Three interactive Plotly figures below (ocean vertical export model, particle-size sinking times, and terrestrial subsurface concentrations) using numbers and measurements extracted from the provided studies; figures are labeled, fully annotated, and immediately rendered with Plotly.newPlot(). Visuals first, short evidence notes and citations after each figure.
Figure notes: numbers (initial mass and mass at 10, 30, 75, 100 years) are taken directly from a mechanistic fragmentationβsedimentation model that tracked a 10 mm PE parent particle and its redistributed mass across size bins; the model reports ~88.4% of mass exported to subsurface by 100 years (subsurface mass 444.53 mg) and 11% remaining at surface in small-size bins at century timescales.
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Figure notes: the model reports median transit times for 25 Β΅m particles to reach 3000 m (~80 days) and to reach bottom (~289.4 days); for 75 Β΅m particles, ~90 days to 3000 m and ~416.7 days to bottom. These reflect sinking together with marine-snow aggregates and parameterized MSA settling velocities in model runs.
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Figure notes: field measurements from 15 agricultural sites (Goa and Udupi; surface and subsurface sampling) show MPs present at every depth sampled (0β40 cm), with regional differences: Goa had higher values at 20β30 cm in this campaign while Udupi showed sharply declining concentrations with depth.
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Major blindspots that would change these visual conclusions if resolved: standardization of sampling & size detection limits across ocean/soil studies; three-dimensional ocean transport and biofouling dynamics not captured by 1-D models; and lack of long-term, globally-distributed depth-resolved time series. If future standardized depth-profiles or 3-D transport models produced systematically different vertical distributions, the interpretation of export speeds and subsurface accumulation would change substantially.
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