Invariants
| Base field: | $\F_{2}$ |
| Dimension: | $4$ |
| L-polynomial: | $( 1 - 3 x + 5 x^{2} - 6 x^{3} + 4 x^{4} )( 1 - x^{2} + 4 x^{4} )$ |
| $1 - 3 x + 4 x^{2} - 3 x^{3} + 3 x^{4} - 6 x^{5} + 16 x^{6} - 24 x^{7} + 16 x^{8}$ | |
| Frobenius angles: | $\pm0.123548644961$, $\pm0.209784688372$, $\pm0.456881978294$, $\pm0.790215311628$ |
| Angle rank: | $1$ (numerical) |
| Jacobians: | $0$ |
| Cyclic group of points: | no |
| Non-cyclic primes: | $2$ |
This isogeny class is not simple, primitive, ordinary, and not supersingular. It is principally polarizable.
Newton polygon
This isogeny class is ordinary.
| $p$-rank: | $4$ |
| Slopes: | $[0, 0, 0, 0, 1, 1, 1, 1]$ |
Point counts
Point counts of the abelian variety
| $r$ | $1$ | $2$ | $3$ | $4$ | $5$ |
|---|---|---|---|---|---|
| $A(\F_{q^r})$ | $4$ | $304$ | $5776$ | $98496$ | $926404$ |
Point counts of the (virtual) curve
| $r$ | $1$ | $2$ | $3$ | $4$ | $5$ | $6$ | $7$ | $8$ | $9$ | $10$ |
|---|---|---|---|---|---|---|---|---|---|---|
| $C(\F_{q^r})$ | $0$ | $4$ | $9$ | $24$ | $30$ | $109$ | $168$ | $240$ | $513$ | $964$ |
Jacobians and polarizations
This isogeny class is principally polarizable, but does not contain a Jacobian.
Decomposition and endomorphism algebra
All geometric endomorphisms are defined over $\F_{2^{6}}$.
Endomorphism algebra over $\F_{2}$| The isogeny class factors as 2.2.ad_f $\times$ 2.2.a_ab and its endomorphism algebra is a direct product of the endomorphism algebras for each isotypic factor. The endomorphism algebra for each factor is: |
| The base change of $A$ to $\F_{2^{6}}$ is 1.64.l 4 and its endomorphism algebra is $\mathrm{M}_{4}($\(\Q(\sqrt{-15}) \)$)$ |
- Endomorphism algebra over $\F_{2^{2}}$
The base change of $A$ to $\F_{2^{2}}$ is 1.4.ab 2 $\times$ 2.4.b_ad. The endomorphism algebra for each factor is: - 1.4.ab 2 : $\mathrm{M}_{2}($\(\Q(\sqrt{-15}) \)$)$
- 2.4.b_ad : \(\Q(\sqrt{-3}, \sqrt{5})\).
- Endomorphism algebra over $\F_{2^{3}}$
The base change of $A$ to $\F_{2^{3}}$ is 2.8.a_l 2 and its endomorphism algebra is $\mathrm{M}_{2}($\(\Q(\sqrt{-3}, \sqrt{5})\)$)$
Base change
This is a primitive isogeny class.