To Study on Soil Nutrient and Physico�Chemical Analysis of Soil in Bar�Phatakhera�Raipur Section of Pali District, Rajasthan, India.

Beena Tripathi; Hemant Prakash; Vikas Bhagasra

Volume : VI, Issue : XII, December - 2016

To Study on Soil Nutrient and Physico�Chemical Analysis of Soil in Bar�Phatakhera�Raipur Section of Pali District, Rajasthan, India.

Beena Tripathi, Hemant Prakash, Vikas Bhagasra

Abstract :

The main constituents of soils are minerals and organic matter, which are produced by eaking up the rock particles. The soil enriching with organic matter from aerial and subterranean parts and are influenced by biological activities. The role of the vegetation is relatively less in arid zones because of the scanty sparse canopy cover and the poor development of aerial parts but the root systems often exhibit exceptional development and have the greatest influence of the cracking of the rocks influencing soils formation processes. The parent rocks had definite relation with the soil nutrient and material which supports the vegetations. But in western Rajasthan the studies of relation between parent rock material and soil and further correlation of these aspects with different types of vegetations e.g. herbs, shrubs and trees supported by the soil is quite deficient. The present paper, therefore, highlights by the fact that the vegetations including herbs, shrubs and trees and most importantly the herbaceous vegetation vary from soil to soil depending upon minerals present in the soil and these minerals are derived from the parent rock materials. The present investigation may idge this gap in the Aravalli hill ranges occurs in semi arid region. Therefore, the objective of this paper are i) to study the type of soils formed under the influence of parent rocks found in and around the Bar region of Delhi Supergroup; and ii) to investigate nutrient availability and different characters in soil for finding out its relation with the different type of vegetations it supports. River sands, gravels, cobbles, pebbles, and boulders are the main and chief sources of soil. ABSTRACT