PIPages
Labs

Sharon Billings

University of Kansas, KS·Earth & Environmental Science

Beneath every forest and grassland, plant roots, soil and bedrock work together to control where rainwater goes and how much carbon stays underground. These processes affect the climate by changing levels of greenhouse gases such as water vapor and carbon dioxide, and human activity can alter them.

Fields

Earth & Environmental Science

Ecology & Evolution

Topics

critical zone

regolith

bedrock weathering

Grants
1 known grant, through Jul 2027

What they work on

  1. Determine when and how strongly bedrock, compared with plant roots, controls water and carbon movement between land and atmosphere, using new field data and existing Critical Zone, NEON and LTER datasets.
  2. Identify how bedrock type and fractures create preferred water flow paths and shape root water uptake, using 3D geophysical surveys and analyses of soil pore structure.
  3. Integrate global field and satellite data with machine learning and numerical models to reveal large-scale subsurface patterns and forecast how climate shapes water flow and the carbon cycle.

More about the research

This collaborative project across seven universities asks how roots, regolith (loose rock and soil above bedrock), rock and climate interact over decades to centuries.

Why it matters

Forecasting how water and carbon move between land and air helps predict how climate change and human land use will affect water supplies, carbon storage and the greenhouse gas balance. A framework linking roots, bedrock and climate could improve the Earth system models that land managers and climate planners rely on.

Known grants

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

Collaborative Research: How roots, regolith, rock and climate interact over decades to centuries — the R3-C Frontier.

NSF · Aug 2021 – Jul 2027

Closest labs

Steven Hall

University of Wisconsin-Madison, WI·Earth & Environmental Science

Test whether variation in soil organic matter properties and cycling across U.S. ecosystems can be explained by three fundamental axes running from fast to slow biogeochemical rates, using samples and data from NEON sites.

Daniella Rempe

University of Texas at Austin, TX·Earth & Environmental Science·Early-career

Test whether slow refilling of deep subsurface moisture, rather than lasting tree physiological damage, explains why forest growth and streamflow stay suppressed after drought ends, using a multiyear deep-moisture record spanning before, during, and after a drought.

Kathleen Treseder

University of California-Irvine, CA·Ecology & Evolution

Test whether soil fungi and bacteria adapt to extreme warming more effectively when they interact with the natural microbial community, through field evolution experiments spanning thousands of generations.

The school

University of Kansas: 26 labs on PI Pages, $546M a year on research, 351 research doctorates a year.

More about University of Kansas

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