neoVULCAN ========= **neoVULCAN** is a one-dimensional photochemical kinetics code for planetary and exoplanetary atmospheres. It is a refactored, JAX-accelerated descendant of the original VULCAN code [Tsai2017]_, [Tsai2021]_ (upstream repository: `shami-EEG/VULCAN `_), designed to integrate the stiff transport–reaction system .. math:: \frac{\partial n_i}{\partial t} = \mathcal{P}_i - \mathcal{L}_i - \frac{\partial \phi_i}{\partial z} forward in time until a numerical steady state is reached. Compared to the original VULCAN, neoVULCAN * uses **JAX** for automatic differentiation of the chemistry Jacobian and for vectorised rate evaluations, * exposes a **library API** (:class:`vulcan_api.VulcanChemistry`) for embedding in three-dimensional general-circulation models, * supports both the second-order Rosenbrock (``Ros2``) and a third-order, L-stable Rosenbrock–Wanner (``Rodas3``) integrator, * implements photochemistry, condensation with particle settling, advection, molecular diffusion with thermal-diffusion drift, and a flexible C–H–N–O–S reaction network. This documentation collects the mathematical background, the numerical schemes used inside neoVULCAN, a complete reference for the configuration file, and a tour of the code architecture. .. toctree:: :maxdepth: 2 :caption: Getting started installation quickstart running .. toctree:: :maxdepth: 2 :caption: Theory math_background numerics .. toctree:: :maxdepth: 2 :caption: Reference config_reference code_architecture api .. toctree:: :maxdepth: 1 :caption: Appendix references Indices and tables ================== * :ref:`genindex` * :ref:`modindex` * :ref:`search`