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Extensive Distribution (extensive + distribution)
Selected AbstractsThe apparent volumes of distribution of H1 receptor antagonistsDERMATOLOGIC THERAPY, Issue 4 2000Jean-Paul Tillement ABSTRACT: The apparent volume of distribution (VD) of a drug estimates its distribution into the body. Referring to the volume of exchangeable water (0.6 L/kg body weight), it indicates if tissue distribution is extensive when VD is greater than 0.6 L/kg or poor if VD is less than 0.6 L/kg. Its interest in the selection of an appropriate drug is found after comparing the map of selected targets (mainly receptors) to be reached by the drug, the accessibility of these targets by the drug, and the VD necessary and sufficient to reach them. This analysis is here applied to H1 receptor antagonists, a pharmacologic class, where target cells, endothelial cells such as eosinophils, mastocytes, basophils, and smooth fibers have receptors on the external side of cell membranes and thus are more readily accessible from blood than toxic sites located inside cells (heart, brain, liver). Of the H1 receptor antagonists marketed today, cetirizine has the lowest VD, 0.4 L/kg, enough to reach selected targets without extensive distribution in organs where it would be useless. These characteristics are related to its chemical amphoteric structure. [source] Tafoni development in a cryotic environment: an example from Northern Victoria Land, AntarcticaEARTH SURFACE PROCESSES AND LANDFORMS, Issue 10 2008Andrea Strini Abstract Tafoni are a type of cavernous weathering widespread around the world. Despite the extensive distribution of the tafoni, their genesis is not clear and is still a matter of debate, also because they occur in such different climatic conditions and on so many different types of substrate. Geomorphological characterization of more than 60 tafoni in three different Antarctic sites (two coastal and one inland) between 74 and 76° S with sampling of weathering products and salt occurrences are described together with thermal data (on different surfaces) and wind speed recorded in different periods of the year in a selected tafone close to the Italian Antarctic station. The aim of this present study is to provide further information to help understand the processes involved in the growth of tafoni in a cryotic environment, and the relationship of these processes to climate, with particular attention to the thermal regime and the role of wind. The new data presented in this paper suggest that there is no single key factor that drives the tafoni development, although thermal stress seems the most efficient process, particularly if we consider the short-term fluctuations. The data also confirm that other thermal processes, such as freezing,thawing cycles and thermal shock, are not really effective for the development of tafoni in this area. The wind speed measured within the tafoni is half that recorded outside, thus favouring snow accumulation within the tafoni and therefore promoting salt crystallization. On the other hand, the wind effect on the thermal regime within the tafoni seems negligible. While both salt weathering and thermal stress appear active in this cryotic environment, these are azonal processes and are therefore active in other climatic areas where tafoni are widespread (such as the Mediterranean region). Copyright © 2007 John Wiley & Sons, Ltd. [source] Pharmacokinetics of gamithromycin in cattle with comparison of plasma and lung tissue concentrations and plasma antibacterial activityJOURNAL OF VETERINARY PHARMACOLOGY & THERAPEUTICS, Issue 3 2010R. A. HUANG Huang, R. A., Letendre, L. T., Banav, N., Fischer, J., Somerville, B. Pharmacokinetics of gamithromycin in cattle with comparison of plasma and lung tissue concentrations and plasma antibacterial activity. J. vet. Pharmacol. Therap.33, 227,237. The pharmacokinetics (PK) and dose proportionality of gamithromycin (ZACTRAN®), a novel azalide, after a single intravenous (i.v.) dose of 3 mg/kg or subcutaneous (s.c.) injection at 3, 6 and 9 mg/kg body weight were studied in 13 male castrate and 13 female Angus cattle. Following i.v. administration, the mean area under the curve extrapolated to infinity (AUCinf) was 4.28 ± 0.536 ,g·h/mL, and mean elimination half-life (t1/2) was 44.9 ± 4.67 h, with a large volume of distribution (Vss) of 24.9 ± 2.99 L/kg and a high clearance rate (Clobs) of 712 ± 95.7 mL/h/kg. For cattle treated with s.c. injection of 3, 6 or 9 mg/kg, mean AUCinf values were 4.55 ± 0.690, 9.42 ± 1.11 and 12.2 ± 1.13 ,g·h/mL, respectively, and the mean elimination half-lives (t1/2) were 51.2 ± 6.10, 50.8 ± 3.80 and 58.5 ± 5.50 h. Gamithromycin was well absorbed and fully bioavailable (97.6,112%) after s.c. administration. No statistically significant (, = 0.05) gender differences in the AUCInf or elimination half-life values were observed. Dose proportionality was established based on AUCInf over the range of 0.5 to 1.5 times of the recommended dosage of 6 mg/kg of body weight. Further investigations were conducted to assess plasma PK, lung/plasma concentration ratios and plasma antibacterial activity using 36 cattle. The average maximum gamithromycin concentration measured in whole lung homogenate was 18 500 ng/g at first sampling time of 1 day (,24 h) after treatment. The ratios of lung to plasma concentration were 265, 410, 329 and 247 at 1, 5, 10 and 15 days postdose. The lung AUCinf was 194 times higher than the corresponding plasma AUCinf. The apparent elimination half-life for gamithromycin in lung was 90.4 h (,4 days). Antibacterial activity was observed with plasma collected at 6 h postdose with a corresponding average gamithromycin plasma concentration of 261 ng/mL. In vitro plasma protein binding in bovine plasma was determined to be 26.0 ± 0.60% bound over a range of 0.1,3.0 ,g/mL of gamithromycin. The dose proportionality of AUC, high bioavailability, rapid and extensive distribution to lung tissue and low level of plasma protein binding are beneficial PK parameters for an antimicrobial drug used for the treatment and prevention of bovine respiratory disease. [source] Hydrocarbon Accumulation Conditions of Ordovician Carbonate in Tarim BasinACTA GEOLOGICA SINICA (ENGLISH EDITION), Issue 5 2010LI Qiming Abstract: Based on comprehensive analysis of reservoir-forming conditions, the diversity of reservoir and the difference of multistage hydrocarbon charge are the key factors for the carbonate hydrocarbon accumulation of the Ordovician in the Tarim Basin. Undergone four major deposition-tectonic cycles, the Ordovician carbonate formed a stable structural framework with huge uplifts, in which are developed reservoirs of the reef-bank type and unconformity type, and resulted in multistage hydrocarbon charge and accumulation during the Caledonian, Late Hercynian and Late Himalayan. With low matrix porosity and permeability of the Ordovician carbonate, the secondary solution pores and caverns serve as the main reservoir space. The polyphase tectonic movements formed unconformity reservoirs widely distributed around the paleo-uplifts; and the reef-bank reservoir is controlled by two kinds of sedimentary facies belts, namely the steep slope and gentle slope. The unconventional carbonate pool is characterized by extensive distribution, no obvious edge water or bottom water, complicated oil/gas/water relations and severe heterogeneity controlled by reservoirs. The low porosity and low permeability reservoir together with multi-period hydrocarbon accumulation resulted in the difference and complex of the distribution and production of oil/gas/water. The distribution of hydrocarbon is controlled by the temporal-spatial relation between revolution of source rocks and paleo-uplifts. The heterogenetic carbonate reservoir and late-stage gas charge are the main factors making the oil/ gas phase complicated. The slope areas of the paleo-uplifts formed in the Paleozoic are the main carbonate exploration directions based on comprehensive evaluation. The Ordovician of the northern slope of the Tazhong uplift, Lunnan and its periphery areas are practical exploration fields. The Yengimahalla-Hanikatam and Markit slopes are the important replacement targets for carbonate exploration. Gucheng, Tadong, the deep layers of Cambrian dolomite in the Lunnan and Tazhong-Bachu areas are favorable directions for research and risk exploration. [source] Widespread dispersal of Icelandic tephra: how does the Eyjafjöll eruption of 2010 compare to past Icelandic events?,JOURNAL OF QUATERNARY SCIENCE, Issue 5 2010Siwan M. Davies Abstract The Eyjafjöll AD 2010 eruption is an extraordinary event in that it led to widespread and unprecedented disruption to air travel over Europe , a region generally considered to be free from the hazards associated with volcanic eruptions. Following the onset of the eruption, satellite imagery demonstrated the rapid transportation of ash by westerly winds over mainland Europe, eventually expanding to large swathes of the North Atlantic Ocean and the eastern seaboard of Canada. This small-to-intermediate size eruption and the dispersal pattern observed are not particularly unusual for Icelandic eruptions within a longer-term perspective. Indeed, the Eyjafjöll eruption is a relatively modest eruption in comparison to some of the 20 most voluminous eruptions that have deposited cryptotephra in sedimentary archives in mainland Europe, such as the mid Younger Dryas Vedde Ash and the mid Holocene Hekla 4 tephra. The 2010 eruption, however, highlights the critical role that weather patterns play in the distribution of a relatively small amount of ash and also highlights the spatially complex dispersal trajectories of tephra in the atmosphere. Whether or not the preservation of the Eyjafjöll 2010 tephra in European proxy archives will correspond to the extensive distributions mapped in the atmosphere remains to be seen. The Eyjafjöll 2010 event highlights our increased vulnerability to natural hazards rather than the unparalleled explosivity of the event. Copyright © 2010 John Wiley & Sons, Ltd. [source] | |||||||||||||