Hydrogen peroxide formation: The interaction of ultraviolet radiation and dissolved organic carbon in lake waters along a 43–75°N gradient
Hydrogen peroxide (H 2 O 2 ) formation rates (nM h −1 ), photoproductive capacity (nM W −1 h −1 m −2 ), and H 2 O 2 formation efficiency ( ϕ H 2 O 2 ) were measured on water samples exposed to a standard light source with a spectral composition similar to natural sunlight. Samples were from lakes an...
| Published in: | Limnology and Oceanography |
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| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
1996
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.4319/lo.1996.41.3.0540 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1996.41.3.0540 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1996.41.3.0540 |
| Summary: | Hydrogen peroxide (H 2 O 2 ) formation rates (nM h −1 ), photoproductive capacity (nM W −1 h −1 m −2 ), and H 2 O 2 formation efficiency ( ϕ H 2 O 2 ) were measured on water samples exposed to a standard light source with a spectral composition similar to natural sunlight. Samples were from lakes and wetlands with varying levels of dissolved organic C (DOC), P, Fe, Ca, and pH. The relationship between H 2 O 2 formation rates and DOC was a power function (H 2 O 2 = 49.65 DOC 1.71 r 2 = 0.94), whereas the relationships between formation rates and DOC fluorescence (DOCFL) (H 2 O 2 = 118.32 + 33.06 DOCFL; r 2 = 0.98) and absorption coefficients at 310 ( K a 310 ) were linear (H 2 O 2 = 185.0 + 55.50 K a 310 r 2 = 0.91). ϕ H 2 O 2 was independent of DOC ( r 2 = 0.12). Apparent quantum yields decreased with increasing wavelengths (300–400 nm). However, when apparent quantum yields were corrected with solar irradiance data, values were greatest in the UV‐A (320–400 nm) region. The patterns observed were consistent for samples from temperate to arctic regions. |
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