-
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.
相似文献:
[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.
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é
r<
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?
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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.
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é
onard
C
é
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á
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ammonia on orotic acid and urea
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
.
相似文献:
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Molecular
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is?
nen
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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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