###
气象:2026,52(10):1232-1245
本文二维码信息
码上扫一扫!
泰山地区降水酸度和离子成分的长期变化特征
贾小芳,汤洁,张本志,陈怡羽,尹祥坤,刘明
(中国气象局气象探测中心,北京 100081; 临近空间环境特性及效应全国重点实验室,北京 100081; 中国气象局气象探测工程技术研究中心,北京 100081; 泰山国家基准气候站,山东泰安 271000; 泰安农业气象试验站,山东泰安 271000)
Long-Term Variation Characteristics of Precipitation Acidity and Ion Composition in the Mount Taishan Area
JIA Xiaofang, TANG Jie, ZHANG Benzhi, CHEN Yiyu, YIN Xiangkun, LIU Ming
(CMA Meteorological Observation Centre, Beijing 100081; State Key Laboratory of Environment Characteristics and Effects for Near-Space, Beijing 100081; CMA Research Centre of Meteorological Observation Engineering Technology, Beijing 100081; Taishan National Reference Climatological Station, Shandong, Tai’an 271000; Tai’an Agricultural Meteorological Experiment, Shandong, Tai’an 271000)
摘要
图/表
参考文献
相似文献
本文已被:浏览 62次   下载 29次
投稿时间:2025-11-14    修订日期:2026-06-23
中文摘要: 为深入了解我国典型北方地区酸雨污染的新变化,本文在对1993—2021年泰山站和2007—2021年泰安站降水pH值和电导率资料统计分析的基础上,进一步利用2018年5月至2019年4月在2个站同步开展的降水化学加强观测资料,分析云下过程和远距离输送对泰山地区酸性降水的贡献,并结合早期研究结果,探讨近年来泰山地区酸雨变化的新形势及其成因。结果表明,1993—2021年泰山站降水pH年均值在4.36~6.47,2007—2021年泰安站在4.73~6.66。泰安站在较强云下冲刷作用下,碱性污染物中和作用更强,降水酸性较泰山站显著降低。1993—2021年,泰山站降水酸性经历了减弱—增强—较缓的减弱—相对平稳或轻微增强的阶段性变化,碱性污染物中和作用在酸雨污染长期变化趋势中呈现重要影响。泰山地区降水中SO2-4离子浓度约下降到2004—2008年的50%,泰山站SO2-4/NO-3离子浓度平均比值由2.84~3.98下降到1.21,降水酸化的污染物来源已经由SO2主导转变为SO2、NOx并重。泰山站和泰安站降水中NO-3离子浓度约分别增加了47%和20%,与同时段全国和山东省NOx排放量呈下降趋势的结果相反。后向轨迹气团分析显示泰山站降水特性主要受山东、京津冀及内蒙古等周边省份污染排放影响。
Abstract:To understand the new variation features of acid rain pollution deeply in typical northern regions of China, the precipitation pH value and conductivity at Taishan Station during 1993-2021 and Tai’an Station during 2007-2021 are analyzed. On this basis, synchronous intensive observation data of precipitation chemistry which was performed from May 2018 to April 2019 are analyzed to get the contributions of below-cloud processes and long-distance transport to acid precipitation in the Mount Taishan Area. Combined with the results of earlier studies, the new situation and causes of acid rain in the Mount Taishan Area in recent years are investigated. The study results show that the annual precipitation pH value at Taishan Station varied in the range from 4.36 to 6.47 during 1993-2021, while that at Tai’an Station ranged from 4.73 to 6.66 during 2007-2021. Owing to the strong below-cloud scavenging effect at Tai’an Station, the neutralization effect of alkaline pollutants was more pronounced, leading to a significant reduction in precipitation acidity compared with that at Taishan Station. During 1993-2021, the precipitation acidity at Taishan Station experienced a phased variation process, i.e., weakening, intensifying, moderately weakening, and relatively stabilizing or slightly intensifying. The neutralization effect of alkaline pollutants exerted an important influence on the long-term variation trend of acid rain pollution. The concentration of SO2-4 in precipitation in the Mount Taishan Area decreased to approximately 50% of that from 2004 to 2008 and the SO2-4/NO-3 at Taishan Station dropped from 2.84-3.98 to 1.21, which indicates that the source of acid rain had shifted from SO2 dominated to SO2 and NOx dominated. It is noteworthy that the NO-3 concentration in precipitation at Taishan Station and Tai’an Station increased by approximately 47% and 20%, respectively, which was contrary to the decreasing trend of NOx emissions in the whole China and Shandong Province during the same period. Backward trajectory air mass analysis shows that the precipitation characteristics at Taishan Station were mainly affected by the pollution emissions from Shandong Province and its surrounding provinces, including the Beijing-Tianjin-Hebei Region and Inner Mongolia.
文章编号:     中图分类号:    文献标志码:
基金项目:国家重点研发计划(2016YFC0200506)和中国气象局大气化学重点开放实验室2024年开放课题(2024B03)共同资助
引用文本:
贾小芳,汤洁,张本志,陈怡羽,尹祥坤,刘明,2026.泰山地区降水酸度和离子成分的长期变化特征[J].气象,52(10):1232-1245.
JIA Xiaofang,TANG Jie,ZHANG Benzhi,CHEN Yiyu,YIN Xiangkun,LIU Ming,2026.Long-Term Variation Characteristics of Precipitation Acidity and Ion Composition in the Mount Taishan Area[J].Meteor Mon,52(10):1232-1245.