Lake Victoria the second largest fresh water body in the world located in East Africa is a shared resource between Kenya, Tanzania and Uganda and enjoys a wide range of streams and rivers from as far as Burundi and Rwanda  . The Kenyan waters of L. Victoria lie just south of the equator between 004'S - 0032'S and 34˚13'E - 34˚52'E, and cover an area of 3600 km2 of which 1400 km2 is the Winam Gulf . Unlike Uganda and Tanzania, the Kenyan waters shoreline is dominated by the Nyanza Gulf an important economic and ecological water front to an estimated 3 million people settled along the gulf shores. The shared vision and strategic frame work for Lake Victoria basin muted in 2003 is to have a prosperous population living in a healthy and sustainably managed environment providing equitable opportunity and benefits . It is documented that human society has over time used freshwater from rivers, lakes, groundwater and wetlands for many different rural, peri-urban and urban agricultural and industrial activities, but in doing so has overlooked its value in supporting ecosystems. Freshwater is vital to human life and societal well-being, and thus its utilization for consumption, irrigation and transport has long taken precedence over other commodities and services provided by freshwater ecosystems . However, this has not been possible due to frequent pollution of the lake thus affecting human health and fish environment . Lake Victoria has environmentally undergone physical, chemical and biological changes in the last four decades, particularly rise in its trophic condition and decline in oxygen level, which affects the water quality and fish population dynamics  . This is attributed to increased nutrient loading from both atmospheric deposition and surface run-off both being factors of rising human population and their associated anthropogenic activities resulting in growing changes in the lake’s phytoplankton community . The pollution impact by municipal and industrial discharge is visible in some of the rivers discharging into the largest East African lake as well as the shoreline mainly along shallow areas of Kenya’s Winam Gulf in Kisumu, Tanzania’s Mwanzaarea and Uganda’s Inner Murchison Bay as well as Jinja catchment    . A number of factors have been listed to affect the quality of Lake Victoria waters among them being rapid population growth, increased agriculture, urbanization, industrial activities, poverty in rural and peri-urban areas, and uncontrolled dumping of waste among others despite existing environmental policies  . According to , forests are being cut down, soils are eroded, wetlands are drained, channels are silted accelerating lake water pollution from non-point sources (NPS) further reducing access to already limited freshwater for human use. According to , the increase in cereal demand in Africa by 2025 estimated at 65% resulting from rising human population will require more water for irrigation. The anticipated threefold increase in water demand by Africa will emanate from municipal and domestic sectors which will account for an estimated 320 billion cubic meters while competition with other water using sectors, notably agriculture will account for 92 billion cubic meters . In this regard,  states that the amount of water available per person in Africa is far below the global average and is declining with annual per capita availability of 4000 cubic meters compared to a global average of 6500 cubic meters. The science challenges dealing with marine international waters such as L. Victoria at a trans-boundary, regional and global level include multiple stressors such as eutrophication, overfishing, habitat destruction, pollution, harmful algal blooms and the movement of opportunistic invasive species .
Lake shore development has also been identified as one of the factors that impact critical ecosystem processes and ecological features of the adjacent lake . Residential development for instance has been associated with increased siltation and fish exploitation rates, and reduction of habitat complexity which collectively affect fish populations and growth more so of species that use the habitats at a given development stage in their life cycle.  reported a negative correlation between size-specific growth rate and degree of residential development in bluegill sunfish. In the same study, bluegill in highly developed lake shores were found to be less productive (2.3 times less) as compared to those in lowly developed lake shores. Despite the enormous knowledge of all these factors affecting water quality, there are no mechanisms for assessing the impact of the resultant loads on the surface and subsurface water, and ultimately the potential of the lake to support productive aquatic life, thus the reason for the current study.
The current study therefore set-out to determine the quality of water in selected fishing beaches of Lake Victoria, Kenya with a view to report the possible pollution levels within the waters that would contribute directly or indirectly to fisheries and fish biology in the region.
2. Materials and Methods
2.1. Study Sites
The study area comprised of near-shore shallow waters at fish landing beaches mainly in the Nyanza Gulf and selected parts of the main lake, Kenya side (Figure 1). The environmental characteristics including aquatic vegetation cover, human settlement and activities at each beach also referred to as site were considered as well as natural conditions influencing water quality and their effect on the quality of harvested fish. In almost all the sites, landed fish were cleaned with water obtained from near the shores of the lake. The choice of the sampling site were as a result of hygienic levels of by-catch and processed fish waste disposal , human settlement associated anthropogenic activities and existing records on Lake Victoria pointing at pollution and eutrophication. A total of 12 fish landing beaches were investigated within the wet and dry seasons (Figure 1; Table 1). Six beaches (sites 1 - 6) were sampled in September 2015 and the other six (sites 7 - 12) in November 2015 between 09:00 hrs and 15:30 hrs. The location of each sampling site was determined using a Geographical Positioning System (Garmin
Figure 1. Map of the study area showing the position of the sampling sites (points (1 - 12)) on Lake Victoria.
tino 130). Three (triplicate) measurements and water samples were taken at each sampling site, one set immediately at the shoreline 2 - 4 meters offshore (≤1 m depth) and a second set 100 - 200 m (≤5 m depth). In situ measurements of water temperature, pH, electrical conductivity and turbidity were taken with a Hydrolab (Hand-held Water Quality Meter WQC-24) and total dissolved solids TDS with an OysterTM meter. Secchi depth was estimated with a 20 cm diameter black and white Secchi disc.
2.2. Water Sampling and Analysis
Water samples were collected from 0.5 m below the surface with polyethylene bottles, stored at 4˚C in a cooler box and later transferred to a refrigerator (−20˚C) in the laboratory until analysis. Prior to determination, water samples were brought to room temperature and filtered through 0.45 µm pore size filters and immediately frozen at −20˚C in readiness for analysis. The water samples
Table 1. Description of the 12 sampling sites on Lake Victoria (Kenya part).
were subjected to various analyses using methods selected from  They included spectrophotometric methods for phosphate-phosphorus PO4-P (soluble reactive phosphorus SRP, ascorbic acid) and Ammonium-nitrogen NH4-N (Manual phenate, indophenol-blue). Total suspended solids (TSS) were estimated from residue filtered on GFC filters and dried at 103˚C - 105˚C. Chlorophyll a and c were determined after 18 - 24 hour cold extraction of the pigment in 90% acetone. All spectrophotometric readings were done using a Spectro UV-11 spectrophotometer. Dissolved oxygen DO values measured with the Hydrolab were cross-checked with the Winkler titration method. Biochemical oxygen demand (BOD) was measured by the 5-day BOD test . Chemical analyses were done at the Department of Biological Sciences, Masinde Muliro University of Science and Technology (MMUST), Kakamega, Kenya.
2.3. Statistical Analysis
Descriptive statistics (means and standard errors) for each treatment were computed using the data analysis pack on excel. QQ plots were used to check the normality of data whereas homogeneity of variance was assessed using Levene’s test. A two way analysis of variance was used to compare means between treatments. Pairwise comparison of treatment was executed using Turkey’s Honest Significant difference method. All statistical tests were conducted using R-statistical software version 3.6.1 with 95 % confidence level.
3.1. Water Quality Characteristics of Sampling Sites
A summary of water quality characteristics of the sampling sites is presented in Table 2 below. The mean pH values varied significantly with sites (p < 0.05) but were insignificantly variable with distance from lakeshore (p > 0.05). The highest pH values were 9.3 ± 0.0 and 9.3 ± 0.1 observed at Luanda Kotieno and Luanda Nyamasari respectively. The lowest pH values were 7.08 ± 0.1 and 7.08 ± 0.0 observed in samples collected from deeper waters at Nyachebe and Kichinjio sites respectively. The mean temperature values observed varied significantly (p < 0.05) with site and distance from the lake. The highest mean temperature was 29.5˚C ± 0.0˚C as observed at Luanda Nyamasari whereas the lowest mean temperature was 23.4˚C ± 0.2˚C at Kichinjio.
The mean conductivity varied significantly (p < 0.05) with site and distance from the lake shore. The highest mean conductivity was 173.0 ± 0.6 mS∙m−1 and as observed at Kichinjio, whereas the lowest was 69.0 ± 1.7 mS∙m−1 as observed at Usenge. The mean TDS values also varied significantly (p < 0.05) with site and distance from the lakeshore. The highest mean TDS was 135.00 ± 0.58 mg∙l−1 at Kagwel whereas the lowest mean TDS was 60.7 ± 1.6 mg∙l−1 at Nyachebe. The mean DO values varied significantly (p < 0.05) with site and distance from the lakeshore too. The highest mean DO value was of 10.3 ± 0.2 mg∙l−1 was observed at Luanda Kotieno whereas the lowest mean DO of 2.40 ± 0.1 mg∙l−1 was recorded at Seka. Similarly, the mean BOD values varied significantly (p < 0.05) with site and distance from the lakeshore. The highest BOD mean value were 7.8 ± 0.3 mg∙l−1 recorded at Luanda Kotieno whereas the lowest BOD values were 0.0 ± 0.0 mg∙l−1 at Mainunga and Ngengu sites.
Mean turbidity values also varied significantly (p < 0.05) with sites and distance from the lakeshore. The highest mean turbidity value was 125.5 ± 0.9 NTU recorded at Uyoga whereas the lowest turbidity value was 2.7 ± 0.1 NTU observed at Osieko. The mean secchi depth readings too varied significantly (p < 0.05) with site and distance from the lakeshore. The highest mean secchi readings were 1.2 ± 0.0 m recorded at Nyachebe and Usenge. The lowest mean secchi value was 0.16 ± 0.00 m as observed at Uyoga. Finally, same trend was recorded for mean TSS values which varied significantly with site (p < 0.05) and distance from the lakeshore. The highest mean TSS value was 10.2 ± 0.3 mg∙l−1 and was observed at Nyamasari whereas the lowest was 0.3 ± 0.1 mg∙l−1 was observed at Usenge. Generally, there was no a clear pattern observed between the values obtained in all the water quality parameters assessed and distance from the lakeshore.
3.2. Nutrients and Chlorophyll Levels
A summary of the nutrients and chlorophyll levels in samples collected from different sampling sites is presented in Table 3 below. Mean values of chlorophyll a (chl a) varied significantly with site (p < 0.05) and distance from the lakeshore. The highest mean chl a value was 66.9 ± 0.9 μg∙l−1 and was observed at Kichinjio (0 m) whereas the lowest was 13.2 ± 0.2 μg∙l−1 recorded at Seka. Mean chlorophyll c (chl c) values similarly varied significantly with site (p < 0.05) and distance from the lakeshore. The highest chl c mean of 134.7 ± 3.8 μg∙l−1 was
Table 2. Mean values (±standard error) of water quality parameters measured in the study area.
TEMP = temperature, COND = conductivity, TDS = total dissolved solids, DO = dissolved oxygen, BOD = biochemical oxygen demand, TURB = turbidity, SECC = secchi depth and TSS = total suspended solids. Units: pH (pH units), temperature (˚C), conductivity (mS∙m−1), TDS (mg∙l−1), DO (mg∙O2∙l−1), BOD5 (mg∙l−1), turbidity (NTU = Nephelometric turbidity units), Secchi depth (m), TSS (mg∙l−1).
recorded at Luanda Kotieno whereas the lowest (0.63 ± 0.1 μg∙l−1) was recorded at Kagwel. Similar trend was observed for mean PO4-P values obtained from the analysis which varied significantly with site (p < 0.05) and distance from the lakeshore too. The highest mean PO4-P was 310.7 ± 1.7 μg∙l−1 observed at Dunga whereas Luanda Kotieno posted the lowest PO4-P of 28.9 ± 1.4 μg∙l−1. Dunga again recorded the highest mean NH4-N of 1278.3 ± 6.7 μg∙l−1 whereas Luanda Nyamasarire corded the least (12.4 ± 0.8 μg∙l−1).
Freshwater ecosystems, such as lakes, wetlands and rivers have specific requirements in terms of quantity, quality and seasonality of their water supplies.
Table 3. Mean (±standard error) of nutrients and chlorophyll levels in samples collected from different sites in the study area.
Units: Chlorophyll a (μg∙l−1), Chlorophyll c (μg∙l−1), Phosphate phosphorous (PO4-P) μg∙l−1, Ammoniacal nitrogen (NH4-N) μg∙l−1.
Sustainability normally requires these systems to fluctuate within a natural range of variation. One of the fundamental factors that are affected by water pollution is the pH. Overally, the pH values observed in the current study had a higher upper limit compared to earlier findings  though all sampling sites with an exception of Kagwel and Nyamasari posted pH values that were still within the optimal range (6.5 - 9.0) for most aquatic chemical reactions as well as aquatic organisms’ life including fish. It is worth noting that pH values outside the optimal range would have negative implications on aquatic life such as increased toxicity of chemical compounds, reduced hatching and survival rates among others . The variations of pH values observed among the sampling sites could be an indication of the different levels of respiration and decomposition activities taking place below the lake surface among the different sampling sites, and varying volumes of wastewater discharged .
Water temperature influences several processes in aquatic environment including metabolic rates, photosynthesis production as well as levels of other water quality parameters such as dissolved gases, pH and conductivity. Current study showed temperature variations across sampling sites and this could be associated with varying loads of total suspended solids discharged by rivers and domestic runoffs into the lake which in turn absorb solar energy hence increasing temperature . Generally, the sites that reported higher temperatures also posted high pH values. , noted that as temperature increases or decreases, a shift in ion concentrations in the water changes thus affecting the pH value. Therefore, the higher temperature directly affected the pH through dissociation and solubility of certain compounds in the water column .
The toxicity of ammonia (NH3) is critically dependent on pH and temperature. As pH increases, ammonium cation ( ) is converted to NH3, and the toxicity increases . In the current study, ammoniacal nitrogen was highest at Luanda Nyamasari an occurrence that is closely linked to the sites high temperature and pH. Higher nutrients levels in the gulf have also been reported in earlier studies by  . This could be an indication that there was municipal, agricultural and industrial pollution in these sites since nutrients and sediments from far inland enter the lake directly without being filtered as a result of clearing of vegetation surrounding the Lake.  noted that fishing shoreline settlements have less than 20% of pit latrines in place thus most human waste is discharged directly into L. Victoria. This nitrogen would equally be flux from the sediments to the water column in most of the landing sites such as Ngegu shoreline . Buildup of aquatic macrophytes including algae and hyacinth contribute significantly to higher NH3 levels as they die off and are swept by waves to decay in sheltered shores of the lake.
Extensive water hyacinth mats frequently settle in near-shore waters for considerable periods of time. When this is tied to the removal of NO3 efficiency of the lake, it should be noted that the higher NO3 removal is as a result of uptake by the dominant phytoplankton species which is reflected by the total dissolved solids, EC and secchi depth readings. Low nutrient removal efficiency even under conditions of high nutrient concentrations could be light limitation of phytoplankton growth due to excessive chlorophyll a, an occurrence witnessed in this study. The highest chl a value, 66.9 µg∙l−1 was recorded at Kichinjio where there was an apparent algal bloom on the water surface. The lowest chl a value, 13.2 µg∙l−1 was recorded at Mainunga a site limited in human activity, runoff and aquatic vegetation degradation compared to high density human population at Kichinjio. The concentration of chl a fluctuated irregularly across the sampling sites although slightly high values occurred in mid Nyanza Gulf sites. Higher values in sites inside the lake indicated larger amounts of photosynthesizing phytoplankton or algae compared to the shoreline. chl c also fluctuated rather irregularly with the highest value being 134.7 µg∙l−1 at Luanda Kotienoan occurrence closely linked to the sites elevated NH4-N at 100 m offshore compared to all the other sites.
Dissolved oxygen is critical for key biological processes such as decomposition and respiration in plants, animals and bacteria in aquatic systems. Aquatic organisms DO requirements vary widely and are also tied to the organisms’ vertical and horizontal trophic position. In the current study, DO fluctuated between 2.0 and 10.0 mg/L across the different sampling sites, however there was no clear pattern with respect to distance from the shore a factor of lake water currents, river inflows, algal blooms and suspended solids among others as has also been previously reported  .
Total Suspended Solids (TSS) are organic and inorganic solid materials that are suspended in water. They include silt, plankton and industrial wastes which will not pass through the filter . Findings from the study in L. Victoria Kenya side had turbidity and TSS increase at the shoreline in most of the sampling sites an indicator of inputs of soil and sediments from the catchments mainly through runoff, shoreline erosion, and re-suspension of bottom sediments by waves, currents, lake mixing as well as human related activities. Whereas, phytoplankton is the main contributor of offshore turbidity and TSS, secchi depth was inverse to the levels of these two variables since it largely depended on the water clarity. The highest secchi depth values recorded at Nyachebe and Usenge off shore were a factor of the sites exposure to north western and southern parts of the open lake. The turbidity values observed in most of sampling sites in the current study were much lower compared to an earlier  perhaps due to the differences in locations of sampling sites. Turbidity and TSS though related did not demonstrate any correlation within and across sampling sites.
Pollution is viewed as a serious threat to water quality for its direct and indirect impacts on lake communities . Silt, clay and other organic particles can suffocate larvae and clog gills of many aquatic organisms and interfere with their normal functioning or even cause death. They can also interfere with light penetration into the water column retarding growth of phytoplankton and macrophytes thereby lowering primary productivity, release of oxygen into the water and life of other aquatic organisms. Silt, clay and other organic particles are also known to form attachment substrates for many types of bacteria and other micro-organisms. The WHO  and EPA  standards for turbidity of drinking water is a value of less than 5 Nephelometric Turbidity Units (NTU) and appear clear . In this study, turbidity values were generally higher in sites of the mid Nyanza Gulf and decreased irregularly towards the north western and Southern sites all exposed to open lake dilution effect. Majority of the high values were recorded near the shoreline than deeper parts of the lake. Similarly, higher values of TSS were recorded in the southern sites and reduced towards the north.
Total dissolved solids (TDS) refer to all ion particles in solution that are smaller than two microns . It is a measure of the combined content of all organic and inorganic substances contained in a liquid in molecular, ionized or microgranular suspended form. The primary sources of TDS are the agricultural and residential runoff, leaching of soil contamination and point source water pollution discharge from industrial and sewerage treatment plants. TDS majorly constitutes the ions; sulphates (SO3−), Cl−, carbonates (CO3−), and cations; potassium (K+), Sodium (Na+), magnesium (Mg2+) and calcium (Ca2+). Like conductivity, the levels of TDS are influenced by dissolved ions and salts, in addition to micro-colloidal substances. The TDS were below 500 mg/l thus were within the acceptable levels according to .
Rain washes sediments and nutrients from bare soil into receiving waters . Sediment analysis showed that nitrogen flux from the sediments to the water column is more pronounced than the phosphorus flux in most of the landing sites. This suggests that the phosphorus loading to the lake may be primarily external rather than from the sediments. Continuous mixing of the Lake waters by the wind, especially during late afternoons and early morning hours when winds are strongest in the gulf   helped to keep the gulf well oxygenated throughout the year and led to the re-suspension of bottom sediments, which contributed to low water transparency in the gulf. Elevated phosphates near the shoreline waters are due to inputs resulting from weathering processes of the substratum and land erosion from the almost bare or cultivated land and other anthropogenic activities, mineralization of organic matter and recycling from decomposing dead water hyacinth plants. Seka which had the highest PO4-P had a black muddy substrate and decomposing water hyacinth plants. The presence of readily measured PO4-P and NO3-N concentrations throughout the gulf and the inverse relation between Secchi disc depth and chl a is consistent with light limitation of algal growth and nutrient demand. The increased release of phosphorus from the sediment that occurred during dry season was associated with elevated temperature and pH   and inversely lower DO concentration thus promoting anaerobic condition.
5. Conclusion and Recommendations
In the current study, water quality parameters varied significantly across the different sampling sites in the area studied. Extreme values of different water quality parameters (DO, pH, turbidity and nutrients) observed in different sites could be an indication that the onshore activities in the different study sites are altering the water quality of the study area. Values outside the recommended ranges in some of the water quality parameters in the current study were posted both in nearshore and offshore sampling site, an indicator that pollution in the study area is not restricted to lakeshore but also offshore probably due to adequate mixing of water in the study area. It is worth noting that much higher values of temperature, pH and ammoniacal nitrogen were posted in the current study compared to earlier studies conducted in the study area which could be an indicator of progressive deterioration of the water quality thus the need to review the management measures and interventions in place. Further studies of this kind more so linking fish populations and catch statistics with water quality and onshore human activities would provide important information for comprehensive sustainable management plan of the resource.
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