Spatial and Temporal Variability of In-Stream Functioning within a Forested, Headwater Piedmont Watershed

As anthropogenic nutrient loads threaten the health of the Chesapeake Bay, lotic processes throughout its headwaters may buffer increased nitrogen inputs by converting them to stable forms, ultimately through denitrification to N2 gas. However, the temporal environmental factors controlling baseflow...

Full description

Bibliographic Details
Main Author: Wildfire, Luke Ethan
Other Authors: Biological Systems Engineering
Format: Others
Published: Virginia Tech 2018
Subjects:
Online Access:http://hdl.handle.net/10919/86443
id ndltd-VTETD-oai-vtechworks.lib.vt.edu-10919-86443
record_format oai_dc
spelling ndltd-VTETD-oai-vtechworks.lib.vt.edu-10919-864432021-08-12T05:27:18Z Spatial and Temporal Variability of In-Stream Functioning within a Forested, Headwater Piedmont Watershed Wildfire, Luke Ethan Biological Systems Engineering Scott, Durelle T. Hession, W. Cully McGuire, Kevin J. Dissolved organic matter in-stream metabolism ammonium uptake Piedmont As anthropogenic nutrient loads threaten the health of the Chesapeake Bay, lotic processes throughout its headwaters may buffer increased nitrogen inputs by converting them to stable forms, ultimately through denitrification to N2 gas. However, the temporal environmental factors controlling baseflow nitrogen retention are poorly understood, particularly temperature, shading, and dissolved organic matter dynamics. This study therefore attempts to elucidate the effects of these environmental variables on nitrogen cycling within the Fair Hill Natural Resources Management Area (Fair Hill), a forested watershed within the Piedmont physiographic province of the Chesapeake Bay. As expected, groundwater and allochthonous organic matter inputs set the foundation for lotic biogeochemistry at Fair Hill, creating a nutrient-limited, heterotrophic reach. Within this setting, three temporal "hot-moments" of in-stream nutrient processing were observed: the release of ammonium and phosphate during the warm - but shaded - growing season; nitrate uptake during autumnal leaf-fall; and a unique spike of nitrate uptake and respiration-induced degradation of labile organic matter during a drought. Consequently, the baseflow capacity of this headwater stream to buffer nutrient exports to the Chesapeake Bay constantly varies throughout the year in response to light availability, temperature, and in-stream organic matter dynamics. Master of Science 2018-12-19T07:01:08Z 2018-12-19T07:01:08Z 2017-06-26 Thesis vt_gsexam:1984 http://hdl.handle.net/10919/86443 In Copyright http://rightsstatements.org/vocab/InC/1.0/ ETD application/pdf Virginia Tech
collection NDLTD
format Others
sources NDLTD
topic Dissolved organic matter
in-stream metabolism
ammonium uptake
Piedmont
spellingShingle Dissolved organic matter
in-stream metabolism
ammonium uptake
Piedmont
Wildfire, Luke Ethan
Spatial and Temporal Variability of In-Stream Functioning within a Forested, Headwater Piedmont Watershed
description As anthropogenic nutrient loads threaten the health of the Chesapeake Bay, lotic processes throughout its headwaters may buffer increased nitrogen inputs by converting them to stable forms, ultimately through denitrification to N2 gas. However, the temporal environmental factors controlling baseflow nitrogen retention are poorly understood, particularly temperature, shading, and dissolved organic matter dynamics. This study therefore attempts to elucidate the effects of these environmental variables on nitrogen cycling within the Fair Hill Natural Resources Management Area (Fair Hill), a forested watershed within the Piedmont physiographic province of the Chesapeake Bay. As expected, groundwater and allochthonous organic matter inputs set the foundation for lotic biogeochemistry at Fair Hill, creating a nutrient-limited, heterotrophic reach. Within this setting, three temporal "hot-moments" of in-stream nutrient processing were observed: the release of ammonium and phosphate during the warm - but shaded - growing season; nitrate uptake during autumnal leaf-fall; and a unique spike of nitrate uptake and respiration-induced degradation of labile organic matter during a drought. Consequently, the baseflow capacity of this headwater stream to buffer nutrient exports to the Chesapeake Bay constantly varies throughout the year in response to light availability, temperature, and in-stream organic matter dynamics. === Master of Science
author2 Biological Systems Engineering
author_facet Biological Systems Engineering
Wildfire, Luke Ethan
author Wildfire, Luke Ethan
author_sort Wildfire, Luke Ethan
title Spatial and Temporal Variability of In-Stream Functioning within a Forested, Headwater Piedmont Watershed
title_short Spatial and Temporal Variability of In-Stream Functioning within a Forested, Headwater Piedmont Watershed
title_full Spatial and Temporal Variability of In-Stream Functioning within a Forested, Headwater Piedmont Watershed
title_fullStr Spatial and Temporal Variability of In-Stream Functioning within a Forested, Headwater Piedmont Watershed
title_full_unstemmed Spatial and Temporal Variability of In-Stream Functioning within a Forested, Headwater Piedmont Watershed
title_sort spatial and temporal variability of in-stream functioning within a forested, headwater piedmont watershed
publisher Virginia Tech
publishDate 2018
url http://hdl.handle.net/10919/86443
work_keys_str_mv AT wildfirelukeethan spatialandtemporalvariabilityofinstreamfunctioningwithinaforestedheadwaterpiedmontwatershed
_version_ 1719459788421595136