669 research outputs found

    Observations of Global and Local Infall in NGC 1333

    Full text link
    We report ``infall asymmetry'' in the HCO+^+ (1--0) and (3--2) lines toward NGC 1333, extended over ∌0.39pc2\sim 0.39 {\rm pc}^2, a larger extent than has been reported be fore, for any star-forming region. The infall asymmetry extends over a major portion of the star-forming complex, and is not limited to a single protostar, or to a single dense core, or to a single spectral line. It seems likely that the infall asymmetry represents inward motions, and that these motions are physically associated with the complex. Both blue-asymmetric and red-asymmetric lines are seen, but in both the (3--2) and (1--0) lines of HCO+^+ the vast majority of the asymmetric lines are blue, indicating inward motions. The (3--2) line, tracing denser gas, has the spectra with the strongest asymmetry and these spectra are associated with the protostars IRAS 4A and 4B, which most likely indicates a warm central source is affecting the line profiles. The (3--2) and (1--0) lines usually have the same sense of asymmetry in common positions, but their profiles differ significantly, and the (1--0) line appears to trace motions on much larger spatial scales than does the (3--2) line. Line profile models fit the spectra well, but do not strongly constrain their parameters. The mass accretion rate of the inward motions is of order 10−4^{-4} M⊙_\odot/yr, similar to the ratio of stellar mass to cluster age.Comment: 28 pages, 11 figures, 1 colour figur

    An S-shaped outflow from IRAS 03256+3055 in NGC 1333

    Full text link
    The IRAS source 03256+3055 in the NGC 1333 star forming region is associated with extended sub-millimeter emission of complex morphology, showing multiple clumps. One of these is found to coincide with the driving source of a bipolar jet of S-shaped morphology seen in the emission lines of H_alpha and [SII] as well as in the H2 emission lines in the K-band. Detailed images of the driving source at the wavelengths of H_alpha and [SII] and in the I, J, H, and K bands as well as a K-band spectrum and polarimetry are discussed. The near-infrared morphology is characterized by a combination of line emission from the jet and scattered light from a source with a steep continuum spectrum. The morphology and proper motion of the jet are discussed in the context of a binary system with a precessing disk. We conclude that the molecular core associated with IRAS 03256+3055 consists of several clumps, only one of which shows evidence of recent star formation at optical and near-infrared wavelengths.We also briefly discuss a second, newly found near-infrared source associated with a compact sub-millimeter continuum source near IRAS 03256+3055, and conclude that this source may be physically unrelated the cluster of molecular clumps.Comment: 25 pages, including 5 figures. Accepted for publication in The Astronomical Journa

    Opening up the Quantum Three-Box Problem with Undetectable Measurements

    Get PDF
    One of the most striking features of quantum mechanics is the profound effect exerted by measurements alone. Sophisticated quantum control is now available in several experimental systems, exposing discrepancies between quantum and classical mechanics whenever measurement induces disturbance of the interrogated system. In practice, such discrepancies may frequently be explained as the back-action required by quantum mechanics adding quantum noise to a classical signal. Here we implement the 'three-box' quantum game of Aharonov and Vaidman in which quantum measurements add no detectable noise to a classical signal, by utilising state-of-the-art control and measurement of the nitrogen vacancy centre in diamond. Quantum and classical mechanics then make contradictory predictions for the same experimental procedure, however classical observers cannot invoke measurement-induced disturbance to explain this discrepancy. We quantify the residual disturbance of our measurements and obtain data that rule out any classical model by > 7.8 standard deviations, allowing us for the first time to exclude the property of macroscopic state-definiteness from our system. Our experiment is then equivalent to a Kochen-Spekker test of quantum non-contextuality that successfully addresses the measurement detectability loophole

    Using radium isotopes to characterize water ages and coastal mixing rates: A sensitivity analysis

    Get PDF
    ISI Document Delivery No.: 893TE Times Cited: 4 Cited Reference Count: 78 Cited References: Abraham DM, 2003, BIOL BULL-US, V205, P246, DOI 10.2307/1543277 Arega F, 2008, J HYDRO-ENVIRON RES, V2, P99, DOI 10.1016/j.jher.2008.07.003 Basu AR, 2001, SCIENCE, V293, P1470, DOI 10.1126/science.1060524 Beck AJ, 2007, MAR CHEM, V106, P419, DOI 10.1016/j.marchem.2007.03.008 Boehm AB, 2006, CONT SHELF RES, V26, P269, DOI 10.1016/j.csr.2005.11.008 Boehm AB, 2004, ENVIRON SCI TECHNOL, V38, P3558, DOI 10.1021/es035385a Breier JA, 2009, LIMNOL OCEANOGR, V54, P1964, DOI 10.4319/lo.2009.54.6.1964 Brooks DA, 1999, ESTUAR COAST SHELF S, V49, P647, DOI 10.1006/ecss.1999.0544 Burnett WC, 2008, ESTUAR COAST SHELF S, V76, P501, DOI 10.1016/j.ecss.2007.07.027 Burnett WC, 2006, SCI TOTAL ENVIRON, V367, P498, DOI 10.1016/j.scitotenv.2006.05.009 Charette MA, 2007, LIMNOL OCEANOGR, V52, P230 Charette MA, 2007, DEEP-SEA RES PT II, V54, P1989, DOI 10.1016/j.dsr2.2007.06.003 Charette MA, 2003, MAR CHEM, V84, P113, DOI 10.1016/j.marchem.2003.07.001 Charette MA, 2001, LIMNOL OCEANOGR, V46, P465 Colbert SL, 2007, CONT SHELF RES, V27, P1477, DOI 10.1016/j.csr.2007.01.003 Crotwell AM, 2003, AQUAT GEOCHEM, V9, P191, DOI 10.1023/B:AQUA.0000022954.89019.c9 de Sieyes NR, 2008, LIMNOL OCEANOGR, V53, P1434, DOI 10.4319/lo.2008.53.4.1434 Dulaiova H, 2008, MAR CHEM, V109, P395, DOI 10.1016/j.marchem.2007.09.001 Dulaiova H, 2006, CONT SHELF RES, V26, P1971, DOI 10.1016/j.csr.2006.07.011 GALLAGHER B, 1980, PAC SCI, V34, P301 Garcia-Orellana J, 2010, J ENVIRON RADIOACTIV, V101, P582, DOI 10.1016/j.jenvrad.2009.12.005 Garcia-Solsona E, 2008, MAR CHEM, V109, P292, DOI 10.1016/j.marchem.2008.02.007 Garcia-Solsona E, 2010, BIOGEOSCIENCES, V7, P2625, DOI 10.5194/bg-7-2625-2010 Garcia-Solsona E, 2008, MAR CHEM, V109, P198, DOI 10.1016/j.marchem.2007.11.006 Garcia-Solsona E, 2010, BIOGEOCHEMISTRY, V97, P211, DOI 10.1007/s10533-009-9368-y Godoy JM, 2006, J BRAZIL CHEM SOC, V17, P730, DOI 10.1590/S0103-50532006000400014 Gomes F. C., 2009, RADIOPROTECTION, V44, P237, DOI [10.1051/radiopro/20095047, DOI 10.1051/RADIOPRO/20095047] Gonneea ME, 2008, MAR CHEM, V109, P250, DOI 10.1016/j.marchem.2007.12.002 Hancock GJ, 1996, EARTH PLANET SC LETT, V138, P145, DOI 10.1016/0012-821X(95)00218-2 Hougham AL, 2007, MAR CHEM, V105, P194, DOI 10.1016/j.marchem.2007.01.013 Hwang DW, 2005, MAR CHEM, V96, P61, DOI 10.1016/j.marchem.2004.11.002 Kim G, 2008, MAR CHEM, V109, P307, DOI 10.1016/j.marchem.2007.07.002 Kim G, 2005, EARTH PLANET SC LETT, V237, P156, DOI 10.1016/j.epsl.2005.06.011 Knee KL, 2008, ESTUAR COAST, V31, P607, DOI 10.1007/s12237-008-9055-6 Knee KL, 2010, LIMNOL OCEANOGR, V55, P1105, DOI 10.4319/lo.2010.55.3.1105 Krest JM, 2000, GLOBAL BIOGEOCHEM CY, V14, P167, DOI 10.1029/1999GB001197 LEE DR, 1977, LIMNOL OCEANOGR, V22, P140 Lee YW, 2009, SCI TOTAL ENVIRON, V407, P3181, DOI 10.1016/j.scitotenv.2008.04.013 Li CY, 2011, J MARINE SYST, V86, P28, DOI 10.1016/j.jmarsys.2011.01.003 LI YH, 1979, EARTH PLANET SC LETT, V43, P343, DOI 10.1016/0012-821X(79)90089-X LONGUETHIGGINS MS, 1983, P ROY SOC LOND A MAT, V390, P283, DOI 10.1098/rspa.1983.0132 Loveless AM, 2008, J HYDROL, V351, P203, DOI 10.1016/j.jhydrol.2007.12.010 Monsen NE, 2002, LIMNOL OCEANOGR, V47, P1545 Montlucon D, 2001, ENVIRON SCI TECHNOL, V35, P480, DOI 10.1021/es9914442 Moore W. S., 2000, J GEOPHYS RES, V105, P117, DOI DOI 10.1029/1999JC000289 Moore WS, 2006, CONT SHELF RES, V26, P852, DOI 10.1016/j.csr.2005.12.004 Moore WS, 2008, ESTUAR COAST SHELF S, V76, P512, DOI 10.1016/j.ecss.2007.07.042 Moore WS, 2006, J GEOPHYS RES-OCEANS, V111, DOI 10.1029/2005JC003041 Moore WS, 2000, CONT SHELF RES, V20, P1993, DOI 10.1016/S0278-4343(00)00054-6 Moore WS, 1997, EARTH PLANET SC LETT, V150, P141, DOI 10.1016/S0012-821X(97)00083-6 MOORE WS, 1984, NUCL INSTRUM METH A, V223, P407, DOI 10.1016/0167-5087(84)90683-5 OKUBO A, 1976, DEEP-SEA RES, V23, P1213, DOI 10.1016/0011-7471(76)90897-4 OKUBO A, 1971, DEEP-SEA RES, V18, P789, DOI 10.1016/0011-7471(71)90046-5 Paytan A, 2006, LIMNOL OCEANOGR, V51, P343 Peterson RN, 2009, LIMNOL OCEANOGR, V54, P890, DOI 10.4319/lo.2009.54.3.0890 Peterson RN, 2008, CONT SHELF RES, V28, P2700, DOI 10.1016/j.csr.2008.09.002 Portnoy JW, 1998, WATER RESOUR RES, V34, P3095, DOI 10.1029/98WR02167 Rama, 1996, GEOCHIM COSMOCHIM AC, V60, P4645 Rapaglia J, 2010, J ENVIRON RADIOACTIV, V101, P571, DOI 10.1016/j.jenvrad.2009.08.010 Rasmussen L. L., 2003, THESIS MIT Robinson C, 2007, ADV WATER RESOUR, V30, P851, DOI 10.1016/j.advwatres.2006.07.006 Santos IR, 2008, J HYDROL, V353, P275, DOI 10.1016/j.jhydrol.2008.02.010 Scopel CO, 2006, J GREAT LAKES RES, V32, P543, DOI 10.3394/0380-1330(2006)32[543:IONWDA]2.0.CO;2 SHAW RD, 1989, LIMNOL OCEANOGR, V34, P1343 Shellenbarger GG, 2006, LIMNOL OCEANOGR, V51, P1876 Slomp CP, 2004, J HYDROL, V295, P64, DOI 10.1016/j.jhydrol.2004.02.018 Standley LJ, 2008, ENVIRON TOXICOL CHEM, V27, P2457, DOI 10.1897/07-604.1 STOMMEL H, 1949, J MAR RES, V8, P199 Street JH, 2008, MAR CHEM, V109, P355, DOI 10.1016/j.marchem.2007.08.009 Swarzenski PW, 2009, ESTUAR COAST SHELF S, V83, P77, DOI 10.1016/j.ecss.2009.03.027 Swarzenski PW, 2007, MAR CHEM, V104, P69, DOI 10.1016/j.marchem.2006.08.001 Swarzenski PW, 2006, MAR CHEM, V101, P248, DOI 10.1016/j.marchem.2006.03.007 Swearman J. W., 2006, PAPERS SUMMER UNDERG, P51 Taniguchi M, 2003, BIOGEOCHEMISTRY, V66, P35, DOI 10.1023/B:BIOG.0000006090.25949.8d Taylor J. R., 1997, INTRO ERROR ANAL, P160 Turner IL, 1997, J COASTAL RES, V13, P46 Weinstein Y., 2006, RADIOACT ENV, V8, P360, DOI DOI 10.1016/S1569-4860(05)08029-0 Windom HL, 2006, MAR CHEM, V102, P252, DOI 10.1016/j.marchem.2006.06.016 Knee, Karen L. Garcia-Solsona, Ester Garcia-Orellana, Jordi Boehm, Alexandria B. Paytan, Adina 4 AMER SOC LIMNOLOGY OCEANOGRAPHY WACO LIMNOL OCEANOGR-METHNumerous studies have used naturally occurring Ra isotopes (Ra-223, Ra-224, Ra-226, and Ra-228, with half-lives of 11.4 d, 3.7 d, 1600 y, and 5.8 y, respectively) to quantify water mass ages, coastal ocean mixing rates, and submarine groundwater discharge (SGD). Using Monte Carlo models, this study investigated how uncertainties in Ra isotope activities and the derived activity ratios (AR) arising from analytical uncertainty and natural variability affect the uncertainty associated with Ra-derived water ages and eddy diffusion coefficients, both of which can be used to calculate SGD. Analytical uncertainties associated with Ra-224, Ra-226, and Ra-228 activities were reported in most published studies to be less than 10% of sample activity; those reported for Ra-223 ranged from 7% to 40%. Relative uncertainty related to natural variability-estimated from the variability in Ra-223 and Ra-224 activities of replicate field samples-ranged from 15% to 50% and was similar for Ra-223 activity, Ra-224 activity, and the Ra-224/Ra-223 AR. Our analysis revealed that AR-based water ages shorter than 3-5 d often have relative uncertainties greater than 100%, potentially limiting their utility. Uncertainties in eddy diffusion coefficients estimated based on cross-shore gradients in short-lived Ra isotope activity were greater when fewer points were used to determine the linear trend, when the coefficient of determination (R-2) was low, and when Ra-224, rather than Ra-223, was used. By exploring the uncertainties associated with Ra-derived water ages and eddy diffusion coefficients, this study will enable researchers to apply these methods more effectively and to reduce uncertainty

    Picosecond mass spectrometry of a collisionless photodissociation reaction

    Get PDF
    We wish to report on the direct observation (in real time) of a photodissociation reaction under collisionless conditions. This is achieved by the technique of picosecond mass spectrometry in skimmed molecular beams

    Spitzer Observations of NGC 1333: A Study of Structure and Evolution in a Nearby Embedded Cluster

    Full text link
    We present a comprehensive analysis of structure in the young, embedded cluster, NGC 1333 using members identified with Spitzer and 2MASS photometry based on their IR-excess emission. In total, 137 members are identified in this way, composed of 39 protostars and 98 more evolved pre-main sequence stars with disks. Of the latter class, four are transition/debris disk candidates. The fraction of exposed pre-main sequence stars with disks is 83% +/- 11%, showing that there is a measurable diskless pre-main sequence population. The sources in each of the Class I and Class II evolutionary states are shown to have very different spatial distributions relative to the distribution of the dense gas in their natal cloud. However, the distribution of nearest neighbor spacings among these two groups of sources are found to be quite similar, with a strong peak at spacings of 0.045 pc. Radial and azimuthal density profiles and surface density maps computed from the identified YSOs show that NGC 1333 is elongated and not strongly centrally concentrated, confirming previous claims in the literature. We interpret these new results as signs of a low velocity dispersion, extremely young cluster that is not in virial equilibrium.Comment: 59 pages, 20 figures, accepted to ApJ, verion with full resolution figures available at http://www.cfa.harvard.edu/~rgutermuth/preprints/gutermuth_ngc1333.pdf . Updated to fix astro-ph figure garblin

    Infall, Outflow, Rotation, and Turbulent Motions of Dense Gas within NGC 1333 IRAS 4

    Full text link
    Millimeter wavelength observations are presented of NGC 1333 IRAS 4, a group of highly-embedded young stellar objects in Perseus, that reveal motions of infall, outflow, rotation, and turbulence in the dense gas around its two brightest continuum objects, 4A and 4B. These data have finest angular resolution of approximately 2" (0.0034 pc) and finest velocity resolution of 0.13 km/s. Infall motions are seen from inverse P-Cygni profiles observed in H2CO 3_12-2_11 toward both objects, but also in CS 3-2 and N2H+ 1-0 toward 4A, providing the least ambiguous evidence for such motions toward low-mass protostellar objects. Outflow motions are probed by bright line wings of H2CO 3_12-2_11 and CS 3-2 observed at positions offset from 4A and 4B, likely tracing dense cavity walls. Rotational motions of dense gas are traced by a systematic variation of the N2H+ line velocities, and such variations are found around 4A but not around 4B. Turbulent motions appear reduced with scale, given N2H+ line widths around both 4A and 4B that are narrower by factors of 2 or 3 than those seen from single-dish observations. Minimum observed line widths of approximately 0.2 km/s provide a new low, upper bound to the velocity dispersion of the parent core to IRAS 4, and demonstrate that turbulence within regions of clustered star formation can be reduced significantly. A third continuum object in the region, 4B', shows no detectable line emission in any of the observed molecular species.Comment: LateX, 51 pages, 9 figures, accepted by Ap

    Turbulence driven by outflow-blown cavities in the molecular cloud of NGC 1333

    Full text link
    Outflows from young stellar objects have been identified as a possible source of turbulence in molecular clouds. To investigate the relationship between outflows, cloud dynamics and turbulence, we compare the kinematics of the molecular gas associated with NGC 1333, traced in 13CO(1-0), with the distribution of young stellar objects (YSOs) within. We find a velocity dispersion of ~ 1-1.6 km/s in 13CO that does not significantly vary across the cloud, and is uncorrelated with the number of nearby young stellar outflows identified from optical and submillimeter observations. However, from velocity channel maps we identify about 20 cavities or depressions in the 13CO intensity of scales > 0.1-0.2 pc and velocity widths 1-3 km/s. The cavities exhibit limb brightened rims in both individual velocity channel maps and position velocity diagrams, suggesting that they are slowly expanding. We interpret these cavities to be remnants of past YSO outflow activity: If these cavities are presently empty, they would fill in on time scales of a million years. This can exceed the lifetime of a YSO outflow phase, or the transit time of the central star through the cavity, explaining the the absence of any clear correlation between the cavities and YSO outflows. We find that the momentum and energy deposition associated with the expansion of the cavities is sufficient to power the turbulence in the cloud. In this way we conclude that the cavities are an important intermediary step between the conversion of YSO outflow energy and momentum into cloud turbulent motions.Comment: Accepted for publication in ApJ. Check out http://astro.pas.rochester.edu/~aquillen/coolpics.html for channel map and PosVel movies of N133
    • 

    corecore