Zobrazeno 1 - 10
of 53
pro vyhledávání: '"S. L. Butler"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 7, Pp n/a-n/a (2024)
Abstract Computing the velocity field is an expensive process for mantle convection codes. This has implications for particle methods used to model the advection of quantities such as temperature or composition. A common choice for the numerical trea
Externí odkaz:
https://doaj.org/article/d606eb9680c14b429473f3adba919099
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 4, Pp n/a-n/a (2023)
Abstract In this study, we manufacture an exact solution for a set of 2D thermochemical mantle convection problems. The derivation begins with the specification of a stream function corresponding to a non‐stationary velocity field. The method of ch
Externí odkaz:
https://doaj.org/article/c937a6452e46457bbacbc300561266bf
Improving Mass Conservation With the Tracer Ratio Method: Application to Thermochemical Mantle Flows
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 21, Iss 2, Pp n/a-n/a (2020)
Abstract Modeling the evolution of composition in a convecting mantle is difficult since the associated chemical diffusivity is very small. Consequently, compositional evolution is often modeled using the advection equation which is prone to overdiff
Externí odkaz:
https://doaj.org/article/25bea160ae24478394791300da827544
Autor:
S. L. Butler
Publikováno v:
Physics of Fluids. 34:112103
The shapes of rotating fluid drops held together by surface tension are an important field of study in fluid mechanics. Recently, experiments with micrometer-scale droplets of liquid helium have been undertaken and it has proven useful to compare the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::429ab1051303fa2ad00f5605b38a73a6
https://doi.org/10.1063/5.0121208
https://doi.org/10.1063/5.0121208
Autor:
S. L. Butler
Publikováno v:
Geophysical Prospecting. 67:1431-1438
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53c7ede23e5b83fef40188b818e44573
https://doi.org/10.1111/1365-2478.12786
https://doi.org/10.1111/1365-2478.12786
Numerical models of mantle convection help our understanding of the complex feedback between the plates and deep interior dynamics through space and time. Did the early Earth have plate tectonics, a stagnant lid, or something in between? The surface
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fa9aec643a7169bc93d6061a0ae73e05
https://doi.org/10.5194/egusphere-egu2020-10638
https://doi.org/10.5194/egusphere-egu2020-10638
Improving Mass Conservation With the Tracer Ratio Method: Application to Thermochemical Mantle Flows
Publikováno v:
Geochemistry, Geophysics, Geosystems. 21
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba7de8407df08927625709d50a9bc473
https://doi.org/10.1029/2019gc008799
https://doi.org/10.1029/2019gc008799
Publikováno v:
Computers & Geosciences. 154:104797
Numerical simulations are a highly valuable tool for improving our understanding of mantle dynamics. COMSOL Multiphysics® is a commercial software suite designed to numerically model experiments featuring multiple branches of physics. This modeling
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::900865d73a862810d21c3e6df928b6a2
https://doi.org/10.1016/j.cageo.2021.104797
https://doi.org/10.1016/j.cageo.2021.104797
Autor:
S. L. Butler
Publikováno v:
Journal of Applied Geophysics. 143:149-155
It is instructive to consider the sensitivity function for a homogeneous half space for resistivity since it has a simple mathematical formula and it does not require a priori knowledge of the resistivity of the ground. Past analyses of this function
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0fbc05ca22f9b742abb7d7ceade559f9
https://doi.org/10.1016/j.jappgeo.2017.06.005
https://doi.org/10.1016/j.jappgeo.2017.06.005
Autor:
S. L. Butler
Publikováno v:
Physics of the Earth and Planetary Interiors. 264:7-17
Shear-induced porosity bands have been observed experimentally and have been the subject of a number of theoretical and numerical analyses in which a number of rheological laws governing the partial melt system have been proposed. These bands have be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78ea18fa4dfdc59c5f2cda28c67d0ca3
https://doi.org/10.1016/j.pepi.2016.12.006
https://doi.org/10.1016/j.pepi.2016.12.006