aragog.jax
The aragog.jax package contains JAX-traceable replicas of the EOS, phase evaluator, and dSdt right-hand side. They are used to build an analytic Jacobian via jax.jacrev and feed it to SUNDIALS CVODE through the registered factory in aragog.solver.cvode_jax.
This module is loaded only when solver.use_jax_jacobian = true (the production default). The numpy path in aragog.solver.entropy_state remains the reference implementation and is exercised by the standalone tests; both must agree to numerical precision (see first-principles verification).
For when and why to opt into the JAX path, see CVODE and JAX-derived Jacobians.
| Submodule | Role |
|---|---|
aragog.jax.eos |
EntropyEOS_JAX, the JAX-traceable P-S table loader, and PhaseState, the per-cell phase cache. Mirrors the public surface of aragog.eos.EntropyEOS. |
aragog.jax.phase |
PhaseParams, MeshArrays, PhaseProperties, FluxOutput, compute_fluxes, compute_mlt, evaluate_phase. SPIDER-parity two-stage blend, mixing-length convection, and pure-functional flux assembly. |
aragog.jax.solver |
BoundaryParams, SolveResult. The standalone JAX solve path used by the verification suite; in production the JAX path supplies only the Jacobian and CVODE drives the integration. |
aragog.jax.nondim |
NonDimScales. Reference scales used to non-dimensionalise state and time before passing them to the integrator. |
aragog.jax.eos
JAX-traceable P-S equation of state. Loads SPIDER-format two-phase tables and provides temperature, density, melt_fraction, and the latent-heat / phase-boundary derivatives via jax.jit-compatible bilinear interpolation.
eos
JAX-based entropy EOS layer for PALEOS P-S tables.
Drop-in replacement for aragog.eos.entropy.EntropyEOS using JAX arrays and jax.scipy.interpolate.RegularGridInterpolator. All methods are JIT-compilable and differentiable via jax.grad.
Table loading uses the existing numpy loader (disk I/O is not JIT-compiled). The loaded grids are converted to JAX arrays and stored as equinox Module fields so the entire EOS object is a valid JAX pytree.
Dependencies: jax, equinox (both already in PROTEUS ecosystem via atmodeller).
EntropyEOS_JAX(eos_dir)
Bases: Module
JAX-based entropy EOS from PALEOS P-S tables.
Drop-in replacement for aragog.eos.entropy.EntropyEOS with all
lookups JIT-compilable and differentiable. Constructed from the same
SPIDER-format table files.
Parameters:
| Name | Type | Description | Default |
|---|---|---|---|
eos_dir
|
Path or str
|
Directory containing the SPIDER-format P-S table files. |
required |
Notes
A non-finite input entropy (NaN, +inf or -inf) propagates as NaN
through every entropy-derived output of compute_phase_state and
the property methods below, keyed on the input entropy via
jnp.isfinite(S), instead of raising or clamping to a finite
value. latent_heat takes only pressure and stays finite. This
keeps the lookups pure and safe under jax.jit and jax.vmap,
where a Python raise is not possible. A finite entropy outside the
table domain still clamps to the table edge; only non-finite entropy
becomes NaN.
The numpy reference EOS handles non-finite entropy at two different
entry points. The direct property lookups in aragog.eos.entropy
(EntropyEOS.temperature and the others) never raise: a NaN
entropy returns NaN and +-inf or a finite out-of-domain entropy
clamps to the table edge, each with a log warning
(strict_range defaults to False). The phase evaluator
EntropyPhaseEvaluator._update_eos in aragog.eos.entropy_phase
has an eager NaN backstop that raises RuntimeError when a lookup
yields NaN, so a NaN entropy raises there while +-inf and finite
out-of-domain entropy clamp to the edge. The JAX path uses NaN as the
single sentinel across both, because it cannot raise under a
transform.
Source code in src/aragog/jax/eos.py
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compute_phase_state(P, S, k_solid, k_liquid, matprop_smooth_width=0.0)
Single-pass SPIDER-parity phase evaluation (cp_blend='latent').
Bit-for-bit mirror of numpy EntropyPhaseEvaluator._update_eos
with cp_blend='latent'. All properties share the same
intermediates, and each is the smth-blend
smth * mixed + (1 - smth) * single matching SPIDER
combine_matprop (eos_composite.c:278-285).
Parameters:
| Name | Type | Description | Default |
|---|---|---|---|
P
|
Array
|
Pressure [Pa] and entropy [J/kg/K], same shape. |
required |
S
|
Array
|
Pressure [Pa] and entropy [J/kg/K], same shape. |
required |
k_solid
|
float
|
Single-phase thermal conductivities [W/m/K]. |
required |
k_liquid
|
float
|
Single-phase thermal conductivities [W/m/K]. |
required |
matprop_smooth_width
|
float
|
SPIDER's |
0.0
|
Returns:
| Type | Description |
|---|---|
PhaseState
|
All blended properties and shared intermediates. |
Source code in src/aragog/jax/eos.py
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dTdPs(P, S)
Adiabatic temperature gradient dT/dP|_S (P, S) [K/Pa].
Source code in src/aragog/jax/eos.py
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density(P, S)
Density rho(P, S) [kg/m^3], matching numpy EntropyEOS.density.
- Mushy zone (0 < phi < 1): harmonic mean of end-member
densities evaluated at phase-boundary entropies (Lever Rule,
SPIDER
eos_composite.c:236-237). - Pure phase (phi = 0 or phi = 1): evaluate the active single-
phase table at the actual S (clamped by the table itself).
SPIDER
combine_matprop(smth=0, mixed, single)selects the single-phase branch in this regime. Using the harmonic-mean form unconditionally biases the fully-molten density relative to the numpy EntropyEOS.
Source code in src/aragog/jax/eos.py
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entropy_at_temperature(P, T)
Entropy [J/kg/K] at scalar pressure P where temperature(P, S) = T.
A fixed 60-step bisection over the tables' entropy range (its edge where T lies
beyond the range), plus a term that is zero in value and carries the implicit
derivatives dS/dT = 1 / (dT/dS) and dS/dP = -(dT/dP) / (dT/dS), which are zero
where dT/dS is below 1e-12 |T|; NaN for a NaN P or T.
Source code in src/aragog/jax/eos.py
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heat_capacity(P, S)
Specific heat capacity Cp(P, S) [J/kg/K].
Source code in src/aragog/jax/eos.py
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latent_heat(P)
Latent heat L(P) = T_fus x (S_liq - S_sol) [J/kg].
Source code in src/aragog/jax/eos.py
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liquidus_entropy(P)
Liquidus entropy S_liq(P) [J/kg/K].
Source code in src/aragog/jax/eos.py
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liquidus_entropy_dP(P)
dS_liq/dP at the given pressure(s), in J/(kg·K·Pa).
Source code in src/aragog/jax/eos.py
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material_expansivity(P, S)
Thermal expansivity [1/K] of the phases, without the phase-change term.
The volume-weighted blend rho sum_i x_i alpha_i / rho_i of each phase's
rho cp |dT/dP|_S / T at its own entropy, with x_i the Lever-rule mass fractions
and rho the harmonic mixture density of density.
Source code in src/aragog/jax/eos.py
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melt_fraction(P, S)
Melt fraction phi from position between solidus and liquidus.
phi = 0 for S <= S_sol, phi = 1 for S >= S_liq, linear between.
Source code in src/aragog/jax/eos.py
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solidus_entropy(P)
Solidus entropy S_sol(P) [J/kg/K].
Source code in src/aragog/jax/eos.py
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solidus_entropy_dP(P)
dS_sol/dP at the given pressure(s), in J/(kg·K·Pa).
Needed by the SPIDER-parity bracket Jmix in
aragog.jax.phase.compute_fluxes. Mirrors numpy
EntropyEOS.solidus_entropy_dP (entropy.py:377-388).
Source code in src/aragog/jax/eos.py
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temperature(P, S)
Temperature T(P, S) [K].
Source code in src/aragog/jax/eos.py
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thermal_expansivity(P, S)
Thermal expansivity alpha(P, S) [1/K].
Derived: alpha = rho * Cp * |dTdPs| / T.
Source code in src/aragog/jax/eos.py
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PhaseState
Bases: NamedTuple
Material properties at (P, S) following SPIDER eos_composite.c convention.
All scalar properties (T, rho, Cp, alpha, dTdPs, k) result from a
smth-blend between two-phase mixed values (analytical formulas at
the phase boundaries) and single table values (looked up at the
actual P and at S_sol or S_liq when mushy). This matches numpy
EntropyPhaseEvaluator._update_eos step-for-step.
aragog.jax.phase
Phase-aware property evaluation and flux assembly. evaluate_phase performs the SPIDER two-stage tanh blend at one cell; compute_fluxes is the pure-functional RHS that returns heat flux at basic nodes, internal heating at staggered nodes, eddy diffusivity, and capacitance.
phase
JAX phase evaluator and flux computation for the entropy solver.
Pure-functional replacements for entropy_phase.py (phase properties)
and entropy_state.py (MLT convection, heat/mass fluxes). All functions
are JIT-compilable and differentiable.
The numpy versions mutate state arrays in-place. The JAX versions take arrays in and return NamedTuples out, with no side effects.
Dependencies: jax, equinox (already in PROTEUS ecosystem via atmodeller).
PhaseParams(phi_rheo=0.4, phi_width=0.15, viscosity_solid=1e+21, viscosity_liquid=0.1, grain_size=0.001, k_solid=4.0, k_liquid=2.0, matprop_smooth_width=0.0, conduction=True, convection=True, grav_sep=False, mixing=False, eddy_diff_thermal=1.0, eddy_diff_chemical=1.0, kappah_floor=0.0, bottom_up_grav_sep=True, phase_smoothing='tanh', phase_smoothing_width=0.01, separation_viscosity=SEPARATION_VISCOSITY_DEFAULT, convective_threshold=CONVECTIVE_THRESHOLD_DEFAULT)
Bases: Module
Static parameters for phase evaluation and flux computation.
Constructed once from config, passed as args to JIT-compiled
functions. All fields are scalars or 1D JAX arrays.
Source code in src/aragog/jax/phase.py
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MeshArrays(d_dr_matrix, quantity_matrix, area, volume, radii_basic, mixing_length, mixing_length_sq, mixing_length_cu, radii_stag, P_stag, P_basic, gravity, dP_dr_basic=None, gravity_stag=None, top_limited=False, top_ratio=1.0, top_bounds=(-jnp.inf, jnp.inf))
Bases: Module
Static mesh geometry arrays, converted from numpy Mesh once.
All arrays are 1D JAX arrays. The transform matrices are 2D.
from P_basic and radii_basic via numpy gradient (matches
entropy_state._dP_dr_basic = np.gradient(P_basic, r_basic)).
Source code in src/aragog/jax/phase.py
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from_numpy_mesh(mesh)
staticmethod
Build from a numpy Aragog Mesh object.
Source code in src/aragog/jax/phase.py
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PhaseProperties
FluxOutput
compute_fluxes(S_stag, time, eos, params, mesh, heating_rate, S_basic_cmb_override=None, dSdr_cmb_override=None)
Compute all heat and mass fluxes from the entropy profile.
This is the physics kernel called by the ODE RHS. It is a pure function: no mutation, no side effects, fully JIT-compilable.
Parameters:
| Name | Type | Description | Default |
|---|---|---|---|
S_stag
|
Array
|
Entropy at staggered nodes [J/kg/K]. |
required |
time
|
float
|
Current time [yr] (used for radionuclide heating). |
required |
eos
|
EntropyEOS_JAX
|
JAX EOS tables. |
required |
params
|
PhaseParams
|
Static material parameters and transport flags. |
required |
mesh
|
MeshArrays
|
Mesh geometry and transform matrices. |
required |
heating_rate
|
Array
|
Internal heating rate at staggered nodes [W/kg] (radionuclide + tidal, pre-computed by caller). |
required |
S_basic_cmb_override
|
float or None
|
Optional override for the entropy at the CMB basic node (basic-node index 0). Used by the energy_balance and core_module core BCs, which reconstruct S_basic[0] from the state-tracked dSdr_cmb via S[0] + dSdr_cmb * (r_basic[0] - r_stag[0]). When None, the standard quantity_matrix mapping is used. |
None
|
dSdr_cmb_override
|
float or None
|
Optional override for the entropy gradient at the CMB basic node (dSdr[0]). Used by the energy_balance and core_module core BCs, where dSdr_cmb is a state-tracked variable. When None, the standard d_dr_matrix mapping is used. |
None
|
Returns:
| Type | Description |
|---|---|
FluxOutput
|
Heat flux, mass flux, eddy diffusivity, heating. |
Source code in src/aragog/jax/phase.py
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compute_mlt(dSdr, phase_basic, mesh, params)
Compute MLT eddy diffusivity from the entropy gradient.
Parameters:
| Name | Type | Description | Default |
|---|---|---|---|
dSdr
|
Array
|
Entropy gradient at basic nodes [J/kg/K/m]. |
required |
phase_basic
|
PhaseProperties
|
Material properties at basic nodes. |
required |
mesh
|
MeshArrays
|
Mesh geometry. |
required |
params
|
PhaseParams
|
Static parameters. |
required |
Returns:
| Name | Type | Description |
|---|---|---|
kappa_h |
Array
|
Thermal eddy diffusivity at basic nodes [m^2/s]. |
kappa_c |
Array
|
Chemical eddy diffusivity at basic nodes [m^2/s]. |
Source code in src/aragog/jax/phase.py
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evaluate_phase(eos, params, P, S)
Compute all material properties at (P, S) nodes.
Parameters:
| Name | Type | Description | Default |
|---|---|---|---|
eos
|
EntropyEOS_JAX
|
JAX EOS tables. |
required |
params
|
PhaseParams
|
Static material parameters. |
required |
P
|
Array
|
Pressure [Pa], 1D. |
required |
S
|
Array
|
Entropy [J/kg/K], 1D. |
required |
Returns:
| Type | Description |
|---|---|
PhaseProperties
|
All material properties at the given nodes. |
Source code in src/aragog/jax/phase.py
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aragog.jax.solver
Standalone JAX solve path used by the verification suite. The production path uses CVODE driven by aragog.solver.entropy_solver and only borrows the Jacobian from jax.jacrev; this module's solve_entropy is kept for parity tests and gradient-based sensitivity studies.
solver
JAX ODE solver for the entropy equation (research-only).
Direct-JAX integration of the entropy equation via diffrax Kvaerno5 (5th-order ESDIRK, A-L stable). The RHS applies boundary conditions, computes flux divergence, and adds internal heating, all in pure JAX.
Not production-ready: the diffrax ESDIRK solvers (kvaerno3, kvaerno5)
stall at the first crystallisation step on the cubic-Hermite J_grav
smoothing in coupled Earth-mantle runs. Kept for autodiff development. The
production JAX integration path is the CVODE Option-Z path in
aragog/solver/cvode_jax.py, selected by setting
EnergyParams.use_jax_jacobian = True (PROTEUS-side
backend="jax"), which uses CVODE for time stepping and JAX only
for the analytic Jacobian.
Dependencies: jax, equinox, diffrax, lineax (transitive via diffrax).
BoundaryParams(*, outer_bc_type, outer_bc_value, emissivity, T_eq, inner_bc_type, inner_bc_value, core_density, core_heat_capacity, tfac_core_avg, cmb_area=0.0, core_M=0.0, cmb_dr_cmb=0.0, param_utbl=False, param_utbl_const=0.0)
Bases: Module
Boundary condition configuration as a JAX pytree.
Surface BC types: 1 = grey-body (F = emissivity * sigma * (T^4 - T_eq^4)) 4 = prescribed flux (from atmosphere module)
CMB BC types:
0 = insulating (F = 0)
1 = core cooling (Bower+2018 Eq. 37)
2 = prescribed flux
3 = prescribed temperature (preserve conduction-derived flux)
5 = energy_balance (SPIDER bit-parity): F_cmb derived from
the boundary entropy gradient (state-tracked dSdr_cmb).
Used by dSdt_energy_balance.
All float fields are stored as JAX arrays (not Python floats) to avoid JIT recompilation when values change between coupling steps.
Energy-balance constants are optional (default 0); only used when
inner_bc_type == 5 via dSdt_energy_balance.
Source code in src/aragog/jax/solver.py
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SolveResult
aragog.jax.nondim
Reference scales used internally to non-dimensionalise the state vector and time before they enter the integrator. The triplet (state_scale, rhs_scale, t_ref) is built from EntropySolver._S_ref, _dSdr_ref, and _t_ref_yr; it is not user-configurable.
nondim
Nondimensional scaling spec shared by the numpy and JAX RHS paths.
Single source of truth for the (state_scale, rhs_scale, t_ref) triplet and the state offset that scales physical-units state into the BDF integrator's O(1) work space. Built once by the EntropySolver, consumed by both the scipy/CVODE wrapper (entropy_solver.py) and the JAX CVODE factory (cvode_jax.py).
Internal contract enforced by __post_init__:
rhs_scale = t_ref / state_scale (per component)
state_scale > 0, rhs_scale > 0, t_ref > 0
state_scale.shape == rhs_scale.shape
By construction, every NonDimScales instance enforces the internal
contract (rhs_scale = t_ref / state_scale, all positive, shapes
matching) inside its __post_init__ before any caller can use it. The
two callers that consume an instance --- the scipy/CVODE wrapper in
entropy_solver.py and the JAX CVODE factory in cvode_jax.py ---
therefore do NOT need to re-check those invariants on entry.
NonDimScales(state_scale, t_ref, rhs_scale=None, state_offset=None)
dataclass
Per-component nondim scales for the entropy solver state vector.
Parameters:
| Name | Type | Description | Default |
|---|---|---|---|
state_scale
|
(ndarray, shape(n))
|
Physical-units scale per state component:
|
required |
t_ref
|
float
|
Time scale: |
required |
rhs_scale
|
(ndarray, shape(n) or None)
|
Optional precomputed RHS scale |
None
|
state_offset
|
(ndarray, shape(n) or None)
|
Physical offset per state component, |
None
|
n
property
Number of state-vector components.