Abstract
The conceptual site model (CSM) has been designed for Inactive/abandoned mines in the SW part of Cuddapah basin, which gives an overview of Inactive/abandoned mine characterization in terms of physical impacts such as vertical openings, dangerous impoundments, location of steep slopes, waste processing facilities, steep portal abandoned barite mine and assessment of groundwater analytical data. To evaluate the groundwater quality and its suitability for domestic, drinking purposes, 44 groundwater samples were collected from the southwestern part of the Cuddapah basin, were examined for major cations and anions. The suitability of groundwater for drinking purposes is assessed by comparing with the World Health Organization (W.H.O) and Indian standards (IS).
Keywords: Conceptual site model (CSM), Groundwater quality, Inactive/ abandoned mines, Southwestern part of Cuddapah basin
Specifications Table
Subject area | Chemistry |
More specific subject area | Environmental Geochemistry |
Type of Data | Tables and figures |
How data was acquired | The conceptual site model (CSM) was designed for the identification of vertical openings, dangerous impoundments, location of steep slopes, waste processing facilities, and analysis of groundwater. 44 Groundwater samples were collected from bore wells in the southwestern part of Cuddapah basin, Y·S.R District, A.P; pH and EC, TDS (Conductivity cell CD-10) are determined with help of water analyzer 371 field kit respectively; Total Hardness, Ca2+, Mg2+, CO32−, HCO3− and Cl− were determined using titrimetry as laboratory followed standard methods (APHA 2012); F− is determined using ion-selective electrode (Orion 4 star ion meter, Model: pH/ISE). |
Data format | Raw, analyzed |
Parameters for data collection | All the parameters were analyzed according to standard procedures for the examination of groundwater [1] (Table 1) |
Description for data collection | Major cations, anions levels in drinking water were determined and compared with WHO and BIS drinking water standards [2] |
Data Source Location | Southwestern part of Cuddapah basin, A.P India (Fig. 1) |
Data accessibility | Data is available in the article. |
Value of the Data
|
1. Data description
1.1. Study area
The study area falls under the southwestern (SW) part of the Cuddapah basin shown in Fig. 1 and covering four mandals; Lingala, Pulivendula, Vempalli, and Vemula. Lingala, Pulivendula, Vempalli, and Vemula. It lies between latitude 14° 18′ 0″ N to 14° 28′ 0″; longitude 78° 0′ 00″ E 78° 30′ 0″ falls in Topo sheet no 57 J/02, 57J/03, 57J/04,57J07 (Fig. 1). The study area consists of purple shale, massive limestone, intraformational conglomerate, dolostone (uraniferous), shale, quartzite, cherty limestone and basic intrusive in Papaghni and Chitravati groups belongs to Lower Cuddapah supergroup [3]. The major geomorphic units of the study area are Denudational hills, Pediment & Pediplain. The soil types of the study area are black, alluvial, brown and mixed soils. The average annual rainfall is 600–650 mm and the average temperature varies from 20.4 °C in December to 43.2 °C in April [4].
Fig. 1.
Location map of the study area (by Sesha Sai et al. present work; modified after Nagaraja Rao et al., 1987).
1.2. Analytical data
The conceptual site model (CSM) designed for simply approaching for inactive/abandoned mines investigation as shown in Fig. 2. Analytical data of the groundwater samples given in Table 1. The data of physicochemical parameters of individual groundwater samples and statistical parameters like mean, median and mode data are given in Table 2. Graphical representation of statistics of physicochemical parameters is shown in Fig. 3. Fluoride classification of groundwater in the study area 6.8% of people fall under the high-risk category in the view of dental and skeletal fluorosis as shown in Table 4. The physical and chemical impacts due to inactive/abandoned mine site prospects data of the study area were given in Table 5. The frequency distribution of fluoride concentration for risk evaluation in groundwater is shown in Fig. 4. Correlation among physicochemical parameters of the Groundwater samples as depicted in Table 3. As from Fig. 5 shows a strong positive correlation is observed from the correlation coefficient values between EC and TDS (0.9949), EC- TH (0.6685), TH - TDS (0.65), TH – Cl- (0.57) are positively correlated. Dangerous slope and high walls of abandoned clay mine present near Lingala village attractive nuisance and is located within close distance to a populated area, the public road is depicted in Fig. 6 [[5], [6], [7], [8], [9], [10], [11], [12], [13], [14], [15]].
Fig. 2.
CSM model for simplified approaching for dealing with inactive/abandoned mines.
Table 1.
Analytical data for the groundwater samples from the study area.
S·NO | Village | pH | EC μS/cm | TDS mg/L | TH mg/L | Ca2+ mg/L | Mg2+ mg/L | CO32− mg/L | HCO3− mg/L | Cl− mg/L | F− mg/L |
---|---|---|---|---|---|---|---|---|---|---|---|
1 | VS1 | 8.4 | 823 | 382 | 160 | 24 | 34 | 12 | 293 | 28 | 0.4 |
2 | VS2 | 8.8 | 390 | 203 | 160 | 8 | 10 | 24 | 73 | 36 | 0.24 |
3 | VLP3 | 8.1 | 1450 | 750 | 300 | 48 | 59 | 24 | 146 | 312 | 0.27 |
4 | GLD 4 | 8.5 | 2590 | 1340 | 280 | 16 | 16 | 24 | 317 | 454 | 1.27 |
5 | GLD 5 | 8.2 | 369 | 188 | 100 | 40 | 83 | 12 | 122 | 43 | 0.62 |
6 | GLD 6 | 8.8 | 1500 | 800 | 200 | 16 | 20 | 36 | 317 | 36 | 2.06 |
7 | VEM 7 | 8 | 2150 | 1100 | 280 | 16 | 44 | 24 | 293 | 78 | 0.73 |
8 | GON 8 | 8.4 | 1040 | 540 | 200 | 16 | 15 | 12 | 220 | 142 | 0.66 |
9 | VEM 9 | 8.1 | 634 | 327 | 180 | 16 | 40 | 24 | 195 | 135 | 0.46 |
10 | GON 10 | 7 | 1070 | 555 | 220 | 40 | 58 | 12 | 268 | 21 | 0.79 |
11 | VKP 11 | 8.7 | 1430 | 740 | 340 | 24 | 39 | 36 | 244 | 220 | 0.71 |
12 | GUN 12 | 8.2 | 1760 | 910 | 140 | 24 | 20 | 24 | 219 | 135 | 1.6 |
13 | GON 13 | 8.6 | 2170 | 1120 | 520 | 56 | 40 | 36 | 244 | 369 | 1.22 |
14 | RAN 14 | 8.9 | 1450 | 750 | 180 | 16 | 78 | 48 | 366 | 85 | 2.55 |
15 | PRN 15 | 8.6 | 1180 | 610 | 140 | 56 | 40 | 24 | 317 | 57 | 3 |
16 | CGU 16 | 7.8 | 1710 | 880 | 280 | 16 | 63 | 60 | 24 | 234 | 0.87 |
17 | CGU 17 | 8.5 | 826 | 423 | 200 | 40 | 49 | 24 | 122 | 71 | 1.6 |
18 | KGB 18 | 8.8 | 1220 | 630 | 160 | 40 | 68 | 36 | 268 | 120 | 0.88 |
19 | BMP 19 | 8.1 | 1000 | 516 | 260 | 88 | 39 | 24 | 171 | 106 | 0.8 |
20 | MDP 20 | 7.9 | 1150 | 590 | 360 | 40 | 82 | 12 | 195 | 85 | 0.66 |
21 | VEM 21 | 8.1 | 811 | 421 | 200 | 40 | 68 | 24 | 195 | 50 | 0.87 |
22 | BSP 22 | 8.1 | 1070 | 550 | 240 | 24 | 34 | 24 | 48 | 99 | 0.92 |
23 | BSP 23 | 7.7 | 967 | 500 | 260 | 24 | 63 | 36 | 38 | 78 | 0.74 |
24 | VLP 24 | 8.3 | 792 | 409 | 200 | 40 | 63 | 12 | 39 | 43 | 0.66 |
25 | VLP 25 | 8.4 | 774 | 400 | 200 | 40 | 117 | 36 | 40 | 36 | 1.19 |
26 | DUGP 26 | 8.2 | 1170 | 600 | 300 | 32 | 49 | 12 | 41 | 85 | 1.55 |
27 | ALVP 27 | 8.4 | 247 | 127 | 80 | 24 | 44 | 14 | 98 | 35 | 0.38 |
28 | ALVP 28 | 7.6 | 3960 | 2050 | 400 | 56 | 45 | 12 | 293 | 618 | 0.56 |
29 | ALVP 29 | 8.4 | 233 | 121 | 120 | 24 | 117 | 0 | 73 | 28 | 0.55 |
30 | VEM 30 | 8.4 | 639 | 329 | 440 | 40 | 10 | 12 | 122 | 57 | 0.75 |
31 | VEM 31 | 8.1 | 2100 | 1090 | 340 | 40 | 24 | 12 | 244 | 291 | 1.08 |
32 | VEMO 32 | 8.6 | 977 | 502 | 260 | 24 | 44 | 24 | 268 | 64 | 0.81 |
33 | KUPP 33 | 8.2 | 1520 | 790 | 320 | 48 | 24 | 12 | 244 | 149 | 0.52 |
34 | KUPP 34 | 7.8 | 1980 | 1020 | 360 | 24 | 15 | 24 | 195 | 277 | 0.56 |
35 | THP 35 | 8.7 | 1850 | 960 | 300 | 32 | 39 | 24 | 342 | 20 | 0.87 |
36 | CHRP 36 | 7.9 | 1050 | 540 | 240 | 40 | 54 | 24 | 221 | 92 | 0.91 |
37 | GIDVP 37 | 7.6 | 1320 | 680 | 380 | 56 | 63 | 24 | 122 | 49 | 0.83 |
38 | BKP 38 | 7.7 | 961 | 494 | 280 | 48 | 23 | 24 | 195 | 57 | 0.67 |
39 | BKP 39 | 7.8 | 2030 | 1050 | 400 | 64 | 77 | 24 | 196 | 206 | 0.51 |
40 | AMP 40 | 7.9 | 2260 | 1017 | 460 | 32 | 87 | 48 | 244 | 255 | 1.37 |
41 | AMBP 41 | 6.1 | 390 | 250 | 120 | 64 | 29 | 40 | 230 | 28 | 0.6 |
42 | NGP-42 | 7.9 | 410 | 262 | 80 | 104 | 53 | 30 | 220 | 64 | 0.7 |
43 | NGP 43 | 7.8 | 320 | 205 | 120 | 88 | 38 | 26 | 200 | 78 | 0.2 |
44 | MKGP-44 | 8 | 360 | 230 | 100 | 80 | 58 | 30 | 220 | 28 | 0.7 |
Table 2.
Statistical parameters of Southwestern part of Cuddapah basin.
Min | Max | Mean | St.Dev | CV | Median | |
---|---|---|---|---|---|---|
pH | 6.1 | 8.9 | 8 | 0.5 | 6 | 8 |
EC μS/cm | 233 | 3960 | 1229 | 741 | 60 | 1070 |
TDS mg/L | 121 | 2050 | 635 | 375 | 59 | 552 |
TH mg/L | 80 | 520 | 246 | 107 | 43 | 240 |
Ca2+ mg/L | 8 | 104 | 39 | 21 | 55 | 40 |
Mg2+ mg/L | 10 | 117 | 48 | 25 | 52 | 44 |
CO32− mg/L | 0 | 60 | 24 | 11 | 47 | 24 |
HCO3− mg/L | 24 | 366 | 194 | 92 | 47 | 209 |
Cl− mg/L | 20 | 618 | 126 | 127 | 100 | 78 |
F− mg/L | 0.2 | 3 | 0.9 | 0.5 | 62 | 0.7 |
Fig. 3.
Statistics of physico-chemical parameters.
Table 4.
Fluoride classification of groundwater of the study area.
F- mg/L | Health Impact on humans | Frequency |
---|---|---|
<0.5 | Dental caries | 15.90% |
0.6–1.5 | Required levels for human | 70.45% |
1.6–2 | Dental fluorosis | 68.80% |
2.1–3 | Dental and skeletal fluorosis | 6.80% |
>3 | leads to skeletal fluorosis | – |
Table 5.
Distance from rural areas to inactive/abandoned mine sites.
Inactive/abandoned mine | Village | Latitude | Longitude | Distance from villages | Distance from agriculture land | Impacts |
|
---|---|---|---|---|---|---|---|
Physical | Chemical | ||||||
Barite | V. Kottapalli | 14.346 | 78.351 | 50 m | 10 m |
|
Effect on groundwater quality and soil quality |
Vemula | 14.355 | 78.310 | 15 m | 10 m | |||
Vemula | 14.367 | 78.345 | 20 m | 30 m | |||
Vempalli | 14.381 | 78.453 | 50 m | 20 m | |||
Mugguraikona | 14.343 | 78.327 | 100 m | 50 m | |||
Yellow ochre | Alavalapadu | 14.420 | 78.386 | 40 m | 10 m |
|
Effect on groundwater quality and soil quality |
Nagur | 14.447 | 78.408 | 20 m | 15 m | |||
Ammayagari palli | 14.408 | 78.443 | 20 m | 25 m | |||
Chagaleru | 14.397 | 78.363 | 10 m | 5 m | |||
Ramanuthala palli | 14.465 | 78.136 | 35 m | 10 m | |||
Asbestos | Brahmanapalli | 14.416 | 78.185 | 200 m | 10 m |
|
Effect on groundwater quality and soil quality, Acid mine drainage |
White clay | Lingala | 14.482 | 78.115 | 300 m | 10 m |
|
Effect on groundwater quality and soil quality |
Fig. 4.
Frequency distribution of fluoride concentration for risk evaluation in groundwater SW part of Cuddapah basin.
Table 3.
Correlation of water quality parameters.
pH | EC | TDS | TH | Ca2+ | Mg2+ | CO32- | HCO3− | Cl− | F− | |
---|---|---|---|---|---|---|---|---|---|---|
pH | 1 | |||||||||
EC | 0.006597 | 1 | ||||||||
TDS | −0.00364 | 0.997459* | 1 | |||||||
TH | −0.03904 | 0.668526* | 0.650018* | 1 | ||||||
Ca2+ | −0.3805 | −0.1467 | −0.12207 | −0.0536 | 1 | |||||
Mg2+ | −0.03399 | −0.14743 | −0.16732 | −0.08673 | 0.103267 | 1 | ||||
CO32- | −0.03206 | 0.135555 | 0.130064 | 0.069014 | −0.0148 | 0.119485 | 1 | |||
HCO3− | 0.110248 | 0.432164 | 0.440017 | 0.077633 | 0.056673 | −0.27855 | 0.095566 | 1 | ||
Cl− | −0.02906 | 0.821947* | 0.82518* | 0.570965 | −0.01735 | −0.16565 | 0.089897 | 0.224608 | 1 | |
F− | 0.343733 | 0.207242 | 0.202335 | −0.02051 | −0.13886 | 0.037513 | 0.320365 | 0.321828 | −0.03485 | 1 |
Fig. 5.
Correlation among physico - chemical parameters of the Groundwater samples.
Fig. 6.
Abandoned Clay mine near Lingala Village, Y·S.R district.
2. Experimental design, materials, and methods
The conceptual site model (CSM) was developed for a simplified approach to the assessment of the physical and environmental impacts of the Inactive/abandoned mines in the SW part of the Cuddapah basin. The fieldwork began with the identification and location of all the Inactive/abandoned mines in the SW part of the Cuddapah basin. 44 Groundwater samples were collected in and around inactive/Abandoned mines in the Southwestern part of the Cuddapah basin, Andhra Pradesh during September 2018 and taken necessary precautions to avoid contamination. All the groundwater samples were collected in two-liter pre-cleaned and well-dried polyethylene bottles and analyzed electrical conductivity (EC), pH, total dissolved solids (TDS), major cations and anions, adopting the standard methods APHA 2012 [16]; pH and EC, TDS (Conductivity cell CD-10) are determined with help of water analyzer 371 field kit respectively; Total Hardness, Ca2+, Mg2+, CO32−, HCO3− and Cl− were determined using titrimetry as laboratory followed standard methods (APHA 1998); F− is determined using ion-selective electrode (Orion 4 star ion meter, Model: pH/ISE).
Acknowledgment
This work was carried out by the financial support from the DST (Dept. of Science & Technology, New Delhi, India) in the form of INSPIRE Fellowship to the first author.
Footnotes
Supplementary data to this article can be found online at https://doi.org/10.1016/j.dib.2020.105187.
Conflict of Interest
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper
Appendix A. Supplementary data
The following is the Supplementary data to this article:
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