Ammonia Gas Sensors: Comparison of Solid-State and Optical Methods
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Nitrogen Trace Gas Emissions from a Riparian Ecosystem in Sot&Em
CHEMOSPHERE PERGAMON Chemosphere 49 (2002) 1389-l 398 www.elsevier.com/locate/chemosphere Nitrogen trace gas emissions from a riparian ecosystem in sot&em Appalachia John T. Walker aP*, Christopher D. Geron a, James M. Vose b, Wayne T. Swank b ’ US Enviromental Protection Agency, Natkmal R&k Managmt Research Laboratory, iUD-63, Research Triangk Park, NC 27711, USA b US Department of Agricdture, Forest Service, Coweeta Hydrologic Laboratory, Otto, NC 28763, USA Received 11 July 2001; received in revised form 21 May 2002; accepted 19 June 2002 Abstract In this paper, we present two years of seasonal nitric oxide (NO), ammonia (NH3), and nitrous oxide (NrO) trace gas fluxes measured in a recovering riparian zone with cattle excluded and adjacent riparian zone grazed by cattle. In the recovering riparian zone, average NO, NH3, and NrO fluxes were 5.8,2.0, and 76.7 ngNm-* s-i (1.83,0.63, and 24.19 kg N ha-’ y-t), respectively. Fluxes in the grazed riparian zone were larger, especially for NO and NHr, measuring 9.1, 4.3, and 77.6 ng Nm-* s-* (2.87, 1.35, and 24.50 kg N ha-’ y-l) for NO, NHr, and N20, respectively. On average, NzO accounted for greater than 85% of total trace gas flux in both the recovering and grazed riparian zones, though NrO fluxes were highly variable temporally. In the recovering riparian zone, variability in seasonal average fluxes was ex- plained by variability in soil nitrogen (N) concentrations. Nitric oxide flux was positively correlated with soil ammo- nium (NH:) concentration, while N20 flux was positively correlated with soil nitrate (NO;) concentration. -
Relative Importance of Gas Uptake on Aerosol and Ground Surfaces Characterized by Equivalent Uptake Coefficients
Atmos. Chem. Phys., 19, 10981–11011, 2019 https://doi.org/10.5194/acp-19-10981-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Relative importance of gas uptake on aerosol and ground surfaces characterized by equivalent uptake coefficients Meng Li1,a, Hang Su1, Guo Li1, Nan Ma2, Ulrich Pöschl1, and Yafang Cheng1 1Max Planck Institute for Chemistry, Mainz, 55118, Germany 2Center for Air Pollution and Climate Change Research (APCC), Institute for Environmental and Climate Research (ECI), Jinan University, Guangzhou, 511443, China anow at: Chemical Science Division, Earth System Research Laboratory, National Oceanic and Atmospheric Administration (NOAA), Boulder, Colorado 80305, USA Correspondence: Hang Su ([email protected]) and Yafang Cheng ([email protected]) Received: 19 March 2019 – Discussion started: 2 April 2019 Revised: 9 July 2019 – Accepted: 19 July 2019 – Published: 29 August 2019 Abstract. Quantifying the relative importance of gas up- Given the fact that most models have considered the up- take on the ground and aerosol surfaces helps to determine takes of these species on the ground surface, we suggest also which processes should be included in atmospheric chem- considering the following processes in atmospheric models: istry models. Gas uptake by aerosols is often characterized N2O5 uptake by all types of aerosols, HNO3 and SO2 uptake by an effective uptake coefficient (γeff), whereas gas uptake by mineral dust and sea salt aerosols, H2O2 uptake by min- on the ground is usually described by a deposition velocity eral dust, NO2 uptakes by sea salt aerosols and O3 uptake by (Vd). -
Atomic and Molecular Laser-Induced Breakdown Spectroscopy of Selected Pharmaceuticals
Article Atomic and Molecular Laser-Induced Breakdown Spectroscopy of Selected Pharmaceuticals Pravin Kumar Tiwari 1,2, Nilesh Kumar Rai 3, Rohit Kumar 3, Christian G. Parigger 4 and Awadhesh Kumar Rai 2,* 1 Institute for Plasma Research, Gandhinagar, Gujarat-382428, India 2 Laser Spectroscopy Research Laboratory, Department of Physics, University of Allahabad, Prayagraj-211002, India 3 CMP Degree College, Department of Physics, University of Allahabad, Pragyagraj-211002, India 4 Physics and Astronomy Department, University of Tennessee, University of Tennessee Space Institute, Center for Laser Applications, 411 B.H. Goethert Parkway, Tullahoma, TN 37388-9700, USA * Correspondence: [email protected]; Tel.: +91-532-2460993 Received: 10 June 2019; Accepted: 10 July 2019; Published: 19 July 2019 Abstract: Laser-induced breakdown spectroscopy (LIBS) of pharmaceutical drugs that contain paracetamol was investigated in air and argon atmospheres. The characteristic neutral and ionic spectral lines of various elements and molecular signatures of CN violet and C2 Swan band systems were observed. The relative hardness of all drug samples was measured as well. Principal component analysis, a multivariate method, was applied in the data analysis for demarcation purposes of the drug samples. The CN violet and C2 Swan spectral radiances were investigated for evaluation of a possible correlation of the chemical and molecular structures of the pharmaceuticals. Complementary Raman and Fourier-transform-infrared spectroscopies were used to record the molecular spectra of the drug samples. The application of the above techniques for drug screening are important for the identification and mitigation of drugs that contain additives that may cause adverse side-effects. Keywords: paracetamol; laser-induced breakdown spectroscopy; cyanide; carbon swan bands; principal component analysis; Raman spectroscopy; Fourier-transform-infrared spectroscopy 1. -
Inelastic Scattering in Ocean Water and Its Impact on Trace Gas Retrievals from Satellite Data
Atmos. Chem. Phys., 3, 1365–1375, 2003 www.atmos-chem-phys.org/acp/3/1365/ Atmospheric Chemistry and Physics Inelastic scattering in ocean water and its impact on trace gas retrievals from satellite data M. Vountas, A. Richter, F. Wittrock, and J. P. Burrows Institute for Environmental Physics, University of Bremen, Bremen, Germany Received: 4 April 2003 – Published in Atmos. Chem. Phys. Discuss.: 2 June 2003 Revised: 29 August 2003 – Accepted: 4 September 2003 – Published: 15 September 2003 Abstract. Over clear ocean waters, photons scattered within 1 Introduction the water body contribute significantly to the upwelling flux. In addition to elastic scattering, inelastic Vibrational Raman Backscattered light from waters with low concentrations of Scattering (VRS) by liquid water is also playing a role and chlorophyll and gelbstoff – which are commonly referred can have a strong impact on the spectral distribution of the to as oligotrophic waters – is significantly influenced by outgoing radiance. Under clear-sky conditions, VRS has an Vibrational Raman Scattering (VRS) within the water (e.g. influence on trace gas retrievals from space-borne measure- Stavn and Weidemann, 1988; Marshall and Smith, 1990; ments of the backscattered radiance such as from e.g. GOME Haltrin and Kattawar, 1993; Sathyendranath and Platt, 1998; (Global Ozone Monitoring Experiment). The effect is par- Vasilkov et al., 2002b). ticularly important for geo-locations with small solar zenith As inelastic scattering redistributes photons over wave- angles and over waters with low chlorophyll concentration. length, VRS fills-in solar Fraunhofer lines, as well as trace gas absorption lines and therefore changes the spectral dis- In this study, a simple ocean reflectance model (Sathyen- tribution of scattered light in the atmosphere. -
Cris Trace Gas Data Users Workshop
NOAA Unique CrIS/ATMS Processing System (NUCAPS) Trace Gas Data Products and Access A.K. Sharma (OSPO) CrIS Trace Gas Data Users Workshop September 18, 2014 The NOAA Unique CrIS/ATMS Processing System Products Retrieval Products gas Range Precisio d.o.f. Interfering Gases Science Cloud Cleared Radiances 660-750 cm-1 (cm-1) n Code 2200-2400 cm-1 T 650-800 1K/km 6-10 H2O,O3,N2O 100 levels Cloud fracon and Top 660-750 cm-1 2375-2395 emissivity Pressure Surface temperature window H2O 1200-1600 15% 4-6 CH4, HNO3 100 layers O 1025-1050 10% 1+ H2O,emissivity 100 layers Temperature 660-750 cm-1 3 2200-2400 cm-1 CO 2080-2200 15% ≈ 1 H2O,N2O 100 layers Water Vapor 780 – 1090 cm-1 1200-1750 cm-1 CH4 1250-1370 1.5% ≈ 1 H2O,HNO3,N2O 100 layers O3 990 – 1070 cm-1 CO2 680-795 0.5% ≈ 1 H2O,O3 100 layers CO 2155 – 2220 cm-1 2375-2395 T(p) CH4 1220-1350 cm-1 Volcanic 1340-1380 50% ?? < 1 H2O,HNO3 flag SO2 N2O 1290-1300cm-1 2190-2240cm-1 HNO3 860-920 50% ?? < 1 emissivity 100 layers 1320-1330 H2O,CH4,N2O HNO3 760-1320cm-1 N2O 1250-1315 5% ?? < 1 H2O 100 layers SO2 1343-1383cm-1 2180-2250 H2O,CO NH3 860-875 50% <1 emissivity BT diff CFCs 790-940 20-50% <1 emissivity Constant NUCAPS EDR Trace Gas Products The EDR product contains the following trace gas profiles calculated on each CrIS FOR: O3 layer column density (at 100 levels) O3 mixing ratio (at 100 levels) First Guess O3 layer column density (at 100 levels) First Guess O3 mixing ratio (at 100 levels) CH4 layer column density (at 100 levels) CH4 mixing ratio (at 100 levels) CO2 mixing ratio (at 100 levels) HNO3 layer column density (at 100 levels) HNO3 mixing ratio (at 100 levels) N2O layer column density (at 100 levels) N2O mixing ratio (at 100 levels) SO2 layer column density (at 100 levels) SO2 mixing ratio (at 100 levels) 3 AWIPS NUCAPS Products The retrieval product for AWIPS contains the following variaBles. -
Concentrations and Fluxes of Aerosol Particles During the LAPBIAT
Atmos. Chem. Phys. Discuss., 7, 709–751, 2007 Atmospheric www.atmos-chem-phys-discuss.net/7/709/2007/ Chemistry © Author(s) 2007. This work is licensed and Physics under a Creative Commons License. Discussions Concentrations and fluxes of aerosol particles during the LAPBIAT measurement campaign in Varri¨ o¨ field station T. M. Ruuskanen1, M. Kaasik2, P. P. Aalto1, U. Horrak˜ 2, M. Vana1,2, M. Martensson˚ 3, Y. J. Yoon4, P. Keronen1, G. Mordas1, D. Ceburnis4, E. D. Nilsson3, C. O’Dowd4, M. Noppel2, T. Alliksaar5, J. Ivask5, M. Sofiev6, M. Prank2, and M. Kulmala1 1University of Helsinki, Dept. of Physical Sciences, P.O. Box 64, 00014 University of Helsinki, Finland 2Institute of Environmental Physics, University of Tartu, Tartu, Estonia 3Department of Applied Environmental Science, Stockholm University, Stockholm, Sweden 4Department of Experimental Physics, National University of Ireland, Galway, Ireland 5Institute of Geology, Tallinn University of Technology, Tallinn, Estonia 6Air Quality Research, Finnish Meteorological Institute, Finland Received: 21 November 2006 – Accepted: 8 January 2006 – Published: 17 January 2007 Correspondence to: T. M. Ruuskanen (taina.ruuskanen@helsinki.fi) 709 Abstract The LAPBIAT measurement campaign took place in the SMEAR I measurement station located in Eastern Lapland in the spring of 2003 between 26 April and 11 May. In this paper we describe the measurement campaign, concentrations and fluxes of aerosol 5 particles, air ions and trace gases, paying special attention to an aerosol particle for- mation event broken by a polluted air mass approaching from industrial areas of Kola Peninsula, Russia. Aerosol particle number flux measurements show strong downward fluxes during that time. -
Nitrogen-15 Magnetic Resonance Spectroscopy, I
VOL. 51, 1964 CHEMISTRY: LAMBERT, BINSCH, AND ROBERTS 735 11 Felsenfeld, G., G. Sandeen, and P. von Hippel, these PROCEEDINGS, 50, 644 (1963). 12Bollum, F. J., J. Cell. Comp. Physiol., 62 (Suppi. 1), 61 (1963); Von Borstel, R. C., D. M. Prescott, and F. J. Bollum, J. Cell Biol., 19, 72A (1963). 13 Huang, R. C., and J. Bonner, these PROCEEDINGS, 48, 216 (1962); Allfrey, V. G., V. C. Littau, and A. E. Mirsky, these PROCEEDINGS, 49, 414 (1963). 14 Baxill, G. W., and J. St. L. Philpot, Biochim. Biophys. Acta, 76, 223 (1963). NITROGEN-15 MAGNETIC RESONANCE SPECTROSCOPY, I. CHEMICAL SHIFTS* BY JOSEPH B. LAMBERT, GERHARD BINSCH, AND JOHN D. ROBERTS GATES AND CRELLIN LABORATORIES OF CHEMISTRY, t CALIFORNIA INSTITUTE OF TECHNOLOGY Communicated March 23, 1964 Except for the original determination' of nuclear moments, nitrogen magnetic resonance spectroscopy has been limited to the isotope of mass number 14. Al- though N14 is an abundant isotope, it possesses an electric quadrupole moment, which seriously broadens the resonances of nitrogen in all but the most sym- metrical of environments.2 Consequently, nitrogen n.m.r. spectroscopy has seen only limited use in the determination of organic structure. It might be expected that N15, which has a spin of 1/2 and no quadrupole moment, would be very useful, but the low natural abundance (0.36%) and the inherently low signal intensity (1.04 X 10-3 that of H' at constant field) have thus far precluded utilization of N15 in n.m.r. spectroscopy'3 Resonance signals from N'5 have now been obtained from a series of N"5-enriched (30-99%) compounds with a Varian model 4300B spectrometer operated at 6.08 Mc/sec and 14,100 gauss. -
2. Molecular Stucture/Basic Spectroscopy the Electromagnetic Spectrum
2. Molecular stucture/Basic spectroscopy The electromagnetic spectrum Spectral region fooatocadr atomic and molecular spectroscopy E. Hecht (2nd Ed.) Optics, Addison-Wesley Publishing Company,1987 Per-Erik Bengtsson Spectral regions Mo lecu lar spec troscopy o ften dea ls w ith ra dia tion in the ultraviolet (UV), visible, and infrared (IR) spectltral reg ions. • The visible region is from 400 nm – 700 nm • The ultraviolet region is below 400 nm • The infrared region is above 700 nm. 400 nm 500 nm 600 nm 700 nm Spectroscopy: That part of science which uses emission and/or absorption of radiation to deduce atomic/molecular properties Per-Erik Bengtsson Some basics about spectroscopy E = Energy difference = c /c h = Planck's constant, 6.63 10-34 Js ergy nn = Frequency E hn = h/hc /l E = h = hc / c = Velocity of light, 3.0 108 m/s = Wavelength 0 Often the wave number, , is used to express energy. The unit is cm-1. = E / hc = 1/ Example The energy difference between two states in the OH-molecule is 35714 cm-1. Which wavelength is needed to excite the molecule? Answer = 1/ =35714 cm -1 = 1/ = 280 nm. Other ways of expressing this energy: E = hc/ = 656.5 10-19 J E / h = c/ = 9.7 1014 Hz Per-Erik Bengtsson Species in combustion Combustion involves a large number of species Atoms oxygen (O), hydrogen (H), etc. formed by dissociation at high temperatures Diatomic molecules nitrogen (N2), oxygen (O2) carbon monoxide (CO), hydrogen (H2) nitr icoxide (NO), hy droxy l (OH), CH, e tc. -
The Power of Crowding for the Origins of Life
Orig Life Evol Biosph (2014) 44:307–311 DOI 10.1007/s11084-014-9382-5 ORIGIN OF LIFE The Power of Crowding for the Origins of Life Helen Greenwood Hansma Received: 2 October 2014 /Accepted: 2 October 2014 / Published online: 14 January 2015 # Springer Science+Business Media Dordrecht 2015 Abstract Molecular crowding increases the likelihood that life as we know it would emerge. In confined spaces, diffusion distances are shorter, and chemical reactions produce fewer and more regular products. Crowding will occur in the spaces between Muscovite mica sheets, which has many advantages as a site for life’s origins. Keywords Muscovite mica . Molecular crowding . Origin of life . Mechanochemistry. Abiogenesis . Chemical confinement effects . Chirality. Protocells Cells are crowded. Protein molecules in cells are typically so close to each other that there is room for only one protein molecule between them (Phillips, Kondev et al. 2008). This is nothing like a dilute ‘prebiotic soup.’ Therefore, by analogy with living cells, the origins of life were probably also crowded. Molecular Confinement Effects Many chemical reactions are limited by the time needed for reactants to diffuse to each other. Shorter distances speed up these reactions. Molecular complementarity is another principle of life in which pairs or groups of molecules form specific interactions (Root-Bernstein 2012). Current examples are: enzymes & substrates & cofactors; nucleic acid base pairs; antigens & antibodies; nucleic acid - protein interactions. Molecular complementarity is likely to have been involved at life’s origins and also benefits from crowding. Mineral surfaces are a likely place for life’s origins and for formation of polymeric molecules (Orgel 1998). -
Dual Laser Trace Gas Monitor Sensitive, Rapid, Highly Specific and Continuous Measurements of Multiple Atmospheric Trace Gases in Ambient Air
Dual Laser Trace Gas Monitor Sensitive, rapid, highly specific and continuous measurements of multiple atmospheric trace gases in ambient air. APPLICATIONS ADVANTAGES • Extremely sensitive detection of a wide variety of • Absolute trace gas concentrations with atmospheric trace gases, such as: methane, out calibration gases. nitrous oxide, nitric oxide, nitrogen dioxide, carbon monoxide, carbon dioxide, formaldehyde, • Fast time response. formic acid, ethylene, acetylene, carbonyl sulfide, acrolein, ammonia and others. • Free from interferences by other atmospheric gases or water vapor. • Combustion monitoring and characterization. • Turnkey and unattended operation. • Isotopic monitoring of CH4 and N2O for source/ sink characterization. • Ready to be deployed in field measurements and on moving platforms. • Eddy Covariance measurements. • Two lasers allow simultaneous • Fast response plume studies. measurement of more species. • Air quality monitoring. • Optical pathlength of either 76 meters or 210 meters. • Mobile measurements from ship, truck, and Aircraft platforms. AERODYNE RESEARCH, Inc. 45 MANNING ROAD, BILLERICA, MA 01821 (978) 663 9500 www.aerodyne.com CAEC_TILDAS_DUAL POPULAR INSTRUMENTS HIGHER PRECISION AND ACCURACY IS OBTAINABLE WITH MID-INFRARED LASERS Clumped CO2 Isotopes* CH4 Isotopes CO2, Water Isotopes N2O Isotopes NO, NO2 CH4, N2O, CO,CO2, H2O, C2H6 MECHANICAL SPECIFICATIONS FOR DUAL LASER TRACE GAS MONITOR: Dimensions: 560 mm x 770 mm x 640 mm (W x D x H) Weight: 75 kg Electrical Power: 250-500 W, 120/240 V, 55/60 Hz (without pump) MULTIPASS CELL: Choice of 76 meter standard cell (V=0.5 liters) or 210 meter “Super Cell” (V=2liters) *Image attribution by Psammophile [GFDL (http://www.gnu.org/copyleft/fdl.html) or CC-BY-SA-3.0-2.5-2.0-1.0 (http://creativecommons.org/licenses/by-sa/3.0)], via Wikimedia Commons REFERENCES: Nelson, D.D. -
Transportable Aerosol Characterization Trailer with Trace Gas Chemistry: Design, Instruments and Verification
Aerosol and Air Quality Research, 13: 421–435, 2013 Copyright © Taiwan Association for Aerosol Research ISSN: 1680-8584 print / 2071-1409 online doi: 10.4209/aaqr.2012.08.0207 Transportable Aerosol Characterization Trailer with Trace Gas Chemistry: Design, Instruments and Verification T. Petäjä1*, V. Vakkari1, T. Pohja2, T. Nieminen1, H. Laakso2, P.P. Aalto1, P. Keronen1, E. Siivola1, V.-M. Kerminen1,3, M. Kulmala1, L. Laakso3,4 1 Division of Atmospheric Sciences, Department of Physics, University of Helsinki, P.O. Box 64, FI-00014 University of Helsinki, Finland 2 Hyytiälä Forestry Field Station, Hyytiäläntie 124, FI-35500 Korkeakoski, Finland 3 School of Physical and Chemical Sciences, North-West University, Potchefstroom 2520, South Africa 4 Finnish Meteorological Institute, Research and Development, P.O. Box 503, FI-00101, Finland ABSTRACT The characterization of atmospheric aerosol properties and trace gas concentrations in various environments provides a basis for scientific research on the assessment of their roles in the climate system, as well as regional air quality issues. However, measurements of these face many problems in the developing world. In this study we present the design of a transportable aerosol dynamic and atmospheric research trailer, which relies minimally on the existing infrastructure by making use of wireless data transfer. The instrumentation used in this trailer was originally used in various aerosol formation studies, and has been expanded so that it can also monitor air quality. The instruments include a Differential Mobility Particle Sizer (DMPS) for aerosol number size distribution in the range 10–840 nm, a Tapered Element Oscillating Microbalance (TEOM) for aerosol mass concentration, and Air Ion Spectrometer (AIS) for atmospheric ion measurements in the size range 0.5–40 nm. -
Is a Trace Gas in Earth's Atmosphere, with a Mixing Ratio in 2005 Of
Nitrous Oxide Nitrous oxide (chemical formula N 2O), is a trace gas in Earth’s atmosphere, with a mixing ratio in 2005 of 319±0.12 ppb (parts per billion, by volume). Atmospheric nitrous oxide is steadily increasing due to human activities. Nitrous oxide absorbs terrestrial radiation (i.e. radiation emitted by the Earth), and consequently it is an important anthropogenic greenhouse gas; it is one of the gases targeted for control within the Kyoto Protocol. Nitrous oxide also absorbs solar radiation, which can split the molecule, releasing reactive species that contribute towards stratospheric ozone depletion. Various natural and anthropogenic sources add nitrous oxide to the atmosphere. The main natural sources are related to biological activity in soils and the upper ocean. The largest anthropogenic source is from the use of nitrogenous fertilizer in the agricultural sector; others include combustion of fossil fuel, biomass and biofuel, and industrial processes. Nitrous oxide emissions related to biofuel production are an example of reducing emissions of one greenhouse gas (CO 2) at the expense of increasing emissions of another. Nitrous oxide is relatively inert in the troposphere (the atmosphere’s lowest 10-15 km). Higher up, in the stratosphere, energetic ultra-violet radiation starts to break the molecule apart. This photochemical destruction in the upper atmosphere removes about 0.9% of all nitrous oxide every year, determining the average atmospheric residence time of an N 2O molecule, which is currently around 114 years. This is long compared to timescales of most atmospheric transport and mixing processes, which typically range from hours to a few years.