Changes with time in soil biomass C, N and P of mine spoils in a dry tropical environment

Srivastava, S. C. ; Jha, A. K. ; Singh, J. S. (1989) Changes with time in soil biomass C, N and P of mine spoils in a dry tropical environment Canadian Journal of Soil Science, 69 (4). pp. 849-855. ISSN 0008-4271

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Official URL: http://pubs.aic.ca/doi/abs/10.4141/cjss89-085

Related URL: http://dx.doi.org/10.4141/cjss89-085

Abstract

Soil biomass C, N and P were determined for a native forest site, an unmined deforested site and an age-series of adjacent coal mine spoils (5, 10, 12, 16 and 20 yr). Biomass C ranged from 209 to 867 μ g/g−1 soil, biomass N from 20 to 75 μ g/g−1 soil and biomass P from 7 to 29 μ g/g−1 soil. Biomass C, N and P were linearly related to each other. Biomass C was also related to the root biomass. Biomass N with a mean C:N ratio of 11.8 accounted for 2.2-4.2% of the total soil N and was positively related to the mineral N of soil. Biomass C:P ratio ranged from 27.6 to 31.0%. The biomass P was significantly related to the bicarbonate soluble soil Pi. Soil microbial biomass was characterized by a mean C:N:P ratio of 29:3:1. Soil microbial C, N and P were positively related with the age of mine spoils, the values for the youngest spoil (5 yr old) being about four times lower compared to native forest soil. Total soil N was also positively related with age of spoil. The data suggest that microbial biomass can be taken as a functional index of soil redevelopment.

Item Type:Article
Source:Copyright of this article belongs to Agricultural Institute of Canada.
Keywords:Surface Coal Mining; Soil Microbial Biomass C; Biomass N; Biomass P; Mine Spoil
ID Code:73102
Deposited On:03 Dec 2011 04:36
Last Modified:03 Dec 2011 04:36

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