The drivers of freshwater reservoir biogeochemical cycling and greenhouse gas emissions in a changing world
| dc.contributor.author | McClure, Ryan Paul | en |
| dc.contributor.committeechair | Carey, Cayelan C. | en |
| dc.contributor.committeemember | Hanson, Paul C. | en |
| dc.contributor.committeemember | Hotchkiss, Erin R. | en |
| dc.contributor.committeemember | Barrett, John E. | en |
| dc.contributor.committeemember | Schreiber, Madeline E. | en |
| dc.contributor.department | Biological Sciences | en |
| dc.date.accessioned | 2022-03-24T06:00:12Z | en |
| dc.date.available | 2022-03-24T06:00:12Z | en |
| dc.date.issued | 2020-09-29 | en |
| dc.description.abstract | Freshwater reservoirs store, process, and emit to the atmosphere large quantities of carbon (C). Despite the important role of reservoirs in the global carbon cycle, it remains unknown how human activities are altering their carbon cycling. Climate change and land use are resulting in lower dissolved oxygen (DO) concentrations in freshwater ecosystems, yet more frequent, powerful storms are occurring that temporarily increase DO availability. The net effect of these opposing forces results in anoxia (DO < 0.5 mg L-1) punctuated by short-term increases in DO. The availability of DO controls alternate redox reactions in freshwaters, thereby determining the rate and end products of organic C mineralization, which include two greenhouse gases, carbon dioxide (CO2) and methane (CH4). I performed ecosystem-level DO manipulations and evaluated how changing DO conditions affected redox reactions and the production and emission of CO2 and CH4. I also explored how the magnitude and drivers of CH4 emissions changed spatio-temporarily in a eutrophic reservoir using time series models. Finally, I used a coupled data-modeling approach to forecast future emissions of CH4 from the same reservoir. I found that the depletion of DO results in the rapid onset of alternate redox reactions in freshwater reservoirs for organic C mineralization and greater production of CH4. When the anoxia occurred in the water column (vs. at the sediments), diffusive CO2 and CH4 efflux phenology was affected, and resulted in degassing occurring during storms before fall turnover. I observed that the magnitude of CH4 emissions varied along a longitudinal gradient of a small reservoir and that the environmental drivers of ebullition and diffusion can change substantially both over space (within one hundred meters) and time (within a few weeks). Finally, I developed a forecasting workflow that successfully predicted future CH4 ebullition rates during one summer season. My research provides insight to how changing DO conditions will alter redox reactions in the water column and greenhouse gas emissions, as well as provides a new technique for improving future predictions of CH4 emissions from freshwater reservoirs. Althogether, this work improves our understanding of how freshwater lake and reservoir carbon cycling will change in the future. | en |
| dc.description.abstractgeneral | Freshwater reservoirs store a lot of carbon in their sediments and emit a lot of carbon as greenhouse gases (carbon dioxide and methane) to the atmosphere. However, climate change, land use, and water quality management can change the chemical reactions that are responsible for the production of carbon dioxide and methane, which could have substantial effects on the global carbon budget. Here, I manipulated the oxygen conditions of a freshwater reservoir and monitored the chemistry and greenhouse gas emissions in the experimental reservoir relative to an upstream reference reservoir. I then estimated the methane emissions from the reservoir to understand how the chemistry and greenhouse gas emissions in freshwater reservoirs may change in the future. I found that reservoir oxygen availability controls the magnitude and timing of the chemical reactions that produce carbon dioxide and methane, which in turn alters greenhouse gas emissions. Additionally, I developed models that showed how the magnitude and drivers of methane emissions changed within a small reservoir over time. Finally, I was able to predict the timing and magnitude of methane bubbling from the sediments. Altogether, this work provides evidence how climate change, land use change, and water quality management will affect future water chemistry and greenhouse gas emissions from reservoirs. | en |
| dc.description.degree | Doctor of Philosophy | en |
| dc.format.medium | ETD | en |
| dc.identifier.other | vt_gsexam:27467 | en |
| dc.identifier.uri | http://hdl.handle.net/10919/109436 | en |
| dc.publisher | Virginia Tech | en |
| dc.rights | In Copyright | en |
| dc.rights.uri | http://rightsstatements.org/vocab/InC/1.0/ | en |
| dc.subject | biogeochemistry | en |
| dc.subject | carbon dioxide | en |
| dc.subject | climate change | en |
| dc.subject | dissolved oxygen | en |
| dc.subject | ecological forecasting | en |
| dc.subject | ecosystem ecology | en |
| dc.subject | ebullition | en |
| dc.subject | global change | en |
| dc.subject | methane | en |
| dc.subject | reservoir management | en |
| dc.title | The drivers of freshwater reservoir biogeochemical cycling and greenhouse gas emissions in a changing world | en |
| dc.type | Dissertation | en |
| thesis.degree.discipline | Biological Sciences | en |
| thesis.degree.grantor | Virginia Polytechnic Institute and State University | en |
| thesis.degree.level | doctoral | en |
| thesis.degree.name | Doctor of Philosophy | en |