S. K. Srivastava

Pattern of two wheeler road traffic accidents in rural setting: a retrospective study

BACKGROUND: Roads and vehicles which are for making life comfortable and faster, can result in miserable life when one meet a road traffic accident. By 2020 road traffic accident is projected to become the third leading contributor to the global burden of disease in the world and 6th place as a major cause of mortality worldwide. Motor cyclists are about 25 times more risk than passenger car occupants to die because of road traffic accidents. OBJECTIVEs of the study were, to study pattern of two wheeler road traffic accidents in rural setting. Methods: The present research is a retrospective analysis of all the two-wheeler accidents victim admitted in emergency, during the period ranging from September 2015 to February 2016. Results: Among the total 2,544 patient of RTA admitted within the study period; 1,257 patients (i.e.49.41%) were due to two-wheeler accidents. Next is pedestrian (n=516, 20.2%), light motor vehicle (n=464, 18.23%), and heavy motor vehicle accidents contribute (n=307, 12.06%). Conclusions: lack of road driving sense and lack of knowledge of traffic rules. Regarding the type of vehicles involved in these accidents, the maximum number of accidents was due to two wheeler vehicles (scooter/motorcycle). Keywords: Two wheeler RTA, Stray animals, Rural RTA

Radioelement-bearing Secondary Zoned Apatite around Govardhanagiri-Chinnakolumulapalli-L. Banda Areas of Kurnool District, Andhra Pradesh

Zoned Apatite crystals with intrinsic radioactivity are widespread in the S-type basement granite around Govardhanagiri-Chinnakolumulapalli-L.Banda areas of Kurnool District, A.P. The granite is overlain by Gulcheru quartzite and in turn by Vempalle dolostone of Papaghni Group belonging to the Cuddapah Supergroup. The area (4 km x 6 km) is characterized by conjugate fracture system comprising ENE-WSW and WNW-ESE of varying extents, of which, ENE-WSW is sympathetic to the major deep seated Gani Kalva fault. The apatite crystals are frequently zoned and vary in size from few microns to 1000 microns, occur mostly as veins or associated with pulverized matrix of granite cataclasite. Veins (upto 2 cm. thick) generally follow the major fracture-trend (ENE-WSW) in the area. The apatites are also found intimately associated with fluorite, tourmaline and sulphides, which suggest their derivation from pneumatolytic fluids. The intrinsic accessory uranium as scarce grains of uraninite and other labile phases of granite were remobilized consequent upon the deformation and locked up as ferroan-oxy/hydroxyl inclusions in slowly growing apatite crystals under very low temperature conditions.