Assessing Intra-Site Variability of Compaction Magnitudes and Carbon Emissions in an Oil Palm Plantation on the Drained Tropical Peatland

Author(s)

Marshall Kana Samuel ,

Download Full PDF Pages: 33-47 | Views: 235 | Downloads: 79 | DOI: 10.5281/zenodo.7188967

Volume 6 - August 2022 (08)

Abstract

Change of land use from peat secondary forest (SF) to oil palm plantation (OP) involves several specific practices that may contribute to soil property heterogeneity. Specifically, artificial compaction as marked by increased bulk density value was assessed in relation to repeating microsites identified in standard plantation design, and defined as harvesting path ‘HP’, under canopy ‘UC’, frond pile ‘FP’, and far from tree ‘FF’. Along with soil sampling at 25 cm depth, carbon emissions were measured within OP microsites using dynamic closed-chambers. The samples were collected at three different oil palm ages, namely A1 (15 years, 1st generation), A2 (9 years, 2nd generation), and A3 (2 years, second generation and previously burned) between November 2015 and May 2016. Compaction, as indicated by bulk density values, had been comparable among microsites but differed among OP ages. This suggests that compaction source within OP was solely due to period of drainage and the previous fire event. Meanwhile, CO2 emission was positively correlated with water proxies and pH, signifying the important of rainfall to dilute soil pH. Here we suggest that this leads to an increase in the solubility of organic matter and subsequently, an increase the availability of labile C to microbes, thus enhancing respiration and CO2 production. Despite absence of evidence that directly indicated effect of compaction, microsites emission variation was clear and employed to determine Surface Area Correction (SAC) for land use emission factor (EF) calculation. The value retrieved for EF using SAC was between the default value proposed by IPCC (2010) and Environmental Protection Agency (EPA) (2014). The SAC was also applied to estimate EF reduction by limiting the number of palms per hectare and by converting FP microsites into HP and FF, which resulted in up to 11% of carbon reduction. Hence, identification of microsites emission variability offers data for complementary strategies in managing OP across tropical peatlands.

Keywords

Agriculture management, Bulk density, Compaction, Carbon emission, Microsites, Oil palm ages 

References

i.               Adeolu, A.R., Mohammad, T.A., Daud, N.N.N., Mustapha, S., Sayok, A.K., Rory, P., and Stephanie, E., (2015). Investigating the Influence of Rainfall on Soil Carbon Quantity in a Tropical Peatland, in: Procedia Environmental Sciences. Elsevier B.V., pp. 44–49.

ii.             Al-shammary, A.A.G., Kouzani, A.Z., Kaynak, A., Khoo, S.Y., Norton, M., and Gates, W. (2018). Soil Bulk Density Estimation Methods: A Review. Pedosphere 28, 581–596. https://doi.org/10.1016/S1002-0160(18)60034-7

iii.           Alakukku, L., 1996. Persistence of soil compaction due to high axle load traffic. II. Long-term effects on the properties of fine-textured and organic soils. Soil Tillage Res. 37, 223–238. https://doi.org/10.1016/0167-1987(96)01017-3

iv.            Anuar, A.R., Goh, K.J., Heoh, T.B., and Ahmed, O.H. (2008). Spatial Variability of Soil Inorganic N in a Mature Oil Palm Plantation in Sabah, Malaysia. Am. J. Appl. Sci. 5, 1239–1246. https://doi.org/10.3844/ajassp.2008.1239.1246

v.              Ariyanti, M., Yahya, S., Murtilaksono, K., Suwarto, and Siregar, H.H. (2016). Water Balance in Oil Palm Plantation with Ridge Terrace and Nephrolepis biserrata as Cover Crop. J. Trop. Crop Sci. 3, 35–41.

vi.            Blake, G.R. (1958). Particle Density, in: Black, C.A. (Ed.), Methods of Soil Analysis, Part 1, Agronomy. American Society of Agronomy, Madison, Wisc., pp. 371–373. https://doi.org/sis.agr.gc.ca/cansis/publications/manuals/1984-30/84-030-particle-density.pdf

vii.          Brown, M.B. and Forsythe, A.B. (1974). Robust Tests for the Equality of Variances. J. Am. Stat. Assoc. 69, 364. https://doi.org/10.2307/2285659

viii.        Carlson, K.M., Goodman, L.K., and May-Tobin, C.C. (2015). Modeling relationships between water table depth and peat soil carbon loss in Southeast Asian plantations. Environ. Res. Lett. 10, 074006.

ix.            Chalker-Scott, L. (2007). Impact of Mulches on Landscape Plants and the Environment-A Review. J. Environ. Horiculture 25, 239–249.

x.              Comeau, L.-P., Hergoualc’h, K., Smith, J.U., and Verchot, L. (2013). Conversion of intact peat swamp forest to oil palm plantation: Effects on soil CO2 fluxes in Jambi, Sumatra.

xi.            Dariah, A., Marwanto, S., and Agus, F. (2014). Root- and peat-based CO2 emissions from oil palm plantations. Mitig. Adapt. Strateg. Glob. Chang. 19, 831–843. https://doi.org/10.1007/s11027-013-9515-6

xii.          Drösler, M., Verchot, L. V., Freibauer, A., Pan, G., Evans, C.D., Bourbonniere, R.A., Alm, J.P., Page, S., Agus, F., Hergoualc’h, K., Couwenberg, J., Jauhiainen, J., Sabiham, S., Wang, C., Srivastava, N., Borgeau-Chavez, L., Hooijer, A., Minkkinen, K., French, N., Strand, T., Sirin, A., Mickler, R., Tansey, K., and Larkin, N. (2014). Chapter 2: Drained inland organic soils, in: 2013 Supplement to the 2006 IPCC Guidelines for National Greenhouse Gas Inventories: Wetlands. Intergovernmental Panel on Climate Change (IPCC), pp. 1–79.

xiii.        EPA (2014). Emission Factor for Tropical Peatlands Drained for Oil Palm Cultivation Peer - Review Report Emission (EPA-420-R-14-030 ).

xiv.        Firdaus, M.S., Gandaseca, S., and Ahmed, O.H. (2011). Effect of drainage and land clearing on selected peat soil physical properties of secondary peat swamp forest. Int. J. Phys. Sci. 6, 5462–5466. https://doi.org/10.5897/IJPS11.598

xv.          Firdaus, M.S., Gandaseca, S., Haruna Ahmed, O., and Muhamad Majid, N. (2012). Comparison of selected physical properties of deep peat within different ages of oil palm plantation. Int. J. Phys. Sci. 7, 5711–5716. https://doi.org/10.5897/IJPS12.441

xvi.        Fraser, F.C., Corstanje, R., Deeks, L.K., Harris, J.A., Pawlett, M., Todman, L.C., Whitmore, A.P., and Ritz, K. (2016). On the origin of carbon dioxide released from rewetted soils. Soil Biol. Biochem. 101, 1–5. https://doi.org/10.1016/j.soilbio.2016.06.032

xvii.      Hajon, S.K., Mos, H., Jantan, N., and  Mh, H. (2018). Classification of Tropical Peat in Malaysia. Oil Palm Bull. 76, 1–7. https://doi.org/palmoilis.mpob.gov.my/publications/OPB/opb76-khadijah.pdf

xviii.    Henson, I.E., Betitis, T., Tomda, Y., and Chase, L.D.C. (2012). The estimation of frond base biomass (FBB) of oil palm. J. Oil Palm Res. 24, 1473–1479.

xix.        Hooijer, A., Page, S., Jauhiainen, J., Lee, W.A., Lu, X.X., Idris, A., and Anshari, G. (2012). Subsidence and carbon loss in drained tropical peatlands. Biogeosciences 9, 1053–1071. https://doi.org/10.5194/bg-9-1053-2012

xx.          Huat, B.B.K., Kazemian, S., Prasad, A., and Barghchi, M. (2011). State of an art review of peat: General perspective. Int. J. Phys. Sci. 6, 1988–1996. https://doi.org/10.5897/IJPS11.192

xxi.        Ishikura, K., Hirano, T., Okimoto, Y., Hirata, R., Kiew, F., Melling, L., Aeries, E.B., Lo, K.S., Musin, K.K., Waili, J.W., Wong, G.X., and Ishii, Y. (2018). Soil carbon dioxide emissions due to oxidative peat decomposition in an oil palm plantation on tropical peat. Agric. Ecosyst. Environ. 254, 202–212. https://doi.org/10.1016/j.agee.2017.11.025

xxii.      Ishikura, K., Yamada, H., Toma, Y., Takakai, F., Morishita, T., Darung, U., Limin, A., Limin, S.H., and Hatano, R. (2017). Effect of groundwater level fluctuation on soil respiration rate of tropical peatland in Central Kalimantan, Indonesia. Soil Sci. Plant Nutr. 63, 1–13. https://doi.org/10.1080/00380768.2016.1244652

xxiii.    Jauhiainen, J., Hooijer, A., and Page, S.E. (2012). Carbon dioxide emissions from an Acacia plantation on peatland in Sumatra, Indonesia. Biogeosciences 9, 617–630. https://doi.org/10.5194/bg-9-617-2012

xxiv.     Jauhiainen, J., Kerojoki, O., Silvennoinen, H., Limin, S., and Vasander, H. (2014). Heterotrophic respiration in drained tropical peat is greatly affected by temperature—a passive ecosystem cooling experiment. Environ. Res. Lett. 9, 105013. https://doi.org/10.1088/1748-9326/9/10/105013

xxv.       Könönen, M., Jauhiainen, J., Laiho, R., Kusin, K., and Vasander, H. (2015). Physical and chemical properties of tropical peat under stabilised land uses. Mires Peat 16, 1–13. https://doi.org/mires-and-peat.net/media/map16/map_16_08.pdf

xxvi.     Lal, R. (2004). Soil carbon sequestration to mitigate climate change. Geoderma 123, 1–22. https://doi.org/10.1016/j.geoderma.2004.01.032

xxvii.   Lestariningsih, I.D., Widianto, and Hairiah, K. (2013). Assessing Soil Compaction with Two Different Methods of Soil Bulk Density Measurement in Oil Palm Plantation Soil, in: Procedia Environmental Sciences. Elsevier B.V., pp. 172–178. https://doi.org/10.1016/j.proenv.2013.02.026

xxviii. Lim Kim Choo, L.N. and Ahmed, O.H. (2014). Partitioning Carbon Dioxide Emission and Assessing Dissolved Organic Carbon Leaching of a Drained Peatland Cultivated with Pineapple at Saratok, Malaysia. Sci. World J. 2014, 1–9. https://doi.org/10.1155/2014/906021

xxix.     Luskin, M.S., and Potts, M.D. (2011). Microclimate and habitat heterogeneity through the oil palm lifecycle. Basic Appl. Ecol. 12, 540–551. https://doi.org/10.1016/j.baae.2011.06.004

xxx.       Malaysian Meteorological Department (MMD) Annual Report, 2016.

xxxi.     Mancinelli, R., Marinari, S., Brunetti, P., Radicetti, E., and Campiglia, E. (2015). Organic mulching, irrigation and fertilization affect soil CO2 emission and C storage in tomato crop in the Mediterranean environment. Soil Tillage Res. 152, 39–51.

xxxii.   Marshall, C., Large, D.J., Athab, A., Evers, S.L., Sowter, A., Marsh, S., and Sjögersten, S. (2018). Monitoring tropical peat related settlement using ISBAS InSAR, Kuala Lumpur International Airport (KLIA). Eng. Geol. 244, 57–65.

xxxiii. Marwanto, S., Sabiham, S., and Funakawa, S. (2019). Importance of CO2 production in subsoil layers of drained tropical peatland under mature oil palm plantation. Soil Tillage Res. 186, 206–213. https://doi.org/10.1016/j.still.2018.10.021

xxxiv. Marwanto, S., Watanabe, T., Iskandar, W., Sabiham, S., and Funakawa, S. (2018). Effects of seasonal rainfall and water table movement on the soil solution composition of tropical peatland. Soil Sci. Plant Nutr. 64, 386–395. https://doi.org/10.1080/00380768.2018.1436940

xxxv.   Matysek, M., Evers, S., Samuel, M.K., and Sjogersten, S. (2018). High heterotrophic CO2 emissions from a Malaysian oil palm plantations during dry-season. Wetl. Ecol. Manag. 26, 415–424. https://doi.org/10.1007/s11273-017-9583-6

xxxvi. Melling, L., Hatano, R., and Goh, K.J. (2005a). Soil CO2 flux from three ecosystems in tropical peatland of Sarawak, Malaysia. Tellus B 57, 1–11. https://doi.org/www.tellusb.net/index.php/tellusb/article/view/16772

xxxvii.    Melling, L., Hatano, R., and Goh, K.J., (2005b). Methane fluxes from three ecosystems in tropical peatland of Sarawak, Malaysia. Soil Biol. Biochem. 37, 1445–1453. https://doi.org/10.1016/j.soilbio.2005.01.001

xxxviii.  Miao, G., Noormets, A., Domec, J.-C.C., Trettin, C.C., McNulty, S.G., Sun, G., and King, J.S. (2013). The effect of water table fluctuation on soil respiration in a lower coastal plain forested wetland in the southeastern U.S. J. Geophys. Res. Biogeosciences 118, 1748–1762. https://doi.org/10.1002/2013JG002354

xxxix. Moore, T.R. and Dalva, M. (1997). Methane and carbon dioxide exchange potentials of peat soils in aerobic and anaerobic laboratory incubations. Soil Biol. Biochem. 29, 1157–1164. https://doi.org/10.1016/S0038-0717(97)00037-0

xl.            Mutert, E., Fairhurst, T.H.H., and von Uexküll, H.R.R. (1999). Agronomic Management of Oil Palms on Deep Peat. Better Crop. Int. 13, 22–27. https://doi.org/http://www.ipni.net/publication/bci.nsf/0/963CC0D08521253185257BBA006E791B/$FILE/Better%20Crops%20International%201999-1%20p22.pdf

xli.          Parkin, T.B., and Venterea, R.T. (2010). Sampling Protocols. Chapter 3. Chamber-Based Trace Gas Flux Measurements. Sampl. Protoc. 2010, 1–39. https://doi.org/www.ars.usda.gov/ARSUserFiles/np212/chapter 3. gracenet Trace Gas Sampling protocols.pdf

xlii.        Price, J.S. (2003). Role and character of seasonal peat soil deformation on the hydrology of undisturbed and cutover peatlands. Water Resour. Res. 39, 1–10.

xliii.      Price, J.S., and Schlotzhauer, S.M. (1999). Importance of shrinkage and compression in determining water storage changes in peat: the case of a mined peatland. Hydrol. Process. 13, 2591–2601.

xliv.      Pschenyckyj, C.M., Clark, J.M., Shaw, L.J., Griffiths, R.I., and Evans, C.D. (2019). Effects of acidity on dissolved organic carbon in organic soil extracts, pore water and surface litters. Sci. Total Environ. 703, 135585. https://doi.org/10.1016/j.scitotenv.2019.135585

xlv.        Ritzema, H., Limin, S., Kusin, K., Jauhiainen, J., and Wösten, H. (2014). Canal blocking strategies for hydrological restoration of degraded tropical peatlands in Central Kalimantan, Indonesia. Catena 114, 11–20.

xlvi.      Sakata, R., Shimada, S., Arai, H., Yoshioka, N., Yoshioka, R., Aoki, H., Kimoto, N., Sakamoto, A., Melling, L., and Inubushi, K. (2015). Effect of soil types and nitrogen fertilizer on nitrous oxide and carbon dioxide emissions in oil palm plantations. Soil Sci. Plant Nutr. 61, 48–60. https://doi.org/10.1080/00380768.2014.960355

xlvii.    Shapiro, S.S., and Wilk, M.B. (2006). An Analysis of Variance Test for Normality (Complete Samples). Biometrika. https://doi.org/10.2307/2333709

xlviii.  Shestak, C.J., and Busse, M.D. (2005). Compaction Alters Physical but Not Biological Indices of Soil Health. Soil Sci. Soc. Am. J. 69, 236.

xlix.      Tonks, A.J., Aplin, P., Beriro, D.J., Cooper, H., Evers, S., Vane, C.H., and Sjögersten, S. (2017). Impacts of conversion of tropical peat swamp forest to oil palm plantation on peat organic chemistry, physical properties and carbon stocks. Geoderma 289, 36–45. https://doi.org/10.1016/j.geoderma.2016.11.018

l.               Tukey, J.W. (1949). Comparing Individual Means in the Analysis of Variance. Biometrics 5, 99. https://doi.org/10.2307/3001913

li.             van Asselen, S., Erkens, G., Stouthamer, E., Woolderink, H.A.G., Geeraert, R.E.E., and Hefting, M.M., (2018). The relative contribution of peat compaction and oxidation to subsidence in built-up areas in the Rhine-Meuse delta, The Netherlands. Sci. Total Environ. 636, 177–191. https://doi.org/10.1016/j.scitotenv.2018.04.141

lii.           Wakhid, N., Hirano, T., Okimoto, Y., Nurzakiah, S., and Nursyamsi, D. (2017). Soil carbon dioxide emissions from a rubber plantation on tropical peat. Sci. Total Environ. 581–582, 857–865. https://doi.org/10.1016/j.scitotenv.2017.01.035

liii.         Waldron, S., Vihermaa, L., Evers, S., Garnett, M., Newton, J., Padfield, R., and Henderson, A. (2019). Old DOC can fuel the efflux of old carbon dioxide from disturbed tropical peat drainage system, but site recovery can occur. Sci. Rep. 1–12. https://doi.org/10.1038/s41598-019-46534-9

liv.          Wösten, J.H.., Ismail, A.., and van Wijk, A.L. (1997). Peat subsidence and its practical implications: a case study in Malaysia. Geoderma 78, 25–36. https://doi.org/10.1016/S0016-7061(97)00013-X

lv.            Yahya, Z., Husin, A., Talib, J., Othman, J., Darus, S.Z., Ahmed, O.H., and Jalloh, M.B. (2011). Pores Reconfiguration in Compacted Bernam Series Soil. Am. J. Appl. Sci. 8, 212–216. https://doi.org/10.3844/ajassp.2011.212.216

lvi.          Yap, B.W. and Sim, C.H. (2011). Comparisons of various types of normality tests. J. Stat. Comput. Simul. 81, 2141–2155. https://doi.org/10.1080/00949655.2010.520163

lvii.        Ye, R., Jin, Q., Bohannan, B., Keller, J.K., McAllister, S.A., Bridgham, S.D. (2012). pH controls over anaerobic carbon mineralization, the efficiency of methane production, and methanogenic pathways in peatlands across an ombrotrophic–minerotrophic gradient. Soil Biol. Biochem. 54, 36–47. https://doi.org/10.1016/j.soilbio.2012.05.015

lviii.      Zerva, A. (2004). Comparison of closed static and dynamic chamber methods for the measurement of soil CO2 efflux. Edinburgh Univ. Thesis 2, 190–221.

lix.         Zulkifli, H., Halimah, M., Chan, K.W., Choo, Y.M., and  Mohd Basri, W. (2010). Life cycle assessment for oil palm fresh fruit bunch production from continued land use for oil palm planted on mineral soil. J. Oil Palm Res. 22, 887–894.

Cite this Article: