Aim:To evaluate the biocompatibility of a new root canal irrigant Q mix™ 2 in 1 in comparison to 0.9% sterile saline, 3% sodium hypochlorite (NaOCl), 2% chlorhexidine (CHX), and 17% ethylenediaminetetraacetic acid (EDTA).Materials and Methods:Six circles were drawn on the dorsal skin of 24 male Wistar Albino rats, leaving 2cm between each circle. Using a syringe, 0.1mL of each root canal irrigant was injected subcutaneously into five circles. In the sixth circle, the needle of an empty syringe was introduced into the skin, but no irrigant was injected (control group). Evaluations were done at 2 hours, 48 hours, 14 days, and 30 days postprocedure. Tissue samples were excised, embedded in paraffin blocks, and 3 μm thick sections were obtained and stained with hematoxylin and eosin. The areas of inflammatory reaction were evaluated. From each tissue sample, five sections presenting the greatest inflammatory reactions were examined under a light microscope, and analyzed statistically by analysis of variance (ANOVA) and Tukey's test.Results:At the two-hour examination period, all the irrigants showed a slight increase in the number of inflammatory cells, at 48 hours, the number of inflammatory cells were increased significantly, and after 14 and 30 days, they were decreased gradually. Qmix™ 2 in 1 showed a smaller number of inflammatory cells than other irrigants tested.Conclusion:QMix™ 2 in 1 was shown to be less toxic to the rat subcutaneous tissue than 3% NaOCl, 2% CHX, and 17% EDTA.
During the last three decades, the eastern segment of the Makran subduction zone has been more active than the western segment. We analyze Makran seismicity using the NEIC catalog from 1973 to 2008. A temporal decrease of b-value in eastern Makran indicates that stress is increasing, which may signal a future sizable earthquake. Also, the spatial variation of b suggests that the western segment is less stressed compared to the eastern segment. It has been observed that the fractal dimension is approximately twice the b value. The seismicity pattern analyzed does hold a key to understanding the seismotectonics of the region.
Abstract. The complexity in the tsunami phenomenon makes the available warning systems not much effective in the practical situations. The problem arises due to the time lapsed in the data transfer, processing and modeling. The modeling and simulation needs the input fault geometry and mechanism of the earthquake. The estimation of these parameters and other aprior information increases the utilized time for making any warning. Here, the wavelet analysis is used to identify the tsunamigenesis of an earthquake. The frequency content of the seismogram in time scale domain is examined using wavelet transform. The energy content in high frequencies is calculated and gives a threshold for tsunami warnings. Only first few minutes of the seismograms of the earthquake events are used for quick estimation. The results for the earthquake events of Andaman Sumatra region and other historic events are promising.
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