Minimal Weierstrass equation
Minimal Weierstrass equation
Simplified equation
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\(y^2+xy+y=x^3-2001x+34273\)
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(homogenize, simplify) |
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\(y^2z+xyz+yz^2=x^3-2001xz^2+34273z^3\)
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(dehomogenize, simplify) |
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\(y^2=x^3-2592675x+1606830750\)
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(homogenize, minimize) |
Mordell-Weil group structure
\(\Z/{2}\Z\)
Torsion generators
\( \left(\frac{103}{4}, -\frac{107}{8}\right) \)
Integral points
None
Invariants
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sage: E.conductor().factor()
gp: ellglobalred(E)[1]
magma: Conductor(E);
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| Conductor: | \( 75 \) | = | $3 \cdot 5^{2}$ |
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sage: E.discriminant().factor()
gp: E.disc
magma: Discriminant(E);
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| Discriminant: | $234375 $ | = | $3 \cdot 5^{7} $ |
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sage: E.j_invariant().factor()
gp: E.j
magma: jInvariant(E);
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| j-invariant: | \( \frac{56667352321}{15} \) | = | $3^{-1} \cdot 5^{-1} \cdot 23^{3} \cdot 167^{3}$ |
| Endomorphism ring: | $\Z$ | ||
| Geometric endomorphism ring: | \(\Z\) | (no potential complex multiplication) | |
| Sato-Tate group: | $\mathrm{SU}(2)$ | ||
| Faltings height: | $0.40244138413420639985678316945\dots$ | ||
| Stable Faltings height: | $-0.40227757208284378744359649716\dots$ | ||
BSD invariants
sage: E.rank()
magma: Rank(E);
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| Analytic rank: | $0$ | ||
sage: E.regulator()
magma: Regulator(E);
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| Regulator: | $1$ | ||
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);
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| Real period: | $2.5054748897189709891486322013\dots$ | ||
sage: E.tamagawa_numbers()
gp: gr=ellglobalred(E); [[gr[4][i,1],gr[5][i][4]] | i<-[1..#gr[4][,1]]]
magma: TamagawaNumbers(E);
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| Tamagawa product: | $ 2 $ = $ 1\cdot2 $ | ||
sage: E.torsion_order()
gp: elltors(E)[1]
magma: Order(TorsionSubgroup(E));
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| Torsion order: | $2$ | ||
sage: E.sha().an_numerical()
magma: MordellWeilShaInformation(E);
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| Analytic order of Ш: | $1$ (exact) | ||
sage: r = E.rank();
gp: ar = ellanalyticrank(E);
magma: Lr1 where r,Lr1 := AnalyticRank(E: Precision:=12);
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| Special value: | $ L(E,1) $ ≈ $ 1.2527374448594854945743161006 $ | ||
Modular invariants
For more coefficients, see the Downloads section to the right.
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sage: E.modular_degree()
magma: ModularDegree(E);
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| Modular degree: | 24 | ||
| $ \Gamma_0(N) $-optimal: | no | ||
| Manin constant: | 1 | ||
Local data
This elliptic curve is not semistable. There are 2 primes of bad reduction:
| prime | Tamagawa number | Kodaira symbol | Reduction type | Root number | ord($N$) | ord($\Delta$) | ord$(j)_{-}$ |
|---|---|---|---|---|---|---|---|
| $3$ | $1$ | $I_{1}$ | Split multiplicative | -1 | 1 | 1 | 1 |
| $5$ | $2$ | $I_{1}^{*}$ | Additive | 1 | 2 | 7 | 1 |
Galois representations
The $\ell$-adic Galois representation has maximal image for all primes $\ell$ except those listed in the table below.
| prime $\ell$ | mod-$\ell$ image | $\ell$-adic image |
|---|---|---|
| $2$ | 2B | 32.96.0.29 |
$p$-adic regulators
All $p$-adic regulators are identically $1$ since the rank is $0$.
Iwasawa invariants
| $p$ | 2 | 3 | 5 |
|---|---|---|---|
| Reduction type | ord | split | add |
| $\lambda$-invariant(s) | 1 | 1 | - |
| $\mu$-invariant(s) | 0 | 0 | - |
All Iwasawa $\lambda$ and $\mu$-invariants for primes $p\ge 3$ of good reduction are zero.
An entry - indicates that the invariants are not computed because the reduction is additive.
Isogenies
This curve has non-trivial cyclic isogenies of degree $d$ for $d=$
2, 4, 8 and 16.
Its isogeny class 75.b
consists of 8 curves linked by isogenies of
degrees dividing 16.
Growth of torsion in number fields
The number fields $K$ of degree less than 24 such that $E(K)_{\rm tors}$ is strictly larger than $E(\Q)_{\rm tors}$ $\cong \Z/{2}\Z$ are as follows:
| $[K:\Q]$ | $K$ | $E(K)_{\rm tors}$ | Base change curve |
|---|---|---|---|
| $2$ | \(\Q(\sqrt{15}) \) | \(\Z/2\Z \oplus \Z/2\Z\) | 2.2.60.1-15.1-d8 |
| $2$ | \(\Q(\sqrt{5}) \) | \(\Z/8\Z\) | 2.2.5.1-45.1-a8 |
| $2$ | \(\Q(\sqrt{3}) \) | \(\Z/4\Z\) | 2.2.12.1-1875.1-d7 |
| $4$ | \(\Q(\sqrt{3}, \sqrt{5})\) | \(\Z/2\Z \oplus \Z/8\Z\) | 4.4.3600.1-225.1-e7 |
| $4$ | \(\Q(\zeta_{20})^+\) | \(\Z/16\Z\) | 4.4.2000.1-405.1-c6 |
| $4$ | \(\Q(\zeta_{15})^+\) | \(\Z/16\Z\) | 4.4.1125.1-45.1-b6 |
| $8$ | 8.0.746496000000.46 | \(\Z/2\Z \oplus \Z/4\Z\) | Not in database |
| $8$ | 8.0.746496000000.47 | \(\Z/8\Z\) | Not in database |
| $8$ | \(\Q(\zeta_{60})^+\) | \(\Z/2\Z \oplus \Z/16\Z\) | Not in database |
| $8$ | 8.8.14580000000.1 | \(\Z/32\Z\) | Not in database |
| $8$ | 8.2.2767921875.1 | \(\Z/6\Z\) | Not in database |
| $16$ | Deg 16 | \(\Z/4\Z \oplus \Z/8\Z\) | Not in database |
| $16$ | 16.0.891610044825600000000.10 | \(\Z/2\Z \oplus \Z/16\Z\) | Not in database |
| $16$ | Deg 16 | \(\Z/32\Z\) | Not in database |
| $16$ | 16.16.54419558400000000000000.1 | \(\Z/2\Z \oplus \Z/32\Z\) | Not in database |
| $16$ | Deg 16 | \(\Z/2\Z \oplus \Z/6\Z\) | Not in database |
| $16$ | Deg 16 | \(\Z/24\Z\) | Not in database |
| $16$ | Deg 16 | \(\Z/12\Z\) | 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.