2016
DOI: 10.1016/j.cageo.2016.01.009
|View full text |Cite
|
Sign up to set email alerts
|

Evaluation of parallel direct sparse linear solvers in electromagnetic geophysical problems

Abstract: High performance computing is absolutely necessary for large-scale geophysical simulations. In order to obtain a realistic image of a geologically complex area, industrial surveys collect vast amounts of data making the computational cost extremely high for the subsequent simulations. A major computational bottleneck of modeling and inversion algorithms is solving the large sparse systems of linear ill-conditioned equations in complex domains with multiple right hand sides. Recently, parallel direct solvers ha… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
17
0

Year Published

2016
2016
2022
2022

Publication Types

Select...
6
1

Relationship

0
7

Authors

Journals

citations
Cited by 56 publications
(17 citation statements)
references
References 50 publications
0
17
0
Order By: Relevance
“…In addition to the above theoretical considerations, we know that different direct solver implementations exhibit distinct scalability properties, as shown in [34]. Therein, the authors consider specific finite differences and finite element systems and demonstrate via numerical experimentation that for those systems, the parallel scalability of solvers Watson Sparse Matrix Package (WSMP) [22] and MUMPS exhibit large discrepancies.…”
Section: Solution and Communication Cost Estimatesmentioning
confidence: 99%
“…In addition to the above theoretical considerations, we know that different direct solver implementations exhibit distinct scalability properties, as shown in [34]. Therein, the authors consider specific finite differences and finite element systems and demonstrate via numerical experimentation that for those systems, the parallel scalability of solvers Watson Sparse Matrix Package (WSMP) [22] and MUMPS exhibit large discrepancies.…”
Section: Solution and Communication Cost Estimatesmentioning
confidence: 99%
“…The numbers represent the approximate number of unknowns, in millions, in the linear systems associated to each matrix; for example, the linear system corresponding to matrix S21 had about 21 million unknowns. So far, for 3-D geophysical EM problems, the largest reported complex-valued linear system that has been solved with a direct solver had 7.8 million unknowns (Puzyrev et al 2016).…”
Section: Models and System Matricesmentioning
confidence: 99%
“…Therefore the application of direct solvers to 3-D problems has traditionally been considered computationally too demanding. However, recent advances in sparse matrix-factorization packages, for example, MUMPS (Amestoy et al 2001(Amestoy et al , 2006, PARDISO (Schenk & Gärtner 2004), SuperLU (Li & Demmel 2003), UMFPACK (Davis 2004) and WSMP (Gupta & Avron 2000), along with the availability of modern parallel computing environments, have created the necessary conditions to attract interest in direct solvers in the case of 3-D EM problems of moderate size, see for example, Blome et al (2009), Streich (2009), da Silva et al (2012, Puzyrev et al (2016) and Jaysaval et al (2014).…”
Section: Introductionmentioning
confidence: 99%
“…By noticing that basis functions Ψ kq , k = 1, ..., K q , q = 1, .., N s have support over Ω q 2 and the subdomains Ω i 2 , i = 1, ..., N s are non-connected, (25) can be expressed as:…”
Section: Ddffe Formulation With Multiple Subdomainsmentioning
confidence: 99%
“…Typically, the number of sources is in the order of tens to hundreds for land CSEM studies, while it reaches thousands in modern large-scale marine CSEM surveys [21]. Puzyrev et al [25] evaluated modern direct solvers on large-scale geophysical simulations that previously were considered unachievable with these methods.…”
Section: Introductionmentioning
confidence: 99%