Results of Chemical Analyses in Support of Yucca Mountain Studies

Daniels, Jeanette

关键词: ACID NEUTRALIZING CAPACITY;    ANIONS;    AQUIFERS;    BENZOIC ACID;    CHEMICAL ANALYSIS;    DIFFUSION;    GROUND WATER;    HALIDES;    NEVADA TEST SITE;    RADIOACTIVE MATERIALS;    RADIOISOTOPES;    R;   

DOI  :  10.2172/920645
RP-ID  :  DOE/RW12232-4NQ-010
PID  :  OSTI ID: 920645
Others  :  Other: ORD-FY04-010
Others  :  TRN: US0800950

美国|英语

来源: SciTech Connect

【 摘 要 】

Ground water monitoring for the Nye County Early Warning Drilling Program (NCEWDP) was established to monitor underground water sources of the area and to protect communities surrounding the Nevada Test Site (NTS) from potential radionuclide contamination of these water sources. It provides hydrological information pertaining to groundwater flow patterns and recharge issues in the vicinity of Yucca Mountain. The Harry Reid Center for Environmental Studies (HRC) obtained groundwater samples from select NCEWDP wells shown in Figure 1. These samples were analyzed for major cations, major anions, trace elements, rare earth elements, alkalinity, pH and conductivity. These geochemical results can be used to evaluate the degree of interaction between the aquifers sampled, leading to a thorough mapping of the aquifer system. With increased analysis down gradient of the Yucca Mountain area, evaluations can identify viable groundwater flow paths and establish mixing of the groundwater systems. Tracer tests provide insight into groundwater flow characteristics and transport processes of potential contaminants. These tests are important for contaminant migration issues including safe disposal of hazardous and radioactive materials and remediation of potentially released contaminants. At a minimum, two conservative (non-sorbing) tracers with different diffusion coefficients are used for each tracer test. The tracer test performed under this cooperative agreement utilized fluorinated benzoic acids and halides as conservative tracers. The tracers are of differing size and have differing rates of diffusion into the rock. Larger molecules can not enter the pore spaces that are penetrated by the smaller molecules, therefore larger tracers will travel faster through thegroundwater system. Identical responses of the two tracers indicate no appreciable diffusion into pores of the aquifer system tuff. For the Nye County Tracer Tests, the HRC provided chemical analysis for the tracer test being conducted at site 22. Samples were analyzed for multiple tracers throughout the testing period.