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DOE/ORO/2327 Oak Ridge Reservation Annual Site Environmental ...

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<strong>Annual</strong> <strong>Site</strong> <strong>Environmental</strong> Report<br />

well 1191. No other radionuclides exceeded reference standards in the WOC Discharge Area wells. A<br />

statistically significant downward trend exists for all three radiological constituents at both sampling<br />

locations. Aside from the radionuclides that were detected above reference standard concentrations, the<br />

following radionuclides were detected at low levels in WOC Discharge Area wells: gross beta activity,<br />

214 3 40 214 214<br />

Bi, and H in well 857; gross beta activity and K in well 858; Bi and Pb in well 1190; and gross<br />

alpha activity, 214 Bi, and 214 Pb in well 1191.<br />

As in past years, iron, manganese, and aluminum exceeded reference standards in WOC Discharge<br />

Area wells during 2009. Aluminum was found to exceed its reference standard in well 857 in addition to<br />

iron and manganese in wells 1190 and 1191. Statistical trend analyses of metals data for these wells show<br />

a statistically significant historical increase in aluminum and manganese in wells 857 and 1191,<br />

respectively and a statistically significant historical decrease in manganese and iron in wells 1190 and<br />

1191, respectively. Further statistical analyses of historical iron, manganese, and aluminum data from<br />

these wells indicate the 95% UTLs are within the range or below those estimated for the transition<br />

limestone-shale/shale-dominated groundwater clusters established for ORNL (Wolf et al. 1996). The<br />

transition limestone-shale/shale-dominated groundwater clusters were used for comparison because the<br />

WOC Discharge Area wells are screened in strata dominated by shale but interbedded with limestones.<br />

Table 5.24 provides a comparison for these UTLs.<br />

Table 5.24. Comparison of WOC discharge area groundwater and shale-dominated<br />

groundwater upper tolerance limits (UTLs)<br />

Metal<br />

WOC discharge area<br />

estimated 95 th UTL<br />

(mg/L)<br />

Transition limestone-shale<br />

groundwater<br />

estimated 95 th UTL (mg/L)<br />

Shale-dominated<br />

groundwater<br />

estimated 95 th UTL (mg/L)<br />

Iron 9.19 8.0 50<br />

Manganese 0.35 2.6 16<br />

Aluminum 1.11 3.2 2.8<br />

It is likely that the metals are sorbed onto suspended solids in the groundwater samples collected<br />

contributing to the exceedance of the reference standards used for comparison. Other metals were<br />

detected at low concentrations in groundwater samples collected from WOC Discharge Area wells; these<br />

results can be found in the 2009 <strong>Environmental</strong> Monitoring Results (<strong>DOE</strong> 2009).<br />

Detection limits for several semi-volatile organic compounds (atrazine, benzo(a)pyrene,<br />

hexachlorobenzene, and pentachlorophenol) exceeded reference standards in samples collected from<br />

WOC Discharge Area monitoring points. No other organic compounds were present in concentrations<br />

above reference standards in samples collected from WOC Discharge Area wells; however, a common<br />

plasticizer [bis(2-ethylhexyl) phthalate] was detected at low, estimated concentrations in wells 858, 1190,<br />

and 1191 and was detected in well 1239. Bis(2-ethylhexyl) phthalate was also found in laboratory blank<br />

samples from wells 857, 858, and 1239. Given its presence in laboratory blanks, the source of bis(2ethylhexyl)<br />

phthalate may have been due to laboratory cross-contamination of sample aliquots collected<br />

from wells 1190, 1191, and 1239. Departing from past year observations, diethyl phthalate was not<br />

detected in samples collected from WOC Discharge Area wells in 2009.<br />

Low concentrations of volatile organics were also detected in WOC Area Discharge wells in 2009.<br />

Low levels of acetone were detected in wells 1190 and 1191, while a low estimated concentration of<br />

carbon disulfide was reported for a sample collected from well 1190. Subsequent to collection of the 2009<br />

groundwater samples, acetone was found to be present in the deionized water used in preparing blank<br />

samples. This source of deionized water is no longer used for blank samples or for decontamination of<br />

sampling equipment.<br />

7000/Bearden Creek Watershed Discharge Area Exit Pathway Results<br />

Wells 1198 and 1199 were not sampled during 2009 because detailed geotechnical and environmental<br />

characterization of the Multiprogram Computational and Data Center site located east of the 7000 area<br />

<strong>Oak</strong> <strong>Ridge</strong> National Laboratory 5-77

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