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Barium isotope compositions and major elemental compositions of river water and sediment from the Irrawaddy and Salween River catchments

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Type:	Resource
Storage:	The size of this resource is 88.9 KB
Created:	Jan 07, 2026 at 3:12 p.m. (UTC)
Last updated:	Jan 08, 2026 at 5:58 p.m. (UTC) (Metadata update)
Published date:	Jan 08, 2026 at 5:58 p.m. (UTC)
DOI:	10.4211/hs.3521fe4163b24a968af76eed44309043
Citation:	See how to cite this resource

Sharing Status:	Published
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Abstract

This dataset contains major elemental compositions and Ba isotope compositions of filtered river water (tab 2), river sediment (tab 3) and rain samples (tab 4) collected in the Irrawaddy and Salween river catchments. In addition, major elemental compositions and Ba isotope compositions of reference clay samples from the Clay Mineral Society (tab 5) are presented. The river sediment samples were subjected to a 5 stage sequential leaching procedure as described in table 1. Data for tests to this sequential leaching procedure, feature triplicates of step 1 (NH4Cl) are presented in tab 6.

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:

WGS 84 EPSG:4326

Coordinate Units:

Decimal degrees

North Latitude

28.2088°

East Longitude

100.4150°

South Latitude

14.7550°

West Longitude

92.5049°

Temporal

Start Date:
End Date:

Content

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Credits

Funding Agencies

This resource was created using funding from the following sources:

Agency Name	Award Title	Award Number
Natural Environment Research Council		NE/P011659/1
Leverhulme Trust	Leverhulme Trust Early Career Fellowship	ECF-2019-049

How to Cite

Bridgestock, L., E. Stevenson, J. J. Baronas, A. Knight, H. J. Bradbury, A. V. Turchyn, E. T. Tipper (2026). Barium isotope compositions and major elemental compositions of river water and sediment from the Irrawaddy and Salween River catchments, HydroShare, https://doi.org/10.4211/hs.3521fe4163b24a968af76eed44309043

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/

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