INTERNAL
CHEMICAL COMPOSITION OF PLANET MARS
NAME OF
THEORETICAL PARTICLE ASTROPHYSICIST : MUNISHKUMAR.B.CHINNAKAR.
PLACE OF
INVENTIONS: MUNISHKUMAR.B.C’S FIRST FLOOR BUILDING NEAR BHAIRI WELL BOYER
STREET,SHORAPUR,PIN:585224 DIST:YADAGEER,KARNATAKA STATE INDIA.
CO-WORKERS:NO
CO-WORKERS.
DATE OF
ENTRY OF INVENTIONS:OCT,28,2013,
DATE
OF INVENTION: OCT,27,2013,
BRANCH:PARTICLE
ASTROPHYSICS
SUB
BRANCH: PARTICLE ASTRO-GEO- PHYSICS.
PAPER
NO:PACFMJ/G 156/4006
From
the Paper [1] ,it is clear that Mars soil is rich with Fe.Based on the effect
of dark energy on the variation thermal gradient,I found Chemical composition
of Crusts of Mars Planet.Here Instead of 25 degee centigrade as in case of
Earth,I used 25+10=35 degree centigrade.Further I used a Theory variation of
creation temperature with Atomic number and its result as for every 10K
variation in Z=6.5=6 to 7.
Following
are the chemical compositions of Crusts of Mars.
(1) At the
surface at T=2.83 x 10^2K,Abundant Elements are Fe and Co with traces of
Ni,Pd,Er,Tm,Pa,fm,Se
(2) At the
crust at T=1848K at a depth d=6 x 10^3m Abundant Elements are Ge,As,Se,Br,Te,I,W,Re,Os,Bk
alpha,Bk beeta,Zr,Nb
(3) At the
crust at T=3080K at a depth d=10x10^3m Abundant Elements are Molten lava of
Os,Ir,Re,Pt,Au,Mo,Ru,Te,S
(4) At the crust at T=3.0800 X10^4K at a depth
d=100x10^3m Abundant Elements are in Molten lava and Plasma state
(5) At the crust at T=3.0800 X10^5K at a depth
d=1000x10^3m Abundant Elements are in Molten lava containing
Hydrogen,Helium,N,O,inert gases and Plasma in discharge state
(6) At the crust
at T=3.0800 X10^-2K to T<3 .0800="" a="" at="" d="" depth="" x10="">1000x10^3m to 1900x10^3m Abundant Elements are in
Superconducting state and are usually Co,Ni,Pd and other superconducting elements3>
(7) At a
distance d>1900X10^3m,at temperature 10^-12K,crust is in Black hole state.
REFERENCE:
[1]ROLE
OF DARK ENERGY IN THE FORMATION OF MARS SOIL , BY MUNISHKUMAR.B.C PUBLISHED IN
HIS ONLINE JOURNAL PARTICLE ASTROPHYSICS/BLOGGER/SITE IN GOOGLE DATED20/10/2013
[2] GEOTHERMAL GRADIENT,IN WIKIPEDIA
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