lSTUDY OF THE FEATURES OF GEOLOGICALLY CONSISTENT HISTORY MATCHING OF FLOW MODELS. PART 2. PILOT POINTS

Author(s):  
I.M Shiryaev ◽  
I.M. Indrupskiy ◽  
E.S. Zakirov
2003 ◽  
Vol 9 (1) ◽  
pp. 83-90 ◽  
Author(s):  
M. Lygren ◽  
K. Fagervik ◽  
T.S. Valen ◽  
A. Hetlelid ◽  
G. Berge ◽  
...  

2001 ◽  
Author(s):  
K. Fagervik ◽  
M. Lygren ◽  
T. S. Valen ◽  
A. Hetlelid ◽  
G. Berge ◽  
...  

1994 ◽  
Vol 353 ◽  
Author(s):  
K. Andrew Jackson

AbstractWe present a new method for conditioning realizations of the logarithm Y of transmissivity on head data. Each realization is conditioned by subtracting a linear combination of certain basis functions, each corresponding to a measurement, obtained by a process based on co-kriging. The required cross covariance between head and Y can be numerically computed very efficiently using the adjoint method. The coefficients in the linear combination are chosen to try to rninimise the differences between computed and measured heads. The most efficient methods for such non-linear optimisation problems are those that exploit information about the second derivatives of the function being minimised. We show how these second derivatives can be computed very efficiendy using the adjoint method for certain classes of finite-element schemes. We illustrate our method by application to the WIPP-2 test case of the international INTRAVAL project. We show that the match between computed and measured heads is greatly improved. We compare our method with approaches that use pilot points. Our method is exact if the variability of the Y field and the deviations of the measured heads from the values computed for the mean of the Y field are both small, whereas pilot-point methods are only approximate. However, our method may be more expensive computationally. Finally, we discuss the extension of our method to conditioning on transient head data and to dealing with boundary conditions.


2001 ◽  
Author(s):  
K. Fagervik ◽  
M. Lygren ◽  
T.S. Valen ◽  
A. Hetlelid ◽  
G. Berge ◽  
...  

2000 ◽  
Vol 627 ◽  
Author(s):  
M. E. Swanson ◽  
M. Landreman ◽  
J. Michel ◽  
J. Kakalios

ABSTRACTWhen an initially homogeneous binary mixture of granular media such as fine and coarse sand is poured near the closed edge of a “quasi-two-dimensional” Hele-Shaw cell consisting of two vertical transparent plates held a narrow distance apart, the mixture spontaneously forms alternating segregated layers. Experimental measurements of this stratification effect are reported in order to determine which model, one which suggests that segregation only occurs when the granular material contained within a metastable heap between the critical and maximum angle of repose avalanches down the free surface, or one for which the segregation results from smaller particles becoming trapped in the top surface and being removed from the moving layer during continuous flow. The result reported here indicate that the Metastable Wedge model provides a natural explanation for the initial mixed zone which precedes the formation of the layers, while the Continuous Flow model explains the observed upward moving kink of segregated material for higher granular flux rates, and that both mechansims are necessary in order to understand the observed pairing of segregated layersfor intermediate flow rates and cell separations.


2017 ◽  
Author(s):  
Boris V. Dzyubenko ◽  
Guenrikh A. Dreitser

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