Base field \(\Q(\sqrt{5}, \sqrt{21})\)
Generator \(a\), with minimal polynomial \( x^{4} - 13 x^{2} + 16 \); class number \(1\).
sage: R.<x> = PolynomialRing(QQ); K.<a> = NumberField(R([16, 0, -13, 0, 1]))
gp: K = nfinit(Polrev([16, 0, -13, 0, 1]));
magma: R<x> := PolynomialRing(Rationals()); K<a> := NumberField(R![16, 0, -13, 0, 1]);
Weierstrass equation
sage: E = EllipticCurve([K([1/2,17/8,0,-1/8]),K([-3,1/2,1/2,0]),K([-3/2,13/8,1/2,-1/8]),K([-1599,-1327,137,114]),K([6413/2,22183/8,-559/2,-1915/8])])
gp: E = ellinit([Polrev([1/2,17/8,0,-1/8]),Polrev([-3,1/2,1/2,0]),Polrev([-3/2,13/8,1/2,-1/8]),Polrev([-1599,-1327,137,114]),Polrev([6413/2,22183/8,-559/2,-1915/8])], K);
magma: E := EllipticCurve([K![1/2,17/8,0,-1/8],K![-3,1/2,1/2,0],K![-3/2,13/8,1/2,-1/8],K![-1599,-1327,137,114],K![6413/2,22183/8,-559/2,-1915/8]]);
This is a global minimal model.
sage: E.is_global_minimal_model()
Invariants
Conductor: | \((-1/8a^3+1/2a^2+5/8a-7/2)\) | = | \((1/8a^3+1/2a^2+3/8a-1/2)\cdot(1/4a^3+1/2a^2-11/4a-6)\) |
sage: E.conductor()
gp: ellglobalred(E)[1]
magma: Conductor(E);
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Conductor norm: | \( 20 \) | = | \(4\cdot5\) |
sage: E.conductor().norm()
gp: idealnorm(ellglobalred(E)[1])
magma: Norm(Conductor(E));
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Discriminant: | \((1/4a^3-2a^2-5/4a+6)\) | = | \((1/8a^3+1/2a^2+3/8a-1/2)\cdot(1/4a^3+1/2a^2-11/4a-6)^{4}\) |
sage: E.discriminant()
gp: E.disc
magma: Discriminant(E);
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Discriminant norm: | \( 2500 \) | = | \(4\cdot5^{4}\) |
sage: E.discriminant().norm()
gp: norm(E.disc)
magma: Norm(Discriminant(E));
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j-invariant: | \( \frac{1706787717742615889506073}{200} a^{3} + \frac{2909494317952668385276541}{100} a^{2} - \frac{2349435309500436933786543}{200} a - \frac{400499055174224721007173}{10} \) | ||
sage: E.j_invariant()
gp: E.j
magma: jInvariant(E);
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Endomorphism ring: | \(\Z\) | ||
Geometric endomorphism ring: | \(\Z\) | (no potential complex multiplication) | |
sage: E.has_cm(), E.cm_discriminant()
magma: HasComplexMultiplication(E);
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Sato-Tate group: | $\mathrm{SU}(2)$ |
Mordell-Weil group
Rank: | \(1\) |
Generator | $\left(-\frac{79}{32} a^{3} - \frac{37}{8} a^{2} + \frac{947}{32} a + \frac{521}{8} : \frac{1333}{32} a^{3} + \frac{131}{4} a^{2} - \frac{15201}{32} a - \frac{1479}{4} : 1\right)$ |
Height | \(4.0451606213247928586260012143926262297\) |
Torsion structure: | \(\Z/2\Z\) |
sage: T = E.torsion_subgroup(); T.invariants()
gp: T = elltors(E); T[2]
magma: T,piT := TorsionSubgroup(E); Invariants(T);
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Torsion generator: | $\left(\frac{65}{32} a^{3} + \frac{5}{2} a^{2} - \frac{769}{32} a - \frac{259}{8} : -\frac{99}{32} a^{3} - \frac{7}{2} a^{2} + \frac{1187}{32} a + 41 : 1\right)$ |
sage: T.gens()
gp: T[3]
magma: [piT(P) : P in Generators(T)];
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BSD invariants
Analytic rank: | \( 1 \) | ||
sage: E.rank()
magma: Rank(E);
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Mordell-Weil rank: | \(1\) | ||
Regulator: | \( 4.0451606213247928586260012143926262297 \) | ||
Period: | \( 10.585860643248826299960442534841755676 \) | ||
Tamagawa product: | \( 2 \) = \(1\cdot2\) | ||
Torsion order: | \(2\) | ||
Leading coefficient: | \( 3.26259098033540 \) | ||
Analytic order of Ш: | \( 4 \) (rounded) |
Local data at primes of bad reduction
sage: E.local_data()
magma: LocalInformation(E);
prime | Norm | Tamagawa number | Kodaira symbol | Reduction type | Root number | ord(\(\mathfrak{N}\)) | ord(\(\mathfrak{D}\)) | ord\((j)_{-}\) |
---|---|---|---|---|---|---|---|---|
\((1/8a^3+1/2a^2+3/8a-1/2)\) | \(4\) | \(1\) | \(I_{1}\) | Split multiplicative | \(-1\) | \(1\) | \(1\) | \(1\) |
\((1/4a^3+1/2a^2-11/4a-6)\) | \(5\) | \(2\) | \(I_{4}\) | Non-split multiplicative | \(1\) | \(1\) | \(4\) | \(4\) |
Galois Representations
The mod \( p \) Galois Representation has maximal image for all primes \( p < 1000 \) except those listed.
prime | Image of Galois Representation |
---|---|
\(2\) | 2B |
Isogenies and isogeny class
This curve has non-trivial cyclic isogenies of degree \(d\) for \(d=\)
2 and 4.
Its isogeny class
20.2-b
consists of curves linked by isogenies of
degrees dividing 4.
Base change
This elliptic curve is not a \(\Q\)-curve.
It is not the base change of an elliptic curve defined over any subfield.