scholarly journals XIII. The Bakerian Lecture.—Researches in spectrum-analysis in connexion with the spectrum of the sun.—No. III

1874 ◽  
Vol 164 ◽  
pp. 479-494 ◽  

The Researches in Spectrum-Analysis in which I have been engaged are opening out into so many lines of work that I think it desirable to communicate to the Royal Society the present state of the inquiry on its most general aspect, and also to enter somewhat into detail on some of the points to which my attention has specially been directed, the more so as the methods employed are such as can be, and I sincerely trust will be, taken up by other workers. To commence, then, by a general statement, I may remark that I have in the first place endeavoured to determine whether the new method of spectroscopic observation, which I have before described to the Royal Society, is really as competent as it promised to be in the quantitative direction, what are the conditions essential to its successful employment, and how far it would take us.

1874 ◽  
Vol 22 (148-155) ◽  

Archibald Smith, only son of James Smith, of Jordanhill, Renfrewshire, was born on the 10th of August, 1813, at Greenhead, Glasgow, in the house where his mother’s father lived. His father, who also was a Fellow of the Royal Society, had literary and scientific tastes with a strongly practical turn, fostered no doubt by his education in the University of Glasgow and his family connexion with some of the chief founders of the great commercial community which has grown up by its side. In published works on various subjects he left enduring monuments of a long life of actively employed leisure. His discovery of different species of Arctic shells, in the course of several years dredging from his yacht, and his inference of a previously existing colder climate in the part of the world now occupied by the British Islands, constituted a remarkable and important advancement of Geological Science. In his 'Voyage and Shipwreck of St. Paul,’ a masterly application of the principles of practical seamanship renders St. Luke’s narrative more thoroughly intelligible to us now than it can have been to contemporary readers not aided by nautical knowledge. Later he published a ‘Dissertation on the Origin and Connexion of the Gospels;’ and he was engaged in the collection of further materials for the elucidation of the same subject up to the time of his death, at the age of eighty-five. Archibald Smith’s mother was also of a family distinguished for intellectual activity. Her paternal grandfather was Dr. Andrew Wilson, Professor of Astronomy in the University of Glasgow, whose speculations on the constitution of the sun are now generally accepted, especially since the discovery of spectrum-analysis and its application to solar physics. Her uncle, Dr. Patrick Wilson, who succeeded to his father’s Chair in the University, was author of papers in the ‘Philosophical Transactions’ on Meteorology and on Aberration.


1873 ◽  
Vol 21 (139-147) ◽  
pp. 508-514 ◽  

The paper commences with an introduction, in which the general line of work since the last paper is indicated. Roughly speaking, this has been to ascertain the capabilities of the new method in a quantitative direction. It is stated that while qualitative spectrum-analysis depends upon the positions of the lines, quantitative spectrum-analysis on the other hand depends not on position but on the length, brightness , and thickness of the lines.


My Dear Sir, —This evening, at half-past seven o’clock, I received notice from one of my servants of a luminous appearance in the sky, visible towards the S. W., which I immediately ran out to ob­serve, and which, as it differed in some remarkable particulars from any phenomenon of the kind I have ever before observed or seen described, I think it not unlikely to prove interesting to the Royal Society. The evening was one of uncommon serenity and beauty: the moon, only thirty-eight hours after the full, having considerable south declination, was not yet risen. In consequence, the sun being already far enough below the horizon to leave only a faint glow of twilight in the west, the stars shone with unsubdued brilliancy, no cloud being visible in any quarter. Orion in particular was seen in all its splendour; and commencing below that constellation, and stretch­ing obliquely westward and downwards, nearly, but not quite to the horizon, was seen the luminous appearance in question. Its general aspect was that of a perfectly straight, narrow band of con­siderably bright white cloud, thirty degrees in length, and about a degree and a quarter, or a degree and a half in breadth in the middle of its length; its brightness nearly uniform, except towards the ends, where it faded gradually, so that to define its exact termination at either end was difficult. However, by the best judgement I could form, it might be considered as terminating, to the eastward or fol­lowing side, at, or a very little beyond, the stars t, k , λ Leporis, which stars (being of the fifth, or at most 5.4 magnitude) were pretty con­spicuously visible; from which circumstance the degree of bright­ness of the ground of the sky in that region may be well estimated. Between these stars and μ Leporis, the luminous band then commenced, involving neither of them, but more nearly contiguous to k and λ than to μ . From thence its course was towards π Eridani, which star must have been covered by it, and was not seen; this judgement of its direction having been formed by noticing that it passed clearly above γ Eridani, and as clearly below and parallel to the direction of δ, ε Eridani, which two stars being dimmed by the vapours of tie horizon and the twilight, were so little conspicuous as perfectly to account for π not having been noticed. At the point of its passage between γ and δ it was still considerably bright, and as it terminated with somewhat more abruptness at a point beyond ε (then about 12° high) than at its upper extremity, I am rather disposed to consider this end as somewhat curtailed by the vapours Making no allowance, however, for this, and estimating its visible termina­tion at a point on a celestial globe nearly opposite ζ Eridani (which star however was not noticed at the time), the length above assigned to the luminous band (30°) has been concluded by measurement on the globe.


1873 ◽  
Vol 163 ◽  
pp. 639-658 ◽  

In my former communication under the above title I pointed out that the new method of spectroscopic research adopted by Dr. Frankland and myself had enabled me to establish:— (1) That when a metallic vapour is subjected to admixture with another gas or vapour, or to reduced pressure, its spectrum becomes simplified by the abstraction of the shortest lines and by the thinning of many lines. (2) That when metals are chemically combined with another element (I used chlorine) only the longest lines of the metal remain in the spectrum of the chloride— the number being large in the case of elements of low atomic weight, and small in the case of elements of high atomic weight and of twice the atom-fixing power of hydrogen.


1869 ◽  
Vol 17 ◽  
pp. 74-80 ◽  

My dear Sir, —I hasten to send you an account of the observations I have fortunately been able to make at Beejapoor of the total eclipse on the 18th instant with one of the hand-spectroscopes sent out by the Royal Society in the care of Lieut. Herscliel, R.E., not waiting to let my report be forwarded by Colonel Walker, R.E., my departmental superior, on account of the delay which would necessarily be caused thereby. I may state at once that I observed the spectra of two red flames close to each other, and in their spectra two broad bright bands quite sharply defined, one rose-madder and the other light golden. These spectra were soon lost in the spectrum of the moon’s edge just before emergence, which had also two well-defined bright bands (one green and one indigo) about a quarter the width of the bands in the spectra of the flames, this spectrum being again soon lost in the bright sunlight.


1877 ◽  
Vol 25 (171-178) ◽  
pp. 546-546

The author submits to the Royal Society the first portion of a new map of the solar spectrum, w.l. 39-40 ten millionths, constructed after the manner described in a previous “Preliminary Note.”


Author(s):  
Asle Toje

We do not want to place anyone into the shadow, we also claim our place in the sun.” In a foreign policy debate in the German parliament on December 6. 1897 the German Secretary of State for Foreign Affairs, Bernhard von Bülow, articulated the foreign policy aspirations of the ascendant Wilhelmine Germany. This proved easier said than done. In 1907, Eyre Crowe of the British Foreign Office penned his famous memorandum where he accounted for “the present state of British relations with France and Germany.” He concluded that Britain should meet imperial Germany with “unvarying courtesy and consideration” while maintaining “the most unbending determination to uphold British rights and interests in every part of the globe.”...


1898 ◽  
Vol 62 (379-387) ◽  
pp. 376-385 ◽  

On a previous occasion I gave some boiling points of salt solutions under atmospheric pressure. As the dimensions of that abstract made a full account of the experimental method impossible, I have been given this opportunity, by the courtesy of the Council of the Royal Society, of describing the apparatus and procedure by which those results were obtained.


1909 ◽  
Vol 6 (4) ◽  
pp. 145-148 ◽  
Author(s):  
E. H. L. Schwarz

Dr. J. R. Sutton has recently read a most important paper to the Royal Society of South Africa on the diurnal variation of level at Kimberley. The paper gave the preliminary results of observations made during the course of three years upon the variation of the level of the ground as recorded by a large horizontal pendulum of a special design made for the author by the Cambridge Instrument Company. It appeared from the results that the movements in the surface of the ground, which set up corresponding movements in the pendulum, were very great. The maximum westerly elongation of the extremity of the pendulum occurred about 5.30 a.m., the maximum easterly about 4.15 p.m., the medium positions a little before 11 a.m. and 9.30 p.m. Geometrically these movements may be represented on the hypothesis that the hemisphere facing the sun bulges out, forming a sort of meniscus to the geosphere. The rise and fall of the surface of the ground which such a supposition would postulate is enormous, and the very magnitude has led Dr. Sutton to hesitate in giving the figures. There can, however, be very little doubt that some rise and fall in the earth's surface is occasioned by the sun's gravitational pull, although the present figures may have to be lessened by taking into consideration other causes which contribute to the disturbance of the pendulum.


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