Age dating old groundwater table,
The natural and non-natural processes that impart a dissolved gas composition to recharging groundwater are complex and variable.
Characterization of mean groundwater age and recharge temperature through the use of noble gas techniques provides information that is relevant to answering these questions and that is not accessible through traditional hydrogeologic approaches.
When mixing is ignored, as it often is, tritium alone can overestimate the mean age of the modern less than 50 year age component.
Less model-dependent than tritium age dating: Accurate analysis of dissolved Neon allows determination of excess air concentration; analysis of the heavy noble gases, Krypton and Xenon allows a robust calculation of the noble gas recharge temperature; an estimate of accumulated radiogenic 4-Helium can be made from total dissolved helium.
Groundwater samples may or may not contain tritium above the method detection limit.
Natural or non-natural processes may incorporate significant excess air concentrations or conversely strip groundwater of dissolved gases. Thus no simple algorithm exists that will produce reliable groundwater ages for all samples. Full elemental analysis of all noble gases: Groundwater Age-Dating for Water Resource Characterization Background The increasing national and international demand for water has led to increasing reliance on subsurface storage, both for naturally and artificially recharged water.
The facility is staffed by Ph. This system represents a capability for characterizing groundwater recharge conditions by dissolved gas analysis that is unmatched by any other laboratory.
How much and on what time scales groundwater can be recharged and withdrawn in specific sub-basins, Groundwater flow fields at both recharge and basin scales, Water quality impacts of recharge water storage and recovery in a subsurface that is bio-geochemically active, How changes in management practices have and will affect water quality, and Future distributions of contaminants in the subsurface.
Construction of this facility was funded by LLNL. High throughput and rapid turn-around: Supporting capabilities for isotopic characterization of groundwater and groundwater contaminants.
Expertise in the use of noble gas tracers: The nitrate isotopic capability is state of the art, and uses the microbial method to determine the isotopic composition of both nitrate nitrogen and oxygen in small volume samples containing very low concentrations of nitrate.
Isotopically enriched noble gases are inexpensive, commercially available, and non-toxic, allowing them to be used as introduced tracers to tag large volumes of recharging water. Supporting capabilities for the characterization of groundwater and surface water gas composition: The facility also provides membrane inlet mass spectrometry for rapid determination of major and minor gases in groundwater, including argon, nitrogen, oxygen, carbon dioxide and methane.
The ability to use a variety of different isotopes for each element and the low backgrounds in natural waters allows tracing different sources of recharge to a given receptor well at very low mixing ratios and with large dynamic range.
This increased reliance on the groundwater in concert with the strict regulation on water quality has led to a need by water managers and regulators to understand: The fully automated, computer-controlled manifold system allows for rapid analysis of the full suite of noble gases, and allows determination of tritium through helium-3 accumulation.
Traditional tritium age-dating is confounded by mixing between old tritium-dead water and young tritiated water, and requires modeling, assumptions or independent estimates of the mixing ratio to convert measured tritium activity into a groundwater age.
Description LLNL has developed a noble gas mass spectrometry facility that houses a state-of-the-art water-gas separation manifold and mass spectrometry system designed specifically for high throughput of groundwater samples. Expertise in interpretation of groundwater data: In-situ biological processes may alter dissolved gas composition.
LLNL scientists carry out ongoing collaborative research on interpretation of dissolved gas composition for groundwater applications and continue to gain experience with sample analysis, data analysis, and derived results interpretation. The facility is closely integrated with a stable isotope mass spectrometry laboratory capable of providing supporting information for groundwater transport studies, including stable isotopic composition of water, nitrate, and carbon.
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