Soil taxonomical classification and organic carbon sequestration potential of coastal acid sulfate soils: Kari and Kayal ecosystems of Kerala, India

Purpose A study was carried out to understand the carbon sequestration potential of the coastal acid sulfate soils of wetland agroecosystems Kari and Kayal of Kuttanad , Kerala. Methods Soil profiles excavated in these lands were studied for their physico-chemical and morphological properties and cl...

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Veröffentlicht in:Journal of coastal conservation 2024-02, Vol.28 (1), p.26, Article 26
Hauptverfasser: K. S., Karthika, Anil Kumar, K. S., Nair, K. M., M., Jayaramaiah, S., Parvathy
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Anil Kumar, K. S.
Nair, K. M.
M., Jayaramaiah
S., Parvathy
description Purpose A study was carried out to understand the carbon sequestration potential of the coastal acid sulfate soils of wetland agroecosystems Kari and Kayal of Kuttanad , Kerala. Methods Soil profiles excavated in these lands were studied for their physico-chemical and morphological properties and classified according to USDA based soil taxonomy. Results The soils were very deep with moderately deep (97 cm) and moderately shallow (75 cm) solum thickness and both the soils were acidic,sulfuric and/or sulfidic and saline.The BaCl 2 acidity,exchangeable Al,total exchangeable bases and cation exchange capacity were higher in Kari soils.Both the soils recorded high sulfate S,which was higher in Kari soils.Based on the USDA soil taxonomy, Kari soils were classified to ferrihumic, euic, isohyperthermic, Typic Sulfohemists and Kayal soils to loamy, mixed, super-active, isohyperthermic, Salidic Sulfaquepts at the family level. Conclusion The organic carbon stock was higher in the sub-surface layer (30-100 cm) which recorded 2769.63 and 645.45 Mgha − 1 in Kari and Kayal lands respectively. The soil carbon sequestration potential was higher in Kari soils and the highest rate of C sequestration was at the depth 30–60 cm(656.09 kgm − 3 ) and soil layer was proved to have the capacity to hold 20.40 TgC with a total of 58.86 TgC in 11,250 ha of Kari lands for a thickness of 150 cm, while Kayal soils recorded the maximum at the depth 60-90 cm (163.43 kgm − 3 ) with a capacity to hold 3.29 TgC with a total of 21.02 TgC in 13,000 ha of Kayal lands for a thickness of 150 cm in 13,000 ha of Kayal lands.
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S., Karthika ; Anil Kumar, K. S. ; Nair, K. M. ; M., Jayaramaiah ; S., Parvathy</creator><creatorcontrib>K. S., Karthika ; Anil Kumar, K. S. ; Nair, K. M. ; M., Jayaramaiah ; S., Parvathy</creatorcontrib><description>Purpose A study was carried out to understand the carbon sequestration potential of the coastal acid sulfate soils of wetland agroecosystems Kari and Kayal of Kuttanad , Kerala. Methods Soil profiles excavated in these lands were studied for their physico-chemical and morphological properties and classified according to USDA based soil taxonomy. Results The soils were very deep with moderately deep (97 cm) and moderately shallow (75 cm) solum thickness and both the soils were acidic,sulfuric and/or sulfidic and saline.The BaCl 2 acidity,exchangeable Al,total exchangeable bases and cation exchange capacity were higher in Kari soils.Both the soils recorded high sulfate S,which was higher in Kari soils.Based on the USDA soil taxonomy, Kari soils were classified to ferrihumic, euic, isohyperthermic, Typic Sulfohemists and Kayal soils to loamy, mixed, super-active, isohyperthermic, Salidic Sulfaquepts at the family level. Conclusion The organic carbon stock was higher in the sub-surface layer (30-100 cm) which recorded 2769.63 and 645.45 Mgha − 1 in Kari and Kayal lands respectively. The soil carbon sequestration potential was higher in Kari soils and the highest rate of C sequestration was at the depth 30–60 cm(656.09 kgm − 3 ) and soil layer was proved to have the capacity to hold 20.40 TgC with a total of 58.86 TgC in 11,250 ha of Kari lands for a thickness of 150 cm, while Kayal soils recorded the maximum at the depth 60-90 cm (163.43 kgm − 3 ) with a capacity to hold 3.29 TgC with a total of 21.02 TgC in 13,000 ha of Kayal lands for a thickness of 150 cm in 13,000 ha of Kayal lands.</description><identifier>ISSN: 1400-0350</identifier><identifier>EISSN: 1874-7841</identifier><identifier>DOI: 10.1007/s11852-023-01022-1</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>Acidic soils ; Acidity ; Agricultural ecosystems ; Barium chloride ; Carbon sequestration ; Cation exchange ; Cation exchanging ; Cations ; Coastal Sciences ; Earth and Environmental Science ; Exchange capacity ; Geography ; Nature Conservation ; Oceanography ; Organic carbon ; Organic soils ; Remote Sensing/Photogrammetry ; Soil ; Soil classification ; Soil layers ; Soil profiles ; Soil properties ; Soils ; Sulfates ; Surface layers ; Taxonomy ; Thickness</subject><ispartof>Journal of coastal conservation, 2024-02, Vol.28 (1), p.26, Article 26</ispartof><rights>The Author(s), under exclusive licence to Springer Nature B.V. 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c270t-cd1b46f1104ee4471779eeda6e1ae8975a70a48e93ee281d29d797b0e650a6ea3</cites><orcidid>0000-0003-2122-3732</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11852-023-01022-1$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11852-023-01022-1$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>K. 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Results The soils were very deep with moderately deep (97 cm) and moderately shallow (75 cm) solum thickness and both the soils were acidic,sulfuric and/or sulfidic and saline.The BaCl 2 acidity,exchangeable Al,total exchangeable bases and cation exchange capacity were higher in Kari soils.Both the soils recorded high sulfate S,which was higher in Kari soils.Based on the USDA soil taxonomy, Kari soils were classified to ferrihumic, euic, isohyperthermic, Typic Sulfohemists and Kayal soils to loamy, mixed, super-active, isohyperthermic, Salidic Sulfaquepts at the family level. Conclusion The organic carbon stock was higher in the sub-surface layer (30-100 cm) which recorded 2769.63 and 645.45 Mgha − 1 in Kari and Kayal lands respectively. The soil carbon sequestration potential was higher in Kari soils and the highest rate of C sequestration was at the depth 30–60 cm(656.09 kgm − 3 ) and soil layer was proved to have the capacity to hold 20.40 TgC with a total of 58.86 TgC in 11,250 ha of Kari lands for a thickness of 150 cm, while Kayal soils recorded the maximum at the depth 60-90 cm (163.43 kgm − 3 ) with a capacity to hold 3.29 TgC with a total of 21.02 TgC in 13,000 ha of Kayal lands for a thickness of 150 cm in 13,000 ha of Kayal lands.</description><subject>Acidic soils</subject><subject>Acidity</subject><subject>Agricultural ecosystems</subject><subject>Barium chloride</subject><subject>Carbon sequestration</subject><subject>Cation exchange</subject><subject>Cation exchanging</subject><subject>Cations</subject><subject>Coastal Sciences</subject><subject>Earth and Environmental Science</subject><subject>Exchange capacity</subject><subject>Geography</subject><subject>Nature Conservation</subject><subject>Oceanography</subject><subject>Organic carbon</subject><subject>Organic soils</subject><subject>Remote Sensing/Photogrammetry</subject><subject>Soil</subject><subject>Soil classification</subject><subject>Soil layers</subject><subject>Soil profiles</subject><subject>Soil properties</subject><subject>Soils</subject><subject>Sulfates</subject><subject>Surface layers</subject><subject>Taxonomy</subject><subject>Thickness</subject><issn>1400-0350</issn><issn>1874-7841</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNp9kEFP3DAQhaMKpMKWP9CTpV6bMuMk64RbhUpZLVIPhbM160yQUTZePF6p-z_4wZgNEree5mn0vTeaVxRfEX4ggLkUxLbRJeiqBAStS_xUnGFr6tK0NZ5kXQOUUDXwuTgXeQLQTdtUZ8XL3-BHlehfmMLWOxqVG0nED1knHyZFU69CfKTJO-UobvJK-HnPkuIM7ELiKfnsDINygSRlSc73SvbjQImV5BNypdYU_TFuTYeMsAtykMRbeTOuOdJI39Vq6j19KU4HGoUv3ueieLj5dX99W979-b26_nlXOm0gla7HTb0cEKFmrmuDxnTMPS0ZidvONGSA6pa7ilm32OuuN53ZAC8byBBVi-LbnLuL4fiSfQr7OOWTVndYNaZr2i5TeqZcDCKRB7uLfkvxYBHsW_t2bt_m9u2xfYvZVM0myfD0yPEj-j-uV94uim4</recordid><startdate>20240201</startdate><enddate>20240201</enddate><creator>K. 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S., Karthika</creatorcontrib><creatorcontrib>Anil Kumar, K. S.</creatorcontrib><creatorcontrib>Nair, K. M.</creatorcontrib><creatorcontrib>M., Jayaramaiah</creatorcontrib><creatorcontrib>S., Parvathy</creatorcontrib><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Sustainability Science Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 3: Aquatic Pollution &amp; Environmental Quality</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><jtitle>Journal of coastal conservation</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>K. S., Karthika</au><au>Anil Kumar, K. S.</au><au>Nair, K. 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Results The soils were very deep with moderately deep (97 cm) and moderately shallow (75 cm) solum thickness and both the soils were acidic,sulfuric and/or sulfidic and saline.The BaCl 2 acidity,exchangeable Al,total exchangeable bases and cation exchange capacity were higher in Kari soils.Both the soils recorded high sulfate S,which was higher in Kari soils.Based on the USDA soil taxonomy, Kari soils were classified to ferrihumic, euic, isohyperthermic, Typic Sulfohemists and Kayal soils to loamy, mixed, super-active, isohyperthermic, Salidic Sulfaquepts at the family level. Conclusion The organic carbon stock was higher in the sub-surface layer (30-100 cm) which recorded 2769.63 and 645.45 Mgha − 1 in Kari and Kayal lands respectively. The soil carbon sequestration potential was higher in Kari soils and the highest rate of C sequestration was at the depth 30–60 cm(656.09 kgm − 3 ) and soil layer was proved to have the capacity to hold 20.40 TgC with a total of 58.86 TgC in 11,250 ha of Kari lands for a thickness of 150 cm, while Kayal soils recorded the maximum at the depth 60-90 cm (163.43 kgm − 3 ) with a capacity to hold 3.29 TgC with a total of 21.02 TgC in 13,000 ha of Kayal lands for a thickness of 150 cm in 13,000 ha of Kayal lands.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s11852-023-01022-1</doi><orcidid>https://orcid.org/0000-0003-2122-3732</orcidid></addata></record>
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subjects Acidic soils
Acidity
Agricultural ecosystems
Barium chloride
Carbon sequestration
Cation exchange
Cation exchanging
Cations
Coastal Sciences
Earth and Environmental Science
Exchange capacity
Geography
Nature Conservation
Oceanography
Organic carbon
Organic soils
Remote Sensing/Photogrammetry
Soil
Soil classification
Soil layers
Soil profiles
Soil properties
Soils
Sulfates
Surface layers
Taxonomy
Thickness
title Soil taxonomical classification and organic carbon sequestration potential of coastal acid sulfate soils: Kari and Kayal ecosystems of Kerala, India
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