Spatial Distribution of Visible Desert Salts in the McMurdo Region, Antarctica
Desert environments are distinctive in that they are the only landscapes that accumulate salts in measureable quantities. The McMurdo Dry Valleys in Antarctica are classified as a polar desert, as they maintain very low relative humidities by the sweeping katabatic winds that descend upon the contin...
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ftohiostateu:oai:kb.osu.edu:1811/54728 2023-05-15T13:37:41+02:00 Spatial Distribution of Visible Desert Salts in the McMurdo Region, Antarctica Bisson, Kelsey Lyons, Berry 2013-05 application/pdf http://hdl.handle.net/1811/54728 en_US eng The Ohio State University The Ohio State University. School of Earth Sciences Honors Theses; 2013 http://hdl.handle.net/1811/54728 Attribution-NonCommercial-NoDerivs 3.0 United States http://creativecommons.org/licenses/by-nc-nd/3.0/us/ CC-BY-NC-ND Antarctica geochemistry salt environmental polar science Thesis 2013 ftohiostateu 2020-08-22T19:17:17Z Desert environments are distinctive in that they are the only landscapes that accumulate salts in measureable quantities. The McMurdo Dry Valleys in Antarctica are classified as a polar desert, as they maintain very low relative humidities by the sweeping katabatic winds that descend upon the continent and produce very little (<3cm annual) precipitation. Salts are abundant and a notable feature of the soils. Surficial salt crusts were sampled in the top 2 cm of soils in the Dry Valleys and on Ross Island in the area surrounding McMurdo Station to determine their source for formation, as well as to identify spatial trends in the data. Unlike previous salt studies, this one focuses on visible, surface salt crusts with soil depth possibly through sequential evaporation of groundwater as it moves to the surface. Using structural and textural criteria, 2 types of salt crusts may be distinguished: (1) widespread surface crusts with little structure; and (2) thicker salt crusts with amorphous shape that form near boulders. Subsurface soluble salts and stratified salt crusts were not sampled in this study. Chemical analysis of the major ions indicates conflicting trends in major marine ions, suggesting that the marine influence in salt formation is not as significant as was hypothesized. Sodium is the major cation, averaging 70-90% of all major cations measured. Chloride and sulfate are the major anions in the salts, with chloride being the most abundant (<70%) in Taylor Valley surface salts, though it is less abundant at McMurdo station. Higher elevation coastal areas have abundant calcium, up to 60 meq/kg sediment sampled. Statistical analysis reveals that salt chemistries are not significantly different with respect to their sampling elevation, location, and proximity to a water source. Qualitative comparisons of salt chemistries show an influence of formation “type,” as salts accumulated under large particle faces are chemically distinct from those that were found alongside streambeds. NSF ANT 1115245 No embargo Academic Major: Earth Sciences Thesis Antarc* Antarctica McMurdo Dry Valleys polar desert Ross Island Ohio State University (OSU): Knowledge Bank McMurdo Dry Valleys McMurdo Station ENVELOPE(166.667,166.667,-77.850,-77.850) Ross Island Taylor Valley ENVELOPE(163.000,163.000,-77.617,-77.617) |
institution |
Open Polar |
collection |
Ohio State University (OSU): Knowledge Bank |
op_collection_id |
ftohiostateu |
language |
English |
topic |
Antarctica geochemistry salt environmental polar science |
spellingShingle |
Antarctica geochemistry salt environmental polar science Bisson, Kelsey Spatial Distribution of Visible Desert Salts in the McMurdo Region, Antarctica |
topic_facet |
Antarctica geochemistry salt environmental polar science |
description |
Desert environments are distinctive in that they are the only landscapes that accumulate salts in measureable quantities. The McMurdo Dry Valleys in Antarctica are classified as a polar desert, as they maintain very low relative humidities by the sweeping katabatic winds that descend upon the continent and produce very little (<3cm annual) precipitation. Salts are abundant and a notable feature of the soils. Surficial salt crusts were sampled in the top 2 cm of soils in the Dry Valleys and on Ross Island in the area surrounding McMurdo Station to determine their source for formation, as well as to identify spatial trends in the data. Unlike previous salt studies, this one focuses on visible, surface salt crusts with soil depth possibly through sequential evaporation of groundwater as it moves to the surface. Using structural and textural criteria, 2 types of salt crusts may be distinguished: (1) widespread surface crusts with little structure; and (2) thicker salt crusts with amorphous shape that form near boulders. Subsurface soluble salts and stratified salt crusts were not sampled in this study. Chemical analysis of the major ions indicates conflicting trends in major marine ions, suggesting that the marine influence in salt formation is not as significant as was hypothesized. Sodium is the major cation, averaging 70-90% of all major cations measured. Chloride and sulfate are the major anions in the salts, with chloride being the most abundant (<70%) in Taylor Valley surface salts, though it is less abundant at McMurdo station. Higher elevation coastal areas have abundant calcium, up to 60 meq/kg sediment sampled. Statistical analysis reveals that salt chemistries are not significantly different with respect to their sampling elevation, location, and proximity to a water source. Qualitative comparisons of salt chemistries show an influence of formation “type,” as salts accumulated under large particle faces are chemically distinct from those that were found alongside streambeds. NSF ANT 1115245 No embargo Academic Major: Earth Sciences |
author2 |
Lyons, Berry |
format |
Thesis |
author |
Bisson, Kelsey |
author_facet |
Bisson, Kelsey |
author_sort |
Bisson, Kelsey |
title |
Spatial Distribution of Visible Desert Salts in the McMurdo Region, Antarctica |
title_short |
Spatial Distribution of Visible Desert Salts in the McMurdo Region, Antarctica |
title_full |
Spatial Distribution of Visible Desert Salts in the McMurdo Region, Antarctica |
title_fullStr |
Spatial Distribution of Visible Desert Salts in the McMurdo Region, Antarctica |
title_full_unstemmed |
Spatial Distribution of Visible Desert Salts in the McMurdo Region, Antarctica |
title_sort |
spatial distribution of visible desert salts in the mcmurdo region, antarctica |
publisher |
The Ohio State University |
publishDate |
2013 |
url |
http://hdl.handle.net/1811/54728 |
long_lat |
ENVELOPE(166.667,166.667,-77.850,-77.850) ENVELOPE(163.000,163.000,-77.617,-77.617) |
geographic |
McMurdo Dry Valleys McMurdo Station Ross Island Taylor Valley |
geographic_facet |
McMurdo Dry Valleys McMurdo Station Ross Island Taylor Valley |
genre |
Antarc* Antarctica McMurdo Dry Valleys polar desert Ross Island |
genre_facet |
Antarc* Antarctica McMurdo Dry Valleys polar desert Ross Island |
op_relation |
The Ohio State University. School of Earth Sciences Honors Theses; 2013 http://hdl.handle.net/1811/54728 |
op_rights |
Attribution-NonCommercial-NoDerivs 3.0 United States http://creativecommons.org/licenses/by-nc-nd/3.0/us/ |
op_rightsnorm |
CC-BY-NC-ND |
_version_ |
1766096525943898112 |