4.1 Quality Assurance/Quality Control
The accuracy of the analyses was determined using the percentage recovery for the NIST 2711a while precision was accessed with the relative percent difference (RPD) for the duplicate samples. The percentage recovery for NIST 2711a varied from 73.6–127% (Table 2). Apart from Ag, the recovery obtained were within the range of ± 30% for Cr and ± 20% for all other elements as specified in USEPA Method 6200 [15]. The RPD values obtained (Table 2) were less than 20% which showed acceptable results for duplicate samples [15].
Table 2
Mean Recovery for NIST 2711a and Relative Percent Differences for Duplicate Samples
Element | Mean Recovery for NIST 2711a (%) | Relative Percent Difference for Duplicate Samples (%) |
Ag | 73.6 | n/a |
As | 104 | n/a |
Ba | 90.4 | 5.1 |
Cd | 84.8 | n/a |
Cr | 127 | 13.8 |
Cu | 95.9 | 1.6 |
Fe | 101 | 0.3 |
Hg | 87.9 | n/a |
Mn | 89.1 | 1.5 |
Ni | 102 | 18.8 |
Pb | 108 | 16.7 |
V | 104 | 8.2 |
Zn | 100 | 2.9 |
n/a = RPD was not calculated since concentrations were below the limit of detection
4.2 Physiochemical Parameters
Physiochemical parameters determined for the 23 creeks in Metro Vancouver are provided in Table 3. The minimum and maximum pH levels of the water samples were 5.50 and 8.27 at Noons Creek (MVC 44) and Quibble Creek (MVC 13), respectively (Table 3). The pH for the sediments ranged from 5.77 at Beaver Creek (MVC 33) to 8.16 at King Lake (MVC 7). The pH affects most chemical and biological processes in water. It is one of the most important environmental factors limiting species distributions in aquatic habitats [24]. According to CCME [2], the pH of fresh waters should fall within the range of 6.5–9.0 units unless it can be demonstrated that such a pH is a result of natural processes. Two water samples at Noons Creek (MVC44 and MVC45) did not have their pH within the standard range of the Canadian water quality guidelines for the protection of aquatic life [2]. The low pH in those sites may be attributed to serpentine geology [24], since those sites were rocky and hilly in nature [25].
Total dissolved Solids (TDS) concentrations in the sampled creeks ranged from 14.0–633 ppm with the minimum at Noons Creek (MVC44) and the maximum of 633 ppm at Quibble Creek (MVC13). According to Garrison Investigative Board [26], in areas of Precambrian rock, TDS concentrations in water are generally less than 65 ppm. The two samples from Bon Accord Creek (MVC3 and MVC4) and the two samples from Noons Creek (MVC44 and MVC45) had their concentrations less than 65 ppm. According to the geology of the study area, rock formation in those sampled sites could predominantly be Precambrian. The highest TDS concentration at MVC13 may suggest a higher residential (urban) runoff as the site was closer to the very busy Surrey Memorial Hospital. The highest EC value (903 uS/cm) was also recorded at MVC13. The lowest EC value was recorded at MVC44 which is a sparsely populated area hence less chemicals such as chloride and phosphate from businesses and household products which might cause an increase in EC in the surface water.
Table 3
Physicochemical parameters for sediment and surface samples collected from Metro Vancouver Creeks
Creeks Sample sites | Sediment | Surface Water |
| pH | pH | EC (uS/cm) | TDS (ppm) |
exc | Bolivar | 7.71 | 7.49 | 310 | 340 |
MVC 2 | Bolivar | 7.72 | 7.62 | 314 | 224 |
MVC 3 | Bon Accord | 7.58 | 6.89 | 82 | 58 |
MVC 4 | Bon Accord | 7.22 | 6.26 | 198 | 14 |
MVC 5 | Bon Accord | 6.25 | 7.05 | 176 | 124 |
MVC 6 | King | 6.66 | 7.22 | 391 | 270 |
MVC 7 | King (Lake) | 8.16 | 6.99 | 148 | 104 |
MVC 8 | King | 7.08 | 6.71 | 225 | 157 |
MVC 9 | King (Kiyo) | 7.01 | 7.34 | 279 | 198 |
MVC 10 | Bear | 7.03 | 7.74 | 348 | 244 |
MVC 11 | Bear | 7.27 | 7.37 | 429 | 305 |
MVC 12 | Bear | 6.82 | 7.81 | 429 | 306 |
MVC 13 | Quibble | 6.87 | 8.27 | 903 | 633 |
MVC 14 | Quibble | 7.41 | 7.41 | 403 | 288 |
MVC 15 | Healy | 6.80 | 7.32 | 155 | 111 |
MVC 16 | Healy | 7.15 | 6.80 | 436 | 325 |
MVC 17 | Hyland | 7.10 | 7.24 | 436 | 310 |
MVC 18 | Hyland | 7.18 | 7.42 | 158 | 113 |
MVC 19 | Hyland (Industrial) | 6.97 | 7.24 | 532 | 373 |
MVC 20 | Stoney | 6.61 | 7.32 | 457 | 328 |
MVC 21 | Stoney | 6.84 | 7.43 | 411 | 293 |
MVC 22 | Surrey Lake | 6.62 | 7.39 | 463 | 325 |
MVC 23 | Bear | 6.27 | 7.02 | 486 | 347 |
MVC 24 | Bear | 6.17 | 7.46 | 502 | 356 |
MVC 25 | Bolivar | 6.25 | 6.85 | 468 | 335 |
MVC 26 | Robson | 6.12 | 6.75 | 149 | 106 |
MVC 27 | Cougar Lake | 6.57 | 6.58 | 232 | 166 |
MVC 28 | Cougar | 6.59 | 7.40 | 119 | 85 |
MVC 29 | Cougar | 6.76 | 7.13 | 111 | 79 |
MVC 30 | First Beach | 6.22 | 7.46 | 386 | 276 |
MVC 31 | Buckingham | 6.56 | 7.55 | 344 | 243 |
MVC 32 | Dear Lake Brook | 6.55 | 7.13 | 336 | 109 |
MVC 33 | Beaver | 5.77 | 6.83 | 368 | 262 |
MVC 34 | Eagle (Industrial) | 6.81 | 7.82 | 306 | 219 |
MVC 35 | Eagle | 6.59 | 7.77 | 311 | 222 |
MVC 36 | Guichon | 6.68 | 7.59 | 388 | 276 |
MVC 37 | Guichon | 6.97 | 7.59 | 380 | 270 |
MVC 38 | Chubb | 6.46 | 7.07 | 563 | 400 |
MVC 39 | Chubb | 6.14 | 6.83 | 580 | 410 |
MVC 40 | Hoy | 6.72 | 7.02 | 605 | 430 |
MVC 41 | Hoy | 6.79 | 7.11 | 249 | 178 |
MVC 42 | Scott | 6.79 | 7.54 | 218 | 155 |
MVC 43 | Scott | 7.20 | 7.35 | 227 | 161 |
MVC 44 | Noons | 6.10 | 5.50 | 19 | 14 |
MVC 45 | Noons | 6.41 | 6.48 | 44 | 31 |
MVC 46 | Hyde | 6.73 | - | - | - |
MVC 47 | Cedar | 6.35 | 6.61 | 283 | 201 |
4.3 Heavy Metals in Sediments
Heavy metal concentrations in sediments collected from the 23 creeks are presented in Table 4. The concentrations of Ag, As and Cd representing 96.6%, 94.4% and 94.4%, respectively were below the detection limit while all Hg concentrations were below the detection limit. Ag (2.53–4.11 mg/kg), As (7.51–16.27 mg/kg) and Cd (2.72–9.10 mg/kg) concentrations detected at Bon Accord (MVC5), King Creek (MVC8, MVC9), Bolivar Creek (MVC25) and Beaver Creek (MVC33) exceeded the LEL and SEL. The concentration of Cr ranged from 22.83–136.68 mg/kg in the study area. The lowest and highest concentrations were recorded at Hoy Creek (MVC40) and Hyland Creek (MVC19), respectively. The higher concentration of Cr at MVC19 may be due to effluent from an iron fabrication industry close to the sampled site and treated stormwater runoff from a concrete ready-mix operation at the site.
The highest Cu concentration (146 mg/kg) was recorded at Beaver Creek (MVC33) and the lowest (6.70 mg/kg) at King Lake. In the study area, 21.2% of sediment samples had Cu concentrations above the TEL. On the other hand, all Cu concentrations were below the PEL. For Ni concentration, 21.27% of sediment samples were below the detection limit while 32 sampling sites representing 68.0% had concentrations above the LEL. King Creek (MVC9) with a concentration of 75.9 mg/kg and Cedar Creek with a concentration of 102.12 mg/kg are the only sites with concentrations above the SEL (Table 4), hence 10.6% of the sampling sites was within the LEL and SEL. The major sources of Cu in the study area include the use of pesticides and herbicides especially on farmlands close to Bear Creek (MVC23 and MVC24), and wood preservatives such as chromated copper arsenate (CCA) used in the construction industry in the Metro Vancouver area. Corrosion of household plumbing, faucets, and water fixtures may also introduce Cu in the study area [27]. The potential sources of Ni are commercial effluents and leachates, as well as through atmospheric deposition after release from anthropogenic sources [28].
The Fe concentrations in the sediment ranged from 14,516.76–62,755.68 mg/kg with the lowest at Bon Accord Creek (MVC4) and highest at Cedar Creek (MVC47). The sediment at MVC47 had a reddish nature which was attributed to the high concentration of Fe. According to the United States Geological Survey (USGS) [29], Fe tends to add a rusty, reddish-brown color to water and sediments. With the exception of Bon Accord Creek (MVC4) with a Fe concentration of 14,516.76 mg/kg which is below the LEL, all the sampling sites in the study area had Fe concentration above the LEL representing 97.8% of the sampling sites. According to the standard for SEL, King Creek (MVC9), Bolivar Creek (MVC25), Scott Creek (MVC42, MVC43), Noons Creek (MVC45) and Cedar Creek (MVC47) had concentrations of Fe above the required limit representing 12.7% of the sampling sites in the study area. The rest of the sampling sites were below the SEL. For Mn, Bon Accord Creek (MVC4) had the lowest concentration of 385.16 mg/kg and King Lake (MVC7) had the highest concentration of 5,126.12 mg/kg. Forty-three sediment samples out of the 47 samples representing 91.4% had Mn concentrations above the LEL limit. Bon Accord Creeks (MVC4, MVC5), Stoney Creek (MVC20) and Cougar Lake (MVC27) had Mn concentrations below the LEL limit. Twelve sampling sites (25.5%) had Mn concentrations above the SEL. The concentration of vanadium (V) ranged from 50.93 mg/kg at Hyde Creek (MVC46) which was the lowest and 151.63 mg/kg at Cedar Creek (MVC47) which was the highest. The increased concentration of Fe, Mn and V in the study area may be attributed to geogenic sources naturally occurring from weathering of Fe, Mn and V bearing minerals and rocks [30].
The elevated concentrations of Pb above the TEL (Table 4) in Bon Accord Creek (MVC5-64.78 mg/kg), Quibble Creek (MVC14, 56.66 mg/kg), Bear Creek (MVC23, 68.53 mg/kg), Chubb Creek (MVC39, 38.44 mg/kg) and Beaver Creek (MVC33, 161.83 mg/kg) may be due to the sites being under heavy vehicular traffic. MVC33 with a Pb concentration of 161.83 mg/kg was the only site in the study area above the PEL. The concentration for Zn ranged from 21.40 mg/kg at Bon Accord Creek (MVC3) to 660.87 mg/kg at Beaver Creek (MVC33). Twenty-three sediment samples representing 48.9% were above the TEL. On the other hand, Beaver Creek (MVC33) and Chubb creek (MVC39) had concentrations above the PEL. The lowest Ba concentration was at Beaver Creek (MVC33; 98.06 mg/kg) and highest at Hyde Creek (MVC46; 674.21 mg/kg). According to Bonnevie et al. [31], Kennedy & Gadd [32] and Al-Masri et al. [33] as cited by Giri et al. [30], vehicular anthropogenic activities are known to be associated with augmentation of Pb, Zn and Ba.
The concentrations of heavy metals in the sampling area were also compared to background values [19], Table 4. It was observed that apart from Bon Accord Creek (MVC4), all the sampling sites in the study area had at least one heavy metal above the background level (Table 4), suggesting that there were probably some anthropogenic inputs at the sites [34]. According to results in Table 4, Bolivar Creek (MVC25) and Beaver Creek (MVC33) had at least nine heavy metals at each site above the TEL/LEL hence these sites were considered the most polluted. The high levels of these heavy metals may be due to the closeness of these sites to major highways with heavy vehicular activities. According to Awonaike et al. [35], chemicals commonly used in vehicle fluids, tires and paints were much higher in rivers next to roads with heavy traffic due to road surface runoffs thus suggesting a strong relationship between traffic and the concentration of these chemicals. Sediment contamination in this regard could pose a risk and cause adverse impacts to aquatic life.
Table 4
Concentrations of metals (mg/kg) in sediment samples collected from creeks in Metro Vancouver
Sample | Ag | As | Ba | Cd | Cr | Cu | Fe | Hg | Mn | Ni | Pb | V | Zn |
MVC-1 | < 1.91 | < 1.63 | 599.20 | < 3.10 | 62.05 | 34.18 | 33006 | < 3.89 | 693.99 | 29.76 | 14.20 | 89.10 | 163.50 |
MVC-2 | < 2.02 | < 2.47 | 533.44 | < 3.22 | 63.69 | 28.87 | 39157 | < 3.63 | 1265.82 | 53.58 | 16.39 | 98.56 | 163.30 |
MVC-3 | < 1.93 | < 1.80 | 552.71 | < 3.09 | 58.56 | 23.70 | 29042 | < 3.45 | 815.05 | 51.95 | 21.80 | 90.24 | 140.30 |
MVC-4 | < 1.60 | < 1.33 | 221.82 | < 2.63 | 52.31 | 13.84 | 14516 | < 3.18 | 385.16 | < 13.85 | 9.20 | 51.40 | 21.40 |
MVC-5 | < 2.57 | 16.27 | 176.42 | 3.13 | 65.61 | 85.79 | 23754 | < 3.43 | 398.79 | < 13.50 | 64.78 | 71.42 | 425.90 |
MVC-6 | < 1.88 | < 1.41 | 460.89 | < 3.03 | 46.68 | 15.01 | 28801 | < 3.591 | 505.86 | 11.89 | 7.77 | 80.16 | 57.23 |
MVC-7 | < 1.91 | < 1.39 | 518.04 | < 3.06 | 116.45 | 6.70 | 31141 | < 4.82 | 5126.12 | 43.92 | 5.02 | 86.24 | 87.22 |
MVC-8 | 2.53 | < 1.49 | 211.03 | 2.72 | 55.94 | 30.01 | 31904 | < 3.08 | 708.16 | 35.25 | 13.45 | 91.82 | 134.80 |
MVC-9 | < 1.97 | 10.26 | 530.23 | < 3.15 | 56.31 | 24.33 | 53432 | < 4.91 | 2600.33 | 75.95 | 13.11 | 105.48 | 218.80 |
MVC-10 | < 1.90 | < 1.63 | 527.16 | < 3.05 | 50.37 | 15.85 | 31213 | < 3.62 | 1192.16 | 38.27 | 9.44 | 89.82 | 107.30 |
MVC-11 | < 2.03 | < 1.68 | 607.90 | < 3.23 | 47.70 | 28.68 | 34936 | < 4.68 | 744.58 | 25.30 | 12.61 | 96.68 | 135.80 |
MVC-12 | < 1.84 | < 1.84 | 498.79 | < 3.01 | 54.34 | 21.09 | 27010 | < 3.41 | 449.58 | 22.02 | 27.34 | 86.12 | 123.60 |
MVC-13 | < 1.91 | < 1.76 | 429.99 | < 3.04 | 59.01 | 68.74 | 33579 | < 3.91 | 717.88 | 21.77 | 24.03 | 97.73 | 288.30 |
MVC-14 | < 1.97 | < 2.31 | 464.47 | < 3.04 | 104.33 | 26.16 | 31786 | < 5.28 | 546.85 | < 14.85 | 56.66 | 100.83 | 124.70 |
MVC-15 | < 1.86 | < 1.64 | 464.20 | < 2.96 | 104.27 | 37.10 | 28640 | < 3.65 | 479.25 | 38.41 | 15.75 | 90.71 | 174.40 |
MVC-16 | < 1.87 | < 1.90 | 467.74 | < 3.00 | 50.69 | 30.75 | 28546 | < 3.46 | 564.52 | < 10.23 | 30.41 | 82.71 | 166.70 |
MVC-17 | < 1.91 | < 1.86 | 510.62 | < 3.08 | 53.39 | 55.45 | 32765 | < 3.96 | 1097.41 | 44.73 | 26.67 | 92.52 | 303.10 |
MVC-18 | < 1.86 | < 1.59 | 433.10 | < 2.95 | 61.82 | 11.76 | 32090 | < 3.46 | 697.84 | 14.85 | 10.82 | 99.06 | 77.75 |
MVC-19 | < 1.82 | < 1.54 | 509.80 | < 2.98 | 136.68 | 11.77 | 28446 | < 3.59 | 651.98 | 31.72 | 9.72 | 77.48 | 101.00 |
MVC-20 | < 1.79 | < 1.76 | 380.08 | < 2.88 | 53.10 | 13.10 | 25275 | < 3.73 | 453.92 | < 15.01 | 29.57 | 79.90 | 89.11 |
MVC-21 | < 1.87 | < 1.54 | 515.51 | < 3.05 | 61.91 | 22.77 | 33177 | < 3.42 | 1271.15 | 47.03 | 11.09 | 93.99 | 134.70 |
MVC-22 | < 1.86 | < 1.54 | 472.74 | < 2.99 | 46.07 | 7.77 | 25100 | < 3.55 | 479.73 | 17.75 | 11.48 | 69.97 | 78.59 |
MVC-23 | < 2.44 | 5.82 | 410.51 | < 2.96 | 76.58 | 37.89 | 36285 | < 3.35 | 661.77 | 43.90 | 68.53 | 109.48 | 150.40 |
MVC-24 | < 1.90 | < 1.73 | 461.41 | < 3.07 | 41.77 | 15.24 | 34715 | < 3.55 | 993.76 | 39.06 | 17.28 | 81.98 | 186.30 |
MVC-25 | 3.31 | 7.51 | 139.46 | 6.57 | 44.37 | 44.05 | 51343 | < 3.39 | 607.70 | 41.57 | 15.56 | 86.10 | 208.80 |
MVC-26 | < 1.83 | < 1.89 | 448.18 | < 2.94 | 65.04 | 35.01 | 28504 | < 3.47 | 524.46 | 12.54 | 33.55 | 91.91 | 152.80 |
MVC-27 | < 1.83 | < 1.41 | 505.23 | < 2.95 | 61.56 | 27.96 | 26350 | < 3.43 | 405.01 | < 10.17 | 8.51 | 115.03 | 57.60 |
MVC-28 | < 1.89 | < 1.56 | 507.66 | < 3.03 | 48.62 | 20.25 | 28638 | < 3.54 | 625.88 | 25.31 | 10.61 | 89.83 | 146.30 |
MVC-29 | < 1.87 | < 1.51 | 499.78 | < 3.06 | 66.93 | 25.33 | 33789 | < 3.51 | 673.26 | 31.52 | 10.33 | 99.73 | 122.80 |
MVC-30 | < 1.82 | < 1.66 | 485.34 | < 2.93 | 47.78 | 21.80 | 25163 | < 3.41 | 602.25 | 13.90 | 16.07 | 82.21 | 94.11 |
MVC-31 | < 1.88 | < 1.60 | 545.91 | < 3.06 | 44.60 | 18.24 | 32662 | < 3.51 | 601.40 | 26.92 | 10.97 | 89.44 | 86.85 |
MVC-32 | < 1.93 | < 1.94 | 522.03 | < 3.09 | 45.28 | 48.04 | 40056 | < 3.60 | 1620.03 | 48.95 | 27.68 | 106.63 | 174.10 |
MVC-33 | 4.11 | 15.41 | 98.06 | 9.10 | 39.02 | 146.02 | 41751 | < 3.65 | 1123.22 | < 15.56 | 161.83 | 87.62 | 660.80 |
MVC-34 | < 2.06 | < 1.61 | 608.36 | < 3.26 | 35.31 | 16.48 | 42896 | < 3.65 | 1537.73 | 34.36 | 10.40 | 104.38 | 108.00 |
MVC-35 | < 1.86 | < 1.49 | 537.81 | < 2.97 | 43.73 | 11.44 | 26907 | < 3.52 | 777.22 | 14.53 | 9.510 | 70.41 | 72.22 |
MVC-36 | < 1.98 | < 1.46 | 601.95 | < 3.14 | 37.45 | 19.25 | 33047 | < 3.39 | 831.35 | 26.82 | 10.55 | 95.25 | 120.60 |
MVC-37 | < 1.87 | < 1.71 | 510.29 | < 2.96 | 36.44 | 19.02 | 27221 | < 3.47 | 868.41 | < 10.73 | 19.40 | 70.00 | 103.50 |
MVC-38 | < 1.95 | < 1.85 | 600.38 | < 3.14 | 47.37 | 40.24 | 36137 | < 3.56 | 606.32 | 30.56 | 24.90 | 88.49 | 128.90 |
MVC-39 | < 1.97 | < 3.26 | 483.37 | < 3.16 | 42.52 | 82.67 | 43252 | < 4.34 | 675.20 | 33.29 | 38.44 | 75.02 | 359.50 |
MVC-40 | < 1.95 | < 1.39 | 565.89 | < 3.13 | 22.83 | 18.13 | 36024 | < 3.78 | 743.81 | 17.09 | 5.95 | 94.9 | 58.73 |
MVC-41 | < 1.88 | < 1.52 | 490.26 | < 3.02 | 29.17 | 19.59 | 30084 | < 3.48 | 744.19 | < 12.87 | 8.90 | 71.27 | 89.92 |
MVC-42 | < 2.10 | < 1.48 | 574 | < 3.35 | 32.46 | 28.96 | 51067 | < 4.98 | 1240.94 | 39.57 | 5.88 | 125.05 | 118.6 |
MVC-43 | < 2.05 | < 1.51 | 626.75 | < 3.24 | 40.35 | 24.01 | 45407 | < 3.65 | 1279.39 | 38.00 | 5.35 | 106.37 | 90.28 |
MVC-44 | < 1.98 | < 1.59 | 612.79 | < 3.19 | 30.40 | 11.46 | 42975 | < 3.59 | 896.90 | 22.34 | 11.44 | 127.60 | 54.89 |
MVC-45 | < 2.10 | 2.22 | 584.51 | < 3.33 | 32.87 | 15.01 | 53484 | < 4.54 | 1924.81 | 64.82 | 15.90 | 140.39 | 102.36 |
MVC-46 | < 1.89 | < 1.45 | 674.21 | < 2.99 | 24.15 | 10.58 | 22071 | < 3.38 | 620.50 | < 9.28 | 11.19 | 50.93 | 52.30 |
MVC-47 | < 2.11 | < 1.72 | 541.59 | < 3.36 | 34.35 | 25.25 | 62755 | < 4.01 | 742.67 | 102.12 | 12.72 | 151.63 | 76.30 |
| Ag | As | Ba | Cd | Cr | Cu | Fe | Hg | Mn | Ni | Pb | V | Zn |
ISQG/TELa | | 5.9 | | 0.6 | 37.3 | 35.7 | | 0.17 | | | 35 | | 123 |
PELa | | 17 | | 3.5 | 90 | 190 | | 0.486 | | | 91.3 | | 315 |
LEL, BCb | 0.5 | 5.9 | | 0.6 | 37.3 | 37.7 | 21200 | 0.17 | 460 | 16 | 35 | | 123 |
SEL, BCb | 0.5 | 17 | | 3.5 | 90 | 190 | 43766 | 0.486 | 1100 | 75 | 91.3 | | 315 |
Backgroundc | 0.06 | 1.8 | 400 | 0.1 | 100 | 55 | 56300 | 0.07 | 900 | 75 | 14 | 135 | 70 |
Notes |
Bold values are above Threshold effect levels (TEL)
Interim freshwater sediment quality guidelines (ISQGs (CCME, [2]a
BC MOE Working Guidelines for Sediments [36]b
Kabata-Pendias & Mukherjee [19]c
Threshold effect levels (TELs), Probable effect levels (PEL), Lowest Effect Level (LEL), Severe Effect Level (SEL)
4.4 Contamination and Toxicity Assessment of Metals in Sediments
4.4.1 Enrichment Factor (EF)
The enrichment factors are presented in Table 5. According to the data, enrichment factors indicate natural weathering to moderate contamination with a range for Ag (0.06–0.09), Ba (0.22 to 2.45), Cr (0.30 to 2.63), Ni (0.44 to 1.92) and V (1.03 to 2.27) in the study area. EF for As at Bon Accord Creek (MVC5, EF = 7.19) shows severe contamination. King Creek (MVC9, EF = 2.02) and Beaver Creek (MVC33, EF = 3.87) showed moderate contamination whereas Bear Creek (MVC23, EF = 1.68) and Bolivar Creek (MVC25, EF = 1.54) show minimal contamination. The EF value for Cu showed severe contamination at Bon Accord Creek (MVC5, EF = 6.50) and Beaver Creek (MVC33, EF = 6.30). The EF for Mn was 8.30 at King Lake (MVC7) which indicates severe contamination. The EF for Pb recorded severe contamination at Bon Accord Creek (MVC5, EF = 8.08), Quibble Creek (MVC14, EF = 5.28) and Beaver Creek (MVC33, EF = 11.49). The rest of the sampling sites in terms of Cu, Mn and Pb, in the study area showed natural weathering to moderate contamination. The EF for Zn was the highest at Bon Accord Creek (MVC5, EF = 13.49) indicating severe contamination. Quibble Creek (MVC13, EF = 6.46), Hyland Creek (MVC17, EF = 6.96), Beaver Creek (MVC33, EF = 11.91) and Chubb Creek (MVC39, EF = 6.25) also recorded severe contamination. The EF shows Zn at the other sampling sites in the study area to be minimal to moderately contaminated. For Cd, EF shows extremely high contamination for Beaver Creek (MVC33) with a value of 122.00. Subsequently, Bon Accord Creek (MVC5), Bolivar Creek (MVC25) and King Creek (MVC8) had EF values of 73.79, 71.62 and 47.66 respectively and shows high level of contamination in the study area. EF values exceeding 20 in sediments are considered significantly enriched with metals and such high EF values are usually associated with anthropogenic inputs according to Silva Y.J, et al., [37] as cited by Nkinda et al., [34].
4.4.2 Pollution Load Index (PLI)
To evaluate the sediment pollution severity, PLI was used to find out the mutual pollution effect at different stations by different metals (Table 5). A PLI value close to 1 indicates metal loads near the background level, while values > 1 indicate pollution according to Cabrera et al., [38] as cited by Giri et al., [30]. According to Table 5, PLI values range from 0.50 to 1.09 in the study area. The joint pollution effect of different metals at different sampling locations in the study area is depicted in Fig. 3. King Creek (MVC9), Hyland Creek (MVC17), Bear Creek (MVC23), Dear Lake Brook (MVC32) and Chubb Creek (MVC39) had PLI values above 1 and indicate pollution. The rest of the sampling sites had PLI values < 1 indicating baseline level of pollution.
4.4.3 Contamination Factor
To quantify the magnitude of contamination by different metals, contamination factor (CF) was used (Table 6). The calculated CF values applied in this study were based on the four categories: CF values less than 1 (low degree of contamination); CF values starting from 1 but less than 3 (moderate degree of contamination); CF values ranging from 3 but less than 6 (considerable degree of contamination); and CF values greater than 6 (very high degree of contamination) [34]. With respect to the CF values for Cd and Ag, high degree of contamination in the sediments persist and may be indicative of anthropogenic influence in elemental loadings in the study area as stipulated by Gomez-Alvarez et al., [39]; Gajere & Okegye, [40] as cited by Nkinda., et al., [34].
Contamination factors for Ba, Cr, Cu, Fe, Ni and Mn show low to moderate contamination in the study area with the exception of Mn at King Lake (MVC7, CF = 5.7) which indicates considerable degree of contamination (Table 6). The CF for Zn at Bon Accord Creek (MVC5, CF = 6.09) and Beaver Creek (MVC33, CF = 9.44) were above the threshold limit of 6 and show high degree of contamination. King Creek (MVC9, CF = 3.13), Hyland Creek (MVC17, CF = 4.33) and Chubb Creek (MVC39, CF = 5.14) for Zn shows considerable degree of contamination in the study area (Table 6). The highest CF values for As were determined at Bon Accord Creek (MVC5, CF = 9.04) and Beaver Creek (MVC33, CF = 8.56). The CF value for Pb was also highest at Beaver Creek (MVC33, CF = 11.56), with a high degree of contamination. For As, CF values for King Creek (MVC9, CF = 5.70), Bear Creek (MVC23, CF = 3.23) and Bolivar Creek (CF = 4.17) shows moderate degree of contamination. CF values for Pb in the study area on the other hand shows moderate contamination at Bon Accord Creek (MVC5, CF = 4.63), Quibble Creek (MVC14, EF = 4.05) and Bear Creek (MVC23, EF = 4.9). The CF value for Cd (CF = 90.96) and Ag (68.45) was the highest at Beaver Creek (MVC33) in the study area. Bolivar Creek (MVC25) recorded CF values of 65.66 and 55.17 for Cd and Ag, respectively. King Creek (MVC8) recorded CF value of 27.15 for Cd and 42.12 for Ag in the present study. The CF for Cd at Bon Accord Creek (MVC5) was 31.3 and above the threshold limit of 6. The calculated contamination factors (Table 6) for the heavy metals in sediments in the study area are found to fall in the following sequences: Cd > Ag > As > Pb > Zn > Mn > Cu > Ba > Cr > Ni > V > Fe > Hg.
4.4.4 Geo-Accumulation Index (Igeo)
The sediment Igeo values for Ag and Cd in the study area were negative and indicate no contamination or enrichment above background value (Table 7). For As, Igeo values at Bon Accord Creek (MVC5, Igeo = 4.29) and Beaver Creek (MVC33, Igeo = 4.21) indicate high to highly contaminated sediment. At King Creek (MVC9, Igeo = 3.62) and Bolivar Creek (MVC25, Igeo = 3.17), Igeo values for As indicates highly contaminated sediment. At Bear Creek (MVC23, Igeo = 2.80) As indicates moderately to heavily contaminated level while Noons Creek (MVC45, Igeo = 1.41) indicates moderately contaminated level in the study area. The Igeo values for Ba, Cr, Cu, Fe, Mn, Ni, Pb, V and Zn represents extremely contaminated sediment and > 64-fold increase [20]. Hence these metals pose an environmental risk to sediment quality in the study area.
Table 5
Enrichment Factor of Metals in Creeks Sediments in Metro Vancouver
Sample | Ag | As | Ba | Cd | Cr | Cu | Fe | Hg | Mn | Ni | Pb | V | Zn | PLI |
MVC-1 | 0.00 | 0.00 | 1.46 | 0.00 | 1.03 | 1.86 | 1.00 | 0.00 | 1.06 | 0.97 | 1.28 | 1.4 | 3.73 | 0.82 |
MVC-2 | 0.00 | 0.00 | 1.09 | 0.00 | 0.89 | 1.33 | 1.00 | 0.00 | 1.63 | 1.47 | 1.24 | 1.31 | 3.14 | 0.95 |
MVC-3 | 0.00 | 0.00 | 1.53 | 0.00 | 1.10 | 1.47 | 1.00 | 0.00 | 1.41 | 1.92 | 2.23 | 1.61 | 3.64 | 0.85 |
MVC-4 | 0.00 | 0.00 | 1.23 | 0.00 | 1.97 | 1.72 | 1.00 | 0.00 | 1.34 | 0.00 | 1.88 | 1.84 | 1.11 | 0.00 |
MVC-5 | 0.00 | 7.19 | 0.60 | 73.79 | 1.51 | 6.50 | 1.00 | 0.00 | 0.85 | 0.00 | 8.08 | 1.56 | 13.49 | 0.00 |
MVC-6 | 0.00 | 0.00 | 1.28 | 0.00 | 0.89 | 0.94 | 1.00 | 0.00 | 0.89 | 0.44 | 0.8 | 1.45 | 1.49 | 0.50 |
MVC-7 | 0.00 | 0.00 | 1.34 | 0.00 | 2.05 | 0.39 | 1.00 | 0.00 | 8.30 | 1.51 | 0.48 | 1.44 | 2.11 | 0.77 |
MVC-8 | 0.08 | 0.00 | 0.53 | 47.66 | 0.96 | 1.69 | 1.00 | 0.00 | 1.12 | 1.18 | 1.25 | 1.5 | 3.18 | 0.70 |
MVC-9 | 0.00 | 2.02 | 0.80 | 0.00 | 0.58 | 0.82 | 1.00 | 0.00 | 2.45 | 1.52 | 0.73 | 1.03 | 3.08 | 1.09 |
MVC-10 | 0.00 | 0.00 | 1.36 | 0.00 | 0.88 | 0.91 | 1.00 | 0.00 | 1.92 | 1.31 | 0.9 | 1.5 | 2.59 | 0.72 |
MVC-11 | 0.00 | 0.00 | 1.40 | 0.00 | 0.75 | 1.48 | 1.00 | 0.00 | 1.07 | 0.78 | 1.07 | 1.44 | 2.92 | 0.76 |
MVC-12 | 0.00 | 0.00 | 1.48 | 0.00 | 1.10 | 1.41 | 1.00 | 0.00 | 0.84 | 0.87 | 3.00 | 1.66 | 3.44 | 0.70 |
MVC-13 | 0.00 | 0.00 | 1.03 | 0.00 | 0.96 | 3.68 | 1.00 | 0.00 | 1.08 | 0.70 | 2.12 | 1.51 | 6.46 | 0.94 |
MVC-14 | 0.00 | 0.00 | 1.17 | 0.00 | 1.80 | 1.48 | 1.00 | 0.00 | 0.87 | 0.00 | 5.28 | 1.65 | 2.95 | 0.00 |
MVC-15 | 0.00 | 0.00 | 1.30 | 0.00 | 1.99 | 2.33 | 1.00 | 0.00 | 0.84 | 1.44 | 1.63 | 1.65 | 4.58 | 0.84 |
MVC-16 | 0.00 | 0.00 | 1.32 | 0.00 | 0.97 | 1.94 | 1.00 | 0.00 | 1.00 | 0.00 | 3.16 | 1.51 | 4.39 | 0.00 |
MVC-17 | 0.00 | 0.00 | 1.25 | 0.00 | 0.89 | 3.05 | 1.00 | 0.00 | 1.69 | 1.46 | 2.41 | 1.47 | 6.96 | 1.06 |
MVC-18 | 0.00 | 0.00 | 1.08 | 0.00 | 1.06 | 0.66 | 1.00 | 0.00 | 1.00 | 0.50 | 1.00 | 1.60 | 1.82 | 0.58 |
MVC-19 | 0.00 | 0.00 | 1.44 | 0.00 | 2.63 | 0.75 | 1.00 | 0.00 | 1.16 | 1.20 | 1.01 | 1.42 | 2.67 | 0.68 |
MVC-20 | 0.00 | 0.00 | 1.21 | 0.00 | 1.15 | 0.93 | 1.00 | 0.00 | 0.91 | 0.00 | 3.47 | 1.64 | 2.65 | 0.00 |
MVC-21 | 0.00 | 0.00 | 1.25 | 0.00 | 1.02 | 1.24 | 1.00 | 0.00 | 1.93 | 1.52 | 0.99 | 1.47 | 3.06 | 0.83 |
MVC-22 | 0.00 | 0.00 | 1.51 | 0.00 | 1.01 | 0.56 | 1.00 | 0.00 | 0.96 | 0.76 | 1.36 | 1.45 | 2.36 | 0.50 |
MVC-23 | 0.00 | 1.68 | 0.91 | 0.00 | 1.16 | 1.88 | 1.00 | 0.00 | 0.92 | 1.30 | 5.60 | 1.57 | 3.12 | 1.03 |
MVC-24 | 0.00 | 0.00 | 1.07 | 0.00 | 0.66 | 0.79 | 1.00 | 0.00 | 1.44 | 1.21 | 1.48 | 1.23 | 4.04 | 0.77 |
MVC-25 | 0.06 | 1.54 | 0.22 | 71.62 | 0.47 | 1.54 | 1.00 | 0.00 | 0.60 | 0.87 | 0.90 | 0.87 | 3.06 | 0.76 |
MVC-26 | 0.00 | 0.00 | 1.26 | 0.00 | 1.25 | 2.21 | 1.00 | 0.00 | 0.93 | 0.47 | 3.49 | 1.68 | 4.03 | 0.76 |
MVC-27 | 0.00 | 0.00 | 1.54 | 0.00 | 1.28 | 1.91 | 1.00 | 0.00 | 0.77 | 0.00 | 0.96 | 2.27 | 1.64 | 0.00 |
MVC-28 | 0.00 | 0.00 | 1.42 | 0.00 | 0.93 | 1.27 | 1.00 | 0.00 | 1.10 | 0.95 | 1.10 | 1.63 | 3.84 | 0.67 |
MVC-29 | 0.00 | 0.00 | 1.19 | 0.00 | 1.09 | 1.35 | 1.00 | 0.00 | 1.00 | 1.00 | 0.91 | 1.53 | 2.73 | 0.74 |
MVC-30 | 0.00 | 0.00 | 1.55 | 0.00 | 1.04 | 1.56 | 1.00 | 0.00 | 1.21 | 0.59 | 1.89 | 1.70 | 2.81 | 0.61 |
MVC-31 | 0.00 | 0.00 | 1.34 | 0.00 | 0.75 | 1.01 | 1.00 | 0.00 | 0.93 | 0.88 | 1.00 | 1.42 | 2.00 | 0.64 |
MVC-32 | 0.00 | 0.00 | 1.05 | 0.00 | 0.62 | 2.16 | 1.00 | 0.00 | 2.04 | 1.31 | 2.05 | 1.38 | 3.27 | 1.06 |
MVC-33 | 0.09 | 3.87 | 0.19 | 122 | 0.51 | 6.30 | 1.00 | 0.00 | 1.36 | 0.00 | 11.49 | 1.09 | 11.91 | 0.00 |
MVC-34 | 0.00 | 0.00 | 1.14 | 0.00 | 0.45 | 0.69 | 1.00 | 0.00 | 1.81 | 0.86 | 0.72 | 1.26 | 1.90 | 0.76 |
MVC-35 | 0.00 | 0.00 | 1.60 | 0.00 | 0.89 | 0.77 | 1.00 | 0.00 | 1.46 | 0.58 | 1.05 | 1.36 | 2.02 | 0.53 |
MVC-36 | 0.00 | 0.00 | 1.46 | 0.00 | 0.62 | 1.05 | 1.00 | 0.00 | 1.27 | 0.87 | 0.95 | 1.50 | 2.75 | 0.69 |
MVC-37 | 0.00 | 0.00 | 1.50 | 0.00 | 0.73 | 1.26 | 1.00 | 0.00 | 1.61 | 0.00 | 2.11 | 1.34 | 2.86 | 0.00 |
MVC-38 | 0.00 | 0.00 | 1.33 | 0.00 | 0.72 | 2.00 | 1.00 | 0.00 | 0.85 | 0.91 | 2.04 | 1.27 | 2.69 | 0.83 |
MVC-39 | 0.00 | 0.00 | 0.90 | 0.00 | 0.54 | 3.44 | 1.00 | 0.00 | 0.79 | 0.83 | 2.64 | 0.90 | 6.25 | 1.05 |
MVC-40 | 0.00 | 0.00 | 1.26 | 0.00 | 0.35 | 0.91 | 1.00 | 0.00 | 1.04 | 0.51 | 0.49 | 1.37 | 1.23 | 0.53 |
MVC-41 | 0.00 | 0.00 | 1.31 | 0.00 | 0.53 | 1.17 | 1.00 | 0.00 | 1.25 | 0.00 | 0.88 | 1.23 | 2.25 | 0.00 |
MVC-42 | 0.00 | 0.00 | 0.90 | 0.00 | 0.35 | 1.02 | 1.00 | 0.00 | 1.22 | 0.83 | 0.34 | 1.27 | 1.75 | 0.78 |
MVC-43 | 0.00 | 0.00 | 1.11 | 0.00 | 0.49 | 0.95 | 1.00 | 0.00 | 1.42 | 0.90 | 0.35 | 1.22 | 1.50 | 0.73 |
MVC-44 | 0.00 | 0.00 | 1.14 | 0.00 | 0.39 | 0.48 | 1.00 | 0.00 | 1.05 | 0.56 | 0.79 | 1.54 | 0.96 | 0.62 |
MVC-45 | 0.00 | 0.00 | 0.88 | 0.00 | 0.34 | 0.51 | 1.00 | 0.00 | 1.81 | 1.30 | 0.88 | 1.36 | 1.44 | 0.90 |
MVC-46 | 0.00 | 0.00 | 2.45 | 0.00 | 0.60 | 0.86 | 1.00 | 0.00 | 1.42 | 0.00 | 1.50 | 1.20 | 1.79 | 0.00 |
MVC-47 | 0.00 | 0.00 | 0.69 | 0.00 | 0.30 | 0.72 | 1.00 | 0.00 | 0.60 | 1.74 | 0.60 | 1.26 | 0.91 | 0.87 |
Table 6
Contamination Factor of Metals in Creeks Sediments in Metro Vancouver
Sample | Ag | As | Ba | Cd | Cr | Cu | Fe | Hg | Mn | Ni | Pb | V | Zn |
MVC-1 | 0.00 | 0.00 | 1.50 | 0.00 | 0.62 | 0.62 | 0.59 | 0.00 | 0.77 | 0.40 | 1.01 | 0.66 | 2.34 |
MVC-2 | 0.00 | 0.00 | 1.33 | 0.00 | 0.64 | 0.52 | 0.70 | 0.00 | 1.41 | 0.71 | 1.17 | 0.73 | 2.33 |
MVC-3 | 0.00 | 0.00 | 1.38 | 0.00 | 0.59 | 0.43 | 0.52 | 0.00 | 0.91 | 0.69 | 1.56 | 0.67 | 2.01 |
MVC-4 | 0.00 | 0.00 | 0.55 | 0.00 | 0.52 | 0.25 | 0.26 | 0.00 | 0.43 | 0.00 | 0.66 | 0.38 | 0.31 |
MVC-5 | 0.00 | 9.04 | 0.44 | 31.3 | 0.66 | 1.56 | 0.42 | 0.00 | 0.44 | 0.00 | 4.63 | 0.53 | 6.09 |
MVC-6 | 0.00 | 0.00 | 1.15 | 0.00 | 0.47 | 0.27 | 0.51 | 0.00 | 0.56 | 0.16 | 0.55 | 0.59 | 0.82 |
MVC-7 | 0.00 | 0.00 | 1.30 | 0.00 | 1.16 | 0.12 | 0.55 | 0.00 | 5.70 | 0.59 | 0.36 | 0.64 | 1.25 |
MVC-8 | 42.12 | 0.00 | 0.53 | 27.15 | 0.56 | 0.55 | 0.57 | 0.00 | 0.79 | 0.47 | 0.96 | 0.68 | 1.93 |
MVC-9 | 0.00 | 5.70 | 1.33 | 0.00 | 0.56 | 0.44 | 0.95 | 0.00 | 2.89 | 1.01 | 0.94 | 0.78 | 3.13 |
MVC-10 | 0.00 | 0.00 | 1.32 | 0.00 | 0.50 | 0.29 | 0.55 | 0.00 | 1.32 | 0.51 | 0.67 | 0.67 | 1.53 |
MVC-11 | 0.00 | 0.00 | 1.52 | 0.00 | 0.48 | 0.52 | 0.62 | 0.00 | 0.83 | 0.34 | 0.90 | 0.72 | 1.94 |
MVC-12 | 0.00 | 0.00 | 1.25 | 0.00 | 0.54 | 0.38 | 0.48 | 0.00 | 0.50 | 0.29 | 1.95 | 0.64 | 1.77 |
MVC-13 | 0.00 | 0.00 | 1.07 | 0.00 | 0.59 | 1.25 | 0.60 | 0.00 | 0.80 | 0.29 | 1.72 | 0.72 | 4.12 |
MVC-14 | 0.00 | 0.00 | 1.16 | 0.00 | 1.04 | 0.48 | 0.56 | 0.00 | 0.61 | 0.00 | 4.05 | 0.75 | 1.78 |
MVC-15 | 0.00 | 0.00 | 1.16 | 0.00 | 1.04 | 0.67 | 0.51 | 0.00 | 0.53 | 0.51 | 1.13 | 0.67 | 2.49 |
MVC-16 | 0.00 | 0.00 | 1.17 | 0.00 | 0.51 | 0.56 | 0.51 | 0.00 | 0.63 | 0.00 | 2.17 | 0.61 | 2.38 |
MVC-17 | 0.00 | 0.00 | 1.28 | 0.00 | 0.53 | 1.01 | 0.58 | 0.00 | 1.22 | 0.60 | 1.90 | 0.69 | 4.33 |
MVC-18 | 0.00 | 0.00 | 1.08 | 0.00 | 0.62 | 0.21 | 0.57 | 0.00 | 0.78 | 0.20 | 0.77 | 0.73 | 1.11 |
MVC-19 | 0.00 | 0.00 | 1.27 | 0.00 | 1.37 | 0.21 | 0.51 | 0.00 | 0.72 | 0.42 | 0.69 | 0.57 | 1.44 |
MVC-20 | 0.00 | 0.00 | 0.95 | 0.00 | 0.53 | 0.24 | 0.45 | 0.00 | 0.50 | 0.00 | 2.11 | 0.59 | 1.27 |
MVC-21 | 0.00 | 0.00 | 1.29 | 0.00 | 0.62 | 0.41 | 0.59 | 0.00 | 1.41 | 0.63 | 0.79 | 0.70 | 1.92 |
MVC-22 | 0.00 | 0.00 | 1.18 | 0.00 | 0.46 | 0.14 | 0.45 | 0.00 | 0.53 | 0.24 | 0.82 | 0.52 | 1.12 |
MVC-23 | 0.00 | 3.23 | 1.03 | 0.00 | 0.77 | 0.69 | 0.64 | 0.00 | 0.74 | 0.59 | 4.90 | 0.81 | 2.15 |
MVC-24 | 0.00 | 0.00 | 1.15 | 0.00 | 0.42 | 0.28 | 0.62 | 0.00 | 1.10 | 0.52 | 1.23 | 0.61 | 2.66 |
MVC-25 | 55.17 | 4.17 | 0.35 | 65.66 | 0.44 | 0.80 | 0.91 | 0.00 | 0.68 | 0.55 | 1.11 | 0.64 | 2.98 |
MVC-26 | 0.00 | 0.00 | 1.12 | 0.00 | 0.65 | 0.64 | 0.51 | 0.00 | 0.58 | 0.17 | 2.40 | 0.68 | 2.18 |
MVC-27 | 0.00 | 0.00 | 1.26 | 0.00 | 0.62 | 0.51 | 0.47 | 0.00 | 0.45 | 0.00 | 0.61 | 0.85 | 0.82 |
MVC-28 | 0.00 | 0.00 | 1.27 | 0.00 | 0.49 | 0.37 | 0.51 | 0.00 | 0.70 | 0.34 | 0.76 | 0.67 | 2.09 |
MVC-29 | 0.00 | 0.00 | 1.25 | 0.00 | 0.67 | 0.46 | 0.60 | 0.00 | 0.75 | 0.42 | 0.74 | 0.74 | 1.75 |
MVC-30 | 0.00 | 0.00 | 1.21 | 0.00 | 0.48 | 0.4 | 0.45 | 0.00 | 0.67 | 0.19 | 1.15 | 0.61 | 1.34 |
MVC-31 | 0.00 | 0.00 | 1.36 | 0.00 | 0.45 | 0.33 | 0.58 | 0.00 | 0.67 | 0.36 | 0.78 | 0.66 | 1.24 |
MVC-32 | 0.00 | 0.00 | 1.31 | 0.00 | 0.45 | 0.87 | 0.71 | 0.00 | 1.80 | 0.65 | 1.98 | 0.79 | 2.49 |
MVC-33 | 68.45 | 8.56 | 0.25 | 90.96 | 0.39 | 2.65 | 0.74 | 0.00 | 1.25 | 0.00 | 11.56 | 0.65 | 9.44 |
MVC-34 | 0.00 | 0.00 | 1.52 | 0.00 | 0.35 | 0.3 | 0.76 | 0.00 | 1.71 | 0.46 | 0.74 | 0.77 | 1.54 |
MVC-35 | 0.00 | 0.00 | 1.34 | 0.00 | 0.44 | 0.21 | 0.48 | 0.00 | 0.86 | 0.19 | 0.68 | 0.52 | 1.03 |
MVC-36 | 0.00 | 0.00 | 1.50 | 0.00 | 0.37 | 0.35 | 0.59 | 0.00 | 0.92 | 0.36 | 0.75 | 0.71 | 1.72 |
MVC-37 | 0.00 | 0.00 | 1.28 | 0.00 | 0.36 | 0.35 | 0.48 | 0.00 | 0.96 | 0.00 | 1.39 | 0.52 | 1.48 |
MVC-38 | 0.00 | 0.00 | 1.50 | 0.00 | 0.47 | 0.73 | 0.64 | 0.00 | 0.67 | 0.41 | 1.78 | 0.66 | 1.84 |
MVC-39 | 0.00 | 0.00 | 1.21 | 0.00 | 0.43 | 1.50 | 0.77 | 0.00 | 0.75 | 0.44 | 2.75 | 0.56 | 5.14 |
MVC-40 | 0.00 | 0.00 | 1.41 | 0.00 | 0.23 | 0.33 | 0.64 | 0.00 | 0.83 | 0.23 | 0.43 | 0.70 | 0.84 |
MVC-41 | 0.00 | 0.00 | 1.23 | 0.00 | 0.29 | 0.36 | 0.53 | 0.00 | 0.83 | 0.00 | 0.64 | 0.53 | 1.28 |
MVC-42 | 0.00 | 0.00 | 1.43 | 0.00 | 0.32 | 0.53 | 0.91 | 0.00 | 1.38 | 0.53 | 0.42 | 0.93 | 1.69 |
MVC-43 | 0.00 | 0.00 | 1.57 | 0.00 | 0.40 | 0.44 | 0.81 | 0.00 | 1.42 | 0.51 | 0.38 | 0.79 | 1.29 |
MVC-44 | 0.00 | 0.00 | 1.53 | 0.00 | 0.30 | 0.21 | 0.76 | 0.00 | 1.00 | 0.30 | 0.82 | 0.95 | 0.78 |
MVC-45 | 0.00 | 1.23 | 1.46 | 0.00 | 0.33 | 0.27 | 0.95 | 0.00 | 2.14 | 0.86 | 1.14 | 1.04 | 1.46 |
MVC-46 | 0.00 | 0.00 | 1.69 | 0.00 | 0.24 | 0.19 | 0.39 | 0.00 | 0.69 | 0.00 | 0.80 | 0.38 | 0.75 |
MVC-47 | 0.00 | 0.00 | 1.35 | 0.00 | 0.34 | 0.46 | 1.11 | 0.00 | 0.83 | 1.36 | 0.91 | 1.12 | 1.09 |
Table 7
Geo-accumulation of Metals in Creeks Sediments in Metro Vancouver
Sample | Ag | As | Ba | Cd | Cr | Cu | Fe | Hg | Mn | Ni | Pb | V | Zn |
MVC-1 | 0.00 | 0.00 | 17.29 | 0.00 | 12.01 | 10.29 | 30.21 | 0.00 | 18.67 | 10.54 | 7.05 | 12.97 | 12.90 |
MVC-2 | 0.00 | 0.00 | 17.12 | 0.00 | 12.05 | 10.05 | 30.45 | 0.00 | 19.53 | 11.39 | 7.26 | 13.11 | 12.90 |
MVC-3 | 0.00 | 0.00 | 17.17 | 0.00 | 11.93 | 9.76 | 30.02 | 0.00 | 18.90 | 11.34 | 7.67 | 12.99 | 12.68 |
MVC-4 | 0.00 | 0.00 | 15.85 | 0.00 | 11.77 | 8.99 | 29.02 | 0.00 | 17.82 | 0.00 | 6.42 | 12.18 | 9.96 |
MVC-5 | 0.00 | 4.29 | 15.52 | -2.26 | 12.09 | 11.62 | 29.73 | 0.00 | 17.87 | 0.00 | 9.24 | 12.65 | 14.28 |
MVC-6 | 0.00 | 0.00 | 16.91 | 0.00 | 11.60 | 9.10 | 30.01 | 0.00 | 18.21 | 9.22 | 6.18 | 12.82 | 11.38 |
MVC-7 | 0.00 | 0.00 | 17.08 | 0.00 | 12.92 | 7.94 | 30.12 | 0.00 | 21.55 | 11.10 | 5.55 | 12.92 | 11.99 |
MVC-8 | -3.31 | 0.00 | 15.78 | -2.47 | 11.86 | 10.10 | 30.16 | 0.00 | 18.70 | 10.78 | 6.97 | 13.01 | 12.62 |
MVC-9 | 0.00 | 3.62 | 17.11 | 0.00 | 11.87 | 9.80 | 30.90 | 0.00 | 20.57 | 11.89 | 6.94 | 13.21 | 13.32 |
MVC-10 | 0.00 | 0.00 | 17.1 | 0.00 | 11.71 | 9.18 | 30.13 | 0.00 | 19.45 | 10.90 | 6.46 | 12.98 | 12.29 |
MVC-11 | 0.00 | 0.00 | 17.31 | 0.00 | 11.63 | 10.04 | 30.29 | 0.00 | 18.77 | 10.30 | 6.88 | 13.09 | 12.63 |
MVC-12 | 0.00 | 0.00 | 17.02 | 0.00 | 11.82 | 9.59 | 29.92 | 0.00 | 18.04 | 10.10 | 8.00 | 12.92 | 12.49 |
MVC-13 | 0.00 | 0.00 | 16.81 | 0.00 | 11.94 | 11.30 | 30.23 | 0.00 | 18.72 | 10.09 | 7.81 | 13.10 | 13.72 |
MVC-14 | 0.00 | 0.00 | 16.92 | 0.00 | 12.76 | 9.91 | 30.15 | 0.00 | 18.32 | 0.00 | 9.05 | 13.15 | 12.51 |
MVC-15 MVC-16 | 0.00 0.00 | 0.00 0.00 | 16.92 16.93 | 0.00 0.00 | 12.76 11.72 | 10.41 10.14 | 30.00 30.00 | 0.00 0.00 | 18.13 18.37 | 10.91 0.00 | 7.20 8.15 | 13.00 12.86 | 12.99 12.93 |
MVC-17 | 0.00 | 0.00 | 17.06 | 0.00 | 11.80 | 10.99 | 30.20 | 0.00 | 19.33 | 11.13 | 7.96 | 13.02 | 13.79 |
MVC-18 | 0.00 | 0.00 | 16.82 | 0.00 | 12.01 | 8.75 | 30.17 | 0.00 | 18.68 | 9.54 | 6.66 | 13.12 | 11.83 |
MVC-19 | 0.00 | 0.00 | 17.05 | 0.00 | 13.15 | 8.75 | 29.99 | 0.00 | 18.58 | 10.63 | 6.50 | 12.77 | 12.20 |
MVC-20 | 0.00 | 0.00 | 16.63 | 0.00 | 11.79 | 8.91 | 29.82 | 0.00 | 18.06 | 0.00 | 8.11 | 12.81 | 12.02 |
MVC-21 | 0.00 | 0.00 | 17.07 | 0.00 | 12.01 | 9.71 | 30.21 | 0.00 | 19.54 | 11.20 | 6.69 | 13.05 | 12.62 |
MVC-22 | 0.00 | 0.00 | 16.94 | 0.00 | 11.58 | 8.15 | 29.81 | 0.00 | 18.13 | 9.79 | 6.74 | 12.62 | 11.84 |
MVC-23 | 0.00 | 2.80 | 16.74 | 0.00 | 12.32 | 10.44 | 30.34 | 0.00 | 18.60 | 11.10 | 9.32 | 13.27 | 12.78 |
MVC-24 | 0.00 | 0.00 | 16.91 | 0.00 | 11.44 | 9.13 | 30.28 | 0.00 | 19.19 | 10.93 | 7.33 | 12.85 | 13.09 |
MVC-25 MVC-26 MVC-27 | -2.92 0.00 0.00 | 3.17 0.00 0.00 | 15.18 16.87 17.04 | -1.19 0.00 0.00 | 11.53 12.08 12.00 | 10.66 10.33 10.00 | 30.84 29.99 29.88 | 0.00 0.00 0.00 | 18.48 18.26 17.89 | 11.02 9.29 0.00 | 7.18 8.29 6.31 | 12.92 13.01 13.34 | 13.25 12.80 11.39 |
MVC-28 | 0.00 | 0.00 | 17.05 | 0.00 | 11.66 | 9.54 | 30.00 | 0.00 | 18.52 | 10.31 | 6.63 | 12.98 | 12.74 |
MVC-29 | 0.00 | 0.00 | 17.02 | 0.00 | 12.12 | 9.86 | 30.24 | 0.00 | 18.62 | 10.62 | 6.59 | 13.13 | 12.48 |
MVC-30 | 0.00 | 0.00 | 16.98 | 0.00 | 11.64 | 9.64 | 29.81 | 0.00 | 18.46 | 9.44 | 7.23 | 12.85 | 12.10 |
MVC-31 | 0.00 | 0.00 | 17.15 | 0.00 | 11.54 | 9.39 | 30.19 | 0.00 | 18.46 | 10.39 | 6.68 | 12.97 | 11.98 |
MVC-32 | 0.00 | 0.00 | 17.09 | 0.00 | 11.56 | 10.78 | 30.49 | 0.00 | 19.89 | 11.26 | 8.01 | 13.23 | 12.99 |
MVC-33 | -2.61 | 4.21 | 14.67 | -0.72 | 11.35 | 12.39 | 30.55 | 0.00 | 19.36 | 0.00 | 10.56 | 12.95 | 14.91 |
MVC-34 | 0.00 | 0.00 | 17.31 | 0.00 | 11.20 | 9.24 | 30.58 | 0.00 | 19.82 | 10.75 | 6.60 | 13.20 | 12.30 |
MVC-35 | 0.00 | 0.00 | 17.13 | 0.00 | 11.51 | 8.71 | 29.91 | 0.00 | 18.83 | 9.51 | 6.47 | 12.63 | 11.72 |
MVC-36 | 0.00 | 0.00 | 17.29 | 0.00 | 11.29 | 9.46 | 30.21 | 0.00 | 18.93 | 10.39 | 6.62 | 13.07 | 12.46 |
MVC-37 | 0.00 | 0.00 | 17.05 | 0.00 | 11.25 | 9.45 | 29.93 | 0.00 | 18.99 | 0.00 | 7.50 | 12.62 | 12.24 |
MVC-38 | 0.00 | 0.00 | 17.29 | 0.00 | 11.62 | 10.53 | 30.34 | 0.00 | 18.47 | 10.58 | 7.86 | 12.96 | 12.56 |
MVC-39 | 0.00 | 0.00 | 16.98 | 0.00 | 11.47 | 11.57 | 30.60 | 0.00 | 18.63 | 10.7 | 8.49 | 12.72 | 14.03 |
MVC-40 | 0.00 | 0.00 | 17.20 | 0.00 | 10.57 | 9.38 | 30.33 | 0.00 | 18.77 | 9.74 | 5.80 | 13.06 | 11.42 |
MVC-41 | 0.00 | 0.00 | 17.00 | 0.00 | 10.93 | 9.49 | 30.07 | 0.00 | 18.77 | 0.00 | 6.38 | 12.65 | 12.03 |
MVC-42 | 0.00 | 0.00 | 17.22 | 0.00 | 11.08 | 10.05 | 30.84 | 0.00 | 19.51 | 10.95 | 5.78 | 13.46 | 12.43 |
MVC-43 | 0.00 | 0.00 | 17.35 | 0.00 | 11.39 | 9.78 | 30.67 | 0.00 | 19.55 | 10.89 | 5.64 | 13.22 | 12.04 |
MVC-44 | 0.00 | 0.00 | 17.32 | 0.00 | 10.98 | 8.72 | 30.59 | 0.00 | 19.04 | 10.13 | 6.74 | 13.49 | 11.32 |
MVC-45 | 0.00 | 1.41 | 17.25 | 0.00 | 11.10 | 9.10 | 30.90 | 0.00 | 20.14 | 11.66 | 7.21 | 13.63 | 12.22 |
MVC-46 | 0.00 | 0.00 | 17.46 | 0.00 | 10.65 | 8.60 | 29.63 | 0.00 | 18.51 | 0.00 | 6.71 | 12.16 | 11.26 |
MVC-47 | 0.00 | 0.00 | 17.14 | 0.00 | 11.16 | 9.85 | 31.13 | 0.00 | 18.77 | 12.32 | 6.89 | 13.74 | 11.80 |
4.5 Principal Component Analysis (PCA)/Factor Analysis (FA)
Correlation among the heavy metals in the sediments and the results of PCA are provided in Tables 8, 9 and 10. PCA was adopted to assist in the interpretation of elemental data. This powerful method allows identifying the different groups of metals that correlate and thus can be considered as having a similar behavior and common origin [41]. The number of significant principal components is selected on the basis of Kaiser criterion with eigenvalue higher than 1 [17].
Four factors were discriminated based on the Kaiser criterion and explain 76.61% of the total variance in the study area (Table 7). The first factor has high loadings for Fe, Ni and V. PC1 may be associated with the earth’s crust and the geological formation of the study area [30]. These variables were demonstrated to be correlated (Table 8). PC2 was negatively loaded with Ba and positively loaded with Cu, Pb and Zn that explained 22.20% of the total variance. The negative loading for Ba may suggest a different origin and its loading in the sediment samples in the study area was influenced by different factors compared to Cu, Pb and Zn. From Table 8, it could be observed that Cu, Pb and Zn were correlated. This component appears to be from anthropogenic sources such as industrial wastes and vehicular pollution. Barium is reported to be associated with many industries like manufacture of alloys, paints, soaps, paper, rubber, glass, ceramics, television picture tubes, brick and tile refractories. Barium is also present in fuel additives and in fillers [32, 42]. According to Cheng & Hu [43] as cited by Giri et al., [30], Pb is known to be introduced into the environment by anthropogenic activities like industrial uses and inadequate or inappropriate municipal water treatment. Lead is also used for batteries, fuel tanks, solder, seals, bearings, and wheel weights according to Sander et al., [44] as cited by Giri et al., [30]. Zinc is known to be used in galvanizing on iron products, in alloys, rubber, glazes, enamels, paper and glass [45]. Zinc, typically as zinc oxide (ZnO) particles, is also added to tire rubber to aid in the vulcanization process [46, 47]. Copper on the other hand is used in electrical wiring, wiring in cars roofing, plumbing, and industrial machinery [48].
The third component which is PC3 represents 12.55% of the total variance with high loadings on pH, TDS and conductivity. Moderately high positive correlation can be observed between pH, EC and TDS and these variables were demonstrated to be correlated (Table 8). PC3 thus can be interpreted as water mineralization of the creeks, physical, chemical and biological activities [49, 50]. PC4 explains 11.02% of the total variance and has high loadings for Cr and Mn. PC4 represents domestic effluent discharges which may contain high levels of Cr and Mn that contaminate aquatic environments.
Table 8
Pearson correlation matrix between different metals in creek sediment in Metro Vancouver (n = 47) collected in 2023. The bold values indicate a statistically significant correlation
| Ba | Cr | Cu | Fe | Mn | Ni | Pb | V | Zn | pH | TDS | Con |
Ba | 1.000 | | | | | | | | | | | |
Cr | − .179 | 1.000 | | | | | | | | | | |
Cu | − .255 | − .052 | 1.000 | | | | | | | | | |
Fe | .079 | − .392 | .178 | 1.000 | | | | | | | | |
Mn | .181 | .277 | − .210 | .226 | 1.000 | | | | | | | |
Ni | .067 | .005 | .091 | .722 | .375 | 1.000 | | | | | | |
Pb | − .232 | .096 | .571 | − .036 | − .212 | .060 | 1.000 | | | | | |
V | .275 | − .316 | − .041 | .765 | .161 | .621 | − .002 | 1.000 | | | | |
Zn | − .276 | .062 | .870 | .120 | − .036 | .171 | .487 | − .176 | 1.000 | | | |
pH | .083 | .085 | .037 | − .352 | − .070 | − .236 | − .118 | − .416 | .144 | 1.000 | | |
TDS | − .146 | − .015 | .430 | − .134 | − .287 | − .219 | .247 | − .392 | .397 | .460 | 1.000 | |
Con | − .170 | − .031 | .462 | − .120 | − .262 | − .197 | .279 | − .375 | .409 | .450 | .975 | 1.000 |
Table 9
Extraction values of the total variance using PCA for 12 parameters between different metals in creek sediment and physicochemical parameters in surface water in Metro Vancouver
Component | Initial Eigenvalues | Extraction Sums of Squared Loadings |
Total | % of Variance | Cumulative % | Total | % of Variance | Cumulative % |
1 | 3.699 | 30.826 | 30.826 | 3.699 | 30.826 | 30.826 |
2 | 2.665 | 22.208 | 53.034 | 2.665 | 22.208 | 53.034 |
3 | 1.506 | 12.552 | 65.586 | 1.506 | 12.552 | 65.586 |
4 | 1.323 | 11.026 | 76.612 | 1.323 | 11.026 | 76.612 |
Table 10
Loadings of 12 experimental variables on four significant principal components in creek sediment and physicochemical parameters in surface water in Metro Vancouver
| Component |
| 1 | 2 | 3 | 4 |
Ba | .294 | − .601 | .140 | − .034 |
Cr | − .371 | .177 | − .067 | .781 |
Cu | .200 | .815 | .345 | − .102 |
Fe | .925 | .058 | − .091 | − .112 |
Mn | .348 | − .238 | − .066 | .766 |
Ni | .820 | .109 | − .121 | .315 |
Pb | .003 | .775 | .017 | − .080 |
V | .816 | − .113 | − .348 | − .162 |
Zn | .172 | .772 | .387 | .138 |
pH | − .262 | − .215 | .746 | .143 |
TDS | − .138 | .279 | .864 | − .165 |
Con | − .115 | .309 | .858 | − .160 |
Extraction Method: Principal Component Analysis. Rotation Method: Varimax with Kaiser Normalization. The bold values indicate a statistically significant correlation. |
4.6 Cluster Analysis
Cluster analysis grouped variables into clusters on the basis of similarities or dissimilarities such that each cluster represents a specific process in the system. Unlike PCA that normally uses only two or three PCs for display purposes, cluster analysis uses all the variance or information contained in the original data set. In this study, the hierarchical cluster analysis (HCA) was applied to the raw data. Two distinct clusters are visible from the results of the HCA (Fig. 4). These groups, respectively, represent the effects of two main factors in the study area.: anthropogenic and natural factors. Group 1 comprises Pb, pH, Cu, Ni, Cr, V, Zn and TDS which represents anthropogenic activities affecting the sediment quality in the study area. Sediment particles can carry toxic industrial and domestic effluents in the form of compounds and may have negative impact on aquatic organisms. Cluster 2 comprises EC, Ba, Mn and Fe and reflects the natural weathering of rocks enriching the study area with these elements.