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. 2019 Mar 27;4(3):5915–5922. doi: 10.1021/acsomega.9b00312

Table 1. Detection of Hg2+, Co2+, Fe2+, and Fe3+ in Natural Water Samples after Adding Standard Concentration of the Corresponding Metal Ions.

    Hg2+a
Co2+a
Fe2+a
Fe3+a
samples spiked/ppb found/ppb RDS% ICP-AES found/ppb RDS% ICP-AES found/ppb RDS% ICP-AES found/ppb RDS% ICP-AES
tap water blank b                      
30.0 26.5 6.4 31.9 28.5 4.8 32.1 31.5 4.6 27.8 28.9 6.1 26.7
100.0 97.4 3.1 104.3 97.6 2.9 92.4 97.3 3.1 94.5 92.1 2.9 109.2
300.0 317.4 2.9 302.6 291.3 1.7 278.3 292.0 2.0 278.3 311.2 1.8 284.4
Yangtze River water blank     1.8 0.9 10.7   0.8 11.5 2.5c     2.5c
30.0 25.4 7.1 29.1 27.9 5.1 25.9 32.1 3.8 32.7 31.3 8.3 27.9
100.0 101.2 3.2 105.4 98.4 2.7 91.3 102.5 1.7 105.5 111.2 3.2 102.6
300.0 329.9 1.9 305.6 287.5 2.2 264.7 314.0 1.3 308.7 317.4 2.7 315.4
Jianghan Plain groundwater blank     2.6 1.4 9.4 2.3 1.6 9.1 3.7c     3.7c
30.0 25.7 7.5 36.5 32.2 2.5 31.0 27.4 3.5 32.4 31.2 7.4 31.9
100.0 104.5 3.7 110.2 104.3 1.6 97.5 110.1 1.4 106.5 98.7 2.3 107.6
300.0 335.8 2.6 308.7 291.4 1.0 271.6 325.6 0.9 319.4 308.9 2.0 322.2
a

Average of three measurements.

b

Below the detection limit.

c

Specified speciation cannot be measured and the values are the total iron concentration.