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Effect of Profile Morphology on Root Development of Sal (Shorea robusta) Seedlings


     

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The article describes the effect of stratified profiles consisting of alternate layers of soil and sand of different thickness on ischolar_main development of sal seedlings. The seedlings were grown in two separate profiles of 18 inches thickness, one consisting of 6 inch thick sand layer in between two 6 inch thick soil layers and the other of 6 alternate layers of soil and sand each 3 inch thick with a soil layer at the top. The results indicate that 6 inch thick sand layer underlying soil layer of equal depth is unfavourable for ischolar_main development. It appears that a 3 inch thick top soil layer is incapable of supplying adequate amount of moisture and nutrients to meet the demand of seedlings and that 3 inch thick sand layer is not an impediment for deep ischolar_main penetration. The inference may be drawn that the soli profiles having sand layers 6 inch or more in thickness, especially if they underlie a thin top soil layer, may prove detrimental to the growth of sal seedlings particularly during the establishment stage and may be the cause of die-back or stagnation in such localities. On the contrary lengthy ischolar_mains stimulated by 3 inch thick alternate layers of soil and sand may be better able to tolerate drought conditions than those produced in the profile having a 6 inch thick intermediate sand layer where the ischolar_main development was arrested at the transition boundary between soil and sand.
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S. K. Seth

P. B. L. Srivastava


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  • Effect of Profile Morphology on Root Development of Sal (Shorea robusta) Seedlings

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Abstract


The article describes the effect of stratified profiles consisting of alternate layers of soil and sand of different thickness on ischolar_main development of sal seedlings. The seedlings were grown in two separate profiles of 18 inches thickness, one consisting of 6 inch thick sand layer in between two 6 inch thick soil layers and the other of 6 alternate layers of soil and sand each 3 inch thick with a soil layer at the top. The results indicate that 6 inch thick sand layer underlying soil layer of equal depth is unfavourable for ischolar_main development. It appears that a 3 inch thick top soil layer is incapable of supplying adequate amount of moisture and nutrients to meet the demand of seedlings and that 3 inch thick sand layer is not an impediment for deep ischolar_main penetration. The inference may be drawn that the soli profiles having sand layers 6 inch or more in thickness, especially if they underlie a thin top soil layer, may prove detrimental to the growth of sal seedlings particularly during the establishment stage and may be the cause of die-back or stagnation in such localities. On the contrary lengthy ischolar_mains stimulated by 3 inch thick alternate layers of soil and sand may be better able to tolerate drought conditions than those produced in the profile having a 6 inch thick intermediate sand layer where the ischolar_main development was arrested at the transition boundary between soil and sand.