Reforestation with loblolly pine can restore the initial soil carbon stock relative to a subtropical natural forest after 30years

被引:14
作者
Veloso, Murilo Gomes [1 ,3 ]
Dieckow, Jeferson [1 ]
Zanatta, Josileia Acordi [2 ]
Bayer, Cimelio [3 ]
Higa, Rosana C. V. [2 ]
Brevilieri, Reinaldo C. [1 ]
Comerford, Nicholas B. [4 ]
Stoppe, Aja M. [5 ]
机构
[1] Univ Fed Parana, Programa Posgrad Ciencia Solo, Dept Solos & Engn Agr, Rua Funcionarios 1540, BR-80035050 Curitiba, PR, Brazil
[2] Embrapa Florestas, Estr Ribeira Km 111, BR-83411000 Colombo, PR, Brazil
[3] Univ Fed Rio Grande do Sul, Dept Solos, BR-91540000 Porto Alegre, RS, Brazil
[4] North Florida Res & Educ Ctr, 155 Res Rd, Quincy, FL 32351 USA
[5] Univ Florida, Soil & Water Sci Dept, POB 110290,2181, Gainesville, FL 32611 USA
关键词
Soil carbon accumulation; Physical fractionation; Forest floor; Southern Brazil; ORGANIC-MATTER; CROPPING SYSTEMS; MANAGEMENT INDEX; NITROGEN STOCKS; FRACTIONS; TILLAGE; ACRISOL; STORAGE; ROOT; SEQUESTRATION;
D O I
10.1007/s10342-018-1127-y
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
We hypothesized that long-term loblolly pine (Pinus taeda L.) land-use restores SOC stock and lability of a subtropical Cambisol to the original levels of the natural forest (NF). Additionally, we hypothesized that roots are the major contributor to SOC and that soil stores most of the ecosystem total carbon (ETC). We investigated a chronosequence of loblolly pine land-use of 17 (first rotation) and 32years (second rotation, unthinned or thinned) following clearing of the NF. The original SOC stock to 100cm of NF (209 +/- 9.4MgCha(-1)) was depleted by 22% after 17years of pine, possibly because of intense soil disturbance and low quantity and quality of the residue inputted during the pine stand implementation. However, the SOC stock was restored to the original stock of NF after 32years of pine, with the input of above and belowground biomass at harvest of the first rotation possibly playing a role in this recovery. Thinning did not affect SOC stocks after 1year. The POM-C reduced after 17years and was not recovered after 32years. We could not ascertain in 5-year evaluation whether root or litter was the major contributor to SOC. Soil held 72% of the ETC in NF and 48-59% in pine plantations, confirming that it stores most of the ETC. Overall, long-term loblolly pine land-use seems to restore the original soil carbon stock in this subtropical site, regardless of some lability losses.
引用
收藏
页码:593 / 604
页数:12
相关论文
共 49 条
[1]  
ABNT, 2010, NBR 7989: Pulp and Wood-Determination of Acid-insoluble Lignin
[2]  
[Anonymous], THESIS
[3]  
[Anonymous], 2016, GLOBAL FOREST RESOUR
[4]  
BALBINOT R., 2003, Ciencias Exatas e Naturais, Curitiba, v, V5, n, P59
[5]  
Baldock JA, 2012, HANBOOK SOIL SCI PRO
[6]   Organic matter storage in a sandy clay loam Acrisol affected by tillage and cropping systems in southern Brazil [J].
Bayer, C ;
Mielniczuk, J ;
Amado, TJC ;
Martin-Neto, L ;
Fernandes, SV .
SOIL & TILLAGE RESEARCH, 2000, 54 (1-2) :101-109
[7]   SOIL CARBON FRACTIONS BASED ON THEIR DEGREE OF OXIDATION, AND THE DEVELOPMENT OF A CARBON MANAGEMENT INDEX FOR AGRICULTURAL SYSTEMS [J].
BLAIR, GJ ;
LEFROY, RDB ;
LISE, L .
AUSTRALIAN JOURNAL OF AGRICULTURAL RESEARCH, 1995, 46 (07) :1459-1466
[8]   Influence of site characteristics and thinning intensity on litterfall production in two Pinus sylvestris L. forests in the western Pyrenees [J].
Blanco, Juan A. ;
Imbert, J. Bosco ;
Castillo, Federico J. .
FOREST ECOLOGY AND MANAGEMENT, 2006, 237 (1-3) :342-352
[9]   PARTICULATE SOIL ORGANIC-MATTER CHANGES ACROSS A GRASSLAND CULTIVATION SEQUENCE [J].
CAMBARDELLA, CA ;
ELLIOTT, ET .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1992, 56 (03) :777-783
[10]   Alterations in litter decomposition patterns in tropical montane forests of Colombia: a comparison of oak forests and coniferous plantations [J].
Carlos Loaiza-Usuga, Juan ;
Leon-Pelaez, Juan D. ;
Gonzalez-Hernandez, Maria I. ;
Fernando Gallardo-Lancho, Juan ;
Osorio-Vega, Walter ;
Correa-Londono, Guillermo .
CANADIAN JOURNAL OF FOREST RESEARCH, 2013, 43 (06) :528-533