PIPages
Labs

Veronica Morales

University of California-Davis, CA·Earth & Environmental Science

Riverbeds release nitrous oxide, a potent greenhouse gas that warms the climate. Yet how much they release is hard to estimate.

Fields

Earth & Environmental Science

Engineering

Microbiology & Immunology

Topics

nitrous oxide

greenhouse gas emissions

hyporheic zone

Grants
1 known grant, through Jul 2027

What they work on

  1. Test whether coupling between water flow and bacterial biofilm growth in sediment pores controls where and when oxygen-free microzones form and how reactants reach them.
  2. Quantify nitrous oxide production at the macroscale using sediment column experiments that mimic riverbed (hyporheic zone) conditions.
  3. Characterize the timing and location of anoxic microzones at the pore scale with microfluidic experiments, and link scales using process-based numerical simulations.

More about the research

The gas forms in tiny pockets within the sediment where oxygen runs out. These pockets are so small that they are extremely difficult to find and measure. This collaborative project asks how bacteria living in sediments control where these low-oxygen pockets form, how large they get, and how long they last.

Why it matters

Uncertain estimates of nitrous oxide from rivers hamper climate accounting. Knowing how bacteria control oxygen-free pockets in riverbeds could improve these estimates and inform strategies to reduce greenhouse gas emissions. It could also help water managers understand how contaminants and nutrients are transformed in shallow groundwater that feeds rivers.

Known grants

From NIH and NSF research grants. Labs often have other funding we can't see.

Collaborative Research: Investigating Hyporheic Zone Reaction Enhancement by Bioclogging Across Scales

NSF · Aug 2024 – Jul 2027

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Mark Warner

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The school

University of California-Davis: 49 labs on PI Pages, $1.0B a year on research, 647 research doctorates a year.

More about University of California-Davis

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