Indonesian propolis: chemical composition, biological activity and botanical origin

From a biologically active extract of Indonesian propolis from East Java, 11 compounds were isolated and identified: four alk(en)ylresorcinols (obtained as an inseparable mixture) (1-4) were isolated for the first time from propolis, along with four prenylflavanones (6-9) and three cycloartane-type triterpenes (5, 10 and 11). The structures of the components were elucidated based on their spectral properties. All prenylflavanones demonstrated significant radical scavenging activity against diphenylpicrylhydrazyl radicals, and compound 6 showed significant antibacterial activity against Staphylococcus aureus. For the first time Macaranga tanarius L. and Mangifera indica L. are shown as plant sources of Indonesian propolis.     

Application of Validated TLC—Densitometric Method for Simultaneous Identification and Determination of Losartan Potassium,Telmisartan, and Valsartan in Tablets

JPC – Journal of Planar Chromatography – Modern TLC - The antihypertensive effect of sartans is a result of inhibition of the binding of angiotensin (AT) II to the AT1 receptor in...     

Measurements of soil radon in south Russia for seismological application: Methodological aspects

As a first step in the monitoring of soil radon in search of harbingers of earthquakes, an investigation of suitable measurement techniques was conducted. As a result of these investigations, the following recommendations are made. Semiconductor and scintillation (ZnS) counters are the most suitable for Rn monitoring with chambers for natural drift of emanations to the detector. The method of compulsory selection of soil air is hardly effective. Soil aerosols might enter the drift chamber; these aerosols transfer many radioactive isotopes. The most suitable locations for placement of detectors of radon are cellars. Measurements should be continuous in character. The choice of a place for monitoring near mud volcanoes and faults should be determined by an Rn survey. In mud volcanoes, the best locations are areas with an average concentration of radon. For faults, identical tendencies of change in radon are maintained at some distance from the borders of the fault. For large faults, this distance is equal to half the width of the fault. For small faults, this distance increases by up to 3 times the fault width. All the recommendations were applied in the Northern Caucasus. Reliable results of the changes in soil radon were obtained during strong geophysical processes.