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Natural organic-matter interactions with Cu(II) in ground water

Thesis/Dissertation ·
OSTI ID:5622251
The influence of dissolved natural organic matter (NOM) on the transport of Cu(II) in saturated media was investigated in controlled batch and column experiments. Six sources of natural organic matter were chosen to represent different environments and different humic fractions. SiO{sub 2} and {alpha}-Al{sub 2}O{sub 3} comprised the mineral surfaces with which the NOM and Cu(II) interacted. The experiments were conducted at a constant ionic strength and buffer concentration and at pH 6.2 and pH 7.5. Equilibrium Cu(II) concentrations were monitored with an ion specific electrode and atomic absorption spectrophotometer and NOM was measured as UV absorbance at 254 nm. Adsorbate effect on particle surface charge was evaluated using microelectrophoresis and the effect of molecular weight on NOM breakthrough was determined with ultrafiltration of column influent and effluent. Column studies showed significant variation in NOM breakthrough as a function of source on a mixed bed of SiO{sub 2} and {alpha}-Al{sub 2}O{sub 3}. Humic acid from the Suwannee River showed greater adsorption than the fulvic acid from the same source. The presence on Cu(II) resulted in greater retardation of all the NOM sources than in the Cu(II) free systems. Cu(II) transport was slightly facilitated at pH 6.2 by the Orange County NOM and Biscayne aquifer NOM, while the other NOM sources inhibited Cu(II) movement. At pH 7.5 the Orange County and Biscayne Aquifer sources greatly facilitated the transport of the Cu(II) in a mixed bed column.
Research Organization:
Arizona Univ., Tucson, AZ (United States)
OSTI ID:
5622251
Country of Publication:
United States
Language:
English