The crepuscular planet. A model for the exhausted continental crust

We propose a model for an exhausted upper continental crust. The Crepuscular Earth represents a degraded planet where all resources have been extracted and dispersed, and all fossil fuels have been burned. The starting point of the model of crepuscular crust is the composition given by the geochemist Grigor’ev, which is constrained by the conservation of mass statement between the chemical composition of the crust in terms of elements and in terms of minerals. Additionally, the model is given geological consistence, by introducing a series of assumptions based on geological observations. As a result, the obtained crepuscular crust is composed of the 294 most abundant minerals. Together with the model of exhausted atmosphere and hydrosphere developed in a previous paper, the study will serve as a reference for calculating the exergy of the current mineral capital on Earth and its degradation velocity.

[1]  M. Javoy Chemical earth models , 1999 .

[2]  Antonio Valero,et al.  The crepuscular planet. A model for the exhausted atmosphere and hydrosphere , 2011 .

[3]  H. Newsom,et al.  The depletion of tungsten in the bulk silicate earth: Constraints on core formation , 1996 .

[4]  Scott M. McLennan,et al.  Relationships between the trace element composition of sedimentary rocks and upper continental crust , 2001 .

[5]  S. Taylor,et al.  The continental crust: Its composition and evolution , 1985 .

[6]  N. N. Greenwood,et al.  Chemistry of the elements , 1984 .

[7]  Benren Zhang,et al.  Chemical composition of the continental crust as revealed by studies in East China , 1998 .

[8]  W. Fahrig,et al.  The chemical evolution of the Canadian Shield , 1968 .

[9]  Andrés F. Agudelo,et al.  THE CREPUSCULAR PLANET PART I: A MODEL FOR THE EXHAUSTED ATMOSPHERE , 2009 .

[10]  K. Condie Earth as an Evolving Planetary System , 2004 .

[11]  Charles H. Langmuir,et al.  The chemical composition of subducting sediment and its consequences for the crust and mantle , 1998 .

[12]  G. Pattenden,et al.  An Estimate of the Chemical Composition of the Canadian Precambrian Shield , 1967 .

[13]  F. J. Turner,et al.  Igneous and Metamorphic Petrology , 1960 .

[14]  Jan Szargut,et al.  Exergy Analysis of Thermal, Chemical, and Metallurgical Processes , 1988 .

[15]  Göran Finnveden,et al.  Exergies of natural resources in life-cycle assessment and other applications , 1997 .

[16]  K. H. Wedepohl The Composition of the Continental Crust , 1995 .

[17]  Antonio Valero,et al.  Exergoecology: A thermodynamic approach for accounting the Earth's mineral capital. The case of bauxite–aluminium and limestone–lime chains , 2010 .

[18]  P. J. Petit,et al.  Second law analysis, for pinpointing the true inefficiencies in fuel conversion systems , 1976 .

[19]  W. McDonough,et al.  Lithium isotopic composition and concentration of the upper continental crust , 2004 .