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a Dep. of Chemistry and Bioengineering, Tampere Univ. of Technology, P.O. Box 541, 33101 Tampere, Finland
b Geological Survey of Finland, P.O. Box 96, 02150 Espoo, Finland
c Geological Survey of Finland, Tutkijankatu 1, 83500 Outokumpu, Finland
* Corresponding author (reija.kolehmainen{at}tut.fi).
Received for publication January 30, 2008.
The role of biodegradation in the attenuation of natural organic matter (NOM) was investigated in long-term experiments that simulate artificial ground water recharge (AGR) for drinking water production. Lake water containing 5.8 mg L–1 total organic carbon (TOC) was continuously fed into an 18.5-m-long sand column. During the 941 d of operation, on average 76 and 81% of TOC was removed within the first 0.6 m and the entire column length, respectively. Large molecular size fractions (approximately 1800–2200 Da) of NOM were removed more efficiently than smaller ones (approximately 250–1400 Da). The biodegradation of dissolved organic carbon (DOC) within the first 0.6 m, measured by the stable inorganic carbon isotope (
13C) method, depended on temperature and hydraulic load: The extent of mineralization was 32% at 6°C (Day 442) and 38% at 23°C (Day 708) with a 0.3 m3 (m2d)–1 hydraulic load and 52% at 5.5°C (Day 883) with a 3.1 m3 (m2d) –1 hydraulic load. The rest of the DOC removal was likely due to entrapment or sorption onto the sand particles. Decreases in DOC and the total cell counts in the water along the column were positively correlated (r = 0.99; P = 0.001). The accumulation of biomass was minor, with the highest concentration amounting to 7.2 mg g–1 dw of sand. In summary, this study demonstrated that biodegradation has a key role in NOM removal in AGR and is dependent on temperature.
Abbreviations: AGR, artificial ground water recharge COD, chemical oxygen demand DAPI, 4',6-diamidino-2-phenylindole
13C, the isotopic ratio of carbon as a per mil (
) difference relative to the international VPDB standard DO, dissolved oxygen DOC, dissolved organic carbon HPSEC, high-performance size-exclusion chromatography HRT, hydraulic retention time NOM, natural organic matter SUVA, specific ultraviolet absorbance TOC, total organic carbon UVA, ultraviolet absorbance VPDP, Vienna Peedee Belemnite VS, volatile solids
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