Carbon footprint of terrestrial and coastal enhanced weathering systems for carbon sequestration

One of the solutions to reduce carbon emissions is enhanced weathering (EW) using basalt. EW is defined as the artificial acceleration of the weathering process of silicate-bearing rocks for carbon sequestration. Life cycle carbon footprint analysis is utilized in this study to analyze the potential...

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Main Authors: Hao, Lucian Trinidad, Santos, Patricia Antoinette Andres, Shi, Claudette Bernice Ng
Format: text
Language:English
Published: Animo Repository 2021
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Online Access:https://animorepository.dlsu.edu.ph/etdb_chemeng/13
https://animorepository.dlsu.edu.ph/cgi/viewcontent.cgi?article=1014&context=etdb_chemeng
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Institution: De La Salle University
Language: English
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spelling oai:animorepository.dlsu.edu.ph:etdb_chemeng-10142022-08-25T00:43:00Z Carbon footprint of terrestrial and coastal enhanced weathering systems for carbon sequestration Hao, Lucian Trinidad Santos, Patricia Antoinette Andres Shi, Claudette Bernice Ng One of the solutions to reduce carbon emissions is enhanced weathering (EW) using basalt. EW is defined as the artificial acceleration of the weathering process of silicate-bearing rocks for carbon sequestration. Life cycle carbon footprint analysis is utilized in this study to analyze the potential of EW. This method calculates the greenhouse gas (GHG) emissions produced from quarry, crushing, transportation, application operations, and the extracted carbon dioxide (CO2) from the atmosphere through the chemical reaction of silicates in basalt. These values were used to compute the net carbon dioxide removal (CDR). The net CDR is defined as the stoichiometric CDR from the weathering reactions minus the GHG emissions from all activities in the system. The effect of distance between basalt sources (quarries) and sinks (application site) was found to have a major effect on net CDR. The break-even distance at which net CDR becomes zero was determined for both types of EW. Results showed that coastal EW removes more carbon than terrestrial EW for any given transportation distance. In addition, the gap in net CDR is equivalent to terrestrial EW to coastal EW at a transportation distance of about 180 km. The distance at which net CDR drops to zero for terrestrial and coastal EW are 129 km and 302 km, respectively. Furthermore, representative basalt sources (quarries) and sinks (application site) from the Philippines are shown to illustrate the plausibility of EW for the Philippine setting. The results stayed consistent that coastal EW removes more carbon than terrestrial EW. 2021-11-01T07:00:00Z text application/pdf https://animorepository.dlsu.edu.ph/etdb_chemeng/13 https://animorepository.dlsu.edu.ph/cgi/viewcontent.cgi?article=1014&context=etdb_chemeng Chemical Engineering Bachelor's Theses English Animo Repository Carbon sequestration Weathering Chemical Engineering
institution De La Salle University
building De La Salle University Library
continent Asia
country Philippines
Philippines
content_provider De La Salle University Library
collection DLSU Institutional Repository
language English
topic Carbon sequestration
Weathering
Chemical Engineering
spellingShingle Carbon sequestration
Weathering
Chemical Engineering
Hao, Lucian Trinidad
Santos, Patricia Antoinette Andres
Shi, Claudette Bernice Ng
Carbon footprint of terrestrial and coastal enhanced weathering systems for carbon sequestration
description One of the solutions to reduce carbon emissions is enhanced weathering (EW) using basalt. EW is defined as the artificial acceleration of the weathering process of silicate-bearing rocks for carbon sequestration. Life cycle carbon footprint analysis is utilized in this study to analyze the potential of EW. This method calculates the greenhouse gas (GHG) emissions produced from quarry, crushing, transportation, application operations, and the extracted carbon dioxide (CO2) from the atmosphere through the chemical reaction of silicates in basalt. These values were used to compute the net carbon dioxide removal (CDR). The net CDR is defined as the stoichiometric CDR from the weathering reactions minus the GHG emissions from all activities in the system. The effect of distance between basalt sources (quarries) and sinks (application site) was found to have a major effect on net CDR. The break-even distance at which net CDR becomes zero was determined for both types of EW. Results showed that coastal EW removes more carbon than terrestrial EW for any given transportation distance. In addition, the gap in net CDR is equivalent to terrestrial EW to coastal EW at a transportation distance of about 180 km. The distance at which net CDR drops to zero for terrestrial and coastal EW are 129 km and 302 km, respectively. Furthermore, representative basalt sources (quarries) and sinks (application site) from the Philippines are shown to illustrate the plausibility of EW for the Philippine setting. The results stayed consistent that coastal EW removes more carbon than terrestrial EW.
format text
author Hao, Lucian Trinidad
Santos, Patricia Antoinette Andres
Shi, Claudette Bernice Ng
author_facet Hao, Lucian Trinidad
Santos, Patricia Antoinette Andres
Shi, Claudette Bernice Ng
author_sort Hao, Lucian Trinidad
title Carbon footprint of terrestrial and coastal enhanced weathering systems for carbon sequestration
title_short Carbon footprint of terrestrial and coastal enhanced weathering systems for carbon sequestration
title_full Carbon footprint of terrestrial and coastal enhanced weathering systems for carbon sequestration
title_fullStr Carbon footprint of terrestrial and coastal enhanced weathering systems for carbon sequestration
title_full_unstemmed Carbon footprint of terrestrial and coastal enhanced weathering systems for carbon sequestration
title_sort carbon footprint of terrestrial and coastal enhanced weathering systems for carbon sequestration
publisher Animo Repository
publishDate 2021
url https://animorepository.dlsu.edu.ph/etdb_chemeng/13
https://animorepository.dlsu.edu.ph/cgi/viewcontent.cgi?article=1014&context=etdb_chemeng
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