Heavy and less common metals in rainwater and the kinetics of the oxidation of hydrogen sulfide by oxygen in rainwater medium
As a sequel to our recent study on the oxidation by O 2 , i. e., autoxidation of dissolved hydrogen sulfide, H 2 S, in aqueous medium, we present here the results of a similar study in rain water medium. The rainwater sampling was done sequentially for four years (2016–2019). In all 67 samples of ra...
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Veröffentlicht in: | Environmental monitoring and assessment 2023-06, Vol.195 (6), p.762-762, Article 762 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | As a sequel to our recent study on the oxidation by O
2
, i. e., autoxidation of dissolved hydrogen sulfide, H
2
S, in aqueous medium, we present here the results of a similar study in rain water medium. The rainwater sampling was done sequentially for four years (2016–2019). In all 67 samples of rainwater were collected on event basis during monsoon period (June-October) in and around the Campus of University of Rajasthan, Jaipur (26°50̛ N-75°52̛ E), which is situated in a semi-arid region adjacent to the Thar Desert in the North-Western part of the India having an annual average rainfall of 54 cm. ICP-MS technique was used in the analysis of rainwater and more than 30 metals were detected, which included transition metals, rare earths, less common metals. Beryllium, vanadium, silver, selenium, manganese, cerium, gallium, yttrium, barium, cesium, copper, rubidium, arsenic, lanthanum, cadmium, lead, uranium and bismuth were common to all rain water samples.
H
2
S oxidation by dissolved oxygen was studied in rainwater as well as in laboratory water media for comparison. The kinetics rate law was: -d[O
2
]/dt = k
1
K
1
[H
+
][S][O
2
]
t
/( [H
+
]
2
+ K
1
[H
+
] + K
1
K
2
), where K
1
is first dissociation constant of H
2
S and k
1
is the rate constant for the dominant reaction step:
HS
−
+ O
2
→ products. |
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ISSN: | 0167-6369 1573-2959 |
DOI: | 10.1007/s10661-023-11374-8 |