How gases travel in lakes

An international team of researchers used several miniRUEDIs to study the 3D transport of dissolved gases in a eutrophic lake. The water in the littoral zone cools faster during the night and therefore causes a lateral «syphon stream» that transports water along the sediment, and which is balanced by corresponding water flow at the surface. Krypton was injected into the littoral water to track the syphon stream, and to quantify the transport of other, naturally abundant gases in the lake. High-frequency miniRUEDI measurements demonstrate that daily convective horizontal circulation generates littoral-pelagic transport one order of magnitude larger than typical horizontal fluxes assumed in previous gas budgets. These lateral fluxes are sufficient to redistribute gases at the basin-scale and generate concentration anomalies reported in other lakes.

Tomy Doda, et al., “Lake surface cooling drives littoral-pelagic exchange of dissolved gases”, Science Advances, 2024. DOI: 10.1126/sciadv.adi0617

miniRUEDI sniffs groundwater flow

The Swiss Federal Institute of Aquatic Science and Technology (Eawag) and their partners at CHYN and Rhesi used a miniRUEDI to track the groundwater flow near a large channelized river. The river bed was excavated to simulate a natural erosion event, as it might occur after river revitalisation. Different groundwater flow paths were artificially spiked with different noble gases, and their break-through curves at a nearby pumping well were monitored with a miniRUEDI. The spiking was repeated several times over a period of one year. These measurements show how the river/groundwater exchange evolves in response to the excavation and to the «healing» of the eroded river bed. This new tracer tool and the resulting insights will be important for groundwater management and drinking water production near revitalised river systems.

An unusual marriage of miniRUEDI data, environmental DNA and vanadium tracers shows that Mt. Fuji isn’t as easy as previously thought

Mount Fuji’s freshwater springs are not only fed by water recharged at high altitude, but also by the upwelling of deep groundwater. This was observed by Oliver Schilling and his team, who used miniRUEDI data combined with environmental DNA and vanadium tracers. Read the full story in Nature Water.

miniRUEDI as a new tool for multi-gas tracer tests (not only) in groundwaters

Eawag and Uni Neuchatel teamed up to develop and test the miniRUEDI as a tool for artificial tracer tests using different noble gases.

In a first test, helium pulses were injected into a river. A miniRUEDI was used to analyse the He concentrations in the nearby groundwater system, where the observed He breakthrough indicated a substantial loss of river water to the underlying aquifer.

In a second test, multiple pulses of different noble gases (He, Kr and Xe) were repeatedly injected at different locations into an aquifer. A miniRUEDI was used to record the breakthrough curves of the different gases in the downstream groundwater flow, which provided insights into the groundwater flow field, and showed how the flow field responded to modifications in the hydraulic connectivity of a nearby river to the aquifer.

In both tests, the miniRUEDIs efficiently provided valuable new insights into river/groundwater exchange and its effects on the groundwater quality.

Publications:

  1. T. Blanc, M. Peel, M.S. Brennwald, R. Kipfer, P. Brunner: Use of helium as an artificial tracer to study surface water/groundwater exchange. EGU21-9005, doi: 10.5194/egusphere-egu21-9005

  2. M.S. Brennwald, M. Peel, T. Blanc, Y. Tomonaga, R. Kipfer, P. Brunner, D. Hunkeler: New Experimental Tools to Use Noble Gases as Artificial Tracers for Groundwater Flow. Frontiers Water, doi: 10.3389/frwa.2022.925294

Remote control your miniRUEDI

Setting up a remote control for the miniRUEDI is easy with the right software. So far, we really like DWService! It’s open source, and you can use if for free. The DWService system works by installing an «agent» software on the miniRUEDI computer, which connects to an account on the DWService website. The website allows screen sharing, file uploads and downloads, shell access, a text editor, and other useful remote management tools for the miniRUEDI computer.

Connecting the agent to the DWService website requires a code, which is generated from the DWService account. To this end, you’ll either create your own account (it’s free!), or you can ask us to create a code for you from our DWService account.

Here’s how to install and configure the DWService agent software on the miniRUEDI computer:

  1. Connect the miniRUEDI computer to the internet.
  2. Download and and save the installer file (do not “open as text”).
  3. Install the DWService agent by using the installer (run the commands in a Terminal window):
    1. Change to the directory where you downloaded the installer file. For example:
      cd /home/ruedi/Downloads/
    2. Make sure the installer file is executable:
      chmod +x dwagent.sh
    3. Run the installer file with admin permissions (you may have to enter the admin password), using your DWService code. For example, if your code is 123-456-789:
      sudo ./dwagent.sh -silent key=123-456-789
  4. Once the installation of the DWService agent is completed, the miniRUEDI computer should be accessible via the internet using the DWService website.

New Software!

We spent some time to revamp the miniRUEDI software for instrument control and gas analysis!

The new software is not only prettier but is also easier to configure. You don’t need to write Python code anymore (but you still can!).

If you want to try the new software with your miniRUEDI, please get in touch with us.

In-situ monitoring of noble gases in groundwater during rock fracking

Clement Roques and his colleagues published a paper in Nature Scientific Reports, where they used a miniRUEDI to study changes of dissolved-gas concentrations in groundwater in response to hydraulic stimulation and fracturing of the reservoir rocks (Nature Scientific Reports, 10, 6949, 2020). The miniRUEDI was installed on-site to continuously analyse the dissolved-gas concentrations of the groundwater. The high-frequency He and Ar measurements indicate that trapped fluids were mobilized from the rocks in response to the fracking. The miniRUEDI revealed the nature and evolution of the fracture network and flow paths, and showed the effect of the fracking procedures on groundwater quality.

Full paper: “In situ observation of helium and argon release during fluid-pressure-triggered rock deformation.” Sci Rep 10, 6949 (2020). https://doi.org/10.1038/s41598-020-63458-x

Eawag News article: https://www.eawag.ch/en/news-agenda/news-portal/news-detail/observing-how-fissure-systems-are-formed-thanks-to-the-gas-sniffer/

miniRUEDI goes sailing

Researchers from the Max Planck Institute for Chemistry (Germany) installed a miniRUEDI on the Eugen Seibold, the world’s greenest research vessel. Since May of 2019, the innovative yacht has been sailing the high seas, and the miniRUEDI is set up to continuously analyse the dissolved gas concnetration in the surface water. By gradually gathering data on the various marine provinces, the climate geochemists at the Max Planck Institute for Chemistry in Mainz will be able to chart a detailed description of the world’s oceans, characterising their current properties and even reconstructing how they change over time.

A New in Situ Method for Tracing Denitrification in Riparian Groundwater

Andrea Popp and her colleagues used a miniRUEDI to study the dynamics of the biogeochemical N2 turnover in a river/groundwater system over a six-month period (Environ. Sci. Technol. 2020, 54). In addition to N2, they analysed He, Ar and Kr concentrations in the water in order to quantify the air-derived N2 component in the groundwater. These miniRUEDI data allowed them to rigorously quantify the N2 excess produced by denitrification, and to unravel the spatio-temporal dynamics of N2 denitrification in the riparian groundwater system. The results show that denitrification is highly variable in space and time, emphasizing the need for spatially and temporally resolved data to accurately account for denitrification dynamics in groundwater.

Full paper: “A New in Situ Method for Tracing Denitrification in Riparian Groundwater”, Environ. Sci. Technol. 2020, 54, 3, 1562-1572, DOI: 10.1021/acs.est.9b05393