A study of methods for the classification of bottom deposits of natural waters
The study of the role of bottom sediments of rivers and maturation ponds in the purification of polluted waters which flow over them has been handicapped by lack of suitable methods for classifying sediments according to their physical, chemical and biochemical characteristics . Bottom deposits of lakes, rivers and dams may be regarded as soils which have developed under humid and water-logged conditions . The judicious application of the methods developed by soil scientists for the assessment of agricultural soils to the evaluation of certain important characteristics of sediments is therefore a logical development. Pioneering work in this respect was done by ZULLIG (1955) who applied a number of the methods of soil analysis to bottom deposits of eutrophic and oligotrophic lakes in Switzerland and attempted to correlate the results with the degree of trophy of the lake. Both he and OHLE (1955) pointed out that bottom deposits have ion-exchange properties which can contribute to the removal of ions from the water phase into the muds, but neither of these workers attempted to measure the extent to which this occurs quantitatively. In the present study a number of methods used to determine chemical, physical and biochemical properties of soils have been applied to bottom sediments from the Apies River near Pretoria, including samples taken near its origin where it is free from pollution, below the point of discharge of treated effluent from the Pretoria Sewage Works, where considerable pollution occurs and further
Summer bacterial populations in Mississippi River Pool 19: implications for secondary production
Bacterial populations were sampled at 37 sites in Mississippi River Pool 19. Bacterial biomass was calculated from direct epifluorescent cell counts. Bacterial production was estimated by incubating cells in situ in predator-free water inside membrane chambers and the frequency of dividing cells. Bacterial biomass in the water column ranged from 0.05 to 1.13 mg C ℓ -1, biomass in the vegetated areas of the pool was significantly higher than that in other habitats (P < 0.05, ANOVA). Biomass in sediments (to a depth of 10 cm) ranged from 24 to 1,073 mg C m-2, biomass in muddy sediments was significantly higher (P < 0.05) than that in sandy sediments. Biomass on the submersed surfaces of hydrophytes was 0.06–4.90 mg bacterial C g-1 dry weight of plant material. The vegetated habitat (water column plus vegetation) contained approximately 45 times the concentration of bacterial carbon found in nonvegetated main channel border areas and more than 100 times the concentration in the main river channel.Bacterial production rates in the water column of a vegetated section of the pool ranged from 0.03 to 3.28 g C m -3 s d -1 ; production (m -3) in a vegetation bed was 5.5 times that in the adjacent nonvegetated channel border areas and approximately 50 times that in the main channel. Aquatic macrophytes and associated microorganisms may be capable of providing significant inputs of carbon to secondary consumers in the pool during the summer low flow.
A device for uranium series leaching from glass fiber in HEPA filter
For the disposal of a high efficiency particulate air (HEPA) glass filter into the environment, the glass fiber should be leached to lower its radioactive concentration to the clearance level. To derive an optimum method for the removal of uranium series from a HEPA glass fiber, five methods were applied in this study. That is, chemical leaching by a 4.0 M HNO3–0.1 M Ce(IV) solution, chemical leaching by a 5 wt% NaOH solution, chemical leaching by a 0.5 M H2O2–1.0 M Na2CO3 solution, chemical consecutive chemical leaching by a 4.0 M HNO3 solution, and repeated chemical leaching by a 4.0 M HNO3 solution were used to remove the uranium series. The residual radioactivity concentrations of 238U, 235U, 226Ra, and 234Th in glass after leaching for 5 h by the 4.0 M HNO3–0.1 M Ce(IV) solution were 2.1, 0.3, 1.1, and 1.2 Bq/g. The residual radioactivity concentrations of 238U, 235U, 226Ra, and 234Th in glass after leaching for 36 h by 4.0 M HNO3–0.1 M Ce(IV) solution were 76.9, 3.4, 63.7, and 71.9 Bq/g. The residual radioactivity concentrations of 238U, 235U, 226Ra, and 234Th in glass after leaching for 8 h by a 0.5 M H2O2–1.0 M Na2CO3 solution were 8.9, 0.0, 1.91, and 6.4 Bq/g. The residual radioactivity concentrations of 238U, 235U, 226Ra, and 234Th in glass after consecutive leaching for 8 h by the 4.0 M HNO3 solution were 2.08, 0.12, 1.55, and 2.0 Bq/g. The residual radioactivity concentrations of 238U, 235U, 226Ra, and 234Th in glass after three repetitions of leaching for 3 h by the 4.0 M HNO3 solution were 0.02, 0.02, 0.29, and 0.26 Bq/g. Meanwhile, the removal efficiencies of 238U, 235U, 226Ra, and 234Th from the waste solution after its precipitation–filtration treatment with NaOH and alum for reuse of the 4.0 M HNO3 waste solution were 100, 100, 93.3, and 100%.