Research

Overview

I am broadly interested in how ecosystem functioning responds to global climate change impacts such as increased temperatures and rainfall intensification. My research uses interdisciplinary approaches to explore how chemical transformations in natural and managed terrestrial ecosystems respond to these global changes.


Soil greenhouse gas emissions in response to intensified precipitation

Global climate change is predicted to result in increased intensity and variability of precipitation events throughout much of the United States. Large rain events can lead to ponding of topographic depressions in otherwise flat agricultural fields, allowing for the occurrence of microbial reactions that produce and consume potent greenhouse gases such as nitrous oxide (N2O). My research examines how soil N2O and carbon dioxide emissions respond to large rain events, and if this response is mediated by topographic position. Specific projects include:


Topographic position mediates soil nitrous oxide emissions in response to rainfall

I have demonstrated that depressional and upslope soils in agricultural ecosystems have distinct controls over N2O emissions. Specifically, upslope soils have higher rates of N2O production via denitrification in response to large rain events, and depressional areas produce more N2O in between large rain events.

Publication: Krichels A, DeLucia EH, Sanford RA, Chee-Sanford, JC, Yang, WH (2019) Historical soil drainage mediates the response of soil greenhouse gas emissions to intense precipitation events. Biogeochemistry 143, 425-442


Microbial community composition varies by landscape position

We have demonstrated that the community composition of denitrifying microorganisms consistently varies between depressional and upslope soils. These differences likely mediate N2O production and consumption in response to intense rainfall.

Publication: Suriyavirun N, Krichels A, Kent A, Yang WH (2019) Microtopographic differences in soil properties and microbial community composition at the field scale. Soil Biology and Biochemistry 131,71-80


Dynamic controls on soil nitrous oxide hot spots and hot moments

I conducted a field experiment to determine if topography can help explain field-scale spatial variation in soil N2O emissions over the course of the growing season. We found evidence that cool temperatures may limit N2O production in response to spring rainfall. However, topography did not consistently explain variation in N2O emissions

Publications: Krichels A, Yang WH. Dynamic controls on soil nitrous oxide hot spots and hot moments. In preparation for submission to JGR Biogeosciences

 


Do mycorrhizal associations mediate soil carbon storage in montane tropical forests?

Whether trees associate with arbuscular mycorrhizal (AM) or ectomycorrhizal (EM) fungi has important consequences for soil nutrient cycling. Specifically, EM assicated treees can promote the accumulation of soil organic matter. As part of a NSF Funded IGERT program in association with the Smithsonian Tropical Research Institute, I investigated the mechanisms behind this pattern.

Publication: Yang WH, Lawrence N, Dalling J, Krichels A. Mycorrhizal mediation of soil organic matter characteristics under focal tree species in a diverse lower montane tropical forest. In preparation for submission to New Phytologist


How does ecosystem respiration respond to increased temperatures?

As part of an NSF funded Research Experience for Undergraduates program through the University of Alaska Anchorage, I worked with Dr. Paddy Sullivan to examine how warming affects ecosystem respiration in the arctic tundra. I also designed an independent project examining the contribution of lichens to ecosystem respiration.

 

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