Comparison of soil respiration among three temperate forests in Changbai Mountains, China
CO2 efflux from forest soils is an important process in the global carbon cycle; however, effects of stand age and successional status remain uncertain. We compared soil respiration and its relationship to soil carbon content, forest floor mass, root biomass, soil temperature, and soil moisture cont...
Gespeichert in:
| Veröffentlicht in: | Canadian journal of forest research 2010-04, Vol.40 (4), p.788-795 |
|---|---|
| Hauptverfasser: | , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 795 |
|---|---|
| container_issue | 4 |
| container_start_page | 788 |
| container_title | Canadian journal of forest research |
| container_volume | 40 |
| creator | Wang, Xu Jiang, Yanling Jia, Bingrui Wang, Fengyu Zhou, Guangsheng |
| description | CO2 efflux from forest soils is an important process in the global carbon cycle; however, effects of stand age and successional status remain uncertain. We compared soil respiration and its relationship to soil carbon content, forest floor mass, root biomass, soil temperature, and soil moisture content among three temperate forest ecosystems in Changbai Mountains, northeastern China, from 2003 to 2005. Forest types included an old-growth, mixed coniferous and broad-leaved primary forest (MN), a middle-aged, broad-leaved secondary forest (BL), and a young coniferous plantation forest (CP). Average annual soil CO2 efflux at BL (1477.9 +/- 61.8 g C·m-2·year-1) was significantly higher than at CP (830.7 +/- 48.7 g C·m-2·year-1) and MN (935.4 +/- 53.3 g C·m-2·year-1). Differences in soil temperature among those sites were not statistically significant but contributed to the differences in annual CO2 efflux. In addition, the temperature response of soil CO2 efflux was higher at MN (Q10 = 2.78) than that at BL (Q10 = 2.17) and CP (Q10 = 2.02). Our results suggest that successional stage affects soil respiration by the differences in substrate quantity and quality, environmental conditions, and root respiration. |
| doi_str_mv | 10.1139/x10-010 |
| format | Article |
| fullrecord | <record><control><sourceid>gale_proqu</sourceid><recordid>TN_cdi_proquest_miscellaneous_745703394</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A227866623</galeid><sourcerecordid>A227866623</sourcerecordid><originalsourceid>FETCH-LOGICAL-c670t-e69b0421a1085277affbce1cbeb15ead2fc3d35fc977b15967b50dd80712231d3</originalsourceid><addsrcrecordid>eNqV0l2L1DAUBuAiCo6r-BMsKyqKXU-SNmkvl8GPhVXBdUGvwmmadLK0STfpwPjvzTCDODIK0ouUw5OXcHiz7DGBM0JY82ZDoAACd7IFoVAXHJi4my0AyqqogIv72YMYbwCAcQaL7PvSjxMGG73Lvcmjt0MedJxswNmmGY7e9fm8Clrnsx4nneY6Nz6ZOebW5csVur5Fm3_0azejdfF1mlmHD7N7BoeoH-3Pk-z63duvyw_F5ef3F8vzy0JxAXOhedNCSQkSqCsqBBrTKk1Uq1tSaeyoUaxjlVGNEGnScNFW0HU1CEIpIx07yV7scqfgb9fpWXK0UelhQKf9OkpRVgIYa8okT_-QN34dXHqcpFCxhtGySujpDvU4aGmd8XNAtY2U55SKmnNOWVLFEdVrl_YzeKeNTeMDf3rEq8neyt_R2RGUvk6PVh1NfXlwIZlZb-Ye1zHKi6sv_2E_Hdr9SlXwMQZt5BTsiOGHJCC3JZPf0k8qWZLP9ivFqHAwAZ2y8RentG44L7eJr3bOBZWqozGo1T9Cn_8db3ZITp1J8MkOGvQS-9RieX1FgTAgNeOp_ewnSTjv2w</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>205393245</pqid></control><display><type>article</type><title>Comparison of soil respiration among three temperate forests in Changbai Mountains, China</title><source>Alma/SFX Local Collection</source><creator>Wang, Xu ; Jiang, Yanling ; Jia, Bingrui ; Wang, Fengyu ; Zhou, Guangsheng</creator><creatorcontrib>Wang, Xu ; Jiang, Yanling ; Jia, Bingrui ; Wang, Fengyu ; Zhou, Guangsheng</creatorcontrib><description>CO2 efflux from forest soils is an important process in the global carbon cycle; however, effects of stand age and successional status remain uncertain. We compared soil respiration and its relationship to soil carbon content, forest floor mass, root biomass, soil temperature, and soil moisture content among three temperate forest ecosystems in Changbai Mountains, northeastern China, from 2003 to 2005. Forest types included an old-growth, mixed coniferous and broad-leaved primary forest (MN), a middle-aged, broad-leaved secondary forest (BL), and a young coniferous plantation forest (CP). Average annual soil CO2 efflux at BL (1477.9 +/- 61.8 g C·m-2·year-1) was significantly higher than at CP (830.7 +/- 48.7 g C·m-2·year-1) and MN (935.4 +/- 53.3 g C·m-2·year-1). Differences in soil temperature among those sites were not statistically significant but contributed to the differences in annual CO2 efflux. In addition, the temperature response of soil CO2 efflux was higher at MN (Q10 = 2.78) than that at BL (Q10 = 2.17) and CP (Q10 = 2.02). Our results suggest that successional stage affects soil respiration by the differences in substrate quantity and quality, environmental conditions, and root respiration.</description><identifier>ISSN: 0045-5067</identifier><identifier>EISSN: 1208-6037</identifier><identifier>DOI: 10.1139/x10-010</identifier><identifier>CODEN: CJFRAR</identifier><language>eng</language><publisher>Ottawa, ON: National Research Council of Canada</publisher><subject>biogeochemical cycles ; Biological and medical sciences ; Carbon cycle ; Carbon dioxide ; Comparative analysis ; Coniferous forests ; deciduous forests ; Environmental aspects ; Environmental conditions ; equations ; Forest ecosystems ; Forest floor ; forest plantations ; Forest soils ; forest stands ; forest succession ; Forestry ; Forests ; Fundamental and applied biological sciences. Psychology ; gas emissions ; Moisture content ; Mountains ; old-growth forests ; Respiration ; Soil moisture ; soil respiration ; Soil temperature ; soil water ; soil-plant-atmosphere interactions ; Soils ; Temperate climates ; Temperate forests ; Temperature</subject><ispartof>Canadian journal of forest research, 2010-04, Vol.40 (4), p.788-795</ispartof><rights>2015 INIST-CNRS</rights><rights>COPYRIGHT 2010 NRC Research Press</rights><rights>Copyright National Research Council of Canada Apr 2010</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c670t-e69b0421a1085277affbce1cbeb15ead2fc3d35fc977b15967b50dd80712231d3</citedby><cites>FETCH-LOGICAL-c670t-e69b0421a1085277affbce1cbeb15ead2fc3d35fc977b15967b50dd80712231d3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=22896643$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Wang, Xu</creatorcontrib><creatorcontrib>Jiang, Yanling</creatorcontrib><creatorcontrib>Jia, Bingrui</creatorcontrib><creatorcontrib>Wang, Fengyu</creatorcontrib><creatorcontrib>Zhou, Guangsheng</creatorcontrib><title>Comparison of soil respiration among three temperate forests in Changbai Mountains, China</title><title>Canadian journal of forest research</title><addtitle>Revue canadienne de recherche forestière</addtitle><description>CO2 efflux from forest soils is an important process in the global carbon cycle; however, effects of stand age and successional status remain uncertain. We compared soil respiration and its relationship to soil carbon content, forest floor mass, root biomass, soil temperature, and soil moisture content among three temperate forest ecosystems in Changbai Mountains, northeastern China, from 2003 to 2005. Forest types included an old-growth, mixed coniferous and broad-leaved primary forest (MN), a middle-aged, broad-leaved secondary forest (BL), and a young coniferous plantation forest (CP). Average annual soil CO2 efflux at BL (1477.9 +/- 61.8 g C·m-2·year-1) was significantly higher than at CP (830.7 +/- 48.7 g C·m-2·year-1) and MN (935.4 +/- 53.3 g C·m-2·year-1). Differences in soil temperature among those sites were not statistically significant but contributed to the differences in annual CO2 efflux. In addition, the temperature response of soil CO2 efflux was higher at MN (Q10 = 2.78) than that at BL (Q10 = 2.17) and CP (Q10 = 2.02). Our results suggest that successional stage affects soil respiration by the differences in substrate quantity and quality, environmental conditions, and root respiration.</description><subject>biogeochemical cycles</subject><subject>Biological and medical sciences</subject><subject>Carbon cycle</subject><subject>Carbon dioxide</subject><subject>Comparative analysis</subject><subject>Coniferous forests</subject><subject>deciduous forests</subject><subject>Environmental aspects</subject><subject>Environmental conditions</subject><subject>equations</subject><subject>Forest ecosystems</subject><subject>Forest floor</subject><subject>forest plantations</subject><subject>Forest soils</subject><subject>forest stands</subject><subject>forest succession</subject><subject>Forestry</subject><subject>Forests</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>gas emissions</subject><subject>Moisture content</subject><subject>Mountains</subject><subject>old-growth forests</subject><subject>Respiration</subject><subject>Soil moisture</subject><subject>soil respiration</subject><subject>Soil temperature</subject><subject>soil water</subject><subject>soil-plant-atmosphere interactions</subject><subject>Soils</subject><subject>Temperate climates</subject><subject>Temperate forests</subject><subject>Temperature</subject><issn>0045-5067</issn><issn>1208-6037</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><recordid>eNqV0l2L1DAUBuAiCo6r-BMsKyqKXU-SNmkvl8GPhVXBdUGvwmmadLK0STfpwPjvzTCDODIK0ouUw5OXcHiz7DGBM0JY82ZDoAACd7IFoVAXHJi4my0AyqqogIv72YMYbwCAcQaL7PvSjxMGG73Lvcmjt0MedJxswNmmGY7e9fm8Clrnsx4nneY6Nz6ZOebW5csVur5Fm3_0azejdfF1mlmHD7N7BoeoH-3Pk-z63duvyw_F5ef3F8vzy0JxAXOhedNCSQkSqCsqBBrTKk1Uq1tSaeyoUaxjlVGNEGnScNFW0HU1CEIpIx07yV7scqfgb9fpWXK0UelhQKf9OkpRVgIYa8okT_-QN34dXHqcpFCxhtGySujpDvU4aGmd8XNAtY2U55SKmnNOWVLFEdVrl_YzeKeNTeMDf3rEq8neyt_R2RGUvk6PVh1NfXlwIZlZb-Ye1zHKi6sv_2E_Hdr9SlXwMQZt5BTsiOGHJCC3JZPf0k8qWZLP9ivFqHAwAZ2y8RentG44L7eJr3bOBZWqozGo1T9Cn_8db3ZITp1J8MkOGvQS-9RieX1FgTAgNeOp_ewnSTjv2w</recordid><startdate>20100401</startdate><enddate>20100401</enddate><creator>Wang, Xu</creator><creator>Jiang, Yanling</creator><creator>Jia, Bingrui</creator><creator>Wang, Fengyu</creator><creator>Zhou, Guangsheng</creator><general>National Research Council of Canada</general><general>NRC Research Press</general><general>Canadian Science Publishing NRC Research Press</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>ISN</scope><scope>ISR</scope><scope>7SN</scope><scope>7SS</scope><scope>7T7</scope><scope>8FD</scope><scope>C1K</scope><scope>FR3</scope><scope>P64</scope><scope>RC3</scope><scope>U9A</scope><scope>7ST</scope><scope>7U6</scope><scope>SOI</scope></search><sort><creationdate>20100401</creationdate><title>Comparison of soil respiration among three temperate forests in Changbai Mountains, China</title><author>Wang, Xu ; Jiang, Yanling ; Jia, Bingrui ; Wang, Fengyu ; Zhou, Guangsheng</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c670t-e69b0421a1085277affbce1cbeb15ead2fc3d35fc977b15967b50dd80712231d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2010</creationdate><topic>biogeochemical cycles</topic><topic>Biological and medical sciences</topic><topic>Carbon cycle</topic><topic>Carbon dioxide</topic><topic>Comparative analysis</topic><topic>Coniferous forests</topic><topic>deciduous forests</topic><topic>Environmental aspects</topic><topic>Environmental conditions</topic><topic>equations</topic><topic>Forest ecosystems</topic><topic>Forest floor</topic><topic>forest plantations</topic><topic>Forest soils</topic><topic>forest stands</topic><topic>forest succession</topic><topic>Forestry</topic><topic>Forests</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>gas emissions</topic><topic>Moisture content</topic><topic>Mountains</topic><topic>old-growth forests</topic><topic>Respiration</topic><topic>Soil moisture</topic><topic>soil respiration</topic><topic>Soil temperature</topic><topic>soil water</topic><topic>soil-plant-atmosphere interactions</topic><topic>Soils</topic><topic>Temperate climates</topic><topic>Temperate forests</topic><topic>Temperature</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wang, Xu</creatorcontrib><creatorcontrib>Jiang, Yanling</creatorcontrib><creatorcontrib>Jia, Bingrui</creatorcontrib><creatorcontrib>Wang, Fengyu</creatorcontrib><creatorcontrib>Zhou, Guangsheng</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Gale In Context: Canada</collection><collection>Gale In Context: Science</collection><collection>Ecology Abstracts</collection><collection>Entomology Abstracts (Full archive)</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Engineering Research Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Genetics Abstracts</collection><collection>Environment Abstracts</collection><collection>Sustainability Science Abstracts</collection><collection>Environment Abstracts</collection><jtitle>Canadian journal of forest research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, Xu</au><au>Jiang, Yanling</au><au>Jia, Bingrui</au><au>Wang, Fengyu</au><au>Zhou, Guangsheng</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Comparison of soil respiration among three temperate forests in Changbai Mountains, China</atitle><jtitle>Canadian journal of forest research</jtitle><addtitle>Revue canadienne de recherche forestière</addtitle><date>2010-04-01</date><risdate>2010</risdate><volume>40</volume><issue>4</issue><spage>788</spage><epage>795</epage><pages>788-795</pages><issn>0045-5067</issn><eissn>1208-6037</eissn><coden>CJFRAR</coden><abstract>CO2 efflux from forest soils is an important process in the global carbon cycle; however, effects of stand age and successional status remain uncertain. We compared soil respiration and its relationship to soil carbon content, forest floor mass, root biomass, soil temperature, and soil moisture content among three temperate forest ecosystems in Changbai Mountains, northeastern China, from 2003 to 2005. Forest types included an old-growth, mixed coniferous and broad-leaved primary forest (MN), a middle-aged, broad-leaved secondary forest (BL), and a young coniferous plantation forest (CP). Average annual soil CO2 efflux at BL (1477.9 +/- 61.8 g C·m-2·year-1) was significantly higher than at CP (830.7 +/- 48.7 g C·m-2·year-1) and MN (935.4 +/- 53.3 g C·m-2·year-1). Differences in soil temperature among those sites were not statistically significant but contributed to the differences in annual CO2 efflux. In addition, the temperature response of soil CO2 efflux was higher at MN (Q10 = 2.78) than that at BL (Q10 = 2.17) and CP (Q10 = 2.02). Our results suggest that successional stage affects soil respiration by the differences in substrate quantity and quality, environmental conditions, and root respiration.</abstract><cop>Ottawa, ON</cop><pub>National Research Council of Canada</pub><doi>10.1139/x10-010</doi><tpages>8</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0045-5067 |
| ispartof | Canadian journal of forest research, 2010-04, Vol.40 (4), p.788-795 |
| issn | 0045-5067 1208-6037 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_745703394 |
| source | Alma/SFX Local Collection |
| subjects | biogeochemical cycles Biological and medical sciences Carbon cycle Carbon dioxide Comparative analysis Coniferous forests deciduous forests Environmental aspects Environmental conditions equations Forest ecosystems Forest floor forest plantations Forest soils forest stands forest succession Forestry Forests Fundamental and applied biological sciences. Psychology gas emissions Moisture content Mountains old-growth forests Respiration Soil moisture soil respiration Soil temperature soil water soil-plant-atmosphere interactions Soils Temperate climates Temperate forests Temperature |
| title | Comparison of soil respiration among three temperate forests in Changbai Mountains, China |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-06T14%3A56%3A14IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Comparison%20of%20soil%20respiration%20among%20three%20temperate%20forests%20in%20Changbai%20Mountains,%20China&rft.jtitle=Canadian%20journal%20of%20forest%20research&rft.au=Wang,%20Xu&rft.date=2010-04-01&rft.volume=40&rft.issue=4&rft.spage=788&rft.epage=795&rft.pages=788-795&rft.issn=0045-5067&rft.eissn=1208-6037&rft.coden=CJFRAR&rft_id=info:doi/10.1139/x10-010&rft_dat=%3Cgale_proqu%3EA227866623%3C/gale_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=205393245&rft_id=info:pmid/&rft_galeid=A227866623&rfr_iscdi=true |