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Evaluations of transmissivity and storativity by various measures are given.
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Bayesian epistemologists have attempted to formalise extant explanations of transmissivity and non-transmissivity of justification; they have concentrated on the information-dependence template.
Theis (1935) introduced the hydraulic characteristic transmissivity or coefficient of transmissivity in groundwater.
In case the erroneous transmissivity data are treated as error-free, the ensemble standard deviation of transmissivity becomes unrealistic low.
From the results, values of transmissivity (T) could be derived.
Table 6 Calibrated parameter set Parameter Value Decay factor of transmissivity (m) 0.067 m Block average roughness coefficient (n0) 0.4 Saturated transmissivity (T0) T0_sand: 12 m2/h T0_silT0 5 m2/h T0_clay: 1 m2/h.
It can be calculated as a ratio of transmissivity (T) and aquifer thickness.
Additionally, a thorough derivation of directional responses of transmissivity and reflectivity of different commonly used plastics is provided.
Within this range of transmissivity (10−6 10−5), the phase shifts at the frequency of the M2 wave will increase as the permeability (transmissivity) increases (Appendix Fig. 11; Doan et al. 2006).
The spatial distributions of transmissivity and storativity for the whole aquifer system are shown in Figs. 6 and 7.
Decay factor of transmissivity (m), Block average roughness coefficient (n0), and Saturated transmissivity (T0) were identified through trial-and-error calibration while the maximum storage capacities at root zone were presumed based on literature values.
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