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Hindenburg — Part 3
Page 38
38 / 76
telegraph communications. It included a
ort-Wwive abd a iong-wave transmitter,
each with 200-watt antenna capacity; two
all-wave receivers and two direction Snders.
The frequeucy of the short waye trans-
maicter was 4160. tg 17500 kilocycles, The
frequency of the long wave transmitter wae
120 to 600 kilocycles. The frequency range
of the receivers was 12 to 20000 kilocycies.
Power for the transmitters was obtained
from a 220-volt direct current supply gen-
erated by the ship's electric power Plant.
The receivers obtained their high voltage
from batteries, and power for their filaments
was obtained through a series resistor from
the 24-volt ship's generator. For the short
wave transmitter, there was a trailing an:
tenpa of 26 meters length, Kor the loug-
wave transmitter, a trailing antenna of
about #0 meters length was uged. These
trailing antennas were located | rectly be-
jow the transmitters and ram throu an
aperture in the Heel of the ship. here
was a fixed antenna extending from the
contro] car about 15 meters toward the
stern, The fixed antenna was used only
for receiving purposes, In addition to thix
equipment, there was Iocated in the bow un
emergency transmitter and receiver, cur-
rent for which was obtained from a gen-
erator driven by pedal power. This emer-
goney set employed a trailing antenna about
meters in length.
Lifting Gas
The ship was inflated with hydrogen.
According to the evidence adduced, this
eas bas the following characteristics: It ix
colorless, odorless, and tends to diffuse in
all directions, The only way that hydrogen
could be detected by smell would be due ta
the presence of impurities as a result of
the process by which It was produced, or
contamination from some source such as
rubberized fabric. Hydrogen, for lifting
purposes, bes a density of approximately 5
Bounds per 1,000 cuble feet, depending on
the temperature and pressure. Its lifting
power is the difference between the density
of air and fta own density. The density
of alr ia about 75 pounds per 1,000 cubie
feet. Assuming pure hydrogen, its lifting
power would therefore be about 70 pounds
per 1,000 cubic feet. An opinion was ad-
vanced that the general order of pressure of
the gas within the cells of the ship was
somewhere between half an inch and i inch
of water pressure, It was stited that the
density of hydrogen corresponds to air at a
temperature of 5,000° F. and that the
chimney effect of its escape through the Fas
shafts of the ship was go very great that
there was no possibility of its moving
down the shafts into the lower parts of
the ship.
The fammable Mmits of a mixture of
hydrogen and air are probably between
4.5 percent and 62 percent of bydrogen.
Other experiments have shown veriances
from 8-9.8 percent to 68 percent. The tem-
perature ot which chemical activity be-
tween hydrogen and oxygen takes place is
between 507° to 557° C. This temper.
ature range ig dependent upon the amount
of hydrogen present. The range of ac-
tivity ef combustion will be from the lower
limit of 4.5 pereent at which there will
probably be an invisible union without evi-
dence of flame. A combustible mixture
would be more hazardous in an atmospheric
condition of ®8 percent relative humidity,
and temperature 60° F. than in dry air
with relatively low humidity, since dry
hydro-oxygen ig more difficult to {gnite and
its ignition temperature ig higher. In an
erplosion the flame propagates in all direc-
tions in the combustible range between
15 to 45 percent of hydrogen. These
.
= ’ AIR COMMEECE BULLETIN J 25
figures were arrived at experiinentallp with
gluas or inetallic apparatus which did not
have effect upon the combustion tempt.
atures. Catalytic metals having adsorption
propertica woud. ve Hkely to affect the com-
bustion at lower Temperatures, Finished
dorainmin would not be expected to have
material catalytic effect upon hydrogen.
Bounding
The whole metallic structure of the craft
was bonded.
Part Ill—The Landing Maneuver
Meteorological Conditions
With respect to the meteorological con-
ditions fn which the Junding was conducted,
a summary of ihe general weather 1s given
ag well as the Jocul conditiuus prevailing
at Lakchurst at the time of the accident.
GENERAL
The 7:50 a.m, E. 8. T. United States
Weather Bureau) may of the vicinity, in-
cluding the northeastern tier of Staies,
shows a disturbance over ceniral New
York and northeastern Pennsylvania, with
a cold front extending frum this center
southwestward to West Virginia, This front
separated neutralized polur vir tu tle east
of the cold front which had become warmer
and more Moist and neutralized colder wir
to the west of the front. The warmer atid
more moist miss of air covered the Middle
Atlantic States, southedstern New York, aud
southern New England.
The cold front advanced enstward during
the day from central Pennsylvanin ut a
rate of 12 to 15 miles per hour, passing
Lakehurst shortly after 3:30 p.m.) There
was not quite sufficient surface beac
during the early afternoon to set of a
thundersturm at Lakehurst, and it was not
until the front passed and some slivht lirs-
ing of the air mass occurred that a thunder-
storm began. The records of the naval air
station show that the thunderstorm begau
at 3:40 p.m. and ended at 4:45 p. m.
Telegraphic reports indicate, the thuuder-
storms in and to the west of New Jersey
Were not severe; nor were they cf a well-ile-
fined squall character. Between 12 p. m.
and 1:30 p.m. E. 8, T., these storms ex-
yended in a definite belt over the region of
Harrisburg, Pa, northeastward toe Bear
Mountain, N. Y., and New Hackensack, N. ¥.
Between 1:30 and 2:40 p. m. none was re.
ported. Between 2:40 and 3:40 P: m.. Cam-
den and Fort Monmouth, N. J., onfy, reported
thunderstorms. Between 3:36 and 4: 80
p. m., Lakehurst, Mitchel Field, N. ¥.. and
Floyd Bennett Field, N, Y¥., reported them.
Between 4:40 and 5:40 p. m, nene was
reported ; und between 5:40 and 6:40 p. m.,
Floyd Bennett only reported one. Sune
marized. the thunderstorms in eastern New
Jersey were of a local character and not
severe.
The New York Weather Bureau offie:
bulletin issued at 1:20 p.m. May 6, fol-
OWS :
“1800 G. C. T. Moderate wind shift with
focrensing and Jowering clouds possible
tbundershowers New York and vicinity ex-
ected in middle or late afternoon Stop
ew York scattered cumulus and = smalt
cumulo nimbus approaching from west -—
visibility excellent surface wind sonth 12
miles—barometer 29,68 falling steadity-—
temperature 66."
LOCAL
With the passage of the front at Lake-
burst, the wind shifted to the werlbwest
with gusts up to 20 Enots, and was aec-
ask
Lag teem tn a Peto
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