LGR是世界上激光痕量氣體和穩(wěn)定性同位素分析技術(shù)的領(lǐng)導(dǎo)者。隨著OA-ICOS技術(shù)日臻完善，為研究者帶來了更大的方便，在以往很難測量的領(lǐng)域提供了測量的可能。

      因?yàn)閮x器性能優(yōu)良，數(shù)據(jù)穩(wěn)定，越來越得到用戶的認(rèn)可，目前全世界已有400多臺(tái)分析儀在為人類更好的服務(wù)。儀器廣泛應(yīng)用在碳水通量測定，大氣痕量氣體變化的測量，水文同位素研究，CO₂/H₂O穩(wěn)定性同位素廓線測量和土壤CH₄通量等方向的研究。在近幾年在國際權(quán)威刊物如Nature、Science上發(fā)表了大量的文獻(xiàn)；同時(shí)，很多研究者對(duì)LGR激光分析儀做了性能等方面的測試，結(jié)果表明分析儀精度高、穩(wěn)定性好，是目前世界上最先進(jìn)的激光分析儀。現(xiàn)將部分文獻(xiàn)目錄列出，共各位用戶參考。

 

Los Gatos 參考文獻(xiàn)：

[1] Natalia Shakhova, Igor Semiletov, Anatoly Salyuk, Vladimir Yusupov, Denis Kosmach, Örjan Gustafsson.

Extensive Methane Venting to the Atmosphere from Sediments of the East Siberian Arctic Shelf. Science, 2010, 327: 1246-1250.

[2] D. R. Bowling, J. B. Miller, M. E. Rhodes, S. P. Burns, R. K. Monson, D. Baer. Soil, plant, and transport influences on methane in a subalpine forest under high ultraviolet irradiance. Biogeosciences, 2009,

6: 1311-1324.

[3] P. Sturm, A. Knohl. Water vapor δ²H and δ¹⁸O measurements using off-axis integrated cavity output spectroscopy. Atmospheric Measurement Techniques Discussions, 2009, 2: 2055–2085.

[4] Christopher T. et al., The influence of environmental water on the hydrogen stable isotope ratio in aquatic consumers. Oecologia, 2009, 161: 313-324.

[5] D. Penna, B. Stenni, M. S. Wrede. et al.. On the reproducibility and repeatability of laser absorption spectroscopy measurements for δ²H and δ¹⁸O isotopic analysis. Hydrology and Earth System Sciences Discussions, 2010, 7: 2975–3014.

[6] G. Lis, L. I. Wassenaar, M. J. Hendry. High-Precision Laser Spectroscopy D/H and ¹⁸O/¹⁶O Measurements of Microliter Natural Water Samples. Analytical Chemistry, 2007.

[7] Mikhail Mastepanov, Charlotte Sigsgaard, Edward J. Dlugokencky. et al.. Nature, 2008, 456: 628-631.

[8] Hideki TOMITA, Kenichi WATANABE, Yu TAKIGUCHI, Jun KAWARABAYASHI, Tetsuo IGUCHI. Rapid-Swept CW Cavity Ring-down Laser Spectroscopy for Carbon Isotope Analysis. NUCLEAR SCIENCE and TECHNOLOGY, 2006, 43(4): 311-315.

[9] Irmantas Kakaras. Developing the Method For Collecting Water Vapor From the Atmosphere. Niels Bohr Institute University of Copenhagen, 2009.

[10] Joshua B. Paul, Larry Lapson, James G. Anderson. Ultrasensitive absorption spectroscopy with a high-finesse optical cavity and off-axis alignment. APPLIED OPTICS, 2001, 40(27): 4904-4910.

[11] I. Vigano, H. van Weelden, R. Holzinger, F. Keppler, A. McLeod. Effect of UV radiation and temperature on the emission of methane from plant biomass and structural components. Biogeosciences, 2008, 5: 937–947.

[12] Lixin Wang, Kelly K. Caylor, Danilo Dragoni. On the calibration of continuous, high-precision δ¹⁸O and δ²H measurements using an off-axis integrated cavity output spectrometer. RAPID COMMUNICATIONS IN MASS SPECTROMETRY, 2009, 23: 530-536.

[13] Elena S. F. Berman, Manish Gupta, Chris Gabrielli, Tina Garland, Jeffrey J. McDonne. High-frequency field-deployable isotope analyzer for hydrological applications. WATER RESOURCES RESEARCH, 2009, 45: 1-7.

[14] Xinning Zhang, Aimee L. Gillespieb, Alex L. Sessionsa. Large D/H variations in bacterial lipids reflect central metabolic pathways. PNAS, 2009, 106(31): 12580-12586.

[15] D. Zona, W. C. Oechel, J. Kochendorfer, K. T. Paw U, A. N. Salyuk, P. C. Olivas, S. F. Oberbauer, D. A. Lipson. Methane fluxes during the initiation of a large-scale water table manipulation experiment in the Alaskan Arctic tundra. GLOBAL BIOGEOCHEMICAL CYCLES, 2009, 23, GB2013: 1-11.

[16] STEPHANIE. SHAW, FRANK M. MITLOEHNER, WENDI JACKSON..et al. Volatile Organic Compound

Emissions from Dairy Cows and Their Waste as Measured by Proton-Transfer-Reaction Mass Spectrometry. ENVIRON. SCI. 2007.

[17] D. M. D. Hendriks, A. J. Dolman, M. K. van der Molen, J. van Huissteden. A compact and stable eddy covariance set-up for methane measurements using off-axis integrated cavity output spectroscopy. Atmospheric Chemistry and Physics. 2008, 8: 431-443.

[18] L.I. Wassenaar, S.L. Van Wilgenburg, K. Larson, K.A. Hobson. A groundwater isoscape (δD, δ¹⁸O) for Mexico. Geochemical Exploration, 2009, 102: 123–136.

[19] C. J. P. P. Smeets, R. Holzinger, I. Vigano, A. H. Goldstein. Eddy covariance methane measurements

at a Ponderosa pine plantation in California. Atmospheric Chemistry and Physics Disscusions, 2009, 9: 5201–5229.

[20] L. I. WASSENAAR, M. J. HENDRY, V. L. CHOSTNER, G. P. LIS. High Resolution Pore Water δ²H and δ¹⁸O Measurements by H₂O(liquid)-H₂O(vapor) Equilibration Laser Spectroscopy. ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2008.

[21] Steve W. Lyon, Sharon L. E. Desilets, Peter A. Troch. A tale of two isotopes: differences in hydrograph separation for a runoff event when using δD versus δ¹⁸O. HYDROLOGICAL PROCESSES, 2009, 23: 2095-2101.

[22] Patrick D. Broxton, Peter A. Troch, Steve W. Lyon. On the role of aspect to quantify water transit times

in small mountainous catchments. WATER RESOURCES RESEARCH, 2009, 45, W08427: 1-15.

[23] M. Barthel, P. Sturm, L. Gentsch, A. Knohl. Technical Note: A combined soil/canopy chamber system for tracing δ¹³C in soil respiration after a ¹³CO₂ canopy pulse labelling. Biogeosciences Discussions, 2010, 7:1603-1631.

[24] Anna K. Henderson1, Bryan Nolan Shuman. Hydrogen and oxygen isotopic compositions of lake water

in the western United States. GSA Bulletin, 2009, 121(7-8): 1179–1189.

[25] Stephen D. Sebestyen, Elizabeth W. Boyer, James B. Shanley, Carol Kendall, Daniel H. Doctor, George R. Aiken, Nobuhito Ohte. Sources, transformations, and hydrological processes that control stream nitrate and dissolved organic matter concentrations during snowmelt in an upland forest. WATER RESOURCES RESEARCH, 2008, 44, W12410: 1-14.

[26] T. Vogel, M. Sanda, J. Dusek, M. Dohnal, J.Votrubova. Using Oxygen-18 to Study the Role of Preferential Flow in the Formation of Hillslope Runoff. Faculty of Civil Engineering, 2010, 9: 252-259.

[27] Peter E. Sauer, Arndt Schimmelmann, Alex L. Sessions, Katarina Topalov. Simplified batch equilibration for D/H determination of non-exchangeable hydrogen in solid organic material. RAPID COMMUNICATIONS IN MASS SPECTROMETRY. 2009, 23: 949-956.