Constraining alkalinity sources to a secondary bay in South Texas

A thesis Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE in ENVIRONMENTAL SCIENCE from Texas A&M University-Corpus Christi in Corpus Christi, Texas. Submarine groundwater discharge (SGD) is an important pathway for solute transfer from land to sea. With r...

Full description

Bibliographic Details
Main Author: Trevino, Melissa
Other Authors: Murgulet, Dorina
Format: Thesis
Language:English
Published: 2016
Subjects:
Online Access:http://hdl.handle.net/1969.6/694
id fttexasamucorpus:oai:tamucc-ir.tdl.org:1969.6/694
record_format openpolar
spelling fttexasamucorpus:oai:tamucc-ir.tdl.org:1969.6/694 2023-10-25T01:42:30+02:00 Constraining alkalinity sources to a secondary bay in South Texas Trevino, Melissa Murgulet, Dorina 2016-08 application/pdf http://hdl.handle.net/1969.6/694 en_US eng http://hdl.handle.net/1969.6/694 This material is made available for use in research, teaching, and private study, pursuant to U.S. Copyright law. The user assumes full responsibility for any use of the materials, including but not limited to, infringement of copyright and publication rights of reproduced materials. Any materials used should be fully credited with its source. All rights are reserved and retained regardless of current or future development or laws that may apply to fair use standards. Permission for publication of this material, in part or in full, must be secured with the author and/or publisher. Alkalinity Alkalinity constraints Carbonate Flooding Secondary Bay submarine groundwater discharge Text Thesis 2016 fttexasamucorpus 2023-09-25T10:23:24Z A thesis Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE in ENVIRONMENTAL SCIENCE from Texas A&M University-Corpus Christi in Corpus Christi, Texas. Submarine groundwater discharge (SGD) is an important pathway for solute transfer from land to sea. With recent atmospheric carbon dioxide (CO2) increase, global concerns over oceanic and estuarine acidification have ascended. To better understand the natural ability of estuaries to buffer decreasing pH levels and assist in ocean acidification mitigation studies, overlooked sources of total alkalinity (TA) need to be considered. This study investigates TA changes in Nueces Bay (a secondary bay adjacent to Corpus Christi Bay in the Gulf of Mexico), at scales spanning from hours to seasonal, by incorporating submarine groundwater discharge (SGD) rates. TA concentrations within the bay fluctuated from December 2014 to December 2015 (December, 2014: 2527.6 µM; March, 2015: 2341.0 µM; June, 2015: 2765.1 µM; September, 2015: 2869.8 µM; December, 2015: 2638.6 µM). These observed changes in TA among the sampling events were mostly affected by different rates of SGD and biogeochemical reactions, while discharge from Nueces River was only important after significant rain events and flooding (June 2015), increasing the average TA (March, 2015: 2341.0 µM to June, 2015: 2765.1 µM) of the bay. Dry periods (March 2015) indicated consumption of DIC in the form of calcification may occur at some locations. SGD rates are the highest during the dry seasons (March 2015: 9.2 · 10-1 m3/d), thus there is an increased export of TA from groundwater. SGD, also has a lag effect post flooding (September-2015 to December-2015), as discharge at the shoreline increased (north shoreline of the Nueces Bay: 6.5 · 10-1 to 9.0 · 10-1 m3/d; south shoreline: 4.5 · 10-1 to 8.8 · 10-1 m3/d) and elevated SGD-derived TA input. Under unimpaired conditions, Nueces River would likely have a significant role on the bay’s alkalinity given the high groundwater ... Thesis Ocean acidification Texas A&M University - Corpus Christi: DSpace Repository
institution Open Polar
collection Texas A&M University - Corpus Christi: DSpace Repository
op_collection_id fttexasamucorpus
language English
topic Alkalinity
Alkalinity constraints
Carbonate
Flooding
Secondary Bay
submarine groundwater discharge
spellingShingle Alkalinity
Alkalinity constraints
Carbonate
Flooding
Secondary Bay
submarine groundwater discharge
Trevino, Melissa
Constraining alkalinity sources to a secondary bay in South Texas
topic_facet Alkalinity
Alkalinity constraints
Carbonate
Flooding
Secondary Bay
submarine groundwater discharge
description A thesis Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE in ENVIRONMENTAL SCIENCE from Texas A&M University-Corpus Christi in Corpus Christi, Texas. Submarine groundwater discharge (SGD) is an important pathway for solute transfer from land to sea. With recent atmospheric carbon dioxide (CO2) increase, global concerns over oceanic and estuarine acidification have ascended. To better understand the natural ability of estuaries to buffer decreasing pH levels and assist in ocean acidification mitigation studies, overlooked sources of total alkalinity (TA) need to be considered. This study investigates TA changes in Nueces Bay (a secondary bay adjacent to Corpus Christi Bay in the Gulf of Mexico), at scales spanning from hours to seasonal, by incorporating submarine groundwater discharge (SGD) rates. TA concentrations within the bay fluctuated from December 2014 to December 2015 (December, 2014: 2527.6 µM; March, 2015: 2341.0 µM; June, 2015: 2765.1 µM; September, 2015: 2869.8 µM; December, 2015: 2638.6 µM). These observed changes in TA among the sampling events were mostly affected by different rates of SGD and biogeochemical reactions, while discharge from Nueces River was only important after significant rain events and flooding (June 2015), increasing the average TA (March, 2015: 2341.0 µM to June, 2015: 2765.1 µM) of the bay. Dry periods (March 2015) indicated consumption of DIC in the form of calcification may occur at some locations. SGD rates are the highest during the dry seasons (March 2015: 9.2 · 10-1 m3/d), thus there is an increased export of TA from groundwater. SGD, also has a lag effect post flooding (September-2015 to December-2015), as discharge at the shoreline increased (north shoreline of the Nueces Bay: 6.5 · 10-1 to 9.0 · 10-1 m3/d; south shoreline: 4.5 · 10-1 to 8.8 · 10-1 m3/d) and elevated SGD-derived TA input. Under unimpaired conditions, Nueces River would likely have a significant role on the bay’s alkalinity given the high groundwater ...
author2 Murgulet, Dorina
format Thesis
author Trevino, Melissa
author_facet Trevino, Melissa
author_sort Trevino, Melissa
title Constraining alkalinity sources to a secondary bay in South Texas
title_short Constraining alkalinity sources to a secondary bay in South Texas
title_full Constraining alkalinity sources to a secondary bay in South Texas
title_fullStr Constraining alkalinity sources to a secondary bay in South Texas
title_full_unstemmed Constraining alkalinity sources to a secondary bay in South Texas
title_sort constraining alkalinity sources to a secondary bay in south texas
publishDate 2016
url http://hdl.handle.net/1969.6/694
genre Ocean acidification
genre_facet Ocean acidification
op_relation http://hdl.handle.net/1969.6/694
op_rights This material is made available for use in research, teaching, and private study, pursuant to U.S. Copyright law. The user assumes full responsibility for any use of the materials, including but not limited to, infringement of copyright and publication rights of reproduced materials. Any materials used should be fully credited with its source. All rights are reserved and retained regardless of current or future development or laws that may apply to fair use standards. Permission for publication of this material, in part or in full, must be secured with the author and/or publisher.
_version_ 1780739112356020224