ISSN:
1573-1626
Source:
Springer Online Journal Archives 1860-2000
Topics:
Architecture, Civil Engineering, Surveying
,
Geosciences
,
Physics
Description / Table of Contents:
Summary The possibility of solving the stationary heat equation with the convective term is demonstrated in the case that the velocity field of the continuum, and the temperature and heat flow on the Earth's surface are known, and that an assumption is made about the magnitude of heat flows on another part of the boundary of the two-dimensional region being investigated, whereas no boundary condition is imposed on the remainder of the region's boundary. The problem has been solved numerically for a kinematic model of the lithosphere in the region of mid-ocean ridges, based on the assumption of a broad deflected convective flow moving at a distance of more than about 150 km from the ridge modelled as a plate.
Notes:
Резюме Покaзaнa возможносmь решенuя сmaцuонaрно о урaвненuя nереносa mеnлa в случaе, ко ¶rt;a uзвесmно nоле скоросmеŭ конmuнуумa u нa nоверхносmu Землu uзвесmны mемnерamурa u mеnловоŭ nоmок. Нa ¶rt;ру оŭ чaсmu рaнuцы рaссмamрuвaемоŭ ¶rt;вухмерноŭ облaсmu вво¶rt;umся nре¶rt;nоложенuе о велuчuне mеnлово о nоmокa a нa осmaльноŭ чaсmu рaнuцы крaевое условuе не зa¶rt;aно. Эma nроблемa былa чuсленным меmо¶rt;ом решенa ¶rt;ля кuнемamuческоŭ мо¶rt;елu лumосферы в облaсmu сре¶rt;uнно-океaнuческuх хребmов, основaнноŭ нa nре¶rt;сmaвленuu шuроко сверmывaюще ося конвекmuвно о nоmокa нa рaссmоянuях оm хребma nревышaющuх 150 км ¶rt;вuжуще ося кaк орuзонmaльныŭ nоmок.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1007/BF01642993
