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Journal of Applied Sciences and Environmental Management
World Bank assisted National Agricultural Research Project (NARP) - University of Port Harcourt
ISSN: 1119-8362
Vol. 11, No. 2, 2007, pp. 71-75
Bioline Code: ja07028
Full paper language: English
Document type: Research Article
Document available free of charge

Journal of Applied Sciences and Environmental Management, Vol. 11, No. 2, 2007, pp. 71-75

 en Influence of Physical Raking and Biological Process in the Mud-water Exchange Dynamics of P in Fish Culture Ponds
Bhakta, Jatindra N.; Biswas, Jayanta K. & Jana, Bana B.

Abstract

Experiment was conducted in the laboratory using radioactive 32P for ascertaining the dynamics and quantifying the exchangeable amount of P between sediment and water phase under the influence of physical raking and biological processes. Collected sediment (100 g) was dispensed in a glass beaker and treated with radioactive 32P after reaction with CaCO3. Each beaker filled with 250 ml tap water. Four different treatments: physical raking once (RO), repeated raking (RR), bacteria (Bacillus, 167 X 102 ml-1) inoculum (BI) and bacteria inoculum (Bacillus, 167 X 102 ml-1) plus repeated raking (BI + RR) were used in the study. Water samples were collected and tested for specific activity of radioactive 32P, concentration of orthophosphate and count of heterotrophic bacterial (HB) population. The 32P value of BI+RR treatment was 20, 25, 37 and 56% higher than BI, RR, RO and control, respectively. Therefore, it can be concluded that synergistic effect of bacteria inoculum plus repeated raking (BI + RR) released maximum amount of phosphorus than the rest three treatments. Critical appraisal of data clearly revealed four states of dynamic of 32P between sediment and overlaying water: initial rapid increase of 32P level in water - rapid desorption period (RDP) from day 0 to 12, slow increase of 32P level of water - slow desorption period (SDP) from day >12 to 55, the 32P moves to sediment resulting in decrease 32P level in water - absorption period (AP) from day >55 to 90 and steady period (SP) from day >90 to 124, when 32P concentration of water and sediment supposed to be equal indicating no movement of 32P occurred between the water and sediment phase

 
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