“Scattered Wave Energy” Attribute Application to Conceptual Oil Field Model Construction

Author(s):  
V.A. Pozdnyakov ◽  
N.B. Krasilnikova ◽  
A.A. Antonenko
2019 ◽  
Vol 22 (03) ◽  
pp. 0998-1014 ◽  
Author(s):  
Feyi Olalotiti-Lawal ◽  
Tsubasa Onishi ◽  
Hyunmin Kim ◽  
Akhil Datta-Gupta ◽  
Yusuke Fujita ◽  
...  

2021 ◽  
Author(s):  
Jeffrey Uncu ◽  
Nicolas Grisouard

<p>The Surface Water and Ocean Topography (SWOT) mission is the next generation of satellite altimetry, set to launch in early 2022. It will be the first of its kind to provide global sea surface height (SSH) measurements fine enough to begin resolving the submesoscale. In this newly resolvable regime, “slow” flows (jets, vortices…) interact with internal waves by redistributing wave energy to other wave-vectors and frequencies. This introduces the challenge of distinguishing “slow” flows from waves, which is of key importance for inferring ocean circulation, from SSH measurements. I run numerical simulations of the one layer rotating shallow water equations to model the interaction between a single internal tide mode and vortices in (cyclo)geostrophic balance to characterize scattering and map its relevant parameter space. Preliminary results show wave scattering by vortices with Rossby numbers ranging from 0.1-4 that are not explained by the standard methods (frozen-field approximation, ray tracing…) which have been successful in the mesoscale. We find that the Rossby number, the Burger number, and the ratio of the length and velocity scales of the wave and vortex are all necessary to characterize the interaction in submesoscale regimes. Harmonic analysis is used to highlight the direction of the scattered wave energy.</p>


2019 ◽  
Vol 862 ◽  
pp. 34-74 ◽  
Author(s):  
Grgur Tokić ◽  
Dick K. P. Yue

We consider the hydrodynamics of wave energy converter (WEC) arrays consisting of periodically repeated single bodies or sub-arrays. Of special interest is the array gain due to wave interactions as a function of the spatial configuration of the array. For simplicity, we assume identical WECs oscillating in heave only, although the results should extend to general motions. We find that array gains can be as high as $O(10)$ compared to the same WECs operating in isolation. We show that prominent decreases in array gain are associated with Laue resonances, involving the incident and scattered wave modes, for which we obtain an explicit condition. We also show theoretically that Bragg resonances can result in large decreases in gain with as few as two rows of strong absorbers. For general WEC geometries, we develop a multiple-scattering method of wave–body interactions applicable to generally spaced periodic arrays. For arrays of truncated vertical cylinders, we perform numerical investigations confirming our theoretical predictions for Laue and Bragg resonances. For a special class of multiple-row rectangular WEC arrays, our numerical results show that motion-trapped Rayleigh–Bloch waves can exist and be excited by an incident wave, resulting in sharp, narrow-banded spikes in the array gain.


2015 ◽  
pp. 74-79
Author(s):  
I. A. Schetinin ◽  
I. N. Maksimyuk

The article is based on the practical experience of the Tivanskoye oil field geological model construction. The main part of the article is dedicated to the problem of creation of the WOC (water saturated contact) surface taking into account a significant gradient of the WOC’s depth marks over the field area. The possibility of a block-type structure of the deposit and a plicated type is considered as the most probable hypotheses. As a result a comparison is made of the forecast on the absolute depth mark of the WOC for each of the models and the actual information is presented on the results of pilot wells drilling.


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