Spatial variation in acid and some heavy metal composition of rainwater harvesting

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Nat Hazards(2010)55:307–319DOI10.1007/s11069-010-9529-2O R I G I N A L P A P E RSpatial variation in acid and some heavy metal composition of rainwater harvesting in the oil-producing region of NigeriaS.I.EfeReceived:2January2008/Accepted:24March2010/Published online:5May2010ÓSpringer Science+Business Media B.V.2010Abstract The study adopted the experimental research design andfield survey of the oil-producing region of Nigeria for the past10years.A total of100sterilized rain gauges were randomly distributed on the basis of50each to the eastern and western division of the oil company operating in the region.The rainwater samples harvested through this process were transferred into sterilized plastic containers and kept in coolers and taken immediately to the laboratory for analysis soon after every rain event.The rainwater samples were analysed in the laboratory with the most appropriate techniques.The physicochemical characteristics of rainwater harvested were subjected to paired t test and3-year moving average statistical analysis.The following are the results:There is widespread acid rain in the region,this is evident from pH values that span4.98–5.15and5.06mean values.The result also revealed that acid rain(pH)varied significantly(P[0.05),and it decreases with increasing distance from gasflare sites throughout the period of study.Other physico-chemical characteristics of rainwater resources conform to safe limit with the exception of turbidity,TSS,Pb and NO3,which is also significant at P[0.05with increasing distance from the gasflare sites,as such they decreases with increasing distance.This certainly has serious environmental effects on the human and other species,soil,water and vegetation resources and calls for the extinction of gasflaring,in this region.Sources of water that are acidified should be periodically limed to reduce the acid concentration in such water. Keywords Acid rainÁHeavy metalÁGasflareÁNiger Delta1IntroductionAcid rain is one of the major environmental problems that have characterized the oil-producing region of Nigeria in recent times.There are a series of widespread allegations that gasflaring in the Niger Delta region of Nigeria was contributing greatly to acid rain in this region(Shell Petroleum Development Company SPDC1995).The consequences of S.I.Efe(&)Geography and Regional Planning,Delta State University Abraka,Abraka,Nigeriae-mail:efesunday@this according to the host communities are not only limited to the corrosion of metals,but also lowers the quality of rainwater harvesting,acidifies other water sources and depletes soil fertility leading to the extinction of vegetation species in the area(Akporido et al. 2000;Okecha2000).Shell Petroleum Development Company(1995)asserted that although the occurrence of acid rain is restricted to the foci or vicinity of the gasflares,there is no evidence that gas flaring is the major factor.However,Alakpodia(2000)and Okecha(2000)suggested that gasflaring is the major cause of acid rain in the Niger Delta region of Nigeria and called for more studies to regularly assess the issue of acid rain and its causes in this region. More recently,the occurrence of acid rain has also been confirmed in18rural coastal communities of Delta State(2006).A mean pH value of6.4was observed in the open atmosphere,whereas lower pH values of5.0–5.3were seen in roof catchments of buildings in some coastal communities of Delta State,which was attributed to the proximity of these buildings to gasflare sites and the nature of the roofing materials(Efe2006).Acidification of surface and ground water by acid rain in the Western Niger Delta has also been reported (Olobaniyi and Owoyemi2004;Omo-Irabor et al.2008).In addition to impacts on rain pH, it has been suggested that routineflaring in the Niger Delta is linked to thermal pollution, climatic anomalies,extinction of vegetation and animal species and an increase in roof leakages due to a lower rain quality(Ogbe1999;Alakpodia2000;Efe2002;Onianwa et al. 2002).Despite these results,the operatingfirms still hold the view point that gasflaring has no negative impact on the region.Thus,the issue of acid rain in the oil-producing region of Nigeria is still a subject of controversy.It is therefore imperative to empirically assess the precise nature and mag-nitude of the occurrence of acid rain in the region.This study examines the level of acid and heavy metals in rainwater,with the specific aim of ascertaining the spatial distribution of acid rain(if any),its trend and possible environmental implications in the oil-producing region of Nigeria.The concept of acid rain wasfirst referred to by Robert Augus in1872during the industrial revolution to mean any acidic precipitation(such as rain,fog)or depositions that occur downwind of areas where major emission of SO2,CO2,NO x etc.from human activities take place(Oden1976;Botkin and Keller1998;Efe2005).Using this concept,Fig.1shows the various atmospheric pollutants from gasflaring, which react with water in the atmosphere to produce acid rain.It is evident that gaseous emissions of SO2,CO2,NO x,NH3,etc.from burning fossil fuels,form the major source of acid deposition in the region.Once airborne,these pollutants can travel for several thou-sand kilometres,and this long atmospheric lifetime enables their oxidation into acidic species(Wright et al.1976;Berret et al.1983;Pickering and Owen1994;Tripathy and Panda1999).Subsequent deposition of these acids onto land,leads to widespread soil and surface water acidification.Through infiltration processes acid rain also leaches various heavy metals from the soil into subsurface water,which impacts aquatic life.Acid rain also affects theflora and fauna on land as well as causing damage to sculptures and buildings (Pickering and Owen1994;Tripathy and Panda1999).2Study areaThe oil-producing region of Nigeria otherwise referred as Niger Delta region falls within the central coastlands of southern Nigeria.It lies at the intersection of latitude5°31N and5°33Nand longitude 5°30E and 5°32E,one-third of the region is made up of wetlands and house the third largest mangrove forest in the world (Efe 2002).Alakpodia (2000)found oil spillages and gas flaring in the region have resulted in the extinction of many species of vegetation.The region is characterized with subequatorial climate,but this climate has been influenced by the gas flaring in this region with higher temperatures observed closed to gas flare sites.Rainfall is over 3,000mm per year with no dry season,as rain in all months is over 2.5cm.Relative humidity is normally over 90%in the mornings,but drops to 80%in the afternoons (Efe 2002).Although there are other industries in the region like Delta Steel Company Aladja,Warri,Beta Glass Factory Ughelli,Coca Cola Bottling Company Benin and many other oil servicing company these have little influence on the observed climate anomalies (Efe 2003,2005).The region is also characterized with high traffic clogged areas in the cities of Benin,Warri,Yenagoa,Port Harcourt,etc.The pollution from the traffic area in Warri has resulted in mildly acidic rainwater in the city and its environs (Efe 2005).Over 75%of the gas in the Niger Delta gas province has been flared (Oyekunle 1999;Efe 2003),and the year 2010has been pegged by the Nigerian government for the extinction of gas flaring.3Methodology and data collectionThis study adopted the experimental research design,which utilizes data from direct field survey that last from January to December for 10years (1997–2006).A total of 100sterilized plastic rain gauges were randomly distributed on the basis of 50gauges to the western and eastern division each of the SPDC area of operation.The base map of the region,where the oil fields and gas flare sites are located,was obtained and used as basis for the choice of the gauge stations (Fig.2).The rain gauges were positioned at the designated study sites (at distances of 500m,4,8,12km from the flare sites)at 1.5m above the ground.To avoid deposition of dry precipitation on the gauges,they were removed immediately after the rain and returned to the sites when rain bearing cloud was observed.The rainwater samples were collected from the first rain events for every month,Black BoxWater acidificationAquatic biological effect OUTPUTSSoil acidification Terrestrial, biological effectlinking emissions of SO 2,NO x etc.to soil and water acidification modifiedand for time lapse experiment samples were taken at 5,10,15and 20min from the start of the rain event with a final sample for any subsequent rain.All the rain events studied were collected as time lapse samples.The volume of rain in each time interval was recorded,and the samples were analysed for their physicochemical parameters,the average values of the time lapse samples for each rain event were utilized for this study.This technique has been used by Somboon (1997)and Efe (2005,2006).A sub sample of the rain was used to measure pH and temperature immediately upon collection using a Teledo MC236pH meter and digital mercury thermometer.The remaining rainwater collected was poured into sterilized plastic containers with and kept in a cooler containing ice to reduce the degradation of samples before analysis.Upon arrival at the laboratory,turbidity was estimated with a turbidity meter (APHA 214A).NO 3-was determined by colorimetric spectrophotometry,and SO 42-was determined with spectrometry via precipitation with BalCl 2.A digital MC 226conductivity meter was used to determine the electrical con-ductivity and total dissolved solid (TDS)of the water sample.Na ?and K ?were deter-mined with a flame Emission Analyser.Lead,cadmium,magnesium and iron were analysed with an Atomic Absorption Spectrophotometer (AAS)3200Metler model.The details of the analytical methods are listed in Table 1.The paired t test statistical technique was used to test the level of significance difference of elemental concentrations with increasing distance and over the years.The 3-years moving average was employed to describe the trend over the years.Multiple regression and cluster analysis were also adopted to ascertain the causer factors of acid concentration in rain water.4Results and discussionThe data collected for the study are presented in Table 2,Fig.2and discussed later.Bonny platformKALAEKULEOPOBO SOUTHBONNY TERMINALBONNYUTAPATE SOUTHAKASOKRAKAMACAWTHORNE CHBODO WYORLABOMUKOROKORO TAI OBEAKPU AFAM ONNEALAKIRI UBAAJOKPORIEBUBUASARITORUORURIRI PORTHARCOURTISIMIRI APARAELELENWA BUGUMA CR.OBIGBO N.UMUECHEMAGBADANKALIIMO RIVERAWOBAOTAMINI EKULAMASOKUENWHEEBELERUMUEKPE MINI NTAAHIAUBIEMAMBE CR.ODEAMA CR.BELEMAKOLO CR.DIEBU CR.NUN RIVERBENI SEDEPOUKUSHI NOPUKUSHIGBARETELEBOUADIBAWAADIBAWA N.E.AVWERNIORONIOSIOKAUZERE E.UZERE W.UTOROGUURHUREOWEHISOKOOLOMOROUGHELLI E.UGHELLI W.AFIESEREOGINIERIEMUKOKORIWARRI R.WARRI ASSAUGADAEGBEMA W.OGUTAEGBEMARAPELEEGWA E.AJUJURATANEGWA W.FORC. YORKIODIDI ESCRAVOSBEACHJONES CR.UBEFANSAGHARAOTUMARAFORCADOS TERMINALForcados platformAFREMOOPUAMASAPELEOBENWESTERN DIVISION EASTERN DIVISION0250Km NOVHORAMUKPEKEY TERMINALSCITIES OIL PIPELINES OIL FIELDS/flare sites 4.89-4.974.98-5.055.06-5.15Fig.2Spatial distribution of acid rain in Niger DeltaThe mean pH values of rainwater samples collected for the 10-year period (1997–2006)were generally lower than the WHO (1993)threshold of 6.5for potable water and 5.6for normal rainwater.The pH values range from 4.98to 5.15with 5.07mean values (Table 2),Table 1Standards and methods of analysisTest parameter Units Standard test method Description of methods pH pH ASTM D1293B pH meter Temperature °C Thermometer Turbidity NTU APHA 214A Turbidity meter TSS mg/l Gravimetric Gravimetric TDS mg/l APHA 2080TDS meter Conductivity l s/cm -1APHA 145Conductivity meter DO mg/l APHA4500C Iodometric Cl 2mg/l Titration Titration Nitrate (NO 3-)mg/l APHA 419C Diazotization Sulphate (SO 42-)mg/l APHA 427C Colorimetric Ca 2?mg/l ASTM93-77AAS K?mg/l ASTM D93-77AAS Na ?mg/l ASTM D93-77AAS Pb 2?mg/l ASTM D3559FAAS Cd2?mg/l ASTM D511AAS Fe2?mg/l ASTM D106C FAAS Mg2?mg/lASTM D 511AASTable 2Statistical summary of physicochemical characteristics of rainwater resources in the Niger Delta RegionSource FieldworkaSignificant difference exists with increasing distance(P \0.05),but no significant difference over the years (P [0.05)Parameters Mean ±range pH 5.06±4.98–5.15a H ?12.3±0.5–39.9Temperature (°C)27.4±26–28.2a Turbidity (NTU) 6.56±5.18–6.80a TSS (mg/l)408±400–415a TDS (mg/l)29.65±28.5–31.5a Conductivity (Scm -1)70.2±65.9–69.3a DO (mg/l) 5.7±5.44–5.70a Cl 2(mg/l)26.3±25–27.3a Nitrate (mg/l NO 3)13.5±10.5–16a Sulphate (mg/l SO 42-)30.7±28–34a Ca 2?11.4±0–28K ?7±2–18Na?13±1–35Pb 2?(mg/l)0.99±0.88–1.04a Cd 2?(mg/l)0.001±0.00–0.001a Fe 2?(mg/l)0.03±0.02–0.03a Mg 2?(mg/l)0.7±0.6–0.8aindicating the occurrence of acid rain in the oil-producing region of Nigeria.Acid rain was widespread over the entire region where rainwater samples were harvested for this study as illustrated by Fig.2,which shows the spatial distribution of acid rain in the Niger Delta.Low pH values of 4.89–4.97were observed in rains in number oil fields in both western and eastern regions.The mean rain pH was slightly lower in the eastern region but no significant difference was observed between the western (pH 5.14±0.25and eastern regions (pH 5.14±0.25).Acid rain in the region varies with distance from gas flare sites,with lowest pH at sites closest to the gas flares (Table 3;Fig.3).The occurrence of acid rain is not limited to the communities where gas is flared,but it is spread to other non-gas flared communities in the region where pH values of 5.15to 5.30were generally observed (see Fig.2).For instance,a pH of 5.15,5.18,5.27,5.29and 5.30was observed in rains from Patani,Benin–city,Ibagba,Abraka and Agbor in western Niger Delta areas,and rain pH values of 5.1,5.16,5.28and 5.29were observed at Nkarahia,Calabar,Uyo and Umuahia in the eastern Niger Delta.The acidic concentration in rainwater harvested varied with the duration of rainfall.Higher acidic concentrations were generally recorded in the first 5min of rainfall and lowest at the end of the rain (see Table 4;Fig 4).This increase in rain pH throughout a rain event has been reported previously in rains in Bangkok,Thailand and in Warri and rural areas of the Delta State Nigeria (Somboon 1997;Efe 2005,2006).This decrease in acidity is attributed to acidic species being washed out of the atmosphere during rain events.Table 3Variation of mean pH in rainwater with distance from gas flare over the years Distance 1997199819992000200120022003200420052006Mean Range 500m 5.05 5.00 5.01 5.09 4.99 4.98 4.89 4.99 5.00 5.03 5.010.204km 5.09 5.12 5.08 5.10 5.01 4.99 4.98 5.00 5.08 5.07 5.050.148km 5.11 5.14 5.09 5.18 5.03 5.03 5.00 5.02 5.08 5.05 5.080.1812km 5.12 5.15 5.09 5.19 5.03 5.03 5.08 5.03 5.08 5.08 5.090.16Mean5.105.105.065.145.025.014.995.015.065.075.050.17Source Fieldwork4k 8k 12k 12k mDistancesSulphate NitrateThe low pH values in rainwater during this period correlated significantly with SO 42-and NO 3-(r =0.86and 0.51,respectively),with sites where the rain pH was lowest (for example Egwa,Sapele,Kokori,Uzere,Adibawe,Ahia,Soku,Bonny,Afam,Ogula)having the highest SO 42-and NO 3-concentration.Figure 4illustrates that in addition to an increase in pH,sulphate and nitrate rain concentrations increase with increasing distance from gas flare sites.The high concentration of SO 42-and NO 3-reflected in rainfall acidity has been linked to emission of SO 2and NO 2gases that subsequently dissolve in rainwater (Efe 2005;Olobaniyi and Efe 2007).The natural gas flared in the region at an average rate of 42.5million m 3day -1is rich in oxides of sulphur and nitrogen is likely to be a source of such species (Olobaniyi and Efe 2007).Cluster analysis revealed that study sites close to gas flaring had contributed 94%to acidity recorded in the region.Most of the sites had coefficient [11.45,which is significant at P [0.05.The concentrations of SO 42-,Ca 2?,Cl -and NO 3-ions correlatedTable 4Temporal variation in pH and estimated gas flares rate (BCM)Years 5min 10min 15min 20min [20min Mean Gas flare rates (a BCM)1997 4.89 4.9 4.98 5.06 5.12 4.9929.411998 4.995 5.05 5.16 5.2 5.0826.181999 4.89 4.93 5.06 5.12 5.11 5.02224.612000 4.92 4.985 5.03 5.17 5.0226.762001 4.89 4.935 5.08 5.11 5.00227.012002 4.9 4.99 5.06 5.14 5.19 5.05621.052003 4.9 4.98 5.08 5.1 5.16 5.04424.262004 4.93 4.99 5.03 5.12 5.17 5.04822.92005 4.95 5.06 5.1 5.18 5.04821.562006 4.98 5.03 5.1 5.16 5.19 5.09218.94Mean 4.919 4.973 5.042 5.107 5.16 5.040224.27Min 4.99 5.03 5.1 5.16 5.2Maxa4.894.94.985.035.11Source Authors’Fieldwork and Estimated gas flares (National geophysical data center (NGDC)NOAA Satellite and Information Service 2009)aThe lower the pH,the higher the acidity;BCM ,billion cubicmeterssignificantly to moderately(r=0.86,0.72,0.58and0.51,respectively)with low pH values in the sites that are close toflare sites and had combined cluster[10.34in the region.However,while a significant relationship exists between SO42-,Ca2?and Cl-(r=0.78),poor correlation exists between H?and SO42-(r=0.12).The high rela-tionship among SO42-,Ca2?,K?and Cl-,NO3-suggest an excess acidic anion,and the poor relationship between SO42-and H?shows that the inorganic acid anion present in rain water was not only associated with free acidity.This is consistent with a previous study of rain in Warri region,which found SO42-and NO3-contributed74and26%, respectively,to free acidity when they were at their highest(Ogunkoya and Efi2003).The lowest pH in rain was recorded in2000,when sulphate and nitrate concentrations were also at their highest with mean values of pH values of4.90,SO42-28.9mg/l and NO3-10.3mg/l,respectively(see Fig.5).Throughout the study,pH values span4.93in2006to 5.20in1998.Sulphate rain concentration ranged from30mg/l in2007to31.5mg/l in 2005and NO3-ranged from10.7mg/l in1997to16.9mg/l in2005(see Fig.5).These variation in the pH,sulphate and nitrate concentration of rainwater are not significant (P[0.05)over the years of study.On the other hand,paired t test analysis shows a significant difference in pH with increasing distances from gasflare sites(P\0.05).The most acidic rain was collected in the region in1997(see Table4;Fig.7,this coincided with a reported increase in gas flaring from18.94BCM in2006to29.41BCM in1997(see Figs.6,7).Thefluctuating pattern of acid rain in the region is a reflection of thefluctuating gasflaring rate,the higher theflaring rates the more the occurrence of acid in the region(See Table4).Rain in the non-oil producing region was less acidic than those in the oil-producing belts of Nigeria, but still showed some acidity.Gas released throughflaring into the atmosphere can be carried several thousand of kilometre,degrading the atmospheric environment over vast areas(Somboon1997;Efe2005,2006)Thus,this mildly acid rain observed in the non-oil-producing area could be attributed to the influence of gasflaring.The seasonal variation of pH showed that December generally had the highest acid concentration in rainwater(4.7mean pH value),while July had lowest acidity(5.3mean pH value),indicating lowest acid concentration over the months.It was generally observed that the dryer months of December,January and February had more acidic rain(pH4.7to4.8)than the wetter months (May–September)(pH5.2–5.3)(see Fig.7).An improvement in water quality during the wet season has also been reported in a previous study of the region (Efe 2006).Rainwater in the region is colourless and tasteless but often shows high levels of turbidity and total suspended solids (TSS).For instance,turbidity values ranges from 5.18to 5.80NTU with a mean of 6.56NTU which is [5NTU threshold of WHO (1993),while TSS span 400–415mg/l with a mean of 408mg/l which is far beyond [5mg/l maximum acceptable of WHO (1993)limit for potable water.Conductivity and total dissolved solids (TDS)and temperature were generally low,lower than WHO thresholds during the period of observation.These physical parameters showed significant variation (P [0.05)with distance and no significant difference (P \0.05)over the years.The concentrations of anions (NO 3-,SO 42-and Cl -)and metals (Pb,Cd,Mg and Fe)investigated in the rain also changed significantly with distance (P [0.05)from gas flaring site but not from year to year (P \0.05).It should be noted that NO 3was generally higher than the 10mg/l WHO (1993)thresholds;this could be partly responsible for the occurrence of acid rain in the entire region.Lead concentrations were higher than WHO drinking water guidelines (0.01mg 1-1)in the rain samples (0.88–1.04mg 1-l).Elevated Pb concentrations in rain from this region has been observed in a number of studies (Ogunkoya and Efi2003;Efe 2005,2006;Olobaniyi et al.2007;Olobaniyi and Efe 2007).Increased Pb concentrations have also been reported in groundwater and soil of the Niger Delta region (Olobaniyi and Efe 2007;4.44.64.855.25.45.6JFMAMJJASONDp HMonthsFig.7Seasonal variation in acid rainOrigho2009).The increased Pb may be linked to an increase in the rate of gas faring and high level of pollution from anthropogenic activities in the region(Efe2005,2006).5Environmental implications of acid rain in Niger Delta RegionThis study has revealed that there is widespread occurrence of acid rain in the oil-pro-ducing region of Nigeria.This varied significantly in space and has strong environmental implications on terrestrial aquatic lives as well as the soil components.It was observed and gathered from the inhabitants during the time of data generation that acid rain in the area has precipitated the following:At the leaf surface,chlorosis and yellowing of leaves,wilting of the leaf tips,abscission of leaves and accelerated senescence was observed and,over the past13years,more than 40%of tree and other plant species have been lost.These effects were most pronounced closest to the gasflaring sites where rain pH was lowest(pH3.39)in most of theflares sites.Deleterious effects of acid rain on plants have been reported previously(Jacobson 1984;Neufeld et al.1985).Acid also damages roots and stems in addition to the leaves of plant.Such damage to plants is also an indirect threat to the microorganisms which decompose them,and subsequently the rest of the ecosystem.Jeffrey et al.(1981)found application of simulated sulphuric acid to a number of crops resulted in decreased yield and growth and foliar injury.A decrease in the growth and yield of crops like cassava,sweet potatoes,maize,melon plantain,rubber among others has also been reported in the area potentially due to such effects from acid rain.This has invariably affected the socio economic life of the inhabitants of the oil-producing communities in these agrarian communities.Acid rain has also affected soils by removal of essential nutrients leading to soil infertility in the region.The quality of other sources of water in the area is also affected by acid rain as most of the rivers and streams are acidified and as a result contain high concentrations of anions and cations(Okecha2000;Ogunkoya and Efi2003;Olobaniyi and Efe2007).According the inhabitants acidification in the region has also led to productive failure in aquatic life. The eggs of somefish species such as goldfish,salamonide,roach and tilapia have reportedly been killed by high acidity.In addition,amphibians that spawn in streams in the early wet season have been unable to reproduce.Similarly,reduced Ca and increased Cd and Pb concentration in surface water as a result of acidification,result in deformed bone structures and poor growth infish(Olobaniyi and Efe2007;Efe and Mogborukor2008). Consequently,birds such as loons and osprey that predominate in the area and feed onfish are no longer found.The cornea and mucous layer of the respiratory tracts are very sensitive to acid rain. Rates of acidosis,irritation of eye,conjunctivitis,bronchitis and prolonged coughing and lung disease have been found around the gasflare sites are higher than in non-oil-producing regions of Nigeria(Asonye and Bello2004;Efe and Mogborukor2008).Health problems have been linked to exposure to airborne acidity previously(Lippmann1985) and Keratoconjunctivitis has been reported in a previous study among children in oil-producing industrial areas of Delta State,Nigeria where it was attributed to pollution in the area(Asonye and Bello2004).The high level of toxic heavy metals in fresh waters can also impact human health via consumption of birds andfish contaminated by exposure to these polluted waters.Buildings and structures in the area according to the residents have been decoloured and disfigured.Most landlords in the region asserted that they have to carry out routinerepainting of their houses every2years because of decolouration by acid rain.Similarly, because of corrosion of their roofs most buildings in most of the area suffer leakages. Recent surveys found over40%of houses in the region(especially those at the foci of the flare sites)were leaking and roof repairs or replacement was carried out every3years (Alakpodia2000;Efe2005),however,in the non-oil-producing region such repairs were required much less frequently.In addition most car owners in the region reported that their cars were regularly decoloured that they had to carry out re-spraying once every three to 4years.The bottom plate and body of the car were also affected by corrosion,leading to rust age,requiring annual body work on the car.Based on these environmental consequences,there is the need for legislation to put an immediate end to gasflaring;alternatively it should be converted to industrial raw material for the production of domestic gases.There should be reduction in emission of acid gases. Acidified well,rivers and other water bodies should be treated with lime to restore the pH to a level at whichfish and other organism can survive and rainwater harvested for domestic uses should be purified.All environmental laws for the protection of the envi-ronment should be implemented,mass education for the inhabitants of the area;should be available and periodic environmental impact assessment of the region by both the oil company and the federal government of Nigeria should be carried out.The gasflaring operators should plough back part of their profits for the provision of social infrastructures in the region and employment should be given to the inhabitants of the host communities that have the requisites qualifications.6ConclusionThe study has revealed that there is the occurrence of acid rain in the oil-producing region of Nigeria,which is not limited to the foci of gasflaring communities alone but it is widespread in the region.This is evident in5.06mean pH recorded in the region.Lower pH values of3.97–4.98were reported in area that are close to the gasflare sites.Over the years,acid rain in the region showed afluctuating pattern,reflecting variation in the gas flaring rate,with more acidic rain at higher gasflaring rates.Rain in the non-oil-producing region was less acidic than the oil-producing belts of Nigeria.Physicochemical charac-teristics of rain water resources were within WHO guidelines for drinking water,with the exception of turbidity,pH,TSS,NO3and Pb.However,these physicochemical parameters (pH,SO42-,NO3and Pb etc.)varied significantly in rainwater with distance from the gas flare sites(P[0.05),but showed no significant difference from year to years(P\0.05). The occurrence of acid rain in the region has far reaching environmental implications on the soil,vegetation and crops,aquatic life,water resources.It is therefore recommended that there should be an immediate extinction of gasflaring in the region,and there should be strict adherence to all environmental laws in the country by the oil companies operating the region.ReferencesAkporido SO,Emuobonoviel IJ,Akporideo CE(2000)A study of the quality characteristics of surface and underground water in Sapele and Ogharefe oil producing areas of Delta State.Niger J Sci Environ 2:75–86123。