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Spatial Decay of Groundwater Quality Along a Dumpsite-To-
Receptor Distance Gradient: Water Quality Index Assessment and
Human Health Risk Estimation for Peri-Urban Benin City, Nigeria
Okojie, M. E
1
, Osayande, A. D
2*
1
Department of Geology, Faculty of Physical Sciences, University of Benin, P.M.B 1154, Benin City,
Nigeria.
2
Department of Geology and Mining Technology, University of Port Harcourt, P.M.B 5323 Choba,
Port Harcourt, Nigeria.
*Corresponding Author
DOI:
https://doi.org/10.51583/IJLTEMAS.2026.150300087
Received: 27 March 2026; Accepted: 02 April 2026; Published: 17 April 2026
ABSTRACT
Groundwater contamination by open dumpsites is one of the most widespread but least quantified public health
concerns in Sub-Saharan Africa's peri-urban areas. Although individual-level drinking water standard violation
has been reported at many dumpsites in Nigeria, combined Water Quality Index (WQI) rating of the
groundwater contamination level as a function of distance from the dumpsite via spatial decay analysis of
contamination intensity remains unprecedented in Benin City's Benin Formation aquifer system. This study
utilizes the WQI method and Human Health Risk Assessment (HHRA) protocol as per the USEPA guidelines
to analyze the groundwater quality data from eight borehole wells located at varying distances ranging from
100 meters up to about 800 meters from the Upper Ekehuan (Asoro) open dumpsite in Ovia North-East LGA,
Edo State, Nigeria. WQI scores ranged from 198.4 (100 m borehole, 'Very Poor') to 89.3 (500 m borehole,
'Poor'), with no sampled well achieving a 'Good' WQI classification. Spatial regression analysis reveals a
statistically significant exponential decay in composite contamination intensity with increasing distance (R² =
0.84). HHRA calculations indicate non-carcinogenic Hazard Index (HI) values exceeding 1.0 at all proximate
locations for both adult and child receptors, with child HI values reaching 29.4. Carcinogenic risk from
Chromium(VI) and Cadmium exceeds the USEPA acceptable risk level of 1×10⁻⁴ at all wells within 300
meters. These findings provide the first empirical basis for evidence-based buffer zone design and mandatory
groundwater treatment policy for dumpsite-adjacent communities in Edo State.
Keywords: water quality index, human health risk assessment, hazard quotient, spatial decay, dumpsite
leachate, groundwater contamination, Benin Formation, Nigeria
INTRODUCTION
Access to potable drinking water is arguably one of the most fundamental development challenges facing Sub-
Saharan Africa as a continent, where about 400 million people rely on unprotected groundwater as their
primary source of drinking water (UNICEF/WHO, 2023). Groundwater exploitation in peri-urban areas of
Nigeria is complicated by the failure of the municipal-level drinking water supply infrastructure, thereby
forcing residents of many peri-urban areas adjacent to open dumpsites to exploit the groundwater resource
from aquifer systems that are constantly being recharged by leachate infiltration (Ayantobo et al., 2022; Longe
& Balogun, 2021). Although individual-level violation of drinking water standards by individual parameters of
groundwater is commonly assessed via conventional methods of groundwater quality assessment, these
methods are incapable of capturing the cumulative effect of violation of drinking water standards by multiple
parameters of groundwater (Ijaz et al., 2020). The Water Quality Index (WQI), as first proposed by Horton
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(1965), has undergone many methodological evolutions over the years (Brown et al., 1972; Tyagi et al., 2020).
The quantification of the actual health risk is further achieved through the Hazard Quotient (HQ) for non-
carcinogenic effects and Cancer Risk (CR) for carcinogenic heavy metals, as quantified through the Human
Health Risk Assessment (HHRA) framework of USEPA (1989, updated 2023). A critical analytical gap is also
recognized in the absence of spatial decay modeling for this site’s Benin Formation unconfined sandy aquifer
with high permeability and low attenuation capacity, which is different from clay-rich aquifers studied in most
Western dumpsite literature (Akujieze & Irabor, 2014). This study is intended to address: (1) the composite
WQI classification at varying distances from the dumpsite; (2) non-carcinogenic and carcinogenic health risks
to human health; and (3) the rate of groundwater quality improvement with lateral distance.
THEORETICAL FRAMEWORK
This paper employs the theoretical framework known as the Risk-Based Environmental Assessment (RBEA).
Simply stated, RBEA posits that health-risk assessment of environmental quality should take as its starting
point quantified estimates of health risks faced by individuals, rather than mere comparison to regulatory
standards and guidelines (USEPA, 2023; Lim et al., 2020). RBEA incorporates a number of components,
including consideration of multi-contaminant co-occurrence patterns, population exposure, and chronic/acute
toxicity factors. Within the scope of this paper, the use of WQI represents an important step in linking
technical findings to stakeholders' decision-making processes, whereby multi-parameter data is condensed into
a single index (Tyagi et al., 2020; Kachroud et al., 2022).
Study Area and Hydrogeological Context
The Upper Ekehuan (Asoro) dumpsite, located in Ovia North-East Local Government Area, Edo State, has a
basin topography and lies within the latitude and longitude 6°19'20"6°19'40"N and 5°35'0"5°35'20"E,
respectively. The hydrogeology in the study area is characterized by the Benin Formation, which is an
unconfined sandy aquifer with porosity exceeding 30% and hydraulic conductivity of 1050 m/day (Akujieze
& Oteze, 2007). The absence of a confining clay layer provides no natural attenuation barrier between leachate
and the saturated aquifer. Eight borehole groundwater samples (GW1GW8) were collected at distances from
100 m (GW1) to 500 m (GW4), with additional directional samples. Two leachate samples (L1, L2) were
collected from active seepage zones as source characterization.
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Figure 2 Map of Ovia North East
MATERIALS AND METHODS
Sample Collection
Groundwater samples were collected from boreholes using dedicated submersible pump sampling with three-
volume purging prior to collection. Samples were collected in pre-cleaned HDPE bottles, acidified to pH < 2
with trace-metal grade HNO₃ for heavy metal preservation, and stored at 4°C. Field measurements of pH, EC,
and temperature were conducted in situ using calibrated multiparameter probes.
Laboratory Analysis
pH and EC were measured using digital meters. Turbidity was measured by HACH DR 2010
spectrophotometer. TDS was determined gravimetrically (Ademoroti, 1996). Total hardness, alkalinity, and
sulphate were determined titrimetrically and turbidimetrically. Nitrate and chloride were determined
colorimetrically (APHA, 1993). Phosphate was analyzed using the ascorbic acid reduction method (ASTM,
1990). Heavy metals were quantified by AAS (BUCK SCIENTIFIC Model 210 VGP, USA). COD was
determined by the dichromate reflux method.
Water Quality Index Computation
WQI = Σ (Wi × qi) / Σ Wi, where Wi is the relative weight of the i-th parameter (derived from its inverse
permissible limit) and qi = [(Ci Ci_ideal) / (Si Ci_ideal)] × 100. Parameters included: pH, EC, TDS, Cl⁻,
SO₄²⁻, NO₃, Fe³⁺, Zn²⁺, Cu²⁺, Ni²⁺, Cd²⁺, Cr⁶⁺, Pb²⁺. WQI classification: Excellent (< 25), Good (2550), Poor
(50100), Very Poor (100200), Unsuitable for drinking (> 200) (Tyagi et al., 2020).
Human Health Risk Assessment
HHRA was conducted by following the guidelines provided by USEPA (1989, 2023). CDI = (C × IR × EF ×
ED) / (BW × AT), where IR = 2.0 L/day (adults), 1.0 L/day (children); ED = 30 years (adults), 6 years
(children); BW = 70 kg (adults), 15 kg (children); AT = 10,950 days (non-carcinogenic); 25,550 days
(carcinogenic). HQ = CDI / RfD; HI = Σ HQi. HI > 1.0 indicates potential non-carcinogenic health risk.
Cancer Risk (CR) = CDI × CSF; CR > 1×10⁻⁴ indicates unacceptable cancer risk.
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Spatial Decay Analysis
The exponential decay model is given by the equation C(d) = C₀e^(-kd), where C(d) is the concentration at a
distance 'd', C₀ is the original concentration, 'k' is the decay constant, and 'd' is the distance. The values for the
boreholes at different distances (GW1: 100 m, GW2: 150 m, GW3: 160 m, and GW4: 500 m) and leachate
samples at a distance of 0 m have been used to obtain the values for the decay constant 'k', which includes the
effect of all the processes occurring in the aquifer.
RESULTS
Water Quality Index Analysis
WQI values range from 286.4 (GW6, 'Unsuitable for drinking') to 89.3 (GW4 at 500 m, 'Poor'). Both leachate
samples produce WQI scores exceeding 800 ('Extremely unsuitable'). No borehole sample achieves a 'Good'
classification at any location. The dominant WQI contributors at near-field sites are Ni²⁺ (38% of total score),
Cd²⁺ (24%), Cr⁶⁺ (18%), and Pb²⁺ (12%) collectively over 90% of the total WQI score at proximal wells
underscoring that the potability crisis is fundamentally a heavy metal problem driven by leachate infiltration.
Spatial Decay of Contamination
The distance-WQI regression reveals strong exponential decay (R² = 0.84 for WQI; = 0.790.91 for
individual metals). Decay constants (k, m⁻¹): Nickel = 0.0042; Cadmium = 0.0051; Chromium(VI) = 0.0038;
Lead = 0.0078; Iron = 0.0089. Extrapolated distances for the wells to approach the WHO limits for the
contaminant concentrations: Ni - 1,800 m, Cd - 1,200 m, Cr(VI) - 2,200 m, Pb - 850 m, indicating the effect of
contamination at much larger distances than the radius of 600 m, within which the present study has been
conducted.
Human Health Risk Assessment
Non-Carcinogenic Risk
Adult HI values vary from 3.84 (GW4) to 12.6 (GW6), all higher than the acceptable value of 1.0. Similarly,
child HI values vary from 8.97 (GW4) to 29.4 (GW6). Nickel is the major non-carcinogenic contaminant,
followed by Cadmium and then Chromium(VI). The major non-carcinogenic health risks: Nickel - Renal
Tubular Damage, Cadmium - Irreversible Proximal Tubular Kidney Disease, Chromium(VI) - Hepatotoxicity
and Immune System Inhibition, and Lead - Neurodevelopmental Impairment in Children.
Carcinogenic Risk
All wells exceed USEPA's acceptable carcinogenic risk threshold of 1×10⁻⁴ for at least one metal. At GW6:
CR(Cr⁶⁺) = 4.2×10⁻³ and CR(Cd) = 2.8×10⁻³ (adult), both exceeding the high-risk threshold of 1×10⁻³. At GW1
(100 m): CR(Cr⁶⁺) = 1.8×10⁻³ and CR(Cd) = 1.6×10⁻³. Even at GW4 (500 m), adult CR values for Cr⁶⁺
(5.1×10⁻⁴) and Cd (3.8×10⁻⁴) remain above 1×10⁻⁴. Child carcinogenic risks are consistently 1.52.3 times
higher than adult values at equivalent locations.
DISCUSSION
WQI as a Decision Support Framework
The lack of a 'Good' or 'Excellent' WQI classification at any of the sampled boreholes up to 500 meters in
depth has major implications for water governance in Ovia North-East LGA. WQI's communication clarity is
also in line with WHO's (2022) recommendations on risk communication in water safety planning, which
emphasize composite indicators for non-expert decision-making (Tyagi et al., 2020; Kachroud et al., 2022).
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The Benin Formation as a High-Risk Hydrogeological Setting
The lower decay constants (k = 0.0038-0.0089 m⁻¹) compared with those of European glaciofluvial aquifers (k
= 0.012-0.025 m⁻¹) and North American alluvial aquifers (k = 0.015-0.030 m⁻¹) confirm the minimal natural
attenuation of the Benin Formation. A scientifically defensible buffer zone for unlined open dumpsites in this
setting should be a minimum of 1,500-2,000 meters, in accordance with the precautionary principle of
Nigeria's National Environmental Policy and NESREA Act (2007).
Child Health Risk as a Priority Policy Dimension
The consistency of Child HI values (8.97-29.4) being 2.3 times higher than adult values also indicates weight-
based dose amplification of developmental risk from neurotoxic Pb, nephrotoxic Cd, and immunotoxic Cr and
Ni. Achievement of the SDG 3 targets for reduction of mortality and morbidity from chemical hazards in the
environment cannot be realized without mandatory GQ monitoring, central supply of treated water, and
leachate source remediation.
Iron as an Indicator Contaminant
Iron has the greatest absolute leachate concentration (L1 = 103.85 mg/L) and the fastest spatial decay rate (k =
0.0089 m⁻¹), which can be attributed to pH-dependent precipitation as ferric hydroxide complexes. However,
all GW Fe concentrations fall above the WHO limit of 1.0 mg/L and NSDWQ limit of 0.3 mg/L, ranging from
1.05 to 8.90 mg/L. Most importantly, the fast spatial decay rate of Iron, as compared to Ni and Cd, reveals the
danger associated with using easily measurable indicator parameters as surrogates for more toxic substances,
as the relatively “normal” Iron concentration does not guarantee “safe” Ni and Cd concentrations.
Study Limitations and Future Research Directions
While this study provides a critical assessment of groundwater risk in the Benin Formation, several limitations
must be acknowledged to guide appropriate interpretation of the findings and to direct future research. First,
the data represents a single sampling event; given Nigeria’s distinct wet and dry seasons, temporal variations in
leachate dilution and hydraulic head were not captured. Wet-season high-recharge conditions may dilute
leachate plumes, while dry-season drawdown may concentrate contaminantsdynamics that a single cross-
sectional dataset cannot resolve. Second, the lack of vertical profiling (borehole depth data) means the spatial
decay model focuses strictly on lateral migration, potentially overlooking vertical stratification of contaminants
within the unconfined aquifer. Benin Formation's heterogeneous composition can support some vertical
pathways of pollutant flow that will not be accounted for by a two-dimensional decay model. In addition,
because the human-health risk of Chromium is evaluated based on total concentration, carcinogenic risk
estimates obtained in this study should be considered conservative since a fraction of the total amount of
Chromium can exist as Cr(III) in the sub-neutral environments of the Benin Formation. As such, further
speciation of the contaminant can lower calculated cancer risk. Despite the significant correlation between
distance and contamination, lack of an adequately situated deep reference well makes it impossible to isolate
contaminants coming from the dumpsite from other possible anthropogenic pollution sources such as pit
latrines and agricultural discharge. Informal waste disposal close to the site may contribute to pollution
detection.
Several actions should be undertaken to increase the impact of the paper and its utility for policy development,
as described above. Seasonal monitoring throughout the year could help capture the dynamics of dilution and
migration of pollutants in the system over time. Collecting information about the borehole depths and
groundwater flow direction (hydraulic gradient) could aid in constructing the three-dimensional map of a
plume in the unconfined aquifer. It is critical that speciation of Cr(VI) be performed to better estimate the
calculated risk. Finally, a buffer zone (such as 600 m based on the decay rate constant) should be defined,
which will convert the findings into a readily implementable policy tool for Sub-Saharan Africa.
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Policy Recommendations
The 1,500 meter buffer zone between the dumpsite boundary and the boreholes from which drinking water is
extracted should be made a national standard for all Nigerian unlined waste disposal facilities overlying the
Benin Formation aquifer. Those living within 1,000 meters should be given priority access to a safe, treated,
and piped water supply, or a point-of-use treatment system such as reverse osmosis/ion exchange. A biannual
GWQ monitoring program should be developed, with WQI and HI calculations conducted for sentinel
boreholes 100 m, 250 m, 500 m, and 1,000 m radial distance from the dumpsite. Given child HI values
exceeding 8.0 at proximate locations, a pediatric blood metal screening program is urgently recommended for
children under 12 residing within 500 meters, in partnership with Edo State Primary Healthcare Development
Agency.
CONCLUSION
This study provides the first WQI-based composite water quality assessment and USEPA-protocol human
health risk analysis for dumpsite-affected groundwater in the Benin Formation hydrogeological setting. None
of the boreholes within 500 meters from the pollution source have water suitable for human consumption.
Spatial decay modeling reveals contamination of the groundwater in a much wider band, ranging from 850 to
2,200 meters, depending on the type of metal analyzed. This finding demonstrates that risk zones created using
a spatial decay model can greatly extend the contamination area as opposed to a more attenuating geological
formation. Thus, the frameworks of WQI and Human Health Risk Assessment developed here offer replicable
and internationally recognized methods that Nigeria's regulators can utilize for transitioning from snapshot
monitoring into risk-based water management. Limitations associated with this study include a single-season
monitoring period, lack of borehole vertical profiling, total rather than speciated Chromium, and an absence of
reference well upstream.
Author Contributions
M.E.O., Conceptualization, data collection, laboratory analyses, writingoriginal draft.
A.D.O., methodology validation, writingreview and editing.
ACKNOWLEDGEMENT
The author would like to thank the encouragement of my supervisor Prof E.G Imeokparia.
Funding: This research received no external funding.
Competing Interests
The authors declare no competing interests in relation to this manuscript.
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