Suitability of Drinking Water Sources from Nyaruzinga Wetland for Domestic Use in Bushenyi Municipality, Uganda

This study determined the physico-chemical and bacterial quality of raw (borehole, springs, wells) and tap water sources from Nyaruzinga wetland for domestic use in Bushenyi Municipality. Forty samples of raw water were randomly collected from Kacuncu, Kyeitembe and Kikuba tributaries of the wetland and 40 samples of tap water generated from the same wetland were randomly drawn from Ishaka, Nyakabirizi and Central divisions of the Municipality. The samples were analyzed for apparent colour (AC), turbidity, electrical conductivity (EC), total hardness, pH, total iron, residual alum, free residual chlorine and faecal coliforms using standard methods and their values compared with standard local UNBS (2008) and international WHO (2011) drinking water quality guidelines. The results showed that the mean pH of the protected spring below Kikuba Hill (5.21); the AC (Pt/Co) of the borehole below Bweranyangi Junior School (17.28) and the surface well below Nyandozo Primary School (157.58) both situated in Kacuncu as well as the free residual chlorine (mg/L) in tap water at Kanyamabona Trading Centre, Ishaka division (0.192) were below the standard values of WHO (pH, 6.0 8.0; free residual chlorine, 0.2 0.5) and UNBS (AC, <15). The electrical conductivity, EC (μS/cm) and total hardness (mg/L) of all the selected water sources were within the WHO standards (EC, <1500 (raw water), 0 300 (tap water); total hardness, <1500 (raw water), <100 (tap water)). The residual alum (mg/L) in all the tap water sources was also within the WHO guideline (<0.2). On the other hand, the turbidity (27.38 NTUs) and total iron content (0.32 mg/L) of the surface well below Nyandozo Primary School were above WHO guidelines of <15 and <0.3 respectively. Furthermore, the mean faecal coliform counts (CFU/100 ml) in the surface well below Nyandozo Primary School (6.90) and the borehole below Bweranyangi Junior School (16.83) including the surface well below Kyeitembe Trading Centre (9.25) were above the WHO standard How to cite this paper: Muhangane, L., Nkurunungi, J.B., Yatuha, J. and Andama, M. (2017) Suitability of Drinking Water Sources from Nyaruzinga Wetland for Domestic Use in Bushenyi Municipality, Uganda. Journal of Water Resource and Protection, 9, 1587-1611. https://doi.org/10.4236/jwarp.2017.913100 Received: November 24, 2017 Accepted: December 25, 2017 Published: December 28, 2017 Copyright © 2017 by authors and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY 4.0). http://creativecommons.org/licenses/by/4.0/ Open Access


Introduction
Safe drinking water of adequate quantities is universally recognized as a basic human need and one of the most essential factors of human development as well as social and economic existence [1] [2].However, millions of people in developing countries do not have access to adequate and safe water supply due to the increasing population and urbanization [3].For instance, access to safe water remains a challenge in Africa with an overall estimate of 62% while access in rural areas is approximated at 47% [4] [5].The overall access in Uganda is about 66% with 42% in rural areas [6].
Uganda is highly endowed with water resources and wetlands covering 17% (about 40,000 km 2 ) of the total area of Uganda (241,550 km 2 ) with wetlands constituting about 13% or 30,000 km 2 of the country [7] [8].With the rise in human population, and the subsequent demand for more resources to sustain their livelihood, wetlands and their benefits (e.g.water purification) are now under pressure both in rural and urban areas [8].For example, it is estimated that about 75% of the wetland area in Uganda has been significantly affected by human activity, and about 13% is severely degraded [9].Overall 67.8 km 2 or 27.2% of the total wetland area in Bushenyi district has been modified for various activities, mostly dairy farming and cultivation.As a result, there are severe environmental problems of pollution of water resources in Uganda including Bushenyi [10].
However, addressing such current and future water pollution risks requires accurate data from consistent monitoring.
In the case of Bushenyi District, the safe water coverage is estimated at 85%, with 93% in rural areas and 59% in urban areas [11].Bushenyi Municipality gets raw water from Nyaruzinga Swamp, which is first purified in a water treatment plant before supplying to the municipality [12].However, the coverage of piped tap water within the municipality stands at 40% in Central, 20% in Ishaka and 20% in Nyakabirizi divisions with respective population densities of 496/km 2 , 881/km 2 and 245/km 2 .Despite the above coverage, only 12% of the municipality's population is served by piped tap water due to reduced functionality of tap sources for domestic use [11].The percentage distribution of households without access to safe water in the divisions of Bushenyi municipality is as follows: Ishaka (21.3%),Central (19.7%) and Nyakabirizi (25.6%) [13].
Unfortunately, to date, there is scanty literature on water quality characteristics of Nyaruzinga wetland, a source for treated tap water and raw water (surface wells, springs and boreholes) for domestic usage in Bushenyi Municipality.Thus there is need to analyze the quality of both raw water sources and piped tap water from the same wetland.Therefore, this study determined the physico-chemical parameters and faecal coliform content in raw water sources and piped tap water from Nyaruzinga wetland in Bushenyi Municipality.

Location and Description of the Study Area
Nyaruzinga wetland is located in Bushenyi Municipality, Bushenyi District, South-Western Uganda (Figure 1).The district lies between the coordinates; 0˚ N and 0˚46' S of the equator and 29˚41' East and 30˚30' West, with its headquarters located 340 kilometers from the capital city of Uganda, Kampala.Bushenyi district has a landscape comprising of hills, valleys (mostly occupied by wetlands which are drained by streams and rivers) and some stretches of plain land all located within an elevation of 910 -2500 meters above sea level [14].Greater Bushenyi district has a total area of 4287 km 2 of which 369 km 2 is covered by open water.Wetlands cover an area of 250 km 2 (5.8% of the district) of which 132 km 2 (52.8%) is permanent and 118 km 2 (47.2%) is seasonal.The wetlands receive water mainly from rivers, precipitation and groundwater with Bushenyi having peak rains between March to April and September to December.The seasonal wetlands are usually flooded during the peak rainfall periods [8].A total of 67.8 km 2 of the wetland area (27.2%) has been converted into pasture land for dairy cattle (about 36 km 2 or 14%) and for cultivation (32 km 2 or 13%) [8].
Nyaruzinga wetland (Figure 1) is the only source of tap water that supplies the towns of Bushenyi, Nyakabirizi and Ishaka.The wetland is located about 2 km South of Bushenyi town in Bushenyi Municipality and has three major tributaries of Kyeitembe, Kacuncu and Kikuba streams.Nyaruzinga wetland is a tributary of Koga wetland system which drains into Lake Edward/George Drainage System through the Kasharara system.Nyaruzinga is a permanent converted wetland found in Mutara Sub-county occupying an area of 0.99 km 2 .It lies along a narrow valley (altitude, 1524 -1585 m a.s.l.) surrounded by steep hills [8].Flowing through the wetland is River Nyaruzinga which drains into Kateizi.The main plants in the wetland are sedges and papyrus dominated by Cyprus papyrus.Nyaruzinga wetland is used for livestock grazing, domestic water collection and fishing while the surrounding area is used for subsistence agriculture, livestock grazing and harvesting of plants for various uses.Heavy draining of the wetland for livestock grazing and crop growing are the major threats facing the wetland including soil erosion in the catchment.However, no conservation measures have been put in place to curb the wetland degradation [8].

Geology of the Study Area
Geology has an important bearing on drainage, geomorphologic processes and topography.The geology of Bushenyi district consists of the Precambrian rocks like shales, quarttzites, mudstones, schists, phyllites, gneisses and conglomerates which are rich in minerals [14].The mineral ores in the district include beryl at Mutaka, columbite-tantalite in Jemubi and Kabira, copper-cobalt in Buhweju, gold in Kyamuhunga, quartz crystals (constituent of sandstone and granite rocks) in Buhweju, kaolin in Mutaka and Kibalya, pozzolana in Bunyaruguru volcanic fields.There are also potential mineral deposits of thorium in Buhweju, barites in Katoma hill, diamonds in volcanic fields in Bushenyi, feldspar in Mutaka and talc in Kyamuhunga [15].These mineral ores influence some properties of the water bodies in Bushenyi District including Nyaruzinga wetland.

Sampling Sites
Five sites for raw water were purposively selected from the three tributaries of Nyaruzinga wetland (Figure 1) basing on the length of the tributaries.Two sites each were chosen along Kacuncu and Kyeitembe tributaries while one site was selected along Kikuba tributary.Similarly, five tap water sources (Figure 1) were also purposively selected from the three divisions of Bushenyi Municipality basing on the population sizes of the divisions.Two tap water sources were each selected from Ishaka and Central divisions while one was chosen from Nyakabirizi Division.

Water Collection
Sample bottles were washed with dilute hydrochloric acid and rinsed with distilled water under aseptic conditions, to avoid contamination of water with other atmospheric bacteria.Using a sterilized dip sampling jug, water was scooped and transferred into the sample bottles for raw water while for tap water the sample bottle was placed under the tap and the tap was opened to run water into the bottle.Turbidity and pH were determined on site for raw water plus free residual chlorine for tap water and the bottle was then capped and transported in a transport box for microbial analysis at the Nyaruzinga water treatment plant.
Forty samples were collected per study site within 40 days starting from 12 th September 2016 to 22 nd October, 2016.

Laboratory Analysis
The water samples were analysed according to Standard ISO Methods for Ex-amination of Water and Waste Water [16] [17] [18] and the Standards Operations Manual [19].

pH
pH was measured using a pH/EC multimeter.The wet cap of the electrode was removed and the electrode was rinsed with distilled water.The meter was switched on and the electrode dipped in the sample.The pH reading was left to stabilize and then recorded [19].

Electrical Conductivity (EC)
Electrical conductivity was also measured using a pH/EC multimeter.The electrical conductivity electrode was removed from the wet cap and rinsed with distilled water.The MODE button was pressed to change from pH to EC measurement.The electrode was then dipped in the water sample and the meter left to stabilize and EC reading then recorded in µs/cm [19].

Turbidity
Turbidity was measured using a turbidity meter.The turbidity meter was switched on.A volume of 10 ml of the sample was put in the turbidity meter cell and inserted into the turbidity meter and the READ button pressed.The reading was left to stabilize and recorded in Nephlometeric Turbidity Units, (NTUs).

Apparent Colour
Apparent colour was measured using a Hach DR 5000 Spectrophotometer.The spectrophotometer was switched on and left to go through self check.A selection of the stored programs was made and scrolled to the parameter, colour.A volume of 10 mls of distilled water was put into the sample cell and used to blank/zero the machine.The sample cell was then removed and emptied and 10 mls of the water sample put in it.The sample cell was put in the spectrophotometer and the option; READ was pressed.The value shown on the screen was recorded in TCUs.

Total Hardness
To measure Total Hardness, a burette was filled to the Zero mark with EDTA solution.A sample volume of 50 mls was measured into a conical flask.Three drops of hardness buffer was added followed by 0.1 g of hardness indicator.The mixture was shaken and its colour turned pink.It was then titrated against EDTA solution until the colour turned from pink to blue/purple.The volume used was determined by subtracting initial burette reading from final burette reading and recorded.The value of total hardness in mg/l was computed by multiplying the volume used by 20.

Total Iron
Total iron was measured using a Hach DR 5000 spectrophotometer.A sample volume of 50 mls was measured and diluted with distilled water to 100 mls.The solution was divided into two 50 ml portions and put into two separate reaction bottles.One portion was kept as a blank and to the second portion was added an ample of ferrozine reagent, shaken and left for a 5 minute reaction time to lapse.
The machine was zeroed using the blank.The ZERO button was pushed and the display showed 0.00 mg/L Fe.The prepared sample cell was cleaned and the prepared sample inserted into the cell holder.The READ button was then pushed and results showed in mg/L Fe.

Residual Alum
Residual alum was also measured using a Hach DR 5000 Spectrophotometer.A sample volume of 50 mls was measured into a reaction bottle.A pillow of ascorbic acid was added and shaken, followed by Awa 3 pillow reagent and also shaken.The solution was divided into two, 25 ml portions.To one portion, a pillow of bleaching reagent was added for use as a blank to zero the machine.It was left for a reaction time of 15 minutes to elapse.After 15 minutes, the machine was blanked and the reacted sample value seen was multiplied by 2 to give the value of residual alum in mg/l.

Free Residual Chlorine
Free residual chlorine was measured using a chlorine meter.The chlorine meter was switched on and a sample volume of 10 mls was put into a sample cell.The machine was adjusted to zero using the sample.In the same volume, 0.1 mg of DPD powder reagent was added, shaken and measured to record the value in mg/l.

Faecal Coliform Counts
Faecal coliforms were measured using the membrane filtration method.Water was boiled in a sterilizing pan to sterilize the filtering gadgets.An absorbance pad was then put in a sterilizing dish and soaked with an enriched lactose culture media of about 2 mls.The sterilized filtering gadgets were then removed and fixed on the vacuum pump.The sterile filter membrane was put and 100 ml of the sample was filtered through it.The membrane was then removed aseptically using forceps, put in the dish containing the lactose culture media and closed.The dish was then put in an incubator at an incubation temperature of 44.5˚C ± 0.2˚C and the incubator was switched on for 24 hours.The incubator was then switched off from the power source.The sample was removed and a count of the number of blue colonies on the membrane was made and recorded in CFUs/100 ml.

Data Analysis
The descriptive statistics (minimum, maximum, standard deviation, mean, standard error of the mean) of the measured physico-chemical and biological parameters were tabulated.The variations of physico-chemical parameters and faecal coliform counts among the raw and tap water sources were established using one-way ANOVA (F) test while variations of the parameters between raw and tap water sources were ascertained by a z-test.Relationships between the measured water parameters (physico-chemical and faecal coliforms) were determined using Pearson correlation coefficient (r).Results were significant at 5% level of significance.The data presentations and analyses were done using Microsoft Excel 2007 and SPSS 20.0 Statistical packages.

. pH
The pH is a measure of the hydrogen ion concentration in water [20].The pH of water is important to living organisms as many biological processes occur only within a narrow pH range [21] [22].There was low variability of pH within the samples of raw and tap water as well as the overall raw and tap water sources (CV; raw water, 0.94% -9.98%; tap, 0.63% -6.61%; overall raw, 10.29%; overall tap, 9.57%) as shown in Tables 1-3.There was a significant variation (p < 0.05) in the mean pH of the raw water sources with values ranging from 5.21 to 6.75 (Table 1).The highest pH was recorded in the surface well below Nyandozo Primary School and the lowest in the protected spring below Kikuba Hill.Similarly, pH varied significantly (p < 0.05) among the tap water sites (Table 2).Tap water at Kanyamabona Trading Centre recorded the highest pH (7.06) while the least pH (5.72) was found in tap water at Nyakabirizi Trading Centre.On overall, raw water (pH = 6.17) recorded significantly higher pH than tap water (pH = 6.03).
The mean pH ranges of most of the raw water sources fall within the WHO [23] standard limit of 6.0 -8.0 apart from the protected spring below Kikuba Hill with mean pH below the WHO limit (Table 1).On the other hand, most of the raw water sources had mean pH below the UNBS [24] guideline of 6.5 -8.5 except the surface well below Nyandozo Primary School (Table 1) with mean pH within the UNBS guideline.The pH ranges of tap water from all the sites (Table 2) fall within either the standard [24] or [23] values of 5.5 -8.5 and 6.5 -8.5 respectively.The overall mean pH of the raw water sources (Table 3) was also within the WHO guideline but below the UNBS standard.On the other hand, the overall mean pH of the tap water sources (Table 3) was within the UNBS guideline but below the WHO standard.
The mean pH values of the drinking water sources from Nyaruzinga wetland were slightly acidic possibly due to decomposition of organic material within the wetland forming acidic compounds which lower the pH.According to Bot and Benites [25], the decomposition of organic wastes produces organic acids.The slight acidity of tap water is possibly attributed to the incomplete removal of the acidic compounds during the treatment process.Acidic pH was also recorded by Safari et al. [26] in most of the Nyaruzinga wetland water obtained near human activities as well as the treated tap water.

Electrical Conductivity (EC)
Electrical conductivity is the measure of the capability of water to transmit electric current and is a useful tool for assessment of the purity of water [27].Conductivity does not directly affect human health.However it is measured to determine the rate of mineralization (existence of minerals such as potassium, calcium, and sodium) and also to estimate the amount of chemical reagents used to treat water [28] [29] [30] [31] [32].
The within sample variability of electrical conductivity in the raw (Table 1) and tap water (Table 2) sources were relatively low with CV ranging from 3.35% -17.66% (raw water) and 6.35% -20.10% (tap water).Furthermore, the variability of EC within samples of the overall tap water sources were relatively low (CV = 15.83%).However, the overall sample variability of EC in raw water sources was moderate (CV = 47.29%).There was significant variation (p < 0.05) in EC among the various raw and tap water sources (Table 1 and Table 2) and between the overall raw and tap water sources (Table 3).This signifies that there is very little dissolution in the groundwater, rapid ionexchange between the soil and water, or a poor and rather insoluble geologic rock and mineral types underlying Nyaruzinga wetland [3].
However the high EC in the surface well below Nyandozo Primary School could be associated with deposition of metal ions (e.g.iron etc) into the water through surface runoff despite some level of protection of the surface well.This is supported by the very high total iron in the surface well compared to other raw water sources (Table 1).Furthermore, there is an overall significant positive correlation between EC and Total iron content (Table 4) in all the water sources (r = 0.75, p < 0.01).The EC in the drinking water sources in this study were also low compared to the EC of the direct wetland water obtained by Safari et al. [26] near sewage discharge grounds though the EC values of the drinking water sources were higher than the wetland water near fish ponds, dip tank, raw water reservoir and car washing bay.This implied that there was possibly an increased surface runoff of the metal ion into the wetland from human activities as the wetland does not receive any form of protection in its natural state.According to Mugyenyi and Mujurizi [8], there are no conservation measures put in place to prevent the degradation of Nyaruzinga wetland.
The electrical conductivity of the tap water sources is as a result of metal ions coming from the corrosion of the water pipes under acidic conditions (Table 2).
Acidic water can leach metals from pipes and fixtures, such as copper, lead, zinc, iron and manganese [28] [33].In addition, there were also significant (p < 0.01) negative and positive correlations of Total iron with pH (r = −0.45)and EC (r = 0.34) respectively for tap water (Table 4).These therefore signify that corrosion tap water sources to the corrosion of metals which led to the accumulation of heavy metals.The very high EC of the tap water (176.17µS/cm) obtained by Safari et al. [26] compared to EC values of the tap water sources in this current study (Table 2) can be associated with increased corrosion of metal pipes which were exclusively used for supply of tap water in the past years.However, there has been a replacement of most of the metal pipes with plastic pipes in the recent years.

Apparent Colour (AC)
Drinking-water should ideally have no visible colour.Nevertheless, colour in drinking-water is usually due to the presence of coloured organic matter (primarily humic and fulvic acids) associated with the humus fraction of soil as well as the presence of iron and other metals, either as natural impurities or as corrosion products [23].However, the most common cause of water color is the presence of minerals mainly iron and manganese, eroded soil followed by algal growth [35].There were highly variable values of apparent colour of water within samples for the raw water sources (CV, 10.81% -86.08%), tap water sources (CV, 17.49% -54.22%) and the overall raw (CV = 181.74%)and tap water (CV = 36.33%)sources.The apparent colour of water significantly (p < 0.05) varied among the raw and tap water sources and between the raw and tap water sources on overall.The surface well below Nyandozo Primary School had the highest apparent colour (157.58Pt/Co) while the protected spring below Kyeitembe Vocational Secondary School had the least apparent colour (3.28 Pt/Co).
Tap water near St. Agnes Girls Secondary School had the highest apparent colour (9.65 Pt/Co) and that near Bassajjabalaba Primary School had the least (5.60 Pt/Co).On overall, raw water registered a higher apparent colour (37.42 Pt/Co) than tap water (7.94Pt/Co).The apparent colour (AC) of the protected spring below Kyeitembe Vocational Secondary School, Surface well below Kyeitembe Trading Centre and the protected spring below Kikuba Hill were within the UNBS standard of <15 Pt/Co (Table 1).On the other hand, the AC of the Borehole below Bweranyangi Junior School and the Surface well below Nyandozo Primary School were above the UNBS guideline value.However, the apparent colour of all the raw water sources were within the WHO guideline of <1500 Pt/Co.Similarly the apparent colour of all the tap water sources were within the UNBS (<15 Pt/Co) and WHO (<300 Pt/Co) standard values (Table 2).The raw water sources on overall had apparent colour beyond UNBS guideline value but within the WHO standard value.On the other hand, the tap water sources on overall recorded low apparent colour but within both UNBS and WHO guideline values.
The relatively high apparent colour of the surface well below Nyandozo Primary School as opposed to the other water sources is due to surface runoff of some particulate matter especially from gardens within the watershed causing high turbidity and total iron content in the water (Table 1).This is supported by the overall significant positive correlation of apparent colour with turbidity (r = 0.97, p < 0.01) and total iron (r = 0.77, p < 0.01) as shown in Table 4.According to Walakira [35], water color is attributed to the presence of minerals mainly iron as well as eroded soil.The low apparent colour of the drinking water sources from Nyaruzinga wetland signifies low concentration of total suspended and dissolved solids possibly due to some level of protection of the water sources.However, the high apparent colour of the water obtained directly from the wetland in a previous study [26] is associated with siltation from the degraded surrounding areas by human activities.According to Mugyenyi and Mujurizi [8], Nyaruzinga wetland has been threatened mainly by the increased rate of conversion and siltation resulting from soil erosion from the surrounding agricultural activities and settlement.
The low apparent colour of water from the protected spring is due to filtration of suspended materials as the water percolates through the soil while the lower apparent colour of the tap water compared to raw water is due to the removal of most of the particles responsible for colour in water during the water treatment process.Hence the compliance of the apparent colour of the tap water with WHO standards reflects efficiency in the water treatment process by National Water and Sewerage Corporation.However, the higher apparent colour of the tap water (109.00Pt/Co) reported by Safari et al. [26] than the apparent colour of the tap water sources in the present study (Table 2) is also attributable to corrosion under rampart use of metal pipes in the supply of water in the past years as opposed to the recent years where most of the metal pipes have been replaced with plastic pipes.

Turbidity
Turbidity is the measure of the clarity or cloudiness of water [21].Turbidity in water is caused by the presence of suspended matter such as clay, silt, finely divided organic and inorganic matter, plankton, and other microscopic organisms [35].Water turbidity had relatively low variability within samples among the raw (CV, 4.65% -39.61%) and tap water sources (CV, 8.13% -40.20%).However the within sample variability was moderately high for tap water (CV = 47.35%) and very high for raw water (CV = 172.69%)on overall.The turbidity of water from the various raw and tap water sources as well as the overall raw and tap Similarly, the high turbidity of the surface wells and the direct wetland water obtained by Safari et al. [26] is attributed to siltation from the increased rates of soil erosion within the catchment.The generally higher turbidity of the surface wells than other water sources and the least turbidity of the tap water sources are consistent with the findings of Yasin et al. [34] who obtained higher mean turbidity in unprotected wells compared to tap water.Nevertheless the very high turbidity of the tap water [26] compared to the turbidity values of the tap water sources in this current study also points to increased corrosion under the sole use of metal pipes in supply of water in the past years.However, most of the metal pipes have now being replaced by plastic pipes.The significant positive correlation of turbidity and total iron (r = 0.28, p < 0.01) in tap water (Table 4) supports the fact that turbidity of tap water increases under corrosion of metallic pipes which release iron and other metals.
According to Rahmanian et al. [28], turbidity is also related to the content of disease causing organisms in water originating from soil runoff.The overall significant positive correlation between turbidity and faecal coliforms (r = 0.11, p < 0.05) justify the surface runoff of soil particles with faecal coliforms into the surface wells.Mugyenyi and Mujurizi [8] reported that most fertile soils have been eroded down to the valleys (wetlands) due to the hilly terrain and poor farming methods in Bushenyi.

Total Hardness
Hardness of water is attributed to mainly the bicarbonates, carbonates, sulphates and chlorides of calcium and magnesium [20].Total hardness of the raw and tap water sources exhibited low variability within the samples i.e. raw water (CV = 2.58% -11.79%), tap water (CV = 2.75% -11.81%).However the within sample variability for the overall tap water sources was moderate (CV = 41.19%) while that for the raw water sources was high (CV = 70.25%).There were significant differences (p < 0.05) in the total hardness among the various raw and tap water sources.The surface well below Kyeitembe Trading Centre had the highest total hardness (85.45 mg/L) while that below Nyandozo Primary School had the least hardness (17.23 mg/L).On the other hand, the tap water at Kanyamabona Trading Centre recorded the highest total hardness (60.85 mg/L) with the least hardness (23.03 mg/L) being registered in tap water near St. Agnes Girls Secondary School.However there was no significant variation (p > 0.05) in the overall total hardness of the raw and tap water sources though raw water (36.05 mg/L) recorded slightly higher total hardness than tap water (34.19 mg/L) on (<0.3 mg/L).The rest of the raw water sources had total iron concentrations within the WHO guideline value.Tap water from all the selected sites (Table 2) had total iron contents within the UNBS and WHO guidelines of <0.2 mg/L and <0.3 mg/L respectively.Similarly, the overall raw and tap water sources (Table 3) contained total iron concentrations within the accepted UNBS and WHO standards.The high iron concentrations in the Surface well below Nyandozo Primary School could be associated with sewage runoff from the latrines and landfills (waste sites) in the school especially during rainfall.There is also a possibility of direct ground seepage of iron from the latrines into the surface well.
According to Water Stewardship Information Series [39], sewage and landfill leachate are sources of iron to local groundwater.However, the high total iron in the tap water near Bassajjabalaba Primary School can be associated with the high corrosion of metal pipes under acidic pH conditions.On the other hand the low iron content in the tap water at Kanyamabona Trading Centre is due to reduced corrosion of the metal pipes under neutral water conditions.This is further supported by the significant negative correlation between total iron and pH (r = −0.45,p < 0.01) of tap water (Table 4).Rahmanian et al. [28] asserts that acidic water corrodes metal pipes and plumping system.

Residual Alum
Aluminium or iron salts (granules, powders or tablets) added to water, coagulate and flocculate impurities and promote rapid and efficient sedimentation and also enable the inactivation of microbes by free chlorine [23].The aluminium forms aluminosilicates which frequently deposit onto plumbing materials in distribution systems thus protecting the pipes from corrosion [40].The residual alum in the tap water sources exhibited relatively moderate variability within the water samples (CV = 22.81% -40.63%) with significant variations (p < 0.05) of the mean residual alum among the various tap water sources.Tap water near Bushenyi Town School had the highest mean residual alum (0.113 mg/L) while the tap water at Kanyamabona Trading Centre recorded the least residual alum (0.092 mg/L).The overall mean residual alum was 0.103 mg/L.The amounts of the residual alum in the tap water sources were within the UNBS and WHO standard of <0.2 mg/L.The mean residual alum for tap water was within the WHO recommended range for safe domestic potable water attributable to the efficient water treatment process that uses proportionate doses of these chemicals.The high residual alum in the tap water near Bushenyi Town School can also be associated with the increased corrosion of the metal pipes under acidic pH conditions (Table 2) to release aluminium into the water.Conversely, the low residual alum in the tap water at Kanyamabona Trading Centre is due to reduced corrosion of the metal pipes under neutral water conditions (Table 2).This is also in line with the fact that acidic water leaches metals from pipes [28] [33] as opposed to neutral and alkaline waters.The significant negative correlation between residual alum and pH (r = −0.22,p < 0.01) in tap water

Figure 1 .
Figure 1.Map of Uganda showing the location of Bushenyi district, Nyaruzinga wetland and the study sites.

3. 1 .
Physico-Chemical Parameters in the Raw and Tap Water Sources in Bushenyi Municipality 3.1.1 water were significantly (p < 0.05) different from one another.The surface well below Nyandozo Primary School had the highest turbidity (27.38 NTUs) while the surface well below Kyeitembe Trading Centre recorded the least turbidity (0.40 NTUs).The tap water near Bushenyi Town School was the most turbid (2.46 NTUs) whereas the tap water at Kanyamabona Trading Centre was the least turbid (0.46 NTUs).On overall, raw water sources (6.64 NTUs) were also more turbid than tap water sources (1.68 NTUs).The turbidity of the Borehole below Bweranyangi Junior School, Protected spring below Kyeitembe Vocational Secondary School, Surface well below Kyeitembe Trading Centre and the protected spring below Kikuba Hill were within both UNBS (<10 NTUs) and WHO (<15 NTUs) guideline values for raw water.However, the surface well below Nyandozo Primary School recorded turbidity beyond the UNBS and WHO standard values.On the other hand, the turbidity of the tap water sources were all within the UNBS and WHO guideline of <5 NTUs.Similarly, the overall raw water sources registered turbidity (6.64 NTUs) in the range of UNBS and WHO standard values.The overall turbidity of the tap water sources (1.68 NTUs) was also within the UNBS and WHO standards for tap water.

Table 1 .
Descriptive statistics of water quality parameters for raw water from Nyaruzinga wetland.

Table 2 .
Descriptive statistics of water quality parameters for tap water in Ishaka, Central and Nyakabirizi divisions of Bushenyi Municipality.

Table 3 .
Descriptive statistics for physico-chemical parameters between raw and tap water.
The surface well below Nyandozo Primary School also had the highest EC (200.90 µS/cm) while the Protected spring below Kikuba Hill recorded the least value (65.08 µS/cm).
bona Trading Centre.On overall, raw water also recorded higher EC (108.94 µS/cm) than tap water (EC = 74.89µS/cm).The EC values in each of the raw and tap water sources as well as the overall raw and tap water fall within the standard UNBS (raw water, <2500 µS/cm; tap water, <1500 µS/cm) and WHO (raw water, <1500 µS/cm; tap water, 0 -300 µS/cm) values.The EC of the groundwater sources (borehole and spring) were much lower than that of the surface wells.