Råne River Geochemistry
https://doi.org/10.5878/mnfe-a623
This dataset contains element concentrations of quantitative element screenings (ICP-MS, 70+ elements), conducted on filtered water samples and the filtered material (cut-off 0.22 μm) from samples taken in the Råne River and in the Råne River estuary during three sampling campaigns (2013, 2014, and 2016). The purpose of the study was to observe changes in the dissolved and particulate element concentrations during spring flood and along a slowly increasing salinity gradient.
Water samples in the Råne River estuaries were collected during the spring flood in February, March and April 2014, in May and June 2013, and in May, June and July 2014. Water samples from the Råne River estuaries were taken from the coastguard vessel KBV005 in May and June 2013. Samples at all sampling stations were collected at 0.5, 5 and 10 meters deep if they were deep enough. At the sampling in March 2014, samples were taken from the first three stations in the estuaries while they were still covered with ice. In 2014, the tests were carried out through a hole in the ice. The hole was drilled with an ice drill and the samples pumped up from depths of 0.5, 5 and 10 meters.
Water samples from the Råne River were collected during the spring flood 2016, from March to July. In Råneälven, at the sampling station Orrbyn, samples were taken from a bridge in the middle of the river.
Documentation files
Documentation files
Citation and access
Citation and access
Data access level:
Creator/Principal investigator(s):
Research principal:
Data contains personal data:
No
Citation:
Language:
Method and outcome
Method and outcome
Time period(s) investigated:
Variables:
111
Data format/data structure:
Data collection - Physical measurements and tests
Data collection - Physical measurements and tests
Mode of collection:
Physical measurements and tests
Description of the mode of collection:
The sampled river waters were filtered in situ through 0.45 /um filters using a peristaltic pump. The filtered samples were then acidified with 25 ml of ultrapure HCI. All bottles, tubing, filters and filter holders were acid-cleaned before use.
Time period(s) for data collection:
1991-04 - 1992-09
Data collection - Physical measurements and tests
Data collection - Physical measurements and tests
Mode of collection:
Physical measurements and tests
Description of the mode of collection:
The samples in 2013 were collected from the coast guard vessel KBV005 with 2 × 2 L Niskin bottles (Hydros-Bios, Kiel, Germany, which had been custom-made trace metal clean and contained only Ti screws, on a Dyneema rope, acid-cleaned 2-L LDPE bottles - all parts acid cleaned), on a line at depths of 0.5, 5 and 10 m. In 2014, the samples were collected through a hole in the ice, drilled with an ice auger and pumped up from depths of 0.5, 5 and 10 meters.
Time period(s) for data collection:
2013 - 2016
Geographic coverage
Geographic coverage
Geographic location:
Geographic description:
The Råne River and the Råne River estuary were sampled, at 4 chosen sampling locations. Latitude and longitude points of each sample are included in the "Sampling Information" tabs within the dataset for each sampling event.
Administrative information
Administrative information
Responsible department/unit:
Department of Civil, Environmental and Natural Resources Engineering
Contributor(s):
- Katelyn Murphy – Luleå University of Technology - Department of Civil, Environmental and Natural Resources Engineering
- Per S. Andersson – California Institute of Technology - Division of Geological and Planetary Sciences
- Katherina Wortberg – RWTH Aachen University
- Nils Jansen – University of Tasmania - Institute for Marine and Antarctic Studies
Funding
Funding
Funding agency:
- Bio4Energy
Funding agency:
- European Commission
Opens a new window at ror.org.
ROR
Award number:
290336
Funding information:
Marie Skłodowska Curie Actions (MSCA)
Topic and keywords
Topic and keywords
Swedish Standard Classification of Research Subjects 2025:
INSPIRE topic categories:
Relations
Relations
Related research data:
Publications
Publications
Citation:
Conrad, S., Wuttig, K., Jansen, N., Rodushkin, I., & Ingri, J. (2018). The stability of Fe isotope signatures during low salinity mixing in subarctic estuaries. In Aquatic geochemistry (Vol. 25, Issues 5–6, pp. 195–218). https://doi.org/10.1007/s10498-019-09360-z
SwePub:
Citation:
Herzog, S. D., Conrad, S., Ingri, J., Persson, P., Kritzberg, E. S., Herzog, S. D., Conrad, S., Kritzberg, E. S., Ingri, J., & Persson, P. (2019). Spring flood induced shifts in Fe speciation and fate at increased salinity. In Applied Geochemistry (No. 104385; Vol. 109). https://doi.org/10.1016/j.apgeochem.2019.104385
SwePub:
Citation:
Conrad, S. (2019). Iron isotopes in aquatic systems.
ISBN:
