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Withdrawing radioisotopes can be considered by using alternative: magnetic, ultrasonic or optical methods for tracer detection.
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We describe a semi-Lagrangian method for tracer transport that is stable for arbitrary Courant numbers, and we test a parallel implementation discretized on the cubed sphere.
Table 5 Regional binding potential (BPND or DVR 1) estimates from the different methods for the tracer dose group (n = 10).
The interpretation methods for interwell tracer test considering the geologic model have three kinds: analytic method, numerical simulation method, semi-analytic method.
The method is applicable for tracer studies, and the method was able to quantify rate constants of greater than 10−5 s−10−5
The interpretation software for interwell tracer test was developed, based on the system of streamline solving method, and a practical and reliable interpretation method for interwell tracer test was formed.
At present, the interpretation method for interwell tracer test not considering the geologic model was called landmark.
Two different methods for determination of tracer diffusion coefficients in molten salts are presented.
In fact, several published papers on [18F]HX4 use these simplified methods for quantification of tracer uptake [16 19].
Traditional methods for selecting isotopic tracers and labeling measurements did not fully utilize the power of 13C-MFA.
The Logan plot is a model-independent graphical method for reversible tracers [18].
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