The relative merits of open- and closed-path analysers for measurement of eddy fluxes

被引:159
作者
Leuning, R [1 ]
Judd, MJ [1 ]
机构
[1] HORTICULTURE & FOOD RES INST, KERIKERI RES CTR, KERIKERI, NEW ZEALAND
关键词
eddy covariance; trace gas fluxes;
D O I
10.1111/j.1365-2486.1996.tb00076.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Theoretical and practical aspects of measuring eddy fluxes of trace gases using open- and closed-path analysers are presented. Trace gas fluxes measured with an open-path analyser require the concurrent measurement of sensible and latent heat fluxes to correct for density fluctuations in trace gas concentration caused by these fluxes. A closed-path analyser eliminates the corrections due to sensible heat flux, but not for water vapour, provided temperature fluctuations are completely removed without significantly reducing fluctuations in the trace gas mixing ratio. Theory for the design of heat exchangers and for the attenuation of concentration fluctuations during air now through tubes is used to provide design criteria for closed-path systems. Spectral transfer functions are used to estimate flux losses caused by now through the sampling tube and gas analyser. Other factors considered include cross-sensitivity of infrared COP analysers to water vapour, and deterioration of system performance caused by contaminants on the walls of sampling tubes, Of two open-path, infrared CO2 analysers tested, one showed a strong interaction between CO2 and water vapour, while the other showed little sensitivity to the presence of water vapour, other than caused by dilution. A commercial closed-path CO2 analyser also showed little cross-sensitivity to water vapour. Compared to results for a clean sampling tube, the spectral bandwidth for water vapour fluctuations decreased significantly after several weeks of sampling. No such deterioration in bandwidth was observed for CO2. These findings are attributed to differential adsorption/desorption of water vapour by dust or salt on the tubing walls. Rain and dust must be removed from open-path analysers to obtain satisfactory measurements, Careful. system design and maintenance is required for both open- and closed-path systems to ensure satisfactory long-term measurement of trace gas fluxes. With these precautions, both approaches will provide satisfactory flux measurements.
引用
收藏
页码:241 / 253
页数:13
相关论文
共 25 条
[1]   AN OPEN PATH, FAST RESPONSE INFRARED-ABSORPTION GAS ANALYZER FOR H2O AND CO2 [J].
AUBLE, DL ;
MEYERS, TP .
BOUNDARY-LAYER METEOROLOGY, 1992, 59 (03) :243-256
[2]   CARBON-DIOXIDE AND LATENT-HEAT FLUX MEASUREMENTS IN A WINDBREAK-SHELTERED ORCHARD [J].
JUDD, MJ ;
PRENDERGAST, PT ;
MCANENEY, KJ .
AGRICULTURAL AND FOREST METEOROLOGY, 1993, 66 (3-4) :193-210
[3]  
KAIMAL JC, 1972, Q J ROY METEOR SOC, V98, P563, DOI 10.1002/qj.49709841707
[4]   MINIMIZING FLOW DISTORTION ERRORS IN A SONIC ANEMOMETER [J].
KAIMAL, JC ;
GAYNOR, JE ;
ZIMMERMAN, HA ;
ZIMMERMAN, GA .
BOUNDARY-LAYER METEOROLOGY, 1990, 53 (1-2) :103-115
[5]  
Kays W. M., 1980, CONVECTIVE HEAT MASS
[6]   DETERMINATION OF HEAT AND WATER-VAPOR FLUXES ABOVE A SPRUCE FOREST BY EDDY-CORRELATION [J].
LAUBACH, J ;
RASCHENDORFER, M ;
KREILEIN, H ;
GRAVENHORST, G .
AGRICULTURAL AND FOREST METEOROLOGY, 1994, 71 (3-4) :373-401
[7]   COMPARISON OF FLUX MEASUREMENTS WITH OPEN-PATH AND CLOSED-PATH GAS ANALYZERS ABOVE AN AGRICULTURAL FIELD AND A FOREST FLOOR [J].
LEE, XH ;
BLACK, TA ;
NOVAK, MD .
BOUNDARY-LAYER METEOROLOGY, 1994, 67 (1-2) :195-202
[8]   THE ATTENUATION OF FLUCTUATIONS IN SCALAR CONCENTRATIONS THROUGH SAMPLING TUBES [J].
LENSCHOW, DH ;
RAUPACH, MR .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1991, 96 (D8) :15259-15268
[9]   EFFECTS OF HEAT AND WATER-VAPOR TRANSPORT ON EDDY COVARIANCE MEASUREMENT OF CO2 FLUXES [J].
LEUNING, R ;
DENMEAD, OT ;
LANG, ARG ;
OHTAKI, E .
BOUNDARY-LAYER METEOROLOGY, 1982, 23 (02) :209-222
[10]   EDDY-COVARIANCE CO2 FLUX MEASUREMENTS USING OPEN-PATH AND CLOSED-PATH CO2 ANALYZERS - CORRECTIONS FOR ANALYZER WATER-VAPOR SENSITIVITY AND DAMPING OF FLUCTUATIONS IN AIR SAMPLING TUBES [J].
LEUNING, R ;
MONCRIEFF, J .
BOUNDARY-LAYER METEOROLOGY, 1990, 53 (1-2) :63-76