Numerical and granulometric approaches to geophysical granular flows

Volcanic ash clouds can be fed by an upward-directed eruption column (Plinian column) or by elutriation from extensive pyroclastic-flows (coignimbrite cloud). For large-scale eruptions, there is considerable uncertainty about which mechanism is dominant. Here we analyze in a novel way a comprehensive grainsize database for pyroclastic deposits. We demonstrate that the Mount Pinatubo climactic eruption deposits were substantially derived from coignimbrite clouds, and not only by a Plinian cloud as generally thought. Coignimbrite ash-fall deposits are much richer in breathable <10 m ash (5–25 wt%) than pure Plinian ash at most distances from the source volcano. We also show that coignimbrite ash clouds, as at Pinatubo, are expected to be more water rich than Plinian clouds, leading to removal of more HCl prior to stratospheric injection, thereby reducing their atmospheric impact.

Weber fractions and time-order errors for long and short durations: Implications for modeling

Using a weighted up-down procedure, in each of eight conditions 28 participants compared durations of auditory (noise bursts) or visual (LED flashes) intervals; filled or unfilled with 3-ms markers; with or without feedback. Standards (Sts) were 100 and 1000 ms, and the ISI 900 ms. Intermixedly, presentation orders were St-Comparison (Co) and Co-St. TOEs were positive for St=100-ms and negative for St=1000 ms. Weber fractions (WFs, JND/St) were lowered by feedback. For visual-filled and visual-empty, WFs were highest for St=100 ms. For auditory-filled and visual-empty, St interacted with Order: lowest WFs occurred for St-Co with St=1000 ms, but for Co-St with St=100 ms. Lowest average WFs occurred with St-Co for visual-filled, but with Co-St for visual-empty. The results refute the generalization of better discrimination with St-Co than with Co-St (”type-B effect”), and support the notion of sensation weighting: flexibly differential impact weights of the compared durations in generating the response.

Fossil and Non-Fossil Sources of Different Carbonaceous Fractions in Fine and Coarse Particles by Radiocarbon Measurement

Radiocarbon offers a unique possibility for unambiguous source apportionment of carbonaceous particles due to a direct distinction of non-fossil and fossil carbon. In this work, particulate matter of different size fractions was collected at 4 sites in Switzerland to examine whether fine and coarse carbonaceous particles exhibit different fossil and contemporary sources. Elemental carbon (EC) and organic carbon (OC) as well as water-soluble OC (WSOC) and water-insoluble OC (WINSOC) were separated and determined for subsequent 14C measurement. In general, both fossil and non-fossil fractions in OC and EC were found more abundant in the fine than in the coarse mode. However, a substantial fraction (~20 ± 5%) of fossil EC was found in coarse particles, which could be attributed to traffic-induced non-exhaust emissions. The contribution of biomass burning to coarse-mode EC in winter was relatively high, which is likely associated to the coating of EC with organic and/or inorganic substances emitted from intensive wood burning. Further, fossil OC (i.e. from vehicle emissions) was found to be smaller than non-fossil OC due to the presence of primary biogenic OC and/or growing in size of wood-burning OC particles during aging processes. 14C content in WSOC indicated that the second organic carbon rather stems from non-fossil precursors for all samples. Interestingly, both fossil and non-fossil WINSOC concentrations were found to be higher in fine particles than in coarse particles in winter, which is likely due to primary wood burning emissions and/or secondary formation of WINSOC.

IN VITRO METABOLISM OF 6-THIOGUANINE IN RAT SUBCELLULAR FRACTIONS

The metabolism of the antitumor agent 6-thioguanine (TG, NSC-752) by rat liver was studied in vitro. Livers from adult male Sprague-Dawley rats were homogenized and the "liver homogenate" was subjected to differential centrifugation to obtain the "10,000 x g pellet", the "post-mitochondrial fraction", the "cytosol fraction", and the "microsomes". The homogenity of each fraction was estimated by appropriate marker enzyme assays. To delineate the in vitro metabolism of TG by rat liver, 0.2 mM of {8-('14)C}TG was incubated with different subcellular fractions in KCl-Tris-MgCl(,2) buffer, pH 7.4 at 37(DEGREES). The metabolites formed were identified by chromatography, UV spectrometry, as well as mass spectrometry. After a 1 hr incubation, TG was metabolized by the liver homogenate, the 10,000 x g pellet and the post-mitochondrial fraction mainly to 6-thioguanosine (TGR), accompanied by varying lesser amounts of 6-thiouric acid (TUA), allantoin, guanine-6-sulfinic acid (G-SO(,2)H) and an unknown product. In comparison, the cytosal fraction converted TG almost entirely to TGR and TUA in equal amounts. The formation of TGR from TG was limited by the endogenous supply of ribose-1-phosphate. With the microsomal fraction, however, TG was metabolized significantly to G-SO(,2)H and the unknown, accompanied with some TGR. After a 5 hr incubation the metabolism of TG was changed to favor the catabolic route, yielding mostly TUA in the post-mitochondrial and cytosol fractions; but mainly allantoin in the liver homogenate fraction. The kinetic studies of TG metabolism by the subcellar fractions indicated that the formation of TGR served as a depot form of TG. The level of TGR decreased when the catabolism of TG became prominent. The oxidation of TG to GSO(,2)H mediated by the hepatic microsomes represented a new catabolic pathway of TG. This GSO(,2)H, under acidic conditions, readily decomposes to guanine and inorganic sulfate. In the presence of reduced glutathione in Tris buffer, pH 7.8 at 25(DEGREES), GSO(,2)H is adducted to glutathione chemically to form S-(2-amino-purin-6-yl) glutathione and conceivably, inorganic sulfate. Therefore, the formation of GSO(,2)H from TG might have implication in the desulfuration mechanism of TG. On the other hand, the unknown formed from TG by the action of the microsomal enzymes appeared to be a TG conjugate. However, it is neither a glutathione, a glucuronide, nor a ribose conjugate. Additionally, the deamination of TG by guanine deaminase (E.C.3.5.4.3) isolated from rat liver was also investigated. TG is a poorer substrate (Km = 4.8 x 10('-3)M) for guanine deaminase than that of guanine (Km = 4.7 x 10('-6)M) at pH 7.25, optimal pH for TG as a substrate. TG is also a competitive inhibitor of guanine for guanine deaminase, with a ki of 2.2 x 10('-4)M. ^

Lability of Proteinaceous Material in Estuarine Seston and Subcellular Fractions of Phytoplankton

The rate of proteolysis of amino acids was used to assess the nutritional lability of various materials making up estuarine seston in 3 Maine, USA, estuaries. Physical separations of subcellular fractions of phytoplankton cells led to higher proteolysis rate constants for the cytoplasmic fraction (>1.2 h(-1)) than for the membrane fraction (0.2 to 1 h(-1)). Whole cells, copepod fecal pellets, bottom sediments, and estuarine seston had overlapping ranges of rate constants of 0.17 to 1.3 h(-1), which were indistinguishable from one another. Protein pools in the seston of these estuaries throughout the seasons were dominated by phytoplankton production and its fresh detrital products. Inverse relationships between proteolysis rate constants for estuarine seston and the ratios of pheopigments to chlorophyll indicates that the average lability of seston decreases with the disappearance of cytoplasmic material in suspension. This kinetic approach to the quality of food resources implies the existence of different pools of digestible protein for estuarine heterotrophs with different gut residence times. Preferential enrichment of membrane components in sestonic detritus may result from the differential lability of proteins in cytoplasm versus membrane components of cells.

Continued fractions built from convex sets and convex functions

In a partially ordered semigroup with the duality (or polarity) transform, it is pos- sible to define a generalisation of continued fractions. General sufficient conditions for convergence of continued fractions are provided. Two particular applications concern the cases of convex sets with the Minkowski addition and the polarity transform and the family of non-negative convex functions with the Legendre–Fenchel and Artstein-Avidan–Milman transforms.