Controls on the net dissolved organic carbon production in tropical peat

Siti Nurzakiah, Atang Sutandi, Supiandi Sabiham, Gunawan Djajakirana, Untung Sudadi

Abstract

Soil factors such as pH and the presence of polyvalent cations can influence the net production of dissolved organic carbon (DOC). This study aimed to determine the main factors that control net DOC production. The study was conducted at Buatan Village, Siak Indrapura Regency, Riau Province, Indonesia. Soil and water sampling were done every month for a year observation, from July 2018 to June 2019. Soil sampling was carried out to determine the concentration of C-organic acids, pH, N, P, K, Cu, and soil water content (SWC). Peat water sampling was carried out using modified pore water sampling to measure DOC concentration. Groundwater level (GWL) and soil temperature were also observed. Multiple regression analysis was performed to find out the soil and environmental factors controlling the net DOC production. The results showed that the net DOC production fluctuated with seasonal changes and soil pH was a significant controlling factor (P = 0.035) and positively correlated (P = 0.040) to the net DOC production. In addition, N-mineral, PO4, and Cu were positively correlated with net DOC production (P-value: 0.026; 0.033; and 0.028; respectively) while C-organic acids and SWC were negatively correlated (P-value: 0.033; and 0.020; respectively). There was no correlation between net DOC production with GWL, soil temperature, and K concentration. This finding confirmed that pH was the main factor controlling the net DOC production and reflects DOC contribution to the solution acidity.

Keywords

Copper; C-organic acids; N and P nutrients; Soil pH; Soil water content

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Araújo, E., Strawn, D. G., Morra, M., Moore, A., & Alleoni, L. R. F. (2019). Association between extracted copper and dissolved organic matter in dairy-manure amended soils. Environmental Pollution, 246, 1020–1026. https://doi.org/10.1016/j.envpol.2018.12.070.

Arvola, L., Rask, M., Ruuhijärvi, J., Tulonen, T., Vuorenmaa, J., Ruoho-Airola, T., & Tulonen, J. (2010). Long-term patterns in pH and colour in small acidic boreal lakes of varying hydrological and landscape settings. Biogeochemistry, 101(1), 269–279. https://doi.org/10.1007/s10533-010-9473-y.

Baziramakenga, R., Simard, R. R., & Leroux, G. D. (1995). Determination of organic acids in soil extracts by ion chromatography. Soil Biology and Biochemistry, 27(3), 349–356. https://doi.org/https://doi.org/10.1016/0038-0717(94)00178-4.

Bengtson, P., & Bengtsson, G. (2007). Rapid turnover of DOC in temperate forests accounts for increased CO 2 production at elevated temperatures. Ecology Letters, 10(9), 783–790. https://doi.org/10.1111/j.1461-0248.2007.01072.x.

Bourbonniere, R. A. (1989). Distribution patterns of dissolved organic matter fractions in natural waters from eastern Canada. Organic Geochemistry, 14(1), 97–107. https://doi.org/10.1016/0146-6380(89)90023-5.

Carrera, N., Barreal, M. E., Rodeiro, J., & Briones, M. J. I. (2011). Interactive effects of temperature, soil moisture, and enchytraeid activities on C losses from a peatland soil. Pedobiologia, 54(5–6), 291–299. https://doi.org/10.1016/j.pedobi.2011.07.002

Casas-Ruiz, J. P., Catalán, N., Gómez-Gener, L., von Schiller, D., Obrador, B., Kothawala, D. N., López, P., Sabater, S., & Marcé, R. (2017). A tale of pipes and reactors: Controls on the in-stream dynamics of dissolved organic matter in rivers. Limnology and Oceanography, 62, S85–S94. https://doi.org/10.1002/lno.10471.

Clark, J. M., Heinemeyer, A., Martin, P., & Bottrell, S. H. (2012). Processes controlling DOC in pore water during simulated drought cycles in six different UK peats. Biogeochemistry, 109(1–3), 253–270. https://doi.org/10.1007/s10533-011-9624-9.

Clark, J. M., Van Der Heijden, G. M. F., Palmer, S. M., Chapman, P. J., & Bottrell, S. H. (2011). Variation in the sensitivity of DOC release between different organic soils following H2SO4 and sea-salt additions. European Journal of Soil Science, 62(2), 267–284. https://doi.org/10.1111/j.1365-2389.2010.01344.x.

Creed, I. F., McKnight, D. M., Pellerin, B. A., Green, M. B., Bergamaschi, B. A., Aiken, G. R., Burns, D. A., Findlay, S. E., Shanley, J. B., Striegl, R. G., Aulenbach, B. T., Clow, D. W., Laudon, H., McGlynn, B. L., McGuire, K. J., Smith, R. A., & Stackpoole, S. M. (2015). The river as a chemostat: fresh perspectives on dissolved organic matter flowing down the river continuum. Canadian Journal of Fisheries and Aquatic Sciences, 72(8), 1272–1285. https://doi.org/10.1139/cjfas-2014-0400.

Dillon, P. J., & Molot, L. A. (2005). Long-term trends in catchment export and lake retention of dissolved organic carbon, dissolved organic nitrogen, total iron, and total phosphorus: The Dorset, Ontario, study, 1978–1998. Journal of Geophysical Research, 110(G1), 3–9. https://doi.org/10.1029/2004jg000003.

Fasching, C., Ulseth, A. J., Schelker, J., Steniczka, G., & Battin, T. J. (2016). Hydrology controls dissolved organic matter export and composition in an Alpine stream and its hyporheic zone. Limnology and Oceanography, 61(2), 558–571. https://doi.org/10.1002/lno.10232.

Fierer, N. (2017). Embracing the unknown: Disentangling the complexities of the soil microbiome. Nature Reviews Microbiology, 15(10), 579–590. https://doi.org/10.1038/nrmicro.2017.87.

Franchini, J. C., Hoffmann-Campo, C. B., Torres, E., Miyazawa, M., & Pavan, M. A. (2003). Organic composition of green manure during growth and its effect on cation mobilization in an acid oxisol. Communications in Soil Science and Plant Analysis, 34(13–14), 2045–2058. https://doi.org/10.1081/CSS-120023237.

Girkin, N. T., Turner, B. L., Ostle, N., Craigon, J., & Sjögersten, S. (2018). Root exudate analogues accelerate CO2 and CH4 production in tropical peat. Soil Biology and Biochemistry, 117, 48–55. https://doi.org/10.1016/j.soilbio.2017.11.008.

Gmach, M. R., Cherubin, M. R., Kaiser, K., & Pellegrino, C. (2018). Processes that influence dissolved organic matter in the soil: a review. Scientia Agricola, 77(3), e20180164.

Guggenberger, G., Zech, W., & Schulten, H. R. (1994). Formation and mobilization pathways of dissolved organic matter: evidence from chemical structural studies of organic matter fractions in acid forest floor solutions. Organic Geochemistry, 21(1), 51–66. https://doi.org/10.1016/0146-6380(94)90087-6.

Hagedorn, F., Bruderhofer, N., Ferrari, A., & Niklaus, P. A. (2015). Tracking litter-derived dissolved organic matter along a soil chronosequence using 14C imaging: Biodegradation, physico-chemical retention or preferential flow? Soil Biology and Biochemistry, 88, 333–343. https://doi.org/10.1016/j.soilbio.2015.06.014

Hentschel, K., Borken, W., & Matzner, E. (2007). Leaching losses of inorganic N and DOC following repeated drying and wetting of a spruce forest soil. Plant Soil, 300, 21–34. https://doi.org/10.1007/s11104-007-9385-3

Hornberger, G. M., Bencala, K. E., & McKnight, D. M. (1994). Hydrological controls on dissolved organic carbon during snowmelt in the Snake River near Montezuma, Colorado. Biogeochemistry, 25(3), 147–165. https://doi.org/10.1007/BF00024390.

Jandl, R., & Sollins, P. (1997). Water-extractable soil carbon in relation to the belowground carbon cycle. Biology and Fertility of Soils, 25(2), 196–201. https://doi.org/10.1007/s003740050303.

Kalbitz, K., & Kaiser, K. (2008). Contribution of dissolved organic matter to carbon storage in forest soils. Journal of Soil Science and Plant Nutrition, 171, 52–60. https://doi.org/10.1002/jpln.200700043

Kalbitz, K., Solinger, S., Park, J. H., Michalzik, B., & Matzner, E. (2000). Controls on the dynamics of dissolved organic matter in soils: A review. Soil Science, 165(4), 277–304. https://doi.org/10.1097/00010694-200004000-00001.

Kane, E. S., Mazzoleni, L. R., Kratz, C. J., Hribljan, J. A., Johnson, C. P., Pypker, T. G., & Chimner, R. (2014). Peat porewater dissolved organic carbon concentration and lability increase with warming: A field temperature manipulation experiment in a poor-fen. Biogeochemistry, 119(13), 161–178. https://doi.org/10.1007/s10533-014-9955-4.

Kang, H., Kwon, M. J., Kim, S., Lee, S., Jones, T. G., Johncock, A. C., Haraguchi, A., & Freeman, C. (2018). Biologically driven DOC release from peatlands during recovery from acidification. Nature Communications, 9(1), 1–7. https://doi.org/10.1038/s41467-018-06259-1.

Kortelainen, P., & Mannio, J. (1988). Natural and anthropogenic acidity sources for Finnish Lakes. Water, Air, and Soil Pollution, 42, 341–352. https://doi.org/10.1007/BF00279278.

Kuzyakov, Y. (2002). Review: Factors affecting rhizosphere priming effects. Journal of Plant Nutrition and Soil Science, 165(4), 382–396. https://doi.org/10.1002/1522-2624(200208)165:4<382::AID-JPLN382>3.0.CO;2-#.

Liechty, H. O., Kuuseoks, E., & Mroz, G. D. (1995). Dissolved Organic Carbon In Northern Hardwood Stands With Differing Acidic Inputs and Temperature Regimes. Journal of Environmental Quality, 24(5), 927–933. https://doi.org/10.2134/jeq1995.00472425002400050021x.

Limpens, J., Berendse, F., Blodau, C., Canadell, J. G., Freeman, C., Holden, J., Roulet, N., Rydin, H., & Schaepman-Strub, G. (2008). Peatlands and the carbon cycle: From local processes to global implications - A synthesis. Biogeosciences, 5, 1475–1491. https://doi.org/10.5194/bg-5-1475-2008.

Lundquist, E. J., Jackson, L. E., & Scow, K. M. (1999). Wet-dry cycles affect dissolved organic carbon in two California agricultural soils. Soil Biology and Biochemistry, 31(7), 1031–1038. https://doi.org/10.1016/S0038-0717(99)00017-6.

Mao, R., Li, S. Y., Zhang, X. H., Wang, X. W., & Song, C. C. (2017). Effect of long-term phosphorus addition on the quantity and quality of dissolved organic carbon in a freshwater wetland of Northeast China. Science of the Total Environment, 586, 1032–1037. https://doi.org/10.1016/j.scitotenv.2017.02.084

Marschner, B., & Bredow, A. (2002). Temperature effects on release and ecologically relevant properties of dissolved organic carbon in sterilized and biologically active soil samples. Soil Biology and Biochemistry, 34(4), 459–466. https://doi.org/10.1016/S0038-0717(01)00203-6.

McDowell, W. H., & Wood, T. (1984). Podzolization: Soil processes control dissolved organic carbon concentrations in stream water. Soil Science, 137, 23–32. https://doi.org/10.1097/00010694-198401000-00004.

Michalzik, B., & Matzner, E. (1999). Dynamics of dissolved organic nitrogen and carbon in a central European Norway spruce ecosystem. European Journal of Soil Science, 50, 579–590. https://doi.org/10.1046/j.1365-2389.1999.00267.x.

Moyano, F. E., Manzoni, S., & Chenu, C. (2013). Responses of soil heterotrophic respiration to moisture availability : An exploration of processes and models. Soil Biology and Biochemistry, 59, 72–85. https://doi.org/10.1016/j.soilbio.2013.01.002

Mulholland, P. J., Wilson, G. V, & Jardine, P. M. (1990). Hydrogeochemical response of a forested watershed to storms: effects of preferential flow along shallow and deep pathways. Water Resources Research, 26(12), 3021–3036.

Page, S. E., Rieley, J. O., & Banks, C. J. (2011). Global and regional importance of the tropical peatland carbon pool. Global Change Biology, 17(2), 798–818. https://doi.org/10.1111/j.1365-2486.2010.02279.x.

Raymond, P. A., Saiers, J. E., & Sobczak, W. W. (2016). Hydrological and biogeochemical controls on watershed dissolved organic matter transport: pulse-shunt concept. Ecology, 97(1), 5–16. https://doi.org/10.1890/14-1684.1.

Roulet, N., & Moore, T. R. (2006). Environmental chemistry: Browning the waters. Nature, 444(7117), 283–284. https://doi.org/10.1038/444283a.

Ryder, E., de Eyto, E., Dillane, M., Poole, R., Linnane, S., & Jennings, E. (2012). Impact of climate on export of DOC from a peatland catchment. Annual Meeting of Freshwater Biologists.

Schwalm, M., & Zeitz, J. (2015). Concentrations of dissolved organic carbon in peat soils as influenced by land use and site characteristics — A lysimeter study. Catena, 127, 72–79.

Soil Survey Staff. (2010). Keys to Soil Taxonomy (11th ed.). U.S. Department of Agriculture-Natural Resources Conservation Service.

Tipping, E., & Hurley, M. A. (1992). A unifying model of cation binding by humic substances. Geochimica et Cosmochimica Acta, 56(10), 3627–3641. https://doi.org/10.1016/0016-7037(92)90158-F.

Tipping, E., & Woof, C. (1990). Humic substances in acid organic soils: modeling their release to the soil solution in terms of humic charge. Journal of Soil Science, 41, 573–586. https://doi.org/10.1111/j.1365-2389.1990.tb00227.x

Veum, K. S., Goyne, K. W., Motavalli, P. P., & Udawatta, R. P. (2009). Runoff and dissolved organic carbon loss from a paired-watershed study of three adjacent agricultural Watersheds. Agriculture, Ecosystems, and Environment, 130, 115–122. https://doi.org/10.1016/j.agee.2008.12.006.

Zhang, T., Shi, S., Zhang, W., Wu, Y., Yang, M., & Wang, P. (2016). Environmental factors and dissolved organic carbon content in a Jinchuan peatland. Acta Ecologica Sinica, 36(3), 160–165. https://doi.org/10.1016/j.chnaes.2016.04.001.

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