3.1.1. Physico-chemical properties of surface water of river
The river Kali-East originates in Khatauli town in the Muzaffarnagar district of Uttar Pradesh. The river flows for approximately 550 km before meeting river Ganga in Kannauj. During the time of sampling (March-May), the river was not receiving any water due to precipitation and the river Kali-East primarily carried sewage and industrial discharge. The physico-chemical properties of the river water are driven by the discharge of sewage and industrial effluents from sugar, distillery, chemical, food & dairy, pulp & paper, slaughter house and textile industries in the catchment area. The sugar industries only operate seasonally however, other industries run throughout the year.
In river water, the color varied as 20–200 Hazen, DO as 0-8.16 mg/l, BOD as 6.6–410 mg/l, COD as 22-1409 mg/l, TSS as 38-4368 mg/l, TDS as 180–2536 mg/l, Cl¯ as 27–845 mg/l, NH3-N as 1.5–77.4 mg/l, NO3-N as 0.1–5.8 mg/l and PO4-P as 0.2–5.2 mg/l. The physico-chemical properties of river water at 27 selected monitoring locations are presented in Table 3.
Table 3
Physico-chemical properties of surface water of river Kali-East in India
Sampling code
|
Monitoring location on river
|
Parameter
|
Color
|
pH
|
DO
|
BOD
|
COD
|
TSS
|
TDS
|
Cl¯
|
NH3-N
|
NO3-N
|
PO4-P
|
TC
|
FC
|
S1
|
Before confluence of Sugar mill drain at Khatauli
|
Dry
|
-
|
-
|
S2
|
After confluence of Sugar mill drain
|
30
|
4.9
|
0
|
410
|
1070
|
259
|
1094
|
142
|
3.9
|
1.6
|
2.2
|
7 × 105
|
22 × 104
|
S3
|
Downstream of Muzaffarnagar-Khatauli near Khadli Village
|
51
|
7.3
|
0
|
78
|
167
|
88
|
1120
|
199
|
13.5
|
4.4
|
4.2
|
28 × 103
|
14 × 103
|
S4
|
Upstream of Saini village
|
Dry
|
-
|
-
|
S5
|
Downstream of Saini village
|
bdl
|
6.7
|
0
|
132
|
421
|
254
|
2536
|
845
|
13.4
|
2.2
|
1
|
46 × 105
|
31 × 105
|
S6
|
Upstream of Abu drain-1
|
bdl
|
7.2
|
0
|
80
|
246
|
132
|
2376
|
781
|
12.6
|
1.4
|
1.1
|
22 × 104
|
45 × 103
|
S7
|
Downstream of Abu drain-1
|
bdl
|
7.6
|
0
|
146
|
289
|
177
|
1176
|
316
|
77.4
|
3.9
|
3.4
|
16 × 106
|
92 × 105
|
S8
|
After confluence of Abu drain-2
|
bdl
|
7.1
|
0
|
130
|
375
|
411
|
708
|
113
|
27.2
|
0.8
|
3.4
|
54 × 107
|
22 × 107
|
S9
|
Downstream of Odean Nala
|
bdl
|
7.0
|
0
|
154
|
474
|
765
|
608
|
96
|
29.7
|
0.6
|
3.8
|
2 × 109
|
17 × 107
|
S10
|
Upstream of Hapur drain-1
|
200
|
7.3
|
0
|
80
|
778
|
466
|
804
|
121
|
54.2
|
1.4
|
4.9
|
13 × 108
|
34 × 107
|
S11
|
Downstream of Hapur drain-1
|
143
|
7.2
|
0
|
49
|
555
|
280
|
752
|
126
|
64
|
2.5
|
4.5
|
49 × 106
|
49 × 106
|
S12
|
Downstream of Chhoiya drain
|
178
|
7.2
|
0
|
86
|
1074
|
226
|
752
|
118
|
49
|
2.4
|
4.1
|
11 × 106
|
11 × 106
|
S13
|
Downstream of Hapur drain
|
154
|
7.2
|
0
|
92
|
469
|
265
|
836
|
146
|
55.8
|
2.6
|
5.2
|
33 × 105
|
33 × 105
|
S14
|
Downstream of Kadrabad drain
|
173
|
7.3
|
0
|
73
|
567
|
384
|
960
|
165
|
47.8
|
2.8
|
5
|
78 × 105
|
2 × 106
|
S15
|
Downstream of Gulaothi drain
|
bdl
|
7.5
|
0
|
78
|
209
|
206
|
828
|
146
|
30.8
|
1.5
|
3.2
|
94 × 105
|
94 × 105
|
S16
|
Upstream of Bulandshahar drains
|
bdl
|
7.4
|
0
|
33
|
114
|
92
|
844
|
171
|
29.5
|
1
|
3.4
|
22 × 105
|
13 × 105
|
S17
|
Upstream of Bulandshahar Devipura drain
|
bdl
|
7.4
|
0
|
45
|
219
|
308
|
816
|
156
|
26.7
|
1.5
|
3.3
|
22 × 105
|
79 × 104
|
S18
|
Downstream of Bulandshahar Devipura drain
|
bdl
|
7.4
|
0
|
52
|
135
|
72
|
820
|
142
|
37.6
|
1.5
|
3.6
|
38 × 106
|
12 × 106
|
S19
|
Downstream of Bulandshahar drains
|
bdl
|
7.3
|
0
|
186
|
1409
|
4368
|
870
|
127
|
32.6
|
1.5
|
3.8
|
16 × 106
|
54 × 105
|
S20
|
Upstream of M/s Wave Distilleries and Breweries Ltd.
|
bdl
|
7.6
|
0.8
|
22
|
76
|
48
|
870
|
160
|
33.3
|
0.1
|
4.4
|
35 × 103
|
17 × 103
|
S21
|
Downstream of M/s Wave Distilleries and Breweries Ltd.
|
bdl
|
7.6
|
0.6
|
23
|
67
|
38
|
848
|
158
|
31.7
|
0.2
|
4.4
|
24 × 104
|
24 × 104
|
S22
|
Downstream of Neem drain
|
bdl
|
6.6
|
5.7
|
28
|
111
|
98
|
1108
|
394
|
27.1
|
5.8
|
1.6
|
13 × 103
|
34 × 102
|
S23
|
Upstream of Kasganj drain
|
bdl
|
7.2
|
5.9
|
27
|
43
|
72
|
294
|
59
|
6.2
|
0.4
|
0.4
|
790
|
490
|
S24
|
Downstream of Kasganj drain
|
bdl
|
7
|
8.2
|
6.9
|
22
|
74
|
180
|
27
|
2.6
|
0.3
|
0.2
|
13 × 103
|
93 × 102
|
S25
|
At Khudaganj bridge
|
80
|
8.6
|
7.7
|
15.7
|
61.9
|
-
|
316
|
40.4
|
1.5
|
3.4
|
0.6
|
3.3 × 104
|
2 × 103
|
S26
|
Upstream of Patta drain
|
70
|
8.3
|
7.6
|
8.2
|
50.3
|
-
|
415
|
75
|
3.3
|
3.9
|
0.7
|
3.3 × 105
|
3.3 × 104
|
S27
|
Downstream of Patta drain
|
60
|
8.1
|
7.7
|
15.6
|
57.2
|
-
|
504
|
75
|
2.2
|
3.1
|
0.7
|
1.6 × 107
|
2.4 × 106
|
DO dissolved oxygen, BOD biochemical oxygen demand, COD chemical oxygen demand, TSS total suspended solids, TDS total dissolved solids, Cl¯ chloride, NH3-N ammoniacal nitrogen, NO3-N nitrate, PO4-P phosphate, TC total coliform, FC fecal coliform |
All parameters are presented in mg/l except colour (Hazen), pH, TC (MPN/100 ml), and FC (MPN/100 ml) |
bdl below detection limit |
The color of water influences the photosynthesis process due to differential penetration of light, energy budget, stratification due to thermal gradients, and the aesthetic appearance of the aquatic ecosystems (Branco and Torgersen 2009). Color is a prominent feature of natural water when good quality water is produced from it for domestic and industrial purposes (Chow et al. 2007). In filtered water, the color chiefly arises from the dissolved organic carbon (fraction of total organic carbon) and ferric iron (Fe (III)) bound on it (Weyhenmeyer et al. 2014). The temperature drives certain chemical and biological reactions taking place in water and aquatic organisms (Shrivastava and Patil 2002). The pH rigorously affects the water quality by changing the alkalinity, the solubility of metals and hardness of the water (Osibanjo et al. 2011; Sener et al. 2017). The pH is driven by several factors such as aerosol and dust particles, dissolved materials, human-made wastes as well as wastes from plants through photosynthesis (Mitra et al. 2018).
The dissolved oxygen governs the metabolism of the biological community in an aquatic ecosystem and indicates the trophic status of a water body (Saksena et al. 2008). The dissolved oxygen reduces in the water due to respiration of biota, decomposition of organic matter, rise in temperature, oxygen demanding wastes and inorganic reductants such as hydrogen sulfide, ammonia, nitrates, ferrous iron, etc. (Sahu et al. 2000). Dissolved oxygen is frequently used to evaluate the water quality in reservoirs, bays, and rivers (Sanchez et al. 2007). In a study conducted by Rudolf et al. (2002) on water quality of San Vicente Bay (Chile), the dissolved oxygen content was considered as an index of water quality to assess the influence of industrial and municipal effluents on aquatic ecosystems.
Dissolved oxygen content and biochemical oxygen demand are greatly influenced by a combination of physical, chemical, and biological properties of oxygen demanding substances, encompassing algal biomass, dissolved organic matter, ammonia, volatile suspended solids, and sediment oxygen demand (Quinn et al. 2005; Kannel et al. 2007). Biochemical oxygen demand accounts for the extent of organic pollution in aquatic ecosystems (Khan et al. 2016). The oxygen requirement during the decomposition of organic matter and oxidation of inorganic chemicals is predicted through COD tests. Theoretically, if COD concentration is higher, then the water is considered polluted (Amneera et al. 2013).
Nitrates are the most thermodynamically stable and non-toxic form of inorganic nitrogen as it is the end product of the aerobic decomposition of the organic nitrogenous compound (Jaji et al. 2007). The nitrate concentration in the surface water is normally low (0–18 mg/l) however it may reach to elevated levels due to agricultural runoff (excess application of nitrogenous fertilizers and manures), oxidation of nitrogenous waste products in human and animal excreta and refuse dump runoff (Pillay and Olaniran 2016; Mitra et al. 2018). The excess nitrogen transported as nitrate-nitrogen to rivers leads to eutrophication and episodic and persistent hypoxia (dissolved oxygen < 2 mg/l) (Mitsch et al. 2005). The existence of chloride in river water is due to the organic waste in water, primarily of animal origin. Also, major sources of phosphate in river water are domestic sewage, agricultural effluents and industrial wastewaters (Saksena et al. 2008). The properties of surface water in Indian rivers are shown in Table 4.
Table 4
Properties of surface water in rivers in India and in the present study
Location
|
River
|
Year
|
Parameter
|
Reference
|
pH
|
DO
|
BOD
|
COD
|
TDS
|
Clˉ
|
NO3ˉ
|
Rishikesh (India)
|
Ganga
|
2008
|
9-10.5
|
7.8–16.1
|
4.3–19.5
|
-
|
18–85
|
10-32.5
|
-
|
Haritash et al. (2014)
|
Haridwar (India)
|
Ganga
|
2012-13
|
6.9-8
|
-
|
2.1–2.9
|
4.6–6.8
|
-
|
-
|
0.02–0.04
|
Matta et al. (2017)
|
Haridwar to Garh Mukteshwar (India)
|
Ganga
|
2014-15
|
7.1–8.9
|
1.2–9.3
|
2–87
|
19–791
|
108.6–1743
|
-
|
1.7–15.8
|
Chaudhary et al. (2017)
|
Kolkata (India)
|
Ganga
|
2005-06
|
6.7–7.3
|
-
|
35.1–121
|
129–342
|
40–78
|
-
|
-
|
Aktar et al. (2010)
|
Uttarakhand and Uttar Pradesh (India)
|
Ramganga
|
2014
|
7.3
|
-
|
15
|
29.4
|
22.2
|
8.6
|
4.7
|
Khan et al. (2016)
|
Ramganga (India)
|
Ramganga
|
2014-15
|
7.2–8.3
|
0.2–9.2
|
0.6–46.3
|
3-229
|
27.2-619.1
|
3.7–27.8
|
-
|
Gurjar and Tare (2019)
|
Gomti (India)
|
Gomti
|
2002-03
|
7.5–8.9
|
0.5-9
|
1.8–19
|
8.7–54
|
213–275
|
5–14
|
-
|
Singh et al. (2005)
|
Uttar Pradesh (India)
|
Gandak
|
2006
|
6.2–8.6
|
-
|
-
|
-
|
60.1-192.6
|
3.5–121
|
14–38
|
Bhardwaj et al. (2010)
|
Uttar Pradesh (India)
|
Kali-East
|
2019
|
4.9–8.6
|
0-8.2
|
6.9–410
|
22-1409
|
180–2536
|
27–845
|
0.1–4.4
|
Present study
|
DO dissolved oxygen, BOD biochemical oxygen demand, COD chemical oxygen demand, TDS total dissolved solids, Cl¯ chloride, NO3 nitrate |
All parameters are expressed in mg/l except pH |
In the present study, the river was highly polluted until approximately 143 km downstream from the origin of the river. In this stretch (Muzaffarnagar to Bulandshahar district), DO was NIL and BOD was high (up to 410 mg/l). However, after the mixing of the upper and lower Ganga canal in the polluted water of the river Kali-East, the water quality improved (DO increased and BOD decreased). The DO level increased to 7.7 mg/l and BOD decreased to 15.6 mg/l before meeting the river Ganga.
In Muzaffarnagar district, high BOD (410 mg/l), COD (1070 mg/l) and TDS (1094 mg/l) in the river water downstream sugar mill drain were observed. Also, low pH (4.9) in river water indicates industrial discharge from near-by industries. In Meerut district, pronounced foul smell around the river was observed D/s Chhoiya drain and Hapur drain. The color of the river water at these locations varied as 154–178 Hazen. The foul smell in the river water may be attributed to anaerobic decomposition of organic matter present in the river. Also, it was observed that river water U/s Chhoiya drain, D/s Chhoiya drain, and D/s Hapur drain is being utilized for irrigation of adjoining agricultural fields. Irrigation of agricultural fields with the polluted river water may deteriorate human health due to the bio-amplification of pollutants to the human food chain. In Bulandshahar district, the river water quality (BOD-186 mg/l, COD-1409 mg/l) deteriorated after the discharge of 11 drains into the river. Till Bulandshahar, there is no DO in the river. However, after traversing a distance of approximately 143 km, the river meets upper Ganga canal and the river water quality improved substantially (DO-0.8 mg/l, BOD-22 mg/l, and COD-76 mg/l) at U/s Wave Distilleries and Breweries Ltd., Aligarh after meeting the canal. In Aligarh district, the river further meets another canal i.e. lower Ganga canal and the river water quality after meeting the canal improved further (DO-5.9 mg/l and fecal coliform-490 MPN/100 ml) at U/s Kasganj drain. In Kannauj district, the DO in the river Kali-East increased to 7.7 mg/l before the confluence with river Ganga.
3.1.2 DO-sag curve
The DO-sag curve in the river Kali-East is presented in Fig. 2. Considering bathing water quality criteria (pH 6.5–8.5, DO ≥ 5 mg/l, BOD ≤ 3 mg/l, and FC < 500 MPN/100 ml), the water quality of the river Kali-East was found complying with bathing water standards w.r.t. pH except for one location namely, U/s Sugar mill drain in Muzaffarnagar. Low pH (4.9) in the river at this location may be attributed to the discharge of untreated effluent from near-by sugar industries. With respect to DO, no location in the stretch from Muzaffarnagar to Aligarh was found suitable for bathing. Due to the mixing of freshwater from the Ganga canal in the river Kali-East, the water quality in Kasganj and Kannauj before meeting the river Ganga was meeting the primary water quality criteria w.r.t. DO. Also, no location in the whole stretch of the river meets bathing water quality w.r.t. BOD. High BOD in the river is due to the discharge of untreated domestic sewage and industrial effluents from the catchment area.
For fecal coliform, only two locations, namely, (i) U/s Kasganj drain in Kasganj and (ii) at Khudaganj bridge in Kannauj were meeting bathing water quality standards.
3.1.4 Metals concentration in surface water of river
Metals (As, Cd, Cr, Cu, Fe, Pb, Mn, Ni, Hg, Zn, Sb, Co, Se, and V) concentration in surface river water samples are shown in Table 5.
Table 5
Metal concentration (mg/l) in surface river water collected from different locations on river Kali-East in India
Location
|
Metals
|
As
|
Cd
|
Cr
|
Cu
|
Fe
|
Pb
|
Mn
|
Ni
|
Hg
|
Zn
|
Sb
|
Co
|
Se
|
V
|
S1
|
Dry
|
S2
|
bdl
|
bdl
|
0.02
|
0.08
|
15.70
|
0.11
|
0.28
|
0.01
|
bdl
|
0.14
|
bdl
|
bdl
|
bdl
|
bdl
|
S3
|
bdl
|
bdl
|
bdl
|
bdl
|
1.96
|
bdl
|
0.25
|
bdl
|
bdl
|
0.02
|
bdl
|
bdl
|
bdl
|
bdl
|
S4
|
Dry
|
S5
|
bdl
|
bdl
|
bdl
|
0.02
|
1.75
|
0.01
|
0.21
|
bdl
|
bdl
|
0.07
|
bdl
|
bdl
|
bdl
|
bdl
|
S6
|
bdl
|
bdl
|
bdl
|
0.01
|
0.73
|
bdl
|
0.13
|
bdl
|
bdl
|
0.06
|
bdl
|
bdl
|
bdl
|
bdl
|
S7
|
bdl
|
bdl
|
bdl
|
0.13
|
2.87
|
0.02
|
0.17
|
bdl
|
bdl
|
0.10
|
bdl
|
bdl
|
bdl
|
bdl
|
S8
|
bdl
|
0.15
|
0.09
|
0.36
|
10.52
|
0.09
|
0.32
|
0.11
|
bdl
|
1.02
|
bdl
|
bdl
|
bdl
|
bdl
|
S9
|
bdl
|
0.05
|
0.05
|
0.25
|
11.32
|
0.07
|
0.29
|
0.05
|
bdl
|
0.65
|
bdl
|
bdl
|
bdl
|
0.06
|
S10
|
bdl
|
0.03
|
0.04
|
0.13
|
5.17
|
0.03
|
0.25
|
0.04
|
bdl
|
0.42
|
bdl
|
bdl
|
bdl
|
bdl
|
S11
|
bdl
|
0.04
|
0.06
|
0.17
|
7.44
|
0.05
|
0.28
|
0.05
|
bdl
|
0.5
|
bdl
|
bdl
|
bdl
|
bdl
|
S12
|
bdl
|
0.02
|
0.03
|
0.09
|
3.46
|
0.03
|
0.24
|
0.03
|
bdl
|
0.28
|
bdl
|
bdl
|
bdl
|
bdl
|
S13
|
bdl
|
0.02
|
0.03
|
0.1
|
4.19
|
0.03
|
0.25
|
0.03
|
bdl
|
0.3
|
bdl
|
bdl
|
bdl
|
bdl
|
S14
|
bdl
|
0.02
|
0.03
|
0.08
|
3.89
|
0.02
|
0.26
|
0.02
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
0.06
|
S15
|
bdl
|
0.02
|
0.02
|
0.07
|
3.63
|
0.02
|
0.22
|
0.02
|
bdl
|
0.22
|
bdl
|
bdl
|
bdl
|
bdl
|
S16
|
bdl
|
bdl
|
bdl
|
0.03
|
1.82
|
bdl
|
0.21
|
bdl
|
bdl
|
0.13
|
bdl
|
bdl
|
bdl
|
bdl
|
S17
|
bdl
|
0.02
|
0.03
|
0.11
|
7.31
|
0.03
|
0.29
|
0.03
|
bdl
|
0.32
|
bdl
|
bdl
|
bdl
|
0.05
|
S18
|
bdl
|
bdl
|
bdl
|
0.03
|
1.15
|
0.01
|
0.21
|
bdl
|
0.11
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
S19
|
bdl
|
0.10
|
0.19
|
0.77
|
67.6
|
0.32
|
0.89
|
0.17
|
bdl
|
1.96
|
bdl
|
0.03
|
bdl
|
0.17
|
S20
|
bdl
|
bdl
|
bdl
|
bdl
|
1.16
|
bdl
|
0.26
|
bdl
|
bdl
|
0.03
|
bdl
|
bdl
|
bdl
|
bdl
|
S21
|
bdl
|
bdl
|
bdl
|
bdl
|
1.08
|
bdl
|
0.33
|
bdl
|
bdl
|
0.04
|
bdl
|
bdl
|
bdl
|
bdl
|
S22
|
bdl
|
bdl
|
bdl
|
bdl
|
2.38
|
bdl
|
0.31
|
bdl
|
bdl
|
BDL
|
0.01
|
bdl
|
bdl
|
bdl
|
S23
|
bdl
|
bdl
|
bdl
|
bdl
|
1.69
|
bdl
|
0.09
|
bdl
|
bdl
|
0.01
|
bdl
|
bdl
|
bdl
|
bdl
|
S24
|
bdl
|
bdl
|
bdl
|
bdl
|
3.33
|
bdl
|
0.10
|
bdl
|
bdl
|
0.02
|
bdl
|
bdl
|
bdl
|
bdl
|
S25
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
0.08
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
S26
|
bdl
|
0.01
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
0.08
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
S27
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
0.12
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl
|
bdl below detection limit |
Metals concentrations (mg/l) ranged as Cd bdl (below detection limit)-0.15, Cr bdl-0.19, Cu bdl-0.77, Fe bdl-15.7, Pb bdl-0.32, Mn bdl-0.89, Ni bdl-0.17, Hg bdl-0.11, Zn bdl-1.96, Sb bdl-0.01, Co bdl-0.03 and V bdl-0.17. Arsenic and Selenium were not found in river water. Metals in river water may be attributed to the discharge of untreated sewage from the catchment areas into the river. Also, the discharge of untreated/improperly treated industrial wastewater could also release toxic metals into the river water. The sources of metals such as Cd, Cr, and Cu are reported to be domestic as well as commercial (ATSDR 2012; Masood and Malik 2011). Apart from domestic wastewater, the catchment area of the river Kali-East comprises of several industries pertaining to sugar, textile, pulp & paper, dairy & food, distillery, and chemical sectors. These industries may also contribute to metal pollution in the river Kali-East. For e.g., textile wastewater consists of Cu, Fe, Mn, Pb, Zn, Cd, and Cr (Fenta 2014; Oyebamiji et al. 2019), and distillery wastewater contains Cu, Cr, Zn, Fe, Ni, Mn, and Pb (Chowdhary et al. 2018). The composition of wastewater generated by food and dairy and chemical industries depends upon the product-specific raw materials.