Geoelectrical classification of Gypsum Rocks
Abstract Gypsum rocks are widely exploited in the world as industrial minerals. The purity of the gypsum rocks (percentage in gypsum mineral in the whole rock) is a critical factor to evaluate the potential exploitability of a gypsum deposit. It is considered than purities higher than 80% in gypsum...
| Autores: | , , , , |
|---|---|
| Formato: | artículo |
| Estado: | Versión aceptada para publicación |
| Fecha de publicación: | 2010 |
| País: | España |
| Recursos: | Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya) |
| Repositorio: | Recercat. Dipósit de la Recerca de Catalunya |
| OAI Identifier: | oai:recercat.cat:2445/163394 |
| Acesso em linha: | https://hdl.handle.net/2445/163394 |
| Access Level: | acceso abierto |
| Palavra-chave: | Guix Propietats elèctriques Classificació dels minerals Plaster Electric properties Classification of minerals |
| id |
ES_2c30a7b2e12f863f2129f603534992b2 |
|---|---|
| oai_identifier_str |
oai:recercat.cat:2445/163394 |
| network_acronym_str |
ES |
| network_name_str |
España |
| repository_id_str |
|
| spelling |
Geoelectrical classification of Gypsum RocksGuinea Maysounave, AnderPlayà i Pous, ElisabetRivero Marginedas, LluísHimi, MahjoubBosch, RicardGuixPropietats elèctriquesClassificació dels mineralsPlasterElectric propertiesClassification of mineralsAbstract Gypsum rocks are widely exploited in the world as industrial minerals. The purity of the gypsum rocks (percentage in gypsum mineral in the whole rock) is a critical factor to evaluate the potential exploitability of a gypsum deposit. It is considered than purities higher than 80% in gypsum are required to be economically profitable. Gypsum deposits have been studied with geoelectrical methods; a direct relationship between the electrical resistivity values of the gypsum rocks and its lithological composition has been established, with the presence of lutites being the main controlling factor in the geoelectrical response of the deposit. This phenomenon has been quantified in the present study, by means of a combination of theoretical calculations, laboratory measurements and field data acquisition. Direct modelling has been performed; the data have been inverted to obtain the mean electrical resistivity of the models. The laboratory measurements have been obtained from artificial gypsum-clay mixture pills, and the electrical resistivity has been measured using a simple electrical circuit with direct current power supply. Finally, electrical resistivity tomography data have been acquired in different evaporite Tertiary basins located in North East Spain; the selected gypsum deposits have different gypsum compositions. The geoelectrical response of gypsum rocks has been determined by comparing the resistivity values obtained from theoretical models, laboratory tests and field examples. A geoelectrical classification of gypsum rocks defining three types of gypsum rocks has been elaborated: (a) Pure Gypsum Rocks ([75% of gypsum content), (b)Transitional Gypsum Rocks (75 55%), and (c) Lutites and Gypsum-rich Lutites (\55%). From the economic point of view, the Pure Gypsum Rocks, displaying a resistivity value of [800 ohm.m, can be exploited as industrial rocks. The methodology used could be applied in other geoelectrical rock studies, given that this relationship between the resistive particles embedded within a conductive matrix depends on the connectivity of the matrix particles.Springer Science + Business Media2020202020102020info:eu-repo/semantics/articleinfo:eu-repo/semantics/acceptedVersion31 p.application/pdfhttps://hdl.handle.net/2445/163394Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)reponame:Recercat. Dipósit de la Recerca de Catalunyainstname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)InglésVersió postprint del document publicat a: https://doi.org/10.1007/s10712-010-9107-xSurveys in Geophysics, 2010, vol. 31, p. 557-580https://doi.org/10.1007/s10712-010-9107-x(c) Springer Science + Business Media, 2010info:eu-repo/semantics/openAccessoai:recercat.cat:2445/1633942026-05-29T05:05:01Z |
| dc.title.none.fl_str_mv |
Geoelectrical classification of Gypsum Rocks |
| title |
Geoelectrical classification of Gypsum Rocks |
| spellingShingle |
Geoelectrical classification of Gypsum Rocks Guinea Maysounave, Ander Guix Propietats elèctriques Classificació dels minerals Plaster Electric properties Classification of minerals |
| title_short |
Geoelectrical classification of Gypsum Rocks |
| title_full |
Geoelectrical classification of Gypsum Rocks |
| title_fullStr |
Geoelectrical classification of Gypsum Rocks |
| title_full_unstemmed |
Geoelectrical classification of Gypsum Rocks |
| title_sort |
Geoelectrical classification of Gypsum Rocks |
| dc.creator.none.fl_str_mv |
Guinea Maysounave, Ander Playà i Pous, Elisabet Rivero Marginedas, Lluís Himi, Mahjoub Bosch, Ricard |
| author |
Guinea Maysounave, Ander |
| author_facet |
Guinea Maysounave, Ander Playà i Pous, Elisabet Rivero Marginedas, Lluís Himi, Mahjoub Bosch, Ricard |
| author_role |
author |
| author2 |
Playà i Pous, Elisabet Rivero Marginedas, Lluís Himi, Mahjoub Bosch, Ricard |
| author2_role |
author author author author |
| dc.subject.none.fl_str_mv |
Guix Propietats elèctriques Classificació dels minerals Plaster Electric properties Classification of minerals |
| topic |
Guix Propietats elèctriques Classificació dels minerals Plaster Electric properties Classification of minerals |
| description |
Abstract Gypsum rocks are widely exploited in the world as industrial minerals. The purity of the gypsum rocks (percentage in gypsum mineral in the whole rock) is a critical factor to evaluate the potential exploitability of a gypsum deposit. It is considered than purities higher than 80% in gypsum are required to be economically profitable. Gypsum deposits have been studied with geoelectrical methods; a direct relationship between the electrical resistivity values of the gypsum rocks and its lithological composition has been established, with the presence of lutites being the main controlling factor in the geoelectrical response of the deposit. This phenomenon has been quantified in the present study, by means of a combination of theoretical calculations, laboratory measurements and field data acquisition. Direct modelling has been performed; the data have been inverted to obtain the mean electrical resistivity of the models. The laboratory measurements have been obtained from artificial gypsum-clay mixture pills, and the electrical resistivity has been measured using a simple electrical circuit with direct current power supply. Finally, electrical resistivity tomography data have been acquired in different evaporite Tertiary basins located in North East Spain; the selected gypsum deposits have different gypsum compositions. The geoelectrical response of gypsum rocks has been determined by comparing the resistivity values obtained from theoretical models, laboratory tests and field examples. A geoelectrical classification of gypsum rocks defining three types of gypsum rocks has been elaborated: (a) Pure Gypsum Rocks ([75% of gypsum content), (b)Transitional Gypsum Rocks (75 55%), and (c) Lutites and Gypsum-rich Lutites (\55%). From the economic point of view, the Pure Gypsum Rocks, displaying a resistivity value of [800 ohm.m, can be exploited as industrial rocks. The methodology used could be applied in other geoelectrical rock studies, given that this relationship between the resistive particles embedded within a conductive matrix depends on the connectivity of the matrix particles. |
| publishDate |
2010 |
| dc.date.none.fl_str_mv |
2010 2020 2020 2020 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/acceptedVersion |
| format |
article |
| status_str |
acceptedVersion |
| dc.identifier.none.fl_str_mv |
https://hdl.handle.net/2445/163394 |
| url |
https://hdl.handle.net/2445/163394 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
Versió postprint del document publicat a: https://doi.org/10.1007/s10712-010-9107-x Surveys in Geophysics, 2010, vol. 31, p. 557-580 https://doi.org/10.1007/s10712-010-9107-x |
| dc.rights.none.fl_str_mv |
(c) Springer Science + Business Media, 2010 info:eu-repo/semantics/openAccess |
| rights_invalid_str_mv |
(c) Springer Science + Business Media, 2010 |
| eu_rights_str_mv |
openAccess |
| dc.format.none.fl_str_mv |
31 p. application/pdf |
| dc.publisher.none.fl_str_mv |
Springer Science + Business Media |
| publisher.none.fl_str_mv |
Springer Science + Business Media |
| dc.source.none.fl_str_mv |
Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada) reponame:Recercat. Dipósit de la Recerca de Catalunya instname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya) |
| instname_str |
Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya) |
| reponame_str |
Recercat. Dipósit de la Recerca de Catalunya |
| collection |
Recercat. Dipósit de la Recerca de Catalunya |
| repository.name.fl_str_mv |
|
| repository.mail.fl_str_mv |
|
| _version_ |
1869405211060076544 |
| score |
15.812429 |