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By this approach, a mean 3H transit time of 4.6 years for the fissured-porous karst aquifer was determined, whereas the fast flowing water in the conduit system showed a mean transit time of days.
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In this paper, and in the context of size distributions, we present an alternative to the Euclidean-based mean-variance approach: a mean-equality approach that is based on an underlying socioeconomic perspective.
The computational complexity of the KF approach, a mean-square error (MSE) sense estimator, with decoupling X and Y dimensions is also illustrated in Table 4, where the count of multiplication involved either a 1 or a 0 is eliminated; the count of division involved a 1 is eliminated; the count of additions and subtraction involved a 0 is eliminated.
Its excretion in urine, however, did not start until about 10 weeks, when the cadmium concentration in kidney approached a mean value of 212 microgram/g.
Our approach achieves a mean improvement of 17% over a Hidden Markov Model baseline.
In our data this approach gives a mean coverage of approximately 2-4X (Table 5).
Our approach is a mean field one, i.e. we investigate the average quantities of these molecular species [ 32- 36].
To determine the critical distance two approaches were evaluated, a mean value approach and a cycle dependent approach.
Using a different approach, a static mean-field study of multi-population network activity was developed by Treves in [60].
We subsequently demonstrated PRB using Peyton's four-step approach, a validated means of teaching technical skills [ 13].
This approach offers a means of reducing computation times.
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