Seasonal Dynamics of Soil CO2 Concentration and CO2 Fluxes from the Soil of the Former Lake Texcoco, Mexico
Seasonal changes of the soil CO 2 concentration and the rate of CO 2 fluxes emission from the soil formed on the sediments of the former Lake Texcoco, which occupied a significant part of the Mexico Valley until the mid-17th century, were studied. The soils (Fluvic Endogleyic Phaeozems) were charact...
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| Veröffentlicht in: | Eurasian soil science 2018-06, Vol.51 (6), p.674-681 |
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| creator | Ikkonen, E. N. García-Calderón, N. E. Ibáñez-Huerta, A. Etchevers-Barra, J. D. Krasilnikov, P. V. |
| description | Seasonal changes of the soil CO
2
concentration and the rate of CO
2
fluxes emission from the soil formed on the sediments of the former Lake Texcoco, which occupied a significant part of the Mexico Valley until the mid-17th century, were studied. The soils (Fluvic Endogleyic Phaeozems) were characterized by a low CO
2
fluxes rate, which is related to their high alkalinity. The mean values of soil respiration were 6.0–14.1 mg C/(m
2
h) depending on vegetation type, which corresponds to 60–157 g C/(m
2
yr). The contribution of plants to the CO
2
fluxes insignificantly varied by seasons and depended on the species composition of vegetation. The soil CO
2
concentration and soil respiration in eucalypt (
Eucalyptus globulus
Labill.) plantation were two times higher than those in the grass–subshrub area, the ground cover of which consisted of
Distichlis spicata
(L.) Greene and
Suaeda nigra
(Raf.) J.F. Macbr. species. This can be related to the significant volumes of gas production during the respiration of eucalypt roots and associated rhizosphere community. The contribution of the root systems of grass cover to the soil CO
2
fluxes in eucalypt plantation slightly varied within the year and was equal to 24% on the average. In the grass–subshrub area, its value varied from 41% in the cold season to 60% in the warm season. The spatial variability of soil CO
2
concentration and its flux rate to the atmosphere was due to the differences in plant species composition and hydrothermal conditions, and their temporal trend was closely related to the seasonal accumulation of plant biomass and soil temperature. |
| doi_str_mv | 10.1134/S106422931806008X |
| format | Article |
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2
concentration and the rate of CO
2
fluxes emission from the soil formed on the sediments of the former Lake Texcoco, which occupied a significant part of the Mexico Valley until the mid-17th century, were studied. The soils (Fluvic Endogleyic Phaeozems) were characterized by a low CO
2
fluxes rate, which is related to their high alkalinity. The mean values of soil respiration were 6.0–14.1 mg C/(m
2
h) depending on vegetation type, which corresponds to 60–157 g C/(m
2
yr). The contribution of plants to the CO
2
fluxes insignificantly varied by seasons and depended on the species composition of vegetation. The soil CO
2
concentration and soil respiration in eucalypt (
Eucalyptus globulus
Labill.) plantation were two times higher than those in the grass–subshrub area, the ground cover of which consisted of
Distichlis spicata
(L.) Greene and
Suaeda nigra
(Raf.) J.F. Macbr. species. This can be related to the significant volumes of gas production during the respiration of eucalypt roots and associated rhizosphere community. The contribution of the root systems of grass cover to the soil CO
2
fluxes in eucalypt plantation slightly varied within the year and was equal to 24% on the average. In the grass–subshrub area, its value varied from 41% in the cold season to 60% in the warm season. The spatial variability of soil CO
2
concentration and its flux rate to the atmosphere was due to the differences in plant species composition and hydrothermal conditions, and their temporal trend was closely related to the seasonal accumulation of plant biomass and soil temperature.</description><identifier>ISSN: 1064-2293</identifier><identifier>EISSN: 1556-195X</identifier><identifier>DOI: 10.1134/S106422931806008X</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Agriculture ; Alkalinity ; Annual variations ; Carbon dioxide ; Cold season ; Dynamics ; Earth and Environmental Science ; Earth Sciences ; Eucalyptus ; Fluxes ; Gas production ; Geotechnical Engineering & Applied Earth Sciences ; Grasses ; Ground cover ; Lakes ; Oil and gas production ; Plant biomass ; Plant species ; Plantations ; Respiration ; Rhizosphere ; Roots ; Seasonal variation ; Seasonal variations ; Seasons ; Sediments ; Soil ; Soil dynamics ; Soil Physics ; Soil temperature ; Spatial variations ; Species composition ; Vegetation ; Vegetation type</subject><ispartof>Eurasian soil science, 2018-06, Vol.51 (6), p.674-681</ispartof><rights>Pleiades Publishing, Ltd. 2018</rights><rights>Eurasian Soil Science is a copyright of Springer, (2018). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c316t-e8f2c7aa85bf41b8e1a5b9901a4a6e7720f0679582dc818acfe6ed7dd09644673</citedby><cites>FETCH-LOGICAL-c316t-e8f2c7aa85bf41b8e1a5b9901a4a6e7720f0679582dc818acfe6ed7dd09644673</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S106422931806008X$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S106422931806008X$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>315,781,785,27929,27930,41493,42562,51324</link.rule.ids></links><search><creatorcontrib>Ikkonen, E. N.</creatorcontrib><creatorcontrib>García-Calderón, N. E.</creatorcontrib><creatorcontrib>Ibáñez-Huerta, A.</creatorcontrib><creatorcontrib>Etchevers-Barra, J. D.</creatorcontrib><creatorcontrib>Krasilnikov, P. V.</creatorcontrib><title>Seasonal Dynamics of Soil CO2 Concentration and CO2 Fluxes from the Soil of the Former Lake Texcoco, Mexico</title><title>Eurasian soil science</title><addtitle>Eurasian Soil Sc</addtitle><description>Seasonal changes of the soil CO
2
concentration and the rate of CO
2
fluxes emission from the soil formed on the sediments of the former Lake Texcoco, which occupied a significant part of the Mexico Valley until the mid-17th century, were studied. The soils (Fluvic Endogleyic Phaeozems) were characterized by a low CO
2
fluxes rate, which is related to their high alkalinity. The mean values of soil respiration were 6.0–14.1 mg C/(m
2
h) depending on vegetation type, which corresponds to 60–157 g C/(m
2
yr). The contribution of plants to the CO
2
fluxes insignificantly varied by seasons and depended on the species composition of vegetation. The soil CO
2
concentration and soil respiration in eucalypt (
Eucalyptus globulus
Labill.) plantation were two times higher than those in the grass–subshrub area, the ground cover of which consisted of
Distichlis spicata
(L.) Greene and
Suaeda nigra
(Raf.) J.F. Macbr. species. This can be related to the significant volumes of gas production during the respiration of eucalypt roots and associated rhizosphere community. The contribution of the root systems of grass cover to the soil CO
2
fluxes in eucalypt plantation slightly varied within the year and was equal to 24% on the average. In the grass–subshrub area, its value varied from 41% in the cold season to 60% in the warm season. The spatial variability of soil CO
2
concentration and its flux rate to the atmosphere was due to the differences in plant species composition and hydrothermal conditions, and their temporal trend was closely related to the seasonal accumulation of plant biomass and soil temperature.</description><subject>Agriculture</subject><subject>Alkalinity</subject><subject>Annual variations</subject><subject>Carbon dioxide</subject><subject>Cold season</subject><subject>Dynamics</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Eucalyptus</subject><subject>Fluxes</subject><subject>Gas production</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Grasses</subject><subject>Ground cover</subject><subject>Lakes</subject><subject>Oil and gas production</subject><subject>Plant biomass</subject><subject>Plant species</subject><subject>Plantations</subject><subject>Respiration</subject><subject>Rhizosphere</subject><subject>Roots</subject><subject>Seasonal variation</subject><subject>Seasonal variations</subject><subject>Seasons</subject><subject>Sediments</subject><subject>Soil</subject><subject>Soil dynamics</subject><subject>Soil Physics</subject><subject>Soil temperature</subject><subject>Spatial variations</subject><subject>Species composition</subject><subject>Vegetation</subject><subject>Vegetation type</subject><issn>1064-2293</issn><issn>1556-195X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kM1OwzAQhC0EEuXnAbhZ4krA68SOc0SBAlJRDy1Sb5HrrCFtEhc7ldq3JyVIHBCnHe18M9IuIVfAbgHi5G4GTCacZzEoJhlTiyMyAiFkBJlYHPe6t6ODf0rOQlgxFiuVqBFZz1AH1-qaPuxb3VQmUGfpzFU1zaec5q412HZed5VrqW7L7-243u4wUOtdQ7sPHPA-dtBj5xv0dKLXSOe4M864G_qKu8q4C3JidR3w8meek7fx4zx_jibTp5f8fhKZGGQXobLcpForsbQJLBWCFsssY6ATLTFNObNMpplQvDQKlDYWJZZpWbJMJolM43NyPfRuvPvcYuiKldv6_sZQcCak5LEA3lMwUMa7EDzaYuOrRvt9Aaw4_LT489M-w4dM6Nn2Hf1v8_-hLy1xd2w</recordid><startdate>20180601</startdate><enddate>20180601</enddate><creator>Ikkonen, E. 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N.</au><au>García-Calderón, N. E.</au><au>Ibáñez-Huerta, A.</au><au>Etchevers-Barra, J. D.</au><au>Krasilnikov, P. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Seasonal Dynamics of Soil CO2 Concentration and CO2 Fluxes from the Soil of the Former Lake Texcoco, Mexico</atitle><jtitle>Eurasian soil science</jtitle><stitle>Eurasian Soil Sc</stitle><date>2018-06-01</date><risdate>2018</risdate><volume>51</volume><issue>6</issue><spage>674</spage><epage>681</epage><pages>674-681</pages><issn>1064-2293</issn><eissn>1556-195X</eissn><abstract>Seasonal changes of the soil CO
2
concentration and the rate of CO
2
fluxes emission from the soil formed on the sediments of the former Lake Texcoco, which occupied a significant part of the Mexico Valley until the mid-17th century, were studied. The soils (Fluvic Endogleyic Phaeozems) were characterized by a low CO
2
fluxes rate, which is related to their high alkalinity. The mean values of soil respiration were 6.0–14.1 mg C/(m
2
h) depending on vegetation type, which corresponds to 60–157 g C/(m
2
yr). The contribution of plants to the CO
2
fluxes insignificantly varied by seasons and depended on the species composition of vegetation. The soil CO
2
concentration and soil respiration in eucalypt (
Eucalyptus globulus
Labill.) plantation were two times higher than those in the grass–subshrub area, the ground cover of which consisted of
Distichlis spicata
(L.) Greene and
Suaeda nigra
(Raf.) J.F. Macbr. species. This can be related to the significant volumes of gas production during the respiration of eucalypt roots and associated rhizosphere community. The contribution of the root systems of grass cover to the soil CO
2
fluxes in eucalypt plantation slightly varied within the year and was equal to 24% on the average. In the grass–subshrub area, its value varied from 41% in the cold season to 60% in the warm season. The spatial variability of soil CO
2
concentration and its flux rate to the atmosphere was due to the differences in plant species composition and hydrothermal conditions, and their temporal trend was closely related to the seasonal accumulation of plant biomass and soil temperature.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S106422931806008X</doi><tpages>8</tpages></addata></record> |
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| ispartof | Eurasian soil science, 2018-06, Vol.51 (6), p.674-681 |
| issn | 1064-2293 1556-195X |
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| source | SpringerLink Journals - AutoHoldings |
| subjects | Agriculture Alkalinity Annual variations Carbon dioxide Cold season Dynamics Earth and Environmental Science Earth Sciences Eucalyptus Fluxes Gas production Geotechnical Engineering & Applied Earth Sciences Grasses Ground cover Lakes Oil and gas production Plant biomass Plant species Plantations Respiration Rhizosphere Roots Seasonal variation Seasonal variations Seasons Sediments Soil Soil dynamics Soil Physics Soil temperature Spatial variations Species composition Vegetation Vegetation type |
| title | Seasonal Dynamics of Soil CO2 Concentration and CO2 Fluxes from the Soil of the Former Lake Texcoco, Mexico |
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