M. HARSHITHA1*, S.L. BUDHIHAL2
1Department of Soil Science and Agricultural Chemistry, University of Agricultural Sciences, Raichur, 584 104, Karnataka, India
2Department of Soil Science and Agricultural Chemistry, University of Agricultural Sciences, Raichur, 584 104, Karnataka, India
* Corresponding Author : harshireddym29@gmail.com
Received : 31-05-2018 Accepted : 10-06-2018 Published : 15-06-2018
Volume : 10 Issue : 11 Pages : 6249 - 6252
Int J Agr Sci 10.11 (2018):6249-6252
Keywords : Associated red and black pedons, Clay mineralogy, Sand mineralogy
Academic Editor : Dr A. K. Singh, Dr Rishikesh Thakur
Conflict of Interest : None declared
Acknowledgements/Funding : Author thankful to University of Agricultural Sciences, Raichur, 584 104, Karnataka, India
Author Contribution : All author equally contributed
The Hira region of Hatti schist belt a transect of associated red and black soils were selected and studied for their properties. Soils were moderately deep to deep, reddish brown (5YR 3/4) to dark black (10YR3/2), clay in texture. Smectite was overwhelmingly the dominant mineral with the traces of kaolinite and shows interstratification on ethylene glycol solvation. Quartz, plagioclase feldspar, olivines, siderites, amphiboles and ferrihydrides were found in all the pedons.
1. Anonymous (1987) Gazetteers of Bombay State, Dharwad district, 985.
2. Desai D. (1942) Hyderabad Department of Agricultural Bulletin No 10, Hyderabad
3. Ferraj A. S. (2008) J. of Agron.,7, 115-126.
4. Jackson M. L. (1969) Soil chemical analysis- Advanced course. Edition 2 ,895.
5. Krienitz M. (2008) Min. Dep.,43, 421-34.
6. Manikyamba C., Naqvi S., Mohan M. and Rao T., (2004) Ore Geology Reviews, 24, 199-227.
7. Padole V.R. and Thakare G.A. (1999) PKV Research J.,23(1), 28-35.
8. Rajamani V., And Siddaiah N. and Rajamani V., Ramgiri (1989) Economic Geology, 84, 2155-2172.