Development of nitrogen cycling in recently deglaciated watersheds
Perturbation of natural environments through anthropogenic nitrogen (N) inputs and climate change significantly alter soil systems. Few pristine environments remain in which to study natural controls on the development of soil N cycling over time and thus increase our understanding of the natural de...
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ftunibirmitheses:oai:etheses.bham.ac.uk:5338 2023-05-15T16:20:42+02:00 Development of nitrogen cycling in recently deglaciated watersheds Malone, Edward Thomas Milner, Alexander (Sandy) Pinay, Gilles nerc 2014-12 application/pdf http://etheses.bham.ac.uk//id/eprint/5338/1.hassmallThumbnailVersion/Malone14PhD.pdf http://etheses.bham.ac.uk//id/eprint/5338/ http://etheses.bham.ac.uk//id/eprint/5338/1/Malone14PhD.pdf English eng http://etheses.bham.ac.uk//id/eprint/5338/1/Malone14PhD.pdf Malone, Edward Thomas (2014). Development of nitrogen cycling in recently deglaciated watersheds. University of Birmingham. Ph.D. GB Physical geography Thesis NonPeerReviewed 2014 ftunibirmitheses 2021-11-15T09:47:06Z Perturbation of natural environments through anthropogenic nitrogen (N) inputs and climate change significantly alter soil systems. Few pristine environments remain in which to study natural controls on the development of soil N cycling over time and thus increase our understanding of the natural development of such mechanisms. This study took place in Glacier Bay National Park and Preserve (GBNP), southeast Alaska. This area presented a unique opportunity to study microbial cycling in near pristine soil systems. Six river catchments were selected for study across a chronosequence of 200 years of primary succession. Within each watershed soil nutrient content and microbial processes where evaluated to determine a time frame for development. Samples were collected from riparian and wider catchment areas in order to investigate the effects of dominant vegetation types and slope steepness. These data were coupled with percent vegetation type generated by analysis of satellite imagery allowing the scaling up of soil variables. A key finding of this research was that vegetation type is the primary influence on nitrogen cycling processes and soil characteristics. With increasing age potential microbial activity increased in particular nitrification, which linked with the low soil NO\(_3\)- indicated a large heterotrophic microbial community in older soils. Thesis glacier Alaska University of Birmingham: eTheses Repository Glacier Bay |
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Open Polar |
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University of Birmingham: eTheses Repository |
op_collection_id |
ftunibirmitheses |
language |
English |
topic |
GB Physical geography |
spellingShingle |
GB Physical geography Malone, Edward Thomas Development of nitrogen cycling in recently deglaciated watersheds |
topic_facet |
GB Physical geography |
description |
Perturbation of natural environments through anthropogenic nitrogen (N) inputs and climate change significantly alter soil systems. Few pristine environments remain in which to study natural controls on the development of soil N cycling over time and thus increase our understanding of the natural development of such mechanisms. This study took place in Glacier Bay National Park and Preserve (GBNP), southeast Alaska. This area presented a unique opportunity to study microbial cycling in near pristine soil systems. Six river catchments were selected for study across a chronosequence of 200 years of primary succession. Within each watershed soil nutrient content and microbial processes where evaluated to determine a time frame for development. Samples were collected from riparian and wider catchment areas in order to investigate the effects of dominant vegetation types and slope steepness. These data were coupled with percent vegetation type generated by analysis of satellite imagery allowing the scaling up of soil variables. A key finding of this research was that vegetation type is the primary influence on nitrogen cycling processes and soil characteristics. With increasing age potential microbial activity increased in particular nitrification, which linked with the low soil NO\(_3\)- indicated a large heterotrophic microbial community in older soils. |
author2 |
Milner, Alexander (Sandy) Pinay, Gilles nerc |
format |
Thesis |
author |
Malone, Edward Thomas |
author_facet |
Malone, Edward Thomas |
author_sort |
Malone, Edward Thomas |
title |
Development of nitrogen cycling in recently deglaciated watersheds |
title_short |
Development of nitrogen cycling in recently deglaciated watersheds |
title_full |
Development of nitrogen cycling in recently deglaciated watersheds |
title_fullStr |
Development of nitrogen cycling in recently deglaciated watersheds |
title_full_unstemmed |
Development of nitrogen cycling in recently deglaciated watersheds |
title_sort |
development of nitrogen cycling in recently deglaciated watersheds |
publishDate |
2014 |
url |
http://etheses.bham.ac.uk//id/eprint/5338/1.hassmallThumbnailVersion/Malone14PhD.pdf http://etheses.bham.ac.uk//id/eprint/5338/ http://etheses.bham.ac.uk//id/eprint/5338/1/Malone14PhD.pdf |
geographic |
Glacier Bay |
geographic_facet |
Glacier Bay |
genre |
glacier Alaska |
genre_facet |
glacier Alaska |
op_relation |
http://etheses.bham.ac.uk//id/eprint/5338/1/Malone14PhD.pdf Malone, Edward Thomas (2014). Development of nitrogen cycling in recently deglaciated watersheds. University of Birmingham. Ph.D. |
_version_ |
1766008671568920576 |