Spatial distribution characteristics of soil organic carbon density in a tropical mountain rainforest of Jianfengling, Hainan Island, China
Forest soil organic carbon ( SOC) is the main component of the terrestrial carbon reservoir, and plays a crucial role in the Earth's carbon cycle. This study aimed to quantify the spatial heterogeneity and distribution patterns of SOC density. The study was conducted in a 60 hm2 forest plot in...
Gespeichert in:
Veröffentlicht in: | Sheng tai xue bao 2015-01, Vol.35 (23), p.7878-7886 |
---|---|
Hauptverfasser: | , , , , , , , |
Format: | Artikel |
Sprache: | chi |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 7886 |
---|---|
container_issue | 23 |
container_start_page | 7878 |
container_title | Sheng tai xue bao |
container_volume | 35 |
creator | Guo, Xiaowei Luo, Tushou Li, Yide Xu, Han Chen, Dexiang Lin, Mingxian Zhou, Zhang Yang, Huai |
description | Forest soil organic carbon ( SOC) is the main component of the terrestrial carbon reservoir, and plays a crucial role in the Earth's carbon cycle. This study aimed to quantify the spatial heterogeneity and distribution patterns of SOC density. The study was conducted in a 60 hm2 forest plot in a tropical mountain rainforest of Jianfengling, Hainan Island, China, using field investigation, laboratory analysis, and geostatistical methods. The results showed that the mean SOC density at different soil profile depths (A [0-10 cm], B [10-30 cm], and C [30-60 cm]) was 2.699, 2.782, 2.434 kg/m2, respectively. The differences for A versus C and, B versus C layers were statistically significant (P < 0.05), but there was no significant difference between A and B layers ( P > 0.05) . Cross-validation results showed that the most fitted models for SOC density at different layers was exponential for A and spherical for B and C. The ranges of SOC density were 54.2 m, 70.9 m, and 97.2 m for A, B, and C, respectively, while |
doi_str_mv | 10.5846/stxb201404180761 |
format | Article |
fullrecord | <record><control><sourceid>proquest</sourceid><recordid>TN_cdi_proquest_miscellaneous_1837343875</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1837343875</sourcerecordid><originalsourceid>FETCH-LOGICAL-p103t-3871aee62c51328e939af7a6cfbc154bebcdfdaf8c75c677205b2f04727126c73</originalsourceid><addsrcrecordid>eNotjjFPwzAQhT2ARCnsjB4ZGjjbSZyMqAJaVIkBmKuLY6dGqR1sR4LfwJ_GCJZ7undP3z1CrhjcVE1Z38b02XFgJZSsAVmzE7JgAFBAK8QZOY_xHUAAE-2CfL9MmCyOtLcxBdvNyXpH1QEDqqRDNq2K1BsavR2pDwM6q6jC0OVYr1206YtaR5Gm4CerMunoZ5cweyEP44OO6RfwZNEZ7YbRumFFN_mGjm7jiK5f0fUhrxfk1OAY9eW_Lsnbw_3relPsnh-367tdMTEQqRCNZKh1zVXFBG90K1o0EmtlOsWqstOd6k2PplGyUrWUHKqOGygll4zXSooluf7jTsF_zLne_mij0mOuov0c96wRUpT5TSV-AFTAaMA</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1837343875</pqid></control><display><type>article</type><title>Spatial distribution characteristics of soil organic carbon density in a tropical mountain rainforest of Jianfengling, Hainan Island, China</title><source>EZB-FREE-00999 freely available EZB journals</source><creator>Guo, Xiaowei ; Luo, Tushou ; Li, Yide ; Xu, Han ; Chen, Dexiang ; Lin, Mingxian ; Zhou, Zhang ; Yang, Huai</creator><creatorcontrib>Guo, Xiaowei ; Luo, Tushou ; Li, Yide ; Xu, Han ; Chen, Dexiang ; Lin, Mingxian ; Zhou, Zhang ; Yang, Huai</creatorcontrib><description>Forest soil organic carbon ( SOC) is the main component of the terrestrial carbon reservoir, and plays a crucial role in the Earth's carbon cycle. This study aimed to quantify the spatial heterogeneity and distribution patterns of SOC density. The study was conducted in a 60 hm2 forest plot in a tropical mountain rainforest of Jianfengling, Hainan Island, China, using field investigation, laboratory analysis, and geostatistical methods. The results showed that the mean SOC density at different soil profile depths (A [0-10 cm], B [10-30 cm], and C [30-60 cm]) was 2.699, 2.782, 2.434 kg/m2, respectively. The differences for A versus C and, B versus C layers were statistically significant (P < 0.05), but there was no significant difference between A and B layers ( P > 0.05) . Cross-validation results showed that the most fitted models for SOC density at different layers was exponential for A and spherical for B and C. The ranges of SOC density were 54.2 m, 70.9 m, and 97.2 m for A, B, and C, respectively, while</description><identifier>ISSN: 1000-0933</identifier><identifier>DOI: 10.5846/stxb201404180761</identifier><language>chi</language><ispartof>Sheng tai xue bao, 2015-01, Vol.35 (23), p.7878-7886</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></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>Guo, Xiaowei</creatorcontrib><creatorcontrib>Luo, Tushou</creatorcontrib><creatorcontrib>Li, Yide</creatorcontrib><creatorcontrib>Xu, Han</creatorcontrib><creatorcontrib>Chen, Dexiang</creatorcontrib><creatorcontrib>Lin, Mingxian</creatorcontrib><creatorcontrib>Zhou, Zhang</creatorcontrib><creatorcontrib>Yang, Huai</creatorcontrib><title>Spatial distribution characteristics of soil organic carbon density in a tropical mountain rainforest of Jianfengling, Hainan Island, China</title><title>Sheng tai xue bao</title><description>Forest soil organic carbon ( SOC) is the main component of the terrestrial carbon reservoir, and plays a crucial role in the Earth's carbon cycle. This study aimed to quantify the spatial heterogeneity and distribution patterns of SOC density. The study was conducted in a 60 hm2 forest plot in a tropical mountain rainforest of Jianfengling, Hainan Island, China, using field investigation, laboratory analysis, and geostatistical methods. The results showed that the mean SOC density at different soil profile depths (A [0-10 cm], B [10-30 cm], and C [30-60 cm]) was 2.699, 2.782, 2.434 kg/m2, respectively. The differences for A versus C and, B versus C layers were statistically significant (P < 0.05), but there was no significant difference between A and B layers ( P > 0.05) . Cross-validation results showed that the most fitted models for SOC density at different layers was exponential for A and spherical for B and C. The ranges of SOC density were 54.2 m, 70.9 m, and 97.2 m for A, B, and C, respectively, while</description><issn>1000-0933</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><recordid>eNotjjFPwzAQhT2ARCnsjB4ZGjjbSZyMqAJaVIkBmKuLY6dGqR1sR4LfwJ_GCJZ7undP3z1CrhjcVE1Z38b02XFgJZSsAVmzE7JgAFBAK8QZOY_xHUAAE-2CfL9MmCyOtLcxBdvNyXpH1QEDqqRDNq2K1BsavR2pDwM6q6jC0OVYr1206YtaR5Gm4CerMunoZ5cweyEP44OO6RfwZNEZ7YbRumFFN_mGjm7jiK5f0fUhrxfk1OAY9eW_Lsnbw_3relPsnh-367tdMTEQqRCNZKh1zVXFBG90K1o0EmtlOsWqstOd6k2PplGyUrWUHKqOGygll4zXSooluf7jTsF_zLne_mij0mOuov0c96wRUpT5TSV-AFTAaMA</recordid><startdate>20150101</startdate><enddate>20150101</enddate><creator>Guo, Xiaowei</creator><creator>Luo, Tushou</creator><creator>Li, Yide</creator><creator>Xu, Han</creator><creator>Chen, Dexiang</creator><creator>Lin, Mingxian</creator><creator>Zhou, Zhang</creator><creator>Yang, Huai</creator><scope>7SN</scope><scope>7ST</scope><scope>7UA</scope><scope>C1K</scope><scope>SOI</scope></search><sort><creationdate>20150101</creationdate><title>Spatial distribution characteristics of soil organic carbon density in a tropical mountain rainforest of Jianfengling, Hainan Island, China</title><author>Guo, Xiaowei ; Luo, Tushou ; Li, Yide ; Xu, Han ; Chen, Dexiang ; Lin, Mingxian ; Zhou, Zhang ; Yang, Huai</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-p103t-3871aee62c51328e939af7a6cfbc154bebcdfdaf8c75c677205b2f04727126c73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>chi</language><creationdate>2015</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Guo, Xiaowei</creatorcontrib><creatorcontrib>Luo, Tushou</creatorcontrib><creatorcontrib>Li, Yide</creatorcontrib><creatorcontrib>Xu, Han</creatorcontrib><creatorcontrib>Chen, Dexiang</creatorcontrib><creatorcontrib>Lin, Mingxian</creatorcontrib><creatorcontrib>Zhou, Zhang</creatorcontrib><creatorcontrib>Yang, Huai</creatorcontrib><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Environment Abstracts</collection><jtitle>Sheng tai xue bao</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Guo, Xiaowei</au><au>Luo, Tushou</au><au>Li, Yide</au><au>Xu, Han</au><au>Chen, Dexiang</au><au>Lin, Mingxian</au><au>Zhou, Zhang</au><au>Yang, Huai</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Spatial distribution characteristics of soil organic carbon density in a tropical mountain rainforest of Jianfengling, Hainan Island, China</atitle><jtitle>Sheng tai xue bao</jtitle><date>2015-01-01</date><risdate>2015</risdate><volume>35</volume><issue>23</issue><spage>7878</spage><epage>7886</epage><pages>7878-7886</pages><issn>1000-0933</issn><abstract>Forest soil organic carbon ( SOC) is the main component of the terrestrial carbon reservoir, and plays a crucial role in the Earth's carbon cycle. This study aimed to quantify the spatial heterogeneity and distribution patterns of SOC density. The study was conducted in a 60 hm2 forest plot in a tropical mountain rainforest of Jianfengling, Hainan Island, China, using field investigation, laboratory analysis, and geostatistical methods. The results showed that the mean SOC density at different soil profile depths (A [0-10 cm], B [10-30 cm], and C [30-60 cm]) was 2.699, 2.782, 2.434 kg/m2, respectively. The differences for A versus C and, B versus C layers were statistically significant (P < 0.05), but there was no significant difference between A and B layers ( P > 0.05) . Cross-validation results showed that the most fitted models for SOC density at different layers was exponential for A and spherical for B and C. The ranges of SOC density were 54.2 m, 70.9 m, and 97.2 m for A, B, and C, respectively, while</abstract><doi>10.5846/stxb201404180761</doi><tpages>9</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 1000-0933 |
ispartof | Sheng tai xue bao, 2015-01, Vol.35 (23), p.7878-7886 |
issn | 1000-0933 |
language | chi |
recordid | cdi_proquest_miscellaneous_1837343875 |
source | EZB-FREE-00999 freely available EZB journals |
title | Spatial distribution characteristics of soil organic carbon density in a tropical mountain rainforest of Jianfengling, Hainan Island, China |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-05T21%3A02%3A42IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Spatial%20distribution%20characteristics%20of%20soil%20organic%20carbon%20density%20in%20a%20tropical%20mountain%20rainforest%20of%20Jianfengling,%20Hainan%20Island,%20China&rft.jtitle=Sheng%20tai%20xue%20bao&rft.au=Guo,%20Xiaowei&rft.date=2015-01-01&rft.volume=35&rft.issue=23&rft.spage=7878&rft.epage=7886&rft.pages=7878-7886&rft.issn=1000-0933&rft_id=info:doi/10.5846/stxb201404180761&rft_dat=%3Cproquest%3E1837343875%3C/proquest%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1837343875&rft_id=info:pmid/&rfr_iscdi=true |