Je. Capilla et al., STOCHASTIC SIMULATION OF TRANSMISSIVITY FIELDS CONDITIONAL TO BOTH TRANSMISSIVITY AND PIEZOMETRIC DATA 2 - DEMONSTRATION ON A SYNTHETIC AQUIFER, Journal of hydrology, 203(1-4), 1997, pp. 175-188
In the first paper of this series a methodology for the generation of
transmissivity fields conditional to both transmissivity and piezometr
ic head data was presented. This methodology, termed the self-calibrat
ed approach, consists of two steps: first, the generation of a seed tr
ansmissivity field conditioned only to transmissivity data, and second
, the perturbation of the seed field up until the piezometric head dat
a are reproduced. The methodology is now demonstrated on a set of cont
rolled numerical experiments carried out on synthetic aquifers. The ob
jective of these experiments is not just to show that the methodology
works, but also to explore its robustness under different situations.
A total of 12 experiments have analyzed the performance of the method
as a function of: (i) the log(10) T transmissivity variance (from 0.2
to 2.0); (ii) the number of log(10) T conditioning data (from 10 to 30
); (iii) the number of piezometric head data (from 30 to 90); (iv) the
number of master points (from 25 to 1000); (v) the magnitude of allow
ed departure of the final T field from the seed field (up to four time
s the kriging standard deviation). In all cases, the method was able t
o generate transmissivity fields conditional to both transmissivity an
d head measurements, at the same time preserving the spatial variabili
ty of the transmissivity field. It was found that the performance of t
he method increases with both the number of log(10) T data and the num
ber of master points, whereas it decreases as either the log(10) T var
iance or the number of piezometric head data increases. (C) 1997 Elsev
ier Science B.V.