Title:
Influence of linked hydrologic and geomorphic processes on the terrestrial carbon cycle

dc.contributor.advisor Bras, Rafael L.
dc.contributor.author Dialynas, Ioannis Minas
dc.contributor.committeeMember Georgakakos, Aris P.
dc.contributor.committeeMember Wang, Jingfeng
dc.contributor.committeeMember Richter, Daniel D.
dc.contributor.committeeMember Nenes, Athanasios
dc.contributor.department Civil and Environmental Engineering
dc.date.accessioned 2017-06-07T17:39:40Z
dc.date.available 2017-06-07T17:39:40Z
dc.date.created 2017-05
dc.date.issued 2017-01-19
dc.date.submitted May 2017
dc.date.updated 2017-06-07T17:39:41Z
dc.description.abstract Soil erosion driven by hydro-climatic factors and anthropogenic activity is closely linked to the global carbon (C) cycle. Elucidating complex interrelations between climate, vegetation, soils, and human impacts is critical for advancing our understanding on how diverse ecosystems respond to global environmental change. This work introduces a spatially-explicit process-based model of soil organic C dynamics (Triangulated Irregular Network-based Real-time Integrated Basin Simulator-Erosion and Carbon Oxidation), developed within with an existing coupled physically-based hydro-geomorphic model, to quantify the influence of linked hydrologic and geomorphic processes on the C cycle in a range of ecosystems. Two sites are studied: the Calhoun Critical Zone Observatory (CZO) in South Carolina, USA, which has experienced some of the most serious agricultural soil erosion in North America, and the Luquillo CZO (Puerto Rico), a tropical site of particular hydro-geomorphological interest. This study uses multiple observations of hydrologic and geomorphic processes and soil biogeochemical properties. The substantial topographic variability in the redistribution of soil organic C in agricultural landscapes as soil erosion and deposition proceed is highlighted. The uncertainty characterizing estimates of the hydrologically driven CO2 exchange with the atmosphere in intensively managed landscapes is significant. In the Luquillo CZO, the capacity of contrasting tropical landscapes to act as a net atmospheric C source or a C sink in response to hydro-climatic perturbations is demonstrated. This work highlights that the natural spatial variation of soil hydrological and geotechnical properties greatly influences slope instability in tropical watersheds. Also, as shown, hillslope erosion and landslide occurrence in the Luquillo CZO are expected to remain significant in the 21st century, despite a projected precipitation decline in south Caribbean. It is recommended that future studies assessing the contribution of erosion on atmospheric CO2, and the response of diverse landscapes to natural and anthropogenic perturbations systematically account for the fine spatio-temporal variability of linked hydro-climatic, geomorphological, and biogeochemical processes at a range of settings.
dc.description.degree Ph.D.
dc.format.mimetype application/pdf
dc.identifier.uri http://hdl.handle.net/1853/58233
dc.language.iso en_US
dc.publisher Georgia Institute of Technology
dc.subject Soil organic carbon
dc.subject Atmospheric CO2
dc.subject tRIBS
dc.subject Spatially explicit model
dc.subject Carbon replacement
dc.subject tRIBS-ECO
dc.subject Erosion
dc.subject Tropical forests
dc.subject Landscape
dc.subject Coupled processes
dc.subject Rainfall
dc.subject Distributed hydrologic modeling
dc.subject Parameters uncertainty
dc.subject Probability of failure
dc.subject Puerto Rico
dc.subject Landslides
dc.subject Climate change
dc.subject Critical zone
dc.subject Tropical watersheds
dc.subject Contrasting lithology
dc.title Influence of linked hydrologic and geomorphic processes on the terrestrial carbon cycle
dc.type Text
dc.type.genre Dissertation
dspace.entity.type Publication
local.contributor.advisor Bras, Rafael L.
local.contributor.corporatename School of Civil and Environmental Engineering
local.contributor.corporatename College of Engineering
relation.isAdvisorOfPublication 64e45b8f-3df1-4e41-84d2-0cd91b9a0d61
relation.isOrgUnitOfPublication 88639fad-d3ae-4867-9e7a-7c9e6d2ecc7c
relation.isOrgUnitOfPublication 7c022d60-21d5-497c-b552-95e489a06569
thesis.degree.level Doctoral
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