API PUBL 309-1992 Current Status and Research Needs Related to Biogenic Hydrocarbons《现状与研究需求相关的生源烃》.pdf
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1、API PUBL*309 92 W 0732290 0529644 2T2 = CURRENTSTATUSANDRESEARCH NEEDS RELATED TO BIOGENIC HYDROCARBONS HEALTH AND ENVIRONMENTAL AFFAIRS API PUBLICATION NUMBER 309 JUNE 1992 American Petroleum Institute 1220 L Street. Northwest 11 Washington: D.C. 20005 API PUBL+309 92 = 0732290 0527645 139 = CURREN
2、TSTATUSANDRESEARCHNEEDS RELATED TO BIOGENIC HYDROCARBONS HEALTH AND ENVIRONMENTAL AFFAIRS DEPARTMENT API PUBLICATION NUMBER 309 JUNE 1992 PREPARED BY: INDACO AIR QUALITY SERVICES, INC. RESEARCH ANDTECHNOLOGYPARK 1345 TERREVIEW DRIVE PULLMAN, WA 99163 American Petroleum Institute API PUBL+309 92 0732
3、290 0529646 075 FOREWORD API PUBLICATIONS NECESSARILY ADDRESS PROBLEMS OF A GENERAL NATURE. WITH RESPECT TO PARTICULAR CIRCUMSTANCES, LOCAL, STATE, AND FEDERAL LAWS AND REGULATIONS SHOULD BE REVIEWED. API IS NOT U“G TO MEET THE DUTIES OFEMPLOm, MANUFAC- TURERS, OR SUPPLIERS To WARN AND PROPERLY TRAI
4、N AND EQUIP THEIR EMPLOYEES, AND OTHERS EXPOSED, CONCERNING HEALTH AND SAFETY RISKS AND PRECAUTIONS, NOR UNDERTmG THEIR OBLIGATIONS UNDER LOCAL, STATE, OR FEDERAL LAWS. NOTHING CONTAINED IN ANY API PUBLICATION IS To BE CONSTRUED AS GRANTING ANY RIGHT, BY IMPLICATZON OR OTHERWISE, FOR THE MANU- FACTU
5、RE, SALE, OR USE OF ANY METHOD, APPARATUS, OR PRODUCT COV- ERED BY LETTERS PAmNT. NEITHER SHOULD ANYTHING CONTAINED IN THE PUBLICATION BE CONSTRUED AS INSURING ANYONE AGAINSTLIABIL- lTY FOR INFRINGEMEN“ OF LETTERS PAm. API PUBL*309 92 O732290 O529647 TO1 Executive Summary 1. O Literature Compilation
6、 11 TABLE OF CONTENTS 1.1 Introduction 1.2 Methods: Literature Sources and Data Bases 1.3 Overview of Biogenic Emissions Measurements 1.3.1 Vegetation Species, Identified Compounds, and Emission Rates 1.3.2 Emission Patterns and Environmental Effects 1.4 Ambient Biogenic VOC Concentration Measuremen
7、ts 1.5 Biogenic Emission Inventones 1.6 Atmospheric Chemistry of Biogenic VOCs 1.7 Current Biogenic Studies Critical Review of the Literature 2.1 Introduction 2.0 2.2 Emission Inventory Systems 2.3 Emission Rate Measurements 2.4 Atmospheric Chemistry 2.5 Summary of the SOW-EE Biogenic Emission Works
8、hop 1v 2 10 12 13 14 18 21 21 26 29 31 API PUBL*Pinene Mpne 3-Carene 1 -Pheilandrene B -Phellandrene CI -Terpinene -Terpinene y -Tapinene Limonene Terpinolene knchone ujone . Camphor 1,8-Cineol PCymene Menthane .6 .5 I,11 b10,15 I- 17 r,8*,9-10 ?,lo, 13-17 3,(7,8,11,12,14)* 9,10,13,15,17) * * , 16 2
9、,12 7-17 7-10,12 j,10,12 3,(7,9,10,12)*,*(8,11)* 12,13,15,17 ,( 14,16) * 13-17 3,7-11,15 7-13,14*,15-17 7*,8-10,12-15,16*, 17 3,8-11 8-1 1,14 8-10,17 3,8-10,13- 15 9.1 3-1 5,17 3,7- 17 9-17 3,8,14 16* 16* 8 7-17 #1. Bay-ieavedwillow; 2. Aspen; 3. Balsam poplar; 4. European oak; 5. European birch; 6.
10、 Sorb; 7. Eutopean larch; 8. European e, 9. Scots pine; 10. Siberian pine; 11. Silver fx; 12. Common juniper, 13. Zeravshan juniF, 14. Pend 16. Nwthern white Trainer et al., 1987; Chameides et al., 1988). Methods have ranged from the use of simple box models to Lagrangian chemical reactor models to
11、fully three dimensional Eulerian grid models. The influence of biogenic hydrocarbons in the Regional Acid Deposition Model (RADM) (Chang et al., 1988) and the Regional Oxidant Model (ROM) (Roselle and Schere, 1990) have been of parbcular interest. Similar concern for the importance of biogenic VOC s
12、 in formation of CO and tropospheric ozone on a global basis has been addressed through tropospheric chemical models (Lopez et al., 1989; Jacob and Wofsy, 1988; and Atherton and Penner, 1990). Lin et ai. (1988) employed a photochemical box model to investigate the nonlinear dependence of ozone forma
13、tion upon precursor concentrations. The results indicated that the composition of hydrocarbons, the ratio of VOC/NO, and the background concentrations of biogenic VOCs, CO, and CHq all are important in determining the nonlinearity of ozone formation with respect to NOx loss. Atherton and Penner (199
14、0) performed a similar study using a photochemical box model to investigate the importance of odd nitrogen species beyond those normally included in models: NO, Ne, PAN, “03, and NO3- (particulate nitrate). The shortfall of odd nitrogen was defmed as the ratio of other nitrogen species to the sum of
15、 the above compounds. For cases with biogenic VOCs, the nitrogen shortfall was 0.25 with background isoprene and pinene emissions and 0.45 with high pinene emissions. In comparison, the shortfall varied between 0.02 to 0.33 for various urban simulations. The implications from this work are that inco
16、rrect specification of odd nitrogen chemistry may be a significant source of error in chemical modeling studies of biogenic emissions. Jacob and Wofsy (1988) compared photochemical model predictions against isoprene and ozone concentrations measured over the Amazon forest. The results were in good a
17、greement with observations and showed that biogenic isoprene and NOx can supply most of the ozone observed in the boundary layer. In agreement with the suggestion made previously API PUBL+30 92 m 0732290 0529bb8 73b m 18 about the dry deposition of isoprene at night, the model comparison with observ
18、ations indicated the importance of dry deposition. Lopez et al. (1989) modeled the vertical profiles of photochemical species in a Lagrangian air parcel moving over homogeneous land cover. For cases with terpene emissions into an air mass with low NOx, ozone was depleted, while emissions into an air
19、 mass with high NOx caused an enhancement of ozone. The degree of change was larger for alpha-pinene emissions than for isoprene emissions. The effects of biogenic emissions upon the urban plume of London was investigated by MacKenzie et al. (1991) using a detailed photochemical expanding air parcel
20、 model. The results seemed quite similar to the early work by Lunnann et al. (1984) since the predicted effect of adding biogenic emissions increased the ozone concentrations by about 8 ppb. The sum of these modeling studies have provided insight into the role of biogenic VOCs in atmospheric chemist
21、ry. However, until a better understanding of the biogenic emission fluxes is obtained, the identity of important biogenic species is clarified, and more complete chemical mechanisms are compiled, the modeling results provide an incomplete and uncertain picture of biogenic VOCs in the atmosphere. 1.7
22、 CURRENT BIOGENIC STUDIES The NOAA ROSE (Rural Oxidants in a southeastern Environment) program recently completed a 2 month field study in an Alabama pine plantation designed to measure precursors and products related to ozone formation in the Southeastern U.S. The programs included sampling of biog
23、enic emissions, measurements of VOC reactant and product concentrations, and performance of vertical prole tracer flux studies. Similar work was performed in the predecessor to ROSE which was conducted in Scotia, Pennsylvania, in 1988 (see Martin et al., 1991). The unique feature of the ROSE program
24、 is the combined measurement of essentially all carbon and nitrogen species thought to be important in ozone air chemistry along with detailed boundary layer meteorological measurements and vertid transport tracer studies. In ROSE 1990, this included diurnal sampling of VOC emissions using a vegetat
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