Longueyhigginsintell2.Pdf

Longueyhigginsintell2.Pdf

. .IB A ,1, " , , ,, " , , , , ," , ,, , , ,, , " , , , , , , , , , L, , " , , , , , , , , , , " , , , ," , , , , , ,, F A," , , , , , , , , , I , , ,, B D A' C *GB ' , , *' 'C E, and F denote the feet of the altitudes AH, BH, and CH; ",', GA,' see Figure 6. Then, HDCE, for example,is a cyclic quadri- I " " ',' , lateral;hence, LBHD = C. Therefore, " , I "':', " HD = BD cot C = ABcosBcot C. " , ',,~ " BecauseAB = 2Rsin C, this givesus .. IA H = 2R(cos B cas C, cosC cosA, cosA cosB). I' The coordinates of the point L, which is the reflection of i erties of two pencils of rays having the same cross-ratio, H in 0 (i.e., L = 2 X 0 - H), can therefore be written [ b~t with one ray in common. The proof is too long to be L = 2R(a - {3'Y,(3 - 'Ya,'Y - a{3), (2) given here. The fourth and shortest proof goes as follows. The trilinear coordinates of a point P in the plane of a where a, {3, and 'Y stand for cos A, cos B, and cos C, re- triangle ABC may be defmed [4, 10] as the lengths (x, y, z) spectively (see also [4] and [5]). I of the perpendicularsfrom P to the three sidesBC, CA, and What are the coordinatesof the Gergonnepoint G?Now, I AB. By convention, x, y, and z are positive when Plies in- from Figure 3, we see that XC = r cot(iC), and therefore side the triangle. for X, we have Thus, the incenter I, being equidistant from the three y = XC sin C = 2r COS2(lC). sides, has coordinates 2 Similarly, I = r(1, 1, 1), (1) z = XB sin B = 2r cos2(lB). where r is the radius of the incircle. For the circumcenter 2 0, since LBOC = 2 X LBAC, it will be seen that Therefore,the coordinatesof G, which lies on the line AX, must also satisfy 0 = R(cosA, cosB, cos C), where R is the circumradius and A, B, and C are the an- JL = cos2(lC)2 = 1 + cos C gles at the vertices of ABC. For the ortlwcenter H, let D, z cos2(lB) 1 + cosB' 2 Hence, G = [(1 + (3)(1+ 'Y),(1 + 'Y)(1+ a), (1 + a)(1 + {3)]g, (3) where g is a normalizing constant. Therefore, in order to prove the collinearitY of I, G, andL, we have only to show that the determinant 1 1 1 D = (1 + (3)(1+ 'Y) (1 + 'Y)(1+ a) (1 + a)(1 + fJ) a - {3'Y {3 - 'Ya a - {3'Y vanishes.However, upon adding the elementsof the third row to those of the second,we seethat eachterm becomes equalto 1 + a + {3+ 'Y,bringing the first two rows of D into H proportions,so D = O.This provesthat IG passesthrough L. 56 THEMATHEMATlCAL INTEUJGENCER Likewise,the coordinatesof the excenterIA are .O'CiII:la- IA = rA (-1, 1, 1). A In detennining the coordinates of GA, we have only to re- place B and C by 7T- B and 7T- C, respectively,also x by -x. Hence, GA= [-(1 - fJ)(l - y), (1 - y)(l + a), (1 + a)(l - fJ)]gA, where gA is another constant. The correspondingdetemti- nant DA will be found to vanish in a similar way. Hence, we have proved the following theorems: 1. Thefour lines IG, IAGA,InGB' and IcGc all meet in a point L. 2. L lies on the Euler line and is the reflection of the or- B X A thocenter H in the circumcenter O. Thus, the separa- tions of L, 0, M, 0', and H along the Euler line are in the t 6 2 1 3 Figur 5 Zc be defined similarly. Then,the three lines AXA,BY B, and raws.. ,see. e. CZc are concurrent in the pomt N; see Figure 7. Note a corollary. From Figure 5 we see that ML = 2 X To prove this, note that the length of the tangent CXA MH. Now, consider the homotheticity in which points of from C to the excircle center IA is -!ca + b - c), where a, the plane are first reflected in the medianpoint M and then b, and c are the sides of ABC. Ther:fore, enlargedby a factor of 2. All transformed points being de- 1 noted by the suffix 1, the orthocenter HI of the triangle CXA= CYB= 2(a + b - c), AlBlCl is coincident with L. But A, B, C are the midpoints which is equal to the length of the tangent BX from B to of the sides of A lBl Cl, so ABC is the median triangle of the incircle, center I. In fact, XA, YB,and Zc are the re- AlBlCl. Substituting ABC for AlBlCl, we have the follow- flections of X, Y, and Z in the midpoints A', B', and C' of ing theorems: the three sides of ABC. Hence, as before, 3. The orthocenter of a triangle ABC is coUinear with the AYB . BZc . CXA incenter I' of the median triangle (i.e., the Spieker AZc . BXA . CYB = 1, point of ABC) and the Gergonnepoint G' of the me- d le ( Fi 6) and by Ceva'stheorem, the three lines are concurrent. tan. trwng. see g. 4. If I'A, I'B, and I'G are the excentersof the median tri- angle and GA, GR, and Gb are the corresponding .O'CiIJ:I~:- Gergonnepoints, then lAG;', lEGE,and I/;G6 also pass \ IB throughthe orthocenterH. NA "'" "'"'"', , , WhenI wrote to my long-timefriend and colleague "'"'"'"' , H.S.M.Coxeter about these results, he pointed out that the "',"', I, French geometer G.A.G.de Longchamps(1842-1906) had shown [6] that the orthocenterHI of AlBIC 1has certain in- terestingproperties related naturally to the triangle AlBl Cl but having no obvious connection with I or G; see [1], [8]. The point HI has been called the de Longchampspoint of ABC; see [1] and [5]. Thus, theorems 1 and 2 can be stated alternatively as 5. Thelines IG, IAGA,InGB' and IoGc all pass through the de Longchampspoint of ABC. Or more succinctly, , B ".., 'C -. 6. L coincides with HI. "".. " " Nc ..' I The question now arises: Are there any other fourfold "" ", " .. , , concurrenciesanalogous to the one through L? .. .." , There is a somewhat similar situation involving the I ,~~, Nagelpoint N mentionedearlier. The Nagelpoint of the / IA triangle ABC may be defined in the following way [2], [11]. NB As before, let XA denote the point of contact of the excir- / cle, center lA, with the side BC opposite A, and let YB and I VOLUME22,NUMBER 1,2000 57 By similar triangles, it may be shown (see [2, pp. 161- To establish relation (A) we need, by symmetry, to con- 162]) that N is collinear with I and M and that MN = 2MI. sider only the x components of this equation. Thus, we Hence,N is the incenter of the triangle AlBIC!, or N = II. need to show only that Now, corresponding to., each excenter of ABC, say lA, &.fl,'1D(1 - cos B)(1 - cos C) + Oll-OD sm. ( -I A) sm, ( -1 B) sm-. ( 1C) we also have a Nagel pomt, Thus, if t:4, 7lA,~ are reflec- 2 2 2 tions ofXA, YA,ZA, respectively,~ in the midpoints A', B', = 2R sinB sin C. C', respectively(so t:4 = X), thenAt:4, B7lA, C~ meet in the However, from sin(lA) = cos[l(B + C)], this last result be- Nagel point NA, say; and similarly for NB and Nc. comes evident. The~efore,M ~deed divides the line IN in We can now prove two theorems somewhat analogous the ratio 1:2. to Theorems 1 and 2, namely In a similar way, we fmd 7, The!our li~s IN, lANA, InNB' and IcNc all meet in the NA = 2R[(1 + (3)(1 + y), -(1 + y)(1 - a), -(1 - a)(1 + (3)] med'/,anpomt M, 8, M divides each of IN, lANA, IBNB, and IcNc in the ra- and tio 1 : 2. I = r A A ( -1 " 1 1), Hence, where 9. NA, NB, and Nc are the three excentersof the triangle r = 4R sin (lA ) cos (l B) cog ( 1r"\ A B C A 2 2 ZVh 1 1 1. An analytic proof is as follows, Our method will be to show that N + 2/ = 3M, (A) . As earlier, the ratio of the perpendicularsfrom XA to the sidesAC and AB is given by 1L - XAC sin C - XB sin C - r cot(iB) sin C. z - XABsinB - XCsinB - rcot(lB) sinB' 2 that is to say, . 2 sm (k2'-'J 1 1L==~ z sin2(1B) 1 - {3' 2 H th trilin. dinate fN MICHAEL LONGUET-HIGGINS ence, e ear coor s 0 are Instituteof Nonlinear, Science , N = [(1 - (3)(1- y), (1 - y)(1 - a), (1 - a)(1 - {3)]n, UniversityofCalifomia LaJolla . , .. LaJolla, California 92093-0402 USA where n IS a normalizmg constant,which we need to eval- uate. Now,b' theI trilinear. coordinates of any point (x, y, z) The auth or grad uat ed In' math emat ICS' from Camb rl' d ge Unl-' must 0 VlOUSY satIsfy versity in 1946 and did 3 years' NationalService at the ax + by + cz = 211., AdmiraltyResearch Laboratory in Teddington,where he be- A d th f ABC B came interested in various geophysical phenomena. He re- where ~ enotes e area 0 . ecause .' .. tumed to Cambridge to take a Ph.D, In geophysIcs In 1952. 11. = 2R2 sin A sin B sin C He haspublished extensively on topicsin fluiddynamics, par- '1D . A d Ii rth find aft f ticularly on surface waves and ripples, wave breaking and thand a I= .&.fl, smA B' an Cso 0 th" we er some use 0 soundgeneration , In.

View Full Text

Details

  • File Type
    pdf
  • Upload Time
    -
  • Content Languages
    English
  • Upload User
    Anonymous/Not logged-in
  • File Pages
    4 Page
  • File Size
    -

Download

Channel Download Status
Express Download Enable

Copyright

We respect the copyrights and intellectual property rights of all users. All uploaded documents are either original works of the uploader or authorized works of the rightful owners.

  • Not to be reproduced or distributed without explicit permission.
  • Not used for commercial purposes outside of approved use cases.
  • Not used to infringe on the rights of the original creators.
  • If you believe any content infringes your copyright, please contact us immediately.

Support

For help with questions, suggestions, or problems, please contact us