The Ocala evening star. [volume] (Ocala, Fla.) 1895-1943, 1913-10-04
Tremendous Force Exerted at
the Bottom Of the Sea.
AIR THERE COULD NOT RISE.
1t Would Be Compressed to Such
Degree of Density by the Enormous
Weight That the Water Would Float
Upon lt-Lnits Of Diving Depths.

Upon it-ltr1Its OF Diving Depths.
From ordinary considerations +,
would seem that there is no limit to
the depths 20 which a diver or a sub
marine bont might go. Such. how
! ever. is not the case What prevents
| diving to great depths is the enormous
Iy increasing pressure of water No
diver without a suit can 20 over 80
feet. because the pressure on the body
is then about Eve tons To the square
foot on his body. EardrumS would he
STAYED in. and other fearful difficulties
would result
To remedy this the diving suit was
invented. but there is n limit also to
its depth. At depth of one mile the
pressure due to the water alone is lf:
tons to the square foot Even if div
in" suit waS devised to withstand this
enormous pressure trouble wOnld be
found in getting pipe line that long
and withStanding the pressure TINT
would not break of its own weight
In the case Of submarine boat i;
is slightly different Here only the
.,: D.
weight. consequently adding to the
Ill.,, :. 49,, ,;:. 49,,
pronelling the boat is reached If Il
larger engine is procured If itself
-, g.. :. :,
,.:.
e., ,. -.
-. ''''i " '''''' '''' Va II
''''''
N"' ave - az '"' "'''"ill - t"' SEA
III '"e ,'NF q 't>l' wafer 'n!N - >iAif
Nv" """ "''l t"''t">. SAT- ""''t
Nei-h> 'i-'''IE ''''' :" ~ "''' "'~
|" go ~ 'H' ''iF li'>S'ii' "''' |" 'i'T
N"'r' ~ any "'I'H - ~ ''"'l't'' tue
"t'1'll !" ie't ~ N'A'H ~" an" i i'".''
anu 'tIe "liH "'' - "ll"''' at oi'' III
l""'">
W" =, = '''''>' ''''
per o. 'uhic l"eI L" hlnitlpN by >lN'E
TWO ana i hAIi. me answer i l''"'o'
w" l'''!lluS' 81 - '"I'>' 10 Tue squire
io"' pressure NJ NM" Ii hoif'" VS.
SCI 'Hh WILTSHIRE" 'hlS.
ME -" me Su'IpF' ol 'h''f'Sll-
N"''' pressure = "'''''''' vi ih'''''>'''i-
o''N''N"'i"'> can '' 'i''ue l" '"iiilV'
'ioiI w" 'i' '''hi'! '>>''i" NJ
very '",l'i'' H:>'"''' .''' >o'"'''e ue''t
Ing as the l're>S'''" increases. III Dol
tie Is I@h1i| '"rked II VIII contain All
at orhihar! pressure oi hi'eeli l'"uiiu>
10 the square ihch' ana thit II the
pressure II eA'i ., 1 heh ne "ei-ii'
10 the bo'tie ana let II GOWN III Tue sea
ID! iitaii> oi >tilhS. oh piih-lhS II
|" 'he '"i' "-'lh II VIII ne i"t'in INA
,He supper mas Deeii 'o''eu ii.o 'ne
p"t'l' u! ihe water pressure. II 'h'
bottle Is hlIed with water ana stop
pVle' anu ~ W" II no sun 'iiiiiS thh'>
pare showing 'lat water i not com
pressure 10 any great extent.
II ny any means some air couId De
placed 1T the bottom Of sea five miles
deep It would not rise to the top for 1t
would he denSer-that Is. would weigh
more I" the cubic root than water
ANA the water would have to float on
III" AR: hence no man knows IT the
bottom OF our seas Is wet or not.
There IS only one thing that would
prevent the air from becoming this
dense. and that IS If 1t WAS cold enough
IT would llquefy. However. 1t * al
most lmpoSSlbIe-lS in fact. Impossible
for anything ut the bottom Of the sea
10 be colder than degrees c.. for if il
got colder the water around II would
become colder ana larger ana ""ISe-
HuehliF HSh'ei ana rise ana us piace
Wouid be taken by degree water
"hlch "onId bring The OBJECT 70 thA'
temperature 80 we nave no argument
d-HlilSt inc suggestion. Tor the temper
AZURE az or beio" winch air iquene> l.
Iftt W tt'I wv anu wv degrees lbploN