Models of the early diagenesis of neodymium and its radiogenic isotope at deep-sea site HH3000, Oregon margin, Northeast Pacific
Authors/Creators
- 1. ETH Zurich
- 2. Oregon State University
- 3. Coastal Carolina University
- 4. Bigelow Laboratory for Ocean Sciences
Description
Outputs of the early diagenetic model for neodymium and its radiogenic isotope at deep sea station HH3000 (3060 m, 43°52'N, 125°38'W) from the Oregon margin, Northeast Pacific.
Three types of models are included, and the files are named as following:
1. Baseline simulations, "HH3000Nd.baseline.copre_output.xlsx" for the co-precipitation formulation, and "HH3000Nd.baseline.revscan_output.xlsx" for the reversible scavenging formulation.
2. Sensitivity tests of silicate dissolution rate: "HH3000Nd.{mineral}.{dissolution rate}_output.xlsx", where {mineral} can be "Basalt", "Plag" (plagioclase), "Cpx" (clinopyroxene) or "Chl" (chlorite), and {dissolution rate} can be "1e0" to "1e5", referring to the order of magnitude reduction of dissolution rate relative to the laboratory-derived rates.
3. Sensitivity tests of authigenic clay precipitation rate: “HH3000Nd.basalt.{precipitation rate}.illite_output.xlsx", where "{precipitation rate}" can be "no", "slow", "normal", or "fast".
Explanations of the modeled variables in the above files can be found in "model variable note.xlsx".
Notes
Files
Du et al., 2022 EPSL.zip
Additional details
Related works
- Is supplement to
- Journal article: 10.1016/j.epsl.2022.117792 (DOI)
Funding
- U.S. National Science Foundation
- Gulf of Alaska Deep and Intermediate Watermass Changes and Paleoventilation 1357529
- European Commission
- SedTraceFlux - The critical role of sedimentary trace element fluxes in ocean biogeochemistry 891489
- U.S. National Science Foundation
- Behavior of Nd isotopes at the Ocean-Sediment Boundary: Addressing the "Nd Paradox" 1147407