Pages that link to "Item:Q1879285"
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The following pages link to A BME solution of the inverse problem for saturated groundwater flow (Q1879285):
Displaying 12 items.
- An iterative particle filter approach for coupled hydro-geophysical inversion of a controlled infiltration experiment (Q728913) (← links)
- On the use of information theory to quantify parameter uncertainty in groundwater modeling (Q742779) (← links)
- A geostatistically based inverse model for three-dimensional variably saturated flow (Q1291915) (← links)
- Minimum relative entropy and probabilistic inversion in groundwater hydrology (Q1291919) (← links)
- An application of Bayesian inverse methods to vertical deconvolution of hydraulic conductivity in a heterogeneous aquifer at Oak Ridge National Laboratory (Q1430194) (← links)
- Empirical orthogonal functions analysis applied to the inverse problem in hydrogeology: Evaluation of uncertainty and simulation of new solutions (Q1863223) (← links)
- Uncertainty management of a hydrogeological data set in a Greek lignite basin, using BME (Q2001997) (← links)
- Space-time forecasting using soft geostatistics: a case study in forecasting municipal water demand for Phoenix, Arizona (Q2319544) (← links)
- Stochastic inverse method for estimation of geostatistical representation of hydrogeologic stratigraphy using borehole logs and pressure observations (Q2323565) (← links)
- Environinformatics in ecological risk assessment of agroecosystems pollutant leaching (Q2505885) (← links)
- A BME solution of the stochastic three-dimensional Laplace equation representing a geothermal field subject to site-specific information (Q2505936) (← links)
- Efficient estimation of hydraulic conductivity heterogeneity with non-redundant measurement information (Q2663761) (← links)
