Effect of Shifting Cultivation on Nutrient Status of Soil in Silonijan (Karbi-Anglong) Assam

Effect of Shifting Cultivation on Nutrient Status of Soil in Silonijan (Karbi-Anglong) Assam

Authors

  •   J. Singh
  •   I. P. Bora
  •   A. Baruah
  •   M. Hussain

DOI:

https://doi.org/10.36808/if/2003/v129i11/2413

Abstract

The present study highlights the changes of physico-chemical properties of soil during different phases of shifting cultivation and also in fallow lands of different ages. Burning resulted significant increase in soil pH, which decreased soil acidity and acidity increased as the fallow progressed. The percentage of sand increased while the clay percentage decreased after burning the sites. A drastic reduction in moisture content was recorded due to burning operation. Gradual decrease in conductivity was observed at the time of cropping and harvesting period, which increased with the fallow age. Jhuming caused appreciable change in organic matter content resulting nutrient imbalance in soil. Burning of the debris after slashing the forest leads to the depletion of organic carbon and nitrogen content in soil. However, the recovery of nitrogen in cropping phases is quite fast in comparison to carbon. Highest value of carbon content was noticed in winter season while nitrogen showed its highest value during the monsoon. Exchangeable Ca, Mg, K and available P increased just after burning and thereafter a gradual decrease was noticed in cropping phases. As the fallow progressed the value increased gradually. Nutrient status of soil was recorded significantly higher in natural forest than in the fallow lands and in all cases the value was inversely proportional to depth.

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Author Biographies

J. Singh

I. P. Bora

A. Baruah

M. Hussain

Published

2003-11-01

How to Cite

Singh, J., Bora, I. P., Baruah, A., & Hussain, M. (2003). Effect of Shifting Cultivation on Nutrient Status of Soil in Silonijan (Karbi-Anglong) Assam. Indian Forester, 129(11), 1329–1338. https://doi.org/10.36808/if/2003/v129i11/2413
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