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Fate and transport in streams and groundwaters

Luise setting up a stream tracer experiment at the Dry Creek Experimental Watershed

Under this theme, we combine experiments, numerical experiments and analytical modeling in an effort to better predict how societally-relevant materials are transported and transformed in streams. Experiments are primarily conducted at the laboratory scale (micrometers to meters), with some experiments conducted at field scale (meters to kilometers).

Carbon, nutrients, and contaminants are transformed in highly reactive regions of the stream. The overall reactivity therefore depends both on local reactivity of these regions and on the rate that reactive materials are delivered to these regions. For example, while it is relatively simple to determine whether streams are net sources or sinks of CO2, it remains extremely difficult to predict how carbon fluxes will change with changing physical (e.g,. flow, temperature) or chemical (oxygen levels) conditions.

Current projects

Water in rivers and streams regularly exchanges between the water column and a region of groundwater called the hyporheic zone (hypo “below” + rheos “flow”). The hyporheic zone has been called “the river’s liver” due to its high capacity for filtering and transforming harmful contaminants and fertilizer runoff. It also plays a major role in basic ecosystem function by harboring a large quantity of the river’s biomass, which assimilate and transform carbon and nutrients. Transport and reaction rates vary sharply between the sediment-water interface and deeper locations in the hyporheic zone. We study how these variations influence stream-scale reactions.

Relevant publications: Roche et al, 2022; Kim et al., 2022; Kim et al., 2019; Roche et al., 2019