60 



S. GLASENAPP. 



T = 1892*15 



i = o9-77 



u = 27*66 years 



€ = 0-442 



n=13°0177 



^ = 26°228 



Si = 153°30 



a = 2"*04 



A = 255-80 





The comparison of these elements with the observations is given 

 in the following table : — 



t 



e 



e c 



#o-0c 



Po 



Pc 



Po ~Pc 





o 



o 



o 



„ 



w 



II 



1876-52 



240 ± 



235-4 



+4-6 



1-80 



1-47 



+0-33 



77-58 



223-5 



223-9 



-0-4 



1-78 



1-54 



+0-24 



88-72 



147-5 



148-5 



-1-0 



1-89 



1-69 



+0-20 



89-55 



1330 



140-J 



-71 



1-16 



1-41 



-0-25 



90-60 



122-0 



121-3 



+0-7 



0-81 



0-96 



-0-15 



91-53 



823 



80-1 



+2-2 



0-51 



0-61 



-010 



92-38 



24-4 



240 



+0-4 



0-58 



0-69 



-011 



9355 



348-5 



347-8 



+0-7 



0-71 



117 



-0-46 



The differences o — C are very small, but the differences p - p c 

 are considerable, and present a systematical rate ; the three first 

 residuals are positive, the others are negative. 



To verify the results obtained I have determined the corrections 

 of the elements of Mr. T. E. Gore (Monthly Notices, 1892), and 

 have obtained : — 



Elements of T. E. Gore. 



Their Corrections. 



New Elements. 



T= 1891-85 



—0*05 



1891*80 



u = 34*48 years 



—2*25 



32*23 years 



n= — 10°*4413 



— 0°*7276 



— 11 *1689 



Sl = 139°*43 



+ 9°-09 



148° *52 



A= 278°*25 



— 5°*43 



272°*82 



c= 56°-72 



+ 4°-12 



60°*84 



€= 0-5562 



—0-0645 



0*4917 



"¥= 33°-7934 



— 3°-8485 



29*9449 



a= 2"-13 



+ 0"-06 



2 ,, -19 



The obtained corrections approach the elements of Mr. T. E. Gore 

 to those which I have determined ; we may consider this circum- 

 stance as an indication that our elements are near the truth. The 



