A1 Alkuperäisartikkeli tieteellisessä aikakauslehdessä
Biogenic Fenton process : A possible mechanism for the mineralization of organic carbon in fresh waters (2021)


Vähätalo, Anssi V.; Xiao, Yihua; Salonen, Kalevi (2021). Biogenic Fenton process : A possible mechanism for the mineralization of organic carbon in fresh waters. Water Research, 188, 116483. DOI: 10.1016/j.watres.2020.116483


JYU-tekijät tai -toimittajat


Julkaisun tiedot

Julkaisun kaikki tekijät tai toimittajat: Vähätalo, Anssi V.; Xiao, Yihua; Salonen, Kalevi

Lehti tai sarja: Water Research

ISSN: 0043-1354

eISSN: 1879-2448

Julkaisuvuosi: 2021

Volyymi: 188

Artikkelinumero: 116483

Kustantaja: Elsevier

Julkaisumaa: Britannia

Julkaisun kieli: englanti

DOI: http://doi.org/10.1016/j.watres.2020.116483

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Tiivistelmä

To explore the mechanisms that mineralize poorly bioavailable natural organic carbon (OC), we measured the mineralization of OC in two lake waters over long-term experiments (up to 623 days) at different pH and iron (Fe) levels. Both the microbial and photochemical mineralization of OC was higher at pH acidified to 4 than at the ambient pH 5 or an elevated pH 6. During 244 days, microbes mineralized up to 60% of OC in the 10-µm filtrates of lake water and more than 27% in the 1-µm filtrates indicating that large-sized microbes/grazers enhance the mineralization of OC. A reactivity continuum model indicated that the acidification stimulated the microbial mineralization of OC especially in the later (>weeks) phases of experiment when the bioavailability of OC was poor. The reactive oxygen species produced by light or microbial metabolism could have contributed to the mineralization of poorly bioavailable OC through photochemical and biogenic Fenton processes catalyzed by the indigenous Fe in lake water. When Fe was introduced to artificial lake water to the concentration found in the study lakes, it increased the densities of bacteria growing on solid phase extracted dissolved organic matter and in a larger extent at low pH 4 than at pH 5. Our results suggest that in addition to the photochemical Fenton process (photo-Fenton), microbes can transfer poorly bioavailable OC into labile forms and CO2 through extracellular Fe-catalyzed reactions (i.e., biogenic Fenton process).


YSO-asiasanat: hiilen kierto; liuennut orgaaninen hiili; mineralisaatio; järvet; mikrobit; kemialliset reaktiot; rauta

Vapaat asiasanat: biogenic Fenton; iron; microbes; organic carbon; reactive oxygen species; reactivity continuum.


Liittyvät organisaatiot


Hankkeet, joissa julkaisu on tehty

Miksi ruskeat vedet pitävät värinsä - ra
Xiao, Yihua
Suomen Akatemia
01.09.2016-31.12.2019


OKM-raportointi: Kyllä

Alustava JUFO-taso: 3


Viimeisin päivitys 2020-28-10 klo 12:11