Long-Term Carbon Sequestration in Pine Forests under Different Silvicultural and Climatic Regimes in Spain
Proactive silviculture treatments (e.g., thinning) may increase C sequestration contributing to climate change mitigation, although, there are still questions about this effect in Mediterranean pine forests. The aim of this research was to quantify the storage of biomass and soil organic carbon in P...
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creator | Navarro-Cerrillo, Rafael M. Ruiz-Gómez, Francisco J. Camarero, Jesús J. Castillo, Víctor Barberá, Gonzalo G. Palacios-Rodríguez, Guillermo Navarro, Francisco B. Blanco, Juan A. Imbert, Juan B. Cachinero-Vivar, Antonio M. Molina, Antonio J. del Campo, Antonio D. |
description | Proactive silviculture treatments (e.g., thinning) may increase C sequestration contributing to climate change mitigation, although, there are still questions about this effect in Mediterranean pine forests. The aim of this research was to quantify the storage of biomass and soil organic carbon in Pinus forests along a climatic gradient from North to South of the Iberian Peninsula. Nine experimental Pinus spp trials were selected along a latitudinal gradient from the pre-Pyrenees to southern Spain. At each location, a homogeneous area was used as the operational scale, and three thinning intensity treatments: unthinned or control (C), intermediate thinning (LT, removal of 30–40% of the initial basal area) and heavy thinning (HT, removal of 50–60%) were conducted. Growth per unit area (e.g., expressed as basal area increment-BAI), biomass, and Soil Organic Carbon (SOC) were measured as well as three sets of environmental variables (climate, soil water availability and soil chemical and physical characteristics). One-way ANOVA and Structural Equation Modelling (SEM) were used to study the effect of thinning and environmental variables on C sequestration. Biomass and growth per unit area were higher in the control than in the thinning treatments, although differences were only significant for P. halepensis. Radial growth recovered after thinning in all species, but it was faster in the HT treatments. Soil organic carbon (SOC10, 0–10 cm depth) was higher in the HT treatments for P. halepensis and P. sylvestris, but not for P. nigra. SEM showed that Pinus stands of the studied species were beneficed by HT thinning, recovering their growth quickly. The resulting model explained 72% of the variation in SOC10 content, and 89% of the variation in silvicultural condition (basal area and density) after thinning. SOC10 was better related to climate than to silvicultural treatments. On the other hand, soil chemical and physical characteristics did not show significant influence over SOC10- Soil water availability was the latent variable with the highest influence over SOC10. This work is a new contribution that shows the need for forest managers to integrate silviculture and C sequestration in Mediterranean pine plantations. |
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The aim of this research was to quantify the storage of biomass and soil organic carbon in Pinus forests along a climatic gradient from North to South of the Iberian Peninsula. Nine experimental Pinus spp trials were selected along a latitudinal gradient from the pre-Pyrenees to southern Spain. At each location, a homogeneous area was used as the operational scale, and three thinning intensity treatments: unthinned or control (C), intermediate thinning (LT, removal of 30–40% of the initial basal area) and heavy thinning (HT, removal of 50–60%) were conducted. Growth per unit area (e.g., expressed as basal area increment-BAI), biomass, and Soil Organic Carbon (SOC) were measured as well as three sets of environmental variables (climate, soil water availability and soil chemical and physical characteristics). One-way ANOVA and Structural Equation Modelling (SEM) were used to study the effect of thinning and environmental variables on C sequestration. Biomass and growth per unit area were higher in the control than in the thinning treatments, although differences were only significant for P. halepensis. Radial growth recovered after thinning in all species, but it was faster in the HT treatments. Soil organic carbon (SOC10, 0–10 cm depth) was higher in the HT treatments for P. halepensis and P. sylvestris, but not for P. nigra. SEM showed that Pinus stands of the studied species were beneficed by HT thinning, recovering their growth quickly. The resulting model explained 72% of the variation in SOC10 content, and 89% of the variation in silvicultural condition (basal area and density) after thinning. SOC10 was better related to climate than to silvicultural treatments. On the other hand, soil chemical and physical characteristics did not show significant influence over SOC10- Soil water availability was the latent variable with the highest influence over SOC10. This work is a new contribution that shows the need for forest managers to integrate silviculture and C sequestration in Mediterranean pine plantations.</description><identifier>ISSN: 1999-4907</identifier><identifier>EISSN: 1999-4907</identifier><identifier>DOI: 10.3390/f13030450</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>Biomass ; Carbon ; Carbon sequestration ; Climate change ; Climate change mitigation ; Coniferous forests ; Drought ; Environmental policy ; Forest management ; Hypotheses ; International agreements ; Mathematical models ; Moisture content ; Multivariate statistical analysis ; Organic carbon ; Organic soils ; Physical characteristics ; Physical properties ; Pine ; Pine trees ; Pinus ; Pinus halepensis ; Rain ; Silviculture ; Soil chemistry ; Soil water ; Soil water storage ; Structural equation modeling ; Thinning ; Timber ; Trees ; Variance analysis ; Water availability</subject><ispartof>Forests, 2022-03, Vol.13 (3), p.450</ispartof><rights>2022 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c292t-bcaf2a090d2e8d0dc293d411e9d1e53bea380ab5bbe0ba99cd199018f3d6f133</citedby><cites>FETCH-LOGICAL-c292t-bcaf2a090d2e8d0dc293d411e9d1e53bea380ab5bbe0ba99cd199018f3d6f133</cites><orcidid>0000-0003-3470-8640 ; 0000-0002-6524-4335 ; 0000-0003-2436-2922 ; 0000-0002-1999-3415 ; 0000-0001-8786-0211 ; 0000-0002-1294-2148 ; 0000-0002-5279-4215 ; 0000-0001-8782-6873 ; 0000-0003-2166-0633</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27903,27904</link.rule.ids></links><search><creatorcontrib>Navarro-Cerrillo, Rafael M.</creatorcontrib><creatorcontrib>Ruiz-Gómez, Francisco J.</creatorcontrib><creatorcontrib>Camarero, Jesús J.</creatorcontrib><creatorcontrib>Castillo, Víctor</creatorcontrib><creatorcontrib>Barberá, Gonzalo G.</creatorcontrib><creatorcontrib>Palacios-Rodríguez, Guillermo</creatorcontrib><creatorcontrib>Navarro, Francisco B.</creatorcontrib><creatorcontrib>Blanco, Juan A.</creatorcontrib><creatorcontrib>Imbert, Juan B.</creatorcontrib><creatorcontrib>Cachinero-Vivar, Antonio M.</creatorcontrib><creatorcontrib>Molina, Antonio J.</creatorcontrib><creatorcontrib>del Campo, Antonio D.</creatorcontrib><title>Long-Term Carbon Sequestration in Pine Forests under Different Silvicultural and Climatic Regimes in Spain</title><title>Forests</title><description>Proactive silviculture treatments (e.g., thinning) may increase C sequestration contributing to climate change mitigation, although, there are still questions about this effect in Mediterranean pine forests. The aim of this research was to quantify the storage of biomass and soil organic carbon in Pinus forests along a climatic gradient from North to South of the Iberian Peninsula. Nine experimental Pinus spp trials were selected along a latitudinal gradient from the pre-Pyrenees to southern Spain. At each location, a homogeneous area was used as the operational scale, and three thinning intensity treatments: unthinned or control (C), intermediate thinning (LT, removal of 30–40% of the initial basal area) and heavy thinning (HT, removal of 50–60%) were conducted. Growth per unit area (e.g., expressed as basal area increment-BAI), biomass, and Soil Organic Carbon (SOC) were measured as well as three sets of environmental variables (climate, soil water availability and soil chemical and physical characteristics). One-way ANOVA and Structural Equation Modelling (SEM) were used to study the effect of thinning and environmental variables on C sequestration. Biomass and growth per unit area were higher in the control than in the thinning treatments, although differences were only significant for P. halepensis. Radial growth recovered after thinning in all species, but it was faster in the HT treatments. Soil organic carbon (SOC10, 0–10 cm depth) was higher in the HT treatments for P. halepensis and P. sylvestris, but not for P. nigra. SEM showed that Pinus stands of the studied species were beneficed by HT thinning, recovering their growth quickly. The resulting model explained 72% of the variation in SOC10 content, and 89% of the variation in silvicultural condition (basal area and density) after thinning. SOC10 was better related to climate than to silvicultural treatments. On the other hand, soil chemical and physical characteristics did not show significant influence over SOC10- Soil water availability was the latent variable with the highest influence over SOC10. This work is a new contribution that shows the need for forest managers to integrate silviculture and C sequestration in Mediterranean pine plantations.</description><subject>Biomass</subject><subject>Carbon</subject><subject>Carbon sequestration</subject><subject>Climate change</subject><subject>Climate change mitigation</subject><subject>Coniferous forests</subject><subject>Drought</subject><subject>Environmental policy</subject><subject>Forest management</subject><subject>Hypotheses</subject><subject>International agreements</subject><subject>Mathematical models</subject><subject>Moisture content</subject><subject>Multivariate statistical analysis</subject><subject>Organic carbon</subject><subject>Organic soils</subject><subject>Physical characteristics</subject><subject>Physical properties</subject><subject>Pine</subject><subject>Pine trees</subject><subject>Pinus</subject><subject>Pinus halepensis</subject><subject>Rain</subject><subject>Silviculture</subject><subject>Soil chemistry</subject><subject>Soil water</subject><subject>Soil water storage</subject><subject>Structural equation modeling</subject><subject>Thinning</subject><subject>Timber</subject><subject>Trees</subject><subject>Variance analysis</subject><subject>Water availability</subject><issn>1999-4907</issn><issn>1999-4907</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNpNUE1LAzEQDaJgqT34DwKePKxOPrbdHGX9hIJie1-SzaSkbLM12RX896ZWxLnMzGPmzbxHyCWDGyEU3DomQIAs4YRMmFKqkAoWp__qczJLaQs5ykWluJyQ7bIPm2KNcUdrHU0f6Ao_RkxD1IPPnQ_0zQekj33MYKJjsBjpvXcOI4aBrnz36duxG8aoO6qDpXXnd3m3pe-48TtMB4rVXvtwQc6c7hLOfvOUrB8f1vVzsXx9eqnvlkXLFR8K02rHNSiwHCsLNqPCSsZQWYalMKhFBdqUxiAYrVRrszxglRN2ng0QU3J1pN3H_kdJs-3HGPLFhs8ll1KUSuWp6-NUG_uUIrpmH_Pf8ath0BzMbP7MFN9rpWd_</recordid><startdate>20220301</startdate><enddate>20220301</enddate><creator>Navarro-Cerrillo, Rafael M.</creator><creator>Ruiz-Gómez, Francisco J.</creator><creator>Camarero, Jesús J.</creator><creator>Castillo, Víctor</creator><creator>Barberá, Gonzalo G.</creator><creator>Palacios-Rodríguez, Guillermo</creator><creator>Navarro, Francisco B.</creator><creator>Blanco, Juan A.</creator><creator>Imbert, Juan B.</creator><creator>Cachinero-Vivar, Antonio M.</creator><creator>Molina, Antonio J.</creator><creator>del Campo, Antonio D.</creator><general>MDPI AG</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7SN</scope><scope>7SS</scope><scope>7X2</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>M0K</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PYCSY</scope><orcidid>https://orcid.org/0000-0003-3470-8640</orcidid><orcidid>https://orcid.org/0000-0002-6524-4335</orcidid><orcidid>https://orcid.org/0000-0003-2436-2922</orcidid><orcidid>https://orcid.org/0000-0002-1999-3415</orcidid><orcidid>https://orcid.org/0000-0001-8786-0211</orcidid><orcidid>https://orcid.org/0000-0002-1294-2148</orcidid><orcidid>https://orcid.org/0000-0002-5279-4215</orcidid><orcidid>https://orcid.org/0000-0001-8782-6873</orcidid><orcidid>https://orcid.org/0000-0003-2166-0633</orcidid></search><sort><creationdate>20220301</creationdate><title>Long-Term Carbon Sequestration in Pine Forests under Different Silvicultural and Climatic Regimes in Spain</title><author>Navarro-Cerrillo, Rafael M. ; 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The aim of this research was to quantify the storage of biomass and soil organic carbon in Pinus forests along a climatic gradient from North to South of the Iberian Peninsula. Nine experimental Pinus spp trials were selected along a latitudinal gradient from the pre-Pyrenees to southern Spain. At each location, a homogeneous area was used as the operational scale, and three thinning intensity treatments: unthinned or control (C), intermediate thinning (LT, removal of 30–40% of the initial basal area) and heavy thinning (HT, removal of 50–60%) were conducted. Growth per unit area (e.g., expressed as basal area increment-BAI), biomass, and Soil Organic Carbon (SOC) were measured as well as three sets of environmental variables (climate, soil water availability and soil chemical and physical characteristics). One-way ANOVA and Structural Equation Modelling (SEM) were used to study the effect of thinning and environmental variables on C sequestration. Biomass and growth per unit area were higher in the control than in the thinning treatments, although differences were only significant for P. halepensis. Radial growth recovered after thinning in all species, but it was faster in the HT treatments. Soil organic carbon (SOC10, 0–10 cm depth) was higher in the HT treatments for P. halepensis and P. sylvestris, but not for P. nigra. SEM showed that Pinus stands of the studied species were beneficed by HT thinning, recovering their growth quickly. The resulting model explained 72% of the variation in SOC10 content, and 89% of the variation in silvicultural condition (basal area and density) after thinning. SOC10 was better related to climate than to silvicultural treatments. On the other hand, soil chemical and physical characteristics did not show significant influence over SOC10- Soil water availability was the latent variable with the highest influence over SOC10. 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subjects | Biomass Carbon Carbon sequestration Climate change Climate change mitigation Coniferous forests Drought Environmental policy Forest management Hypotheses International agreements Mathematical models Moisture content Multivariate statistical analysis Organic carbon Organic soils Physical characteristics Physical properties Pine Pine trees Pinus Pinus halepensis Rain Silviculture Soil chemistry Soil water Soil water storage Structural equation modeling Thinning Timber Trees Variance analysis Water availability |
title | Long-Term Carbon Sequestration in Pine Forests under Different Silvicultural and Climatic Regimes in Spain |
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