Open Access Open Access  Restricted Access Subscription Access

Influence of Minerology on the Engineering Properties of Lateritic Soil

Amrutha U. A., Anjana S. Kumar, Gopika Chandran, Jaseena Amsaj N., Shruthi Johnson, Dr.Jayamohan J.

Abstract


Laterite is a soil which is having a high content of iron and aluminium and is mostly found in hot and wet tropical areas. They are formed through a process known as Laterization which is a combination of intensive and prolonged chemical process and leaching. The mineralogical compound of various samples of lateritic soils will be identified by carrying out microscopic analysis. The influence of mineralogical composition on bearing capacity will be investigated by carrying out laboratory scale load tests on model footings.


Full Text:

PDF

References


Alexander, L. T., & Cady, J. G. (1962). Genesis and hardening of laterite in soils (Vol. 1281). US Department of Agriculture.

Buchanan, F. (2020). A journey from Madras through the countries of Mysore, Canara, and Malabar. BoD–Books on Demand.

Martin, F. J., & Doyne, H. C. (1927). Laterite and lateritic soils in Sierra Leone. The Journal of Agricultural Science, 17(4), 530-547.

Prasad, T. K., & Parthasarathy, G. R. (2018). Laterite and Laterization-A Geomorphological Review. International Journal of Science and Research (IJSR), 7(4), 578-583.

Chandran, P., Ray, S. V., Bhattacharyya, T., Srivastava, P., Krishnan, P., & Pal, D. K. (2005). Lateritic soils of Kerala, India: their mineralogy, genesis, and taxonomy. Soil Research, 43(7), 839-852.

Balakrishnan, V. C., Palot, M. J., & Rajesh, K. P. (2010). Observations on the flora of Madayipara a midland laterite hill in Kannur district, Kerala. Malabar Trogon, 8(2&3), 14-29.


Refbacks

  • There are currently no refbacks.