Applied Ecology and Forestry Science
ISSN (Print): ISSN Pending ISSN (Online): ISSN Pending Website: https://www.sciepub.com/journal/aefs Editor-in-chief: Romeo Ekoungoulou
Open Access
Journal Browser
Go
Applied Ecology and Forestry Science. 2022, 5(1), 9-13
DOI: 10.12691/aefs-5-1-2
Open AccessArticle

Carbon Storage in Soils: A Case Study of Cocoa Agroforestry in Idanre Forest Reserve, Ondo State, Nigeria

Akinbode O. A1, , Oke D. O.2 and Akinbi O. J.3

1Department of Forestry Technology, Federal College of Agriculture, Akure, Nigeria

2Department of Forestry and Wood Technology, Federal University of Technology, Akure, Nigeria

3Forestry Research Institute of Nigeria, PMB 5054, Ibadan, Nigeria

Pub. Date: January 11, 2022

Cite this paper:
Akinbode O. A, Oke D. O. and Akinbi O. J.. Carbon Storage in Soils: A Case Study of Cocoa Agroforestry in Idanre Forest Reserve, Ondo State, Nigeria. Applied Ecology and Forestry Science. 2022; 5(1):9-13. doi: 10.12691/aefs-5-1-2

Abstract

This study investigated the effects of three land use management systems on the status of total and mineral-associated and particulate soil organic carbon content. The study was carried out in selected cocoa farms established within Idanre Forest Reserve, Ondo State, Nigeria. Based on the number of non-cocoa trees (shade trees) per unit area, the farms were classified into dense cocoa agroforest, sparse cocoa agroforest, and pure cocoa plantation. 3 sample plots of 25m x 25m were mapped out alternate to each other, and soil samples were collected at 5 different points along the diagonal of each plot at depths 0-15cm, 15-30cm and 30-45cm using a 3cm diameter soil auger. The results shows that surface soil (0-15cm) total organic carbon (TOC) content was highest under the sparse cocoa agroforest (5.64%) and lowest in the dense cocoa agroforest (2.86%). It was noted that sparse cocoa agroforest had potential for increasing soil organic carbon of an appreciable concentration due to the presence of few large non-cocoa trees which contributed immensely to the soil carbon stock especially through litter fall. The decreasing order for the % TOC is given as Sparse cocoa agroforest > pure cocoa plantation > dense cocoa agroforest. The result of the analysis shows a significant difference (P<0.05) in the %Particulate organic carbon (POC) and %Mineral-associated organic carbon (MOC) stored in the soil by the different land use management systems and at the different depths considered. Carbon content of MOC were higher than the POC in all land use management systems. The study concluded that soil organic carbon stored decreased with increasing soil depth across land use and sparse cocoa agroforestry with few large trees has the potentials of storing organic carbon of appreciable concentration.

Keywords:
land use cocoa agroforestry carbon fraction mineral-associated particulate organic carbon Nigeria

Creative CommonsThis work is licensed under a Creative Commons Attribution 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

References:

[1]  WMO. Integrated Flood Management Concept Paper. Associated Programme on Flood Management, World Meteorological Organization, WMO-No. 1047, 2009.
 
[2]  Schellnhuber H.J., Cramer W., Nakicenovic N., (eds) Avoiding dangerous climate change. Cambridge University Press, p. 406. 2006.
 
[3]  Ravindranath N. H., Joshi N. V., Sukumar R. Impact of climate change on forests in India. Curr Sci 90(3): 354-361. 2006.
 
[4]  IPCC. Climate Change 2014: Synthesis, Report Contribution of Working Groups I, II and III to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Geneva: IPCC. 2014.
 
[5]  Kerr R.A. Bush backs spending for a “global problem” Science. 2001; 292: 1978. 2001.
 
[6]  O'Connor, W.K., Dahlin, D.C., Nilsen, D.N., Rush, G.E., Walters, R.P. and Turner, P.C. Carbon dioxide sequestration by direct mineral carbonation: results from recent studies and current status. 2001.
 
[7]  Lal R. Soil carbon sequestration impacts on global climate change and food security. Science 304: 1623-1627. 2004a.
 
[8]  Chenu, C., and Plante, A.F. Clay-sized organo-mineral complexes in a cultivation chronosequence: revisiting the concept of the ‘primary organo-mineral complex’. Eur. J. Soil Sci., 57, 596-607, 2006.
 
[9]  Jones, E., and Singh, B. Organo-mineral interactions in contrasting soils under natural vegetation. Front. Environ. Sci., 2, 2. 2014.
 
[10]  Sollins, P., Swanston, C., Kleber, M., Filley, T., Kramer, M., Crow, S., Caldwell, B., Lajtha, K., and Bowden, R. Organic C and N stabilization in a forest soil: evidence from sequential density fractionation. Soil Biol. Biochem., 38, 3313-3324, 2006.
 
[11]  Sollins, P., Kramer, M.G., Swanston, C., Lajtha, K., Filley, T., Aufdenkampe, A.K., Wagai, R., and Bowden, R. D. Sequential density fractionation across soils of contrasting mineralogy: evidence for both microbial- and mineral-controlled soil organic matter stabilization. Biogeochemistry, 96, 209-231, 2009.
 
[12]  Feller, C., and Beare, M.H. Physical control of soil organic matter dynamics in the tropics. Geoderma, 79, 69-116, 1997.
 
[13]  Jobbaggy, E.G., and Jackson, R.B. The vertical distribution of soil organic carbon and its relation to climate and vegetation. Ecol. Appl. 10, 423-436. 2000.
 
[14]  Six, J., Conant, R.T., Paul, E.A. and Paustian, K. Stabilization mechanisms of soil organic matter: Implications for C-saturation of soils. Plant and Soil, 241: 155-176. 2002.
 
[15]  Dixon, R.K. Agroforest Systems: Sources or sinks of greenhouse gases? Agroforestry Systems, 31, 99-116. 1995.
 
[16]  Floret, C. Raccourcissement du temps de jachère, biodiversité et développement durable en Afrique centrale (Cameroun) et en Afrique de l’ouest (Mali, Sénégal) :Projet CEE NTSJ-CT9J-0220 (DG 12 HSMU) ORSTOM, France, 90-104. 1998.
 
[17]  Conant, R.T., Six, J., and Paustian, K. Land use effects on soil carbon fractions in 612 the southeastern United States. II. Changes in soil carbon fractions along a forest to pasture chronosequence. Biol. Fert. Soils, 40, 194-200, 2004.
 
[18]  Franzluebbers, A.J., and Stuedemann, J.A. Particulate and non-particulate fractions of soil organic carbon under pastures in the Southern Piedmont USA. Environ. Pollut., 116, S53-S62, 2002.
 
[19]  Six, J., Elliott, E.T., Paustian, K., and Doran, J.W. Aggregation and soil organic matter accumulation in cultivated and native grassland soils. Soil Sci. Soc. Am. J., 62, 1367-1377, 1998.
 
[20]  Conant, R.T., Six, J., and Paustian, K. Land use effects on soil carbon fractions in the southeastern United States. I. Management intensive versus extensive grazing. Biol. Fert. Soils, 38, 386-392, 2003.
 
[21]  Jastrow, J.D. Soil aggregate formation and the accrual of particulate and mineral-associated organic matter. Soil Biol. Biochem., 28, 665-676, 1996.
 
[22]  Leifeld, J., and Kögel-Knabner, I. Soil organic matter fractions as early indicators for carbon stock changes under different land-use? Geoderma, 124, 143-155, 2005.
 
[23]  Don, A., Schumacher, and J., Freibauer, A. Impact of tropical land-use change on soil organic carbon stocks - a meta-analysis. Global Change Biol., 17, 1658-1670, 2011.
 
[24]  Poeplau, C., Don, A., Vesterdal, L., Leifeld, J., Van Wesemael, B., Schumacher, J., and Gensior, A. Temporal dynamics of soil organic carbon after land-use change in the temperate zone – carbon response functions as a model approach. Global Change Biol., 17, 2415-2427, 2011.
 
[25]  Wright, A.L., Dou, F.G., and Hons, F.M. Crop species and tillage effects on carbon sequestration in subsurface soil. Soil Sci., 172, 124-131, 2017.
 
[26]  Ikemeh, R.A. Sustainable Forest management in a human-dominated landscape and its implications for biodiversity conservation: a Nigerian lowland forest perspective. Dove press; 2013: 9-23. 2013.
 
[27]  Cambardella, C.A. and Elliott, E.T. Particulate soil organic matter changes across a grassland cultivation sequence. Soil Sci. Soc. Am. J., 56; 777-783. 1992.
 
[28]  Walkley, A. and Black, I.A. An examination of the Degtjareff method for determining organic carbon in soils: Effect of variations in digestion conditions and of inorganic soil constituents. Soil Science 63, 251-263. 1934.
 
[29]  Wartenberg, A.C., Blaser, W.J., Roshetko, J.M., Van Noordwijk, M., and Six, J. Soil fertility and Theobroma cacao growth and productivity under commonly intercropped shade-tree species in Sulawesi, Indonesia. Plant and Soil. 2019.
 
[30]  Gusli, S., Sumeni, S., Sabodin, R., and Muq, I. H. Soil Organic Matter, Mitigation of and Adaptation to Climate Change in Cocoa–Based Agroforestry Systems. Land 2, 9, 323; 2020.
 
[31]  Oke, D, and Olatiilu, A. Carbon Storage in Agroecosystems: A Case Study of the Cocoa Based Agroforestry in Ogbese Forest Reserve, Ekiti State, Nigeria Journal of Environmental Protection, 2011, 2, 1069-1075. 2011.
 
[32]  Jamala G.Y. and Oke D.O. Soil organic carbon fractions as affected by land use in the Southern Guinea Savanna ecosystem of Adamawa State, Nigeria. J. Soil Sci. Environ. Mgt. 4(6), pp 116-122.
 
[33]  Bayer C., Mielniczuk J., Giasson E., Martin-Neto L., Pavinato A. Tillage effects on particulate and mineral-associated organic matter in teo tropical Brazilian soils. Soil Sci. Plant Anal. 37: 389-400. 2006.
 
[34]  Bescansa P., Imaz M.J., Virto I., and Enrique A. Particulate Organic matter carbon as a soil quality indicator in semiarid Agricultural soils. Geophys. Res. Abstracts 8:06328, 2006.
 
[35]  Tenkap, P.E. and Balogun, B.O. Land suitability for cocoa production in Idanre, Ondo State, Nigeria. J. Agric. Biotech. Sustain. Dev. Vol. 12(2), pp. 19-33, 2019.