Applied Ecology and Environmental Sciences
ISSN (Print): 2328-3912 ISSN (Online): 2328-3920 Website: Editor-in-chief: Alejandro González Medina
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Applied Ecology and Environmental Sciences. 2013, 1(1), 7-9
DOI: 10.12691/aees-1-1-2
Open AccessArticle

Sequestered Organic Carbon Status in the Soils under Grassland in Uttarakhand State, India

M K Gupta1 and S.D. Sharma2,

1Forest Soil & Land Reclamation Division, Forest Research Institute, Dehra Dun, India

2Forest Informatics Division, Forest Research Institute, P.O. New forests, Dehra Dun, India

Pub. Date: March 05, 2013

Cite this paper:
M K Gupta and S.D. Sharma. Sequestered Organic Carbon Status in the Soils under Grassland in Uttarakhand State, India. Applied Ecology and Environmental Sciences. 2013; 1(1):7-9. doi: 10.12691/aees-1-1-2


Vegetative growth serves as an important means to capture and store atmospheric carbon dioxide in biomass and soil. Grassland soils are high in soil organic carbon and contain an extensive fibrous root system that creates an environment ideal for soil microbial activity. Accurate quantification of SOC pool is needed to generate benchmark information for the present and to determine the changes in future. No systematic study has been undertaken to estimate the soil organic carbon pool in grasslands of Uttarakhand state of India. This study therefore, was conducted to estimate SOC pool in the grasslands occurring between the wide altitudinal range of 500m to 4200m above msl. Maximum SOC pool, 142.14 t ha–1, was observed in the altitudinal range of 2501 to 4200m, followed by 105.28 t ha–1 between 2001-2500 m, 97.80 t ha–1 between 1501–2000 m, 41.15 t ha–1 between 1001-1500m and the least was 37.09 t ha–1 at 501–1000 m altitude. The grasslands in Uttarakhand extend over an area of 2,28,900 hectare at different altitudes and contain 26.77 million tons of soil organic carbon pool. Correlation between altitudes and SOC pool revealed that altitude was significantly positively correlated with SOC pool under the grassland with correlation coefficient 0.955* (Significant at P < 0.05 level). Results of one - way ANOVA indicates that SOC pools at different altitude ranges were significantly different at 0.05 level.

altitudes grasslands soil organic carbon Uttarakhand

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[1]  Makundi, Willy R. and Sathaye, Jayant, A, GHG mitigation potential and cost in tropical forestry – relative role for agroforestry. Environment, Development and Sustainability, 6. 235-260. 2004.
[2]  Melilo, J.M., Kicklighter, D., McGuire, A., Peterjohn, W. and Newkirk, K, Global change and its effects on soil organic carbon stocks. in Dahlem Conference 1995. John Wiley and Sons, New York. Pp. 175-189. 1995.
[3]  Prentice, I.C., Farquhar, G.D., Fasham, M.J.R., Goulden, M.L. and Heimann, M, The carbon cycle and atmospheric CO2. In: The Third Assessment Report of Intergovernmental Panel on Climate Change (IPCC), Chapter 3, Cambridge University Press, Cambridge, 2001.
[4]  Anderson, J. M, The effects of climate change on decomposition processes in grassland and coniferous forest. Ecol. Appl., 1. 326-347. 1991
[5]  Eswaran, H., van den Berg, E. and Reich, P, Organic carbon in soils of the world. Soil Sci. Soc. Am. J., 57. 192-194. 1993.
[6]  Conant, R. T., Paustian, K. and Elliott, E. T, Grassland management and conversion into grassland: effects on soil carbon. Ecol. Appl. 11. 343-355. 2001.
[7]  Frank A. B, Carbon dioxide fluxes over a grazed prairie and seeded pasture in the Northern Great Plains. Environ. Pollut, 116. 397-403. 2002.
[8]  Schwager, S. J. Mikhailova, E. A, Estimating Variability in Soil Organic Carbon Storage Using the Method of Statistical Differentials. Soil Science, 167 (3).194-200. 2002.
[9]  Walkley, A. and Black, I. A, An Examination of Degtjareff Method for Determining Soil Organic Matter and a Proposed Modification of the Chromic Acid Titration Method. Soil Sci. 37, 29-37. 1934.
[10]  Wilde, S.A., Voigt, G.K. and Iyer, J.G, Soil and Plant Analysis for Tree Culture. Oxford Publishing House, Calcutta, India, 1964.
[11]  Ravindranath, N.H. and Ostwald, M, Carbon Inventory Methods: Handbook for Greenhouse Gas Inventory, Carbon Mitigation and Round wood Production Projects. Springer Publishers, 2008.
[12]  IPCC, Good Practice Guidance for Land Use, Land Use Change and Forestry. Published by the Institute for Global Environmental Strategies (IGES) for the IPCC. Publishers Institute for Global Environmental Strategies, Japan, 2003.
[13]  Arrouays, D., Deslais, W. and Badeau, V, The carbon content of topsoil and its geographical distribution in France. Soil Use and Management, 17. 7-11. 2001.
[14]  Jones, R.J.A., Hiederer, R., Rusco, E. and Montanarella, L, Estimating organic carbon in the soils of Europe for policy sup- port. European Journal of Soil Science, 56. 655-671. 2005.
[15]  Rawat, R.S, Studies on interrelationship of woody vegetation density and soil characteristics along an altitudinal gradient in a montane forest of Garhwal Himalayas. The Indian Forester, 131 (8). 990-994. 2005.
[16]  Saby, N.P.A., Arrouays, D., Antony, V., Lemercier, B., Follain, S., Walter, C. and Schvartz, C, Changes in soil organic carbon in a mountainous French region, 1990-2004. Soil Use and Management. 24. 254-262.2008.
[17]  Anonymous, Luquillo Experimental Forest. State University of New York, College of Environmental Science and Forestry, Syracuse, NY, 2000.
[18]  Anonymous, Uttarakhand State Perspective and Strategic plan 2009-2027. Watershed Management Directorate, Dehra Dun, Uttarakhand, 2010.
[19]  Wang, Q., Zhang, L, Li, L., Bai, Y., Cao, J. and Han, X, Changes in carbon and nitrogen of Chernozem soil along a cultivation chronosequence in a semi arid grassland. European J. Soil Science, 60. 916-923. 2009.