Research Interests

I am broadly interested in the physical and biological interactions that drive environmental processes in the Earth's critical zone. This has led me to pursue a variety of research questions that sit at the intersection of hydrology, ecology, and biogeochemistry. My dissertation work focused on how physical drivers (landscape characteristics, climate, etc.) interact with biological drivers (plant physiology) to impact plant water use and plant health outcomes, particularly when water is limited. I studied this using a combination of models, experiments, and field work, and using tools from hydrology, plant ecophsyiology, and stable isotope ecology. Better understanding of these ecohydrological dynamics has the potential to help inform specific management challenges, as well as to help us more broadly understand and predict water fluxes and ecosystem function in a hotter, drier world. In my postdoctoral work, I am particularly focused on ecohydrological dynamics in urban environments in order to better understand how trees can support more resilient and equitable communities under climate change. See below for more information on some of these more recent questions I've been working on.

Understanding Urban Tree Function

REU intern Aidan taking measurements of
urban trees in Minneapolis (Image: JV Wilkening)
Urban trees can provide a number of benefits to communities, but have gained particular attention as a tool for helping to cool cities in the face of increasing heat events under climate change. However, the magnitude and persistence of these benefits is dependent upon the health, function, and survival of trees in urban environments, which can be physically and hydrologically very different than non-urban environments. In this work, we are trying to better understand urban tree function and its variation across cities in order to better inform how cities should expand and manage their urban canopies for more resilient and equitable communities. This is being done using a combination of remote sensing, machine learning, and field studies. Stay tuned as we start to share this work!

Measurement Synthesis to Better Understand Plant Drought Response and Recovery

Populus trichocarpa trees being grown
for the experiment (Image: JV Wilkening)
A central challenge in ecohydrology is being able to predict plant water fluxes and how they change in response to environmental conditions. Despite many advances, it remains a challenging pursuit since these water fluxes are ultimately a function of both the environmental conditions and the physiology of the plant and the emerging dyanmics therein such that the high dimensional nature of the problem is challenging for both theory and modeling. However, synthesis of measurements that capture plant water status, water sources, and water fluxes has the potential to better identify mechanisms and constrain models. To help address this need, we conducted an experimental drydown of potted Populus trichocarpa trees during Summer 2021. During the drydown, we measured sap flow, plant water potentials, leaf gas exchange, meteorological conditions, soil moisture, and the isotopic composition of soil and plant water. We also characterized plant morphology, plant vulnerability to embolism, and soil properties. Through synthesis of the different measurements, we were able to illustrate how relying on individual measurements could have led to incomplete or even incorrect conclusions about mechanisms and plant behavior. Additionally, we used metrics from information theory to identify which measurements offered better constraints on plant behavior and over which time periods multiple measurements are particularly necessary. The manuscript for this work will be submitted in early 2024, but you can check out a talk from AGU 2021 with some initial analyses of the work here.

Role of Vulnerability Segmentation in Plant Function

The model used in this study represents the soil-plant-atmosphere
continuum as a series of variable resistors
Plants exhibit a great diversity in their vulnerability to drought-induced embolism, usually characterized by the P50 value, which corresponds to the water potential at which there is a 50% loss in conductivity. While there is a wide range of P50 values for plant stems, there is also variation in how the P50 of the stem tissue in a plant corresponds with the P50 of the leaf tissue in the same plant, termed vulnerability segmentation. A hypothesis in plant physiology posits that it can be advantageous to plants to have leaves that are more vulnerable to embolism relative to their stems. This allows the leaves to act as a sort of "safety valve" on the hydraulic system of the plant. However, while some plants do exhibit this pattern of vulnerability segmentation, many show now vulnerabliity segmentation and some even exhibit the reverse, having leaves that are more resistant to embolism relative to their stems. In this work, I examined how the presence or absence of hydraulic segmentation, along with other hydraulic characteristics, impact plant function under different environmental conditions. To do this, I am using both measurements of hydraulic vulnerability, as well as a plant hydraulic model to understand the implications of hydraulic segmentation under different scenarios.

Publications

  • Wilkening, J. V., Skelton, R. P., Feng, X., Dawson, T. E., & Thompson, S. E. (2023). Exploring within‐plant hydraulic trait variation: A test of the vulnerability segmentation hypothesis. Plant, Cell & Environment. Manuscript available here and model code available here.

Improving Resiliency of Landscape Rehabilitation in Arid Ecosystems

Plants grown on an engineered soil cover at a site in Western Australia as part of experiment
from which data were used to validate model (Image: Sebastian Lamoureux)
Evapotranspiration (ET) covers, which consist of an engineered soil layer supporting vegetation, are an increasingly popular rehabilitation tool for former mining and landfill sites. They take advantage of plant water uptake to manage the water balance in the soil cover, limiting deep drainage that could potentially mobilize contaminants and waste products from the prior site operations. However, in arid ecosystems there is the potential that the plant water uptake could be hydraulically limited, possibly increasing the risk of contaminant mobilization and mortality of the vegetation. In this work, I am using a plant hydraulic model to optimize the design of these systems while accounting for hydraulic limitation and variable climatic conditions. Initial results from this work were presented at the AGU 2019 Fall Meeting (slides available here) and a manuscript is currently in review.

Role of Hydrologic Mechanisms in Plant Pathogen Spread

Model output showing predicted pathogen spread (light blue shading) from initial observed
patches (light blue line) when accounting for overland transport (left) and without overland
transport (right) as compared to observed spread patterns (dark blue line)
I developed a model to predict the biological growth and transport of the plant pathogen Phytophthora cinnamomi at the landscape scale. Using this model and case studies of disease progression in Western Australia and Spain, I investigated the role of overland runoff as a spread mechanism and how simple hydrological analysis can be used to create more quantitative and spatially-explicit management strategies for disease containment. Model code is available on my Github Page and forcing data is available on Hydroshare.



Publications

  • Wilkening, J. V., Cardillo, E., Abad, E., & Thompson, S.E. (2021). Saturation excess overland flow accelerates the spread of a generalist soil-borne pathogen. Journal of Hydrology, 593, 125821. Available from publisher here or as final, but unformatted preprint here

Biogeochemical Cycling in Salt Marshes

In situ sampling of pore fluids from salt marsh pond
in Norfolk, UK (Image: JV Wilkening)
During my time at the University of Cambridge, I studied interactions of sulfur, iron, and carbon cycling in salt marshes. As part of this work, I looked at seasonal dynamics of biogeochemical cycling and this work was published in coordination with other work from the Turchyn lab in early 2019. I also studied differences in the formation of volatile organosulfur compound formation between sulfidic and ferruginous sedimentary environments and this work was published in late 2019.

Publications

  • Wilkening, J. V., Turchyn, A. V., Redeker, K. R., Mills, J. V., Antler, G., Carrión, O., & Todd, J. D. (2019). The production and fate of volatile organosulfur compounds in sulfidic and ferruginous sediment. Journal of Geophysical Research: Biogeosciences, 124(11), 3390-3402. Available here
  • Hutchings, A.M., Antler, G., Wilkening, J.V., Basu, A., Bradbury, H.J., Clegg, J.A., Gorka, M., Lin, C.Y., Mills, J.V., Pellerin, A., Redeker, K.R., Sun, X., & Turchyn, A.V. (2019). Creek dynamics determine pond subsurface geochemical heterogeneity in East Anglian (UK) salt marshes. Frontiers in Earth Science, 7, 41. Available here