Humicrete in Northwest Florida an Analysis of Formation and Characteristics

The formation process by which sand becomes cemented with humate compounds to form humicrete is not well understood, likely due in part to limited exposures of this material around the world. Humicrete layers along the Intracoastal Waterway in northwest Florida are some of the most well exposed unit...

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Other Authors: Shelfer, Megan L. (Megan Lee) (author)
Format: Others
Language:English
English
Published: Florida State University
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Online Access:http://purl.flvc.org/fsu/fd/2019_Spring_Shelfer_fsu_0071N_15012_comp
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spelling ndltd-fsu.edu-oai-fsu.digital.flvc.org-fsu_7100392019-11-22T03:30:08Z Humicrete in Northwest Florida an Analysis of Formation and Characteristics Shelfer, Megan L. (Megan Lee) (author) Kish, Stephen A. (Professor Directing Thesis) Ray, Peter (Committee Member) Wang, Yanchang (Committee Member) Means, Guy H. (Committee Member) Florida State University (degree granting institution) College of Arts and Sciences (degree granting college) Department of Earth, Ocean and Atmospheric Science (degree granting departmentdgg) Text text master thesis Florida State University English eng 1 online resource (64 pages) computer application/pdf The formation process by which sand becomes cemented with humate compounds to form humicrete is not well understood, likely due in part to limited exposures of this material around the world. Humicrete layers along the Intracoastal Waterway in northwest Florida are some of the most well exposed units in the western hemisphere. Over a length of about ten kilometers, multiple beds with varying humate cementation can be observed throughout the lower two-thirds of bluffs that are nine to fifteen meters high. Dune deposits overlay the humicrete layers. The most prominent humicrete layer is approximately one to two meters thick and can be traced nearly continuously for over a kilometer. These layers were catalogued, photographed, and sampled for this study, in an effort to learn more about their depositional conditions, chemical composition, and the age of the material hosting the humate cementation. Specifically, this project sought to understand whether the organic matter present in the humate layers was transported laterally from nearby areas with high organic accumulation, or leached from overlying peat layers. Samples of disaggregated humate were analyzed via Fourier Transform Infrared (FTIR) spectroscopy and carbon/nitrogen isotopic analysis. The FTIR data produced indicated high concentrations of lignins and hydroxyls, similar to the chemical signature of younger humicrete samples. A table of the individual FTIR data points is included as a supplementary file titled “Appendix B - FTIR.pdf.” Isotopic analysis of these samples yielded δ13C values of -23.6‰ to -26.8‰ and a C/N ratio of 62 to 85, both of which point to terrestrial plants as the originating vegetation. Results of these tests, as well as observation of the current environment along the northwest Florida coastline, suggest that the organic matter found in these humicrete layers was carried laterally by near-surface groundwater from nearby forested swamps. The age of these host layers and the humicrete cementation is believed to be around 115,000-130,000 years old, as they are thought to have formed by interaction with groundwater during the Sangamonian interglacial period. Additional testing, especially with regard to extent, age and nature of movement of organic-rich water, would be helpful in further understanding how humicrete forms. A Thesis submitted to the Department of Earth, Ocean and Atmospheric Science in partial fulfillment of the requirements for the degree of Master of Science. Spring Semester 2019. March 8, 2019. FTIR, humate, humicrete Includes bibliographical references. Stephen Kish, Professor Directing Thesis; Peter Ray, Committee Member; Yang Wang, Committee Member; Guy Means, Committee Member. Geology 2019_Spring_Shelfer_fsu_0071N_15012_comp http://purl.flvc.org/fsu/fd/2019_Spring_Shelfer_fsu_0071N_15012_comp http://diginole.lib.fsu.edu/islandora/object/fsu%3A710039/datastream/TN/view/Humicrete%20in%20Northwest%20Florida%20an%20Analysis%20of%20Formation%20and%20Characteristics.jpg
collection NDLTD
language English
English
format Others
sources NDLTD
topic Geology
spellingShingle Geology
Humicrete in Northwest Florida an Analysis of Formation and Characteristics
description The formation process by which sand becomes cemented with humate compounds to form humicrete is not well understood, likely due in part to limited exposures of this material around the world. Humicrete layers along the Intracoastal Waterway in northwest Florida are some of the most well exposed units in the western hemisphere. Over a length of about ten kilometers, multiple beds with varying humate cementation can be observed throughout the lower two-thirds of bluffs that are nine to fifteen meters high. Dune deposits overlay the humicrete layers. The most prominent humicrete layer is approximately one to two meters thick and can be traced nearly continuously for over a kilometer. These layers were catalogued, photographed, and sampled for this study, in an effort to learn more about their depositional conditions, chemical composition, and the age of the material hosting the humate cementation. Specifically, this project sought to understand whether the organic matter present in the humate layers was transported laterally from nearby areas with high organic accumulation, or leached from overlying peat layers. Samples of disaggregated humate were analyzed via Fourier Transform Infrared (FTIR) spectroscopy and carbon/nitrogen isotopic analysis. The FTIR data produced indicated high concentrations of lignins and hydroxyls, similar to the chemical signature of younger humicrete samples. A table of the individual FTIR data points is included as a supplementary file titled “Appendix B - FTIR.pdf.” Isotopic analysis of these samples yielded δ13C values of -23.6‰ to -26.8‰ and a C/N ratio of 62 to 85, both of which point to terrestrial plants as the originating vegetation. Results of these tests, as well as observation of the current environment along the northwest Florida coastline, suggest that the organic matter found in these humicrete layers was carried laterally by near-surface groundwater from nearby forested swamps. The age of these host layers and the humicrete cementation is believed to be around 115,000-130,000 years old, as they are thought to have formed by interaction with groundwater during the Sangamonian interglacial period. Additional testing, especially with regard to extent, age and nature of movement of organic-rich water, would be helpful in further understanding how humicrete forms. === A Thesis submitted to the Department of Earth, Ocean and Atmospheric Science in partial fulfillment of the requirements for the degree of Master of Science. === Spring Semester 2019. === March 8, 2019. === FTIR, humate, humicrete === Includes bibliographical references. === Stephen Kish, Professor Directing Thesis; Peter Ray, Committee Member; Yang Wang, Committee Member; Guy Means, Committee Member.
author2 Shelfer, Megan L. (Megan Lee) (author)
author_facet Shelfer, Megan L. (Megan Lee) (author)
title Humicrete in Northwest Florida an Analysis of Formation and Characteristics
title_short Humicrete in Northwest Florida an Analysis of Formation and Characteristics
title_full Humicrete in Northwest Florida an Analysis of Formation and Characteristics
title_fullStr Humicrete in Northwest Florida an Analysis of Formation and Characteristics
title_full_unstemmed Humicrete in Northwest Florida an Analysis of Formation and Characteristics
title_sort humicrete in northwest florida an analysis of formation and characteristics
publisher Florida State University
url http://purl.flvc.org/fsu/fd/2019_Spring_Shelfer_fsu_0071N_15012_comp
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