Introduction

Water the most important resource of nature is increasingly becoming a scare resource. Rivers are playing an important role as major water resource. Unfortunately, rivers are being polluted by indiscriminate disposal of sewage and industrial waste, which affects its physico-chemical properties and microbiological quality (Koshy and Nayar 1999). In the recent past, expanding human population, industrialisation, intensive agricultural practices and discharge of massive amount of wastewater into the river have resulted in deterioration in water quality. Water is playing an important role in the transmission of human disease. Faecal matter in water contains human enteric bacteria and therefore faecal contamination is one of the most important criteria for water quality assessment (Scott et al. 2003). Coliforms are the major microbial indicator of water quality monitoring. Therefore, bacteriological assessment, particularly for total coliforms or faecal coliforms, is routinely carried out to ascertain the quality and potability of water. The determination of total coliform and total faecal coliform count is the most widely used bacteriological methods for assessment of the quality of drinking water. The presence of such bacteria can be taken as an indicator of faecal contamination of the water and thus, to determine why such contamination is present, how serious it is and what steps can be taken to eliminate is important.

The World Health Organisation (1996) provided guidelines for drinking water quality and recommended that no faecal coliform should be found in drinking water. Presence of faecal coliforms as E. coli serves as an indicator for the possible presence of other disease causing pathogens. Faecal coliforms are selected members of the coliform group of bacteria which are able to ferment lactose at 37 °C and fairly specific for the faeces of warm blooded animals. The bacteriological parameters of different river systems have been studied by various groups (Badra et al. 2003; Arvanitidou et al. 2005). The bacteriological examination of water has a special significance in pollution studies, as it is a direct measurement of deleterious effect of pollution on human health. The present study focuses on the culturable bacterial diversity of the Barak River system for its pollution status. This study assesses seasonal water quality of Barak River water with the uses of bacteriological variables.

Materials and methods

Study area

The Barak River is one of the major river system in north-east India. It is located in the southern part of Assam, India. Geographically the site is situated at longitude of 24°41″ 29.9″N and latitude at 92°45″ 25.9″E with an altitude of about 36 m above mean sea level. The Barak River originates from the Nagaland–Manipur states of India passes through Assam and merges with Brahmaputra in Bangladesh before emerging into the Bay of Bengal. The main tributaries of the Barak River in India are the Jiri, the Dhaleswari, the Singla, the Longai, the Madhura, the Sonai, the Rukni and the Katakhal.

Weather condition

Generally, the daily temperature in the Barak Valley is about 15 °C in January. From April it rises and in July, the mean temperature ranges from 25 to 27 °C. During October, the daily mean temperature is above 25 °C. The subtropical climate of this valley is characterised by high rainfall and high humidity and can be characterised by three dominant seasons viz; winter (November–February), summer (March–May) and monsoon (June–October).

Sampling sites and sampling methods

Water samples were collected from four different sites of the Barak River, viz; (a) Panchgram (near Hindustan Paper Corporation). (b) Katakhal (upstream)—tributary merging with Barak River. (c) Annapurnaghat (upstream)—municipal waste water mixing point. (d) Sadarghat (upstream)—water intake point of PHE. Samples were collected during the winter, summer and monsoon seasons (2010–2011). One litre of water from each location was collected into pre-sterilised bottles. All samples were collected with precautions required for microbiological analysis and transmitted to the laboratory for microbial analysis.

Physico-chemical analysis

The water samples from different sites and seasons were analysed for pH, dissolved oxygen, alkalinity and FCO2. Dissolved oxygen was determined by modified Winkler’s azide method, pH by digital pH meter, alkalinity and FCO2 were measured by titrimetric method. All the physico-chemical parameters were analysed following the standard protocols of APHA (1998).

Bacteriological analysis

For the isolation and enumeration of bacteria, each water sample was serially diluted in sterile distilled water and plated on nutrient agar and different selective media. The bacterial populations in different samples were estimated by the spread plating method on different media using 1 ml of suitable dilutions. All media plates were incubated at 37 °C for 24–48 h and final counts of colonies were noted. The water quality was determined by the standard most probable number (MPN) method. Fermentation tubes were inoculated with 10, 1 and 0.1 ml aliquots of water sample (APHA 1998). The tubes were incubated at 37 °C for 24 h. Positive tubes producing acid and gas were used in estimating the presumptive MPN/100 ml. Confirmed test was carried out by transferring a loopful of broth from a positive tube into Brilliant green lactose bile (BGLB) broth, followed by incubation at 37 °C for 24–48 h. The tubes were observed for gas formation. Completed test was performed by plating a loopful of broth from a positive BGLB tube on to an Eosine Methylene Blue (EMB) Agar plate. The plates were incubated at 37 °C for 24–48 h and observed for dark red colonies with metallic green sheen. Final faecal coliform or E. coli count as MPN/100 ml was calculated based on the completed test. All the culture media were obtained from HiMedia Pvt. Ltd., Bombay, India (Table 1).

Table 1 Detail of specific culture media used for quantitative bacterial analysis

Statistical analysis

All experiments were performed in triplicates and two-way analysis of variance (ANOVA) was performed according to the standard method (Steel and Torrie 1992).

Results and discussion

The physico-chemical analysis carried out from different sites during different seasons has been presented in Table 2. The data show the average of three samples per season. Total alkalinity showed a rising trend during summer and winter season. In contrast, the values declined during monsoon season. Measurement of hydrogen ion concentration enables us to understand the chemical conditions prevalent in aquatic ecosystem. pH values, however, showed a narrow range of fluctuations over the seasons as well as among the study sites. In the site Panchgram higher values of dissolved oxygen (DO) were observed during the monsoon season which gradually declined attaining minimum during winter season. More or less similar trend was also observed in the other three sites. During the monsoon season, the free carbon dioxide (FCO2) value was found to be high whereas lower values of FCO2 were observed during the summer and winter seasons. Microbial analyses are presented in Table 3. All samples were found to have total viable counts (TVC) higher than those prescribed by Bureau of Indian Standards (ISI 1991). The TVC was higher in the monsoon season as compared to summer and winter. TVC for water samples were the highest during monsoon and the least during the winter season. In the Barak River the TVC was in the range of 22–42 (×103) ml−1, 12–34 (×103) ml−1 and 10–19 (×103) ml−1 during monsoon, summer and winter season, respectively. Total viable count was found highest in the site Panchgram. The overall TVC was higher during monsoon than other seasons. The total coliform (TC) count was also relatively higher in the monsoon season than summer and winter in all the sites. The total coliform was in the range of 13–49 (×103) ml−1, 11–42 (×103) ml−1 and 8–26 (×103) ml−1 during monsoon, summer and winter season, respectively. The range of SA/SH observed in the Barak River were 11–63 (×103) ml−1, 3–45 (×103) ml−1 and 5–49 (×103) ml−1 in monsoon, summer and winter, respectively. Pseudomonas spp. were recorded from all sites in all seasons, but were higher in monsoon in comparison to other seasons. The Pseudomonas spp. were in the range of 8–16 (×103) ml−1, 5–14 (×103) ml−1 and 3–11 (×103) ml−1 in monsoon, summer and winter, respectively. The faecal coliform group of bacteria has been the principal indicator of the suitability of water for domestic use. In the present study, the total faecal coliform count in the Barak River was in the range of 910–1,600 (MPN/100 ml), 210–350 (MPN/100 ml) and 110–280 (MPN/100 ml) in monsoon, summer and winter season, respectively. The highest value of MPN was found in the site Panchgram and Annapurnaghat (1,600 MPN/100 ml) during monsoon season and lowest in the site Katakhal (110 MPN/100 ml) during winter season.

Table 2 Physico-chemical analysis of the water samples from different sites and seasons
Table 3 Bacterial quantity analysis of the water samples from different sites and seasons

Populations of aquatic microbiota are influenced by many environmental parameters. High level of pollution indicator bacteria in river water is also a common problem in urban and rural areas that often leads to outbreaks of serious water-borne diseases like cholera, dysentery, etc. The bacteriological analysis revealed that the entire sample collected from four different sites of the Barak River was contaminated with coliform, faecal coliform and some other pathogenic bacteria. In the present study, all sites were found to possess high total viable counts. Hindustan Paper Corporation near Panchgram has direct connection with the river water of the Barak River and they are directly discharging the industrial effluents to the river. The TVC values suggest that they are discharging the industrial effluent to the river water. This practice should be avoided. The total viable count in the site Panchgram near Hindustan Paper Corporation was higher than other three sites which may be attributed to pollution by industrial wastes. The statistical analysis of different sites and seasons also showed significant variations (ANOVA, P < 0.05).The population of total faecal coliform (TFC) from all the sites showed more or less similar values but marked differences were observed in different seasons. Therefore, significant variations were noted between different seasons (ANOVA, P < 0.01). In the present study, the Panchgram site showed the highest population of TC followed by Annapurnaghat site during monsoon season. The high bacterial population at the Annapurnaghat site indicated mixing of some domestic wastes along with rain water in monsoon time. A similar pattern was obtained at the Sadarghat and Katakhal sites. Statistical analysis also showed significant variations between different sites and different seasons (ANOVA, P < 0.05 and 0.01). The TC count was relatively higher in monsoon and summer seasons than winter. Similar observations were made in the Gangetic River by Sood et al. (2008). The highest coliform bacterial population in the monsoon season in the present study is similar with the reports of earlier studies (Badge and Varma 1982; Badge and Rangari 1999). The highest population of SA/SH was observed in the Panchgram site during the monsoon season followed by Annapurnaghat and Sadarghat whereas population of SA/SH in the Katakhal site was almost negligible. Therefore, significant variation was noted between different sites (ANOVA, P < 0.01). But insignificant variations were observed between different seasons (ANOVA, P < 0.05 and 0.01). Sewage contamination of river water particularly in the Panchgram site is detected by enumerating the coliform groups of bacteria (Fujioka 2002). Panchgram site near the Hindustan Paper Corporation and Annapurnaghat showed relatively high level of total coliform, total viable count, SA/SH and Pseudomonas spp. High values of bacterial populations near the Panchgram site might be due to discharge of high volumes of pulp paper mill wastes. This result coincides with observations of the Gola River by Chandra et al. (2006). It is universally accepted that, higher sewage contamination would lead to increased number of coliform and faecal coliform in natural water bodies. Hansen and Bech (1996) clearly suggest the proliferation of allochthonous microflora in the river environment. Further, as inestimable pathogenic bacteria will constitute the microflora of effluents discharged from different activities, quantifying different groups of pathogenic bacteria have to be part of such surveys. For instance, information on occurrence, abundance and distribution of potent human pathogens, Vibrio cholera (causing cholera in humans), Vibrio parahaemolyticus (gastroenteritis), Salmonella and Shigella sp. (typhoid fever, food poisoning), Streptococcus sp.(meningitis and skin infections) and Pseudomonas aeruginosa (pulmonary and lung infections) in aquatic environment may prove useful in public health management. The highest population of all the examined groups of bacteria was observed during the monsoon season. Kistemann et al. (2002) observed that in the case of rainfall, the microbial loads of running water may suddenly increase and reach reservoir bodies very quickly. Pathogenic bacteria which may cause serious problem for human health have been studied mostly for their survival in the aquatic ecosystem (Sood et al. 2008; Nagvenkar and Ramaiah 2009). The presence of Pseudomonas spp. in all the sites during all seasons may be attributed to human activities and sewage discharge to these sites.

The rising trend of total alkalinity during summer and winter seasons may be due to higher evaporation of water during low rainfall period which led to an increase in the concentration of carbonates and bicarbonates of calcium and magnesium. On the other hand, a decline in the alkalinity value from monsoon season was brought about by dilution due to heavy rainfall (Sahu 1991; Shinde et al. 2011). The pH values in all the sites were found to be high indicating the water bodies are not so acidic. Higher values of dissolved oxygen (DO) during the monsoon season may be due to heavy rainfall during this period led to increased aeration of river water (Sridhar et al. 2006; Adeyemo et al. 2008). Higher values of CO2 during monsoon season may be attributed to the heavy input of sewage and other organic and inorganic pollutants due to surface run off as a result of heavy showers during this period. These materials in course of time oxidised which led to their decomposition and consequent release of CO2 onto water, whereas lower values of CO2 were observed during the summer and winter seasons, which may be due to more transparency and more photosynthesis (Shinde et al. 2011). The effect of different seasons was statistically analysed within different physico-chemical parameters. The two-way ANOVA test revealed that there were significant variations noted (ANOVA, P < 0.05 and 0.01) among different physico-chemical parameters except pH. Irregular pattern of pH values over the seasons as well as among the study sites may be due to high mixing rate of river water. Similar results were also observed in Narmada River (Gupta et al. 2000).

In this study, most of the sites were not suitable for domestic purpose with respect to the maximum permissible limits of total coliform and total faecal coliform as per the standards of National River Conservation Directorate, India. McLellan et al. (2001) stated that faecal pollution indicator organisms can be used to determine the number of cases related to the impacts on human health as well as health of aquatic ecosystems. The presence of such indicator organisms may provide information regarding water-borne diseases and is a direct threat to human, animal and aquatic organisms. The study clearly revealed that, the water becomes unfit for drinking as well as domestic purposes because of contamination due to industrial and domestic wastes. The present study also clearly stated that there is a significant presence of bacterial pollution indicators and pathogenic bacterial groups. The situation of the Barak River is not very serious but very alarming.

Conclusions

The observations clearly indicate that, all the studied sites of the Barak River have been contaminated with water-borne pathogenic bacteria. This may be due to increased anthropogenic and socio-cultural activities at different sites of the Barak River. Occurrence of pathogenic bacterial genera in the Barak River suggests that they may be explored as indicator organisms. Overall bacteriological analysis of the Barak River water revealed that the river water was polluted by sewage, faecal contaminants and industrial wastes and the water of the Barak River is not suitable for drinking and other recreational purposes. Regular monitoring of microbial contamination in the water of Barak River should be an essential component for the protection strategy of the public health.