Photochemical production of dissolved inorganic carbon from suwannee river humic acid

Xuejun Wang; Tao Lou; Huixiang Xie

doi:10.1007/s00343-009-9156-5

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Photochemical production of dissolved inorganic carbon from suwannee river humic acid

OriginalPaper | Updated：2023-05-16

- Photochemical production of dissolved inorganic carbon from suwannee river humic acid
- Photochemical production of dissolved inorganic carbon from suwannee river humic acid
- 海洋湖沼学报（英文） 2009年27卷第3期页码：570-573
- Affiliations：
  
  1. College of Chemistry Chemical Engineering & Environmental Science Qingdao University
  2. Institut des sciences de la mer de Rimouski Université du Québec à Rimouski
- Author bio：
- Funds：
  
  Supported by the National Science and Engineering Research Committee of Canada (No.213327)
- DOI：10.1007/s00343-009-9156-5
  中图分类号：
- 网络首发：2009-11-07，
  
  纸质出版：2009
- Accepted：
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Photochemical production of dissolved inorganic carbon from suwannee river humic acid[J]. 海洋湖沼学报（英文）, 2009,27(3):570-573.

Wang, X., Lou, T. & Xie, H. Photochemical production of dissolved inorganic carbon from suwannee river humic acid., Chin. J. Ocean. Limnol. 27, 570–573 (2009). https://doi.org/10.1007/s00343-009-9156-5
Photochemical production of dissolved inorganic carbon from suwannee river humic acid[J]. 海洋湖沼学报（英文）, 2009,27(3):570-573. DOI： 10.1007/s00343-009-9156-5.

Wang, X., Lou, T. & Xie, H. Photochemical production of dissolved inorganic carbon from suwannee river humic acid., Chin. J. Ocean. Limnol. 27, 570–573 (2009). https://doi.org/10.1007/s00343-009-9156-5 DOI：

摘要

Abstract

The photochemical mineralization of dissolved organic carbon (DOC) to dissolved inorganic carbon (DIC) is a key process in carbon cycling. Using a Suntest CPS solar simulator

Suwannee River humic acid (SRHA) was photooxidated to examine the effects of O2 levels

the wavelength of incident light

and the concentration of Fe on the photoproduction of DIC. Increasing the O2 abundance enhanced photodegradation of SRHA. The rate of DIC photoproduction under air saturation in the first 24 h (4.40 µmol/(L h)) was increased by a factor of 1.56 under O2 saturation

but fell by only 36% under N2 saturation. To evaluate the relative importance of UV-B

UV-A

and visible radiation in the photodegradation

we examined the above process using Mylar-d films and UF-3 and UF-4 plexiglass filters. The results indicated that the UV-B

UV-A and visible wavelengths accounted for 31.8%

32.6% and 25.6%

respectively

of DIC production with simulated sunlight irradiation. The above results also indicated that photoproduction of DIC could take place in natural water at depths greater than those that UV light can reach. When 20 µmol/L desferrioxamine mesylate (DFOM

a strong Fe complexing ligand) was added

the rate of DIC photoproduction fell to 55.6% that of the original SRHA samples with 5.46 µmol/L Fe.

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references

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