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1 ΕΘΝΙΚΟ ΜΕΤΣΟΒΙΟ ΠΟΛΥΤΕΧΝΕΙΟ ΕΚΕΦΕ "ΔΗΜΟΚΡΙΤΟΣ" ΣΧΟΛΗ ΕΦΑΡΜΟΣΜΕΝΩΝ ΜΑΘΗΜΑΤΙΚΩΝ ΚΑΙ ΦΥΣΙΚΩΝ ΕΠΙΣΤΗΜΩΝ ΣΧΟΛΗ ΜΗΧΑΝΟΛΟΓΩΝ ΜΗΧΑΝΙΚΩΝ ΙΝΣΤΙΤΟΥΤΟ ΝΑΝΟΕΠΙΣΤΗΜΗΣ ΚΑΙ ΝΑΝΟΤΕΧΝΟΛΟΓΙΑΣ ΙΝΣΤΙΤΟΥΤΟ ΠΥΡΗΝΙΚΗΣ ΚΑΙ ΣΩΜΑΤΙΔΙΑΚΗΣ ΦΥΣΙΚΗΣ Διατμηματικό Πρόγραμμα Μεταπτυχιακών Σπουδών "Φυσική και Τεχνολογικές Εφαρμογές" Βαρυτική Κατάρρευση Ομογενούς Βαθμωτού Πεδίου σε Χωροχρόνο McVittie Μεταπτυχιακή Διπλωματική Εργασία του Κυριάκου Δεστούνη Επιβλέπων Καθηγητής: Ελευθέριος Παπαντωνόπουλος Αθήνα, Ιούλιος, 2016

2 Περίληψη Σε αυτή την εργασία θα μελετηθούν λύσεις των εξισώσεων πεδίου Einstein οι οποίες περιγράφουν μια μελανή οπή σε διαστελλόμενο σύμπαν. Η γνωστή και ως μετρική McVittie αναπαριστά χρονικά εξαρτόμενη μελανή οπή Schawarzschild σε υπόβαθρο Friedmann-Robertson-Walker (FRW) χωρίς προσαύξηση μάζας, ομογενής ενεργειακή πυκνότητα και ανομοιογενής πίεση. Σκοπός μας είναι η απόδειξη ύπαρξης της μετρικής McVittie ως λύση των εξισώσεων πεδίου της Γενικής Σχετικότητας, η ανασκόπηση των βασικών ιδιοτήτων της συγκεκριμένης γεωμετρίας και η μελέτη της βαρυτικής κατάρρευσης ενός ομογενούς βαθμωτού πεδίου στον χωροχρόνο McVittie. Αναλυτικότερα, στον Κεφάλαιο 2 δίνεται μια σύντομη περιγραφή των ιδιοτήτων και εφαρμογών του χωροχρόνου McVittie και αναφέρονται οι αξιοσημείωτες έρευνες που έχουν γίνει στο θέμα αυτό. Στο Κεφάλαιο 3, αποδεικνύεται η μετρική McVittie και παραθέτεται η γενικευμένη μορφή της η οποία περιέχει μη μηδενική χωρική καμπυλότητα. Στο Κεφάλαιο 4, οι ιδιότητες και τα χαρακτηριστικά αποδεικνύονται και η δυναμική των φαινομενικών οριζόντων μελετάται λεπτομερώς. Τέλος, στο Κεφάλαιο 5, μελετάται η βαρυτική κατάρρευση της ύλης στο χωρχρόνο McVittie. Το κέλυφος ύλης παραμετροποιείται από ένα χρονοεξαρτόμενο βαθμωτό πεδιο συζευγμένο με την βαρύτητα σε ένα καταρρέων σύμπαν με αρνητική κοσμολογική σταθερά. Η συνθήκη που πρέπει να ισχύει για να συμβαίνει η βαρυτική κατάρρευση ȧ(t) < 0, όπου a(t) ο παράγοντας κλίμακας. Η ιδιομορφία σχηματίζεται όταν a(t) = 0. Η διαδικασία κατάρρευσης μοντελοποιείται λύνοτνας τις εξισώσης Einstein και Klein-Gordon στο χωρχρόνο McVittie, αριθμητικά, χρησιμοποιώντας το πρόγραμμα Mathematica. Η διαδικασία μελετάται χρησιμοποιώντας γραφικές παραστάσεις. Στην τελευταία παράγραφο της περίληψης θα ήθελα να ευχαριστήσω θερμά των επιβλέπων καθηγητή μου, κύριο Ελευθέριο Παπαντωνόπουλο, για την ευκαιρία που μου έδωσε να δουλέψω με αυτόν και τους συνεργάτες του, για την εμπιστοσύνη που έδειξε στο πρόσωπό μου και για την υποστήριξη την οποία έλαβα με γεναιοδωρία καθόλη τη διάρκεια της εκπόνησης της διπλωματικής μου εργασίας. Επίσης, θα ήθελα να ευχαριστήσω των καθηγητή Γεώργιο Κουτσούμπα και τον υποψήφιο διδάκτορα, Κωσταντίνο Ντρέκη, για τις χρήσιμες συμβουλές τους και την απλόχερη βοήθειά τους σε θέματα Γενικής Σχετικότητας και μελανών οπών. 1

3 Abstract In this thesis we study solutions of the Einstein s field equations that describe a black hole in an expanding universe. The, so-called, McVittie metric represents a time-varying Schwarzschild black hole in a Friedmann-Robertson-Walker (FRW) background with no mass accretion, homogeneous energy density and inhomogeneous pressure. Our purpose is to prove the existence of McVittie s metric as a solution of the field equations of General Relavity, review the basic properties of this particular geometry and study the gravitational collapse of a homogeneous scalar field in the McVittie spacetime. In more detail, in Chapter 2 we give a brief introduction of the features and applications of McVittie spacetime and denote remarkable previous work on the subject. In Chapter 3, we derive McVittie s metric by proving that it is indeed a solution to Einstein s field equations and review its generalized form which contain non-zero spatial curvature. In Chapter 4, the properties and features are proven and the dynamics of the apparent horizons of this geometry are reviewed in detail. Finally, in Chapter 5 we study the gravitational collapse of matter in the McVittie spacetime. The matter shell is parameterized by a time-dependent scalar field coupled to gravity in a collapsing universe with the presence of a negative cosmological constant. The condition we want to be true for us to have gravitational collapse will be the time derivative of the scale factor to be negative. The singularity is reached when the scale factor is equal to zero. We simulate the collapsing process in the McVittie geometry by solving the resulting Klein-Gordon and Einstein field equation, numerically, using Mathematica. We visualize the process by utilizing plots showing the evolution of the scale factor, scalar field, energy density and pressure of the system with respect to time. In the last paragraph of the abstract I would like to deeply thank my supervisor, Professor Eleftherios Papantonopoulos, for the opportunity he gave me to work with him and his colleagues, for the trust he has shown me and of course for the support that he generously gave me throughout the time of my thesis preparation. I would, also, like to thank Professor Georgios Koutsoubas and his PhD student, Kostas Drekis, for their useful advice and help in the subjects of General Relativity and Black Holes. 2

4 Περιεχόμενα 1 Αναλυτική Περίληψη Εισαγωγή Ιστορική Αναδρομή Βασικά Χαρακτηριστικά Εύρεση Μετρικής McVittie Εξισώσεις Einstein Επίλυση Εξισώσεων που Καθορίζουν τη Μετρική Χαρακτηριστικά του Χωροχρόνου McVittie Βασικές Ιδιότητες Μελέτη Φαινομενικού Ορίζοντα Βαρυτική Κατάρρευση Ευρεση Εξίσωσης Klein-Gordon Εύρεση Εξισώσεων Einstein Βαρυτική Κατάρρευση με Μηδενικό Δυναμικό Συμπεράσματα Introduction 20 3 Derivation of the McVittie Metric Introduction Equations determining the metric of spacetime Solutions of the equations Properties of the McVittie Spacetime Basic features Coordinate transformation McVittie s apparent horizons

5 4.3.1 The Schwarzschild-de Sitter-Kottler black hole Apparent horizons of the McVittie metric Dynamics of the apparent horizons Gravitational Collapse of a Homogeneous Scalar Field in the McVittie Spacetime Derivation of Klein-Gordon equation Derivation of Einstein s field equations Gravitational collapse with zero potential Singularity formation with respect to the cosmological constant Singularity formation with respect to the McVittie mass Singularity formation with respect to the radius Conclusions Appendices 82 A Mathematica Code 83 A.1 Gravitational Collapse for Various Cosmological Constants A.2 Gravitational Collapse for Various McVittie Masses A.3 Gravitational Collapse for Various Radii Bibliography 94 4

6 Κεφάλαιο 1 Αναλυτική Περίληψη 1.1 Εισαγωγή Ιστορική Αναδρομή Μετρική Schwarzschild (1916): ds 2 = όπου r 1 η συντεταγμένη παρατηρητή. ( ) 1 m 2 ( 2r m dt m ) 4{dr 2 2r 1 2r 1 + r1dω 2 2 }, 1 Μετρική Lemaitre (1930): όπου r η κοσμική συντεταγμένη. { } dr ds 2 = dt 2 e β(t) 2 + r 2 dω 2 (1 + 1, 4 kr2 ) Βασικά Χαρακτηριστικά Μετρική McVittie (1933): ( ) 1 µ(t) 2 ( ds 2 2r = dt µ(t) ) 4e β(t) {dr 2 + r 2 dω 2 }, (1.1) 1 + µ(t) 2r 2r 5

7 όπου e β(t)/2 = a(t) και µ(t) = m/a(t). a(t) 1 μετρική Schwarzschild σε ισοτροπικές συντεταγμένες r σύμπαν FRW ο τανυστής ενέργειασ-ορμής έχει μορφή ιδανικού ρευστού ομοιογενής ενεργειακή πυκνότητα, ανομοιογενής πίεση σταθερή μάζα McVittie m δεν υπάρχει προσαύξηση 1.2 Εύρεση Μετρικής McVittie Εξισώσεις Einstein Εστω η μετρική ds 2 = e ζ(r,t) dt 2 e ν(r,t) {dr 2 + r 2 (dθ 2 + sin 2 θdφ 2 )} (1.2) σε κοσμικές συντεταγμένες με c = 1. Οι εξισώσεις Einstein είναι G µν + Λg µν = κt µν, (1.3) όπου G µν = R µν 1 2 Rg µν. Η ενναλακτική μορφή των εξισώσεων είναι R µν Λg µν = κ(t µν 1 2 T g µν). (1.4) Εστω ο τανυστής ενέργειασ-ορμής T ν µ = {ρ, p 1, p 2, p 2 }, συνεπώς, T 00 = ρ e ζ, T 11 = p 1 e ν, T 22 = p 2 r 2 e ν, T 33 = p 2 r 2 sin 2 θ e ν, T = g µν T µν = ρ p 1 2p 2. Τανυστής Ricci: R µν = R β µβν = Γβ νµ,β Γβ βµ,ν + Γβ βα Γα νµ Γ β ναγ α βµ, (1.5) 6

8 όπου Γ β µν τα σύμβολα Christoffel. Σύμβολα Christoffel: Γ µ νσ = 1 2 gµλ (g λν,σ + g λσ,ν g νσ,λ ). (1.6) Τα μη-μηδενικά σύμβολα Christoffel για την μετρική (1.2) είναι: Γ 0 00 = 1 2 ζ Γ 0 01 = Γ 0 10 = 1 2 ζ Γ 0 11 = eν 2e ζ ν Γ0 22 = r2 e ν 2e ζ Γ 0 33 = r2 sin 2 θe ν 2e ζ ν Γ 1 00 = eζ 2e ν ζ Γ 1 01 = Γ 1 10 = 1 2 ν Γ1 11 = 1 2 ν Γ 1 22 = r r2 2 ν Γ 1 33 = r sin 2 θ 1 2 r2 sin 2 θν Γ 2 02 = Γ 2 20 = 1 2 ν Γ2 12 = Γ 2 21 = 1 r ν ν Γ 2 33 = cos θ sin θ Γ 3 13 = Γ 3 31 = 1 r ν Γ 3 03 = Γ 3 30 = 1 2 ν Γ 3 23 = Γ 3 32 = cos θ sin θ Οι μη-μηδενικοί όροι του τανυστή Ricci για την μετρική (1.2) είναι: R 00 = eζ e ν (ζ 2 + (ζ ) 2 + ζ ν ζ r ) (3 2 ν ( ν)2 3 4 ζ ν), R 11 = eν e ζ ( ν ( ν)2 1 4 ν ζ) ( 1 2 ζ (ζ ) ν ζ + ν + ν r ), R 22 = r 2 [ eν e ζ ( ν ν2 R 33 = r 2 sin 2 θ[ eν e ζ ( ν ν2 R 01 = νζ 2 ν. Οι πεδιακές εξισώσεις Einstein είναι: ν ζ 4 ) ( ζ 2r + ζ ν 4 + 3ν 2r + ν 2 + (ν ) 2 4 )], ν ζ 4 ) ( ζ 2r + ζ ν 4 + 3ν 2r + ν 2 + (ν ) 2 4 )], 7

9 Λ + κ 2 (ρ + p 1 + 2p 2 ) = e ν ( ζ 2 + (ζ ) 2 + ζ ν ζ r ) e ζ ( 3 2 ν ( ν)2 3 4 ζ ν) Λ + κ 2 (2p 2 p 1 ρ) = e ν ( ζ 2 + (ζ ) 2 ν ζ ν + ν r ) e ζ ( ν ( ν)2 1 ν ζ) 4 Λ + κ 2 (p 1 ρ) = e ν ( ζ 2r + ζ ν 4 + 3ν 2r + ν 2 + (ν ) 2 4 ) e ζ ( ν ν2 κt 01 = νζ 2 ν Για ιδανικό ρευστό με T ν µ = {ρ, p, p, p}: ν ζ 4 ) Λ + κ 2 (ρ + 3p 1) = e ν ( ζ 2 + (ζ ) 2 + ζ ν ζ r ) e ζ ( 3 2 ν ν2 3 4 ζ ν) (1.7) Λ + κ 2 (p 1 ρ) = e ν ( ζ 2 + (ζ ) 2 ν ζ ν + ν r ) e ζ ( ν ν2 1 4 ν ζ) (1.8) Λ + κ 2 (p 1 ρ) = e ν ( ζ 2r + ζ ν 4 + 3ν 2r + ν 2 + (ν ) 2 4 ) e ζ ( ν ν2 1 4 ν ζ) (1.9) νζ 2 ν = Επίλυση Εξισώσεων που Καθορίζουν τη Μετρική Από τις (1.8) και (1.9) προκύπτει: (1.10) ζ + ν + (ζ ) 2 2 (ν ) 2 2 ν ζ 1 r (ν + ζ ) = 0. Οι εξισώσεις που καθορίζουν τους συντελεστές της μετρικής (1.2), ζ και ν, είναι: ζ + ν + (ζ ) 2 2 ν νζ = 0, 2 (1.11) (ν ) 2 ν ζ 1 2 r (ν + ζ ) = 0. (1.12) Η (1.11) λύνεται εύκολα: ν = a(t)e ζ(r,t)/2 dt + α(r) (1.13) 8

10 Εστω ότι ζ εξαρτάται μόνο από το r. Τότε, ν = β(t)e 1 2 ζ(r) + α(r), (1.14) όπου β(t) = a(t) dt. Αντικαθιστουμε την (1.14) στην (1.12). Υπάρχουν δύο πιθανές λύσεις: β σταθερό στατική λύση Schwarzschild. β αυθαίρετο ζ σταθερό, α(r) = 2 log ( 1 + 1kr2) μετρική Lemaitre. 4 Συνεπώς, ζ(r, t) και α(r) = 0, αφού το α(r) εξαρτάται από την καμπυλότητα του χώρου. Αναπτύσσουμε τα ζ, ν ως δυναμοσειρές του 1/r: e ζ/2 = γ = 1 + a 1 u m 1 + a 2 u m 2 + a 3 u m , (1.15) ν = β(t) + β s (t)u ms, (1.16) s=1 όπου u = 1/r, a s συναρτήσεις του t, οι δυνάμεις του u είναι σε αύξουσα σειρά, και β(t) = a(t)dt, (1.17) β s (t) = a(t)a s (t)dt. (1.18) Αλλάζοντας μεταβλητή από r σε u και αντικαθιστώντας το ζ ως προς το γ στην (1.12): γu 2 ν ν + 3γ u2 u + γ 2u 2 u + 6 γ 2 u 2u γ ν u u 1 2 uγ( ν u )2 = 0. (1.19) Αντικαθιστώντας τις (1.15), (1.16) στην (1.19) προκύπτει: u ms 1[ ] β s m s (m s 1) + 3β s m s + 2a s m s (m s 1) + 6a s m s s=1 + u 2ms 1[ β s a s m s (m s 1) + 3β s m s a s s=1 2β s a s m 2 s 1 ] 2 β2 sm 2 s + u 3ms 1[ 1 ] 2 β2 sm 2 sa s = 0 9 s=1

11 Η χαμηλότερη δύναμη του u είναι η u m 1 1. Για s = 1 προκύπτει: m 1 (m 1 + 2)(2a 1 + β 1 ) = 0. (1.20) Οι δύο επόμενες δυνάμεις είναι οι u 2m 1 1 και u m 2 1. Άρα, m 2 = 2m 1 και γενικά m s = sm 1. Από την (1.20) παρατηρείται ότι m 1 = 1 και 2a 1 + β 1 = 0. (1.21) Από την (1.21) μαζί με τις (1.17), (1.18) προκύπτει: Από τις επόμενες δυνάμεις u 2m 1 1 και u m 2 1 προκύπτει: a 1 = 1 a 1 2 β. (1.22) 2a 2 + β 2 = 1 2 a2 1 = c 2 a 2 1. (1.23) Παραγωγίζοντας ως προς t και χρησιμοποιώντας τις (1.17), (1.18) προκύπτει: a 2 = c 2 a 2 1, β 2 = c 2 a 2 1. Συνεχίζοντας την ίδια διαδικασία για υψηλότερες δυνάμεις του u έχουμε: a n = c n a n 1, β n = 2c n n an 1, (1.24) Αν η λύση που ψάχνουμε υπάρχει, θα είναι της μορφής (με m 1 = 1, m s = sm 1, u = 1/r, a 1 = µ) γ = 1 + a s u ms = 1 + s=1 ν = β(t) + a s u s = 1 + s=1 u ms β s (t) = β(t) 2 s=1 s=1 c s a s 1u s = 1 + s=1 ( ) s µ(t) c s (1.25) r ( ) s µ(t) (1.26) s=1 u s a s c s 1 s = β(t) 2 c s s s=1 r με 1 2 β = µ µ. 10

12 Εστω, επομένως, η (1.12) γίνεται: ν r 2(γ 1) =, r ν t = 2 µ γ, (1.27) µ και Θέτωντας r = e x η (1.28) γίνεται Η (1.29) έχει δύο μερικές λύσεις: Από την (1.31) προκύπτει: Επιπλέον, ν r r 2 2 γ r(γ 1) γ r2 r γ(γ2 1) = 0 (1.28) 2 γ x 2 γ γ x γ(γ2 1) = 0. (1.29) = 2(γ 1) r γ x γ2 + 1 = 0, (1.30) 2 γ x + γ2 1 = 0. (1.31) γ = 1 µ(t) 2r 1 + µ(t) 2r Αντικαθιστώντας τις (1.32), (1.33) στην (1.2) προκύπτει:. (1.32) ν = β(t) + log(1 + µ(t) 2r )4, (1.33) ν t = 2 µ µ γ β 2 = µ µ. (1.34) ( ) 1 µ(t) 2 ( ds 2 2r = dt 2 e β(t) 1 + µ(t) ) 4{dr 2 + r 2 (dθ 2 + sin 2 θdφ 2 )}. (1.35) 1 + µ(t) 2r 2r Από την (1.34) έχουμε µ(t) = m a(t), (1.36) 11

13 όπου e β(t)/2 = a(t). Τελικά, ds 2 = ( ) 1 m 2 ( 1 + m dt m ) 4a 2 (t){dr 2 + r 2 (dθ 2 + sin 2 θdφ 2 )}. (1.37) Εάν δεν θέταμε α(r) = 0 στην (1.13) και ακολουθούσαμε τα ίδια βήματα, θα προέκυπτε: ds 2 = 1 m kr2 1 + m kr2 με k την καμπυλότητα του χώρου. 2 ( ) m + 14 dt 2 kr2 ( kr2) 2 a 2 (t){dr 2 + r 2 dω 2 }, (1.38) Χαρακτηριστικά του Χωροχρόνου McVittie Βασικές Ιδιότητες Εστω η δράση g R S = d x[ ] 2 (gµν µ φ ν φ) V (φ). (1.39) Διαφορίζοντας ως προς τον αντίστροφο μετρικό τανυστή, g µν, προκύπτουν οι εξισώσεις Einstein: G µν = T µν, (1.40) όπου G µν = R µν 1g 2 µνr και T µν = 1 2 g µνg αβ α φ β φ + µ φ ν φ g µν V (φ). (1.41) Θεωρώντας ιδανικό ρευστό, T ν µ = ( ρ, p, p, p), στο χωροχρόνο McVittie με μετρικό πρόσημο (, +, +, +) και χρησιμοποιώντας την (1.41) προκύπτει: ( ) ρ(t) = m m φ2 (t) + V (φ), (1.42) ( ) p(t) = m m φ2 (t) V (φ). (1.43) 12

14 Οι εξισώσεις Einstein είναι: (tt) : (rr, θθ, φφ) : 3ȧ2 (t) a 2 (t) = ρ [ ] (1.44) ( 5m)ȧ 2 (t) + 2a(t)ä(t)( + m) a 2 (t)( m) = p (1.45) Η (1.45) μπορεί να γραφεί ως όπου H(t) = ȧ(t)/a(t). p = 3H 2 (t) 2 ( ) 1 + m ( )Ḣ(t) (1.46) 1 m Το βαθμωτό Ricci είναι: R = g µν R µν = 6 R = 12H 2 (t) + 6 Από την (1.47) έχουμε: [ ] ( 3m)ȧ 2 (t) + a(t)ä(t)( + m) a 2 (t)( m) ( ) 1 + m ( )Ḣ(t). (1.47) 1 m a(t) 0 ιδιομορφία με άπειρη ενεργειακή πυκνότητα και πίεση m = κοσμολογική ιδιομορφία Μεγάλης Εκρηξης με άπειρη πίεση Ḣ(t) = 0 δεν υπάρχει κοσμολογική ιδιομορφία και για H = 0 μετρική Schwarzschild... H 0 μετρική Schwarzschild-de Sitter Μελέτη Φαινομενικού Ορίζοντα Μια μετασχηματισμένη μορφή της μετρικής McVittie (1.37) είναι: ds 2 = fdt m R dr 2 2H(t)R 1 2m R drdt + R 2 dω 2, (1.48) 13

15 όπου f = 1 2m/R H 2 (t)r 2 και R(r, t) = σφαίρας με εμβαδόν επιφάνειας 4πR 2. Το βαθμωτό Ricci και η πίεση γίνονται όπου η κοσμολογική ιδιομορφία εμφανίζεται για R = 2m. ( 1 + m ) η επιφανειακή ακτίνα μιας p = 3H 2 (t) 2 1 Ḣ(t), (1.49) 1 2m R R = 12H 2 (t) Ḣ(t), (1.50) 1 2m R Η Misner-Sharp μάζα είναι μια ψευδο-τοπική μάζα βαρυτικού πεδίου, ορισμένη στο σύνορο μιας περιοχής του χωροχρόνου. Σε σφαιρικά συμμετρικό χωροχρόνο η Misner-Sharp μάζα είναι: m MS (t, r) = R 2 (1 gαβ α R β R), (1.51) όπου R(t, r) η επιφανειακή ακτίνα και α, β τρέχουν από το 0 μέχρι το 1. Για να ευρεθεί ο φαινομενικό ορίζοντας (apparent horizon) αναζητούμε παγιδευμένες επιφάνειες (trapped surfaces). Κάθε επιφάνεια μέσα στην παγιδευμένη περιοχή θα ικανοποιεί τη σχέση T = {(t, r) : R(t, r) 2m MS (t, r)}. (1.52) Από την (1.51) έχουμε: 2m MS = R(1 g RR ( R R) 2 ) 2m MS = R(1 (1 2m R H2 (t)r 2 )) 2m MS = 2m + H 2 (t)r 3. Για τον φαινομενικό ορίζοντα: R = 2m + H 2 (t)r 3 1 2m R H2 (t)r 2 = 0 (1.53) g RR = 0. (1.54) 14

16 Χρησιμοποιώντας την μέθοδο του Nickalls, η (1.53) έχει ρίζες: όπου sin(3θ) = 3 3mH(t). R 1 (t) = 2 3H(t) sin θ, (1.55) R 2 (t) = 1 H(t) cos θ 1 3H(t) sin θ, (1.56) R 3 (t) = 1 H(t) cos θ 1 3H(t) sin θ, (1.57) Για να υπάρχουν ορίζοντες πρέπει 0 < sin(3θ) < 1 mh(t) < 1/(3 3). Η χρονική στιγμή όπου mh(t) = 1/(3 3) είναι μοναδική για a(t) t 2/3, H(t) = ȧ(t)/a(t) = 2/(3t), και την συμβολίζουμε ως t = 2 3m. t < t : για πρώιμους χρόνους m > 1 3 3H(t) R 1(t), R 2 (t) μιγαδικές και άρα μή-φυσικές λύσεις. Δεν υπάρχουν ορίζοντες. 1 t = t : m = 3 R 3H(t) 1(t) = R 2 (t) πραγματική λύση. Υπάρχει ένας ορίζοντας στη 1 θέση 3H(t). 1 t > t : για αργότερους χρόνους m < 3 3H(t) Υπάρχουν δύο ορίζοντες. R 1 (t), R 2 (t) πραγματικές λύσεις. Σχήμα 1: Συμπεριφορά των φαινομενικών οριζόντων στο χωροχρόνο McVittie σε dustdominated υπόβαθρο για m = 1. 15

17 1.4 Βαρυτική Κατάρρευση Ευρεση Εξίσωσης Klein-Gordon Εστω η δράση g R S = d x[ 4 2 Λ 1 ] 2 (gµν µ φ ν φ) V (φ). (1.58) Διαφορίζοντας ως προς το βαθμωτό πεδίο φ(t) έχουμε: 1 g µ (g µν ν φ g) V φ = 0. (1.59) Θεωρώντας χωροχρόνο McVittie η εξίσωση Klein-Gordon γίνεται: Τελικά, [ ( [ ] 1 g 1 + m 2 ) ] t g 1 m t φ V φ = 0, V φ = φ(t) + m)2 + m)2 ȧ(t)( + m) ] [3ȧ(t)( mȧ(t)( 7m a(t)( m) 2 a(t)( m) 3 a(t)( m) 2 + φ(t) ( + m ) 2. (1.60) m Εύρεση Εξισώσεων Einstein Διαφορίζοντας ως προς g µν παίρνουμε τις εξισώσεις Einstein: G µν + Λg µν = T µν, (1.61) με G µν = R µν 1 2 g µνr και τον τανυστή ενέργειασ-ορμής T µν = 1 2 g µνg αβ α φ β φ + µ φ ν φ g µν V (φ). (1.62) 16

18 (tt) : (rr, θθ, φφ) : 3ȧ2 (t) a 2 (t) = ρ + Λ [ ] ( 5m)ȧ 2 (t) + 2a(t)ä(t)( + m) a 2 (t)( m) = p Λ Αντικαθιστώντας τις (1.42) και (1.43) προκύπτουν οι εξισώσεις Einstein: ( 3ȧ2 (t) a 2 (t) = m m ) 2 φ2 (t) + V (φ) + Λ [ ( 5m)ȧ 2 (t) + 2a(t)ä(t)( + m) a 2 (t)( m) ( ) m 2 m φ2 (t) V (φ) Λ Βαρυτική Κατάρρευση με Μηδενικό Δυναμικό Το μη γραμμικό δυναμικό σύστημα που καθορίζει την εξέλιξη των a(t), φ(t) με V (φ) = 0 είναι: ] = tt Einstein field equation ( ) 3ȧ2 (t) a 2 (t) = m 2 m φ2 (t) + Λ (1.63) Klein-Gordon equation 0 = φ(t) + m)2 + m)2 ȧ(t)( + m) ] [3ȧ(t)( mȧ(t)( 7m a(t)( m) 2 a(t)( m) 3 a(t)( m) 2 + φ(t) ( + m ) 2 (1.64) m Η ενεργειακή πυκνότητα και η πίεση υπολογίζονται από τις σχέσεις: ρ(t) = 3H 2 (t) Λ, (1.65) ( ) 1 + m p(t) = 3H 2 (t) 2( )Ḣ(t) + Λ. (1.66) 1 m 17

19 0. Η συνθήκη βαρυτικής κατάρρευσης ειναι ȧ(t) < 0 και η ιδιομορφία σχηματίζεται όταν a(t s ) = Βαρυτική κατάρρευση ομογενούς βαθμωτού πεδίου με m = 1 και r = 5: Βαρυτική κατάρρευση ομογενούς βαθμωτού πεδίου με Λ = και r = 5: 18

20 Βαρυτική κατάρρευση ομογενούς βαθμωτού πεδίου με Λ = και m = 1: Συμπεράσματα Η αύξηση της κοσμολογικής σταθεράς Λ επιταχύνει την βαρυτική κατάρρευση. Η αύξηση της μάζας McVittie m επιβραδύνει την βαρυτική κατάρρευση. Η αύξηση της ακτίνας r επιταχύνει την βαρυτική κατάρρευση. Για μεγάλες ακτίνες η βαρυτική κατάρρευση δεν επιταχύνεται περαιτέρω. Η έλλειψη δυναμικού "καταστρέφει" την ανομοιογένεια της πίεσης 19

21 Chapter 2 Introduction Finding solutions to Einstein s equations describing anything beyond the simplest and most symmetric configurations of matter or gravity is a hard and uncertain affair. When available they can provide new insights into the nature of gravity beyond the linearized regime or be used in describing objects of astrophysical relevance. For both reasons any solution potentially describing a black hole embedded in an expanding universe is of considerable interest. Solutions representing time-varying black holes are of great interest in themselves and the first spacetime of this kind is the 1933 McVittie solution [1] of the Einstein equations constructed to study the effect of the cosmic dynamics on a local system. It is thus surprising that a proper understanding of a class of solutions found over 70 years ago is still lacking. These solutions have many of the features one would expect of a black hole embedded in a FRW cosmology: they are spherically symmetric with a singularity at the center, parametrized by a function a(t) and a mass parameter m, reduce to FRW cosmology with scale factor a(t) at large radius, and reduce to known black hole metrics or standard FRW cosmology in all the appropriate parametric limits. More precisely, the properties of the McVittie spacetime are the following: (a) The near-field limit a(t) 1 is Schwarzschild in isotropic coordinates, (b) The far-field limit r is a FRW spacetime, (c) The energy-momentum tensor has a perfect fluid form. Moreover, the energy density of this solution is homogeneous while the pressure is inhomogeneous. 20

22 These properties make them not only interesting in their own right as non-linear solutions, but potentially significant and physically relevant for describing real gravitating objects or holes in the universe. On the other hand, there is no accretion, the mass m is constant, an odd property for a physical black hole in a universe full of matter and radiation. One of the most thorough examinations of the properties of the McVittie metric was attempted in a series of papers by Nolan [13], which review past work on the metric and describe many of its features. Because it is spherically symmetric and asymptotically FRW, the McVittie metric can be used to describe external fields of finite size objects, or exteriors of bubbles or shells separating different regions of spacetime. In these applications the McVittie metric is replaced by a different geometry at small radius. Nolan argued that the would-be null black hole horizon of the McVittie metric is at infinite distance and therefore constitutes a null boundary rather than a horizon, and hence that the metric outside this surface is geodesically complete and cannot describe a black hole at all. The most recent work by Kaloper [3] on McVittie spacetime, though, clearly contradicts Nolan s speculations and proves that the null surface is at a finite distance and therefore renders the standard form of McVittie metric geodesically incomplete, a conclusion that validates the black hole interpretation in at least some cases. In conclusion, the purpose of this thesis is to study the features and properties of the McVittie metric and investigate the gravitational collapse of matter in this geometry. In Chapter 2 we derive the McVittie metric as a solution of the Einstein field equations, in Chapter 3 we prove the basic feature and properties of McVittie metric and in Chapter 4 we study the gravitational collapse of a homogeneous scalar field in the specific spacetime. 21

23 Chapter 3 Derivation of the McVittie Metric 3.1 Introduction In the astronomical applications of General Relativity two types of metrics for the universe are used. For discussing the motion of planets around the Sun, the statical Schwarzschild metric is employed, which may be written in isotropic coordinates as ds 2 = ( ) 1 m 2 ( 2r m dt m ) 4{dr 2 2r 1 2r 1 + r1dω 2 2 }. (3.1) 1 On the other hand, for dealing with the phenomenon of the recession of the spiral nebulae non-statical metrics are used, which can be subdivided into two classes: the Lemaitre class, in which and the de Sitter class, in which { } dr ds 2 = dt 2 e β(t) 2 + r 2 dω 2 (1 + 1, (3.2) 4 kr2 ) 2 ds 2 = dt 2 e β(t) { dr 2 + r 2 dω 2), (3.3) where dω 2 = dθ 2 + sin 2 θdφ 2 is the metric of the 2-sphere and c = 1. In (3.2) the constant k, which may be positive or negative, gives the curvature of space as a whole, local irregularities being disregarded. In (3.3) the curvature of space is zero. One important respect in which the metric (3.1) differs from (3.2) and (3.3) is that in the former the coordinate r 1 is what we shall call an "observer s" coordinate, i.e. it is one based on the assumption that the distance between two points in space at relative rest is 22

24 independent of the time. In (3.2) and (3.3) the coordinate r is one which will be called "cosmical". It is used when the system of nebulae is taken as the basis of reference. An observer in the field uses a coordinate r 1 = re β(t 1)/2 at the instant t 1, so that the "observer s" coordinate for a fixed value of r is not independent of the time. When we consider that we are compelled to observe the universe from the near neighbourhood of a mass-particle (the Sun) it becomes of some interest to find a form of metric which will reduce to the statical metric (3.1) in terms of observer s coordinates, but which can be also expressed, approximately at least, in one of the forms (3.2) and (3.3) when cosmical coordinates are used. Some solutions of the problem have already been proposed. G. Lemaitre 1 has put forward one type of metric. Unfortunately his solution appears to depend on the assumption that the pressure of the matter outside the mass-particle is negative if the density is positive and vice versa. This condition is true whatever the coordinate system used. It is difficult to see how such a case should be applied to the actual universe unless, indeed, both pressure and density were zero. But this reduces Lemaitre s result to the well known one of a mass-particle in an, otherwise empty, de Sitter universe. An alternate type of metric put forward by W. H. McCrea and G. McVittie 2 is also open to critisism on the ground that it implies that the matter in the universe outside the Sun is flowing toward it with a high velocity which is certainly not observed. Hitherto it has been assumed that the problem can be solved by the choice of any set of polar coordinates, with origin at the mass-particle, by assuming that it is evenly spread through space as if it were a gas. It will thus be characterized by (i) its density T 0 0, (ii) its pressure components, T 1 1, T 2 2, T 3 3 and (iii) its momentum T 10, if it is flowing towards or away from the mass-particle. These are the only non-zero components of the energy-momentum tensor when spherical symmetry is assumed. Both density and pressure may, however, be in part due to the presence of radiation. It appears to us axiomatic that in any spacetime model applicable to the actual universe, the density and pressure cannot be negative but may, of course, be zero in a first approximation. The solution to the problem now follows if the observer makes the general assumption that the mass-particle does not occupy a peculiar point in the distribution of matter in the universe. This leads him to conclude that, firstly, the pressure is everywhere isotropic, and secondly, that the matter is "at rest" with respect to his coordinate system. By this is meant that it has, on the whole, zero coordinate velocity, and therefore zero momentum, in 1 G. Lemaitre, M.N., 91, , W.H.McCrea and G.C.McVittie, M.N. 91, ; ibid., 92, 7-12,

25 his system. It might be thought that, in the actual universe, this could not be true because of the phenomenon of the recession of the nebulae. But it must be emphasized that we do not observe a velocity in this connection, but only a shift to the red of the lines of the spectrum in the light emitted by distant objects. It is the whole object of the expanding universe theory to show that even if an observer assigns zero velocity to the nebulae at each instant, yet this red-shift will be observed owing to the properties of space. In arriving at the generalized Schwarzschild field we do not employ observer s coordinates, in the first instance. Instead we obtain the metric using cosmical coordinates analogous to those used in (3.2) and (3.3). 3.2 Equations determining the metric of spacetime We consider an observer engaged in setting up a coordinate system in the neighbourhood of a mass-particle, which he takes as his origin of spatial coordinates. He is provided with rigid measuring rods and makes use of lights triangulations for dealing with points he cannot reach with his measuring rods. He works under the assumption made by terrestrial observers, i.e.: (a) The length of a measuring rod is constant in time and independent of orientation around a given point, (b) The backwards and forwards velocity of light between any two points is the same, (c) The velocity of light is the same in every direction around a given point. Under these circumstances he sets up an "observer s" coordinate system of the orthogonal and isotropic type, in terms of which he expresses the metric applicable to the whole universe. In order to determine the coefficients of this metric he will have to make some assumptions regarding the distribution of matter in the universe. If he believes that his part of the universe is similar to every other part (except for the singularity corresponding to the mass-particle), he will be entitled to assume the following: (i) The matter in the universe is distributed with the spherical symmetry around the origin where there is a mass-particle, (ii) There is no flow of the matter as a whole either towards or away from the origin, otherwise it would be necessary to postulate that, at some time or other, the neighbourhood of the origin had been the scene of an explosion great enough to set the matter in the 24

26 whole universe in motion away from that point. Until some physical process, capable of producing an upheaval of such magnitude, is discovered, our observer will be constrained to postulate (ii), (iii) At any point in the universe the pressure is isotropic. This seems a natural consequence of (ii) since there is now no preferential direction towards which the velocities of the particles, or the flow of radiation, might be directed. Our object is now to find, by means of Einstein s equations, the metric which the observer assigns to the universe in this way. We shall not, however, determine it in terms of observer s coordinates directly, but instead find a metric which satisfies the requirements (i) to (iii) in terms of isotropic cosmical co-ordinates. It can be shown then that, on transforming this metric into observer s coordinates, the properties (a)-(c) and (i)-(iii) are all found to hold [1]. He deduces that this metric is the one actually used by our observer. Consider the most general form of metric which is orthogonal, isotropic in the space coordinates and which expresses the condition for spherical symmetry around the origin. Using cosmical coordinates, it can be written as ds 2 = e ζ(r,t) dt 2 e ν(r,t) {dr 2 + r 2 (dθ 2 + sin 2 θdφ 2 )}, (3.4) where we set c = 1. The distribution of energy density and pressure is given by the Einstein s field equations G µν + Λg µν = κt µν, (3.5) where G µν = R µν 1Rg 2 µν, the Einstein tensor, R µν, R, the Ricci tensor and Ricci scalar, respectively, Λ the cosmological constant, g µν the metric tensor, κ a constant that is related to the gravitational constant, G, and T µν the energy-momentum tensor. It is easy to find the alternate form of the Einstein s field equations R µν Λg µν = κ(t µν 1 2 T g µν), (3.6) 25

27 where T is the proper density. From (3.4) we see that the metric tensor components are g 00 = e ζ, g 11 = e ν, g 22 = r 2 e ν, g 33 = r 2 sin 2 θ e ν, and the inverse components are, respectively, We write g 00 = e ζ, g 11 = e ν, g 22 = e ν r 2, e ν g 33 = r 2 sin 2 θ. T 0 0 = ρ, T 1 1 = p 1, T 2 2 = T 3 3 = p 2, so, using the equation we get T ν µ = T µα g αν, (3.7) T µα = T ν µ g αν. (3.8) Therefore, T 00 = T0 0 g 00 = ρ e ζ, T 11 = T1 1 g 11 = p 1 e ν, T 22 = T2 2 g 22 = p 2 r 2 e ν, T 33 = T3 3 g 33 = p 2 r 2 sin 2 θ e ν. 26

28 The proper density is T = g µν T µν = g 00 T 00 + g 11 T 11 + g 22 T 22 + g 33 T 33 (3.9) = e ζ e ζ ρ e ν e ν p 1 e ν r 2 r2 e ν p 2 e ν r 2 sin 2 θ r2 sin 2 θe ν p 2 (3.10) = ρ p 1 2p 2. (3.11) The only thing missing from equation (3.6) is the Ricci tensor. The Ricci tensor is a contraction of the Riemann curvature tensor, as shown below: R µν = R β µβν = Γβ νµ,β Γβ βµ,ν + Γβ βα Γα νµ Γ β ναγ α βµ, (3.12) where Γ β µν are the Christoffel symbols of the first kind and the comma denotes partial derivation with respect to the parameter that follows the comma. The Christoffel symbols are defined as follows: Γ µ νσ = 1 2 gµλ (g λν,σ + g λσ,ν g νσ,λ ). (3.13) First, we calculate all the non-vanishing Christoffel symbols. Differentiation with respect to t will be denoted with a dot and differentiation with respect to r will be denoted with a dash. The property that we use to make half of the calculations is the symmetry that holds when we interchange the two lower indices, i.e. Γ µ νσ = Γ µ σν. 27

29 Γ 0 µν: Γ 0 00 = 1 2 g00 (g 00,0 + g 00,0 g 00,0 ) = 1 2 e ζ ( e ζ ) = 1 t 2 e ζ e ζ ζ t = 1 2 ζ Γ 0 01 = 1 2 g00 (g 00,1 + g 01,0 g 01,0 ) = 1 2 e ζ r eζ = 1 ζ 2 r = 1 2 ζ Γ 0 02 = 1 2 g00 (g 00,2 + g 02,0 g 02,0 ) = 1 2 e ζ θ eζ = 1 ζ 2 θ = 0 Γ 0 03 = 1 2 g00 (g 00,3 + g 03,0 g 03,0 ) = 1 2 e ζ φ eζ = 1 ζ 2 φ = 0 Γ 0 11 = 1 2 g00 ( 0 g 01,1 Γ 0 22 = 1 2 g00 ( 0 g 02,2 Γ 0 33 = 1 2 g00 ( 0 g 03,3 Γ 0 12 = 1 2 g00 ( 0 g 01,2 + 0 g 01,1 + 0 g 02,2 + 0 g 03,3 + 0 g 02,1 g 11,0 ) = 1 2 e ζ t ( eν ) = 1 2 e ζ e ν ν g 22,0 ) = 1 2 e ζ t ( r2 e ν ) = r2 2 e ζ e ν ν g 33,0 ) = 1 2 e ζ t ( r2 sin 2 θe ν ) = r2 sin 2 θ e ζ e ν ν 2 0 g 12,0 ) = 0 = Γ 0 13 = Γ 0 23 Γ 1 µν: Γ 1 00 = 1 2 g11 ( 0 g 10,0 Γ 1 01 = 1 2 g11 ( 0 g 10,1 Γ 1 02 = 1 2 g11 ( 0 g 10,2 + 0 g 10,0 g 00,1 ) = 1 2 ( e ν ) r eζ = 1 2 e ν e ζ ζ + g 11,0 0 g 01,1 ) = 1 2 ( e ν ) t ( eν ) = 1 2 e ν e ν ν = 1 2 ν + 0 g 12,0 0 g 02,1 ) = 0 Γ 1 11 = 1 2 g11 (g 11,1 + g 11,1 g 11,1 ) = 1 2 ( e ν ) r ( eν ) = 1 2 ν Γ 1 22 = 1 2 g11 ( 0 g 12,2 Γ 1 33 = 1 2 g11 ( 0 g 13,3 + 0 g 12,2 g 22,1 ) = 1 2 ( e ν )( r ( r2 e ν )) = 1 2 e ν (2re ν + r 2 e ν ν ) = r r2 2 ν + 0 g 13,3 g 33,1 ) = 1 2 ( e ν ) r ( r2 sin 2 θe ν ) = 1 2 ( e ν )(2r sin 2 θe ν r 2 sin 2 θe ν ν ) = r sin 2 θ r2 sin 2 θ ν 2 Γ 1 12 = 1 2 g11 (g 11,2 + 0 g 12,1 Γ 1 13 = 1 2 g11 (g 11,3 + 0 g 13,1 Γ 1 23 = 1 2 g11 ( 0 g 12,3 + 0 g 13,2 0 g 12,1 ) = 1 2 ( e ν ) θ ( eν ) = 0 0 g 13,1 ) = 1 2 ( e ν ) φ ( eν ) = 0 0 g 23,1 ) = 0 28

30 Γ 2 µν: Γ 2 00 = 1 2 g22 ( 0 g 20,0 Γ 2 01 = 1 2 g22 ( 0 g 20,1 Γ 2 02 = 1 2 g22 ( 0 g 20,2 Γ 2 03 = 1 2 g22 ( 0 g 20,3 Γ 2 11 = 1 2 g22 ( 0 g 21,1 + 0 g 20,0 g 00,2 ) = 1 2 g22 θ g 00 = g 21,0 0 g 01,2 ) = 0 + g 22,0 g 0 02,2 ) = 1 2 ( e ν r ) 2 t ( r2 e ν ) = e ν 2r 2 ( r2 e ν ν) = 1 2 ν + 0 g 23,0 0 g 03,2 ) = g 21,1 g 11,2 ) = 1 2 g22 θ g 11 = 0 Γ 2 22 = 1 2 g22 (g 22,2 + g 22,2 g 22,2 ) = 1 2 g22 θ g 22 = 0 Γ 2 11 = 1 2 g22 ( 0 g 23,3 + 0 g 23,3 = e ν 2r 2 (r2 sin 2 θe ν ) = cos θ sin θ Γ 2 12 = 1 2 g22 ( 0 g 21,2 Γ 2 13 = 1 2 g22 ( 0 g 21,3 g 33,2 ) = 1 2 g22 θ g 33 = 1 2 ( e ν r 2 ) θ ( r2 sin 2 θe ν ) + g 22,1 0 g 12,2 ) = 1 2 ( e ν r ) 2 r ( r2 e ν ) = e ν 2r 2 (2reν + r 2 e ν ν ) = 1 r ν + 0 g 23,1 Γ 2 23 = 1 2 g22 (g 22,3 + 0 g 23,2 0 g 13,2 ) = 0 g 0 23,2 ) = 1 2 g22 φ g 22 = 0 29

31 Γ 3 µν: Γ 3 00 = 1 2 g33 ( 0 g 30,0 Γ 3 01 = 1 2 g33 ( 0 g 30,1 Γ 3 02 = 1 2 g33 ( 0 g 30,2 Γ 3 03 = 1 2 g33 ( 0 g 30,3 Γ 3 11 = 1 2 g33 ( 0 g 31,1 Γ 3 22 = 1 2 g33 ( 0 g 32,2 + 0 g 30,0 + 0 g 31,0 + 0 g 32,0 0 g 00,3 ) = 0 0 g 01,3 ) = 0 0 g 02,3 ) = 0 + g 33,0 g 0 03,3 ) = 1 e ν ( 2 r 2 sin 2 θ ) t ( r2 sin 2 θe ν ) = + 0 g 31,1 + 0 g 32,2 0 g 11,3 ) = 0 0 g 22,3 ) = 0 Γ 3 33 = 1 2 g33 (g 33,3 + g 33,3 g 33,3 ) = 1 2 g33 φ g 33 = 0 Γ 3 12 = 1 2 g33 ( 0 g 31,2 Γ 3 13 = 1 2 g33 ( 0 g 31,3 = + 0 g 32,1 0 g 12,3 ) = 0 + g 33,1 0 g 13,3 ) = 1 e ν ( 2 r 2 sin 2 θ ) r ( r2 sin 2 θe ν ) e ν 2r 2 sin 2 θ (2r sin2 θe ν + r 2 sin 2 θe ν ν ) = 1 r ν Γ 3 23 = 1 2 g33 ( 0 g 32,3 = e ν 2r 2 sin 2 θ (2r2 sin θ cos θe ν ) = cos θ sin θ + g 33,2 g 0 23,3 ) = 1 e ν ( 2 r 2 sin 2 θ ) θ ( r2 sin 2 θe ν ) e ν 2r 2 sin 2 θ (r2 sin 2 θe ν ν) = 1 2 ν 30

32 Finally, the non-vanishing Christoffel symbols are: Γ 0 00 = 1 2 ζ Γ 0 01 = Γ 0 10 = 1 2 ζ Γ 0 11 = eν 2e ζ ν Γ0 22 = r2 e ν 2e ζ Γ 0 33 = r2 sin 2 θe ν 2e ζ ν Γ 1 00 = eζ 2e ν ζ Γ 1 01 = Γ 1 10 = 1 2 ν Γ1 11 = 1 2 ν Γ 1 22 = r r2 2 ν Γ 1 33 = r sin 2 θ 1 2 r2 sin 2 θν Γ 2 02 = Γ 2 20 = 1 2 ν Γ2 12 = Γ 2 21 = 1 r ν ν Γ 2 33 = cos θ sin θ Γ 3 13 = Γ 3 31 = 1 r ν Γ 3 03 = Γ 3 30 = 1 2 ν Γ 3 23 = Γ 3 32 = cos θ sin θ Now, we compute the non-vanishing components of the Ricci tensor: R 00 = Γ 0 00,0 Γ 0 00,0 + Γ 0 00Γ Γ 1 00Γ Γ 2 00Γ Γ 3 00Γ 0 30 Γ 0 00Γ 0 00 Γ 1 00Γ 0 10 Γ 2 00Γ 0 20 Γ 3 00Γ Γ 1 00,1 Γ 1 01,0 + Γ 0 00Γ Γ 1 00Γ Γ 2 00Γ Γ 3 00Γ 1 31 Γ 0 01Γ 1 00 Γ 1 01Γ 1 10 Γ 2 01Γ 1 20 Γ 3 01Γ Γ 2 00,2 Γ 2 02,0 + Γ 0 00Γ Γ 1 00Γ Γ 2 00Γ Γ 3 00Γ 2 32 Γ 0 02Γ 2 00 Γ 1 02Γ 2 10 Γ 2 02Γ 2 20 Γ 3 02Γ Γ 3 00,3 Γ 3 03,0 + Γ 0 00Γ Γ 1 00Γ Γ 2 00Γ Γ 3 00Γ 3 33 Γ 0 03Γ 3 00 Γ 1 03Γ 3 10 Γ 2 03Γ 3 20 Γ 3 03Γ 3 30 = t ( ν 2 ) + r( eζ 2e ν ζ ) ζ 2 ( eζ 2e ν ζ ) ν ν ζ 2 ν 2 + ( eζ 2e ν ζ )( 1 r + ν 2 ) = 3 2 ν 3 4 ( ν) ζ ν + eζ 2e ν ζ + ζ ζ e ζ e ν ν e ζ e ν 1 e ζ 2(e ν ) ( eζ 2e ν ζ )( 1 r + ν 2 ) t( ν 2 ) ( ν 2 )2 + ζ 2 = eζ e ν (ζ 2 + (ζ ) 2 + ζ ν ζ r ) (3 2 ν ( ν)2 3 4 ζ ν) ν 2 + ( eζ 2e ν ζ ) ν 2 t( ν 2 ) ( ν 2 )2 + ζ ν 2 2 e ζ e ν (ζ ) e ν ζ ν + eζ ζ e ν r + eζ ζ ν e ν 4 31

33 R 11 = Γ 0 11,0 Γ 0 10,1 + Γ 0 11Γ Γ 1 11Γ Γ 2 11Γ Γ 3 11Γ 0 30 Γ 0 10Γ 0 01 Γ 1 10Γ 0 11 Γ 2 10Γ 0 21 Γ 3 10Γ Γ 1 11,1 Γ 1 11,1 + Γ 0 11Γ Γ 1 11Γ Γ 2 11Γ Γ 3 11Γ 1 31 Γ 0 11Γ 1 01 Γ 1 11Γ 1 11 Γ 2 11Γ 1 21 Γ 3 11Γ Γ 2 11,2 Γ 2 12,1 + Γ 0 11Γ Γ 1 11Γ Γ 2 11Γ Γ 3 11Γ 2 32 Γ 0 12Γ 2 01 Γ 1 12Γ 2 11 Γ 2 12Γ 2 21 Γ 3 12Γ Γ 3 11,3 Γ 3 13,1 + Γ 0 11Γ Γ 1 11Γ Γ 2 11Γ Γ 3 11Γ 3 33 Γ 0 13Γ 3 01 Γ 1 13Γ 3 11 Γ 2 13Γ 3 21 Γ 3 13Γ 3 31 = 1 2 ζ + eν 2e ν + ν e ν e ζ ν e ν e ζ ζ 1 ζ 2 (e ζ ) 2 2 (ζ ) 2 + ν ζ 2 2 eν 4e ( ζ ν)2 + 1 r ν + ν 2 (1 r + ν 2 ) + 1 r ν 2( 1 r + ν 2 )2 + eν 4e ζ ( ν)2 + ν 2 (1 r + ν 2 ) + eν 4e ζ ν ζ + eν 4e ζ ( ν)2 = eν e ζ ( ν ( ν)2 1 4 ν ζ) ( 1 2 ζ (ζ ) ν ζ + ν + ν r ) R 22 = Γ 0 22,0 Γ 0 20,2 + Γ 0 22Γ Γ 1 22Γ Γ 2 22Γ Γ 3 22Γ 0 30 Γ 0 20Γ 0 02 Γ 1 20Γ 0 12 Γ 2 20Γ 0 22 Γ 3 20Γ Γ 1 22,1 Γ 1 21,2 + Γ 0 22Γ Γ 1 22Γ Γ 2 22Γ Γ 3 22Γ 1 31 Γ 0 21Γ 1 02 Γ 1 21Γ 1 12 Γ 2 21Γ 1 22 Γ 3 21Γ Γ 2 22,2 Γ 2 22,2 + Γ 0 22Γ Γ 1 22Γ Γ 2 22Γ Γ 3 22Γ 2 32 Γ 0 22Γ 2 02 Γ 1 22Γ 2 12 Γ 2 22Γ 2 22 Γ 3 22Γ Γ 3 22,3 Γ 3 23,2 + Γ 0 22Γ Γ 1 22Γ Γ 2 22Γ Γ 3 22Γ 3 33 Γ 0 23Γ 3 02 Γ 1 23Γ 3 12 Γ 2 23Γ 3 22 Γ 3 23Γ 3 32 = t ( r2 e ν 2e ν) + r2 e ν ζ 2e ζ θ cot θ cot 2 θ = ( r2 e ν r2 ν + ν 2eζ 2 ν r 2 (ν ) 2 r 2 4 ζ r2 ν + ( r 2 2 ν ) ζ 2 + r( r r2 2 ν ) + r2 e ν 2e ν ν r2 + ( r ζ 2 2 ν ) ν 2 νe ν e ζ ζe ν e ζ ) + r2 e ν e 2ζ 4e ν ζ ζ r ζ 2 ζ ν r 2 4 sin θ sin θ cos θ cos θ sin 2 cos2 θ θ sin 2 θ 1 rν r2 2 ν + r2 e ν 4e ζ ( ν)2 = r2 e ν 2e ν + r2 e ν ζ 2e ζ ν2 r2 e ν 2e ν ζ + r2 e ν ζ 4e ν ζ ζ r ζ 2 ζ ν r 2 1 rν r2 4 2 ν + r2 e ν 4e ( ζ ν)2 ν r 2 (ν ) 2 r sin 2 θ cos2 θ sin 2 θ = r 2 [ eν e ζ ( ν ν2 ν ζ 4 ) ( ζ 2r + ζ ν 4 + 3ν 2r + ν 2 + (ν ) 2 4 )] 32

34 R 33 = Γ 0 33,0 Γ 0 30,3 + Γ 0 33Γ Γ 1 33Γ Γ 2 33Γ Γ 3 33Γ 0 30 Γ 0 30Γ 0 03 Γ 1 30Γ 0 13 Γ 2 30Γ 0 23 Γ 3 30Γ Γ 1 33,1 Γ 1 31,3 + Γ 0 33Γ Γ 1 33Γ Γ 2 33Γ Γ 3 33Γ 1 31 Γ 0 31Γ 1 03 Γ 1 31Γ 1 13 Γ 2 31Γ 1 23 Γ 3 31Γ Γ 2 33,2 Γ 2 32,3 + Γ 0 33Γ Γ 1 33Γ Γ 2 33Γ Γ 3 33Γ 2 32 Γ 0 32Γ 2 03 Γ 1 32Γ 2 13 Γ 2 32Γ 2 23 Γ 3 32Γ Γ 3 33,3 Γ 3 33,3 + Γ 0 33Γ Γ 1 33Γ Γ 2 33Γ Γ 3 33Γ 3 33 Γ 0 33Γ 3 03 Γ 1 33Γ 3 13 Γ 2 33Γ 3 23 Γ 3 33Γ 3 33 = ( r2 sin 2 θe ν ν + r2 sin 2 θ 2e ζ 2 + r ( r sin 2 θ r2 sin 2 θ 2 cot θ( cos θ sin θ) = r2 sin 2 θe ν 2e ζ ν + r2 sin 2 θe ν 2e ζ sin 2 θ r sin 2 θν r2 sin 2 θν + cos 2 θ = r 2 sin 2 θ[ eν e ζ ( ν ν2 ν νeν ζe ν ) + r2 sin 2 θe ν e ζ 4e ζ ν ) + r2 sin 2 θe ν 4e ζ 2 ν 2 r2 sin 2 θe ν 2e ζ ν ζ + ( r sin 2 θ r2 sin 2 θ ν ) ζ 2 2 ν 2 + ( r sin 2 θ r2 sin 2 θ ν ) ν θ( cos θ sin θ) ν ζ + r2 sin 2 θe ν ν 4e ζ r sin2 θζ r2 sin 2 θζ ν ζ r2 sin 2 θe ν ν 2 r sin2 θν r2 sin 2 θν 2 ( sin 2 θ + cos 2 θ) 2e ζ 2 4 ν ζ 4 ) ( ζ 2r + ζ ν 4 + 3ν 2r + ν 2 + (ν ) 2 4 )] R 01 = Γ 0 01,0 Γ 0 01,0 + Γ 0 01Γ Γ 1 01Γ Γ 2 01Γ Γ 3 01Γ 0 30 Γ 0 00Γ 0 01 Γ 1 00Γ 0 11 Γ 2 00Γ 0 21 Γ 3 00Γ Γ 1 01,1 Γ 1 01,1 + Γ 0 01Γ Γ 1 01Γ Γ 2 01Γ Γ 3 01Γ 1 31 Γ 0 01Γ 1 01 Γ 1 01Γ 1 11 Γ 2 01Γ 1 21 Γ 3 01Γ Γ 2 01,2 Γ 2 02,1 + Γ 0 01Γ Γ 1 01Γ Γ 2 01Γ Γ 3 01Γ 2 32 Γ 0 02Γ 2 01 Γ 1 02Γ 2 11 Γ 2 02Γ 2 21 Γ 3 02Γ Γ 3 01,3 Γ 3 03,1 + Γ 0 01Γ Γ 1 01Γ Γ 2 01Γ Γ 3 01Γ 3 33 Γ 0 03Γ 3 01 Γ 1 03Γ 3 11 Γ 2 03Γ 3 21 Γ 3 03Γ 3 31 = eζ ζ e ν ν 2e ν 2e + νζ ζ 4 νζ 4 + νζ 4 r( ν 2 ) + νζ 4 r( ν 2 ) ν 2 (1 r + ν 2 ) + νζ 4 + ν 2 (1 r + ν 2 ) = νζ 2 ν 33

35 The rest of the components of the Ricci tensor are equal to zero, so the Einstein s field equations (3.6) reduce to the following five: R 00 Λg 00 = κ(t g 00T ) R 00 = e ζ (Λ + κ 2 (2ρ ρ + p 1 + 2p 2 )) e ζ (Λ + κ 2 (ρ + p 1 + 2p 2 )) = eζ e ν (ζ 2 + (ζ ) 2 + ζ ν ζ r ) (3 2 ν ( ν)2 3 4 ζ ν) Λ + κ 2 (ρ + p 1 + 2p 2 ) = e ν ( ζ 2 + (ζ ) 2 + ζ ν ζ r ) e ζ ( 3 2 ν ( ν)2 3 4 ζ ν) R 11 Λg 11 = κ(t g 11T ) R 11 = e ν ( Λ + κ 2 (2p 1 + ρ p 1 2p 2 )) e ν (Λ + κ 2 (2p 2 p 1 ρ)) = eν e ζ ( ν ( ν)2 1 4 ν ζ) ( 1 2 ζ (ζ ) ν ζ + ν + ν r ) Λ + κ 2 (2p 2 p 1 ρ) = e ν ( 1 2 ζ (ζ ) ν ζ + ν + ν r ) e ζ ( ν ( ν)2 1 ν ζ) 4 R 22 Λg 22 = κ(t g 22T ) R 22 = r 2 e ν ( Λ + κ 2 (2p 2 + ρ p 1 2p 2 )) r 2 e ν (Λ + κ 2 (p 1 ρ)) = r 2 [ eν e ζ ( ν ν2 ν ζ 4 ) ( ζ 2r + ζ ν 4 + 3ν 2r + ν 2 + (ν ) 2 4 )] Λ + κ 2 (p 1 ρ) = e ν ( ζ 2r + ζ ν 4 + 3ν 2r + ν 2 + (ν ) 2 4 ) e ζ ( ν ν2 ν ζ 4 ) R 33 Λg 33 = κ(t g 33T ) R 33 = r 2 sin 2 θe ν (Λ + κ 2 (2p 2 ρ + p 1 2p 2 )) r 2 sin 2 θe ν (Λ + κ 2 (p 1 ρ)) = r 2 sin 2 θ[ eν e ζ ( ν ν2 ν ζ 4 ) ( ζ 2r + ζ ν 4 + 3ν 2r + ν 2 + (ν ) 2 4 )] Λ + κ 2 (p 1 ρ) = e ν ( ζ 2r + ζ ν 4 + 3ν 2r + ν 2 + (ν ) 2 4 ) e ζ ( ν ν2 ν ζ 4 ), 34

36 and finally, R 01 Λg 01 = κ(t g 01T ) κt 01 = νζ 2 ν. Altogether, the Einstein s field equations are Λ + κ 2 (ρ + p 1 + 2p 2 ) = e ν ( ζ 2 + (ζ ) 2 + ζ ν ζ r ) e ζ ( 3 2 ν ( ν)2 3 4 ζ ν) (3.14) Λ + κ 2 (2p 2 p 1 ρ) = e ν ( ζ 2 + (ζ ) 2 ν ζ ν + ν r ) e ζ ( ν ( ν)2 1 ν ζ) 4 (3.15) Λ + κ 2 (p 1 ρ) = e ν ( ζ 2r + ζ ν 4 + 3ν 2r + ν 2 + (ν ) 2 4 ) e ζ ( ν ν2 κt 01 = νζ 2 ν ν ζ 4 ) (3.16) (3.17) Considering the conditions (ii) and (iii) the energy-momentum tensor has a perfect fluid form, that is T ν µ = (ρ, p, p, p) p 1 = p 2 = p 3 = p, we get: Λ + κ 2 (ρ + 3p 1) = e ν ( ζ 2 + (ζ ) 2 + ζ ν ζ r ) e ζ ( 3 2 ν ν2 3 4 ζ ν) (3.18) Λ + κ 2 (p 1 ρ) = e ν ( ζ 2 + (ζ ) 2 ν ζ ν + ν r ) e ζ ( ν ν2 1 4 ν ζ) (3.19) Λ + κ 2 (p 1 ρ) = e ν ( ζ 2r + ζ ν 4 + 3ν 2r + ν 2 + (ν ) 2 4 ) e ζ ( ν ν2 1 4 ν ζ) (3.20) νζ 2 ν = 0 (3.21) From (3.19) and (3.20) we see that the left hand sides are equal. Since the left hand sides are equal, the right ones must be equal, too. For the right hand sides to be equal, the coefficients of e ν must be equal, i.e. ζ 2 + (ζ ) 2 4 ν ζ 4 + ν + ν r = ζ 2r + ζ ν 4 + 3ν 2r + ν 2 + (ν ) 2 4 ζ 2 + ν 2 + (ζ ) 2 (ν ) 2 ν ζ ν 2r ζ 2r = 0 ζ + ν + (ζ ) 2 2 (ν ) 2 2 ν ζ 1 r (ν + ζ ) = 0 35

37 Our two fundamental equations for determining the coefficients of the metric (3.4) are ζ + ν + (ζ ) 2 2 ν νζ = 0, 2 (3.22) (ν ) 2 ν ζ 1 2 r (ν + ζ ) = 0. (3.23) 3.3 Solutions of the equations We shall now show that ν and ζ can be determined by the use of (3.22) and (3.23) alone. The equation (3.22) can be solved immediately. Dividing throughout by ν, we get ν ν = ζ 2 (log ν) = ζ 2 (log ν) dr = 1 ζ r 2 r dr log ν = 1 ζ(r, t) + b(t) 2 ν = e ζ(r,t)/2+b(t) ν = e b(t) e ζ(r,t)/2 = a(t)e ζ(r,t)/2 ν = a(t)e ζ(r,t)/2 dt + α(r) (3.24) where, we set a(t) = e b(t) and in the integral, r is treated as a constant and α(r) is a function of r alone. We shall show that the generalized Schwarzschild field we are seeking cannot be included amongst those solutions for which ζ is a function of r alone. For, in such a case, ν = β(t)e 1 2 ζ(r) + α(r), (3.25) where β(t) = a(t) dt. Substitution into (3.23) shows that we can have two possibilities: (1) β is constant, in which case we can only arrive at the statical Schwarzschild solution, or (2) β is arbitrary, ζ is a constant, and α(r) is given by d 2 α dr 1 dα 2 r dr 1 2 ( ) 2 dα = 0, (3.26) dr 36

38 whence α(r) = 2 log ( ) kr2. (3.27) This merely brings us back to the case of solutions of the Lemaitre class. It therefore appears that there is no generalization of the Schwarzschild metric (in terms of cosmical coordinates) in which the mass of the central object enters as a constant independent of time. Turning to solution of (3.22) in which ζ is a function of both r and t, we consider cases in which α(r) = 0. This function is evidently dependent on the curvature of space as a whole, so that putting it equal to zero is equivalent to dealing with metrics analogous to (3.3), where there is zero spatial curvature. The solution we require must have a singularity at the origin similar to that possessed by the Schwarzschild metric in isotropic coordinates. ζ and ν must therefore be expressible as power series in 1/r. We assume e ζ/2 = γ = 1 + a 1 u m 1 + a 2 u m 2 + a 3 u m , (3.28) where u = 1/r, a s are functions of t and the powers of u are arranged in ascending order. Substituting into (3.24) we get ν = a(t)dt(1 + a 1 u m 1 + a 2 u m 2 + a 3 u m ) = a(t)dt + a(t)dt(a 1 u m 1 + a 2 u m 2 + a 3 u m ) = β(t) + β s (t)u ms, (3.29) s=1 where β(t) = β s (t) = a(t)dt, (3.30) a(t)a s (t)dt. (3.31) The equation (3.23) can be written, on changing the independent variable from r to u and 37

39 substituting for ζ in terms of γ, in a new form using the chain rule. First, we write e ζ/2 = γ ζ = 2 ln γ u = 1 r u r = 1 r = 2 u2 2 u r = 2 2 r = 3 2u3 γ r = γ u u r = u2 γ u 2 γ r 2 = 2 γ u 2 ( u r )2 + γ u 2 u r = 2 γ γ 2 u4 + 2u3 u2 u and then we compute the following terms that are present in (3.23): ζ = ζ r = 2 γ γ ζ = 2 ζ r = 2u2 γ γ u r = 2 r ( 2 γ ν = ν r = ν u ν = u2 u r u ν = 2 ν r = 2 ν 2 u ( u 2 r )2 + ν u Equation (3.23), now, becomes γ r ) = 2 γ 2 ( γ r )2 + 2 γ 2 u r = 2 ν ν 2 u4 + 2u3 u2 u ν + ζ uν uζ ν ζ + (ν ) 2 u 4 2 ν ν + 2u3 r2 u 2u4 γ ( γ 2 u )2 + 2u4 2 γ γ u + 4u3 2 γ u4 2 ( ν u )2 + 4u4 2γ 2 ( γ u )2 = 0 2 γ r = 2 2u4 γ ( γ 2 u )2 + 2u4 2 γ γ u + 4u3 γ 2 γ u + (ζ ) 2 2 = 0 2 γ ν + u3 u u + 2u3 γ γ u 2u4 γ γ u ν u Multiplying throughout by γ u 3 we get γu 2 ν ν + 3γ u2 u + γ 2u 2 u + 6 γ 2 u 2u γ ν u u 1 2 uγ( ν u )2 = 0. (3.32) 38

40 We now substitute from (3.28) and (3.29) into (3.32). We first compute ν 0 u = u a(t)dt + a(t)a s (t)dt u u ms s=1 = a(t)a s (t)dt m s u ms 1 s=1 γ u = 0 + a 1m 1 u m1 1 + a 2 m 2 u m2 1 + a 3 m 3 u m = a s m s u ms 1 s=1 2 ν u = 2 Therefore (3.32) becomes s=1 a(t)a s (t)dtm s (m s 1)u ms 2 2 γ u = a 2 s m s (m s 1)u ms 2 s=1 (1 + a 1 u m 1 + a 2 u m 2 + a 3 u m ) [ s=1 s=1 a(t)a s (t)dtm s (m s 1)u ms a s m s (m s 1)u ms a s m s u ms 1 2u( a s m s u ms 1 )( s=1 s=1 1 2 (u + a 1u m1+1 + a 2 u m2+1 + a 3 u m )( s=1 s=1 s=1 a(t)a s (t)dt m s u ms 1] a(t)a s (t)dt m s u ms 1 ) a(t)a s (t)dt m s u ms 1 ) 2 = 0 β s m s (m s 1)u ms 1 + β s a s m s (m s 1)u 2ms β s m s u ms β s a s m s u 2ms 1 s=1 s=1 +2 a s m s (m s 1)u ms a s m s u ms 1 2 β s a s m 2 su 2ms 1 1 β 2 sm 2 2 su 2ms 1 s=1 s=1 s=1 s=1 1 β 2 2 sm 2 sa s u 3ms 1 = 0 s=1 s=1 s=1 39

41 u ms 1[ ] β s m s (m s 1) + 3β s m s + 2a s m s (m s 1) + 6a s m s + u 2ms 1[ β s a s m s (m s 1) + 3β s m s a s s=1 s=1 2β s a s m 2 s 1 ] 2 β2 sm 2 s + u 3ms 1[ 1 ] 2 β2 sm 2 sa s = 0 (3.33) The lowest power of u turns out to be u m1 1. On equating its coefficient to zero we obtain for s = 1 s=1 β 1 m 1 (m 1 1) + 3β 1 m 1 + 2a 1 m 1 (m 1 1) + 6a 1 m 1 = 0 m 2 1β 1 m 1 β 1 + 3β 1 m 1 + 2a 1 m 2 1 2a 1 m 1 + 6a 1 m 1 = 0 m 2 1β 1 + 2β 1 m 1 + 2a 1 m a 1 m 1 = 0 m 1 (m 1 + 2)(2a 1 + β 1 ) = 0 (3.34) The next two powers of u are u 2m1 1 and u m2 1. Hence we have m 2 = 2m 1 and, in general m s = sm 1. It therefore follows from the indicial equation (3.34) that the only way in which we can obtain a solution as a power series in u, is by taking m 1 = 1 and 2a 1 + β 1 = 0. This relation, together with (3.30) and (3.31), gives a 1 = 1 2 β 1 a 1 = 1 β 2 1 a 1 = 1 2 (a a 1) The coefficient of u 2ms 1 for s = 1 when equated to zero gives a 1 = 1 a 1 2 β. (3.35) β 1 a 1 m β 1 m 1 a β2 1m 2 1 = 0. Using m 1 = 1 and β 1 = 2a 1 we get 4a 2 1 = 0. The coefficient of u ms 1 for s = 2 when equated to zero gives, as before, m 2 (m 2 + 2)(2a 2 + β 2 ) = 0 (3.36) 40

42 We see that m 2 (m 2 + 2)(2a 2 + β 2 ) = 4a 2 1, because the powers of u, u 2m1 1 and u m2 1, must be equal. Proceeding with the calculation while using m 2 = 2m 1 and m 1 = 1 we get 2m 1 (2m 1 + 2)(2a 2 + β 2 ) = 4a 2 1 8(2a 2 + β 2 ) = 4a 2 1 2a 2 + β 2 = 1 2 a2 1 = c 2 a 2 1. Differentiating this relation with respect to t and using (3.35) we get 2a 2 + d dt 2a 2 + β 2 = c 2 a 2 1 a(t)a 2 (t)dt = 2c 2 a 1 a 1 2a 2 + a a 2 = 2c 2 a 1 a 1 2a 2 + β a 2 = 2c 2 a 1 a 1 2a 2 2 a 1 a 2 = 2c 2 a 1 a 1 ( 2 ) a 1 a 1 a 2 a 2 = c 2 a 1 a 1 a 1 a 2 a 1 a 2 a 1 = c 2 a 1 a 1 a 1 a 2 a 1 a 2 a 1 = c a 2 2 a 1 1 d dt (a 2 d )dt = a 1 dt (c 2a 1 )dt a 2 = c 2 a 2 1 So, 2a 2 + β 2 = c 2 a 2 1 β 2 = c 2 a 2 1 2c 2 a 2 1 β 2 = c 2 a

43 Proceeding in this manner it soon becomes apparent that a n = c n a n 1, β n = 2c n n an 1, (3.37) where the c n are constants. Hence, if the solution we are seeking exists at all, it must be of the following form (using m 1 = 1, m s = sm 1, u = 1/r, a 1 = µ) with γ = 1 + a s u ms = 1 + s=1 ν = β(t) + s=1 a s u s = 1 + s=1 u ms β s (t) = β(t) 2 s=1 c s a s 1u s = 1 + s=1 ( ) s µ(t) c s (3.38) r ( ) s µ(t) (3.39) s=1 u s a s c s 1 s = β(t) 2 c s s s=1 1 2 β = µ µ. (3.40) We can now show that γ, ν given by (3.38) and (3.39) can be expressed in finite form. By differentiating (3.39) with respect to r we get: ν r = 2 s=1 c s s s ( µ(t) = 2 c s r s=1 ( ) γ 1 = 2, r ( ) s 1 1 µ(t) ( s 1r ) r 2 ) s 1 r where we used (3.38) in the final step. By differentiating (3.39) with respect to t we get: ν t = β(t) 2 = β(t) 2 s=1 s=1 c s s s µ(t)s 1 ( )s µ(t) µ(t) c s r µ(t) = 2 µ(t) µ(t) 2(γ 1) µ(t) µ(t) = 2 µ(t) µ(t) γ, ( ) s 1 µ(t) r r 42

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