Soil organic carbon stocks and flows in New Zealand: System development, measurement and modelling
An IPCC-based Carbon Monitoring System (CMS) was developed to monitor soil organic C stocks and flows to assist New Zealand to achieve its CO 2 emissions reduction target under the Kyoto Protocol. Geo-referenced soil C data from 1158 sites (0.3 m depth) were used to assign steady-state soil C stocks...
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Veröffentlicht in: | Canadian journal of soil science 2005-01, Vol.85 (4), p.481-489 |
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creator | Tate, K.R Wilde, R.H Giltrap, D.J Baisden, W.T Saggar, S Trustrum, N.A Scott, N.A Barton, J.P |
description | An IPCC-based Carbon Monitoring System (CMS) was developed to monitor soil organic C stocks and flows to assist New Zealand to achieve its CO
2
emissions reduction target under the Kyoto Protocol. Geo-referenced soil C data from 1158 sites (0.3 m depth) were used to assign steady-state soil C stocks to various combinations of soil class, climate, and land use. Overall, CMS soil C stock estimates are consistent with detailed, stratified soil C measurements at specific sites and over larger regions. Soil C changes accompanying land-use changes were quantified using a national set of land-use effects (LUEs). These were derived using a General Linear Model to include the effects of numeric predictors (e.g., slope angle). Major uncertainties a rise from estimates of changes in the areas involved, the assumption that soil C is at steady state for all land-cover types, and lack of soil C data for some LUEs. Total national soil organic C stocks estimated using the LUEs for 0–0.1, 0.1–0.3, and 0.3–1 m depths were 1300 ± 20, 1590 ± 30, and 1750 ± 70 Tg, respectively. Most soil C is stored in grazing lands (1480 ± 60 Tg to 0.3 m depth), which appear to be at or near steady state; their conversion to exotic forests and shrubland contributed most to the predicted national soil C loss of 0.6 ± 0.2 Tg C yr
-1
during 1990–2000. Predicted and measured soil C changes for the grazing-forestry conversion agreed closely. Other uncertainties in our current soil CMS include: spatially integrated annual changes in soil C for the major land-use changes, lack of soil C change estimates below 0.3 m, C losses from erosion, the contribution of agricultural management of organic soils, and a possible interaction between land use and our soil-climate classification. Our approach could be adapted for use by other countries with land-use-change issues that differ from those in the IPCC default methodology. Key words: Soil organic carbon, land-use change, stocks, flows, measurement, modelling, IPCC |
doi_str_mv | 10.4141/s04-082 |
format | Article |
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2
emissions reduction target under the Kyoto Protocol. Geo-referenced soil C data from 1158 sites (0.3 m depth) were used to assign steady-state soil C stocks to various combinations of soil class, climate, and land use. Overall, CMS soil C stock estimates are consistent with detailed, stratified soil C measurements at specific sites and over larger regions. Soil C changes accompanying land-use changes were quantified using a national set of land-use effects (LUEs). These were derived using a General Linear Model to include the effects of numeric predictors (e.g., slope angle). Major uncertainties a rise from estimates of changes in the areas involved, the assumption that soil C is at steady state for all land-cover types, and lack of soil C data for some LUEs. Total national soil organic C stocks estimated using the LUEs for 0–0.1, 0.1–0.3, and 0.3–1 m depths were 1300 ± 20, 1590 ± 30, and 1750 ± 70 Tg, respectively. Most soil C is stored in grazing lands (1480 ± 60 Tg to 0.3 m depth), which appear to be at or near steady state; their conversion to exotic forests and shrubland contributed most to the predicted national soil C loss of 0.6 ± 0.2 Tg C yr
-1
during 1990–2000. Predicted and measured soil C changes for the grazing-forestry conversion agreed closely. Other uncertainties in our current soil CMS include: spatially integrated annual changes in soil C for the major land-use changes, lack of soil C change estimates below 0.3 m, C losses from erosion, the contribution of agricultural management of organic soils, and a possible interaction between land use and our soil-climate classification. Our approach could be adapted for use by other countries with land-use-change issues that differ from those in the IPCC default methodology. Key words: Soil organic carbon, land-use change, stocks, flows, measurement, modelling, IPCC</description><identifier>ISSN: 0008-4271</identifier><identifier>EISSN: 1918-1841</identifier><identifier>DOI: 10.4141/s04-082</identifier><language>eng</language><subject>biogeochemical cycles ; carbon dioxide ; carbon sequestration ; environmental monitoring ; gas emissions ; land use change ; linear models ; pollution control ; soil organic matter ; systems analysis</subject><ispartof>Canadian journal of soil science, 2005-01, Vol.85 (4), p.481-489</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a272t-6697e71b2ccde2a18ff7eb43e88f31570153d32d7e41d15b14948638bbaae8dc3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Tate, K.R</creatorcontrib><creatorcontrib>Wilde, R.H</creatorcontrib><creatorcontrib>Giltrap, D.J</creatorcontrib><creatorcontrib>Baisden, W.T</creatorcontrib><creatorcontrib>Saggar, S</creatorcontrib><creatorcontrib>Trustrum, N.A</creatorcontrib><creatorcontrib>Scott, N.A</creatorcontrib><creatorcontrib>Barton, J.P</creatorcontrib><title>Soil organic carbon stocks and flows in New Zealand: System development, measurement and modelling</title><title>Canadian journal of soil science</title><description>An IPCC-based Carbon Monitoring System (CMS) was developed to monitor soil organic C stocks and flows to assist New Zealand to achieve its CO
2
emissions reduction target under the Kyoto Protocol. Geo-referenced soil C data from 1158 sites (0.3 m depth) were used to assign steady-state soil C stocks to various combinations of soil class, climate, and land use. Overall, CMS soil C stock estimates are consistent with detailed, stratified soil C measurements at specific sites and over larger regions. Soil C changes accompanying land-use changes were quantified using a national set of land-use effects (LUEs). These were derived using a General Linear Model to include the effects of numeric predictors (e.g., slope angle). Major uncertainties a rise from estimates of changes in the areas involved, the assumption that soil C is at steady state for all land-cover types, and lack of soil C data for some LUEs. Total national soil organic C stocks estimated using the LUEs for 0–0.1, 0.1–0.3, and 0.3–1 m depths were 1300 ± 20, 1590 ± 30, and 1750 ± 70 Tg, respectively. Most soil C is stored in grazing lands (1480 ± 60 Tg to 0.3 m depth), which appear to be at or near steady state; their conversion to exotic forests and shrubland contributed most to the predicted national soil C loss of 0.6 ± 0.2 Tg C yr
-1
during 1990–2000. Predicted and measured soil C changes for the grazing-forestry conversion agreed closely. Other uncertainties in our current soil CMS include: spatially integrated annual changes in soil C for the major land-use changes, lack of soil C change estimates below 0.3 m, C losses from erosion, the contribution of agricultural management of organic soils, and a possible interaction between land use and our soil-climate classification. Our approach could be adapted for use by other countries with land-use-change issues that differ from those in the IPCC default methodology. Key words: Soil organic carbon, land-use change, stocks, flows, measurement, modelling, IPCC</description><subject>biogeochemical cycles</subject><subject>carbon dioxide</subject><subject>carbon sequestration</subject><subject>environmental monitoring</subject><subject>gas emissions</subject><subject>land use change</subject><subject>linear models</subject><subject>pollution control</subject><subject>soil organic matter</subject><subject>systems analysis</subject><issn>0008-4271</issn><issn>1918-1841</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><recordid>eNotUDtPwzAYtBBIlIL4CXhjIeDPdmOHDVXlIVUwhC4slmN_qQJJXNmBqv-elDKd7nQP6Qi5BHYrQcJdYjJjmh-RCRSgM9ASjsmEMaYzyRWckrOUPkeqJBQTUpWhaWmIa9s3jjobq9DTNAT3lajtPa3bsE206ekrbukH2nYU72m5SwN21OMPtmHTYT_c0A5t-o64J3_JLnhs26Zfn5OT2rYJL_5xSlaPi_f5c7Z8e3qZPywzyxUfsjwvFCqouHMeuQVd1worKVDrWsBMMZgJL7hXKMHDrAJZSJ0LXVXWovZOTMn1odfFkFLE2mxi09m4M8DM_hpTMmnGa0bn1cFZ22DsOjbJrErOQDBg41AuxC_d_2Ab</recordid><startdate>20050101</startdate><enddate>20050101</enddate><creator>Tate, K.R</creator><creator>Wilde, R.H</creator><creator>Giltrap, D.J</creator><creator>Baisden, W.T</creator><creator>Saggar, S</creator><creator>Trustrum, N.A</creator><creator>Scott, N.A</creator><creator>Barton, J.P</creator><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20050101</creationdate><title>Soil organic carbon stocks and flows in New Zealand: System development, measurement and modelling</title><author>Tate, K.R ; Wilde, R.H ; Giltrap, D.J ; Baisden, W.T ; Saggar, S ; Trustrum, N.A ; Scott, N.A ; Barton, J.P</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a272t-6697e71b2ccde2a18ff7eb43e88f31570153d32d7e41d15b14948638bbaae8dc3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2005</creationdate><topic>biogeochemical cycles</topic><topic>carbon dioxide</topic><topic>carbon sequestration</topic><topic>environmental monitoring</topic><topic>gas emissions</topic><topic>land use change</topic><topic>linear models</topic><topic>pollution control</topic><topic>soil organic matter</topic><topic>systems analysis</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Tate, K.R</creatorcontrib><creatorcontrib>Wilde, R.H</creatorcontrib><creatorcontrib>Giltrap, D.J</creatorcontrib><creatorcontrib>Baisden, W.T</creatorcontrib><creatorcontrib>Saggar, S</creatorcontrib><creatorcontrib>Trustrum, N.A</creatorcontrib><creatorcontrib>Scott, N.A</creatorcontrib><creatorcontrib>Barton, J.P</creatorcontrib><collection>AGRIS</collection><collection>CrossRef</collection><jtitle>Canadian journal of soil science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Tate, K.R</au><au>Wilde, R.H</au><au>Giltrap, D.J</au><au>Baisden, W.T</au><au>Saggar, S</au><au>Trustrum, N.A</au><au>Scott, N.A</au><au>Barton, J.P</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Soil organic carbon stocks and flows in New Zealand: System development, measurement and modelling</atitle><jtitle>Canadian journal of soil science</jtitle><date>2005-01-01</date><risdate>2005</risdate><volume>85</volume><issue>4</issue><spage>481</spage><epage>489</epage><pages>481-489</pages><issn>0008-4271</issn><eissn>1918-1841</eissn><abstract>An IPCC-based Carbon Monitoring System (CMS) was developed to monitor soil organic C stocks and flows to assist New Zealand to achieve its CO
2
emissions reduction target under the Kyoto Protocol. Geo-referenced soil C data from 1158 sites (0.3 m depth) were used to assign steady-state soil C stocks to various combinations of soil class, climate, and land use. Overall, CMS soil C stock estimates are consistent with detailed, stratified soil C measurements at specific sites and over larger regions. Soil C changes accompanying land-use changes were quantified using a national set of land-use effects (LUEs). These were derived using a General Linear Model to include the effects of numeric predictors (e.g., slope angle). Major uncertainties a rise from estimates of changes in the areas involved, the assumption that soil C is at steady state for all land-cover types, and lack of soil C data for some LUEs. Total national soil organic C stocks estimated using the LUEs for 0–0.1, 0.1–0.3, and 0.3–1 m depths were 1300 ± 20, 1590 ± 30, and 1750 ± 70 Tg, respectively. Most soil C is stored in grazing lands (1480 ± 60 Tg to 0.3 m depth), which appear to be at or near steady state; their conversion to exotic forests and shrubland contributed most to the predicted national soil C loss of 0.6 ± 0.2 Tg C yr
-1
during 1990–2000. Predicted and measured soil C changes for the grazing-forestry conversion agreed closely. Other uncertainties in our current soil CMS include: spatially integrated annual changes in soil C for the major land-use changes, lack of soil C change estimates below 0.3 m, C losses from erosion, the contribution of agricultural management of organic soils, and a possible interaction between land use and our soil-climate classification. Our approach could be adapted for use by other countries with land-use-change issues that differ from those in the IPCC default methodology. Key words: Soil organic carbon, land-use change, stocks, flows, measurement, modelling, IPCC</abstract><doi>10.4141/s04-082</doi><tpages>9</tpages></addata></record> |
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subjects | biogeochemical cycles carbon dioxide carbon sequestration environmental monitoring gas emissions land use change linear models pollution control soil organic matter systems analysis |
title | Soil organic carbon stocks and flows in New Zealand: System development, measurement and modelling |
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