Craig and Gordon, 1965) and the Okavango Delta evaporation line (ODEL; Atekwana et al. Citation2016).

Figure 5. Piper plot showing the proportions of major cations and anions in shallow groundwater, deep groundwater, island groundwater and surface water.

Figure 5. Piper plot showing the proportions of major cations and anions in shallow groundwater, deep groundwater, island groundwater and surface water.

Figure 6. Cross plots of (a) TDS vs stable isotopic composition of oxygen (δ18O), (b) TDS vs total cations (Ca2+ + Mg2+ + Na+ + K+), (c) TDS vs alkalinity and (d) TDS vs DIC for shallow groundwater, deep groundwater, island groundwater and surface water. TDS: total dissolved solids; DIC: dissolved inorganic carbon.

Figure 6. Cross plots of (a) TDS vs stable isotopic composition of oxygen (δ18O), (b) TDS vs total cations (Ca2+ + Mg2+ + Na+ + K+), (c) TDS vs alkalinity and (d) TDS vs DIC for shallow groundwater, deep groundwater, island groundwater and surface water. TDS: total dissolved solids; DIC: dissolved inorganic carbon.

Figure 7. Cross plots of (a) alkalinity vs pH, (b) DIC vs pH, (c) alkalinity vs Ca2+, (d) DIC vs Ca2+, (e) alkalinity vs Mg2+, (f) DIC vs Mg2+, (g) alkalinity vs Na+ and (h) DIC vs Na+, for shallow groundwater, deep groundwater, island groundwater and surface water.

Figure 7. Cross plots of (a) alkalinity vs pH, (b) DIC vs pH, (c) alkalinity vs Ca2+, (d) DIC vs Ca2+, (e) alkalinity vs Mg2+, (f) DIC vs Mg2+, (g) alkalinity vs Na+ and (h) DIC vs Na+, for shallow groundwater, deep groundwater, island groundwater and surface water.
Supplemental material

Supplemental Material

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Supplemental Material

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