Literature DB >> 29896496

Geochemical behavior of fluoride-rich groundwater in Markapur, Andhra Pradesh, South India.

Venkatayogi Sudarshan1, Adimalla Narsimha2,3, S V G Das4.   

Abstract

Excess fluoride in drinking water has been one of the leading problem faced by the arid and semi-arid regions of the world. Significantly in India the people suffer from fluorosis comparing to other toxic elements like Arsenic etc., in drinking water. Approximately, in India the excessive fluoride in groundwater is noticed in 177 districts covering 21 states, affecting 66 million people, including 6 million children and Moreover, the latest estimation gives nearly 200 million people, from among 25 nations the world over, are affected by the deadly disease of fluorosis [1], [2], [3], [4], [5], [6], [7], [8], [9], [10], [11], [12], [13], [14]. The fluoride of the groundwater varies from 0.4 to 5.8 mg/L with a mean of 1.98 mg/L (Table 1 & 2), which indicates that the concentration of fluoride is not uniform in the study area. In general intake of small quantities of fluoride in the permissible limit of 0.5 to 1 mg/L is known to be beneficial for human health in production and maintenance of proper health. However, in India safe limit of fluoride in potable water is considered to be between 0.6 to 1.2 mg/L, less than 0.6 mg/L can cause dental caries, while higher than 1.2 mg/L leads to fluorosis [1], [2], [3], [4], [5], [6], [7], [8], [9], [10], [11], [12], [13], [14], [15], [16].

Entities:  

Year:  2018        PMID: 29896496      PMCID: PMC5996165          DOI: 10.1016/j.dib.2018.02.084

Source DB:  PubMed          Journal:  Data Brief        ISSN: 2352-3409


Specifications table Value of the data Primarily, this data will be a guide line for the Markapur region people and scientists, hydro-geologists who works on this topic and a basic information for groundwater management studies. Most of the area population depends on groundwater for their daily needs, without any primary treatment and actually they do not know much about the quality of groundwater, but the nature of consequence of fluorosis is in their lifetime, it is because there no cure for it and taking safety measure of drinking water is always preferable. Based on this data the people who live on the current region are advised to not to drink groundwater directly for drinking purposes, if who does this constantly for a period of time will surely meet with deadly diseases of fluorosis. This data will be very useful to develop effective strategies for improving Markapur region water supply and provide scientific evidence for decision and management of the groundwater.

Data

The Markapur provinces is located in central-western part of the Prakasam district (Fig. 1). The area geographically lies between the 79° 10′–79° 22′ south latitudes and 15° 35′–15° 50′ east longitudes (Fig. 1). The vast plains of Markapur and of the adjacent areas are occupied by phyllite/slate. The study area has a hot climate and classified as semi-arid with steppe type of vegetation. However, May is generally the hottest month with 45 °C with a mean minimum temperature of 27 °C, humid weather is experienced during July-November. Winds are generally light to moderate, except during the late summer and early southwest monsoon season. The average annual rainfall of the Prakasam is 798.6 mm, monthly rainfall ranges from nil in March to 182.9 mm in October. October is the wettest month of the year.
Fig. 1

Location map of the Groundwater samples in Markapur region, Prakasam district, Andhra Pradesh, South India.

Location map of the Groundwater samples in Markapur region, Prakasam district, Andhra Pradesh, South India. Groundwater quality of Markapur, Andhra Pradesh, was studied and assessed the fluoride contaminants in groundwater. The fluoride concentrations varies from 0.4 to 5.8 mg/L and it is clear that the level of fluoride is higher in 54 groundwater locations than that of recommended upper limit by WHO (Table 1, Table 2). It is clear from the map that except for extreme north and south parts of the study area, all other areas have excess fluoride (Fig. 3). West-central part is having groundwater with highest fluoride concentration and cross plots are shown in Fig. 2. However, fluoride can gain entry into human body through different routes, probable transmission routes and its health effects are shown in Fig. 4; Table 3.
Table 1

Hydrochemical data from the Markapur, Prakasam district, Andhra Pradesh, South India.

Sample NopHECTDS
TH
Ca2+
Mg2+
Na+
K+
CO32−
HCO3
Cl
SO42−
F
NO3
µS/cmmg/L
PDM-18.072000128040012028024549Nil430335704.130
PDM-28.25180011204001202802153Nil3103051303.715
PDM-38.05370022508803605204324Nil3808801551.2564
PDM-48.11520940340802601852Nil385200661.323
PDM-58.07305018704008032049027Nil5455401203.6110
PDM-68.112600160062016046024588Nil3804251402.5180
PDM-78.2811607153201202001153Nil280142720.870
PDM-88.439305951808010012233033065401.353
PDM-98.181052518080100991Nil29042213.835
PDM-108.44200012504601203402404303103251803.255
PDM-118.3214108603201202001601615365160473.867
PDM-128.7114909251204080280355430165654.412
PDM-138.65147091016025135260455420165603.611
PDM-148.71700105018080100300460480180854.817
PDM-158.7413508401204080245160400140523.411
PDM-168.2519501200200401603504605102351103.615
PDM-178.52312307608010702401Nil390120405.810
PDM-188.551660102020040160285340490185701.4515
PDM-198.7143090016040120255370420155653.615
PDM-208.71810112020080120305560470220751.4520
PDM-218.5715009351208040275340440170355.215
PDM-228.71650102016080802954603302501151.7528
PDM-238.731700960200401602853603802201061.9529
PDM-247.814400264080032048054515Nil4909403001.3594
PDM-258.5223001420320802403702403004401850.731
PDM-268.671620100020040160270150320255741.2540
PDM-278.2618001120240801603001Nil360284901.442
PDM-288.24200250068016052055015Nil3709402851.1597
PDM-298.617401080200601403002403202901101.2526
PDM-308.67125078020050150190260330155621.89
PDM-318.75165099024080160265140365250751.4540
PDM-328.6718001120240402002903603202951221.426
PDM-338.6149092024080160225255410170701.430
PDM-348.531600100014040100290340380215873.68
PDM-358.62148093024440204245230460155443.320
PDM-368.691300820160808021034046071513.637
PDM-378.619101200280802003053404003101091.49
PDM-388.4103065032016016069181533064421.358
PDM-398.621130720160808018223037071393.770
PDM-408.5610400220801403543523035130.814
PDM-418.55122077020040160184325380130353.6518
PDM-428.56870560260801807422526560421.5536
PDM-438.4313008202008012019312052053201.6352
PDM-448.5385055024080160800.54031057161.9515
PDM-458.23830510240120120762Nil34042121.4516
PDM-467.9512307702801401401501Nil215255360.85
PDM-477.181590100036012024017532Nil360260551.456
PDM-488.15700450240120120462Nil2753281.155
PDM-498.3860560220401809071035043101.2522
PDM-508.5900580140401001366303704363.6513
PDM-518.32890580260602001201353653591.4521
PDM-528.5287056024080160837303504361.124
PDM-538.2810606802406018012414Nil41064133.320
PDM-548.2310206502704023010211Nil36078201.422
PDM-558.25870565240601807619Nil3603661.522
Sample NopHECTDSTHCa2+Mg2+Na+K+CO32−HCO3ClSO42−FNO3
PDM-568.51860560270402306793032057100.8526
PDM-578.42870560240601807720303405091.118
PDM-588.41840520220601607712203104381.219
PDM-598.328905802004016010851533057141.816
PDM-608.32760500170401309261029050101.2522
PDM-618.57760470200401608014026078100.8515
PDM-628.54520330160601004713019028171.253
PDM-638.2655034020060140301Nil21025120.422
PDM-648.3389029014080603531516028170.516
PDM-658.1956036016012040531Nil21035131.311
PDM-668.3984051016040120115253006018220
PDM-678.5660430160601007814021050151.422
PDM-688.05930600180401401291Nil3954341.6339
PDM-698.041340845240402001203Nil460135121.454
PDM-708.4690058022040180902420260115131.114
PDM-718.07102066026080180853Nil310120131.0522
PDM-728.3274048024040200508102207890.812
PDM-738.232900178050016034038054Nil3804802301.3525
PDM-748.73100190044012032041511504605101901.63125
PDM-758.23270016204401602803404Nil4203352353.2138
PDM-768.15205012503601602003002Nil4502452002.554
PDM-778.3165010202801201602453104201651552.2518
PDM-788.34235014303601202403254204203051852.19
PDM-798.44710460180801007533025050260.9520
PDM-808.35205012503201202002804202803002151.96
PDM-818.372250137036012024030213202603552101.4519
PDM-828.0426501640240801604855Nil4405001451.4576
PDM-838.52040128016040120390340525285811.8520
PDM-848.632020125016060100390340600230782.259
PDM-858.351880118024040200320415500255651.8524
PDM-868.2116801050240601802677Nil440230651.3510
PDM-878.3226301600200401605052106803401302.8510
PDM-888.224301500200401605573Nil6003301304.212
PDM-898.48153095026080180225920320255681.529
PDM-908.46128079520080120195630380142341.4521
PDM-918.0315509704208034023710Nil390220621.0520
PDM-928.311160730200601401661210360130321.19
PDM-937.813408402006014011812Nil415140471.056
PDM-948.62450152012040808052405303901183.95
PDM-959.3210206551608080150310280130291.520
PDM-968.246604301608080753Nil24043141.8515
PDM-978.34100064020080120130315260142211.214
PDM-988.151450900280802001955Nil260210801.318
PDM-998.071080700240801601325Nil350114172.2564
PDM-1008.06163010203601602002035Nil180340941.518
PDM-1018.5183054020080120953303007210467
PDM-1028.44111070020080120155620350106251.58
PDM-1038181011204802002801785Nil130425951.985
PDM-1048.281060660240801601277Nil280135320.964
PDM-1058.2510606802401201201244Nil330115211.128
PDM-1068.15950610200801201204Nil245130250.8519
PDM-1078.46126078524080160173730380128400.9520
PDM-1088.271180745200801201754Nil280155522.436
PDM-1097.751840114040024016022027Nil360255940.942
PDM-1108.551230760320160160130640360156260.9124
PDM-1117.86162010203301302002207Nil410200851.2510
PDM-1128.1515809803201202002055Nil190341920.961
Sample NopHECTDSTHCa2+Mg2+Na+K+CO32−HCO3ClSO42−FNO3
PDM-1138.32880570200801201065528085232.524
PDM-1148.19143088028012016018415Nil210240821.212
PDM-1158.47920560120804015013034043201.4588
PDM-1168.5610206601206060170403855018227
PDM-1178.5410506701604012016314039057202.1540
PDM-118810907002401001401343Nil38085253.633
PDM-1198.4172045022080140582203002841.4531
PDM-1208.22780500260100160552Nil3203551.29
PDM-1218.59125078020040160184134045085252.820
PDM-1228.31470920200401602426102502151301.632
PDM-1238.21960620265120145925Nil1151411441.4555

PDM-Indicates: Prakasam District Markapur Region.

Table 2

Groundwater samples of the Markapur, Prakasam district, Andhra Pradesh, South India exceeding the permissible limits prescribed by WHO (2004) and ISI (1993) for drinking purpose.

Water quality parametersIndian Standard (ISI 10500, 1993)
WHO International Standards (2004)
Range in the Markapur region
Highest desirableMax. permissibleMost desirable limitMax. allowable limit
pH6.5–8.56.5–9.56.58.57.18–9.32
EC1400520–4400
TDS50020005001500290–2640
TH30060010050080–880
CO32−5–70
HCO3115–680
Cl250100020060025–940
NO345453–180
F0.61.20.51.50.4–5.8
Ca2+752007520010–360
Mg2+301005015040–520
K+120.5–88
Na+20020030–805
Fig. 3

Shaded contour map of F− (mg/L) for the Markapur region, Andhra Pradesh.

Fig. 2

Cross plots (a) TDS vs Cl−, (b) TDS vs NO3−, (c) Cl− vs NO3−, (d) TDS vs Na+, and (e) TDS vs F− (TDS, Cl−, NO3−, Na+, F− are expressed in mg/L).

Fig. 4

Probable transmission routes of fluoride ingestion.

Table 3

Effects of fluoride ingestion on human health (Adimalla and Venkatayogi, 2017).

Fluoride concentration (mg/L)Effect on human health
<0.5Conducive to dental caries
0.5 to 1.5Promotes development of strong bones and teeth
1.5 to 4.0Promotes dental fluorosis in children
>4.0Promotes dental and skeletal fluorosis
>10Crippling skeletal fluorosis, possibly cancer
Cross plots (a) TDS vs Cl−, (b) TDS vs NO3−, (c) Cl− vs NO3−, (d) TDS vs Na+, and (e) TDS vs F− (TDS, Cl−, NO3−, Na+, F− are expressed in mg/L). Shaded contour map of F− (mg/L) for the Markapur region, Andhra Pradesh. Probable transmission routes of fluoride ingestion. Hydrochemical data from the Markapur, Prakasam district, Andhra Pradesh, South India. PDM-Indicates: Prakasam District Markapur Region. Groundwater samples of the Markapur, Prakasam district, Andhra Pradesh, South India exceeding the permissible limits prescribed by WHO (2004) and ISI (1993) for drinking purpose. Effects of fluoride ingestion on human health (Adimalla and Venkatayogi, 2017).

Experimental design, materials, and methods

123 groundwater samples have been collected from bore wells/tube wells in the study area. The bottles were soaking in 1:1 HCl for 24 h and rinsed with distilled water followed by deionized water and samples were collected after pumping out water for about 10 min to remove stagnant water from the well and then transferred and stored at 10 °C. All collected groundwater samples were separately labeled with sample ID starting from PDM-1 to PDM-123, and were transferred to the laboratory and analyzed in the laboratory for analysis of major anionic and cationic constituents using standard methods APHA (1995). The pH, electrical conductivity (EC), total dissolved solids (TDS), were analyzed on the site using pH/EC/TDS meter (Hanna HI 9811-5). Total hardness (TH) was measured by titration method using standard hydrochloric acid and standard EDTA solution. Calcium (Ca2+) and magnesium (Mg) were determined titrimetrically using standard EDTA. Sodium (Na) and potassium (K) concentrations were determined using Flame photometer (Systronics, 130). Chloride (Cl) was determined by standard AgNO titration. Bicarbonate (HCO3−) and carbonate (CO32−) by titration with HCl. Sulphate (SO42−) and Nitrate (NO3−) were determined by using UV-visible spectrophotometer (Spectronic, 21, BAUSCH and LOMB). The fluoride concentration in water was determined electrochemically, using thermo Scientific Orion Star A214 Benchtop pH/ISE meter (9609BNWP fluoride ion-selective electrode) using the USEP ion selective electrode method. This method is applicable to the measurement of fluoride in drinking water in the concentration range of 0.1–1000 mg/L. Standard fluoride solutions (0.1–10 mg/L) were prepared from a stock solution (100 mg/L) of sodium fluoride. As per experimental requirement, 2 ml of total ionic strength adjusting buffer grade III (TISAB III) was added in 20 ml of water sample. The ion meter was calibrated for a slope of −59.2 ± 2. The composition of TISAB solution was as follows: 58 g NaCl, 4 g of CDTA (Cyclohexylene diamine tetraacetic acid) and 57 ml of glacial acetic acid per litre. Eventually, the accuracy of all chemical analyses was verified by calculating ion-charge balance between cations (Ca2+, Mg2+, Na+ and K+) and anions (HCO3−, Cl−,SO42−, NO3− and F−) as (cations - anions)/(cations+anions)X100, all 123 groundwater samples were less than the accepted limit of ±10% and samples.
Subject areaEarth Science
More specific subject areaHydro-geochemistry
Type of dataTable, figure
How data was acquiredThe fluoride concentration in water was determined electrochemically, using thermo Scientific Orion Star A214 Benchtop pH/ISE meter (9609BNWP fluoride ion-selective electrode) using the USEP ion selective electrode method [15]. This method is applicable to the measurement of fluoride in drinking water in the concentration range of 0.1–1000 mg/L. Standard fluoride solutions (0.1–10 mg/L) were prepared from a stock solution (100 mg/L) of sodium fluoride. As per experimental requirement, 2 ml of total ionic strength adjusting buffer grade III (TISAB III) was added in 20 ml of water sample. The ion meter was calibrated for a slope of −59.2±2. The composition of TISAB solution was as follows: 58 g NaCl, 4 g of CDTA (Cyclohexylene diamine tetraacetic acid) and 57 ml of glacial acetic acid per litre. Using pH/EC/TDS meter (Hanna HI 9811-5), the EC, pH and TDS of water samples were measured. Calcium, magnesium, chloride, carbonate and bicarbonate were analyzed by a titration methods. Sodium and potassium concentrations were determined using a flame photometer (Systronics, 130). Sulphate and nitrate were determined using a UV-visible spectrophotometer (Spectronic, 21, BAUSCH and LOMB).
Data formatAnalyzed
Experimental factorsThe bottles were soaking in 1:1 HCl for 24 h and rinsed with distilled water followed by deionized water and samples were collected after pumping out water for about 10 min to remove stagnant water from the well and then transferred and stored at 10 °C.
Experimental featuresDetermine the content levels of fluoride and other Physiochemical parameters using standard procedure.
Data source locationMarkapur, Andhra Pradesh, South India
Data accessibilityData is with this article
  4 in total

1.  Drinking water pollution with respective of fluoride in the semi-arid region of Basara, Nirmal district, Telangana State, India.

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2.  Data on fluoride concentration levels in semi-arid region of Medak, Telangana, South India.

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3.  Hydrogeochemical data on groundwater quality with special emphasis on fluoride enrichment in Munneru river basin (MRB), Telangana State, South India.

Authors:  Adimalla Narsimha; S Venkatayogi; S Geeta
Journal:  Data Brief       Date:  2018-01-31

4.  Elevated fluoride concentration levels in rural villages of Siddipet, Telangana State, South India.

Authors:  Adimalla Narsimha
Journal:  Data Brief       Date:  2017-12-06
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