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Hydrogen peroxide formation: The interaction of ultraviolet radiation and dissolved organic carbon in lake waters along a 43–75°N gradient
Author(s) -
Scully N. M.,
McQueen D. J.,
Lean D. R. S.
Publication year - 1996
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.4319/lo.1996.41.3.0540
Subject(s) - dissolved organic carbon , hydrogen peroxide , chemistry , irradiance , colored dissolved organic matter , analytical chemistry (journal) , absorption (acoustics) , environmental chemistry , phytoplankton , materials science , organic chemistry , quantum mechanics , nutrient , composite material , physics
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.