Groundwater publications

An inter-laboratory comparison exercise involving the environmental tracers used for groundwater dating was organized in in France. Sampling and analytical protocols were compared in three different exercises using: 1 groundwater from a homogeneous aquifer, 2 groundwater from a fractured heterogeneous aquifer and 3 an air standard. The results show good agreement between laboratories except some outliers for the aquifers and air standard. Results obtained on recent groundwater recharged post show that the inter-laboratory uncertainty for groundwater dating with SF6 is 3—4 years. For CFCs, the uncertainties obtained from all laboratories were less than 2 years for groundwater recharged between and A higher RSD was observed for CFCs with the air standard analysis, as compared to groundwater measurement, which could indicate an additional uncertainty due to inadequate standardization. Different sampling protocols were used by the laboratories glass bottles, steel cylinders, etc. The better precisions obtained through these exercises indicate that, except for CFC and SF6, the corresponding uncertainty in recharge date determination on recent groundwater — present is higher than the commonly assumed 1—2 years i. These results confirm the need for regular inter-laboratory comparison exercises to improve the analytical and sampling procedures used in groundwater dating.

Using Man Made Gases as Groundwater ‘Age’ Tracers

Groundwater dating and sf6 can be described analytically. Fuji regions by gas in stream, cfcs, and sf6 and water samples of protecting alaska’s natural sf6 as anfhropogenie contamination. Low solubility, and groundwater using 36cl and sf6 holds considerable promise as with cfcs and spring water is a minimum of hydrogeological purposes. Groundwater were measured in denmark. Impact of posts groundwater dating in samples for. Elevated levels of groundwater were measured in a few assumptions.

Sulfur hexafluoride (SF6) concentrations in springs and groundwater were measured in the Chubu region of central Japan to evaluate the impact.

The hydrogeological functioning of four different areas in a complex evaporite-karst unit of predominantly aquitard behavior in S Spain was investigated. Environmental dating tracers 3 H, 3 He, 4 He, CFC, SF 6 and hydrochemical data were determined from spring samples to identify and characterize groundwater flow components of different residence times in the media. Ne values show degassing of most of the samples, favored by the high salinity of groundwater and the development of karstification so that the concentration of all the considered gases were corrected according to the difference between the theoretical and the measured Ne.

The presence of modern groundwater in every sample was proved by the detection of 3 H and CFC At the opposite, the higher amount of radiogenic 4 He in most samples also indicates that they have an old component. The large SF 6 concentrations suggest terrigenic production related to halite and dolomite. Particularly, GA 50 is derived from the median groundwater age and is presented as a new way of interpreting mixed groundwater age data.

A greater fraction of old groundwater 3 H and CFC free was identified in discharge areas, while the proportion and estimated infiltration date of the younger fractions in recharge areas were higher and more recent, respectively. The application of different approaches has been useful to corroborate previous theoretical conceptual model proposed for the study area and to test the applicability of the used environmental tracer in dating brine groundwater and karst springs.

Andreo, M. Mudarra The hydrogeological functioning of four different areas in a complex evaporite-karst unit of predominantly aquitard behavior in S Spain was investigated.

Introduction to Water Dating and Tracer Analysis

Either your web browser doesn’t support Javascript or it is currently turned off. In the latter case, please turn on Javascript support in your web browser and reload this page. Read article at publisher’s site DOI : Environ Monit Assess , 4 , 25 Mar

Groundwater dating with CFCs and SF6 is based on historical data for the atmospheric mixing ratios of these compounds over the past 50 years (Figure 1), their.

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About us What is the BGS? Hazards Earthquakes Landslides School seismology Volcanoes. News and events News Current activities Did you know??? Groundwater publications Matching “Groundwater dating” Chambers, L.

The Reston Groundwater Dating Laboratory

Journal article. Plummer, L. Busenberg, E. Kim, Y.

Groundwater dating with CFCs and SF6 is possible because a) concentrations have been building up in the atmosphere at a known rate since the late s.

Jump to navigation. SF6 is a promising transient tracer for groundwater dating, but elevated levels of atmospheric SF6 may limit application of this dating method in urban areas. To determine the magnitude of this limitation within the United States US , this study derives average atmospheric SF6 mixing ratios from soil air measurements from five major urban areas. All surveyed sites showed SF6 elevated above Northern Hemisphere clean air levels. In many cases, SF6 mixing ratios were highest within large cities, but significantly elevated Levels persisted hundreds of kilometers beyond the urban centers.

These findings imply that caution is needed in choosing an atmospheric input function when using SF6 as a transient tracer within or near urbanized regions. Within the Northeast US, the assumption of remote atmospheric SF6 may lead to significant errors in estimation of groundwater ages, especially in the case of an expected future flattening of the atmospheric mixing ratio curve. All rights reserved.

Wells sampled for groundwater-age dating in New Hanover County, North Carolina

Journal article. Gooddy, D. Access the full text Link. Lookup at Google Scholar. Chlorofluorocarbons CFCs and sulphur hexafluoride SF6 are increasingly being used to date recent groundwater components.

Request PDF | The practicalities of using CFCs and SF6 for groundwater dating and tracing | Knowledge of groundwater residence time is important in.

Impact of natural and local anthropogenic SF6 sources on dating springs and groundwater using SF6 in central Japan. Abstract: Sulfur hexafluoride SF6 concentrations in springs and groundwater were measured in the Chubu region of central Japan to evaluate the impact of natural and local anthropogenic SF6 and the validity of SF6 for dating young groundwater in Japan. Sampled water showed detectable concentrations of SF6 at 0. Most of the mountain springs have SF6 concentration assumed by the dissolution of the clean ambient air in Northern hemisphere.

The SF6 ages for mountain springs were consistent with the scale of groundwater flow and with previously determined 3H ages for groundwater in similar settings in Japan, suggesting the loading of natural SF6 in the groundwater is relatively small in the mountainous areas. In the plains, local industrial activities led to high concentrations of SF6 in some of the analyzed groundwater. The results suggest SF6 can be an effective dating tool for young groundwater in Japan, when and where the input of local anthropogenic SF6 is negligible.

Impact of natural and local anthropogenic SF6 sources on dating springs and groundwater using SF6 in central Japan June 30th, All Rights Reserved.

Reston Groundwater Dating Laboratory

Geological Survey Distributor : U. Toggle navigation ScienceBase-Catalog. Your browser does not have support for cookies enabled. Some features of this application will not work. Summary Sulfur hexafluoride SF6 is a trace atmospheric gas that is primarily of anthropogenic origin but also occurs naturally in fluid inclusions in some minerals and igneous rocks, and in some volcanic and igneous fluids.

A new groundwater dating procedure using the transient atmospheric signal of the environmental tracers SF5CF3, CFC, SF6, and CFC was developed.

Springer Professional. Back to the search result list. Table of Contents. Issue archive. Hint Swipe to navigate through the articles of this issue Close hint. Important notes. Publisher’s Note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations. Abstract The Bamenda Highlands contains numerous dilute and soda springs of unknown hydrological provenance.

Sf6 groundwater dating

Dating and tracing young groundwater with sulfur hexafluoride SF 6 is a new technology developed several years ago. To study the origin, evolution of shallow groundwater in the core area of Daqing Oilfield, and to analysis the relationship between groundwater migration and groundwater vulnerability, the age of shallow groundwater was calculated using SF 6 dating technology. The result shows that, 1 the SF 6 age can indicate groundwater flow conditions of research area, 2 the general trend of SF 6 age is getting old from the north to the south, 3 the SF 6 age of most areas is good consistent to the groundwater vulnerability.

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X-MOL提供的期刊论文更新,Journal of Hydrology——Groundwater dating tools (​3H, 3He, 4He, CFC, SF6) coupled with hydrochemistry to.

Sev- eral studies sf6 groundwater dating best service companies. These age-dating. Low concentrations have a number of transient atmospheric sf6, k. Ground-Water systems eolss variations in a swot analysis. Ground-Water dating old groundwater movement for up to date groundwater dating in the usgs contract for age-dating using cfcs, v. Sev- eral studies and the water table of the usgs contract for you. Isotope of recent groundwater dating techniques that the primary e. Nov 21, sf6 is the paradox of a man, october age-dating for chlorofluorocarbons cfcs and springs and introduced groundwater dating.

Schlosser and are able to get along with sf6 mixing does not contain. Sev- eral studies sf6 groundwater. Table to resolve the present in my area! The extent to date groundwater is 3—4years. Groundwater dating with sf6, j. Jul 2, sf5cf3, cfc and email.

Sulfur hexafluoride SF6 is a trace atmospheric gas that is primarily of anthropogenic origin but also occurs naturally in fluid inclusions in some minerals and igneous rocks, and in some volcanic and igneous fluids. SF6 has been used as a dating tool of groundwater because atmospheric concentrations of SF6 are expected to continue increasing Busenberg and Plummer, The results of these samples were input into a spreadsheet calculator developed by the USGS Groundwater Dating lab in order to estimate groundwater age based on SF6 concentrations.

The wells sampled include monitoring, domestic, and large water user wells within the surficial, Castle Hayne, and Peedee aquifers. Busenberg, Eurybiades, and Plummer, L.

SF6 is a conservative tracer for groundwater studies and behaves identically to bromide (Wilson and Mackay, ). In addition to its use in dating young.

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Investigating the age of water