Loading…
Space-Time Modeling of the Electrical Conductivity of Soil in a Geothermal Zone
The aim of this study was to generate models to predict the salinity of the soils in the geothermal zone which is located in Michoacán, México, over space and time. Systematic sampling was performed at locations 400 m apart with a sampling period every 48 days. At each site, two soil samples, from d...
Saved in:
Published in: | Communications in Soil Science and Plant Analysis 2018-05, Vol.49 (9), p.1107-1118 |
---|---|
Main Authors: | , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
cited_by | cdi_FETCH-LOGICAL-c281t-9c502a9c524b9c08d7f99ef79e83d473a0311e2a3fc6710ae8e876c51147a2ee3 |
---|---|
cites | cdi_FETCH-LOGICAL-c281t-9c502a9c524b9c08d7f99ef79e83d473a0311e2a3fc6710ae8e876c51147a2ee3 |
container_end_page | 1118 |
container_issue | 9 |
container_start_page | 1107 |
container_title | Communications in Soil Science and Plant Analysis |
container_volume | 49 |
creator | Anaya-Flores, Raquel Cruz-Cárdenas, Gustavo Silva, José Teodoro Ochoa-Estrada, Salvador Álvarez-Bernal, Dioselina |
description | The aim of this study was to generate models to predict the salinity of the soils in the geothermal zone which is located in Michoacán, México, over space and time. Systematic sampling was performed at locations 400 m apart with a sampling period every 48 days. At each site, two soil samples, from depths of 0-30 cm and 30-60 cm, were collected and analysed in laboratory. Regression-Kriging was used to make spatial predictions of the electrical conductivity of soil (ECs). Spherical and Gaussian theoretical models fit the experimental semivariograms. The results showed that the soil samples ranged from slightly saline (2.1-4 dS m-1) to strongly saline (8.1-16 dS m-1). In addition, the ECs was greater at a depth of 30-60 cm than it was at a depth of 0-30 cm. The ECs decreased from more than 8.0 dS m-1 to less than 4.0 dS m-1 after the first sampling period. |
doi_str_mv | 10.1080/00103624.2018.1448862 |
format | article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2029510561</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2029510561</sourcerecordid><originalsourceid>FETCH-LOGICAL-c281t-9c502a9c524b9c08d7f99ef79e83d473a0311e2a3fc6710ae8e876c51147a2ee3</originalsourceid><addsrcrecordid>eNo1kMFKw0AQhhdRsFYfQVjwnDizm2Q3Rym1CpUeWi9elnUz0S1ptm5SoW9vQutlhmE-_h8-xu4RUgQNjwAIshBZKgB1ilmmdSEu2ARzKRKRYXHJJiOTjNA1u-m67XCWCsSErdZ76yjZ-B3xt1BR49svHmrefxOfN-T66J1t-Cy01cH1_tf3x_G9Dr7hvuWWLygMbNwN0Edo6ZZd1bbp6O68p-z9eb6ZvSTL1eJ19rRMnNDYJ6XLQdhhiuyzdKArVZcl1aokLatMSQsSkYSVtSsUgiVNWhUuR8yUFURyyh5OufsYfg7U9WYbDrEdKo0AUeYIeYEDlZ8oF0PXRarNPvqdjUeDYEZ35t-dGd2Zszv5B8-qX-4</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2029510561</pqid></control><display><type>article</type><title>Space-Time Modeling of the Electrical Conductivity of Soil in a Geothermal Zone</title><source>Taylor and Francis Science and Technology Collection</source><creator>Anaya-Flores, Raquel ; Cruz-Cárdenas, Gustavo ; Silva, José Teodoro ; Ochoa-Estrada, Salvador ; Álvarez-Bernal, Dioselina</creator><creatorcontrib>Anaya-Flores, Raquel ; Cruz-Cárdenas, Gustavo ; Silva, José Teodoro ; Ochoa-Estrada, Salvador ; Álvarez-Bernal, Dioselina</creatorcontrib><description>The aim of this study was to generate models to predict the salinity of the soils in the geothermal zone which is located in Michoacán, México, over space and time. Systematic sampling was performed at locations 400 m apart with a sampling period every 48 days. At each site, two soil samples, from depths of 0-30 cm and 30-60 cm, were collected and analysed in laboratory. Regression-Kriging was used to make spatial predictions of the electrical conductivity of soil (ECs). Spherical and Gaussian theoretical models fit the experimental semivariograms. The results showed that the soil samples ranged from slightly saline (2.1-4 dS m-1) to strongly saline (8.1-16 dS m-1). In addition, the ECs was greater at a depth of 30-60 cm than it was at a depth of 0-30 cm. The ECs decreased from more than 8.0 dS m-1 to less than 4.0 dS m-1 after the first sampling period.</description><identifier>ISSN: 0010-3624</identifier><identifier>EISSN: 1532-2416</identifier><identifier>EISSN: 1532-4133</identifier><identifier>DOI: 10.1080/00103624.2018.1448862</identifier><language>eng</language><publisher>Philadelphia: Taylor & Francis Ltd</publisher><subject>Electrical conductivity ; Electrical resistivity ; Kriging interpolation ; Mathematical models ; Modelling ; Regression analysis ; Sampling ; Soil ; Soil conductivity ; Soil salinity ; Statistical methods</subject><ispartof>Communications in Soil Science and Plant Analysis, 2018-05, Vol.49 (9), p.1107-1118</ispartof><rights>2018 Taylor & Francis</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c281t-9c502a9c524b9c08d7f99ef79e83d473a0311e2a3fc6710ae8e876c51147a2ee3</citedby><cites>FETCH-LOGICAL-c281t-9c502a9c524b9c08d7f99ef79e83d473a0311e2a3fc6710ae8e876c51147a2ee3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Anaya-Flores, Raquel</creatorcontrib><creatorcontrib>Cruz-Cárdenas, Gustavo</creatorcontrib><creatorcontrib>Silva, José Teodoro</creatorcontrib><creatorcontrib>Ochoa-Estrada, Salvador</creatorcontrib><creatorcontrib>Álvarez-Bernal, Dioselina</creatorcontrib><title>Space-Time Modeling of the Electrical Conductivity of Soil in a Geothermal Zone</title><title>Communications in Soil Science and Plant Analysis</title><description>The aim of this study was to generate models to predict the salinity of the soils in the geothermal zone which is located in Michoacán, México, over space and time. Systematic sampling was performed at locations 400 m apart with a sampling period every 48 days. At each site, two soil samples, from depths of 0-30 cm and 30-60 cm, were collected and analysed in laboratory. Regression-Kriging was used to make spatial predictions of the electrical conductivity of soil (ECs). Spherical and Gaussian theoretical models fit the experimental semivariograms. The results showed that the soil samples ranged from slightly saline (2.1-4 dS m-1) to strongly saline (8.1-16 dS m-1). In addition, the ECs was greater at a depth of 30-60 cm than it was at a depth of 0-30 cm. The ECs decreased from more than 8.0 dS m-1 to less than 4.0 dS m-1 after the first sampling period.</description><subject>Electrical conductivity</subject><subject>Electrical resistivity</subject><subject>Kriging interpolation</subject><subject>Mathematical models</subject><subject>Modelling</subject><subject>Regression analysis</subject><subject>Sampling</subject><subject>Soil</subject><subject>Soil conductivity</subject><subject>Soil salinity</subject><subject>Statistical methods</subject><issn>0010-3624</issn><issn>1532-2416</issn><issn>1532-4133</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><recordid>eNo1kMFKw0AQhhdRsFYfQVjwnDizm2Q3Rym1CpUeWi9elnUz0S1ptm5SoW9vQutlhmE-_h8-xu4RUgQNjwAIshBZKgB1ilmmdSEu2ARzKRKRYXHJJiOTjNA1u-m67XCWCsSErdZ76yjZ-B3xt1BR49svHmrefxOfN-T66J1t-Cy01cH1_tf3x_G9Dr7hvuWWLygMbNwN0Edo6ZZd1bbp6O68p-z9eb6ZvSTL1eJ19rRMnNDYJ6XLQdhhiuyzdKArVZcl1aokLatMSQsSkYSVtSsUgiVNWhUuR8yUFURyyh5OufsYfg7U9WYbDrEdKo0AUeYIeYEDlZ8oF0PXRarNPvqdjUeDYEZ35t-dGd2Zszv5B8-qX-4</recordid><startdate>20180515</startdate><enddate>20180515</enddate><creator>Anaya-Flores, Raquel</creator><creator>Cruz-Cárdenas, Gustavo</creator><creator>Silva, José Teodoro</creator><creator>Ochoa-Estrada, Salvador</creator><creator>Álvarez-Bernal, Dioselina</creator><general>Taylor & Francis Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7ST</scope><scope>7T7</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H97</scope><scope>L.G</scope><scope>P64</scope><scope>SOI</scope></search><sort><creationdate>20180515</creationdate><title>Space-Time Modeling of the Electrical Conductivity of Soil in a Geothermal Zone</title><author>Anaya-Flores, Raquel ; Cruz-Cárdenas, Gustavo ; Silva, José Teodoro ; Ochoa-Estrada, Salvador ; Álvarez-Bernal, Dioselina</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c281t-9c502a9c524b9c08d7f99ef79e83d473a0311e2a3fc6710ae8e876c51147a2ee3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Electrical conductivity</topic><topic>Electrical resistivity</topic><topic>Kriging interpolation</topic><topic>Mathematical models</topic><topic>Modelling</topic><topic>Regression analysis</topic><topic>Sampling</topic><topic>Soil</topic><topic>Soil conductivity</topic><topic>Soil salinity</topic><topic>Statistical methods</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Anaya-Flores, Raquel</creatorcontrib><creatorcontrib>Cruz-Cárdenas, Gustavo</creatorcontrib><creatorcontrib>Silva, José Teodoro</creatorcontrib><creatorcontrib>Ochoa-Estrada, Salvador</creatorcontrib><creatorcontrib>Álvarez-Bernal, Dioselina</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Environment Abstracts</collection><jtitle>Communications in Soil Science and Plant Analysis</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Anaya-Flores, Raquel</au><au>Cruz-Cárdenas, Gustavo</au><au>Silva, José Teodoro</au><au>Ochoa-Estrada, Salvador</au><au>Álvarez-Bernal, Dioselina</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Space-Time Modeling of the Electrical Conductivity of Soil in a Geothermal Zone</atitle><jtitle>Communications in Soil Science and Plant Analysis</jtitle><date>2018-05-15</date><risdate>2018</risdate><volume>49</volume><issue>9</issue><spage>1107</spage><epage>1118</epage><pages>1107-1118</pages><issn>0010-3624</issn><eissn>1532-2416</eissn><eissn>1532-4133</eissn><abstract>The aim of this study was to generate models to predict the salinity of the soils in the geothermal zone which is located in Michoacán, México, over space and time. Systematic sampling was performed at locations 400 m apart with a sampling period every 48 days. At each site, two soil samples, from depths of 0-30 cm and 30-60 cm, were collected and analysed in laboratory. Regression-Kriging was used to make spatial predictions of the electrical conductivity of soil (ECs). Spherical and Gaussian theoretical models fit the experimental semivariograms. The results showed that the soil samples ranged from slightly saline (2.1-4 dS m-1) to strongly saline (8.1-16 dS m-1). In addition, the ECs was greater at a depth of 30-60 cm than it was at a depth of 0-30 cm. The ECs decreased from more than 8.0 dS m-1 to less than 4.0 dS m-1 after the first sampling period.</abstract><cop>Philadelphia</cop><pub>Taylor & Francis Ltd</pub><doi>10.1080/00103624.2018.1448862</doi><tpages>12</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0010-3624 |
ispartof | Communications in Soil Science and Plant Analysis, 2018-05, Vol.49 (9), p.1107-1118 |
issn | 0010-3624 1532-2416 1532-4133 |
language | eng |
recordid | cdi_proquest_journals_2029510561 |
source | Taylor and Francis Science and Technology Collection |
subjects | Electrical conductivity Electrical resistivity Kriging interpolation Mathematical models Modelling Regression analysis Sampling Soil Soil conductivity Soil salinity Statistical methods |
title | Space-Time Modeling of the Electrical Conductivity of Soil in a Geothermal Zone |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-29T19%3A03%3A45IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Space-Time%20Modeling%20of%20the%20Electrical%20Conductivity%20of%20Soil%20in%20a%20Geothermal%20Zone&rft.jtitle=Communications%20in%20Soil%20Science%20and%20Plant%20Analysis&rft.au=Anaya-Flores,%20Raquel&rft.date=2018-05-15&rft.volume=49&rft.issue=9&rft.spage=1107&rft.epage=1118&rft.pages=1107-1118&rft.issn=0010-3624&rft.eissn=1532-2416&rft_id=info:doi/10.1080/00103624.2018.1448862&rft_dat=%3Cproquest_cross%3E2029510561%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c281t-9c502a9c524b9c08d7f99ef79e83d473a0311e2a3fc6710ae8e876c51147a2ee3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=2029510561&rft_id=info:pmid/&rfr_iscdi=true |