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A new method to reconstruct the sediment transport pathways, which is based on the sediment grain-size distribution and uses principal component analysis (P-GSTA), is proposed here. In this method, a linearly-combined value of six grain-size parameters (mean, coefficient of variance, skewness, kurtosis and log-ratios of mud and gravel contents) with different weighting factors is used as a proxy of sediment transport processes. The combination of this method and cluster analysis is very effective to reconstruct sediment transport patterns in the depositional environments where compositive depositional processes exist.

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Sediment transport pathways on the modern microtidal sand flat reconstructed by the new method of sediment trend analysis (P-GSTA): Case studies of Kushida River and Obitsu River deltas, Japan