Efflux of intracellular versus plasma membrane cholesterol in HepG2 cells: different availability and regulation by apolipoprotein A-I

We have compared the efflux of cholesterol from different cellular pools of human hepatoma cells HepG2 using intact cells or isolated membrane fractions. To label different pools, cells were incubated with either unesterified [14C]cholesterol that had been incorporated into high density lipoproteins ([14C]FC-HDL), low density lipoproteins ([14C]FC-LDL), or phosphatidylcholine liposomes ([14C]FC-PC), or with [14C]acetate. Cell fractionation revealed that labeling of cells with [14C]FC-PC resulted in the incorporation of [14C]cholesterol almost exclusively into the plasma membrane (PM), while incubation with [14C]FC-HDL resulted in the majority of [14C]cholesterol incorporation into the PM, but with a smaller component associated with lysosomes. Labeling with [14C]FC-LDL or [14C]acetate led to an accumulation of [14C]cholesterol predominantly in lysosomes or the endoplasmic reticulum (ER), respectively. When the kinetics of [14C]cholesterol efflux was analyzed after pulse-labeling of different cellular pools, half-times of cholesterol efflux from lysosomes and ER were significantly longer than that from PM. In another set of experiments, when both labeling and efflux times varied, efflux of [14C]cholesterol from the PM to human serum after 1.5 h pulse and chase incubations was double that from lysosomes and 8-fold that from ER. Extension of the incubation times from 1.5 to 3 h diminished the difference in cholesterol efflux from different membranes. Further incubation to 6 h almost abolished the different responses. Cell-free preparations of membranes, obtained from cells labeled with [14C]cholesterol, showed no differences in cholesterol efflux. No differences in the distribution of [14C]cholesterol released into serum among lipoprotein subfractions was observed. Pretreatment of the serum with Fab fragments of polyclonal rabbit anti-human apolipoprotein A-I antibodies reduced its ability to promote efflux of cholesterol from the ER by 77%, but had no effect on cholesterol efflux from the PM. Fab fragments of non-immune IgG had no effect on the efflux of both ER and PM cholesterol. We conclude that the availability of cellular cholesterol for efflux from HepG2 cells is strongly influenced by its subcellular location, and is regulated by apolipoprotein A-I.     

Electron energy distribution in CO2laser discharges

Electrical plasma parameters of the CO2laser were investigated by probe and high-frequency techniques. The electron energy distribution function was measured by the second derivative method. The relatively high-pressure effect on the electron probe current was taken into account when analyzing the experimental curves. The influence of the addition of N2, He, Xe and the influence of CO2dissociation on the plasma discharge properties were studied. Calculations of the pumping rates to vibrational levels taking part in creating inversion show that the influence on output power of a CO2laser usually observed with the addition of N2and He cannot be explained by a changing of the electron component of the plasma. The increase of output power and efficiency with addition of Xe to the CO2laser is connected with an essential changing of plasma parameters of the electron component.     

Determination of static balance in a spiral spring manipulator

Translated from Khimicheskoe i Neftyanoe Mashinostroenie, No. 7, pp. 23–24, July, 1993.     

Density and microhardness of glasses in the SrO-B<Subscript>2</Subscript>O<Subscript>3</Subscript>-SiO<Subscript>2</Subscript> system

The density d at a temperature of 25°C is measured by the hydrostatic weighing method, the Vickers microhardness H _V is determined, and the fluctuation free volume fraction f _g is calculated for glasses in the SrO-B₂O₃-SiO₂ system with a constant strontium oxide content in the range from 35 to 45 mol %. It is demonstrated that the quantities H _V and f _g decrease and the density d increases with an increase in the SrO content.     

An overview of geoengineering of climate using stratospheric sulphate aerosols

We provide an overview of geoengineering by stratospheric sulphate aerosols. The state of understanding about this topic as of early 2008 is reviewed, summarizing the past 30 years of work in the area, highlighting some very recent studies using climate models, and discussing methods used to deliver sulphur species to the stratosphere. The studies reviewed here suggest that sulphate aerosols can counteract the globally averaged temperature increase associated with increasing greenhouse gases, and reduce changes to some other components of the Earth system. There are likely to be remaining regional climate changes after geoengineering, with some regions experiencing significant changes in temperature or precipitation. The aerosols also serve as surfaces for heterogeneous chemistry resulting in increased ozone depletion. The delivery of sulphur species to the stratosphere in a way that will produce particles of the right size is shown to be a complex and potentially very difficult task. Two simple delivery scenarios are explored, but similar exercises will be needed for other suggested delivery mechanisms. While the introduction of the geoengineering source of sulphate aerosol will perturb the sulphur cycle of the stratosphere signicantly, it is a small perturbation to the total (stratosphere and troposphere) sulphur cycle. The geoengineering source would thus be a small contributor to the total global source of 'acid rain' that could be compensated for through improved pollution control of anthropogenic tropospheric sources. Some areas of research remain unexplored. Although ozone may be depleted, with a consequent increase to solar ultraviolet-B (UVB) energy reaching the surface and a potential impact on health and biological populations, the aerosols will also scatter and attenuate this part of the energy spectrum, and this may compensate the UVB enhancement associated with ozone depletion. The aerosol will also change the ratio of diffuse to direct energy reaching the surface, and this may influence ecosystems. The impact of geoengineering on these components of the Earth system has not yet been studied. Representations for the formation, evolution and removal of aerosol and distribution of particle size are still very crude, and more work will be needed to gain confidence in our understanding of the deliberate production of this class of aerosols and their role in the climate system.