KL
Member Since 2006
Kate Lajtha
Professor, Oregon State University
AGU Research
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Composition of Soil Organic Matter Changes After 20 Years of Detrital Manipulation in a Temperate Forest in Central Europe
SOILS IN THE ANTHROPOCENE: MECHANISMS OF STABILIZATION AND CHANGE II ORAL
biogeosciences | 12 december 2022
Isla Wrightson, Maryam Tabatabaei Anaraki, István ...
Global climate change is anticipated to lead to warmer temperatures and increased atmospheric nitrogen deposition to forest soils, which is expected t...
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Responses of Soil Organic Matter Molecular Biogeochemistry to Altered Detrital Inputs are Determined by Site-specific Ecosystem Properties: A Comparison Across Temperate Forests.
SOILS IN THE ANTHROPOCENE: MECHANISMS OF STABILIZATION AND CHANGE ACROSS SCALES V POSTER
biogeosciences | 16 december 2021
Laura C. Gómez, Myrna J. Simpson, Kate Lajtha, Ric...
Forest ecosystems are important global soil carbon (C) sinks but their capacity to sequester C is susceptible to climate change factors influencing th...
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Integrative Molecular Biogeochemistry of Soil Organic Matter After 15 Years of Detrital Manipulation in a Temperate Forest
SOILS IN THE ANTHROPOCENE: MECHANISMS OF STABILIZATION AND CHANGE ACROSS SCALES III ORAL
biogeosciences | 15 december 2021
Isla Wrightson, Maryam Tabatabaei Anaraki, Knute J...
Global climate change is anticipated to increase forest productivity due to warmer temperatures and increase atmospheric nitrogen (N) deposition to fo...
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Molecular biogeochemistry of soil organic matter after twenty years of litter additions and exclusions in a coniferous old-growth forest
SOILS IN THE ANTHROPOCENE: MECHANISMS OF STABILIZATION AND CHANGE I
biogeosciences | 15 december 2020
Myrna J. Simpson, Kate Lajtha, Ricky Chiu, Derek P...
Soil carbon storage and soil organic matter (SOM) composition are sensitive to environmental changes. Shifts in moisture, altered net primary producti...
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Microbes help and hinder the stabilization of soil C
SOIL CARBON CHANGE AND PERSISTENCE IN THE ANTHROPOCENE: RESULTS FROM EMPIRICAL, MODELING, SYNTHESIS, AND LONG-TERM STUDIES III
biogeosciences | 12 december 2019
Derek Pierson, Kamron Kayhani, Lucas Evans, Malak ...
Soils, with their potential to store and stabilize carbon (C), are an essential resource in our effort to reduce atmospheric C concentrations and limi...
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A Perspective Change: Soil C Destabilization, not Stabilization, Drives C Cycle Feedbacks to the Earth System
SOIL CARBON CHANGE AND PERSISTENCE IN THE ANTHROPOCENE: RESULTS FROM EMPIRICAL, MODELING, SYNTHESIS, AND LONG-TERM STUDIES I
biogeosciences | 11 december 2019
Vanessa L. Bailey, Caitlin Hicks Pries, Kate Lajth...
An important body of work exists on the stabilization of carbon in soils. However, C cycle feedbacks to the Earth system result from the destabilizati...
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Soil carbon, where does it come from? Where does it go? Insights from the long-term DIRT network.
SOIL CARBON CHANGE AND PERSISTENCE IN THE ANTHROPOCENE: RESULTS FROM EMPIRICAL, MODELING, SYNTHESIS, AND LONG-TERM STUDIES II
biogeosciences | 11 december 2019
Derek Pierson, Richard Bowden, Serita D. Frey, Knu...
The protection and accumulation of soil carbon (C) is fundamental for reducing atmospheric C concentrations and the associated rise in global temperat...
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Long-term Nitrogen Addition Decreases Organic Matter Decomposition and Increases Forest Soil Carbon
SOIL CARBON CHANGE AND PERSISTENCE IN THE ANTHROPOCENE: RESULTS FROM EMPIRICAL, MODELING, SYNTHESIS, AND LONG-TERM STUDIES IV POSTERS
biogeosciences | 10 december 2019
Richard Bowden, Kate Lajtha, Sarah Wurzbacher, Sus...
Forests in eastern North America receive anthropogenically-elevated nitrogen (N) deposition that alters soil biogeochemistry and forest productivity. ...
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