SOURCES AND CONTROLS ON NATURALLY-OCCURRING BORON IN NORTH CAROLINA COASTAL PLAIN GROUNDWATER: EVIDENCE FROM BORON ISOTOPES
Elevated B has been documented in confined Coastal Plain aquifers - up to 8.6 mg/L in SC (Lee 1984, USGS Open-File Report 84-247). Here we present boron concentrations and δ11B from 14 wells in the confined Cretaceous Upper and Lower Cape Fear aquifer in NC exhibiting Na-bicarbonate to Na-chloride composition. In the Cape Fear, we observed a large range of salinity (Cl- concentration 5-4680 mg/L), boron (overall 0.4-6.6 mg/L), B/Cl- ratios (0.003-0.255 mol/mol), and δ11B (8.5‑51.8‰).
In the overlying Pliocene Yorktown aquifer, B concentrations are lower (0.1-2.6 mg/L) and δ11B (20.9‑34.7‰) is consistent with seawater-derived B desorbing into groundwater (Vinson et al. 2011, Hydrogeol. J., v. 19 p. 981). In both aquifers, B/Cl- ratios are higher than seawater. Also, B/Cl- ratios and δ11B are negatively correlated in both aquifers (high δ11B associated with low B/Cl-), indicating that boron levels are controlled by dilution and desorption.
The combination of high B/Cl- ratio and δ11B >39‰, observed in the Cape Fear aquifer, warrants special attention because this combination is inconsistent with simple desorption of seawater-derived boron. In the Cape Fear, the pattern of B concentration vs. δ11B could indicate: (1) that boron is seawater-derived, but the B mass balance was disrupted by partial flushing events in the past; and/or (2) boron is from a brine rather than seawater source.