Analysis of rocket engine injection combustion processes

Mixing methodology improvement for the JANNAF DER and CICM injection/combustion analysis computer programs was accomplished. ZOM plane prediction model development was improved for installation into the new standardized DER computer program. An intra-element mixing model developing approach was recommended for gas/liquid coaxial injection elements for possible future incorporation into the CICM computer program

Mechanisms regulating IgA class-specific immunoglobulin production in murine gut-associated lymphoid tissues. I. T cells derived from Peyer's patches that switch sIgM B Cells to sIgA B cells in vitro

To explore mechanisms of T cell regulation governing mucosal IgA immune response, concanavalin A-induced cloned T cell lines from Peyer's patches (PP) as well as spleen were established. The cloned cell lines expressed Thy- 1.2(+), Lyt-l(+)2(-) and were radioresistant (1,500 rad). The capacity of the cloned T cells to regulate Ig synthesis was determined by measuring their effect on lipopolysaccharide (LPS)-induced polyclonal Ig synthesis by PP B cells. In initial studies Ig secreted by B cells was determined by double antibody radioimmunoassay. LPS in the absence of cloned T cells induced abundant amounts of IgM (average 8,860 ng/2 × 10(5) B cells) and IgG (average 1,190 ng/2 × 10(5) B cells), but little or no IgA. The addition of PP cloned T cells markedly suppressed production of IgM (88 percent at the highest T/B cell ratio, 4:1), but the addition of spleen cloned T cells suppressed only a little or not at all. IgG production was inhibited by both PP and spleen T clone cells (70 percent at the 4:1 T/B ratio), wheras IgA synthesis was enhanced by both clones, but only to a limited degree. In subsequent studies the expression of class-specific surface Ig (sIg) and cytoplasmic Ig (cIg) on/in unseparated PP B cells as well as Ig class- specific PP B cells and spleen B cells during culture with or without the cloned T cells was determined by immunofluorescence. The major findings were as follows: (a) Compared with unseparated B cell cultures and cultures of purified sIgM B cells derived from PP containing LPS alone, cultures containing LPS and PP cloned T cells showed a marked decrease in cIgM-, sIgG-, and cIgG-expressing cells that was accompanied by a striking increase in sIgA-bearing, but not cIgA-containing, cells. In contrast, unseparated B cell cultures and cultures of purified sIgM B cells derived from PP containing LPS and spleen cloned T cells did not show any increase in sIgA- bearing cells. (b) Compared with purified sIgG-bearing PP B cell cultures containing LPS alone, purified sIgG-bearing PP B cell cultures containing both LPS and PP cloned T cells showed no substantial change in sIgG- or cIgG- expressing cells, and no sIgA- or cIgA- expressing cells appeared. (c) Compared with sIgA-bearing PP B cell cultures containing LPS alone, purified sIgA-bearing PP B cell cultures containing both LPS and PP cloned T cells showed no increased proliferation, and cIgA cells did not occur. Cultures of purified sIgM B cells derived from spleen containing LPS and PP cloned T cells showed qualitatively similar changes. From these results we conclude that PP cloned T cells induced class-specific switching from sIgM- to sIgA- bearing B cells, whereas spleen cloned T cells lacked this property, although they may have induced an IgM {arrow} IgG or intersubclass IgG switch. These processes seem to be in part tissue dependent. Furthermore, the PP switch T cells appear to operate as true switch cells, which govern the pathway of DNA recombination events, rather than as classical helper cells, which act to expand already differentiated cells. Finally, these switch T cells probably account for the fact that PP are an important source of IgA B cells and also a major site of IgA heavy chain class switching during gut-associated mucosal B cell proliferation and differentation

A chemical ionization mass spectrometer for continuous underway shipboard analysis of dimethylsulfide in near-surface seawater

A compact, low-cost atmospheric pressure, chemical ionization mass spectrometer ("mini-CIMS") has been developed for continuous underway shipboard measurements of dimethylsulfide (DMS) in seawater. The instrument was used to analyze DMS in air equilibrated with flowing seawater across a porous Teflon membrane equilibrator. The equilibrated gas stream was diluted with air containing an isotopically-labeled internal standard. DMS is ionized at atmospheric pressure via proton transfer from water vapor, then declustered, mass filtered via quadrupole mass spectrometry, and detected with an electron multiplier. The instrument described here is based on a low-cost residual gas analyzer (Stanford Research Systems), which has been modified for use as a chemical ionization mass spectrometer. The mini-CIMS has a gas phase detection limit of 220 ppt DMS for a 1 min averaging time, which is roughly equivalent to a seawater DMS concentration of 0.1 nM DMS at 20°C. The mini-CIMS has the sensitivity, selectivity, and time response required for underway measurements of surface ocean DMS over the full range of oceanographic conditions. The simple, robust design and relatively low cost of the instrument are intended to facilitate use in process studies and surveys, with potential for long-term deployment on research vessels, ships of opportunity, and large buoys

Air/Sea Transfer of Highly Soluble Gases Over Coastal Waters

The deposition of soluble trace gases to the sea surface is not well studied due to a lack of flux measurements over the ocean. Here we report simultaneous air/sea eddy covariance flux measurements of water vapor, sulfur dioxide (SO2), and momentum from a coastal North Atlantic pier. Gas transfer velocities were on average about 20% lower for SO2 than for H2O. This difference is attributed to the difference in molecular diffusivity between the two molecules (DSO2/DH2O = 0.5), in reasonable agreement with bulk parameterizations in air/sea gas models. This study demonstrates that it is possible to observe the effect of molecular diffusivity on air-side resistance to gas transfer. The slope of observed relationship between gas transfer velocity and friction velocity is slightly smaller than predicted by gas transfer models, possibly due to wind/wave interactions that are unaccounted for in current models

Aerosol chemical composition and distribution during the Pacific Exploratory Mission (PEM) Tropics

Distributions of aerosol-associated soluble ions over much of the South Pacific were determined by sampling from the NASA DC-8 as part of the Pacific Exploratory Mission (PEM) Tropics campaign. The mixing ratios of all ionic species were surprisingly low throughout the free troposphere (2-12 km), despite the pervasive influence from biomass burning plumes advecting over the South Pacific from the west during PEM-Tropics. At the same time, the specific activity of 7Be frequently exceeded 1000 fCi m-3 through much of the depth of the troposphere. These distributions indicate that the plumes must have been efficiently scavenged by precipitation (removing the soluble ions), but that the scavenging must have occurred far upwind of the DC-8 sampling regions (otherwise 7Be activities would also have been low). This inference is supported by large enhancements of HNO3 and carboxylic acids in many of the plumes, as these soluble acidic gases would also be readily scavenged in any precipitation events. Decreasing mixing ratios of NH4 + with altitude in all South Pacific regions sampled provide support for recent suggestions that oceanic emissions of NH3 constitute a significant source far from continents. Our sampling below 2 km reaffirms the latitudinal pattern in the methylsulfonate/non-sea-salt sulfate (MSA/nss SO4 =) molar ratio established through surface-based and shipboard sampling, with values increasing from \u3c0.05 in the tropics to nearly 0.6 at 70°S. However, we also found very high values of this ratio (0.2-0.5) at 10 km altitude above the intertropical convergence zone near 10°N. It appears that wet convective pumping of dimethylsulfide from the tropical marine boundary layer is responsible for the high values of the MSA/nss SO4 = ratio in the tropical upper troposphere. This finding complicates use of this ratio to infer the zonal origin of biogenic S transported long distances. Copyright 1999 by the American Geophysical Union

In-flight lift-drag characteristics for a forward-swept wing aircraft and comparisons with contemporary aircraft)

Lift (L) and drag (D) characteristics have been obtained in flight for the X-29A airplane (a forward swept-wing demonstrator) for Mach numbers (M) from 0.4 to 1.3. Most of the data were obtained near an altitude of 30,000 ft. A representative Reynolds number for M = 0.9, and a pressure altitude of 30,000 ft, is 18.6 x 10(exp 6) based on the mean aerodynamic chord. The X-29A data (forward-swept wing) are compared with three high-performance fighter aircraft: the F-15C, F-16C, and F/A18. The lifting efficiency of the X-29A, as defined by the Oswald lifting efficiency factor, e, is about average for a cantilevered monoplane for M = 0.6 and angles of attack up to those required for maximum L/D. At M = 0.6 the level of L/D and e, as a function of load factor, for the X-29A was about the same as for the contemporary aircraft. The X-29A and its contemporaries have high transonic wave drag and equivalent parasite area compared with aircraft of the 1940's through 1960's