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光腔衰荡光谱(CRDS)技术

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2021-02-08 16:13
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2021年2月8日发(作者:bll)



中国地质大学(武汉)



材化学院





课程名称:文件检索




班级:


031111



姓名:刘欢




学号:


2














题目


(4 )


:光腔衰荡光谱


(CRDS)


技术< /p>






ison of water isotope-ratio determinations using


two


cavity


ring-down


instruments


and


classical


mass


spectrometry in continuous ice-core analysis


作者:


Olivia J. Maselli ,


Diedrich Fritzsche ,


Lawrence Layman ,


Joseph R.


McConnell ,


Hanno Meyer



作者单位:


Desert Research Institute;;Alfred-Wegener Institute for Polar and Marine


Research



刊名:


Isotopes in Environmental and Health Studies, 2013, Vol.49 (3), pp.387-398



来源数据库:


Taylor & Francis


期刊



DOI



10.1080/10256016.2013.781598



关键词:


cavity ring- down


hydrogen-2


ice- core


isotope measurements


methods


and equipment


oxygen-18


paleoclimatology


water


;



原始语种摘要:


We present a detailed comparison between subsequent versions of


commercially available wavelength-scanned cavity ring-down water isotope analysers


(L2120-i and L2130-i, Picarro Inc.). The analysers are used in parallel in a continuous


mode by adaption of a low- volume flash evaporation module. Application of the analysers


to ice-core analysis is assessed by comparison between continuous water isotope


measurements of a glacial ice- core from Severnaya Zemlya with discrete isotope- ratio


mass spectrometry measurements performed on parallel samples from the same ice- core.


The great advances between instrument versions, particularly in the measurement of


δ


2H, allow the continuous technique to achieve the same high level of accuracy and


precision obtained using traditional isotope spectrometry


techniques in a fraction of the


experiment time. However, when applied to continuous ice-core measurements,


increased integration times result in a compromise of the achievable depth resolution of


the ice-core records.



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[1] Olga Garmash. Deposition History of Polychlorinated Biphenyls to the


Lomonosovfonna Glacier, Svalbard: A 209 Congener Analysis. [J].Environ. Sci.


Technol.,2013


[2] Ulrich Schimschal. Mathematical model of gamma-ray spectrometry borehole logging


for quantitative analysis (Open-file report / United.... [M].,1981





a


real-time


measurement


of


atmospheric


mercury


concentrations


using


cavity


ring-down


spectroscopy


作者:


X. Fa?


n ,


H. Moosm


ü


ller ,


D. Obrist



刊名:


Atmospheric Chemistry and Physics Discussions, 2009, Vol.9 (5), pp.22143



来源数据库:


DO AJ


期刊



原始语种摘要:


A new sensor based on cavity ring-down spectroscopy (CRDS) has been


developed for the measurement of gaseous elemental mercury (Hg0) mass concentration


with sub-ng m


3


detection limit and high temporal resolution. Cavity ring-down


?


spectroscopy is a direct absorption technique that utilizes path lengths of up to multiple


kilometers in a compact absorption cell and has a significantly higher sensitivity than


conventional absorption spectroscopy. Our prototype uses a frequency-doubled, tuneable


dye laser emitting pulses at ~253.65 nm with a pulse repetition frequency of 50 Hz. The


dye laser incorporates a unique piezo element attached to its tuning grating allowing it to


tune the laser on and off the Hg0 absorption line on a pulse to pulse basis to facilitate...


differential absorption measurements. Hg0 absorption measurements with this CRDS


laboratory prototype are highly linearly related to Hg0 concentrations determined by a


Tekran 2537B analyzer over a Hg0 concentration range of four orders of magnitude, from


0.2 ng m


3


to 573 ng m


3


implying excellent linearity of both instruments. The current


?


?


CRDS instrument has a~sensitivity of 0.10 ng m


3


at 10 s time resolution. This tool opens


?


new prospects for the study of Hg0 because of its high temporal resolution and reduced


limited sample volume requirements (<0.5 l of sample air). Future applications may


include ambient Hg0 flux measurements with eddy covariance techniques, which require


measurements of Hg0 concentrations with sub-ng m


3


sensitivity and sub- second time


?


resolution.



相似文献:



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é


r< /p>


?


me. Effects of laser phase noise on the injection of a high-finesse


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ó


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Physics),2003,66(6 Pt 2)



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hygienists].. [J].Nederlands Tijdschrift voor Tandheelkunde,1981,88(2)



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AMERICA,2004,101(36)



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resonators.. [J].Optics Letters,1985,10(10)



-time


monitoring


of


breath


ammonia


during


haemodialysis: use of ion mobility spectrometry (IMS) and


cavity ring-down spectroscopy (CRDS) techniques


.


作者:


Neri Giovanni ,


Lacquaniti Antonio ,


Rizzo Giuseppe ,


Donato Nicola ,


Latino


Mariangela ,


Buemi Michele



作者单位:


Correspondence and offprint requests to: Michele Buemi; E-mail:


buemim@.



刊名:


Nephrology, Dialysis, Transplantation, 2012, Vol.27 (7), pp.2945-52


来源数据库:


PubMed


期刊



DOI



10.1093/ ndt/gfr738



原始语种摘要:


Background The diffusion of high-performance analytical technology has


opened prospects for breath diagnosis as a non-invasive diagnostic tool. In this study, ion


mobility spectrometry (IMS) and cavity ring-down spectroscopy (CRDS) techniques were


used to analyse ammonia gas NH


3


in real-time in breath from patients undergoing


haemodialysis (HD) treatment and any correlation with blood urea nitrogen (BUN) levels


and Kt/V were investigated. Methods We studied 20 patients on intermittent HD treatment.


The first breath samples were taken before the start of dialysis and further breath samples


were taken every hour during the treatment and after the end of the session. An


evaluation was also made of 20 healthy volunteers, acting as controls [healthy subjects


(HS)]. Results Breath ammonia... concentrations were higher in CRDS-HD (914.5


±



301.4 versus 280


±



120 parts per billion (p.p.b.), P < 0.0001) and IMS-HD patients


(964.4


±



402.4 versus 280


±



120 p.p.b., P < 0.0001) than in HS. We assessed


real- time variations in the levels of NH


3


and showed a continuous decrease in the levels of


NH


3


. Expired NH


3


correlated directly with BUN levels, both in the IMS-HD (P = 0.002; r =


0.84; P = 0.009; r = 0.76) and in the CRDS-HD group (P = 0.005; r = 0.80; P = 0.008; r =


0.77), respectively, both before and at the end of dialysis. A direct correlation with Kt/V


was found in both groups studied (IMS-HD: P = 0.003; r = 0.82; CRDS-HD: P = 0.006; r =


0.79). Conclusions Breath monitoring of NH


3


with IMS and CRDS techniques could be


useful to assess the real-time clinical status of patients during HD. By using pre-dialysis


ammonia values, an approximate calculation of the Kt/V(urea) ratio can be established.



相似文献:




[1] Neri Giovanni. Real-time monitoring of breath ammonia during haemodialysis: use of


ion mobility spectrometry (IMS) and cavity ring-down spectroscopy (CRDS)


techniques.. [J].Nephrology, Dialysis, Transplantation,2012,27(7)



[2] L


é


onard C


é


line. The vibrational levels of ammonia.. [J].Spectrochimica Acta Part A:


Molecular and Biomolecular Spectroscopy,2002,58(4)



[3] Thompson M. The bilayer lipid membrane as a basis for a selective sensor for


ammonia.. [J].Talanta,1983,30(12)



[4] Kretschmer Robert. Mechanistic aspects and elementary steps of N-H bond activation


of ammonia and C-N coupling induced by gas-phase ions: a combined


experimental/computational exercise.. [J].Chemistry: A European Journal,2011,18(1)



[5] Vinogradoff V. Acetaldehyde solid state reactivity at low temperature: formation of the


acetaldehyde ammonia trimer.. [J].The Journal of Physical Chemistry Part A: Molecules,


Spectroscopy, Kinetics, Environment and General Theory,2012,116(9)



[6] Jetzki Martin. Vibrational delocalization in ammonia aerosol particles.. [J].The Journal


of Chemical Physics,2004,120(24)



[7] Thompson Helen. Structural studies of ammonia and metallic lithium-ammonia


solutions.. [J].American Chemical Society. Journal,2003,125(9)



[8] Amaro Rommie. Developing an energy landscape for the novel function of a


(beta/alpha)8 barrel: ammonia conduction through HisF.. [J].PROCEEDINGS OF THE


NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF


AMERICA,2003,100(13)



[9] Bozoki Zoltan. Near-infrared diode laser based spectroscopic detection of ammonia: a


comparative study of photoacoustic and direct optical absorption methods.. [J].Applied


Spectroscopy,2002,56(6)



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air.. [J].Scandinavian Journal of Work, Environment & Health,1984,10(3)



[11] Rodger M R. Enzymic fluorometric assay of plasma ammonia with a centrifugal


analyzer.. [J].Clinical Chemistry (Washington, DC),1984,30(10)



[12] Svensson G. Rapid determination of ammonia in whole blood and plasma using flow


injection analysis.. [J].Clinica Chimica Acta,1982,119(1-2)



[13] Danielson N D. Fluorometric determination of hydrazine and ammonia separately or


in mixtures.. [J].Talanta,1982,29(5)



[14] Nikolelis D P. Potentiometric determination of certain alpha- aminohydroxy


compounds by using an ammonia gas-sensing electrode.. [J].Talanta,1982,29(11 Pt 1)



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amino acids isolated from biological material].. [J].Voprosy medit?sinsko?


khimii,1981,27(5)



[16] Poppe L


á


szl< /p>


ó


. Preparation of unnatural amino acids with ammonia-lyases and


2,3-aminomutases.. [J].Methods in Molecular Biology,2011,794



[17] W?


rml?


nder S. Imino proton exchange in DNA catalyzed by ammonia and


trimethylamine: evidence for a secondary long-lived open state of the base


pair.. [J].Biochemistry,2000,39(3)



[18] Cermak R. Influence of ammonia on sodium absorption in rat proximal


colon.. [J].Pfluegers Archiv,2000,440(4)



[19] Lv Yuan-Yuan. [Preparation of a zinc porphyrinated nanofibrous membrane and its


ammonia sensing property].. [J].Zhejiang Daxue Xuebao (Yixue Ban),2012,41(3)



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biosynthesis in liver.. [J].The Journal of Nutrition,1984,114(3)


-accuracy continuous airborne measurements of


greenhouse gases (CO2 and


CH4) using the cavity ring- down


spectroscopy (CRDS) technique


作者:


H. Chen ,


J. Winderlich ,


C. Gerbig ,


A. Hoefer ,


C. W. Rella ,


E. R.


Crosson ,


A. D. Van Pelt ,


J. Steinbach ,


O. Kolle ,


V. Beck ,


B. C. Daube ,


E. W.


Gottlieb ,


V. Y. Chow ,


G. W. Santoni ,


S. C. Wofsy




刊名:


Atmospheric Measurement Techniques, 2010, Vol.3 (2), pp.375



来源数据库:


DOAJ


期刊

< br>


原始语种摘要:


High-accuracy continuous measurements of greenhouse gases (CO


2


and


CH


4


) during the BARCA (Balan?


o Atmosf


é


rico Regional de Carbono na Amaz?


nia) phase


B campaign in Brazil in May 2009 were accomplished using a newly available analyzer


based on the cavity ring-down spectroscopy (CRDS) technique. This analyzer was flown


without a drying system or any in- flight calibration gases. Water vapor corrections


associated with dilution and pressure- broadening effects for CO


2


and CH


4


were derived


from laboratory experiments employing measurements of water vapor by the CRDS


analyzer. Before the campaign, the stability of the analyzer was assessed by laboratory


tests under simulated flight conditions. During the campaign, a comparison of CO


2


measurements between the CRDS analyzer and a nondispersive infrared (NDIR)


analyzer on board the same aircraft showed a mean difference of 0.22


±


0.09 ppm for all


flights over the Amazon rain forest. At the end of the campaign, CO


2


concentrations of the


synthetic calibration gases used by the NDIR analyzer were determined by the CRDS


analyzer. After correcting for the isotope and the pressure-broadening effects that resulted


from changes of the composition of synthetic vs. ambient air, and applying those


concentrations as calibrated values of the calibration gases to reprocess the CO


2



measurements made by the NDIR, the mean difference between the CRDS and the NDIR


during BARCA was reduced to 0.05


±


0.09 ppm, with the mean standard deviation of 0.23


±


0.05 ppm. The results clearly show that the CRDS is sufficiently stable to be used in


flight without drying the air or calibrating in flight and the water corrections are fully


adequate for high-accuracy continuous airborne measurements of CO


2


and CH


4


.



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Biology,2001,163



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is?


nen Jouni. On-line monitoring of solvent emission rates using an open path FTIR


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VACUUMS SURFACES AND FILMS,2001



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Box type energy analyzer: Function of the energy analyzer in the partial pressure


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chemiluminescence analyser. [J].Analytica Chimica Acta,2002,461


te measurements of carbon monoxide in humid


air using the cavity ring-down spectroscopy (CRDS)


technique


作者:


H. Chen ,


A. Karion ,


C. W. Rella ,


J. Winderlich ,


C. Gerbig ,


A. Filges ,


T.


Newberger ,


C. Sweeney ,


P. P. Tans



作者单位:



NOAA Earth System Research Laboratory, Boulder, CO 80305,


USA;;Cooperative Institute for Research in Environmental Sciences, University of


Colorado, Boulder, CO, USA;;Picarro, Inc., Santa Clara, CA, USA;;Max Planck Institute


for Chemistry, Mainz, Germany;;Max Planck Institute for Biogeochemistry, Jena,


Germany



刊名:


Atmospheric Measurement Techniques, 2013, Vol.6 (4), pp.1031-1040



来源数据库:

Copernicus


期刊



DO I



10.5194/amt-6-1031-2013



原始语种摘要:


Accurate measurements of carbon monoxide (CO) in humid air have been


madeusing the cavity ring- down spectroscopy (CRDS) technique. The measurementsof


CO mole fractions are determined from the strength of its spectralabsorption in the


near-infrared region (~1.57


μ


m) afterremoving interferences from adjacent carbon


dioxide (CO


2


) and watervapor (H


2


O) absorption lines. Water correction functions that


accountfor the dilution and pressure- broadening effects as well as absorption


lineinterferences from adjacent CO


2


and H


2


O lines have been derivedfor CO


2


mole


fractions between 360



390 ppm and for reported H


2


Omole fractions between 0



4%.


The line interference corrections areindependent of CO mole fractions. The dependence


of the... line interferencecorrection on CO


2


abundance is estimated to be approximately


?


0.3 ppb/100 ppmCO


2


for dry mole fractions of CO. Comparisons of watercorrection


functions from different analyzers of the same type showsignificant differences, making it


necessary to perform instrument- specificwater tests for each individual analyzer. The


CRDS analyzer was flown on anaircraft in Alaska from April to November in 2011, and the


accuracy of theCO measurements by the CRDS analyzer has been validated against


discreteNOAA/ESRL flask sample measurements made on board the same aircraft, with


amean difference between integrated in situ and flask measurements of


?


0.6 ppb and a


standard deviation of 2.8 ppb. Preliminary testing of CRDSinstrumentation that employs


improved spectroscopic model functions forCO


2


, H


2


O, and CO to fit the raw spectral data


(available since thebeginning of 2012) indicates a smaller water vapor dependence than


themodels discussed here, but more work is necessary to fully validate theperformance.


The CRDS technique provides an accurate and low- maintenancemethod of monitoring


the atmospheric dry mole fractions of CO in humid airstreams.



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ü


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Radiotherapia,1984,25(3)


-


-


-


-


-


-


-


-



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