A cost-efficient method to assess carbon stocks in tropical peat soil

被引:74
作者
Warren, M. W. [1 ]
Kauffman, J. B. [2 ,3 ]
Murdiyarso, D. [3 ,4 ]
Anshari, G. [5 ]
Hergoualc'h, K. [3 ]
Kurnianto, S. [3 ,6 ]
Purbopuspito, J. [3 ]
Gusmayanti, E. [5 ]
Afifudin, M. [5 ]
Rahajoe, J. [7 ]
Alhamd, L. [7 ]
Limin, S. [8 ]
Iswandi, A. [9 ]
机构
[1] US Forest Serv, USDA, No Res Stn, Durham, NH 03824 USA
[2] Oregon State Univ, Dept Fisheries & Wildlife, Corvallis, OR 97331 USA
[3] Jalan CIFOR, Ctr Int Forestry Res, Situ Gede 16115, Bogor Barat, Indonesia
[4] Bogor Agr Univ, Dept Geophys & Meteorol, Jalan Meranti 16680, Darmaga Bogor, Indonesia
[5] Univ Tanjungpura, Ctr Wetlands People & Biodivers, Pontianak 78124, West Kalimantan, Indonesia
[6] Univ New Hampshire, Inst Study Earth Oceans & Space, Durham, NH 03824 USA
[7] Cibinong Sci Ctr, Sci Res Ctr Biol, Indonesian Inst, Cibinong, West Java, Indonesia
[8] Univ Palangka Raya, CIMTROP, Cent Kalimantan 73111, Indonesia
[9] Bogor Agr Univ, Dept Soil Sci & Land Management, Lab Soil Biotechnol, Jalan Meranti 16680, Indonesia
关键词
INDONESIAN PEATLANDS; LAND-USE; KALIMANTAN; EMISSIONS; DEGRADATION; DYNAMICS; MALAYSIA; SUMATRA; BORNEO; POOL;
D O I
10.5194/bg-9-4477-2012
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Estimation of belowground carbon stocks in tropical wetland forests requires funding for laboratory analyses and suitable facilities, which are often lacking in developing nations where most tropical wetlands are found. It is therefore beneficial to develop simple analytical tools to assist belowground carbon estimation where financial and technical limitations are common. Here we use published and original data to describe soil carbon density (kgC m(-3); C-d) as a function of bulk density (gC cm(-3); B-d), which can be used to rapidly estimate belowground carbon storage using B-d measurements only. Predicted carbon densities and stocks are compared with those obtained from direct carbon analysis for ten peat swamp forest stands in three national parks of Indonesia. Analysis of soil carbon density and bulk density from the literature indicated a strong linear relationship (C-d = B-d x 495.14+5.41, R-2 = 0.93, n = 151) for soils with organic C content > 40 %. As organic C content decreases, the relationship between C-d and B-d becomes less predictable as soil texture becomes an important determinant of C-d. The equation predicted belowground C stocks to within 0.92% to 9.57% of observed values. Average bulk density of collected peat samples was 0.127 g cm(-3), which is in the upper range of previous reports for Southeast Asian peatlands. When original data were included, the revised equation C-d = B-d x 468.76 + 5.82, with R-2 = 0.95 and n = 712, was slightly below the lower 95% confidence interval of the original equation, and tended to decrease C-d estimates. We recommend this last equation for a rapid estimation of soil C stocks for well-developed peat soils where C content > 40 %.
引用
收藏
页码:4477 / 4485
页数:9
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