Influence of soil aggregate size on greenhouse gas emission and uptake rate from tropical peat soil in forest and different oil palm development years
The influence of oil palm development on tropical peat soil decomposition rate was investigated by an incubation experiment. Soil samples from soil surface and around underground water table were taken from forest site, and oil palm site at 1st and 9th year after development. The soil samples were s...
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| Published in | Geoderma Vol. 185-186; pp. 1 - 5 |
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| Main Authors | , , |
| Format | Journal Article |
| Language | English |
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Elsevier B.V
01.09.2012
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| Abstract | The influence of oil palm development on tropical peat soil decomposition rate was investigated by an incubation experiment. Soil samples from soil surface and around underground water table were taken from forest site, and oil palm site at 1st and 9th year after development. The soil samples were sieved into 0–2mm, 2–8mm and 8–20mm and analyzed for carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) fluxes.
The development of oil palm did not change the CO2 emissions and showed inconsistent influence on CH4 flux according to aggregate size, while significantly higher N2O emissions were found for aggregates 0–2mm at high moisture of oil palm plantation soils compared with the original forest. Nitrous oxide fluxes showed significant positive correlation with the CO2 flux, which indicated that soil organic matter decomposition was closely related to the N2O production. On the other hand, CH4 flux showed clear emission for aggregates bigger than 2mm, while aggregates size 0–2mm showed consistent CH4 uptake. These results showed that investigation of greenhouse gas emissions in tropical peat soil must take into account the aggregate characteristics of the soil, which are inhomogeneous and mixed with fresh organic matter.
► Greenhouse gas flux of incubation was influenced by the aggregate size. ► N2O emission was highly correlated with CO2 emission. ► Oil palm development resulted in higher N2O emissions compared to forest. |
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| AbstractList | The influence of oil palm development on tropical peat soil decomposition rate was investigated by an incubation experiment. Soil samples from soil surface and around underground water table were taken from forest site, and oil palm site at 1st and 9th year after development. The soil samples were sieved into 0–2mm, 2–8mm and 8–20mm and analyzed for carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) fluxes.
The development of oil palm did not change the CO2 emissions and showed inconsistent influence on CH4 flux according to aggregate size, while significantly higher N2O emissions were found for aggregates 0–2mm at high moisture of oil palm plantation soils compared with the original forest. Nitrous oxide fluxes showed significant positive correlation with the CO2 flux, which indicated that soil organic matter decomposition was closely related to the N2O production. On the other hand, CH4 flux showed clear emission for aggregates bigger than 2mm, while aggregates size 0–2mm showed consistent CH4 uptake. These results showed that investigation of greenhouse gas emissions in tropical peat soil must take into account the aggregate characteristics of the soil, which are inhomogeneous and mixed with fresh organic matter.
► Greenhouse gas flux of incubation was influenced by the aggregate size. ► N2O emission was highly correlated with CO2 emission. ► Oil palm development resulted in higher N2O emissions compared to forest. The influence of oil palm development on tropical peat soil decomposition rate was investigated by an incubation experiment. Soil samples from soil surface and around underground water table were taken from forest site, and oil palm site at 1st and 9th year after development. The soil samples were sieved into 0-2 mm, 2-8 mm and 8-20 mm and analyzed for carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) fluxes. The development of oil palm did not change the CO2 emissions and showed inconsistent influence on CH4 flux according to aggregate size, while significantly higher N2O emissions were found for aggregates 0-2 mm at high moisture of oil palm plantation soils compared with the original forest. Nitrous oxide fluxes showed significant positive correlation with the CO2 flux, which indicated that soil organic matter decomposition was closely related to the N2O production. On the other hand, CH4 flux showed clear emission for aggregates bigger than 2 mm, while aggregates size 0-2 mm showed consistent CH4 uptake. These results showed that investigation of greenhouse gas emissions in tropical peat soil must take into account the aggregate characteristics of the soil, which are inhomogeneous and mixed with fresh organic matter. The influence of oil palm development on tropical peat soil decomposition rate was investigated by an incubation experiment. Soil samples from soil surface and around underground water table were taken from forest site, and oil palm site at 1st and 9th year after development. The soil samples were sieved into 0–2mm, 2–8mm and 8–20mm and analyzed for carbon dioxide (CO₂), methane (CH₄) and nitrous oxide (N₂O) fluxes. The development of oil palm did not change the CO₂ emissions and showed inconsistent influence on CH₄ flux according to aggregate size, while significantly higher N₂O emissions were found for aggregates 0–2mm at high moisture of oil palm plantation soils compared with the original forest. Nitrous oxide fluxes showed significant positive correlation with the CO₂ flux, which indicated that soil organic matter decomposition was closely related to the N₂O production. On the other hand, CH₄ flux showed clear emission for aggregates bigger than 2mm, while aggregates size 0–2mm showed consistent CH₄ uptake. These results showed that investigation of greenhouse gas emissions in tropical peat soil must take into account the aggregate characteristics of the soil, which are inhomogeneous and mixed with fresh organic matter. |
| Author | Melling, Lulie Kimura, Sonoko D. Goh, Kah Joo |
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| References | Melling, Hatano, Goh (bb0045) 2005; 57B Denef, Six, Paustian, Merckx (bb0005) 2001; 33 Gulledge, Hywna, Cavanaugh, Steudler (bb0015) 2004; 49 Flessa, Wild, Klemisch, Pfadenhauer (bb0010) 1998; 49 Moore, Dalva (bb0080) 1997; 29 Miettinen, Wang, Hooijer, Liew (bb0050) 2011; 22 Sey, Manceur, Whalen, Gregorich, Rochette (bb0070) 2008; 40 Kremen, Bear, Shavit, Shaviv (bb0030) 2005; 39 Department of Statistics Malaysia (bb1000) 2011 Takakai, Morishita, Hashidoko, Darung, Kuramochi, Dohong, Limin, Hatano (bb0075) 2006; 52 Maltby, Immirzi (bb0040) 1993; 27 Page, Rieley, Shotyk, Weiss (bb0065) 1999; 354 Kalbitz, Geyer (bb0025) 2002; 33 Jastrow, Amonette, Bailey (bb0020) 2007; 80 Kristiansen, Schjnning, Thomsen, Olesen, Kristensen, Christensen (bb0035) 2006; 137 Department of Statistics Malaysia (10.1016/j.geoderma.2012.03.026_bb1000) 2011 Kremen (10.1016/j.geoderma.2012.03.026_bb0030) 2005; 39 Takakai (10.1016/j.geoderma.2012.03.026_bb0075) 2006; 52 Miettinen (10.1016/j.geoderma.2012.03.026_bb0050) 2011; 22 Kristiansen (10.1016/j.geoderma.2012.03.026_bb0035) 2006; 137 Moore (10.1016/j.geoderma.2012.03.026_bb0080) 1997; 29 Sey (10.1016/j.geoderma.2012.03.026_bb0070) 2008; 40 Maltby (10.1016/j.geoderma.2012.03.026_bb0040) 1993; 27 Page (10.1016/j.geoderma.2012.03.026_bb0065) 1999; 354 Flessa (10.1016/j.geoderma.2012.03.026_bb0010) 1998; 49 Melling (10.1016/j.geoderma.2012.03.026_bb0045) 2005; 57B Kalbitz (10.1016/j.geoderma.2012.03.026_bb0025) 2002; 33 Denef (10.1016/j.geoderma.2012.03.026_bb0005) 2001; 33 Gulledge (10.1016/j.geoderma.2012.03.026_bb0015) 2004; 49 Jastrow (10.1016/j.geoderma.2012.03.026_bb0020) 2007; 80 |
| References_xml | – volume: 354 start-page: 1 year: 1999 end-page: 13 ident: bb0065 article-title: Interdependence of peat and vegetation in a tropical peat swamp forest publication-title: Proceedings of the Royal Society of London contributor: fullname: Weiss – volume: 27 start-page: 999 year: 1993 end-page: 1023 ident: bb0040 article-title: Carbon dynamics in peatlands and other wetland soils. 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| SubjectTerms | Aggregate size carbon dioxide Elaeis guineensis forest soils forests greenhouse gas emissions Greenhouse gas flux Incubation methane methane production nitrous oxide Oil palm plantation organic matter Peat soil peat soils soil organic matter soil sampling Tropical forest water table |
| Title | Influence of soil aggregate size on greenhouse gas emission and uptake rate from tropical peat soil in forest and different oil palm development years |
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