Preprints
https://doi.org/10.5194/essd-2026-423
https://doi.org/10.5194/essd-2026-423
13 Jul 2026
 | 13 Jul 2026
Status: this preprint is currently under review for the journal ESSD.

Physical and Geochemical Characterization of Mineral Dust Samples Collected by the DUST^2 Project and Precursors, 2011–2025

Jeffrey S. Munroe and Diego P. Fernandez

Abstract. Mineral dust is a key component of Earth’s Critical Zone, transporting minerals, nutrients, and trace elements across regions and linking distant components of the lithosphere, atmosphere, hydrosphere, and biosphere, yet quantitative understanding of these connections is limited by the availability of spatially distributed, well-characterized datasets. Here, we present a multi-year dataset of mineral dust samples collected as part of the DUST^2 Critical Zone Thematic Cluster and precursor projects using a network of 20 passive dust collectors deployed across a source-to-sink transect from arid dust-emitting regions of the Great Basin to downwind mountain environments in Utah, Nevada, and Idaho. The dataset includes measurements of major and trace element concentrations, CIELAB colour parameters, and grain size distributions, together with metadata describing sampling protocols, site characteristics, temporal coverage, and analytical methods. Consistent sampling and analytical procedures enable direct comparison across sites and years, supporting evaluation of spatial patterns in dust properties, and temporal variability associated with hydroclimatic forcing and land-surface change. This dataset is designed to support a wide range of applications, including dust source apportionment, evaluation of atmospheric transport and deposition models, and assessment of atmospheric contributions to soil development, nutrient cycling, and water quality in downwind ecosystems. By providing a standardized, openly accessible record of dust composition across a well-constrained source-to-sink system, this contribution enhances data availability for studies of aeolian processes and Critical Zone dynamics and provides a transferable framework for investigating dust-driven connectivity in other regions experiencing expanding dust emissions.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
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Jeffrey S. Munroe and Diego P. Fernandez

Status: open (until 19 Aug 2026)

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Jeffrey S. Munroe and Diego P. Fernandez

Data sets

Data from the DUST^2 Project, Collectors DUST-1 through DUST-17, winter 2020-21 and summer 2021 Jeffrey S. Munroe https://doi.org/10.26022/IEDA/112309

Dust Deposition in the Uinta Mountains, 2011-2021 Jeffrey S. Munroe https://doi.org/10.26022/IEDA/112285

Data from the DUST^2 Project, Collectors DUST-1 through DUST-18, winter 2021-22 and summer 2022 Jeffrey S. Munroe https://doi.org/10.26022/IEDA/113001

Data from the DUST^2 Project, collectors DUST-1 through DUST-18, Fall 2022 to Fall 2023 Jeffrey S. Munroe https://doi.org/10.60520/IEDA/113846

Data from the DUST^2 Project, collectors DUST-1 through DUST-19, Fall 2023 to Fall 2024, and collectors DUST-19 through DUST-20, Fall 2022 to Fall 2024 Jeffrey S. Munroe https://doi.org/10.60520/IEDA/113847

Jeffrey S. Munroe and Diego P. Fernandez
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Latest update: 13 Jul 2026
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Short summary
Dust from dry landscapes can travel far, carrying minerals and trace elements into mountains, soils, streams, and ecosystems. We collected dust for more than a decade at 20 sites across Utah, Nevada, and Idaho, then measured its amount, color, grain size, and chemistry. The open dataset shows that dust varies strongly across places and years, and provides a foundation for tracing dust sources and understanding how wind-blown material affects water, soils, and the environment downwind.
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