85 research outputs found

    What\u27s In A Label? The Effects of Substance Types and Labels on Treatment Considerations and Stigma

    Get PDF
    Visitors (N = 579) to a science center read selected scenarios and evaluated the most likely outcome for a hypothetical substance abuser. Respondents were randomly assigned to one of six scenario conditions: a person with one of three different substance abuse problems (alcohol, tobacco, or cocaine) was crossed with two labels reflecting high or low substance dependence. Results indicated that: (1) cigarettes were viewed as a less serious substance abuse problem than were alcohol or cocaine (a person who smoked cigarettes was rated as more likely to recover from his problem, self-change was regarded as more appropriate and less stigma was associated with smoking than with the other two drugs); (2) non-abstinent recoveries of all types were greeted with skepticism; and (3) recovery was rated as more likely to occur from treatment than from self-change

    The Death Throes of a Stripped Massive Star: An Eruptive Mass-Loss History Encoded in Pre-Explosion Emission, a Rapidly Rising Luminous Transient, and a Broad-Lined Ic Supernova SN2018gep

    Get PDF
    We present detailed observations of ZTF18abukavn (SN2018gep), discovered in high-cadence data from the Zwicky Transient Facility as a rapidly rising (1.3 mag/hr) and luminous (M_(g,peak) = −20 mag) transient. It is spectroscopically classified as a broad-lined stripped-envelope supernova (Ic-BL SN). The rapid rise to peak bolometric luminosity and blue colors at peak (t_(rise)∌0.5-3 days, L_(bol)≳3×10^(44) erg sec^(−1), g−r = −0.3) resemble the high-redshift Ic-BL iPTF16asu, as well as several other unclassified fast transients. The early discovery of SN2018gep (within an hour of shock breakout) enabled an intensive spectroscopic campaign, including the highest-temperature (T_(eff) ≳ 40,000K) spectra of a stripped-envelope SN. A retrospective search revealed luminous (M_g ∌ M_r ≈ −14mag) emission in the days to weeks before explosion, the first definitive detection of precursor emission for a Ic-BL. We find a limit on the isotropic gamma-ray energy release E_(Îł,iso) < 4.9×10^(48) erg, a limit on X-ray emission L_X < 10^(40) erg sec^(−1), and a limit on radio emission ÎœL_Îœ â‰Č 10^(37) erg sec^(−1). Taken together, we find that the data are best explained by shock breakout in a massive shell of dense circumstellar material (0.02 M⊙) at large radii (3×10^(14)cm) that was ejected in eruptive pre-explosion mass-loss episodes

    Antimicrobial resistance among migrants in Europe: a systematic review and meta-analysis

    Get PDF
    BACKGROUND: Rates of antimicrobial resistance (AMR) are rising globally and there is concern that increased migration is contributing to the burden of antibiotic resistance in Europe. However, the effect of migration on the burden of AMR in Europe has not yet been comprehensively examined. Therefore, we did a systematic review and meta-analysis to identify and synthesise data for AMR carriage or infection in migrants to Europe to examine differences in patterns of AMR across migrant groups and in different settings. METHODS: For this systematic review and meta-analysis, we searched MEDLINE, Embase, PubMed, and Scopus with no language restrictions from Jan 1, 2000, to Jan 18, 2017, for primary data from observational studies reporting antibacterial resistance in common bacterial pathogens among migrants to 21 European Union-15 and European Economic Area countries. To be eligible for inclusion, studies had to report data on carriage or infection with laboratory-confirmed antibiotic-resistant organisms in migrant populations. We extracted data from eligible studies and assessed quality using piloted, standardised forms. We did not examine drug resistance in tuberculosis and excluded articles solely reporting on this parameter. We also excluded articles in which migrant status was determined by ethnicity, country of birth of participants' parents, or was not defined, and articles in which data were not disaggregated by migrant status. Outcomes were carriage of or infection with antibiotic-resistant organisms. We used random-effects models to calculate the pooled prevalence of each outcome. The study protocol is registered with PROSPERO, number CRD42016043681. FINDINGS: We identified 2274 articles, of which 23 observational studies reporting on antibiotic resistance in 2319 migrants were included. The pooled prevalence of any AMR carriage or AMR infection in migrants was 25·4% (95% CI 19·1-31·8; I2 =98%), including meticillin-resistant Staphylococcus aureus (7·8%, 4·8-10·7; I2 =92%) and antibiotic-resistant Gram-negative bacteria (27·2%, 17·6-36·8; I2 =94%). The pooled prevalence of any AMR carriage or infection was higher in refugees and asylum seekers (33·0%, 18·3-47·6; I2 =98%) than in other migrant groups (6·6%, 1·8-11·3; I2 =92%). The pooled prevalence of antibiotic-resistant organisms was slightly higher in high-migrant community settings (33·1%, 11·1-55·1; I2 =96%) than in migrants in hospitals (24·3%, 16·1-32·6; I2 =98%). We did not find evidence of high rates of transmission of AMR from migrant to host populations. INTERPRETATION: Migrants are exposed to conditions favouring the emergence of drug resistance during transit and in host countries in Europe. Increased antibiotic resistance among refugees and asylum seekers and in high-migrant community settings (such as refugee camps and detention facilities) highlights the need for improved living conditions, access to health care, and initiatives to facilitate detection of and appropriate high-quality treatment for antibiotic-resistant infections during transit and in host countries. Protocols for the prevention and control of infection and for antibiotic surveillance need to be integrated in all aspects of health care, which should be accessible for all migrant groups, and should target determinants of AMR before, during, and after migration. FUNDING: UK National Institute for Health Research Imperial Biomedical Research Centre, Imperial College Healthcare Charity, the Wellcome Trust, and UK National Institute for Health Research Health Protection Research Unit in Healthcare-associated Infections and Antimictobial Resistance at Imperial College London

    Comparative genomics reveals diversity among xanthomonads infecting tomato and pepper

    Get PDF
    <p>Abstract</p> <p>Background</p> <p>Bacterial spot of tomato and pepper is caused by four <it>Xanthomonas </it>species and is a major plant disease in warm humid climates. The four species are distinct from each other based on physiological and molecular characteristics. The genome sequence of strain 85-10, a member of one of the species, <it>Xanthomonas euvesicatoria </it>(<it>Xcv</it>) has been previously reported. To determine the relationship of the four species at the genome level and to investigate the molecular basis of their virulence and differing host ranges, draft genomic sequences of members of the other three species were determined and compared to strain 85-10.</p> <p>Results</p> <p>We sequenced the genomes of <it>X. vesicatoria </it>(<it>Xv</it>) strain 1111 (ATCC 35937), <it>X. perforans </it>(<it>Xp</it>) strain 91-118 and <it>X. gardneri </it>(<it>Xg</it>) strain 101 (ATCC 19865). The genomes were compared with each other and with the previously sequenced <it>Xcv </it>strain 85-10. In addition, the molecular features were predicted that may be required for pathogenicity including the type III secretion apparatus, type III effectors, other secretion systems, quorum sensing systems, adhesins, extracellular polysaccharide, and lipopolysaccharide determinants. Several novel type III effectors from <it>Xg </it>strain 101 and <it>Xv </it>strain 1111 genomes were computationally identified and their translocation was validated using a reporter gene assay. A homolog to Ax21, the elicitor of XA21-mediated resistance in rice, and a functional Ax21 sulfation system were identified in <it>Xcv</it>. Genes encoding proteins with functions mediated by type II and type IV secretion systems have also been compared, including enzymes involved in cell wall deconstruction, as contributors to pathogenicity.</p> <p>Conclusions</p> <p>Comparative genomic analyses revealed considerable diversity among bacterial spot pathogens, providing new insights into differences and similarities that may explain the diverse nature of these strains. Genes specific to pepper pathogens, such as the O-antigen of the lipopolysaccharide cluster, and genes unique to individual strains, such as novel type III effectors and bacteriocin genes, have been identified providing new clues for our understanding of pathogen virulence, aggressiveness, and host preference. These analyses will aid in efforts towards breeding for broad and durable resistance in economically important tomato and pepper cultivars.</p

    Rural Australian community pharmacists' views on complementary and alternative medicine: a pilot study

    Get PDF
    <p>Abstract</p> <p>Background</p> <p>Complementary and alternative medicines (CAMs) are being used increasingly across the world. In Australia, community pharmacists are a major supplier of these products but knowledge of the products and interactions with other medicines is poor. Information regarding the use of CAMs by metropolitan pharmacists has been documented by the National Prescribing Service (NPS) in Australia but the views of rural/regional community pharmacists have not been explored. The aim of this pilot study was to explore the knowledge, attitudes and information seeking of a cohort of rural community pharmacists towards CAMs and to compare the findings to the larger NPS study.</p> <p>Methods</p> <p>A cross sectional self-administered postal questionnaire was mailed to all community pharmacists in one rural/regional area of Australia. Using a range of scales, data was collected regarding attitudes, knowledge, information seeking behaviour and demographics.</p> <p>Results</p> <p>Eighty eligible questionnaires were returned. Most pharmacists reported knowing that they should regularly ask consumers if they are using CAMs but many lacked the confidence to do so. Pharmacists surveyed for this study were more knowledgeable in regards to side effects and interactions of CAMs than those in the NPS survey. Over three quarters of pharmacists surveyed reported sourcing CAM information at least several times a month. The most frequently sought information was drug interactions, dose, contraindications and adverse effects. A variety of resources were used to source information, the most popular source was the internet but the most useful resource was CAM text books.</p> <p>Conclusions</p> <p>Pharmacists have varied opinions on the use of CAMs and many lack awareness of or access to good quality CAMs information. Therefore, there is a need to provide pharmacists with opportunities for further education. The data is valuable in assisting interested stakeholders with the development of initiatives to address the gaps in attitudes, knowledge and to improve effectiveness of information seeking behaviour.</p

    Remdesivir and three other drugs for hospitalised patients with COVID-19: final results of the WHO Solidarity randomised trial and updated meta-analyses.

    Get PDF
    BACKGROUND World Health Organization expert groups recommended mortality trials of four repurposed antiviral drugs - remdesivir, hydroxychloroquine, lopinavir, and interferon beta-1a - in patients hospitalized with coronavirus disease 2019 (Covid-19). METHODS We randomly assigned inpatients with Covid-19 equally between one of the trial drug regimens that was locally available and open control (up to five options, four active and the local standard of care). The intention-to-treat primary analyses examined in-hospital mortality in the four pairwise comparisons of each trial drug and its control (drug available but patient assigned to the same care without that drug). Rate ratios for death were calculated with stratification according to age and status regarding mechanical ventilation at trial entry. RESULTS At 405 hospitals in 30 countries, 11,330 adults underwent randomization; 2750 were assigned to receive remdesivir, 954 to hydroxychloroquine, 1411 to lopinavir (without interferon), 2063 to interferon (including 651 to interferon plus lopinavir), and 4088 to no trial drug. Adherence was 94 to 96% midway through treatment, with 2 to 6% crossover. In total, 1253 deaths were reported (median day of death, day 8; interquartile range, 4 to 14). The Kaplan-Meier 28-day mortality was 11.8% (39.0% if the patient was already receiving ventilation at randomization and 9.5% otherwise). Death occurred in 301 of 2743 patients receiving remdesivir and in 303 of 2708 receiving its control (rate ratio, 0.95; 95% confidence interval [CI], 0.81 to 1.11; P = 0.50), in 104 of 947 patients receiving hydroxychloroquine and in 84 of 906 receiving its control (rate ratio, 1.19; 95% CI, 0.89 to 1.59; P = 0.23), in 148 of 1399 patients receiving lopinavir and in 146 of 1372 receiving its control (rate ratio, 1.00; 95% CI, 0.79 to 1.25; P = 0.97), and in 243 of 2050 patients receiving interferon and in 216 of 2050 receiving its control (rate ratio, 1.16; 95% CI, 0.96 to 1.39; P = 0.11). No drug definitely reduced mortality, overall or in any subgroup, or reduced initiation of ventilation or hospitalization duration. CONCLUSIONS These remdesivir, hydroxychloroquine, lopinavir, and interferon regimens had little or no effect on hospitalized patients with Covid-19, as indicated by overall mortality, initiation of ventilation, and duration of hospital stay. (Funded by the World Health Organization; ISRCTN Registry number, ISRCTN83971151; ClinicalTrials.gov number, NCT04315948.)

    The Zwicky Transient Facility: System Overview, Performance, and First Results

    Get PDF
    The Zwicky Transient Facility (ZTF) is a new optical time-domain survey that uses the Palomar 48 inch Schmidt telescope. A custom-built wide-field camera provides a 47 deg 2 field of view and 8 s readout time, yielding more than an order of magnitude improvement in survey speed relative to its predecessor survey, the Palomar Transient Factory. We describe the design and implementation of the camera and observing system. The ZTF data system at the Infrared Processing and Analysis Center provides near-real-time reduction to identify moving and varying objects. We outline the analysis pipelines, data products, and associated archive. Finally, we present on-sky performance analysis and first scientific results from commissioning and the early survey. ZTF’s public alert stream will serve as a useful precursor for that of the Large Synoptic Survey Telescope

    Kilonova Luminosity Function Constraints Based on Zwicky Transient Facility Searches for 13 Neutron Star Merger Triggers during O3

    Get PDF
    We present a systematic search for optical counterparts to 13 gravitational wave (GW) triggers involving at least one neutron star during LIGO/Virgo's third observing run (O3). We searched binary neutron star (BNS) and neutron star black hole (NSBH) merger localizations with the Zwicky Transient Facility (ZTF) and undertook follow-up with the Global Relay of Observatories Watching Transients Happen (GROWTH) collaboration. The GW triggers had a median localization area of 4480 degÂČ, a median distance of 267 Mpc, and false-alarm rates ranging from 1.5 to 10⁻ÂČ⁔ yr⁻Âč. The ZTF coverage in the g and r bands had a median enclosed probability of 39%, median depth of 20.8 mag, and median time lag between merger and the start of observations of 1.5 hr. The O3 follow-up by the GROWTH team comprised 340 UltraViolet/Optical/InfraRed (UVOIR) photometric points, 64 OIR spectra, and three radio images using 17 different telescopes. We find no promising kilonovae (radioactivity-powered counterparts), and we show how to convert the upper limits to constrain the underlying kilonova luminosity function. Initially, we assume that all GW triggers are bona fide astrophysical events regardless of false-alarm rate and that kilonovae accompanying BNS and NSBH mergers are drawn from a common population; later, we relax these assumptions. Assuming that all kilonovae are at least as luminous as the discovery magnitude of GW170817 (−16.1 mag), we calculate that our joint probability of detecting zero kilonovae is only 4.2%. If we assume that all kilonovae are brighter than −16.6 mag (the extrapolated peak magnitude of GW170817) and fade at a rate of 1 mag day⁻Âč (similar to GW170817), the joint probability of zero detections is 7%. If we separate the NSBH and BNS populations based on the online classifications, the joint probability of zero detections, assuming all kilonovae are brighter than −16.6 mag, is 9.7% for NSBH and 7.9% for BNS mergers. Moreover, no more than 10⁻⁎, or φ > 30° to be consistent with our limits. We look forward to searches in the fourth GW observing run; even 17 neutron star mergers with only 50% coverage to a depth of −16 mag would constrain the maximum fraction of bright kilonovae to <25%

    The Zwicky Transient Facility: Science Objectives

    Get PDF
    The Zwicky Transient Facility (ZTF), a public–private enterprise, is a new time-domain survey employing a dedicated camera on the Palomar 48-inch Schmidt telescope with a 47 deg2 field of view and an 8 second readout time. It is well positioned in the development of time-domain astronomy, offering operations at 10% of the scale and style of the Large Synoptic Survey Telescope (LSST) with a single 1-m class survey telescope. The public surveys will cover the observable northern sky every three nights in g and r filters and the visible Galactic plane every night in g and r. Alerts generated by these surveys are sent in real time to brokers. A consortium of universities that provided funding (“partnership”) are undertaking several boutique surveys. The combination of these surveys producing one million alerts per night allows for exploration of transient and variable astrophysical phenomena brighter than r∌20.5 on timescales of minutes to years. We describe the primary science objectives driving ZTF, including the physics of supernovae and relativistic explosions, multi-messenger astrophysics, supernova cosmology, active galactic nuclei, and tidal disruption events, stellar variability, and solar system objects. © 2019. The Astronomical Society of the Pacific

    Can the discharge of a hyperconcentrated flow be estimated from paleoflood evidence?

    Get PDF
    Many flood events involving water and sediments have been characterized using classic hydraulics principles, assuming the existence of critical flow and many other simplifications. In this paper, hyperconcentrated flow discharge was evaluated by using paleoflood reconstructions (based on paleostage indicators [PSI]) combined with a detailed hydraulic analysis of the critical flow assumption. The exact location where this condition occurred was established by iteratively determining the corresponding cross section, so that specific energy is at a minimum. In addition, all of the factors and parameters involved in the process were assessed, especially those related to the momentum equation, existing shear stresses in the wetted perimeter, and nonhydrostatic and hydrostatic pressure distributions. The superelevation of the hyperconcentrated flow, due to the flow elevation curvature, was also estimated and calibrated with the PSI. The estimated peak discharge was established once the iterative process was unable to improve the fit between the simulated depth and the depth observed from the PSI. The methodological approach proposed here can be applied to other higher-gradient mountainous torrents with a similar geomorphic configuration to the one studied in this paper. Likewise, results have been derived with fewer uncertainties than those obtained from standard hydraulic approaches, whose simplifying assumptions have not been considered. © 2011 by the American Geophysical Union.This work was funded by the Spanish Ministry of Science and Innovation within the framework of the CICYT Dendro-Avenidas project (CGL2007-62063) and the MAS Dendro-Avenidas project (CGL2010-19274). We are especially grateful to Robert D. Jarrett, Vern Manville, and one anonymous reviewer for their comments and helpful suggestions on previous versions of this manuscript.Bodoque, J.; Eguibar GalĂĄn, MÁ.; Diez-Herrero, A.; Gutierrez-Perez, I.; Ruiz-Villanueva, V. (2011). Can the discharge of a hyperconcentrated flow be estimated from paleoflood evidence?. Water Resources Research. 47(W12535). doi:10.1029/2011WR010380S47W12535Alcoverro, J., Corominas, J., & GĂłmez, M. (1999). The Barranco de ArĂĄs flood of 7 August 1996 (Biescas, Central Pyrenees, Spain). Engineering Geology, 51(4), 237-255. doi:10.1016/s0013-7952(98)00076-3Alexandrov, Y., Laronne, J. B., & Reid, I. (2007). Intra-event and inter-seasonal behaviour of suspended sediment in flash floods of the semi-arid northern Negev, Israel. Geomorphology, 85(1-2), 85-97. doi:10.1016/j.geomorph.2006.03.013BAAS, J. H., & BEST, J. L. (2008). The dynamics of turbulent, transitional and laminar clay-laden flow over a fixed current ripple. Sedimentology, 55(3), 635-666. doi:10.1111/j.1365-3091.2007.00916.xBallesteros, J. A., Bodoque, J. M., DĂ­ez-Herrero, A., Sanchez-Silva, M., & Stoffel, M. (2011). Calibration of floodplain roughness and estimation of flood discharge based on tree-ring evidence and hydraulic modelling. Journal of Hydrology, 403(1-2), 103-115. doi:10.1016/j.jhydrol.2011.03.045Bathurst, J. C. (1985). Flow Resistance Estimation in Mountain Rivers. Journal of Hydraulic Engineering, 111(4), 625-643. doi:10.1061/(asce)0733-9429(1985)111:4(625)BERZI, D., & JENKINS, J. T. (2008). A theoretical analysis of free-surface flows of saturated granular–liquid mixtures. Journal of Fluid Mechanics, 608, 393-410. doi:10.1017/s0022112008002401Biron, P. M., Lane, S. N., Roy, A. G., Bradbrook, K. F., & Richards, K. S. (1998). Sensitivity of bed shear stress estimated from vertical velocity profiles: the problem of sampling resolution. Earth Surface Processes and Landforms, 23(2), 133-139. doi:10.1002/(sici)1096-9837(199802)23:23.0.co;2-nBisantino, T., Fischer, P., & Gentile, F. (2009). Rheological characteristics of debris-flow material in South-Gargano watersheds. Natural Hazards, 54(2), 209-223. doi:10.1007/s11069-009-9462-4Bousmar, D., & Zech, Y. (1999). Momentum Transfer for Practical Flow Computation in Compound Channels. Journal of Hydraulic Engineering, 125(7), 696-706. doi:10.1061/(asce)0733-9429(1999)125:7(696)Costa, J. E. (1984). Physical Geomorphology of Debris Flows. Developments and Applications of Geomorphology, 268-317. doi:10.1007/978-3-642-69759-3_9COUSSOT, P., & MEUNIER, M. (1996). Recognition, classification and mechanical description of debris flows. Earth-Science Reviews, 40(3-4), 209-227. doi:10.1016/0012-8252(95)00065-8Coussot, P., Laigle, D., Arattano, M., Deganutti, A., & Marchi, L. (1998). Direct Determination of Rheological Characteristics of Debris Flow. Journal of Hydraulic Engineering, 124(8), 865-868. doi:10.1061/(asce)0733-9429(1998)124:8(865)Desilets, S. L. E., FerrĂ©, T. P. A., & Ekwurzel, B. (2008). Flash flood dynamics and composition in a semiarid mountain watershed. Water Resources Research, 44(12). doi:10.1029/2007wr006159Dietrich, W. E., & Whiting, P. (1989). Boundary shear stress and sediment transport in river meanders of sand and gravel. River Meandering, 1-50. doi:10.1029/wm012p0001Ervine, D. A., Willetts, B. B., Sellin, R. H. J., & Lorena, M. (1993). Factors Affecting Conveyance in Meandering Compound Flows. Journal of Hydraulic Engineering, 119(12), 1383-1399. doi:10.1061/(asce)0733-9429(1993)119:12(1383)Gaume, E., Livet, M., Desbordes, M., & Villeneuve, J.-P. (2004). Hydrological analysis of the river Aude, France, flash flood on 12 and 13 November 1999. Journal of Hydrology, 286(1-4), 135-154. doi:10.1016/j.jhydrol.2003.09.015Grant, G. E. (1997). Critical flow constrains flow hydraulics in mobile-bed streams: A new hypothesis. Water Resources Research, 33(2), 349-358. doi:10.1029/96wr03134Hessel, R. (2006). Consequences of hyperconcentrated flow for process-based soil erosion modelling on the Chinese Loess Plateau. Earth Surface Processes and Landforms, 31(9), 1100-1114. doi:10.1002/esp.1307House, P. K., & Baker, V. R. (2001). Paleohydrology of flash floods in small desert watersheds in western Arizona. Water Resources Research, 37(6), 1825-1839. doi:10.1029/2000wr900408House, P. K., & Pearthree, P. A. (1995). A geomorphologic and hydrologic evaluation of an extraordinary flood discharge estimate: Bronco Creek, Arizona. Water Resources Research, 31(12), 3059-3073. doi:10.1029/95wr02428Hungr, O. (s. f.). Classification and terminology. Springer Praxis Books, 9-23. doi:10.1007/3-540-27129-5_2Iverson, R. M. (1997). The physics of debris flows. Reviews of Geophysics, 35(3), 245-296. doi:10.1029/97rg00426Iverson , R. M. 2003 The debris-flow rheology myth, paper presented at debris-flow hazards mitigation: mechanics, prediction, and assessment 303 314 Millpress Rotterdam, Davos, SwitzerlandIverson, R. M., Logan, M., LaHusen, R. G., & Berti, M. (2010). The perfect debris flow? Aggregated results from 28 large-scale experiments. Journal of Geophysical Research, 115(F3). doi:10.1029/2009jf001514Jarrett, R. D. (1987). Closure to « Hydraulics of High‐Gradient Streams » by Robert D. Jarrett (November, 1984). Journal of Hydraulic Engineering, 113(7), 927-929. doi:10.1061/(asce)0733-9429(1987)113:7(927)Jarrett, R. D., & Tomlinson, E. M. (2000). Regional interdisciplinary paleoflood approach to assess extreme flood potential. Water Resources Research, 36(10), 2957-2984. doi:10.1029/2000wr900098Lavigne, F., & Suwa, H. (2004). Contrasts between debris flows, hyperconcentrated flows and stream flows at a channel of Mount Semeru, East Java, Indonesia. Geomorphology, 61(1-2), 41-58. doi:10.1016/j.geomorph.2003.11.005McCoy, S. W., Kean, J. W., Coe, J. A., Staley, D. M., Wasklewicz, T. A., & Tucker, G. E. (2010). Evolution of a natural debris flow: In situ measurements of flow dynamics, video imagery, and terrestrial laser scanning. Geology, 38(8), 735-738. doi:10.1130/g30928.1Pierson , T. C. 2005 Distinguishing between debris flows and floods from field evidence Small Watersheds U.S. Geological Survey 2004 3142Pierson, T. C. (s. f.). Hyperconcentrated flow — transitional process between water flow and debris flow. Springer Praxis Books, 159-202. doi:10.1007/3-540-27129-5_8Pierson, T. C., & Costa, J. E. (1987). A rheologic classification of subaerial sediment-water flows. Reviews in Engineering Geology, 1-12. doi:10.1130/reg7-p1Pierson, T. C., & Scott, K. M. (1985). Downstream Dilution of a Lahar: Transition From Debris Flow to Hyperconcentrated Streamflow. Water Resources Research, 21(10), 1511-1524. doi:10.1029/wr021i010p01511Rico, M., Benito, G., & Barnolas, A. (2001). Combined palaeoflood and rainfall–runoff assessment of mountain floods (Spanish Pyrenees). Journal of Hydrology, 245(1-4), 59-72. doi:10.1016/s0022-1694(01)00339-0Roca, M., MartĂ­n-Vide, J. P., & Moreta, P. J. M. (2009). Modelling a torrential event in a river confluence. Journal of Hydrology, 364(3-4), 207-215. doi:10.1016/j.jhydrol.2008.10.020Ruiz-Villanueva, V., Bodoque, J. M., DĂ­ez-Herrero, A., & Calvo, C. (2011). Triggering threshold precipitation and soil hydrological characteristics of shallow landslides in granitic landscapes. Geomorphology, 133(3-4), 178-189. doi:10.1016/j.geomorph.2011.05.018Shiono, K., & Knight, D. W. (1991). Turbulent open-channel flows with variable depth across the channel. Journal of Fluid Mechanics, 222(-1), 617. doi:10.1017/s0022112091001246Shu, A., & Fei, X. (2008). Sediment transport capacity of hyperconcentrated flow. Science in China Series G: Physics, Mechanics and Astronomy, 51(8), 961-975. doi:10.1007/s11433-008-0108-4Siviglia, A., & Cantelli, A. (2005). Effect of bottom curvature on mudflow dynamics: Theory and experiments. Water Resources Research, 41(11). doi:10.1029/2005wr004475Sleiti, A. K., & Kapat, J. S. (2008). Effect of Coriolis and centrifugal forces on turbulence and transport at high rotation and density ratios in a rib-roughened channel. International Journal of Thermal Sciences, 47(5), 609-619. doi:10.1016/j.ijthermalsci.2007.06.008SMITH, G. A. (1986). Coarse-grained nonmarine volcaniclastic sediment: Terminology and depositional process. Geological Society of America Bulletin, 97(1), 1. doi:10.1130/0016-7606(1986)972.0.co;2Sohn, Y. K., Rhee, C. W., & Kim, B. C. (1999). Debris Flow and Hyperconcentrated Flood‐Flow Deposits in an Alluvial Fan, Northwestern Part of the Cretaceous Yongdong Basin, Central Korea. The Journal of Geology, 107(1), 111-132. doi:10.1086/314334Sosio, R., & Crosta, G. B. (2009). Rheology of concentrated granular suspensions and possible implications for debris flow modeling. Water Resources Research, 45(3). doi:10.1029/2008wr006920Svendsen, J., Stollhofen, H., Krapf, C. B. ., & Stanistreet, I. G. (2003). Mass and hyperconcentrated flow deposits record dune damming and catastrophic breakthrough of ephemeral rivers, Skeleton Coast Erg, Namibia. Sedimentary Geology, 160(1-3), 7-31. doi:10.1016/s0037-0738(02)00334-2Tinkler, K. J. (1997). Critical flow in rockbed streams with estimated values for Manning’s n. Geomorphology, 20(1-2), 147-164. doi:10.1016/s0169-555x(97)00011-1Trieste , D. J. R. D. Jarrett 1987 Roughness coefficients of large floodsVan Maren, D. S., Winterwerp, J. C., Wu, B. S., & Zhou, J. J. (2009). Modelling hyperconcentrated flow in the Yellow River. Earth Surface Processes and Landforms, 34(4), 596-612. doi:10.1002/esp.1760Wan, Z., Wang, Z., & Julien, P. Y. (1994). Hyperconcentrated Flow. Journal of Hydraulic Engineering, 120(10), 1234-1234. doi:10.1061/(asce)0733-9429(1994)120:10(1234)Winterwerp, J. C. (2001). Stratification effects by cohesive and noncohesive sediment. Journal of Geophysical Research: Oceans, 106(C10), 22559-22574. doi:10.1029/2000jc000435Jiongxin, X. (1999). Erosion caused by hyperconcentrated flow on the Loess Plateau of China. CATENA, 36(1-2), 1-19. doi:10.1016/s0341-8162(99)00009-
    • 

    corecore