Source, transport, and fate of nitrate in shallow groundwater in the eastern Niger Delta

The eastern Niger Delta region in Nigeria is a hotspot for reactive nitrogen pollution due to extensive animal husbandry, pit latrine usage, and agricultural practices. Despite the high level of human activity, the sources and processes affecting nitrogen in groundwater remain understudied. Groundwater nitrate (NO<sub>3</sub><sup>-</sup>) concentrations are highly variable, with some areas recording values well above the safe drinking water threshold of 50 mg/L. This is particularly true near municipal sewage systems. Elevated nitrite (NO<sub>2</sub><sup>-</sup>) and ammonium (NH<sub>4</sub><sup>+</sup>) concentrations were also detected in the study area. Sewage analysis revealed NO<sub>3</sub><sup>-</sup> concentrations ranging from 1 to 145 mg/L, NO<sub>2</sub><sup>-</sup> from 0.2 to 2 mg/L, and notably high NH<sub>4</sub><sup>+</sup> concentrations. A comparison of major ions indicated that 71%, 90%, 87%, and 92% of groundwater samples surpassed reference site levels for calcium (Ca<sup>2+</sup>), sodium (Na<sup>+</sup>), potassium (K<sup>+</sup>), and chloride (Cl<sup>-</sup>), respectively, pointing to sewage as a likely source of contamination. The NO<sub>3</sub><sup>-</sup>/Cl<sup>-</sup> ratios at several sites suggested that most groundwater NO<sub>3</sub><sup>-</sup> originates from human waste. Stable isotope analysis of NO<sub>3</sub><sup>-</sup> showed a general enrichment in <sup>15</sup>N and, in some cases, a depletion in <sup>18</sup>O, indicating that the NO<sub>3</sub><sup>-</sup> originates from sewage-derived NH<sub>4</sub><sup>+</sup> nitrification. Although denitrification, a process that reduces NO<sub>3</sub><sup>-</sup>, is present, the high dissolved oxygen (DO) and NO<sub>3</sub><sup>-</sup> levels in the groundwater suggest that denitrification is insufficient to fully mitigate NO<sub>3</sub><sup>-</sup> pollution. Consequently, there is a risk of NO<sub>3</sub><sup>-</sup> leaching from shallow aquifers into the Niger Delta's surface waters and ultimately into the coastal ocean.

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Publication Details

Journal
Environmental Science and Pollution Research
Published
2024-11-20
DOI
https://doi.org/10.1007/s11356-024-35499-6
Citations
6
Primary Topic
Groundwater and Isotope Geochemistry
Type
article
Field-Weighted Citation Impact
2.08

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article

Source, transport, and fate of nitrate in shallow groundwater in the eastern Niger Delta

Thomas Pichler, Kirstin Dähnke, Dogo Lawrence Aleku
6 citations
Environmental Science and Pollution Research
Groundwater and Isotope Geochemistry
2.08
article

Source, transport, and fate of nitrate in shallow groundwater in the eastern Niger Delta

Thomas Pichler, Kirstin Dähnke, Dogo Lawrence Aleku
article en
6 citations

Abstract

The eastern Niger Delta region in Nigeria is a hotspot for reactive nitrogen pollution due to extensive animal husbandry, pit latrine usage, and agricultural practices. Despite the high level of human activity, the sources and processes affecting nitrogen in groundwater remain understudied. Groundwater nitrate (NO<sub>3</sub><sup>-</sup>) concentrations are highly variable, with some areas recording values well above the safe drinking water threshold of 50 mg/L. This is particularly true near municipal sewage systems. Elevated nitrite (NO<sub>2</sub><sup>-</sup>) and ammonium (NH<sub>4</sub><sup>+</sup>) concentrations were also detected in the study area. Sewage analysis revealed NO<sub>3</sub><sup>-</sup> concentrations ranging from 1 to 145 mg/L, NO<sub>2</sub><sup>-</sup> from 0.2 to 2 mg/L, and notably high NH<sub>4</sub><sup>+</sup> concentrations. A comparison of major ions indicated that 71%, 90%, 87%, and 92% of groundwater samples surpassed reference site levels for calcium (Ca<sup>2+</sup>), sodium (Na<sup>+</sup>), potassium (K<sup>+</sup>), and chloride (Cl<sup>-</sup>), respectively, pointing to sewage as a likely source of contamination. The NO<sub>3</sub><sup>-</sup>/Cl<sup>-</sup> ratios at several sites suggested that most groundwater NO<sub>3</sub><sup>-</sup> originates from human waste. Stable isotope analysis of NO<sub>3</sub><sup>-</sup> showed a general enrichment in <sup>15</sup>N and, in some cases, a depletion in <sup>18</sup>O, indicating that the NO<sub>3</sub><sup>-</sup> originates from sewage-derived NH<sub>4</sub><sup>+</sup> nitrification. Although denitrification, a process that reduces NO<sub>3</sub><sup>-</sup>, is present, the high dissolved oxygen (DO) and NO<sub>3</sub><sup>-</sup> levels in the groundwater suggest that denitrification is insufficient to fully mitigate NO<sub>3</sub><sup>-</sup> pollution. Consequently, there is a risk of NO<sub>3</sub><sup>-</sup> leaching from shallow aquifers into the Niger Delta's surface waters and ultimately into the coastal ocean.

Environmental Science and Pollution ResearchVol. 31(56)
University of Bremen (DE), Helmholtz-Zentrum Hereon (DE)
Deutsche Forschungsgemeinschaft, Universität Bremen, Petroleum Technology Development Fund
Clean water and sanitation
Openalex Percentile: Top 13%
Groundwater and Isotope Geochemistry
2.08
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