Package 'FluvialTracer'

Description

A function that calculates and visualizes the percentage deviation between an experimental artificial mixture and a theoretical virtual mixture calculated from user-defined source proportions. Source proportions should be defined as described in Option A: manual list or Option B: CSV file

Usage

checking_diff_mult_mix(
  data,
  proportions = props_table,
  sample_col = 1,
  source_col = 2
)

Arguments

Value

No return value, called for side effects (draws one plot per mixture showing the deviation between the virtual and artificial mixture).

Description

A function that calculates and visualizes the percentage deviation between an experimental artificial mixture and a theoretical virtual mixture calculated from user-defined source proportions.

Usage

checking_diff_single_mix(
  data,
  proportions = c(1, 0, 0, 0),
  sample_col = 1,
  source_col = 2,
  subtitle_extra = NULL
)

Arguments

Value

Invisibly returns a gtable object with the combined plot (both panels, title, legend and caption). The plot is also drawn on the current graphics device.

Description

Quantifies how consistently each tracer constrains the mixture apportionment when paired with randomly chosen complementary tracers. For each tracer of interest, the function solves a large number of minimal determined systems and records the spread of the resulting source contributions. A narrow spread indicates that the tracer is conservative and highly informative, regardless of which other tracers accompany it.

Usage

CI_Method(
  data,
  points = 2000,
  Means = NULL,
  triangles = "virtual",
  seed = 123456L
)

Arguments

Details

Two strategies are available for selecting the accompanying tracers:

• Virtual method: remaining tracers are replaced by values drawn uniformly from $[0, 1]$, isolating the tracer of interest from correlations with other measured properties.

• Dataset method: remaining tracers are sampled at random from the measured dataset, reflecting realistic geochemical combinations.

Value

A list with one data frame per tracer containing the predicted source contributions across all iterations, followed by two named elements: DB, the input data, and CI, a data frame with the CI score, normalized score, category and status for each tracer.

References

Lizaga, I., Latorre, B., Bodé, S., Gaspar, L., Boeckx, P., & Navas, A. (2024). Combining isotopic and elemental tracers for enhanced sediment source partitioning in complex catchments. Journal of Hydrology*, 631 , 130768.doi:10.1016/j.jhydrol.2024.130768

Lizaga, I., Latorre, B., Gaspar, L., & Navas, A. (2020). Consensus ranking as a method to identify non-conservative and dissenting tracers in fingerprinting studies. Science of The Total Environment, 720, 137537. doi:10.1016/j.scitotenv.2020.137537

Description

Takes the output of CTS_n_sources and groups the tracer combinations into clusters of similar source contributions (w1, w2, ...). This helps identify the dominant apportionment solutions and how many individual tracers support each one.

Usage

cluster_solutions(
  cts_result,
  top_n = 50L,
  k = NULL,
  max_k = 6L,
  interactive = FALSE,
  seed = NULL
)

Arguments

Details

Hierarchical clustering with Ward.D2 linkage is used because contribution clusters are rarely spherical or equal-sized. The optimal number of clusters is selected automatically via the average silhouette width criterion, but can be overridden with the k argument.

Visualisation adapts to the number of sources:

• 2 sources: single 2D panel (w1 vs w2).

• 3 sources: two 2D panels (w1~w2, w1~w3) plus optional interactive 3D plotly scatter.

• 4+ sources: all pairwise 2D panels as a grid. Interactive 3D is not available (dimensionality reduction would obscure interpretation).

The physically feasible region (0-100 shaded white; everything outside it (negative or >100 i.e. not physically possible) is shaded grey.

Value

A named list:

summary

Data frame: one row per cluster with mean/SD of each contribution, n_pairs, n_unique_tracers, avg_silhouette.

tracers

Named list. Each element has $pairs (character vector) and $individual_tracers (data frame ranked by frequency).

plot

ggplot2 or plotly visualisation.

References

Wynants, M., Verboom, C., Lizaga, I., de Boer, H., van der Perk, M., Bennett, W., Boeckx, P., & Brooks, A. Sediment and phosphorus source hysteresis and tracing during an extreme flood in a subtropical Australian river.

Description

Transforms isotopic ratio and elemental content data into virtual scalar tracers that can be directly used in classical unmixing models.

Usage

Conservative_Balance(data, error_propagation = "ratio", impute_nas = FALSE)

CB_Method(data, ...)

cb_method(...)

Arguments

Value

A data frame with isotopic tracers replaced by their CB-transformed scalar equivalents.

Description

Assesses the mathematical consistency of a tracer selection by computing the normalized error between the predicted and observed tracer concentrations in the mixture. A low error (typically below 0.05) for all tracers indicates a consistent selection. High errors point to non-conservative tracers or multiple partial solutions in the dataset.

Usage

consistency_error(data, solution)

CTS_error(data, solution)

cts_error(data, solution)

Arguments

Details

The error for each tracer is the absolute difference between the observed mixture concentration and the virtual mixture reconstructed from the apportionment solution, after normalizing by the range of the source confidence intervals.

Value

A data frame with columns tracer and consistency_error, one row per tracer.

References

Latorre, B., Lizaga, I., Gaspar, L., & Navas, A. (2021). A novel method for analysing consistency and unravelling multiple solutions in sediment fingerprinting. Science of The Total Environment, 789, 147804.

Description

Generates a correlation matrix scatterplot of dataset properties, grouped by source, to aid in collinearity diagnosis and optimal tracer selection.

Usage

Correlation_Chart(
  data,
  tracers = 1:(ncol(data) - 2),
  mixtures = TRUE,
  nmixtures = 2,
  colors = NULL,
  seed = NULL
)

correlationPlot(
  data,
  tracers = 1:(ncol(data) - 2),
  mixtures = TRUE,
  nmixtures = 2,
  colors = NULL,
  seed = NULL
)

correlation_plot(
  data,
  tracers = 1:(ncol(data) - 2),
  mixtures = TRUE,
  nmixtures = 2,
  colors = NULL,
  seed = NULL
)

Arguments

Value

A GGally::ggpairs object.

Description

Computes the Consensus Ranking (CR) method, an ensemble technique to identify non-conservative and dissenting tracers. The method combines predictions from single-tracer models and is based on a scoring function derived from a series of random "debates" between tracers, utilizing advanced thresholding logic for extreme datasets.

Usage

CR_Method(
  data,
  debates = 1000,
  completion_quantile = 1,
  apportionment_threshold = 0,
  seed = 123456
)

CR(
  data,
  debates = 1000,
  completion_quantile = 1,
  apportionment_threshold = 0,
  seed = 123456
)

cr_ns(
  data,
  debates = 1000,
  completion_quantile = 1,
  apportionment_threshold = 0,
  seed = 123456
)

Arguments

Value

A data frame containing the CR score, debates won, and debates lost per tracer.

References

Lizaga, I., Latorre, B., Gaspar, L., & Navas, A. (2020). Consensus ranking as a method to identify non-conservative and dissenting tracers in fingerprinting studies. *Science of The Total Environment*, *720*, 137537. https://doi.org/10.1016/j.scitotenv.2020.137537

Description

Solves determined systems for 1 tracer and 2 sources to assess solution dispersion and discriminant capacity.

Usage

CTS_2_sources(source, mixture, iter = 1000, seed = 123456)

singles(source, mixture, iter = 1000, seed = 123456)

CTS_seeds_singles(source, mixture, iter = 1000, seed = 123456)

Arguments

Value

A data frame with one row per tracer, sorted by max_dw (most discriminant first), with columns: id (tracer name), w1, w2 (source contributions from mean values), dw1, dw2 (dispersion of each contribution, half the 16-84% quantile range), cons (proportion of physically feasible solutions) and max_dw (maximum dispersion).

Description

Solves determined systems for 2 tracers and 3 sources to assess solution dispersion and discriminant capacity.

Usage

CTS_3_sources(source, mixture, iter = 1000, seed = 123456)

pairs(source, mixture, iter = 1000, seed = 123456)

CTS_seeds_pairs(source, mixture, iter = 1000, seed = 123456)

Arguments

Value

A data frame with one row per tracer pair, sorted by max_dw (most discriminant first), with columns: id (tracer pair), w1, w2, w3 (source contributions from mean values), dw1, dw2, dw3 (dispersion of each contribution, half the 16-84% quantile range), cons (proportion of physically feasible solutions) and max_dw (maximum dispersion).

Description

Solves determined systems for 3 tracers and 4 sources to assess solution dispersion and discriminant capacity.

Usage

CTS_4_sources(source, mixture, iter = 1000, seed = 123456)

triplets(source, mixture, iter = 1000, seed = 123456)

CTS_seeds_triplets(source, mixture, iter = 1000, seed = 123456)

Arguments

Value

A data frame with one row per tracer triplet, sorted by max_dw (most discriminant first), with columns: id (tracer triplet), w1 to w4 (source contributions from mean values), dw1 to dw4 (dispersion of each contribution, half the 16-84% quantile range), cons (proportion of physically feasible solutions) and max_dw (maximum dispersion).

Description

Solves determined systems for 4 tracers and 5 sources to assess solution dispersion and discriminant capacity.

Usage

CTS_5_sources(source, mixture, iter = 1000, seed = 123456)

quartets(source, mixture, iter = 1000, seed = 123456)

CTS_seeds_quartets(source, mixture, iter = 1000, seed = 123456)

Arguments

Value

A data frame with one row per tracer quartet, sorted by max_dw (most discriminant first), with columns: id (tracer quartet), w1 to w5 (source contributions from mean values), dw1 to dw5 (dispersion of each contribution, half the 16-84% quantile range), cons (proportion of physically feasible solutions) and max_dw (maximum dispersion).

Description

Identifies the most discriminant minimal tracer combinations (n-1) by solving determined systems and assessing solution dispersion. Lower dispersion indicates higher discriminant capacity.

Usage

CTS_n_sources(data, iter = 1000, seed = 123456)

CTS_seeds(data, iter = 1000, seed = 123456)

Arguments

Value

A data frame with one row per tracer combination, sorted by max_dw (lowest dispersion first), with columns: id (tracer combination), w1, w2, ... (source apportionments), dw1, dw2, ... (solution dispersion), % in sources range (percentage of physically feasible solutions) and max_dw (maximum dispersion).

References

Latorre, B., Lizaga, I., Gaspar, L., & Navas, A. (2021). A novel method for analysing consistency and unravelling multiple solutions in sediment fingerprinting.

Description

Performs stepwise forward variable selection using the Wilks Lambda criterion. Tracers are added one at a time when they improve inter-source discrimination beyond the specified significance threshold.

Usage

DFATest(data, niveau = 0.1)

Arguments

Value

A list with two elements: (1) a data frame retaining only the tracer columns selected by the stepwise procedure, and (2) the object returned by klaR::greedy.wilks with the details of the selection.

Description

A named vector of hex color codes used as the default palette across FluvialTracer's plotting functions (e.g. plot_apportionment, LDA_Chart). Designed to remain visually distinct for up to five sources plus the mixture.

Usage

fluvial_palette

Format

A named character vector of length 20.

Source

Custom palette defined by the FluvialTracer authors.

Description

Virtual dataset in the standard FluvialTracer format, used in the package examples.

Usage

fluvialdata_example

Format

A data frame with one row per sample: sample ID, source/mixture group, and one column per tracer.

Examples

head(fluvialdata_example)

Description

Estimates the fractional contribution of each sediment source to a mixture by solving an overdetermined mass-balance system with least-squares minimisation. Source variability is propagated by Monte Carlo resampling: at each iteration, synthetic source signatures are drawn from a normal distribution defined by the measured mean and standard deviation, and the system is solved independently for each draw.

Usage

frequentist_unconstrained(
  data,
  variability = "SEM",
  iter = 1000,
  means = FALSE,
  seed = 123456L
)

Arguments

Details

This function is the computational back-end called by unmixing. For most users, calling unmixing directly is recommended.

Value

A data frame with one row per iteration containing the mixture ID, goodness-of-fit (GOF), and one column per source with the estimated fractional contribution.

Description

Estimates the fractional contribution of each sediment source to a mixture by solving an overdetermined mass-balance system with least-squares minimisation. Unlike classical Monte Carlo propagation, uncertainty is handled analytically through Linear Variability Propagation (LVP): the Jacobian of the least-squares solution propagates source covariances directly into the apportionment uncertainty, avoiding assumptions of independent normally distributed errors.

Usage

frequentist_unconstrained_lvp(
  data,
  variability = "SEM",
  iter = 1000,
  means = FALSE,
  seed = 123456L
)

Arguments

Details

LVP is recommended when source variability is high or when apportionments are near the physical boundaries (0 or 1), where Monte Carlo resampling tends to underestimate uncertainty.

This function is the computational back-end called by unmixing when lvp = TRUE. For most users, calling unmixing directly is recommended.

Value

A data frame with one row per iteration containing the mixture ID, goodness-of-fit (GOF), and one column per source with the estimated fractional contribution.

References

Latorre, B., Lizaga, I., Gaspar, L., & Navas, A. (2025). Evaluating the impact of high source variability and extreme contributing sources on sediment fingerprinting models. Water Resources Management. doi:10.1007/s11269-025-04169-8

Description

Biplot for Principal Components using ggplot2

Usage

ggbiplot(
  pcobj,
  choices = 1:2,
  scale = 1,
  pc.biplot = TRUE,
  obs.scale = 1 - scale,
  var.scale = scale,
  groups = NULL,
  ellipse = FALSE,
  ellipse.prob = 0.68,
  labels = NULL,
  labels.size = 3,
  alpha = 1,
  var.axes = TRUE,
  circle = FALSE,
  circle.prob = 0.69,
  varname.size = 3,
  varname.adjust = 1.5,
  varname.abbrev = FALSE,
  ...
)

Arguments

Value

A ggplot2 plot.

Description

Visualizes the distribution of continuous tracer variables across sources and mixtures. It compactly displays five summary statistics (the median, two hinges, and two whiskers), alongside individual outliers.

Usage

Graph_boxplots(
  data,
  tracers = 1:(ncol(data) - 2),
  ncol = 3,
  colors = NULL,
  seed = NULL,
  max_per_page = 16,
  label_size = 3
)

boxPlot(
  data,
  tracers = 1:(ncol(data) - 2),
  ncol = 3,
  colors = NULL,
  seed = NULL,
  max_per_page = 16,
  label_size = 3
)

box_plot(
  data,
  tracers = 1:(ncol(data) - 2),
  ncol = 3,
  colors = NULL,
  seed = NULL,
  max_per_page = 16,
  label_size = 3
)

Arguments

Value

Invisibly returns a list of gtable objects, one per page. The plots are also drawn on the current graphics device.

Description

Identifies and returns the rows corresponding to the sediment mixture(s) in a combined source-mixture data frame. The mixture is assumed to be the last unique group in the second column of data. Both raw and averaged (Mean_/SD_) formats are supported.

Usage

inputSample(data)

inputMixture(data)

Arguments

Value

A data frame containing only the mixture rows, with column names standardised to the FluvialTracer convention.

See Also

inputSource for extracting source rows.

Description

Selects and extracts the source samples from the dataset, computing mean, SD and n when the input is in raw format. When a different format dataset is detected, column names are normalised to Mean_/SD_ in the output so that all downstream functions work correctly.

Usage

inputSource(data, na.omit = TRUE)

Arguments

Value

A data frame with one row per source, containing the source identifier (id), the mean of each tracer (Mean_ columns), the standard deviation of each tracer (SD_ columns) and the number of samples (n).

Description

Retains only tracer properties that show statistically significant differences across source groups according to the non-parametric Kruskal-Wallis rank-sum test. Tracers with no discriminant power add noise to the unmixing model and should be removed before unmixing.

Usage

KWTest(data, pvalue = 0.05)

Arguments

Value

A data frame retaining only tracer columns with p-value below pvalue.

Description

Performs a linear discriminant analysis (LDA) to project data into maximum-separation dimensions. Includes a comprehensive discrimination summary detailing variance explained, a leave-one-out cross-validation confusion matrix, and misclassification rates to rigorously assess source separability.

Usage

LDA_Chart(
  data,
  Plot3D = FALSE,
  text = FALSE,
  colors = NULL,
  interactive = FALSE,
  seed = NULL
)

LDA_plot(
  data,
  Plot3D = FALSE,
  text = FALSE,
  colors = NULL,
  interactive = FALSE,
  seed = NULL
)

LDAPlot(
  data,
  Plot3D = FALSE,
  text = FALSE,
  colors = NULL,
  interactive = FALSE,
  seed = NULL
)

Arguments

Value

Invisibly returns a list with: lda (the fitted MASS::lda object), confusion (leave-one-out confusion matrix), prop_var (percentage of variance explained by each discriminant axis) and plot (the plot object).

Description

Displays the relative contribution of sediment sources to each mixture as density or violin plots. Designed to take the output of the unmixing functions directly.

Usage

plot_apportionment(
  data,
  violin = FALSE,
  bounds = c(0, 1),
  scaled = TRUE,
  y_high = 1,
  colors = NULL,
  vlines = NULL,
  title = NULL,
  bw = "nrd"
)

plotResults(
  data,
  violin = FALSE,
  bounds = c(0, 1),
  scaled = TRUE,
  y_high = 1,
  colors = NULL,
  vlines = NULL,
  title = NULL,
  bw = "nrd"
)

plot_results(
  data,
  violin = FALSE,
  bounds = c(0, 1),
  scaled = TRUE,
  y_high = 1,
  colors = NULL,
  vlines = NULL,
  title = NULL,
  bw = "nrd"
)

Arguments

Value

A ggplot2 object.

Description

Performs a PCA on the tracer data and displays a biplot with source group ellipses. Averaged datasets (with Mean_/SD_ or mean_/sd_ columns) are automatically expanded to individual observations by sampling from a normal distribution before the PCA is computed, so all formats are accepted.

Usage

plot_pca(data, components = c(1L, 2L), colors = NULL, seed = NULL)

PCAPlot(data, components = c(1L, 2L), colors = NULL, seed = NULL)

PCA_plot(data, components = c(1L, 2L), colors = NULL, seed = NULL)

Arguments

Value

A ggplot object.

Description

Removes tracer properties whose mixture value falls outside the envelope defined by the minimum and maximum values observed across all source groups. Tracers failing this test cannot be explained by any linear combination of the measured sources and should be excluded before unmixing.

Usage

rangeTest(data)

Arguments

Value

A data frame retaining only tracer columns that pass the range test.

Description

Visualizes Conservativeness Index (CI) predictions using ternary diagrams. Incorporates advanced hierarchical clustering to automatically group and color-code structurally similar apportionment solutions.

Usage

Ternary_Plot(
  data,
  tracers = 1:(length(data) - 2),
  n_row = 4,
  n_col = 5,
  Means = FALSE,
  cluster = FALSE,
  dendro_lvls = 5,
  vrtl_sol = FALSE,
  vrtl = c(1, 0, 0),
  seed = NULL
)

Ternary_diagram(
  data,
  tracers = 1:(length(data) - 2),
  n_row = 4,
  n_col = 5,
  Means = FALSE,
  cluster = FALSE,
  dendro_lvls = 5,
  vrtl_sol = FALSE,
  vrtl = c(1, 0, 0),
  seed = NULL
)

ternary_diagram(
  data,
  tracers = 1:(length(data) - 2),
  n_row = 4,
  n_col = 5,
  Means = FALSE,
  cluster = FALSE,
  dendro_lvls = 5,
  vrtl_sol = FALSE,
  vrtl = c(1, 0, 0),
  seed = NULL
)

Arguments

Value

No return value, called for side effects (draws ternary diagrams of the individual tracer predictions on the current graphics device).

Description

Evaluates the directional bias introduced by individual tracers within Consistent Tracer Selection (CTS) subset models. This function unpacks the unconstrained source apportionments to reveal if specific tracers are systematically pulling source contributions into physically impossible spaces (e.g., >1 or <0).

Usage

tracer_pull_analysis(cts_result)

Arguments

Details

Global unmixing models (using all tracers simultaneously) can suffer from "tracer compensation," where extreme mathematical contradictions between non-conservative tracers cancel each other out, resulting in a misleadingly plausible central solution.

This function exposes that illusion. By taking the output of a CTS run (e.g., CTS_n_sources), it isolates every debate a specific tracer participated in. It then calculates the marginal effect (median, mean, and SD) that the tracer has on the fractional weight of each source.

Visualizations are automatically generated to aid interpretation:

• Boxplots: Display the distribution of calculated weights for each source, grouped by tracer. Red dashed lines denote the physical boundaries of 0 and 1.

• Heatmap: Displays the median weight pull. Deep red indicates a strong positive pull (overestimation), while deep blue indicates a negative pull (pushing the source into negative mass space).

Value

A named list containing four elements:

summary

A tibble containing the Mean, Median, and SD of the weights forced by each tracer on each source.

boxplot

A ggplot object showing the distribution of source weights grouped by tracer.

heatmap

A ggplot object visualizing the median tracer bias across all sources.

raw_expanded

A tibble of the raw, pivoted data used for calculations and plotting.

Description

For each tracer of interest, solves a series of minimal determined linear systems to assess how consistently that tracer constrains the source apportionment. In each iteration the tracer under evaluation is kept fixed while the remaining tracers needed to complete the system are drawn at random from the other measured tracers in the dataset (dataset approach). Because the companion tracers are real geochemical measurements, this strategy reflects realistic co-variation patterns among tracers and produces a less conservative — but more ecologically meaningful — estimate of tracer informativeness compared to the virtual approach.

Usage

triangles_dataset(
  sources,
  mixtures,
  tracer = 0L,
  iter = 100L,
  seed = 69512L,
  pb = NULL,
  pb_offset = 0L,
  tracer_current = NULL,
  tracer_total = NULL
)

Arguments

Details

This function is called internally by CI_Method() and is not usually invoked directly by the user.

Value

A data frame with nrow(mixtures) * iter rows. Columns are ID (mixture index), GOF (set to 1 for all rows), and one weight column per source (w.S1, w.S2, ...).

See Also

CI_Method, triangles_virtual

Description

For each tracer of interest, solves a series of minimal determined linear systems to assess how consistently that tracer constrains the source apportionment. In each iteration the tracer under evaluation is kept fixed while the remaining tracers needed to complete the system are replaced by uniformly random values in $[0, 1]$ (virtual approach). The mixture value for each virtual tracer is drawn inside the range spanned by the virtual source values, ensuring the system is geometrically solvable. Because the companion tracers carry no real geochemical information, any consistency in the resulting source weights is attributable solely to the tracer under evaluation, making this a conservative (worst-case) estimator of tracer informativeness.

Usage

triangles_virtual(
  sources,
  mixtures,
  tracer = 0L,
  iter = 100L,
  seed = 69512L,
  pb = NULL,
  pb_offset = 0L,
  tracer_current = NULL,
  tracer_total = NULL
)

Arguments

Details

This function is called internally by CI_Method() and is not usually invoked directly by the user.

Value

A data frame with nrow(mixtures) * iter rows. Columns are ID (mixture index), GOF (set to 1 for all rows), and one weight column per source (w.S1, w.S2, ...).

See Also

CI_Method, triangles_dataset

Description

A wrapper function that seamlessly formats an 'FluvialTracer' dataset (raw or averaged) and passes it to the 'MixSIAR' Bayesian unmixing engine.

Usage

unmix_mixsiar(
  data,
  tracers,
  prior_type = "uninformative",
  prior_values = NULL,
  run = "normal",
  process_err = FALSE,
  resid_err = TRUE
)

Arguments

Value

A list with three elements:

apportionment

Data frame with the posterior draws of the global source proportions, in the FluvialTracer format (ID, GOF and one column per source), compatible with plot_apportionment.

bayesian_summary

Data frame with the summary statistics of all model parameters returned by JAGS.

jags_model

The full JAGS model object returned by MixSIAR::run_model.

Description

Trains a Random Forest model on simulated virtual mixtures. Features a 'stretch_bounds' parameter to expand training data beyond the 0-1 limits, effectively eliminating the boundary bias typically seen in pure Machine Learning and Bayesian unmixing of extreme sources.

Usage

unmix_rf(
  data,
  n_sim = 10000L,
  n_trees = 500L,
  stretch_bounds = 1.2,
  seed = 123456L
)

Arguments

Value

A list containing the apportionment data frame (one row per tree) and a summary.

Description

Trains an ensemble of XGBoost models on simulated virtual mixtures. Uses bootstrapping to generate uncertainty distributions (density curves).

Usage

unmix_xgboost(
  data,
  n_sim = 5000L,
  n_boot = 100L,
  stretch_bounds = 1.2,
  seed = 123456L
)

Arguments

Value

Invisibly returns a list with two elements: apportionment, a data frame with one row per bootstrapped model (ID, GOF and one column per source), compatible with plot_apportionment; and xgb_summary, a data frame with the mean, SD, median and 95% interval of each source contribution.

Description

Estimates the fractional contribution of each potential source to one or more mixtures. Users can seamlessly switch between a lightning-fast Frequentist least-squares approach (with optional Linear Variability Propagation), a standard Bayesian MCMC approach, or a Machine Learning approach.

Usage

unmixing(
  data,
  model = "frequentist",
  iter = 1000L,
  variability = "SEM",
  lvp = TRUE,
  seed = 123456L,
  ml_type = "RandomForest",
  ...
)

Arguments

Details

Both raw (individual observations) and averaged (Mean_/SD_ columns) input formats are accepted. When multiple mixture samples are present, the model processes each independently.

Value

For the "frequentist" model, a data frame with one row per iteration and mixture. For the "bayesian" model, a named list containing the formatted apportionment data frame, the MixSIAR summary statistics, and the raw JAGS model object. For the "machine_learning" model, a named list containing the apportionment predictions and a statistical summary (rf_summary or xgb_summary).

References

Latorre, B., Lizaga, I., Gaspar, L., & Navas, A. (2025). Evaluating the impact of high source variability and extreme contributing sources on sediment fingerprinting models. Water Resources Management. doi:10.1007/s11269-025-04169-8