Nitrogen removal buffer capacity of the Lubigi wetland in Uganda

https://doi.org/10.1016/j.pce.2020.102883Get rights and content

Highlights

  • Field investigations, data collection and analyses of water, sediments and plants were carried out in the Lubigi wetland.

  • The mechanisms governing nitrogen dynamics in the wetland were modelled using STELLA II software.

  • The dominant pathways of the influx nitrogen were through plants' uptake (40.8%) and sedimentation (42.8%).

  • The studied section of the wetland removed 20.1% of total nitrogen, which is equivalent to 987 tons/year.

  • Wetland plants and sediments played a key role for nitrogen removal in the wetland.

Abstract

Lubigi wetland in Uganda receives sewage from Lubigi sewage treatment plant and polluted storm water from parts of Kampala city, which contain organic pollutants including nitrogen. This research was formulated to investigate and model the mechanisms and processes governing the transformation and removal of nitrogen in the Lubigi wetland. Wetland characteristics, flora and the transformation and removal of nitrogen were investigated in the Lubigi wetland in Uganda. Pertinent field investigations, surveys, data collection and laboratory tests and analyses were carried out. Nitrogen transformation and removal was modelled using STELLA II version 9.0®2006 software. The results revealed that the wetland main study area basin widths varied from 250 m to 450 m and deepest section of the wetland was 2.5 m. The study area basin total surface area and volume are 1,093,740 m2 and 1,073,060 m3, respectively. There are 9 dominant plants species, and the mean plants density, biomass and nitrogen content are 10.19 ± 4.69 plants/m2, 1.25 kgDWm−2 and 67.54 ± 37.9gNm−2, respectively. The mean influent and effluent discharges were 222,378 m3/d and 221,357 m3/d, respectively. The wetland main study area hydraulic residence times, vary between 6 h and 10 days depending on the season of the year. The major nitrogen transformation and removal mechanisms and processes are plants uptake (10.328 gNm−2day−1), sedimentation (2.467 gNm−2day−1) and denitrification (0.027 gNm−2day−1). It was concluded that wetland plants and sedimentation of organic nitrogen play a key role for nitrogen removal as they are responsible for removal of 67.54 ± 37.9 gNm−2 and 157.5 g gNm−2, respectively.

Introduction

Natural wetlands provide a wide variety of bio-physical and socio-economic functions such as promotion of biodiversity, preservation of water quality, storage of floods and control of erosion (Novitzki et al., 1997; Fisher and Acreman, 2004; Muraza et al., 2013). However, they are facing increasingly serious threats from watershed anthropogenic environmental degradation and human and infrastructural encroachments (Co'zar, 2007; Kayima, 2020). With increasing population, urbanization and industrialization, wetlands are increasingly becoming recipients of raw or partially treated wastewater discharges in many countries of the world (UNEP, 2013; Kayima et al., 2018a, Kayima et al., 2018b). For example, wastewater treatment plants of the urban areas of major Ugandan cities discharge their effluents into the nearby natural wetlands (Ministry of Water and Environment, Uganda, 2015), although they have capacities to remove some pollutants from water and wastewater, and thus to some extent filtering and purifying it (Kansiime, 2004; Kayima et al., 2018a, Kayima et al., 2018b; Kayima, 2020). This demand for particular urgency in their efficient management and sustainable utilisation (Ministry of Water and Environment, Uganda, 2015). However, in accordance with Gumm (2011), wetlands in Kampala are inadequately protected because of lack of accountability, conflict of interest and lack of resources, which eventually lead to misuse of the wetlands.

One of the wetlands severely strained from anthropogenic activities is the Lubigi wetland, which is one of the largest Lake Kyoga drainage basin wetlands. The anthropogenic activities affecting this wetland include illegitimate disposal of solid wastes and municipal wastewaters (African Development Fund, 2008) and construction of major projects in the wetland such as high-tension electric power line and a sewage treatment plant (Watebawa, 2012; Kayima, 2020). Lubigi wetland also receives storm water discharge from Nsooba-Lubigi drainage channel with average capacity of about 220,000 m3/day (Kayima and Mayo, 2018). All these human activities in and around the wetland has resulted into the degradation of the wetland. In accordance with Habonimana (2014), GIS mapping showed that 40% of the wetland was degraded, which is well above the national average of 30%, which may reduce its buffering capacity.

The Lubigi wetland buffers Lake Kyoga against pollution from some parts of Kampala city (Kayima, 2020). One of the important functions of the wetland is reduction of nitrogen from raw or partially treated wastewater (Metcalf and Eddy Inc.; 2003; Vymazal, 2007; Kansiime et al., 2007; Mayo et al., 2018). Excessive concentrations of nitrogen can stimulate excessive growth of aquatic flora, which can lead to blockages of receiving fresh water bodies and interfere with navigation (UNEP, 2013). Eutrophication of natural water bodies can lead to dissolved oxygen depletion and toxicity to aquatic fauna, which can cause the death of fish and render water septic and odorous and therefore unfit for human and animal use (Vymazal, 2007). High nitrate levels can lead to methamoglobinaemia in infants and increased cancer risks in human beings (Senzia, 2003).

As nitrogen exists in wastewater in various forms, transformation of nitrogen in the wetland from one form of nitrogen to another may involve volatilization of NH3, nitrification, denitrification, uptake by plants and microorganisms, sedimentation, regeneration from benthic layer, anaerobic ammonia oxidation, mineralisation, sorption and desorption (Vymazal, 2007; Mayo et al., 2018). Some of these transformation routes leads to permanent nitrogen removal. The reduction of nitrogen in wetland ecosystem is influenced by multiple factors including uptake by plant biomass and microorganisms (Lee et al., 1975; Bigambo and Mayo, 2005), sedimentation (Johnston et al., 1984; Kayima, 2020) and denitrification (Lowrance et al., 1984; Jordan et al., 1993; Mayo et al., 2018). Therefore, the performance of the wetland will depend on the wetland characteristics that enhance reduction of the pollutant (Fisher and Acreman, 2004; Vymazal, 2007). The main objective of this research study, is to investigate the wetland ecological factors, and the processes governing the fate of nitrogen in the Lubigi wetland.

Section snippets

The Lubigi wetland area

The Lubigi is one of the largest Lake Kyoga drainage basin wetlands located in the North-western part of Kampala, the capital city of Uganda (Kayima et al., 2018a). The main study area investigated in this research study is as shown in Fig. 1. The study area is a part of Upper Lubigi wetland covering an area of about 1.1 km2 at an altitude of approximately 1158 m above mean sea level, with a total drainage catchment area of about 40 km2. The wetland study area is delineated by Sentema and Hoima

Modelling process

The conceptual model (Fig. 2) was used for prediction of the variations of the state variables in time and/or space. The System Thinking Education Learning Laboratory with Animation (STELLA) II ® 9.0 software tool of 2006 (Jørgensen, 1994), was used to simulate the processes for the transformation and removal of nitrogen in the Lubigi wetland, using the law of conservation of mass. STELLA II ® 9.0 software tool was chosen because it can work well with a moderate number of parameters to be

Physical and hydraulic characteristics of the wetland

In accordance with the data collected from the field, it was observed that the main channel through the wetland has gradually curved towards the Masanafu-Namungoona edge from Ganda-Nansana edge. This is because the wetland has gently tilted at the slope of about 0.15% towards the Masanafu-Namungoona edge. The depth of water in the wetland varies from about 10 cm near the edge of the wetland to about 100 cm and 300 cm in the central channel, during the dry and wet seasons, respectively. The

Conclusions

From the Lubigi wetland final nitrogen model, the major nitrogen transformation and removal mechanisms and processes in the wetland, in descending order of importance are plants uptake (10.33 gNm−2day−1), sedimentation (2.47 gNm−2day−1) and denitrification (0.027 gNm−2day−1). The whole wetland removes approximately 987 tons of total-nitrogen (TN) per year, which is equivalent to about 3290 kg/ha/year. The analyses of the plants nitrogen contents, also indicate that significant amounts of

Declaration of competing interest

No Conflict of Interest.

Acknowledgements

All persons who have made substantial contributions to the work reported in the manuscript (e.g., technical help, writing and editing assistance, general support), but who do not meet the criteria for authorship, are named in the Acknowledgements and have given us their written permission to be named. If we have not included an Acknowledgements, then that indicates that we have not received substantial contributions from non-authors.

References (44)

  • R.W. Dawson et al.

    The temperature dependency of biological denitrification

    Water Res.

    (1972)
  • A.L. Downing

    Population dynamics in biological systems

  • J. Fisher et al.

    Wetland nutrient removal: a review of the evidence

    Hydrology and Earth Sciences

    (2004)
  • J.F. Fritz et al.

    Dynamic process modelling of wastewater stabilisation ponds

    Jour. of Water Poll. Control Fed.

    (1979)
  • E. Gumm

    The use and misuse of wetlands in Kampala. Independent study project (ISP) collection paper 1022, school of international training. Unpublished report

  • H.V. Habonimana

    Integrated Flood Modelling in Lubigi Catchment

    (2014)
  • C.A. Johnston et al.

    Nutrient trapping by sedimentation deposition in a seasonally flooded lakeside wetland

    J. Environ. Qual.

    (1984)
  • T.E. Jordan et al.

    Nutrient interception by a riparian forest receiving inputs from adjacent cropland

    J. Environ. Qual.

    (1993)
  • S.E. Jørgensen

    Fundamentals of Ecological Modelling

    (1994)
  • S.E. Jørgensen et al.

    Hand Book of Ecological Parameters and Eco-Toxicology

    (1991)
  • S.E. Jørgensen et al.

    Fundamentals of Ecological Modelling: Applications in Environmental Management and Research

    (2011)
  • F. Kansiime

    Functioning and dynamics of wetland vegetation of Lake Victoria

    Ecotools. Tools for Wetland Ecosystem Resource Management in Eastern Africa

    (2004)
  • View full text