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This paper studies the perturbation patterns of GPR images as a tool for tracing water seepage pathway in a plastic and concealed water pipe in a full-scale concrete wall specimen.
The artificial isotopes are mostly used for the purpose of tracing water and sediment movement in both surface and groundwater bodies.
Environmental isotopes, such as oxygen-18 and deuterium, are compositions of water molecules and they approximate water behaviors (Clark and Fritz 1997) and serve as suitable tools for tracing water pathways and contributions.
Naturally occurring, non-radioactive isotopes of hydrogen and oxygen in water provide a potential method for tracing water sources.
Stable water isotopes may present one possible method for tracing water sources from ecosystems to individual animals [11], [13].
Although much progress has been made in tracing carbon and nitrogen, difficulty remains in tracing water sources from the ecosystem to animals and among animals (the "water web").
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The temperature effect on the precipitation isotopic content is one of the basis for tracing waters in the hydrologic cycle and hence used to reconstruct paleoclimates and paleohydrology.
These properties mean the sensor will be applicable to trace water detection in various industrial gases.
Isotopic techniques are an increasingly common means to trace water sources.
His 1964 book "Illustrated History of Ships and Boats" (Doubleday) traces water travel from the days when men floated across a river on an inflated animal skin to the days of steel-skinned nuclear submarines.
It was based on the concept of diffusive equilibration whereby a traced water with a composition close to that expected in the formation was continuously circulated and monitored in a packed-off borehole.
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