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Cooling of the Earth, Urey ratios, and the problem of potassium in the core
Author(s) -
Breuer Doris,
Spohn Tilman
Publication year - 1993
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/93gl01680
Subject(s) - mantle (geology) , earth's internal heat budget , crust , geology , continental crust , silicate , thermal , inner core , structure of the earth , geophysics , thermodynamics , mineralogy , mantle convection , physics , lithosphere , tectonics , paleontology , astronomy
The compatibility of mantle Urey ratios U m calculated from thermal evolution models with those calculated from geochemical models is considered. The initial heat generation rate in the mantle used for the thermal evolution models was derived from two geochemical models of the present day primitive mantle with concentrations of U of 20 ppb (2.7 times chondritic) and 26 ppb (3.5 times chondritic), respectively. The depletion of the mantle through continental crust production was allowed for; the effect of including the continental crust on U m is a reduction of its value by about 0.1. To balance the observed average value of the surface heat flow q s it was assumed that the core may contain K up to cosmochemically constrained quantities. For 26 ppb U in the present primitive mantle no core heat sources are required. The present value of U m for this model is 0.57 and the core heat flow is about 12% of q s . With 20 ppb U in the present primitive mantle, heat production equivalent to one to two silicate earth budgets of K is required in the core to balance q s and U m is between 0.35 and 0.4. The core heat flow is then between 25% and 33% of q s .