Controls on soil development and carbon storage on the high-standing island of Taiwan

3rd place at the Denman Undergraduate Research Forum and Sigma Gamma Epsilon’s Austin A. Sartin Award at GSA Studies on weathering rates of high standing islands (HSIs) have shown high observed rates of chemical weathering. However, attempts to correlate these rates to sources have often suffered du...

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Main Author: Von Bargen, Justin
Other Authors: Carey, Anne
Format: Thesis
Language:English
Published: The Ohio State University 2010
Subjects:
Online Access:http://hdl.handle.net/1811/51802
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spelling ftohiostateu:oai:kb.osu.edu:1811/51802 2023-05-15T15:47:39+02:00 Controls on soil development and carbon storage on the high-standing island of Taiwan Von Bargen, Justin Carey, Anne 2010-12 application/pdf http://hdl.handle.net/1811/51802 en_US eng The Ohio State University The Ohio State University. School of Earth Sciences Honors Theses; 2010 http://hdl.handle.net/1811/51802 erosion uplift weathering soil development Thesis 2010 ftohiostateu 2020-08-22T19:24:41Z 3rd place at the Denman Undergraduate Research Forum and Sigma Gamma Epsilon’s Austin A. Sartin Award at GSA Studies on weathering rates of high standing islands (HSIs) have shown high observed rates of chemical weathering. However, attempts to correlate these rates to sources have often suffered due to a lack of sufficient soil geochemical data. Furthermore, few studies have attempted to determine a relationship between soil organic carbon content, storage, and seq uestration with uplift and erosion rates. Taiwan sits on top of a highly active convergent plate boundary between the Eurasian and Philippine Sea Plate, which results in intense uplift, creating the orogenic mountains that make up the island. The plate margin has uplift rates >10 mm/yr and contains erosional features dominated by mass-wasting. The island also contains three of the nine rivers in the world which have average sediment concentrations >10 g/l (Milliman and Syvitski, 1992). This study determined organic carbon, inorganic carbon, and a relative amount of weathering in soils between three locations on Taiwan with different lithology and seismicity and with various rates of uplift, runoff, and erosion. Soils exhibited relatively higher concentrations of organic carbon and more developed soil profiles in areas where these erosional factors play a limited role. The Ohio State University School of Earth Sciences The Ohio State University Byrd Polar Research Center The Ohio State University Undergraduate Student Government The Ohio State University Denman Undergraduate Research Forum Friends of Orton Hall McKenzie Scholarship Sigma Gamma Epsilon A one-year embargo was granted for this item. Thesis Byrd Polar Research Byrd Polar Research Center Ohio State University (OSU): Knowledge Bank Austin Byrd
institution Open Polar
collection Ohio State University (OSU): Knowledge Bank
op_collection_id ftohiostateu
language English
topic erosion
uplift
weathering
soil development
spellingShingle erosion
uplift
weathering
soil development
Von Bargen, Justin
Controls on soil development and carbon storage on the high-standing island of Taiwan
topic_facet erosion
uplift
weathering
soil development
description 3rd place at the Denman Undergraduate Research Forum and Sigma Gamma Epsilon’s Austin A. Sartin Award at GSA Studies on weathering rates of high standing islands (HSIs) have shown high observed rates of chemical weathering. However, attempts to correlate these rates to sources have often suffered due to a lack of sufficient soil geochemical data. Furthermore, few studies have attempted to determine a relationship between soil organic carbon content, storage, and seq uestration with uplift and erosion rates. Taiwan sits on top of a highly active convergent plate boundary between the Eurasian and Philippine Sea Plate, which results in intense uplift, creating the orogenic mountains that make up the island. The plate margin has uplift rates >10 mm/yr and contains erosional features dominated by mass-wasting. The island also contains three of the nine rivers in the world which have average sediment concentrations >10 g/l (Milliman and Syvitski, 1992). This study determined organic carbon, inorganic carbon, and a relative amount of weathering in soils between three locations on Taiwan with different lithology and seismicity and with various rates of uplift, runoff, and erosion. Soils exhibited relatively higher concentrations of organic carbon and more developed soil profiles in areas where these erosional factors play a limited role. The Ohio State University School of Earth Sciences The Ohio State University Byrd Polar Research Center The Ohio State University Undergraduate Student Government The Ohio State University Denman Undergraduate Research Forum Friends of Orton Hall McKenzie Scholarship Sigma Gamma Epsilon A one-year embargo was granted for this item.
author2 Carey, Anne
format Thesis
author Von Bargen, Justin
author_facet Von Bargen, Justin
author_sort Von Bargen, Justin
title Controls on soil development and carbon storage on the high-standing island of Taiwan
title_short Controls on soil development and carbon storage on the high-standing island of Taiwan
title_full Controls on soil development and carbon storage on the high-standing island of Taiwan
title_fullStr Controls on soil development and carbon storage on the high-standing island of Taiwan
title_full_unstemmed Controls on soil development and carbon storage on the high-standing island of Taiwan
title_sort controls on soil development and carbon storage on the high-standing island of taiwan
publisher The Ohio State University
publishDate 2010
url http://hdl.handle.net/1811/51802
geographic Austin
Byrd
geographic_facet Austin
Byrd
genre Byrd Polar Research
Byrd Polar Research Center
genre_facet Byrd Polar Research
Byrd Polar Research Center
op_relation The Ohio State University. School of Earth Sciences Honors Theses; 2010
http://hdl.handle.net/1811/51802
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