INFLUENCE OF SEA SALT AEROSOLS AND LONG-RANGE TRANSPORT ON PRECIPITATION CHEMISTRY AT EL-VERDE, PUERTO-RICO

被引:86
作者
MCDOWELL, WH
SANCHEZ, CG
ASBURY, CE
PEREZ, CRR
机构
[1] UNIV PUERTO RICO,CTR ENERGY & ENVIRONM RES,DIV TERRESTRIAL ECOL,GPO BOX 3682,SAN JUAN,PR 00936
[2] SUNY COLL OSWEGO,RES CTR,OSWEGO,NY 13126
[3] US EPA,DIV EMERGENCY & REMEDIAL RESPONSE,NEW YORK,NY 10278
来源
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS | 1990年 / 24卷 / 11期
关键词
bulk deposition; excess sulfate; rain forest; Saharam dust; Tropical precipitation chemistry; wet deposition;
D O I
10.1016/0960-1686(90)90168-M
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The chemistry of bulk precipitation was measured from November 1983 to September 1987 at El Verde in the Luquillo Experimental Forest, Puerto Rico. Wet-only precipitation was also analyzed as part of the National Atmospheric Deposition Program from 1984 to 1987. Volume-weighted mean pH was 5.14 in bulk precipitation and 5.12 in wet precipitation. Concentrations of most species were correlated negatively with weekly rainfall. Sea salt aerosols contributed most of the Na+, Cl-, Mg2+ and K+ found in wet and bulk precipitation; sulfate and calcium, however, were derived primarily from non-sea salt sources. Due to the high rainfall (3.4 m annually during the study period) and close proximity of the study site to the ocean, deposition rates of the major cations and anions were high relative to many other tropical sites. Precipitation chemistry at El Verde appears to be affected by several factors. During summer, Saharan dusts contribute a significant portion of the excess Ca2+, K+ and Mg2+. During winter months, cold fronts may transport SO42- and NO3- from North America and the western part of Puerto Rico to the sampling site. © 1990.
引用
收藏
页码:2813 / 2821
页数:9
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