Abstract
Radium has been commonly used as a tracer of submarine groundwater discharge to the ocean and embankments, as radium activities are commonly input into box models to calculate a groundwater flux. Similarly, isotopes of radium (Ra224, Ra223, Ra226, Ra228) have been used to calculate water mass ages, which have been used as a proxy for residence times. Less commonly, radium and other tracers have been utilized in mixing models to determine the relative contribution of groundwater to a marine system. In the literature, all of these methods have almost exclusively been solved using analytical methods prone to large errors and other issues. Project Open RaDOM, introduced here, is a collection of open-source R scripts that numerically solve for groundwater flux, residence time, and relative contribution of groundwater to coastal systems. Solving these models numerically allows for over-constrained systems to increase their accuracy and force real solutions. The scripts are written in a way to make them user-friendly, even to scientists unfamiliar with R. This communication includes a description of the scripts in Project Open RaDOM, a discussion of examples in the literature, and case studies of the scripts using previously published data.
| Original language | American English |
|---|---|
| Article number | 106 |
| Pages (from-to) | 1-12 |
| Number of pages | 12 |
| Journal | Hydrology |
| Volume | 9 |
| Issue number | 6 |
| DOIs | |
| State | Published - Jun 14 2022 |
Bibliographical note
Publisher Copyright:© 2022 by the author. Licensee MDPI, Basel, Switzerland.
Article
This article belongs to the Section Marine Environment and Hydrology InteractionsASJC Scopus Subject Areas
- Water Science and Technology
- Earth-Surface Processes
- Waste Management and Disposal
- Oceanography
Keywords
- box model
- mixing model
- submarine groundwater discharge