Study on Ceramic Moon light scattering during
volcanic activity.
by
Kaadambala.
C. K. J,
Asst.
Professor, Physics Department, MITS Engineering College,
Rayagada,
Odisha State. India.
Dt. 16 February 2014.
Dt. 16 February 2014.
ABSTRACT
The object of
present study was to study the ceramic Moon light scattering during days of
volcanic ash dispersal over the sky in Visakhapatnam and compared with observations
made earlier two days in Rayagada before the volcanic activity. The 13 and 14 February 2014 February observations made using a grating element on the
terrace of MITS Engineering College, Rayagada, around 8 PM using grating
element of 15000 lines of our college.
We define a new quantity named lortusity as the ratio of the real path length to the apparent path length in a ceramic material. Since the findings are based on the light intensity variations with coupled movement of intense Volcanic and other preliminary affects of it. The ‘connectivity‘ of pore space, viz., the number of pores meeting at a point, in a porous media by regular packing is predominant in graphite.
Words: lortusity, connectivity.
Words: lortusity, connectivity.
INTRODUCTION AND PRESENTATION
Four ceramic slabs have been used viz.,
Graphite, Marble, White and Blue ceramic plates. The Moon light reflected from
the slabs has been recorded for their spectral display. The observations repeated again on 14 instance, and the spectra recorded using the Digi camera of 12 Mega Pixels. In both the cases the author successful to
obtain the spectra that provided a means to study the ceramic Moon light
scattering. Afterwards when he came to Visakhapatnam on the 15 February, to repeat again the observations, he is fortunate have the effect of
Volcano activity dispersion of the sky and the spectra recorded again.
Listed below: Fig.1a. (only
three from Rayagada), Fig.1b (four photographs from Rayagada) and Fig.2 (only
two photographs from Visakhapatnam with volcano effect) given below project
briefly, the spectra recordings made by the author, are of a unique
character.
FROM RAYAGADA
The
molecules of the graphite are tightly bounded so the spectrum is quite distinct.
The
molecules of the ceramics are bound softer than graphite so the spectrum obtained
here is weaker than the spectra of graphite.
The
molecules are bound softer than white ceramic, so the spectrum obtained is more
weaker than the spectrum of white ceramics.
The dominant colors are the Red and Green.
The
molecules of the graphite are tightly bounded so the spectrum is quite
distinct.
Fig 1(b) spectrum 14 February, Marble ceramic;
Fig 1(b) spectrum 14 February, Marble ceramic;
The
molecules of the marble are bounded slightly less than than graphite molecules
so the spectrum is little distinct. The
blue light seems to have a spread out.
The
molecules of the ceramics are bounded softer than Marble so the spectrum
obtained here is weaker when compared to Marble. The dominant blue light is
very interesting.
Fig. 1(b) spectrum 14 February, Blue ceramic;
The
molecules are bound softer than white ceramic, so the spectrum obtained is
weaker than spectrum of White ceramic. Predominant Red and Green lights are
very distinct.
FROM
VISAKHAPATNAM
Fig.2a
spectrum 16 February, Graphite
ceramic; 00.20am
The
spectrum of granite which appears little bit blurred because of the volcanic
clouds passing by the moon . The yellow light is extremely feeble.
Fig.2b spectrum 16 February, White
ceramic; 00.22am
The
White ceramic spectrum appears quite sharp and almost overlapping due to the
volcanic clouds passing by the moon. Interesting is the Yellow light dominance.
As a contrast the image of 15 Jan 2010 is presented.
As a contrast the image of 15 Jan 2010 is presented.
15 Jan 2010 at 14 57 PM noon Image 1012
Visakhapatnam Ocean View with a sailing ship.
CONCLUSIONSWe define a new quantity named lortusity as the ratio of the real path length to the apparent path length in a ceramic material. Since the findings are based on the light intensity variations with coupled movement of intense Volcanic and other preliminary affects of it. For example the Fig. 2b shows very sharp spectrum while the Fig. 2a shows the broadened spectrum.
The porosity of the ceramic samples
cannot be neglected and we have intelligently chosen the samples from tough
granite to loose-fitting other ceramics. The ‘connectivity‘ of pore space,
viz., the number of pores meeting at a point, in a porous media by regular
packing is predominant in graphite.
Further discussion on the nature of porosity and details of it are to be
specified explicitly in my thesis work. The details form the subject of extensive
research investigation of Ph. D Degree in Physics, by the author.
ACKNOWLEDGEMENT
The author is grateful to his
Research Guide Dr. Ch. V. Srinivas, Principal, Dr. B. V. Raju College,
Bhimavaram and his co-guide Dr. P. Dakshina Murthy, Professor, JNTU, Kakinda. The author worked successfully, for about three years period in Bhimavaram, Dr BVR College.
He is specifically grateful to Prof. Dr. K. L. Narayana, Retd. Prof. of Physics, Shivaji University, Kolhapur - 416004, presently in Visakhapatnam, for his stimulating discussions and presentation of the work of my research.
He is specifically grateful to Prof. Dr. K. L. Narayana, Retd. Prof. of Physics, Shivaji University, Kolhapur - 416004, presently in Visakhapatnam, for his stimulating discussions and presentation of the work of my research.
REFERENCES
“Physics of Finely
divided Matter”, Proc. in Physics 5, Ed. N. Boccara & M . Daoud,
Springer-Verlag, New York and Tokyo, 1985.
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