In complex environmental systems, tracers are indispensable tools for the investigation of various physical, chemical, and biological processes. From the large variety of tracers employed by EAWAG in the aquatic environment, we present some examples relevant to groundwater research. Some tracers (e.g., 222Rn, 3H/3He, chlorofluorocarbons) allow the time since groundwater infiltration to be determined; this information can be used to quantify process rates such as flow velocities, recharge and reaction rates. Other tracers (e.g., conductivity, isotopes of oxygen or boron) can be used to quantify mixing ratios between waters of different origin, for instance, to study the admixture of leachate from a landfill to an aquifer. In contrast to thes...
Groundwater age or residence time is the time water has resided in the subsurface since recharge. De...
Remediating hazardous waste sites requires detailed site characterization. In groundwater remediatio...
Lumped-parameter models are commonly applied for determining the age of water from time records of t...
Aquifer resources continue to be overexploited, leaving the world's most impoverished (or vulnerable...
Environmental tracers are relevant tools for understanding the water cycle and particularly for unde...
In many regions, three dimensional characterization of the groundwater regime is limited by coarse w...
Environmental tracers are physical properties and chemical components of water whose spatial and tem...
Les traceurs environnementaux sont des outils pertinents pour la compréhension du cycle de l’eau et ...
International audiencedentification of biogeochemical reactions in aquifers and determining ...
AbstractNatural tracers, including 222Rn, 226Ra, δ18O, and δ2H are frequently used in hydrological s...
Investigating groundwater residence time and recharge sources is crucial for water resource manageme...
Environmental tracers are used qualitatively fora better formulation of conceptual models and quanti...
Labeling groundwater by injecting an artificial tracer is a standard and widely used method to study...
Natural and artificial tracers can be used for nuclear sites management. Tracer techniques coupled w...
Understanding groundwater–surface water (GW–SW) interactions is vital for water management in karsti...
Groundwater age or residence time is the time water has resided in the subsurface since recharge. De...
Remediating hazardous waste sites requires detailed site characterization. In groundwater remediatio...
Lumped-parameter models are commonly applied for determining the age of water from time records of t...
Aquifer resources continue to be overexploited, leaving the world's most impoverished (or vulnerable...
Environmental tracers are relevant tools for understanding the water cycle and particularly for unde...
In many regions, three dimensional characterization of the groundwater regime is limited by coarse w...
Environmental tracers are physical properties and chemical components of water whose spatial and tem...
Les traceurs environnementaux sont des outils pertinents pour la compréhension du cycle de l’eau et ...
International audiencedentification of biogeochemical reactions in aquifers and determining ...
AbstractNatural tracers, including 222Rn, 226Ra, δ18O, and δ2H are frequently used in hydrological s...
Investigating groundwater residence time and recharge sources is crucial for water resource manageme...
Environmental tracers are used qualitatively fora better formulation of conceptual models and quanti...
Labeling groundwater by injecting an artificial tracer is a standard and widely used method to study...
Natural and artificial tracers can be used for nuclear sites management. Tracer techniques coupled w...
Understanding groundwater–surface water (GW–SW) interactions is vital for water management in karsti...
Groundwater age or residence time is the time water has resided in the subsurface since recharge. De...
Remediating hazardous waste sites requires detailed site characterization. In groundwater remediatio...
Lumped-parameter models are commonly applied for determining the age of water from time records of t...