A Popular History of Astronomy During the Nineteenth Century: Fourth EditionClerke, Agnes M. (Agnes Mary)
History
A Popular History of Astronomy During the Nineteenth Century: Fourth Edition
Clerke, Agnes M. (Agnes Mary)
Astronomy -- History -- 19th century
A more tangible, as well as a less disputable proof of solar radiative
intensity than any mere estimates of temperature, was provided in some
experiments made by Professor Langley in 1878.[724] Using means of
unquestioned validity, he found the sun's disc to radiate 87 times as
much heat, and 5,300 times as much light as an equal area of metal in a
Bessemer converter after the air-blast had continued about twenty
minutes. The brilliancy of the incandescent steel, nevertheless, was so
blinding, that melted iron, flowing in a dazzling white-hot stream into
the crucible, showed "deep brown by comparison, presenting a contrast
like that of dark coffee poured into a white cup." Its temperature was
estimated (not quite securely)[725] at about 2,000° C.; and no
allowances were made, in computing relative intensities, for atmospheric
ravages on sunlight, for the extra impediments to its passage presented
by the smoke-laden air of Pittsburgh, or for the obliquity of its
incidence. Thus, a very large balance of advantage lay on the side of
the metal.
A further element of uncertainty in estimating the intrinsic strength of
the sun's rays has still to be considered. From the time that his disc
first began to be studied with the telescope, it was perceived to be
less brilliant near the edges. Lucas Valerius, of the Lyncean Academy,
seems to have been the first to note this fact, which, strangely enough,
was denied by Galileo in a letter to Prince Cesi of January 25,
1613.[726] Father Scheiner, however, fully admitted it, and devoted some
columns of his bulky tome to the attempt to find its appropriate
explanation.[727] In 1729 Bouguer measured, with much accuracy, the
amount of this darkening; and from his data, Laplace, adopting a
principle of emission now known to be erroneous, concluded that the sun
loses eleven-twelfths of his light through absorption in his own
atmosphere.[728] The real existence of this atmosphere, which is totally
distinct from the beds of ignited vapours producing the Fraunhofer
lines, is not open to doubt, although its nature is still a matter of
conjecture. The separate effects of its action on luminous, thermal, and
chemical rays were carefully studied by Father Secchi, who in 1870[729]
inferred the total absorption to be 88/100 of all radiations taken
together, and added the important observation that the light from the
limb is no longer white, but reddish-brown. Absorptive effects were thus
seen to be unequally distributed; and they could evidently be studied to
advantage only by taking the various rays of the spectrum separately,
and finding out how much each had suffered in transmission.
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