The University of Texas at El Paso

February 27, 1985

Department of Physics
(915) 747-5715
El Peso, Texas 79968-0515

[ name and address of addressee removed to protect his privacy ]

Dear Mr. [ name removed to protect his privacy ]:

These are fiqures on dust influx onto the Earth and also the Moon. The figures I am using below for the calculations come from Hawkins, G.S. ed., 1976. Meteor Orbits and Dust, Smithsonian Contributions to Astrophysics. Volume II, Smithsonian Institution and NASA, Washington, D.C. These collected papers are based on radar, rocket and satellite data well into the "space age".

METEORIC PARTICLE MASS FLUX ON EARTH IN ONE YEAR

(10-12) x (102) x (4π(6.4 x 108)2) x (1.3 x 10-6) x 104 x (3.2 x 107) x (10-6)

a) 10-12 = estimated near earth meteoric flux in particles -cm2

-sec-1 -2πster-1 (in the above reference, n. 268)

b) 102 = the measured flux average frequently showed increase by a factor of 170 for extended periods of time (so this factor is used to estimate changes in the flux) (p. 269).

c) 4π(6.4 x 108)2 = area of Earth's surface.

d) 1.3 x 10-6 = average mass if meteoric particle in grams.

e) 104 = factor from observation and theory for gravitational enhancement of particles sink for the Earth (p. 222).

f) 3.2 x 107 = the seconds in a year.

g) 10-6 = conversion from grams to tons.

In one year 2.14 x 108 tons would come onto the Earth. For the Moon,

(10-12) x (102) x (4π(1.6 x 108)2)x (1.3 x 10-6) x (103) x (3.2 x 107) x (10-6).

So, then 1.34 x l06 tons come in on the Moon in one year.

So, there is plenty of dust to arrive in the alleqed "4.5 x 109" year age of Earth and Moon on the basis of later data than I used before.

Thickness of dust on Moon after 4.5 x 109 years:

ρ (volume of dust)= 4πR2
hρ = IT

where R = radius of the moon, ρ = density of meteoric matter, I = influx rate of dust on the moon, T = 4.5 x 109 years, and h = thickness of dust layer on moon.

So, h = IT / (4πR2 ρ)

For ρ = density of iron = 0.25 lb/in3

h = (1.34 x 106)(4.5 x 109)(2 x 103) (in) / 4π(103 x 5280 x 12)2

= 854.22 in = 71.2 ft

However, for ρ = ordinary density of meteoric material = 0.07 lb/in3

h = 71.2 x 4 = 284.8 ft.

There is another source for the dust-- namely the break up of the moon's surface from high-energy radiation from the Sun. This has been estimated to contribute several miles of dust in 4.5 x 109 years (Lytlleton, R. A., The Modern Universe, Harper and Row Publisher, 1956, p. 72, New York).

Yes, in spite of Mr. Menninca emotional outburst there should be much dust on the Moon on the basis of the evolutionary time-scale but there is only a trace.

If you use the figures (Cassidy, W. A., Cosmic Dust, Science, V 144, June 19, 1964, p. 1476) from a symposium at Brown University the influx rate was estimated as more than 109 tons/year. This will give when transferred to the moon an influx rate of about 6.7 x 106 tons/year. This means a dust layer of thickness after 4.5 x 109 years of approximately 356 ft or 1424 ft, depending on which of the values for density is used.

I hope this is of some help to you.

Sincerely,

Harold S. Slusher, Ph.D.
Assistant Professor of Physics

HSS/ic