Changes in soil organic carbon and aggregate stability following a chronosequence of Liriodendron chinense plantations
The objectives for this study were to determine changes in soil organic carbon (SOC) components and water-stable aggregates for soil profiles from different ages of plantations of Liriodendron chinense and to clarify which organic carbon component is more closely associated with the formation and st...
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| Veröffentlicht in: | Journal of forestry research 2021-02, Vol.32 (1), p.355-362 |
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| creator | Wu, Qicong Jiang, Xianghe Lu, Qianwen Li, Jinbiao Chen, Jinlin |
| description | The objectives for this study were to determine changes in soil organic carbon (SOC) components and water-stable aggregates for soil profiles from different ages of plantations of
Liriodendron chinense
and to clarify which organic carbon component is more closely associated with the formation and stability of soil aggregates. Three layers of soil (depths 0–20 cm, 20–40 cm, 40–60 cm) were collected from young, half-mature and mature stages of
L. chinense
. SOC, readily oxidizable organic carbon, chemically stable organic carbon and aggregate composition were determined. Intermediate stable organic carbon, the microbial quotient and aggregate stability (mean weight diameter) were calculated. SOC and aggregate stability in the
L. chinense
plantation did not increase linearly with an increase in
L. chinense
age; rather, they first decreased, then increased with increasing age of
L. chinense
. The microbial quotient had a negative effect on the level of organic carbon and the stability of aggregates, while chemically stable organic carbon had a positive effect, which explained 55.0% and 19.3% of the total variation, respectively (
P
|
| doi_str_mv | 10.1007/s11676-020-01110-0 |
| format | Article |
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Liriodendron chinense
and to clarify which organic carbon component is more closely associated with the formation and stability of soil aggregates. Three layers of soil (depths 0–20 cm, 20–40 cm, 40–60 cm) were collected from young, half-mature and mature stages of
L. chinense
. SOC, readily oxidizable organic carbon, chemically stable organic carbon and aggregate composition were determined. Intermediate stable organic carbon, the microbial quotient and aggregate stability (mean weight diameter) were calculated. SOC and aggregate stability in the
L. chinense
plantation did not increase linearly with an increase in
L. chinense
age; rather, they first decreased, then increased with increasing age of
L. chinense
. The microbial quotient had a negative effect on the level of organic carbon and the stability of aggregates, while chemically stable organic carbon had a positive effect, which explained 55.0% and 19.3% of the total variation, respectively (
P
< 0.01). Therefore, more attention should be paid of these two indicators in the future.</description><identifier>ISSN: 1007-662X</identifier><identifier>EISSN: 1993-0607</identifier><identifier>DOI: 10.1007/s11676-020-01110-0</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Aggregates ; Biomedical and Life Sciences ; Carbon ; Carbon content ; Forestry ; Life Sciences ; Liriodendron ; Microorganisms ; Organic carbon ; Organic soils ; Original Paper ; Plantations ; Quotients ; Soil aggregates ; Soil layers ; Soil profiles ; Soil properties ; Soil stability ; Soil structure ; Soil water ; Soils</subject><ispartof>Journal of forestry research, 2021-02, Vol.32 (1), p.355-362</ispartof><rights>Northeast Forestry University 2020</rights><rights>COPYRIGHT 2021 Springer</rights><rights>Northeast Forestry University 2020.</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c416t-39553010416586467bf1a1fadb998857690ac45acbe2540e1ee4a9b677af2c5d3</citedby><cites>FETCH-LOGICAL-c416t-39553010416586467bf1a1fadb998857690ac45acbe2540e1ee4a9b677af2c5d3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/lyyj/lyyj.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11676-020-01110-0$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11676-020-01110-0$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Wu, Qicong</creatorcontrib><creatorcontrib>Jiang, Xianghe</creatorcontrib><creatorcontrib>Lu, Qianwen</creatorcontrib><creatorcontrib>Li, Jinbiao</creatorcontrib><creatorcontrib>Chen, Jinlin</creatorcontrib><title>Changes in soil organic carbon and aggregate stability following a chronosequence of Liriodendron chinense plantations</title><title>Journal of forestry research</title><addtitle>J. For. Res</addtitle><description>The objectives for this study were to determine changes in soil organic carbon (SOC) components and water-stable aggregates for soil profiles from different ages of plantations of
Liriodendron chinense
and to clarify which organic carbon component is more closely associated with the formation and stability of soil aggregates. Three layers of soil (depths 0–20 cm, 20–40 cm, 40–60 cm) were collected from young, half-mature and mature stages of
L. chinense
. SOC, readily oxidizable organic carbon, chemically stable organic carbon and aggregate composition were determined. Intermediate stable organic carbon, the microbial quotient and aggregate stability (mean weight diameter) were calculated. SOC and aggregate stability in the
L. chinense
plantation did not increase linearly with an increase in
L. chinense
age; rather, they first decreased, then increased with increasing age of
L. chinense
. The microbial quotient had a negative effect on the level of organic carbon and the stability of aggregates, while chemically stable organic carbon had a positive effect, which explained 55.0% and 19.3% of the total variation, respectively (
P
< 0.01). Therefore, more attention should be paid of these two indicators in the future.</description><subject>Aggregates</subject><subject>Biomedical and Life Sciences</subject><subject>Carbon</subject><subject>Carbon content</subject><subject>Forestry</subject><subject>Life Sciences</subject><subject>Liriodendron</subject><subject>Microorganisms</subject><subject>Organic carbon</subject><subject>Organic soils</subject><subject>Original Paper</subject><subject>Plantations</subject><subject>Quotients</subject><subject>Soil aggregates</subject><subject>Soil layers</subject><subject>Soil profiles</subject><subject>Soil properties</subject><subject>Soil stability</subject><subject>Soil structure</subject><subject>Soil water</subject><subject>Soils</subject><issn>1007-662X</issn><issn>1993-0607</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp9kd9rHCEQx5fSQtK0_0CehNLHTXVd9XwMR3_BQV4ayJvMuuPGY0-vumm4_77TbmkolCDo6Hy-4wzfprkU_Epwbj5UIbTRLe94y4UQtL9ozoW1suWam5cUE9Vq3d2dNa9r3XOuein78-bH9h7ShJXFxGqOM8tlghQ981CGnBikkcE0FZxgQVYXGOIclxMLeZ7zY0wTA-bvS0654vcHTB5ZDmwXS8wjppESlI4JU0V2nCEtsMSc6pvmVYC54ts_50Vz--njt-2Xdnfz-ev2etf6XuillVYpyQWni9roXpshCBABxsHazUYZbTn4XoEfsFM9R4HYgx20MRA6r0Z50bxf6z5CCjSo2-eHkuhHN59O-453gqpLSdy7lTuWTGPU5QnseqOFMpw6-UtNMKOLKeSlgD_E6t21EcZYZawg6uo_FK0RD9HnhCHS-z-CbhX4kmstGNyxxAOUkxPc_TLOrfY6stf9ttdxEslVVAkmB8tTx8-ofgIe36dd</recordid><startdate>20210201</startdate><enddate>20210201</enddate><creator>Wu, Qicong</creator><creator>Jiang, Xianghe</creator><creator>Lu, Qianwen</creator><creator>Li, Jinbiao</creator><creator>Chen, Jinlin</creator><general>Springer Berlin Heidelberg</general><general>Springer</general><general>Springer Nature B.V</general><general>Co-Innovation Center for Sustainable Forestry in Southern China,Nanjing Forestry University,Nanjing 210037,People's Republic of China</general><scope>AAYXX</scope><scope>CITATION</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20210201</creationdate><title>Changes in soil organic carbon and aggregate stability following a chronosequence of Liriodendron chinense plantations</title><author>Wu, Qicong ; Jiang, Xianghe ; Lu, Qianwen ; Li, Jinbiao ; Chen, Jinlin</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c416t-39553010416586467bf1a1fadb998857690ac45acbe2540e1ee4a9b677af2c5d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Aggregates</topic><topic>Biomedical and Life Sciences</topic><topic>Carbon</topic><topic>Carbon content</topic><topic>Forestry</topic><topic>Life Sciences</topic><topic>Liriodendron</topic><topic>Microorganisms</topic><topic>Organic carbon</topic><topic>Organic soils</topic><topic>Original Paper</topic><topic>Plantations</topic><topic>Quotients</topic><topic>Soil aggregates</topic><topic>Soil layers</topic><topic>Soil profiles</topic><topic>Soil properties</topic><topic>Soil stability</topic><topic>Soil structure</topic><topic>Soil water</topic><topic>Soils</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wu, Qicong</creatorcontrib><creatorcontrib>Jiang, Xianghe</creatorcontrib><creatorcontrib>Lu, Qianwen</creatorcontrib><creatorcontrib>Li, Jinbiao</creatorcontrib><creatorcontrib>Chen, Jinlin</creatorcontrib><collection>CrossRef</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Journal of forestry research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wu, Qicong</au><au>Jiang, Xianghe</au><au>Lu, Qianwen</au><au>Li, Jinbiao</au><au>Chen, Jinlin</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Changes in soil organic carbon and aggregate stability following a chronosequence of Liriodendron chinense plantations</atitle><jtitle>Journal of forestry research</jtitle><stitle>J. For. Res</stitle><date>2021-02-01</date><risdate>2021</risdate><volume>32</volume><issue>1</issue><spage>355</spage><epage>362</epage><pages>355-362</pages><issn>1007-662X</issn><eissn>1993-0607</eissn><abstract>The objectives for this study were to determine changes in soil organic carbon (SOC) components and water-stable aggregates for soil profiles from different ages of plantations of
Liriodendron chinense
and to clarify which organic carbon component is more closely associated with the formation and stability of soil aggregates. Three layers of soil (depths 0–20 cm, 20–40 cm, 40–60 cm) were collected from young, half-mature and mature stages of
L. chinense
. SOC, readily oxidizable organic carbon, chemically stable organic carbon and aggregate composition were determined. Intermediate stable organic carbon, the microbial quotient and aggregate stability (mean weight diameter) were calculated. SOC and aggregate stability in the
L. chinense
plantation did not increase linearly with an increase in
L. chinense
age; rather, they first decreased, then increased with increasing age of
L. chinense
. The microbial quotient had a negative effect on the level of organic carbon and the stability of aggregates, while chemically stable organic carbon had a positive effect, which explained 55.0% and 19.3% of the total variation, respectively (
P
< 0.01). Therefore, more attention should be paid of these two indicators in the future.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s11676-020-01110-0</doi><tpages>8</tpages></addata></record> |
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| ispartof | Journal of forestry research, 2021-02, Vol.32 (1), p.355-362 |
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| language | eng |
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| subjects | Aggregates Biomedical and Life Sciences Carbon Carbon content Forestry Life Sciences Liriodendron Microorganisms Organic carbon Organic soils Original Paper Plantations Quotients Soil aggregates Soil layers Soil profiles Soil properties Soil stability Soil structure Soil water Soils |
| title | Changes in soil organic carbon and aggregate stability following a chronosequence of Liriodendron chinense plantations |
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