GPGI

A Generic Particle + Grid data Interface

This small Python library implements fundamental grid deposition algorithms to analyse (rectilinear) grid + particle datasets, with an emphasize on performance. Core algorithms are implemented as Cython extensions.

Table of Contents

• Installation
• Supported applications
  • Supported deposition methods
  • Supported geometries
• Time complexity
• Usage
  • Supplying arbitrary metadata
  • Boundary conditions
    • Builtin recipes
    • Define custom recipes
  • Weight fields (Depositing intensive quantities)
• Deposition algorithm

Installation

python -m pip install --upgrade pip
python -m pip install gpgi

Supported applications

A rectilinear grid is defined as 1D arrays representing cell left edges in each directions. Note that the last point of such an array is interpreted as the right edge of the rightmost cell, so for instance, a 1D grid containing 100 cells is defined by 101 edges.

Particles are defined as points that live within the grid's bounds.

Deposition is the action of going from particle description to a grid description of a field. It is useful to analyze, compare and combine simulation data that exists in a combination of the two formalisms. This process is not reversible as it degrades information.

For instance, here's a simple overlay of a particle set (red dots) against a background that represents the deposited particle count.

This example illustrates the simplest possible deposition method "Particle in Cell", in which each particle contributes only to the cell that contains it.

More refined methods are also available.

Supported deposition methods

Supported geometries

Time complexity

An important step in perfoming deposition is to associate particle indices to cell indices. This step is called "particle indexing". In directions where the grid is uniformly stepped (if any), indexing a particle is an O(1) operation. In the more general case, indexing is performed by bisection, which is a O(log(nx))) operation (where nx represents the number of cells in the direction of interest).

Usage

The API consists in a load function, which returns a Dataset object.

Load data

import numpy as np
import gpgi

nx = ny = 64
nparticles = 600_000

prng = np.random.RandomState(0)
ds = gpgi.load(
    geometry="cartesian",
    grid={
        "cell_edges": {
            "x": np.linspace(-1, 1, nx),
            "y": np.linspace(-1, 1, ny),
        },
    },
    particles={
        "coordinates": {
            "x": 2 * (prng.normal(0.5, 0.25, nparticles) % 1 - 0.5),
            "y": 2 * (prng.normal(0.5, 0.25, nparticles) % 1 - 0.5),
        },
        "fields": {
            "mass": np.ones(nparticles),
        },
    },
)

The Dataset object holds a grid and a particles attribute, which both hold a fields attribute for accessing their data. But more importantly, the Dataset has a deposit method to translate particle fields to the grid formalism.

Deposit Particle fields on the grid

particle_mass = ds.deposit("mass", method="nearest_grid_point")  # or "ngp" for shorts

Visualize In this example we'll use matplotlib for rendering, but note that matplotlib is not a dependency to gpgi

import matplotlib.pyplot as plt

fig, ax = plt.subplots()
ax.set(aspect=1, xlabel="x", ylabel="y")

im = ax.pcolormesh(
    "x",
    "y",
    particle_mass.T,
    data=ds.grid.cell_edges,
    cmap="viridis",
)
fig.colorbar(im, ax=ax)

The example script given here takes about a second (top to bottom).

Supplying arbitrary metadata

new in gpgi 0.4.0

Dataset objects have a special attribute metadata which is a dictionary with string keys. This attribute is meant to hold any special metadata that may be relevant for labelling or processing (e.g. simulation time, author, ...). Metadata can be supplied at load time as

ds = gpgi.load(
    geometry="cartesian",
    grid=...,
    particles=...,
    metadata={"simulation_time": 12.5, "author": "Clément Robert"}
)

Boundary conditions

new in gpgi 0.5.0

With CIC and TSC deposition, particles contribute to cells neighbouring the one that contains them. For particles that live in the outermost layer of the domain, this means some of their contribution is lost. This behaviour corresponds to the default 'open' boundary condition, but gpgi has builtin support for more conservative boundary conditions.

Boundary conditions can selected per field, per axis and per side. Builtin recipes all perform linear combinations of ghost layers (same-side and opposite side) and active domain layers (same-side and opposite side), and replace the same-side active layer with the result.

User-selected boundary conditions take the form of an optional argument to Dataset.deposit, as dictionnary with keys being axes names, and values being 2-tuples of boundary conditions names (for left and right side respectively). For instance, here's how one would require periodic boundary conditions on all axes:

ds.deposit(
    "mass",
    method="cic",
    boundaries={
        "x": ("periodic", "periodic"),
        "y": ("periodic", "periodic"),
    }
)

Unspecified axes will use the default 'open' boundary.

Builtin recipes

Define custom recipes

gpgi's boundary recipes can be customized. Let's illustrate this feature with a simple example. Say we want to fix the value of the deposited field in some outer layer. This is done by defining a new function on the user side:

def ones(
    same_side_active_layer,
    same_side_ghost_layer,
    opposite_side_active_layer,
    opposite_side_ghost_layer,
    weight_same_side_active_layer,
    weight_same_side_ghost_layer,
    weight_opposite_side_active_layer,
    weight_opposite_side_ghost_layer,
    side,
    metadata,
):
   return 1.0

where all first eight arguments are numpy.ndarray objects with the same shape (which includes ghost padding !), to which the return value must be broadcastable, side can only be either "left" or "right", and metadata is the special Dataset.metadata attribute. Not all arguments need be used in the body of the function, but this signature is required.

The method must then be registered as a boundary condition recipe as

ds.boundary_recipes.register("ones", ones)

where the associated key (here "ones") is arbitrary. The recipe can now be used exactly as builtin ones, and all of them can be mixed arbitrarily.

ds.deposit(
    "mass",
    method="cic",
    boundaries={
        "x": ("ones", "wall"),
        "y": ("periodic", "periodic"),
    }
)

Note that all first eight arguments in a boundary recipe function should represent an extensive physical quantity (as opposed to intensive). When depositing an intensive quantity u, a weight field w should be supplied (see next section), in which case, the first four arguments represent u*w and the following four represent w, so that u can still be obtained within the function as a ratio if needed.

Weight fields (Depositing intensive quantities)

new in gpgi 0.7.0

Fundamentally, deposition algorithms construct on-grid fields by performing summations. An implication is that the physical quantities being deposited are required to be extensive (like mass or momentum). Intensive quantities (like velocity or temperature) require additional operations, and necessitate the use of an additional weight field.

This section provides showcases their usage. For a detailled explanation of the deposition algorithm for intensive quantities, see Deposition algorithm.

In order to deposit an intensive field (e.g., vx), an additional weight_field argument must be provided as

ds.deposit(
    "vx",
    method="cic",
    boundaries={
        "y": ("periodic", "periodic"),
        "x": ("antisymmetric", "antisymmetric"),
    },
    weight_field="mass",
    weight_field_boundaries={
        "y": ("periodic", "periodic"),
        "x": ("open", "open"),
    },
)

Boundary recipes may be also associated to the weight field with the weight_field_boundaries argument. This arguments becomes required if boundaries and weight_field are both provided.

Call help(ds.deposit) for more detail.

Deposition algorithm

This section provides details on the general deposition algorithm, as implemented in gpgi.

Without loss of generality, we will illustrate how an intensive field (v) is deposited, since this case requires the most computational steps. As it happens, depositing an extensive field (w) separately is actually part of the algorithm.

Definitions

• v is an intensive field that we want to deposit on the grid
• w is an extensive field that will be used as weights
• u = v * w is an extensive equivalent to v (conceptually, if v is a velocity and w is a mass, u corresponds to a momentum)

u(i), v(i) and w(i) are defined for each particle i.

We note U(x), V(x) and W(x) the corresponding on-grid fields, where V(x) is the final output of the algorithm. These are defined at grid cell centers x, within the active domain.

Last, we note U'(x), V'(x) and W'(x) the raw deposited fields, meaning no special treatment is applied to the outermost layers (boundary conditions). These are defined at grid cell centers, including one ghost layer that will be used to apply boundary conditions.

Algorithm

1. W' and U' are computed as

W'(x) = Σ c(i,x) w(i)
U'(x) = Σ c(i,x) w(i) v(i)

where c(i,x) are geometric coefficients associated with the deposition method. Taking the nearest grid point (NGP) method for illustration, c(i,x) = 1 if particle i is contained in the cell whose center is x, and c(i,x) = 0 elsewhere.

2. boundary conditions are applied

W(x) = W_BCO(W', 1, metadata)
U(x) = U_BCO(U', W', metadata)

where W_BCO and U_BCO denote arbitrary boundary condition operators associated with W and U respectively, and which take 3 arguments, representing the field to be transformed, its associated weight field and a wildcard metadata argument which may contain any additional data relevant to the operator.

Note 1 is used a placeholder "weight" for W, for symmetry reasons: all boundary condition operators must expose a similar interface, as explained in Define custom recipes.

3. Finally, V(x) is obtained as

V(x) = (U/W)(x)