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

Characterization of Salt-Affected Soils of Faizabad District


Affiliations
1 Department of Soil Science and Agricultural Chemistry, College of Agriculture, Narendra Deva University of Agriculture and Technology, Kumarganj, Faizabad (U.P.), India
2 Department of Soil Science and Agricultural Chemistry, College of Agriculture, Narendra Deva University of Agriculture and Technology, Kumarganj, Faizabad (U.P.), India
     

   Subscribe/Renew Journal


A study was undertaken to characterize the soils of Faizabad district, Uttar Pradesh in order to assess their land capability. The soils were described in the morphology, characteristics. Themorphological properties of soils were studied and later on analyzed in laboratory for their physical and chemical properties. Thickness of Ap horizon was less in pedon number 1(20 cm), pedon number 2 and 3 (22 cm) and pedon number 4 and 5 (25 cm). The solum depth of all the profiles ranged from 85 to 100 cm. The colour of surface soil of pedons 1, 2, 3, 4 and 5 were light gray (10 YR 7/1 and 10YR 7/2) when dry and light yellowish brown (10 YR 6/4) when moist.The soil colour of sub-surface horizons was strong brown (7.5YR 5/6). Surface soil structure of the pedon was fine prismatic while it was fine sub-angular blocky of other pedons. The consistency of surface and sub-surface soils varied from slightly hard to very hard, friable to extremely firm.It was non-sticky, non-plastic to sticky, plastic in dry, moist and wet conditions, respectively in all the pedons.

Keywords

Pedon, Horizon, Structure.
Subscription Login to verify subscription
User
Notifications
Font Size


  • Chopra, S. L. and Kanwer, J. S. (1976).Analytical agricultural chemistry. Kalyani Publishers, NEW DELHI, INDIA.

  • Kumar, Arun, Natarajan, V.S. and Sivasamy, R. (2002). Characterization and classification of soils of lower palarmanimuthar watershed of Tamil Nadu. Agropedology, 12: 97-103.

  • Lyon, R.J.P. and Tuddenhan, W.M. (1959). Quantitative mineralogy as a guide in exploration. Mining. Eng., 214 : 1- 5.

  • Pillai, M.Y. and Natarajan, A. (2004). Characterization and classification of dominant soils of parts of Garakahalli watershed using remote sensing technique. Mysore J. Agric. Sci., 38 : 193-200.

  • Schoeneberger, P.J., Wysocki, D.A. and Benham, E.C. (2012). Field Book for Desctibing and Sampling Soils. Ver. 3.0. Lincoln, NE: Natural Resources Conservation Service, National Soil Survey Center, F. A. O., 1993a, Frame work for Land Evaluation. Soils Bulletin, 32, ROME, ITALY.

  • Sehgal, J.L., Challo, O., Gajja, B.L. and Yadav, S.C. (1989). Suitability of swell shrink soils of India for crop growth. In: Soil for development. Ed. Van Cleemut et al. ITC Ghent Publication Series, 1 : 29-53.

  • Sharma, S.S., Totawat, K.L. and Shyampura, R.L. (1996). Characterization and classification of soils to toposequence over basaltic tarrain.J. Indian Soc. Soil Sci.,45 : 480-485.

  • Sharma, V.K., Sharma, P.D., Sharma, S.P., Acharya, C.L. and Sood, R.K. (2004).Characterization of cultivated soils of Neogal watershed in North-West Himalayas and their suitability for major crops.J. Indian Soc. Soil Sci., 52 : 63-68.

  • Singh, I.S. and Agrawal, H.P. (2005). Characterization, genesis and classification of rice soils of Eastern region of Varanasi, Uttar Pradesh. Agropedol., 15 : 29–38.

  • Sitanggang, M., Rao, Y.S., Nayan Ahmed and Mahapatra, S.K. (2006). Characterization and classification of soils in watershed area of Shikohpur, Gurgaon district, Haryana. J. Indian Soc. Soil Sci., 54 : 106–110.

  • Szabolcs, I. (1971). Solonetz soils in Europe. In: European solonetz soils and their reclamation. pp. 9-33 (Szabolcs I. Ed.) AkademiaiKiado, Budapest.

  • Szendrei, G. (1999). Micromorphology of domestic saltaffected soils.AgrokemiaesTalajtan.48:481-490. (in Hungarian)

  • Thomas, M.D. (1921). Aqueous vapor pressure of soil sci. 11 :409-434.

  • Tinker, P.B. and Nye, P.H. (2000). Solute movement in the rhizosphere. Oxford University Press. NEW YORK, U.S.A.

  • Tripathi, D., Verma, J.R., Patial, K.S. and Singh, Karan (2006).Characteristics, classification and suitability of soils for major crops of Kiar-Nagali, micro-water shed in north– west Himalays. J. Indian Soc. Soil Sci., 54 (2) : 131-136.

  • Walkley, A. and Black, I.A. (1934). An estimation of the method for determining soil organic matter and a proposed modification of the chromic acid titration method. Soil Sci., 37: 29-38.

  • Zende, N.A. (1987). Soils of Nagaland and relation to physiography, their characteristics and classification. J. Indian Soc. Soil Sci., 35 : 706.


Abstract Views: 346

PDF Views: 0




  • Characterization of Salt-Affected Soils of Faizabad District

Abstract Views: 346  |  PDF Views: 0

Authors

Maneesh Kumar
Department of Soil Science and Agricultural Chemistry, College of Agriculture, Narendra Deva University of Agriculture and Technology, Kumarganj, Faizabad (U.P.), India
Neeraj Kumar
Department of Soil Science and Agricultural Chemistry, College of Agriculture, Narendra Deva University of Agriculture and Technology, Kumarganj, Faizabad (U.P.), India
Ved Prakash
Department of Soil Science and Agricultural Chemistry, College of Agriculture, Narendra Deva University of Agriculture and Technology, Kumarganj, Faizabad (U.P.), India
S. K. Yadav
Department of Soil Science and Agricultural Chemistry, College of Agriculture, Narendra Deva University of Agriculture and Technology, Kumarganj, Faizabad (U.P.), India
Adesh Kumar
Department of Soil Science and Agricultural Chemistry, College of Agriculture, Narendra Deva University of Agriculture and Technology, Kumarganj, Faizabad (U.P.), India
Ram Bharose
Department of Soil Science and Agricultural Chemistry, College of Agriculture, Narendra Deva University of Agriculture and Technology, Kumarganj, Faizabad (U.P.), India

Abstract


A study was undertaken to characterize the soils of Faizabad district, Uttar Pradesh in order to assess their land capability. The soils were described in the morphology, characteristics. Themorphological properties of soils were studied and later on analyzed in laboratory for their physical and chemical properties. Thickness of Ap horizon was less in pedon number 1(20 cm), pedon number 2 and 3 (22 cm) and pedon number 4 and 5 (25 cm). The solum depth of all the profiles ranged from 85 to 100 cm. The colour of surface soil of pedons 1, 2, 3, 4 and 5 were light gray (10 YR 7/1 and 10YR 7/2) when dry and light yellowish brown (10 YR 6/4) when moist.The soil colour of sub-surface horizons was strong brown (7.5YR 5/6). Surface soil structure of the pedon was fine prismatic while it was fine sub-angular blocky of other pedons. The consistency of surface and sub-surface soils varied from slightly hard to very hard, friable to extremely firm.It was non-sticky, non-plastic to sticky, plastic in dry, moist and wet conditions, respectively in all the pedons.

Keywords


Pedon, Horizon, Structure.

References