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
A semi-analytical model for dissolved oxygen mass transfer coefficient at the sediment–water interface
Relying on the fundamental principles of mass transport in a turbulent flow, we have developed a semi-analytical model for a mass transfer coefficient in a sediment water interface over a smooth bed. The governing equations with boundary conditions reflect a mechanism of shear dispersion in a turbulent flow. The model is formulated in terms of the Sherwood-Reynolds-Schmidt functional dependence. Unlike previous regression-type models, the mass transfer coefficient at the sediment-water interface is parameterized by the friction coefficient. Flow conditions over a smooth bed ranging in Reynolds number from 1800 to 7000 were used to verify the model. The predicted mass transfer coefficients are in very good agreement with the experimental data.
Application of 2μm Tm Laser on Biomedicine
Continuous wave Thulium laser emits at wavelength of 2.0 mm, which is well suited for tissue ablationand thermally stimulating cutaneous nerves due to its high absorption by water. 2 mm laser can be transmitted suffi-ciently by common quartz fibers and it is safe for eyes. A brief introduction of principle of 2 mm CW Tm Laser is giv-en, analyzing the photothermal modeling of thulium laser-tissue interaction, comparing 2 mm CW Tm Laser with tradi-tional laser.