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Characterization and Origin of Dissolved Organic Carbon in Yegua Ground Water in Brazos County, Texas

Routh, Joyanto, 1968- (författare)
Department of Geology and Geophysics, Texas A&M University, College Station, TX 77843, USA
Grossman, Ethan L. (författare)
Department of Geology and Geophysics, Texas A&M University, College Station, TX 77843, USA
Murphy, Ellyn M. (författare)
Environmental and Energy Sciences Division, Battelle Pacific Northwest Laboratory, Richland, WA 99352, USA
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Benner, Ronald (författare)
Department of Biological Sciences, University of South Carolina, Columbia, SC 29208, USA
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 (creator_code:org_t)
John Wiley & Sons, 2005
2005
Engelska.
Ingår i: Groundwater. - : John Wiley & Sons. - 1745-6584. ; 39:5, s. 760-767
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • Abstract Dissolved organic carbon (DOC) concentrations in five shallow (< 20 m) and three deeper wells (27 to 30 m) in the Eocene Yegua Formation (Brazos County in east-central Texas) ranged from 92 to 500 ï¿œm. Characterization of high, intermediate, and low molecular weight DOC fractions (HMW > 3000 amu, IMW 1000 to 3000 amu, and LMW 500 to 1000 amu) and combined neutral sugar analyses provide information on organic matter sources in the Yegua aquifers. Combined neutral sugars ranged in concentration from 0.6 to 2.7 ï¿œmol/L and comprised 0.8% to 6.7% of DOC in ground water. Glucose was the most abundant neutral sugar, followed by xylose and galactose, arabinose, mannose, rhamnose, and fucose. These combined neutral sugars were more diagenetically altered in shallow, oxic ground water as indicated by high mole % fucose + rhamnose and low neutral sugar yield. The precursors for neutral sugars are most probably angiosperm leaves, which show a similar distribution pattern of neutral sugars. Ground water DOC was depleted in 13C relative to soil-zone organic matter (OM) (-16ï¿œ to -19ï¿œ). The d13C values of bulk DOC and HMW DOC ranged from -24ï¿œ to ï¿œ32ï¿œ, whereas LMW and IMW DOC ranged from -32ï¿œ to -34ï¿œ and ï¿œ16ï¿œ to ï¿œ28ï¿œ, respectively. This variability in d13C values is probably related to microbial processes and selective preservation of OM. Carbon isotope analyses in bulk and different molecular weight DOC fractions imply a predominantly C3 OM source and a low contribution of soil-zone OM to DOC.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geokemi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geochemistry (hsv//eng)
LANTBRUKSVETENSKAPER  -- Lantbruksvetenskap, skogsbruk och fiske -- Markvetenskap (hsv//swe)
AGRICULTURAL SCIENCES  -- Agriculture, Forestry and Fisheries -- Soil Science (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Oceanografi, hydrologi och vattenresurser (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Oceanography, Hydrology and Water Resources (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Environmental Sciences (hsv//eng)

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