sage: E = EllipticCurve([0, -1, 0, 9, -9])
gp: E = ellinit([0, -1, 0, 9, -9])
magma: E := EllipticCurve([0, -1, 0, 9, -9]);
oscar: E = elliptic_curve([0, -1, 0, 9, -9])
sage: E.short_weierstrass_model()
magma: WeierstrassModel(E);
oscar: short_weierstrass_model(E)
Z ⊕ Z / 2 Z \Z \oplus \Z/{2}\Z Z ⊕ Z / 2 Z
magma: MordellWeilGroup(E);
P P P h ^ ( P ) \hat{h}(P) h ^ ( P ) Order
( 3 , 6 ) (3, 6) ( 3 , 6 ) 0.64708411008304578402349115724 0.64708411008304578402349115724 0 . 6 4 7 0 8 4 1 1 0 0 8 3 0 4 5 7 8 4 0 2 3 4 9 1 1 5 7 2 4 ∞ \infty ∞
( 1 , 0 ) (1, 0) ( 1 , 0 ) 0 0 0 2 2 2
( 1 , 0 ) \left(1, 0\right) ( 1 , 0 ) , ( 3 , ± 6 ) (3,\pm 6) ( 3 , ± 6 ) , ( 6 , ± 15 ) (6,\pm 15) ( 6 , ± 1 5 ) , ( 41 , ± 260 ) (41,\pm 260) ( 4 1 , ± 2 6 0 )
sage: E.integral_points()
magma: IntegralPoints(E);
Invariants
Conductor :
N N N
=
1920 1920 1 9 2 0 = 2 7 ⋅ 3 ⋅ 5 2^{7} \cdot 3 \cdot 5 2 7 ⋅ 3 ⋅ 5
sage: E.conductor().factor()
gp: ellglobalred(E)[1]
magma: Conductor(E);
oscar: conductor(E)
Discriminant :
Δ \Delta Δ
=
− 57600 -57600 − 5 7 6 0 0 = − 1 ⋅ 2 8 ⋅ 3 2 ⋅ 5 2 -1 \cdot 2^{8} \cdot 3^{2} \cdot 5^{2} − 1 ⋅ 2 8 ⋅ 3 2 ⋅ 5 2
sage: E.discriminant().factor()
gp: E.disc
magma: Discriminant(E);
oscar: discriminant(E)
j-invariant :
j j j
=
281216 225 \frac{281216}{225} 2 2 5 2 8 1 2 1 6 = 2 7 ⋅ 3 − 2 ⋅ 5 − 2 ⋅ 1 3 3 2^{7} \cdot 3^{-2} \cdot 5^{-2} \cdot 13^{3} 2 7 ⋅ 3 − 2 ⋅ 5 − 2 ⋅ 1 3 3
sage: E.j_invariant().factor()
gp: E.j
magma: jInvariant(E);
oscar: j_invariant(E)
Endomorphism ring :
E n d ( E ) \mathrm{End}(E) E n d ( E ) = Z \Z Z
Geometric endomorphism ring :
E n d ( E Q ‾ ) \mathrm{End}(E_{\overline{\Q}}) E n d ( E Q )
=
Z \Z Z
(no potential complex multiplication )
sage: E.has_cm()
magma: HasComplexMultiplication(E);
Sato-Tate group :
S T ( E ) \mathrm{ST}(E) S T ( E ) = S U ( 2 ) \mathrm{SU}(2) S U ( 2 )
Faltings height :
h F a l t i n g s h_{\mathrm{Faltings}} h F a l t i n g s ≈ − 0.39866793906210754893948555570 -0.39866793906210754893948555570 − 0 . 3 9 8 6 6 7 9 3 9 0 6 2 1 0 7 5 4 8 9 3 9 4 8 5 5 5 5 7 0
gp: ellheight(E)
magma: FaltingsHeight(E);
oscar: faltings_height(E)
Stable Faltings height :
h s t a b l e h_{\mathrm{stable}} h s t a b l e ≈ − 0.86076605943540442188430697001 -0.86076605943540442188430697001 − 0 . 8 6 0 7 6 6 0 5 9 4 3 5 4 0 4 4 2 1 8 8 4 3 0 6 9 7 0 0 1
magma: StableFaltingsHeight(E);
oscar: stable_faltings_height(E)
a b c abc a b c quality :
Q Q Q ≈ 0.9000196641005145 0.9000196641005145 0 . 9 0 0 0 1 9 6 6 4 1 0 0 5 1 4 5
Szpiro ratio :
σ m \sigma_{m} σ m ≈ 2.3931036004828496 2.3931036004828496 2 . 3 9 3 1 0 3 6 0 0 4 8 2 8 4 9 6
Analytic rank :
r a n r_{\mathrm{an}} r a n = 1 1 1
sage: E.analytic_rank()
gp: ellanalyticrank(E)
magma: AnalyticRank(E);
Mordell-Weil rank :
r r r = 1 1 1
sage: E.rank()
gp: [lower,upper] = ellrank(E)
magma: Rank(E);
Regulator :
R e g ( E / Q ) \mathrm{Reg}(E/\Q) R e g ( E / Q ) ≈ 0.64708411008304578402349115724 0.64708411008304578402349115724 0 . 6 4 7 0 8 4 1 1 0 0 8 3 0 4 5 7 8 4 0 2 3 4 9 1 1 5 7 2 4
sage: E.regulator()
gp: G = E.gen \\ if available
matdet(ellheightmatrix(E,G))
magma: Regulator(E);
Real period :
Ω \Omega Ω ≈ 1.9560870028882363354219270048 1.9560870028882363354219270048 1 . 9 5 6 0 8 7 0 0 2 8 8 8 2 3 6 3 3 5 4 2 1 9 2 7 0 0 4 8
sage: E.period_lattice().omega()
gp: if(E.disc>0,2,1)*E.omega[1]
magma: (Discriminant(E) gt 0 select 2 else 1) * RealPeriod(E);
Tamagawa product :
∏ p c p \prod_{p}c_p ∏ p c p = 8 8 8
= 2 ⋅ 2 ⋅ 2 2\cdot2\cdot2 2 ⋅ 2 ⋅ 2
sage: E.tamagawa_numbers()
gp: gr=ellglobalred(E); [[gr[4][i,1],gr[5][i][4]] | i<-[1..#gr[4][,1]]]
magma: TamagawaNumbers(E);
oscar: tamagawa_numbers(E)
Torsion order :
# E ( Q ) t o r \#E(\Q)_{\mathrm{tor}} # E ( Q ) t o r = 2 2 2
sage: E.torsion_order()
gp: elltors(E)[1]
magma: Order(TorsionSubgroup(E));
oscar: prod(torsion_structure(E)[1])
Special value :
L ′ ( E , 1 ) L'(E,1) L ′ ( E , 1 ) ≈ 2.5315056350178932346983474172 2.5315056350178932346983474172 2 . 5 3 1 5 0 5 6 3 5 0 1 7 8 9 3 2 3 4 6 9 8 3 4 7 4 1 7 2
sage: r = E.rank();
E.lseries().dokchitser().derivative(1,r)/r.factorial()
gp: [r,L1r] = ellanalyticrank(E); L1r/r!
magma: Lr1 where r,Lr1 := AnalyticRank(E: Precision:=12);
Analytic order of Ш :
Шa n {}_{\mathrm{an}} a n
≈
1 1 1
(rounded )
sage: E.sha().an_numerical()
magma: MordellWeilShaInformation(E);
2.531505635 ≈ L ′ ( E , 1 ) = # Ш ( E / Q ) ⋅ Ω E ⋅ R e g ( E / Q ) ⋅ ∏ p c p # E ( Q ) t o r 2 ≈ 1 ⋅ 1.956087 ⋅ 0.647084 ⋅ 8 2 2 ≈ 2.531505635 \begin{aligned} 2.531505635 \approx L'(E,1) & = \frac{\# Ш(E/\Q)\cdot \Omega_E \cdot \mathrm{Reg}(E/\Q) \cdot \prod_p c_p}{\#E(\Q)_{\rm tor}^2} \\ & \approx \frac{1 \cdot 1.956087 \cdot 0.647084 \cdot 8}{2^2} \\ & \approx 2.531505635\end{aligned} 2 . 5 3 1 5 0 5 6 3 5 ≈ L ′ ( E , 1 ) = # E ( Q ) t o r 2 # Ш ( E / Q ) ⋅ Ω E ⋅ R e g ( E / Q ) ⋅ ∏ p c p ≈ 2 2 1 ⋅ 1 . 9 5 6 0 8 7 ⋅ 0 . 6 4 7 0 8 4 ⋅ 8 ≈ 2 . 5 3 1 5 0 5 6 3 5
sage: # self-contained SageMath code snippet for the BSD formula (checks rank, computes analytic sha)
E = EllipticCurve([0, -1, 0, 9, -9]); r = E.rank(); ar = E.analytic_rank(); assert r == ar;
Lr1 = E.lseries().dokchitser().derivative(1,r)/r.factorial(); sha = E.sha().an_numerical();
omega = E.period_lattice().omega(); reg = E.regulator(); tam = E.tamagawa_product(); tor = E.torsion_order();
assert r == ar; print("analytic sha: " + str(RR(Lr1) * tor^2 / (omega * reg * tam)))
magma: /* self-contained Magma code snippet for the BSD formula (checks rank, computes analytic sha) */
E := EllipticCurve([0, -1, 0, 9, -9]); r := Rank(E); ar,Lr1 := AnalyticRank(E: Precision := 12); assert r eq ar;
sha := MordellWeilShaInformation(E); omega := RealPeriod(E) * (Discriminant(E) gt 0 select 2 else 1);
reg := Regulator(E); tam := &*TamagawaNumbers(E); tor := #TorsionSubgroup(E);
assert r eq ar; print "analytic sha:", Lr1 * tor^2 / (omega * reg * tam);
Modular form
1920.2.a.e
q − q 3 − q 5 + 2 q 7 + q 9 − 2 q 11 − 2 q 13 + q 15 − 2 q 17 + 2 q 19 + O ( q 20 ) q - q^{3} - q^{5} + 2 q^{7} + q^{9} - 2 q^{11} - 2 q^{13} + q^{15} - 2 q^{17} + 2 q^{19} + O(q^{20}) q − q 3 − q 5 + 2 q 7 + q 9 − 2 q 1 1 − 2 q 1 3 + q 1 5 − 2 q 1 7 + 2 q 1 9 + O ( q 2 0 )
sage: E.q_eigenform(20)
gp: \\ actual modular form, use for small N
[mf,F] = mffromell(E)
Ser(mfcoefs(mf,20),q)
\\ or just the series
Ser(ellan(E,20),q)*q
magma: ModularForm(E);
For more coefficients, see the Downloads section to the right.
This elliptic curve is not semistable .
There
are 3 primes p p p
of bad reduction :
sage: E.local_data()
gp: ellglobalred(E)[5]
magma: [LocalInformation(E,p) : p in BadPrimes(E)];
oscar: [(p,tamagawa_number(E,p), kodaira_symbol(E,p), reduction_type(E,p)) for p in bad_primes(E)]
The ℓ \ell ℓ -adic Galois representation has maximal image
for all primes ℓ \ell ℓ except those listed in the table below.
sage: rho = E.galois_representation(); [rho.image_type(p) for p in rho.non_surjective()]
magma: [GaloisRepresentation(E,p): p in PrimesUpTo(20)];
sage: gens = [[181, 6, 0, 1], [211, 4, 167, 9], [5, 8, 48, 77], [233, 8, 232, 9], [1, 0, 8, 1], [161, 8, 82, 17], [3, 8, 10, 27], [97, 6, 0, 1], [1, 8, 0, 1]]
GL(2,Integers(240)).subgroup(gens)
magma: Gens := [[181, 6, 0, 1], [211, 4, 167, 9], [5, 8, 48, 77], [233, 8, 232, 9], [1, 0, 8, 1], [161, 8, 82, 17], [3, 8, 10, 27], [97, 6, 0, 1], [1, 8, 0, 1]];
sub<GL(2,Integers(240))|Gens>;
The image H : = ρ E ( Gal ( Q ‾ / Q ) ) H:=\rho_E(\Gal(\overline{\Q}/\Q)) H : = ρ E ( G a l ( Q / Q ) ) of the adelic Galois representation has
level 240 = 2 4 ⋅ 3 ⋅ 5 240 = 2^{4} \cdot 3 \cdot 5 2 4 0 = 2 4 ⋅ 3 ⋅ 5 , index 48 48 4 8 , genus 0 0 0 , and generators
( 181 6 0 1 ) , ( 211 4 167 9 ) , ( 5 8 48 77 ) , ( 233 8 232 9 ) , ( 1 0 8 1 ) , ( 161 8 82 17 ) , ( 3 8 10 27 ) , ( 97 6 0 1 ) , ( 1 8 0 1 ) \left(\begin{array}{rr}
181 & 6 \\
0 & 1
\end{array}\right),\left(\begin{array}{rr}
211 & 4 \\
167 & 9
\end{array}\right),\left(\begin{array}{rr}
5 & 8 \\
48 & 77
\end{array}\right),\left(\begin{array}{rr}
233 & 8 \\
232 & 9
\end{array}\right),\left(\begin{array}{rr}
1 & 0 \\
8 & 1
\end{array}\right),\left(\begin{array}{rr}
161 & 8 \\
82 & 17
\end{array}\right),\left(\begin{array}{rr}
3 & 8 \\
10 & 27
\end{array}\right),\left(\begin{array}{rr}
97 & 6 \\
0 & 1
\end{array}\right),\left(\begin{array}{rr}
1 & 8 \\
0 & 1
\end{array}\right) ( 1 8 1 0 6 1 ) , ( 2 1 1 1 6 7 4 9 ) , ( 5 4 8 8 7 7 ) , ( 2 3 3 2 3 2 8 9 ) , ( 1 8 0 1 ) , ( 1 6 1 8 2 8 1 7 ) , ( 3 1 0 8 2 7 ) , ( 9 7 0 6 1 ) , ( 1 0 8 1 ) .
The torsion field K : = Q ( E [ 240 ] ) K:=\Q(E[240]) K : = Q ( E [ 2 4 0 ] ) is a degree-11796480 11796480 1 1 7 9 6 4 8 0 Galois extension of Q \Q Q with Gal ( K / Q ) \Gal(K/\Q) G a l ( K / Q ) isomorphic to the projection of H H H to GL 2 ( Z / 240 Z ) \GL_2(\Z/240\Z) GL 2 ( Z / 2 4 0 Z ) .
The table below list all primes ℓ \ell ℓ for which the Serre invariants associated to the mod-ℓ \ell ℓ Galois representation are exceptional.
ℓ \ell ℓ
Reduction type
Serre weight
Serre conductor
2 2 2
additive
2 2 2
1 1 1
3 3 3
nonsplit multiplicative
4 4 4
640 = 2 7 ⋅ 5 640 = 2^{7} \cdot 5 6 4 0 = 2 7 ⋅ 5
5 5 5
nonsplit multiplicative
6 6 6
384 = 2 7 ⋅ 3 384 = 2^{7} \cdot 3 3 8 4 = 2 7 ⋅ 3
gp: ellisomat(E)
This curve has non-trivial cyclic isogenies of degree d d d for d = d= d =
2.
Its isogeny class 1920.e
consists of 2 curves linked by isogenies of
degree 2.
This elliptic curve is its own minimal quadratic twist .
The number fields K K K of degree less than 24 such that
E ( K ) t o r s E(K)_{\rm tors} E ( K ) t o r s is strictly larger than E ( Q ) t o r s E(\Q)_{\rm tors} E ( Q ) t o r s
≅ Z / 2 Z \cong \Z/{2}\Z ≅ Z / 2 Z
are as follows:
[ K : Q ] [K:\Q] [ K : Q ]
K K K
E ( K ) t o r s E(K)_{\rm tors} E ( K ) t o r s
Base change curve
2 2 2
Q ( − 1 ) \Q(\sqrt{-1}) Q ( − 1 )
Z / 2 Z ⊕ Z / 2 Z \Z/2\Z \oplus \Z/2\Z Z / 2 Z ⊕ Z / 2 Z
not in database
4 4 4
4.2.25600.1
Z / 4 Z \Z/4\Z Z / 4 Z
not in database
8 8 8
8.0.530841600.6
Z / 2 Z ⊕ Z / 4 Z \Z/2\Z \oplus \Z/4\Z Z / 2 Z ⊕ Z / 4 Z
not in database
8 8 8
8.0.2621440000.10
Z / 2 Z ⊕ Z / 4 Z \Z/2\Z \oplus \Z/4\Z Z / 2 Z ⊕ Z / 4 Z
not in database
8 8 8
8.2.464380231680000.46
Z / 6 Z \Z/6\Z Z / 6 Z
not in database
16 16 1 6
deg 16
Z / 4 Z ⊕ Z / 4 Z \Z/4\Z \oplus \Z/4\Z Z / 4 Z ⊕ Z / 4 Z
not in database
16 16 1 6
deg 16
Z / 8 Z \Z/8\Z Z / 8 Z
not in database
16 16 1 6
deg 16
Z / 2 Z ⊕ Z / 6 Z \Z/2\Z \oplus \Z/6\Z Z / 2 Z ⊕ Z / 6 Z
not in database
We only show fields where the torsion growth is primitive .
For fields not in the database, click on the degree shown to reveal the defining polynomial.
An entry - indicates that the invariants are not computed because the reduction is additive.
p p p -adic regulators
Note: p p p -adic regulator data only exists for primes p ≥ 5 p\ge 5 p ≥ 5 of good ordinary
reduction.
Choose a prime...
7
11
13
17
19
23
29
31
37
41
43
47
53
59
61
67
71
73
79
83
89
97