Wd. Graham et Cr. Neff, OPTIMAL ESTIMATION OF SPATIALLY-VARIABLE RECHARGE AND TRANSMISSIVITY FIELDS UNDER STEADY-STATE GROUNDWATER-FLOW .2. CASE-STUDY, Journal of hydrology, 157(1-4), 1994, pp. 267-285
The first-order analytical solution of the inverse problem for estimat
ing spatially variable recharge and transmissivity under steady-state
groundwater flow, developed in Part 1 is applied to the Upper Floridan
Aquifer in NE Florida. Parameters characterizing the statistical stru
cture of the log-transmissivity and head fields are estimated from 152
measurements of transmissivity and 146 measurements of hydraulic head
available in the study region. Optimal estimates of the recharge, tra
nsmissivity and head fields are produced throughout the study region b
y conditioning on the nearest 10 available transmissivity measurements
and the nearest 10 available head measurements. Head observations are
shown to provide valuable information for estimating both the transmi
ssivity and the recharge fields. Accurate numerical groundwater model
predictions of the aquifer flow system are obtained using the optimal
transmissivity and recharge fields as input parameters, and the optima
l head field to define boundary conditions. For this case study, both
the transmissivity field and the uncertainty of the transmissivity fie
ld prediction are poorly estimated, when the effects of random recharg
e are neglected.