An Asian Journal of Soil Science

Open Access Open Access  Restricted Access Subscription Access
Open Access Open Access Open Access  Restricted Access Restricted Access Subscription Access

Erodibility Status of Soils under Different Land Uses in West Khasi Hills of Meghalaya


Affiliations
1 Department of Soil and Water Conservation, School of Agricultural Sciences and Rural Development, Nagaland University, Medziphema (Nagaland), India
     

   Subscribe/Renew Journal


The effect of land use on soil erodibility parameters were studied in four villages, viz., Nongstoin, Kynshi, Umyiap and Maweit in West Khasi Hills district, Meghalaya, under four land uses, viz., lowland paddy, potato, forest and Jhum land, in each village. The textural class of the soils varied from silt loam to clay with dominance of clay loam texture. Dispersion ratio and erosion index were recorded to be usually higher than the threshold limits. A highly significant and negative relationship of erosion index with clay, silt + clay and highly significant and positive relationship with sand and dispersion ratio were observed. The increase in erosion index with increase in dispersion ratio indicated the susceptibility of these soils to water erosion. Proper soil and water conservation measures need to be adopted to protect the soils from further degradation.

Keywords

Land Uses, Dispersion Ratio, Erosion Index.
Subscription Login to verify subscription
User
Notifications
Font Size


  • Agnihotri, R.C., Yadav, R.C. and Jha, Pramod (2007). Erodibility characteristics of entisol soils of riparian zone of the Yamuna river in Agra: Impacts of land forms and land uses. Indian J. Soil Cons., 35 (3): 226-229.

  • Baruah, T.C. and Barthakur, H.P. (1997). A text book of soil analysis, Vikas Publishing House Pvt. Ltd., NEW DELHI, INDIA.

  • Gomez, K.A. and Gomez, A.A. (1984). Statistical procedures for agricultural research (2nd Ed.). John Wiley & Sons, INC., UK, 20.

  • Goswami, S.N. and Challa, O. (2006). Land use scenario in Meghalaya – An exploratory analysis. Indian J. Soil Cons., 34: 140-144.

  • Kahlon, M.S. (2006). Investigation on soil erodibility under different land use patterns of certain soils of sub-montane Punjab, India. Indian Forester, 132 (11): 1391-397.

  • Khera, K.L. and Kahlon, M.S. (2005). Impact of land use pattern on soil erosion in sub-montane Punjab. Indian J. Soil Cons., 33 (3): 204-206.

  • Laxminarayana, K. (2010). Nature of soil acidity and lime requirement in acid soils of Meghalaya. J. Indian Soc. Soil Sci., 58: 233-236.

  • Mandal, D., Sharda, V.N. and Tripathi, K.P. (2010). Relative efficiency of two bio physical approaches to assess soil loss tolerance for Doon valley soils of India. J. Soil & Water Cons., 65: 42-49.

  • Mehta, A.K., Khera, K.L. and Bhushan, Bharat (2005). Effect of soil physical properties and land use on soil erodibility. Indian J. Soil Cons., 33 (2): 180-82.

  • Middleton, H.E. (1930). Properties of soils which influence soil erosion. USDA Technical Bull., 178: 1-16.

  • Piper, C.S. (1966). Soil and plant analysis. Hans Publishers, Mumbai (M.S.) INDIA.

  • Saha, R., Mishra, V.K. and Khan, S.K. (2011). Soil erodibility characteristics under modified land-use systems as against shifting cultivation in hilly ecosystems of Meghalaya, India. J. Sustain. Forest., 30 (4): 301-12.

  • Sahi, B.P., Singh, S.N., Sinha, A.C. and Acharya, B. (1977). Erosion index – a new index of soil erodibility. J. Indian Soc. Soil Sci., 25: 7-10.

  • Sharma, J.C. and Kumar, Vipin (2010). Erodibility status of soils under different land uses in Shiwalik hills of Himachal Pradesh. J. Indian Soc. Soil Sci., 58: 467-469.

  • Sharma, Y.K., Sharma, A. and Sharma, S.K. (2012). Distribution of DTPA- extractable micronutrients cations in soils of Zunheboto district of Nagaland in relation to soil characteristics. J. Interaca., 16: 101-08.

  • Singh, M.J. and Khera, K.L. (2006). Run-off and soil loss as affected by land use, rainfall intensity and antecedent soil moisture under simulated rainfall conditions. Indian J. Soil Cons., 34: 254-256.

  • Singh, O.P. and Dutta, B. (1989). Morphology, physical and physico-chemical properties of hill soils of Mizoram in relation to altitude. Indian J. Hill Farm., 2: 9-20.

  • Singh, Ratna, Singh, K.D. and Parandiyal, A.K. (2006). Characterisation and erodibility of soils under different land uses for their management and sustained production. Indian J. Soil Cons., 34: 226-228.

  • Singh, Ravender and Kundu, D.K. (2008). Erodibility of major soil sub-groups of eastern region of India. Indian J. Soil Cons., 36: 172-178.

  • Yilmaz, M., Usta, A., Altun, L. and Tilki, F. (2007). Effects of land-use regime on soil erodibility indices and soil properties in Unye, Turkey. Fresenius Environ. Bull., 16: 1636-642.


Abstract Views: 163

PDF Views: 0




  • Erodibility Status of Soils under Different Land Uses in West Khasi Hills of Meghalaya

Abstract Views: 163  |  PDF Views: 0

Authors

Janshaipharstep Diengdoh
Department of Soil and Water Conservation, School of Agricultural Sciences and Rural Development, Nagaland University, Medziphema (Nagaland), India
Manoj Dutta
Department of Soil and Water Conservation, School of Agricultural Sciences and Rural Development, Nagaland University, Medziphema (Nagaland), India
Sewak Ram
Department of Soil and Water Conservation, School of Agricultural Sciences and Rural Development, Nagaland University, Medziphema (Nagaland), India

Abstract


The effect of land use on soil erodibility parameters were studied in four villages, viz., Nongstoin, Kynshi, Umyiap and Maweit in West Khasi Hills district, Meghalaya, under four land uses, viz., lowland paddy, potato, forest and Jhum land, in each village. The textural class of the soils varied from silt loam to clay with dominance of clay loam texture. Dispersion ratio and erosion index were recorded to be usually higher than the threshold limits. A highly significant and negative relationship of erosion index with clay, silt + clay and highly significant and positive relationship with sand and dispersion ratio were observed. The increase in erosion index with increase in dispersion ratio indicated the susceptibility of these soils to water erosion. Proper soil and water conservation measures need to be adopted to protect the soils from further degradation.

Keywords


Land Uses, Dispersion Ratio, Erosion Index.

References