Research Article | Published: 01 December 2008

Morphology, mineralogy and classification of soils developed on different parent material in Mussoorie forest division, Uttarakhand, India

A. K. Raina

Indian Journal of Forestry | Volume: 31 | Issue: 4 | Page No. 533-540 | 2008
DOI: https://doi.org/10.54207/bsmps1000-2008-UVRW8C | Cite this article

Abstract

Based on reconnaissance soil survey of Kempty Range of Mussoorie Forest Division, Uttarakhand, five soil profiles in different blocks were selected for determining their morphological, physicochemical and mineralogical characteristics. The morphological characteristics show considerable variation in the nature and degree of horizon development. Light and heavy mineral fractions constituted 70 and 30 per cent of total fine sand fractions respectively. Various minerals identified in the light sand fractions included quartz, feldspars and mica (muscovite). In all the pedons studied quartz was the dominating mineral. Heavy mineral fractions comprised opaque minerals, biotite the presence of low to moderate amount of weatherable minerals suggesting their podsolic nature. Clay fractions were characterized by micas and illite as the dominant clay mineral associated with appreciable amount of kaolinite and chlorite and the small amount of mixed layer silicate mineral, vermiculite, montimorillonite and quartz. Soils of the study area belonged to Typic Paleudoll (Kempty Block), Typic Argiudoll (Sainj Block), Typic Paleudult (Mailgarh Block), Typic Hapludult (Kheragarh Block) and Typic Argiudoll (Gandiyala Block). All these polypedons are members of fine loamy, mixed, messic family. These soils developed from different parent materials are in equilibrium with geogenic factors. Mollisols occur on limestone, dolomite, quartzite and slate whereas Ultisols occur on phyllite, shale, sandstone, quartzite, etc.

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References

1. Black, C.A. (1965). Methods of Soil Analysis. Am. Soc. Agron. Inc. Madison, USA.  https://doi.org/10.2134/agronmonogr9.1

Google Scholar

2. Cady, J.G. (1965). Petrographic Microscopic Techniques. In: Methods of Soil Analysis. Part I. Physical and Mineralogical Properties, Black, C.A. (ed). American Society of Agronomy Inc. Madison, Wisconsis, U.S.A. 604.  https://doi.org/10.2134/agronmonogr9.1.c46

Google Scholar

3. Champion, H.G. and Seth, S.K. (1968). A Revised Survey of Forest Types of India. Manager of Publications, New Delhi.

Google Scholar

4. Day, P.R. (1965). Particle fractionation and Particle Size Analysis. Methods of Soil Analysis. Part I, Physical and Mineralogical Properties (C.A. Black, Ed.), Am. Soc. Agron. Inc. Madson, Wisconsis, U.S.A.: 545.  https://doi.org/10.2134/agronmonogr9.1.c43

Google Scholar

5. Gupta, R.D. and Tripathi, B.R. (1996). Minerology Genesis and Classification of soils of North-West Himalayas developed different parent materials and variable topograph. J. Ind. Soc. Sci., 44(4):705-712.

Google Scholar

6. Jackson, M.L. (1967). Soil chemical Analysis. Prentice Hall of India Rt. Ltd., New Delhi.

Google Scholar

7. Kaistha, B.P. and Gupta, R.D. (1993). Morphology, mineralogy, genesis and classification of soils of subhumid temperate high lands of the central Himalayas. J. Ind. Soc. Soil. Sci., 41(1):120-124.

Google Scholar

8. Minhas, R.S., Harminder Minhas and Verma, S.D. (1997). Soil characterization in relation to forest vegetation in the wet temperate zone of Himachal Pradesh. J. Ind. Soc. Soil. Sci., 45(1):146-151.

Google Scholar

9. Pettijohn, F.J. (1957). Sedimentary Rocks. 2nd ed, Harper, New York.

10. Raina, A.K., Pharasi, S.C. and Prasad, K.G. (1994): Clay mineralogical composition in soils under different forest vegetation of Garhwal Himalayas – India. Indian Forester, 112(9):819-832.

Google Scholar

11. Raina, A.K., Jha, M.N. and Pharasi, S.C. (1998). Fine sand mineralogy of some selected soils of Mussoorie forest division of Uttar Pradesh. Indian Forester, 12411):883-890.

Google Scholar

12. Raina, A.K., Jha, M.N. and Pharasi, S.C. (1999). Morphology, mineralogy, genesis and classification of soils of Garhwal Himalayas developed on different parent materials. Annals of Forestry, 7(2):269-276.

Google Scholar

13. Raina, A.K. and Negi, S.S. (2007). Soil mineral relationship with different forest types in Mussoorie forest division of Uttaranchal, India. Himalayan Geology. 28(1):79-86.

Google Scholar

14. Samra, J.S., Singhal, R.M., Banerjee, S.P. and Sharma, S.D. (1985). Forest Soil characteristics with reference to clay mineralogy and natural vegetation Indian Forester, 111(1):22-27.

Google Scholar

15. Singh, K., Minhas, R.S. and Tomar, K.P. (1998). Characterization and classification of some Mid-Siwalik soils in different physiographic units. J. Indian Soc. Soil Sci., 38(3):474-480.

Google Scholar

16. Singhal, R.M. and Sharma, S.D. (1985). Study of the soils of Doon Valley Forest. J. Ind. Soc. Soil. Sci., 33:627-634.

Google Scholar

17. Singhal, R.M., Rawat, V.R.S. and Kumar, Pramod (1987). Soil-Vegetation relationship in some forest ranges of Chakrata Himalaya – India. Ind. J. Rang. Mgmt., 8(2): 91-101.

18. Singhal, R.M., Soni, Sunita and Sharma, S.D. (1989). Study of the soils of Mussoorie area (Garhwal Himalayas). Indian Forester, 149:924-933.

Google Scholar

19. Soil Survey Staff (1975). Soil Survey Laboratory Methods and Procedures for Collecting Soil Samples. Soil Survey Investigation Report No. 1, U.S. Govt. Printing Press, Washington, DC.

20. Yadav, J.S.P. (1963). Studies on soil profiles in Chakrata Division of Uttar Pradesh. Indian Forester, 89(1):18-38.

Google Scholar

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How to cite

Raina, A.K., 2008. Morphology, mineralogy and classification of soils developed on different parent material in Mussoorie forest division, Uttarakhand, India. Indian Journal of Forestry, 31(4), pp.533-540. https://doi.org/10.54207/bsmps1000-2008-UVRW8C

Publication History

Manuscript Published on 01 December 2008

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