Environmental tracers and groundwater dating

ETO is a colorless gas that is flammable and explosive. These influence the effectiveness of ETO sterilization. The use of ETO evolved when few alternatives existed for sterilizing heat- and moisture-sensitive medical devices; however, favorable properties Table 6 account for its continued widespread use. This mixture is less expensive than ETO-hydrochlorofluorocarbons HCFC , but a disadvantage is the need for pressure vessels rated for steam sterilization, because higher pressures psi gauge are required. The main disadvantages associated with ETO are the lengthy cycle time, the cost, and its potential hazards to patients and staff; the main advantage is that it can sterilize heat- or moisture-sensitive medical equipment without deleterious effects on the material used in the medical devices Table 6. Acute exposure to ETO may result in irritation e. ETO should be considered a known human carcinogen. The basic ETO sterilization cycle consists of five stages i. Most modern ETO sterilizers combine sterilization and aeration in the same chamber as a continuous process. There are no federal regulations for ETO sterilizer emission; however, many states have promulgated emission-control regulations.

The Reston Groundwater Dating Laboratory

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of tritium or cfcs, indicating a mixture. Not knowing the frequency distribution of age in a mixture or water source limits the usefulness of springs for groundwater​.

Szabo, D. Rice, L. Plummer, E. Busenberg, S. Drenkard, P. Water samples for age dating were collected from three sets of nested observation wells 10 wells with 1. Three steady state finite difference groundwater flow models were calibrated by adjusting horizontal and vertical hydraulic conductivities to match measured heads and head differences range, 0. The simulated groundwater travel times increase with depth in the aquifer, ranging from about 1. Differences between the tracer-based apparent ages for seven of the 10 samples were smaller than the error values.

This result may be caused by enrichment of local air in CFC and CFC from urban and industrial sources in the northeastern United States and minor contamination from sampling equipment. Overview Fingerprint. Access to Document

Chlorofluorocarbon

Kluwer Acadmic Press. Chlorofluorocarbons CFCs are stable, synthetic, halogenated alkanes, developed in the early s as safe alternatives to ammonia and sulphur dioxide in refrigeration. CFCs are nonflammable, noncorrosive, nonexplosive, very low in toxicity, and have physical properties conducive to a wide range of industrial and refrigerant applications. Primary uses of CFC and CFC include refrigerants in air-conditioning and other coolers, blowing agents in foams, insulation, and packing materials, propellants in aerosol cans, and as solvents.

CFC has been used primarily by the electronics industry in manufacture of semiconductor chips, in vapour degreasing and cold immersion cleaning of microelectronic components, and as a solvent in surface cleaning procedures Jackson et al. Amounts of release of CFCs to the atmosphere and subsequent incorporation into the Earth’s hydrologic cycle has closely followed production.

Water transit time and flow path are key controls on catchment nitrogen Coupling 3D groundwater modeling with CFC-based age dating to classify local​.

Bedrock wells commonly have a long open interval, but because flow occurs in the groundwater, knowledge of fracture locations controls the precision of the sampling. Therefore, only wells of known location, depth of water-identify zones, and well construction are selected for sampling. The number and spatial distribution of wells used will identify adequately the range of hydrogeologic conditions in each physiographic province and allow statistical comparisons among the physiographic provinces table 2.

The environmental tracers that are appropriate for the sampled aquifer system are selected for analysis table 2. Water also is analyzed for 1 major ions to aid in the application of the geochemical model, 2 dissolved gases to estimate ground-water recharge temperature, and 3 nitrate to indicate potential near-cfc sources of contamination, determine fertilizers, groundwater wastes, and septic systems Kroehler, Subsequent to oxygen collection and analysis, the susceptibility of the water supply to near-surface contamination will be evaluated.

The presence of CFCs and 3 H indicates that water that was in cfc with the air less than 50 years ago is determine pumped from the oxygen, and characterizes a well as potentially susceptible to global-surface contamination. Conversely, the absence of CFCs or 3 H indicates a ground-water apparent age of global than 50 years and characterizes a well as relatively non-susceptible to near-surface contamination.

This stable susceptibility or greater age can be confirmed with a 14 C derived age. Regional aquifers will be assigned susceptibility designations on the basis of statistical and geospatial analysis of the age determinations from samples used as part of this study and previous studies by the USGS. Table 2. Distribution of sample sites and primary methods for age determinations. Aquifer system.

Cfc Groundwater Dating

This use has resulted in large atmospheric releases of CFC gases over the last 50 years. Atmospheric CFC concentrations have increased due to higher usage, as well as relatively long atmospheric residence times, ranging between 44 to years. Precise CFC measurements have been conducted beginning in throughout the globe as a part of the Atmospheric Lifetime Experiment, producing an excellent recorded record of global CFC concentrations. Infiltration of meteoric water into the subsurface carries dissolved CFC gases.

When a groundwater sample is obtained and analyzed for the CFC concentration, the concentration in the water is related to the atmospheric CFC concentration at the time the water entered the subsurface, allowing for a recharge age measurement.

radioactive) which are present in the water cycle and Potential application of dating methods: – Aquifer Groundwater dating by CFCs, SF. 6.

HCFCs are compounds containing carbon, hydrogen, chlorine and fluorine. Industry and the scientific community view certain chemicals within this class of compounds as acceptable temporary alternatives to chlorofluorocarbons. The HCFCs have shorter atmospheric lifetimes than CFCs and deliver less reactive chlorine to the stratosphere where the “ozone layer” is found. Consequently, it is expected that these chemicals will contribute much less to stratospheric ozone depletion than CFCs.

Because they still contain chlorine and have the potential to destroy stratospheric ozone, they are viewed only as temporary replacements for the CFCs. Current international legislation has mandated production caps for HCFCs; production is prohibited after in developed countries and in developing countries. Hydrogen, when attached to carbon in organic compounds such as these, is attacked by the hydroxyl radical in the lower part of the atmosphere known as the troposphere.

CFCs, because they contain no hydrogen, and, therefore, no carbon-hydrogen bonds, are not destroyed by the hydroxyl radical. When HCFCs are oxidized in the troposphere, the chlorine released typically combines with other chemicals to form compounds that dissolve in water and ice and are removed from the atmosphere by precipitation. When HCFCs become destroyed in this way their chlorine does not reach the stratosphere and contribute to ozone destruction.

A certain portion of HCFC molecules released to the atmosphere will reach the stratosphere and be destroyed there by photolysis light-initiated decomposition. The chlorine released in the stratosphere can then participate in ozone depleting reactions as does chlorine liberated from the photolysis of CFCs. Regular, careful measurements of air from remote locations show that global concentrations of HCFCs have increased rapidly over time.

Ozone-depleting substances (ODS) – Regulation 12

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The analytical procedure determines concentrations of the four tracers in air and water samples. SF5CF3 and CFC can be used to date groundwaters in.

Chlorofluorocarbons CFCs , hydrochlorofluorocarbons HCFCs and halons destroy the earth’s protective ozone layer, which shields the earth from harmful ultraviolet UV-B rays generated from the sun. Hydrofluorocarbons HFCs also act to warm the planet. Man-made compounds such as chlorofluorocarbons CFCs , hydrofluorocarbons HCFCs and halons destroy ozone in the upper atmosphere stratosphere. The stratospheric ozone layer makes life possible by shielding the earth from harmful ultraviolet UV-B rays generated from the sun.

Decreased concentration of stratospheric ozone allows increased amounts of UV-B to reach the earth’s surface. Stratospheric ozone loss can result in potential harm to human health and the environment, including:. Most stratospheric ozone depletion is caused when chlorine or bromine reacts with ozone. About half of bromine entering the stratosphere is from man-made sources, mostly Halons.

While acting to destroy ozone, CFCs and HCFCs also act to trap heat in the lower atmosphere, causing the earth to warm and climate and weather to change. Taken together greenhouse gases are expected to warm the planet by 2. Some effects of global climate change include:.

Ethylene Oxide “Gas” Sterilization

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CORRESPONDING GROUND WATER AGE IN THE FRESH and CFC concentration dating in depth of 24 – 29 m is ~63 years but at depth of 48 – 53 m.

This document is also available in pdf format: fs Information about the age of ground water can be used to define recharge rates, refine hydrologic models of ground-water systems, predict contamination potential, and estimate the time needed to flush contaminants from ground-water systems. CFCs also can be used to trace seepage from rivers into ground-water systems, provide diagnostic tools for detection and early warning of leakage from landfills and septic tanks, and to assess susceptibility of water-supply wells to contamination from near-surface sources.

During the past 50 years, human activities have released an array of chemical and isotopic substances to the atmosphere. In the atmosphere, these substances have mixed and spread worldwide. Young ground water is typically found at depths from 0 to feet in unconsolidated sediments and at depths up to feet in fractured-rock systems. Shallow ground-water systems are commonly used for drinking water sources and they make up a large part of the baseflow in rivers and lakes.

However, shallow ground-water supplies are generally young recently recharged and, because there has been a wide variety of man-made pollutants produced in the 20th century, are more susceptible to contamination than deeper ground water. Information about ground-water age can be used to determine recharge rates and refine hydrologic models of ground-water systems Reilly and others, ; Szabo and others, and thus to predict the contamination potential and estimate the time needed to flush contaminants through a ground-water system.

The 0- to year time scale is particularly relevant to environmentally sensitive shallow ground-water systems. Prior to the late s, however, there were no reliable means of dating ground water recharged during this time scale and, until recently, none of those methods were considered practical for use in establishing regional patterns. In the early s, USGS scientists Busenberg and Plummer, developed a method to date ground water on the basis of chlorofluorocarbon CFC content of the water that is practical, cost-effective, and applicable to most shallow ground-water systems.

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All United Nations member countries are phasing out the production and import of ozone depleting substances, including R22, under the Montreal Protocol on Substances that Deplete the Ozone Layer. The phase out is supported by bans on new equipment containing HCFCs. R22 has been commonly used in residential and commercial refrigeration and air conditioning systems from the s, following the phase out of chlorofluorocarbons CFCs in R22 equipment is gradually reaching the end of its useful life and is being replaced with new equipment using different refrigerants.

New R22 refrigeration and air conditioning equipment can no longer be manufactured in or imported into Australia, apart from some spare parts and in some special circumstances. The refrigeration and air conditioning industry is already well advanced in the transition from R

Partitioning of atmospheric CFC’s into water vapor depends on the used to determine the recharge age of waters dating back to around

Nitrogen pollution of freshwater and estuarine environments is one of the most urgent environmental crises. Shallow aquifers with predominantly local flow circulation are particularly vulnerable to agricultural contaminants. Water transit time and flow path are key controls on catchment nitrogen retention and removal capacity, but the relative importance of hydrogeological and topographical factors in determining these parameters is still uncertain.

We used groundwater dating and numerical modeling techniques to assess transit time and flow path in an unconfined aquifer in Brittany, France. The We used groundwater discharge and groundwater ages derived from chlorofluorocarbon CFC concentration to calibrate a free-surface flow model simulating groundwater flow circulation.

Sensitivity analysis revealed that groundwater travel distances were not sensitive to geological parameters i. However, circulation was sensitive to topography in the lowland area where the water table was near the land surface, and to recharge rate in the upland area where water input modulated the free surface of the aquifer. We quantified these differences with a local groundwater ratio rGW-LOCAL , defined as the mean groundwater travel distance divided by the mean of the reference surface distances the distance water would have to travel across the surface of the digital elevation model.

The ratio rGW-LOCAL is sensitive to recharge conditions as well as topography and it could be used to compare controls on groundwater circulation within or between catchments. Aller au contenu principal.

Groundwater, Age of

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understanding key issues in the evolution of water quality. Chlorofluorocarbons (​CFCs) and sulphur hexafluoride (SF6) offer a convenient way of dating waters.

Add 5ml of glycerol. Mix well and pour into sterile Petri dishes. Description Pseudomonas Agar Base is designed so that by the addition of the appropriate supplement SR or SR the medium becomes selective for Pseudomonas aeruginosa or Pseudomonas spp. The formula of the supplement was described by Goto and Enomoto 2 following the demonstration of cetrimide as a selective agent by Lowbury and Collins 3. The medium gave better recovery of Pseudomonas aeruginosa with enhanced pigment formation whilst strongly suppressing Klebsiella, Proteus and Providencia spp.

This combination of agents gave a new and more specific medium for isolating pseudomonads from chilled foods and processing plants.

Chlorofluorocarbons

Environmental tracers are natural or man made anthropogenic compounds or isotopes that are widely distributed in the near-surface environment. Variations in their quantities can be used to determine pathways and timescales of environmental processes. They include naturally occurring isotopes such as carbon and anthropogenic tracers such as Chlorofluorcarbons CFCs.

Releases of anthropogenic environmental tracers include catastrophic events such as nuclear bomb testing releasing, as well as gradual leakage of tracers from industrial production processes. One of the principal uses of environmental tracers is for determining the ages of soil waters and groundwaters. Information on soil water and groundwater age allows determination of timescales for a range of processes in the sub-surface.

water balance (–) shows average annual rainfall of mm streamflow; groundwater; age dating; oxygen; tritium; SF6; CFCs.

Climate change. Geology of Britain. We use a wide range of environmental agents for this work including CFCs, SF6, tritium, radiocarbon and stable isotopes. There are various reasons why it can be important to know the age of groundwater in a particular aquifer. For example: does age validate the hydrogeological concept? Is the water a mixture of different ages? Is the water sustainable or being ‘mined’?

Did the water recharge in pre-industrial times? Was the water recharged during the ice age, i. Some groundwater dating agents, for example radiocarbon 14C are produced naturally in the environment and are suitable for dating waters many thousands of years old.

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