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+/*
+ * Copyright 2011-2021 Blender Foundation
+ *
+ * Licensed under the Apache License, Version 2.0 (the "License");
+ * you may not use this file except in compliance with the License.
+ * You may obtain a copy of the License at
+ *
+ * http://www.apache.org/licenses/LICENSE-2.0
+ *
+ * Unless required by applicable law or agreed to in writing, software
+ * distributed under the License is distributed on an "AS IS" BASIS,
+ * WITHOUT WARRANTIES OR CONDITIONS OF ANY KIND, either express or implied.
+ * See the License for the specific language governing permissions and
+ * limitations under the License.
+ */
+
+#include "kernel/camera/projection.h"
+
+#include "kernel/bvh/bvh.h"
+
+CCL_NAMESPACE_BEGIN
+
+/* Random walk subsurface scattering.
+ *
+ * "Practical and Controllable Subsurface Scattering for Production Path
+ * Tracing". Matt Jen-Yuan Chiang, Peter Kutz, Brent Burley. SIGGRAPH 2016. */
+
+/* Support for anisotropy from:
+ * "Path Traced Subsurface Scattering using Anisotropic Phase Functions
+ * and Non-Exponential Free Flights".
+ * Magnus Wrenninge, Ryusuke Villemin, Christophe Hery.
+ * https://graphics.pixar.com/library/PathTracedSubsurface/ */
+
+ccl_device void subsurface_random_walk_remap(const float albedo,
+ const float d,
+ float g,
+ ccl_private float *sigma_t,
+ ccl_private float *alpha)
+{
+ /* Compute attenuation and scattering coefficients from albedo. */
+ const float g2 = g * g;
+ const float g3 = g2 * g;
+ const float g4 = g3 * g;
+ const float g5 = g4 * g;
+ const float g6 = g5 * g;
+ const float g7 = g6 * g;
+
+ const float A = 1.8260523782f + -1.28451056436f * g + -1.79904629312f * g2 +
+ 9.19393289202f * g3 + -22.8215585862f * g4 + 32.0234874259f * g5 +
+ -23.6264803333f * g6 + 7.21067002658f * g7;
+ const float B = 4.98511194385f +
+ 0.127355959438f *
+ expf(31.1491581433f * g + -201.847017512f * g2 + 841.576016723f * g3 +
+ -2018.09288505f * g4 + 2731.71560286f * g5 + -1935.41424244f * g6 +
+ 559.009054474f * g7);
+ const float C = 1.09686102424f + -0.394704063468f * g + 1.05258115941f * g2 +
+ -8.83963712726f * g3 + 28.8643230661f * g4 + -46.8802913581f * g5 +
+ 38.5402837518f * g6 + -12.7181042538f * g7;
+ const float D = 0.496310210422f + 0.360146581622f * g + -2.15139309747f * g2 +
+ 17.8896899217f * g3 + -55.2984010333f * g4 + 82.065982243f * g5 +
+ -58.5106008578f * g6 + 15.8478295021f * g7;
+ const float E = 4.23190299701f +
+ 0.00310603949088f *
+ expf(76.7316253952f * g + -594.356773233f * g2 + 2448.8834203f * g3 +
+ -5576.68528998f * g4 + 7116.60171912f * g5 + -4763.54467887f * g6 +
+ 1303.5318055f * g7);
+ const float F = 2.40602999408f + -2.51814844609f * g + 9.18494908356f * g2 +
+ -79.2191708682f * g3 + 259.082868209f * g4 + -403.613804597f * g5 +
+ 302.85712436f * g6 + -87.4370473567f * g7;
+
+ const float blend = powf(albedo, 0.25f);
+
+ *alpha = (1.0f - blend) * A * powf(atanf(B * albedo), C) +
+ blend * D * powf(atanf(E * albedo), F);
+ *alpha = clamp(*alpha, 0.0f, 0.999999f); // because of numerical precision
+
+ float sigma_t_prime = 1.0f / fmaxf(d, 1e-16f);
+ *sigma_t = sigma_t_prime / (1.0f - g);
+}
+
+ccl_device void subsurface_random_walk_coefficients(const float3 albedo,
+ const float3 radius,
+ const float anisotropy,
+ ccl_private float3 *sigma_t,
+ ccl_private float3 *alpha,
+ ccl_private float3 *throughput)
+{
+ float sigma_t_x, sigma_t_y, sigma_t_z;
+ float alpha_x, alpha_y, alpha_z;
+
+ subsurface_random_walk_remap(albedo.x, radius.x, anisotropy, &sigma_t_x, &alpha_x);
+ subsurface_random_walk_remap(albedo.y, radius.y, anisotropy, &sigma_t_y, &alpha_y);
+ subsurface_random_walk_remap(albedo.z, radius.z, anisotropy, &sigma_t_z, &alpha_z);
+
+ /* Throughput already contains closure weight at this point, which includes the
+ * albedo, as well as closure mixing and Fresnel weights. Divide out the albedo
+ * which will be added through scattering. */
+ *throughput = safe_divide_color(*throughput, albedo);
+
+ /* With low albedo values (like 0.025) we get diffusion_length 1.0 and
+ * infinite phase functions. To avoid a sharp discontinuity as we go from
+ * such values to 0.0, increase alpha and reduce the throughput to compensate. */
+ const float min_alpha = 0.2f;
+ if (alpha_x < min_alpha) {
+ (*throughput).x *= alpha_x / min_alpha;
+ alpha_x = min_alpha;
+ }
+ if (alpha_y < min_alpha) {
+ (*throughput).y *= alpha_y / min_alpha;
+ alpha_y = min_alpha;
+ }
+ if (alpha_z < min_alpha) {
+ (*throughput).z *= alpha_z / min_alpha;
+ alpha_z = min_alpha;
+ }
+
+ *sigma_t = make_float3(sigma_t_x, sigma_t_y, sigma_t_z);
+ *alpha = make_float3(alpha_x, alpha_y, alpha_z);
+}
+
+/* References for Dwivedi sampling:
+ *
+ * [1] "A Zero-variance-based Sampling Scheme for Monte Carlo Subsurface Scattering"
+ * by Jaroslav Křivánek and Eugene d'Eon (SIGGRAPH 2014)
+ * https://cgg.mff.cuni.cz/~jaroslav/papers/2014-zerovar/
+ *
+ * [2] "Improving the Dwivedi Sampling Scheme"
+ * by Johannes Meng, Johannes Hanika, and Carsten Dachsbacher (EGSR 2016)
+ * https://cg.ivd.kit.edu/1951.php
+ *
+ * [3] "Zero-Variance Theory for Efficient Subsurface Scattering"
+ * by Eugene d'Eon and Jaroslav Křivánek (SIGGRAPH 2020)
+ * https://iliyan.com/publications/RenderingCourse2020
+ */
+
+ccl_device_forceinline float eval_phase_dwivedi(float v, float phase_log, float cos_theta)
+{
+ /* Eq. 9 from [2] using precomputed log((v + 1) / (v - 1)) */
+ return 1.0f / ((v - cos_theta) * phase_log);
+}
+
+ccl_device_forceinline float sample_phase_dwivedi(float v, float phase_log, float rand)
+{
+ /* Based on Eq. 10 from [2]: `v - (v + 1) * pow((v - 1) / (v + 1), rand)`
+ * Since we're already pre-computing `phase_log = log((v + 1) / (v - 1))` for the evaluation,
+ * we can implement the power function like this. */
+ return v - (v + 1.0f) * expf(-rand * phase_log);
+}
+
+ccl_device_forceinline float diffusion_length_dwivedi(float alpha)
+{
+ /* Eq. 67 from [3] */
+ return 1.0f / sqrtf(1.0f - powf(alpha, 2.44294f - 0.0215813f * alpha + 0.578637f / alpha));
+}
+
+ccl_device_forceinline float3 direction_from_cosine(float3 D, float cos_theta, float randv)
+{
+ float sin_theta = safe_sqrtf(1.0f - cos_theta * cos_theta);
+ float phi = M_2PI_F * randv;
+ float3 dir = make_float3(sin_theta * cosf(phi), sin_theta * sinf(phi), cos_theta);
+
+ float3 T, B;
+ make_orthonormals(D, &T, &B);
+ return dir.x * T + dir.y * B + dir.z * D;
+}
+
+ccl_device_forceinline float3 subsurface_random_walk_pdf(float3 sigma_t,
+ float t,
+ bool hit,
+ ccl_private float3 *transmittance)
+{
+ float3 T = volume_color_transmittance(sigma_t, t);
+ if (transmittance) {
+ *transmittance = T;
+ }
+ return hit ? T : sigma_t * T;
+}
+
+/* Define the below variable to get the similarity code active,
+ * and the value represents the cutoff level */
+#define SUBSURFACE_RANDOM_WALK_SIMILARITY_LEVEL 9
+
+ccl_device_inline bool subsurface_random_walk(KernelGlobals kg,
+ IntegratorState state,
+ RNGState rng_state,
+ ccl_private Ray &ray,
+ ccl_private LocalIntersection &ss_isect)
+{
+ float bssrdf_u, bssrdf_v;
+ path_state_rng_2D(kg, &rng_state, PRNG_BSDF_U, &bssrdf_u, &bssrdf_v);
+
+ const float3 P = INTEGRATOR_STATE(state, ray, P);
+ const float3 N = INTEGRATOR_STATE(state, ray, D);
+ const float ray_dP = INTEGRATOR_STATE(state, ray, dP);
+ const float time = INTEGRATOR_STATE(state, ray, time);
+ const float3 Ng = INTEGRATOR_STATE(state, subsurface, Ng);
+ const int object = INTEGRATOR_STATE(state, isect, object);
+
+ /* Sample diffuse surface scatter into the object. */
+ float3 D;
+ float pdf;
+ sample_cos_hemisphere(-N, bssrdf_u, bssrdf_v, &D, &pdf);
+ if (dot(-Ng, D) <= 0.0f) {
+ return false;
+ }
+
+ /* Setup ray. */
+ ray.P = ray_offset(P, -Ng);
+ ray.D = D;
+ ray.t = FLT_MAX;
+ ray.time = time;
+ ray.dP = ray_dP;
+ ray.dD = differential_zero_compact();
+
+#ifndef __KERNEL_OPTIX__
+ /* Compute or fetch object transforms. */
+ Transform ob_itfm ccl_optional_struct_init;
+ Transform ob_tfm = object_fetch_transform_motion_test(kg, object, time, &ob_itfm);
+#endif
+
+ /* Convert subsurface to volume coefficients.
+ * The single-scattering albedo is named alpha to avoid confusion with the surface albedo. */
+ const float3 albedo = INTEGRATOR_STATE(state, subsurface, albedo);
+ const float3 radius = INTEGRATOR_STATE(state, subsurface, radius);
+ const float anisotropy = INTEGRATOR_STATE(state, subsurface, anisotropy);
+
+ float3 sigma_t, alpha;
+ float3 throughput = INTEGRATOR_STATE_WRITE(state, path, throughput);
+ subsurface_random_walk_coefficients(albedo, radius, anisotropy, &sigma_t, &alpha, &throughput);
+ float3 sigma_s = sigma_t * alpha;
+
+ /* Theoretically it should be better to use the exact alpha for the channel we're sampling at
+ * each bounce, but in practice there doesn't seem to be a noticeable difference in exchange
+ * for making the code significantly more complex and slower (if direction sampling depends on
+ * the sampled channel, we need to compute its PDF per-channel and consider it for MIS later on).
+ *
+ * Since the strength of the guided sampling increases as alpha gets lower, using a value that
+ * is too low results in fireflies while one that's too high just gives a bit more noise.
+ * Therefore, the code here uses the highest of the three albedos to be safe. */
+ const float diffusion_length = diffusion_length_dwivedi(max3(alpha));
+
+ if (diffusion_length == 1.0f) {
+ /* With specific values of alpha the length might become 1, which in asymptotic makes phase to
+ * be infinite. After first bounce it will cause throughput to be 0. Do early output, avoiding
+ * numerical issues and extra unneeded work. */
+ return false;
+ }
+
+ /* Precompute term for phase sampling. */
+ const float phase_log = logf((diffusion_length + 1.0f) / (diffusion_length - 1.0f));
+
+ /* Modify state for RNGs, decorrelated from other paths. */
+ rng_state.rng_hash = cmj_hash(rng_state.rng_hash + rng_state.rng_offset, 0xdeadbeef);
+
+ /* Random walk until we hit the surface again. */
+ bool hit = false;
+ bool have_opposite_interface = false;
+ float opposite_distance = 0.0f;
+
+ /* TODO: Disable for `alpha > 0.999` or so? */
+ /* Our heuristic, a compromise between guiding and classic. */
+ const float guided_fraction = 1.0f - fmaxf(0.5f, powf(fabsf(anisotropy), 0.125f));
+
+#ifdef SUBSURFACE_RANDOM_WALK_SIMILARITY_LEVEL
+ float3 sigma_s_star = sigma_s * (1.0f - anisotropy);
+ float3 sigma_t_star = sigma_t - sigma_s + sigma_s_star;
+ float3 sigma_t_org = sigma_t;
+ float3 sigma_s_org = sigma_s;
+ const float anisotropy_org = anisotropy;
+ const float guided_fraction_org = guided_fraction;
+#endif
+
+ for (int bounce = 0; bounce < BSSRDF_MAX_BOUNCES; bounce++) {
+ /* Advance random number offset. */
+ rng_state.rng_offset += PRNG_BOUNCE_NUM;
+
+#ifdef SUBSURFACE_RANDOM_WALK_SIMILARITY_LEVEL
+ // shadow with local variables according to depth
+ float anisotropy, guided_fraction;
+ float3 sigma_s, sigma_t;
+ if (bounce <= SUBSURFACE_RANDOM_WALK_SIMILARITY_LEVEL) {
+ anisotropy = anisotropy_org;
+ guided_fraction = guided_fraction_org;
+ sigma_t = sigma_t_org;
+ sigma_s = sigma_s_org;
+ }
+ else {
+ anisotropy = 0.0f;
+ guided_fraction = 0.75f; // back to isotropic heuristic from Blender
+ sigma_t = sigma_t_star;
+ sigma_s = sigma_s_star;
+ }
+#endif
+
+ /* Sample color channel, use MIS with balance heuristic. */
+ float rphase = path_state_rng_1D(kg, &rng_state, PRNG_PHASE_CHANNEL);
+ float3 channel_pdf;
+ int channel = volume_sample_channel(alpha, throughput, rphase, &channel_pdf);
+ float sample_sigma_t = volume_channel_get(sigma_t, channel);
+ float randt = path_state_rng_1D(kg, &rng_state, PRNG_SCATTER_DISTANCE);
+
+ /* We need the result of the ray-cast to compute the full guided PDF, so just remember the
+ * relevant terms to avoid recomputing them later. */
+ float backward_fraction = 0.0f;
+ float forward_pdf_factor = 0.0f;
+ float forward_stretching = 1.0f;
+ float backward_pdf_factor = 0.0f;
+ float backward_stretching = 1.0f;
+
+ /* For the initial ray, we already know the direction, so just do classic distance sampling. */
+ if (bounce > 0) {
+ /* Decide whether we should use guided or classic sampling. */
+ bool guided = (path_state_rng_1D(kg, &rng_state, PRNG_LIGHT_TERMINATE) < guided_fraction);
+
+ /* Determine if we want to sample away from the incoming interface.
+ * This only happens if we found a nearby opposite interface, and the probability for it
+ * depends on how close we are to it already.
+ * This probability term comes from the recorded presentation of [3]. */
+ bool guide_backward = false;
+ if (have_opposite_interface) {
+ /* Compute distance of the random walk between the tangent plane at the starting point
+ * and the assumed opposite interface (the parallel plane that contains the point we
+ * found in our ray query for the opposite side). */
+ float x = clamp(dot(ray.P - P, -N), 0.0f, opposite_distance);
+ backward_fraction = 1.0f /
+ (1.0f + expf((opposite_distance - 2.0f * x) / diffusion_length));
+ guide_backward = path_state_rng_1D(kg, &rng_state, PRNG_TERMINATE) < backward_fraction;
+ }
+
+ /* Sample scattering direction. */
+ float scatter_u, scatter_v;
+ path_state_rng_2D(kg, &rng_state, PRNG_BSDF_U, &scatter_u, &scatter_v);
+ float cos_theta;
+ float hg_pdf;
+ if (guided) {
+ cos_theta = sample_phase_dwivedi(diffusion_length, phase_log, scatter_u);
+ /* The backwards guiding distribution is just mirrored along `sd->N`, so swapping the
+ * sign here is enough to sample from that instead. */
+ if (guide_backward) {
+ cos_theta = -cos_theta;
+ }
+ float3 newD = direction_from_cosine(N, cos_theta, scatter_v);
+ hg_pdf = single_peaked_henyey_greenstein(dot(ray.D, newD), anisotropy);
+ ray.D = newD;
+ }
+ else {
+ float3 newD = henyey_greenstrein_sample(ray.D, anisotropy, scatter_u, scatter_v, &hg_pdf);
+ cos_theta = dot(newD, N);
+ ray.D = newD;
+ }
+
+ /* Compute PDF factor caused by phase sampling (as the ratio of guided / classic).
+ * Since phase sampling is channel-independent, we can get away with applying a factor
+ * to the guided PDF, which implicitly means pulling out the classic PDF term and letting
+ * it cancel with an equivalent term in the numerator of the full estimator.
+ * For the backward PDF, we again reuse the same probability distribution with a sign swap.
+ */
+ forward_pdf_factor = M_1_2PI_F * eval_phase_dwivedi(diffusion_length, phase_log, cos_theta) /
+ hg_pdf;
+ backward_pdf_factor = M_1_2PI_F *
+ eval_phase_dwivedi(diffusion_length, phase_log, -cos_theta) / hg_pdf;
+
+ /* Prepare distance sampling.
+ * For the backwards case, this also needs the sign swapped since now directions against
+ * `sd->N` (and therefore with negative cos_theta) are preferred. */
+ forward_stretching = (1.0f - cos_theta / diffusion_length);
+ backward_stretching = (1.0f + cos_theta / diffusion_length);
+ if (guided) {
+ sample_sigma_t *= guide_backward ? backward_stretching : forward_stretching;
+ }
+ }
+
+ /* Sample direction along ray. */
+ float t = -logf(1.0f - randt) / sample_sigma_t;
+
+ /* On the first bounce, we use the ray-cast to check if the opposite side is nearby.
+ * If yes, we will later use backwards guided sampling in order to have a decent
+ * chance of connecting to it.
+ * TODO: Maybe use less than 10 times the mean free path? */
+ ray.t = (bounce == 0) ? max(t, 10.0f / (min3(sigma_t))) : t;
+ scene_intersect_local(kg, &ray, &ss_isect, object, NULL, 1);
+ hit = (ss_isect.num_hits > 0);
+
+ if (hit) {
+#ifdef __KERNEL_OPTIX__
+ /* t is always in world space with OptiX. */
+ ray.t = ss_isect.hits[0].t;
+#else
+ /* Compute world space distance to surface hit. */
+ float3 D = transform_direction(&ob_itfm, ray.D);
+ D = normalize(D) * ss_isect.hits[0].t;
+ ray.t = len(transform_direction(&ob_tfm, D));
+#endif
+ }
+
+ if (bounce == 0) {
+ /* Check if we hit the opposite side. */
+ if (hit) {
+ have_opposite_interface = true;
+ opposite_distance = dot(ray.P + ray.t * ray.D - P, -N);
+ }
+ /* Apart from the opposite side check, we were supposed to only trace up to distance t,
+ * so check if there would have been a hit in that case. */
+ hit = ray.t < t;
+ }
+
+ /* Use the distance to the exit point for the throughput update if we found one. */
+ if (hit) {
+ t = ray.t;
+ }
+ else if (bounce == 0) {
+ /* Restore original position if nothing was hit after the first bounce,
+ * without the ray_offset() that was added to avoid self-intersection.
+ * Otherwise if that offset is relatively large compared to the scattering
+ * radius, we never go back up high enough to exit the surface. */
+ ray.P = P;
+ }
+
+ /* Advance to new scatter location. */
+ ray.P += t * ray.D;
+
+ float3 transmittance;
+ float3 pdf = subsurface_random_walk_pdf(sigma_t, t, hit, &transmittance);
+ if (bounce > 0) {
+ /* Compute PDF just like we do for classic sampling, but with the stretched sigma_t. */
+ float3 guided_pdf = subsurface_random_walk_pdf(forward_stretching * sigma_t, t, hit, NULL);
+
+ if (have_opposite_interface) {
+ /* First step of MIS: Depending on geometry we might have two methods for guided
+ * sampling, so perform MIS between them. */
+ float3 back_pdf = subsurface_random_walk_pdf(backward_stretching * sigma_t, t, hit, NULL);
+ guided_pdf = mix(
+ guided_pdf * forward_pdf_factor, back_pdf * backward_pdf_factor, backward_fraction);
+ }
+ else {
+ /* Just include phase sampling factor otherwise. */
+ guided_pdf *= forward_pdf_factor;
+ }
+
+ /* Now we apply the MIS balance heuristic between the classic and guided sampling. */
+ pdf = mix(pdf, guided_pdf, guided_fraction);
+ }
+
+ /* Finally, we're applying MIS again to combine the three color channels.
+ * Altogether, the MIS computation combines up to nine different estimators:
+ * {classic, guided, backward_guided} x {r, g, b} */
+ throughput *= (hit ? transmittance : sigma_s * transmittance) / dot(channel_pdf, pdf);
+
+ if (hit) {
+ /* If we hit the surface, we are done. */
+ break;
+ }
+ else if (throughput.x < VOLUME_THROUGHPUT_EPSILON &&
+ throughput.y < VOLUME_THROUGHPUT_EPSILON &&
+ throughput.z < VOLUME_THROUGHPUT_EPSILON) {
+ /* Avoid unnecessary work and precision issue when throughput gets really small. */
+ break;
+ }
+ }
+
+ if (hit) {
+ kernel_assert(isfinite3_safe(throughput));
+ INTEGRATOR_STATE_WRITE(state, path, throughput) = throughput;
+ }
+
+ return hit;
+}
+
+CCL_NAMESPACE_END