“…This can be appreciated by the fact that for a potato crop field of Poland it was reported that particulate input of only 263 g C m 22 resulted in an increase of 103 g C m 22 (Melillo, 1985), while in the maize field in Central Himalayas, similar amount of organic matter input could not even offset the decline in the carbon status of the soil (Singh and Singh, 1992), where deforestation leads to an agricultural land-use, higher rates of erosion will be maintained indefinitely (Rapp, 1975) unless practices of soil conservation are especially followed (Doran, 1980). The throughfall, stemflow, and canopy interception results are similar to that of forests of the Central Himalayas Negi et al, 1998;Jain et al, 2000). Throughfall in the TNFD was highest as a result of more canopy coverage and broad leaf nature of natural forest species than the mixed open forest.…”