John R. White

Associate Dean of Research and Professor Louisiana State University

  • Baton Rouge LA

Dr. White's research focuses on biogeochemical cycling of carbon, nitrogen and phosphorus in aquatic systems.

Contact

Louisiana State University

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Biography

John R. White teaches courses in oceanography, wetlands, and water quality. His interests include biogeochemical cycling of nitrogen and phosphorus in acquatic systems including coastal and freshwater wetlands and estuaries, constructed wetlands, sediment and pharmaceuticals removal, dynamics of internal nutrient loading, activity of soils and sediments, and plant-soil interactions. Dr. White holds a Doctorate degree in wetland biogeochemistry from the University of Florida, Master’s degrees in both coastal zone management and geological oceanography from the Florida Institute of Technology, and Bachelor’s degree in geology from Washington & Lee University.

Areas of Expertise

Coastal Restoration
Biogeochemistry
Oceanography
Water Quality
Wetlands

Research Focus

Carbon & Nitrogen Biogeochemistry

Dr. White’s research focuses on carbon, nitrogen, and phosphorus cycling in coastal and freshwater wetlands, estuaries, and lake sediments. He studies constructed-wetland treatment of nutrients and pharmaceuticals, internal nutrient loading, and microbially driven transformations to guide coastal restoration managers—a body of work honored with the National Wetlands Award.

Education

University of Florida

Ph.D.

Soil & Water Science

1999

Florida Institute of Technology

M.S.

Coastal Zone Management

1993

Florida Institute of Technology

M.S.

Geological Oceanography

1992

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Accomplishments

Dean’s Outstanding Service Award

2018

Fellow, Soil Science Society of America

2017

Coast & Environment Outstanding Faculty Research Award

2015

Media Appearances

Scientists say land is being created at one of two sites on Louisiana's coast

Phys.org  online

2022-12-01

White said that the methodologies used to gather data are significant for the state's planned sediment diversions. Wetlands can prove difficult to measure using standard remote sensing techniques, he said, because the rise and subsequent retreat of flood waters make it difficult to determine where land is building, depending on the changing water level.

"Our study in Davis Pond used appropriate remote sensing tools and combined them with over 140 measurements on the soils and plants to provide ground-truthing and certainty for modeling. If a river diversion is affecting the soil, you need to measure the soil, before and after, to fully understand how the river diversion is affecting the land," he said.

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Articles

Implications of river reconnection on phosphorus cycling in coastal wetlands

Science of The Total Environment

2025

Louisiana's coastal wetlands are experiencing some of the world's largest land loss rates. This problem is partly due to levees along the Mississippi River, isolating the river from the coastal basins. This disconnect prevents delivering of sediment and nutrients to the wetland-dominated coastal basins, where sediments would increase marsh accretion. Louisiana's Coastal Master Plan aims to reconnect the river with riparian areas through construction of a diversion. Baseline phosphorus (P) dynamics were determined before river reconnection and compared to an area with an unmanaged connection to the river.

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On the calculation of carbon and nutrient transport to the oceans

Scientific Reports

2025

Correct estimations of sediment, carbon, and nutrient fluxes are crucial for understanding the impacts of land use, environmental change, and climate change. However, limited measurements—often restricted to surface data or aliased data, i.e., data without repeated observations throughout a tidal cycle—can lead to significant errors in transport calculations, particularly when different water masses interact. To address this issue, our study employed repeated, cross-sectional (cross-channel and through the vertical) measurements of water velocity and concentrations of sediment, carbon, and nutrients over the course of a tidal cycle.

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Patterns and mechanisms of wetland change in the Breton sound estuary, Mississippi River delta: A review

Estuarine, Coastal and Shelf Science

2025

The Breton Sound Estuary, located within the Mississippi River Delta, has experienced significant wetland loss over the past century due to a combination of natural and anthropogenic factors. This study examines the patterns and mechanisms driving wetland change in the upper Breton Sound Basin and focuses on the impacts of riverine isolation, hydrological alterations, and human activities. Prior to human interventions, the basin received regular large riverine input via overbank flooding and crevasse channels. Levee construction began in the 18th century, but it wasn't until the great Mississippi River flood of 1927 that continuous levees were built that completely isolated the river from the upper Breton Sound Basin.

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Affiliations

  • United States EPA : Board of Scientific Counselors, Safe and Sustainable Waters
  • Soil Science Society of America
  • American Geophysical Union
  • Society of Wetland Scientists

Media

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