湖北省旅游景区大气负氧离子浓度分布特征以及气象条件的影响

doi:10.11870/cjlyzyyhj201602018

长江流域资源与环境 >> 2017, Vol. 26 >> Issue (02): 314-323.doi: 10.11870/cjlyzyyhj201602018

•　生态环境　• 上一篇

湖北省旅游景区大气负氧离子浓度分布特征以及气象条件的影响

谭静¹, 陈正洪¹, 罗学荣¹, 阳威¹, 舒斯¹, 徐金华²

1. 湖北省气象服务中心, 湖北武汉 430205;
2. 湖北省旅游发展委员会, 湖北武汉 430077

收稿日期:2016-09-12 修回日期:2016-11-07 出版日期:2017-02-20
作者简介:谭静(1990~),女,硕士研究生,主要从事交通旅游专业气象服务研究.E-mail:jmjwyb@163.com
基金资助:
2017年湖北省气象局科技发展基金项目（2017Q10）

DISTRIBUTION CHARACTERISTICS OF AIR NEGATIVE OXYGEN ION CONCENTRATION AND THE INFLUENCE OF METEOROLOGICAL CONDITIONS IN TOURIST ATTRACTIONS IN HUBEI PROVINCE

TAN Jing¹, CHEN Zheng-hong¹, LUO Xue-rong¹, YANG Wei¹, SHU Si¹, XU Jin-hua²

1. Hubei Meteorological Service Center, Wuhan 430205, China;
2. Hubei Tourism Development Committee, Wuhan 430077, China

Received:2016-09-12 Revised:2016-11-07 Online:2017-02-20
Supported by:
Researh Project of Science and Technology Development Fund of Hubei Meteorogical Bureau in 2017 (2017Q10)

摘要/Abstract

摘要： 通过利用湖北省气象服务中心在全省27个旅游景区内建设的30个大气负氧离子自动监测站数据，对湖北省旅游景区大气负氧离子浓度分布特征及气象条件对负氧离子浓度的影响进行了分析。研究表明：湖北省旅游景区的大气负氧离子资源十分丰富，西部山区高于东部平原地区，整体呈现从东向西、从北向南逐渐增加的趋势，鄂西南地区为全省大气负氧离子最为丰富的地区，负氧离子浓度夏季最高，冬季最低，秋季略大于春季。从3月开始，负氧离子浓度逐月增加，至8月达到最大值，后又逐渐减小。凌晨和上午的负氧离子浓度要大于下午和晚上，夜间呈逐渐上升的趋势。大气负氧离子浓度晴天最大，阴天小于晴天，而雾霾天和小雨天负氧离子浓度均较小；中雨以上降水、闪电活动与负氧离子浓度呈正相关。

关键词: 旅游景区, 负氧离子, 分布特征

Abstract: This paper takes advantage of data from 30 air negative oxygen ions automatic stations in the 27 tourist attractions in Hubei Province constructed by Hubei Meteorological Service Center. We analyzed atmospheric negative oxygen ion concentration distribution characteristics and the influence of meteorological conditions to air negative oxygen ions. The study showed that the air negative oxygen is very rich in the tourist attractions of Hubei Province, being higher in the western mountainous area than in eastern plain area. The level increases gradually from east to west, from north to South, and the Southwest Hubei is area with most abundant negative oxygen ions. The concentration of negative oxygen ions is highest in summer, lowest in winter and slightly larger in autumn than in spring. From the beginning of March, the concentration of negative oxygen ions increased month by month, reached the maximum in August, and then decreased gradually. The concentration of negative oxygen ions in the morning is higher in the afternoon and evening, and gradually increased in the midnight. The air negative oxygen ion concentration is highest in sunny day, and lower in cloudy day rain days and haze days have lower negative oxygen ions. The moderate rainfall and lightning activity was positively correlated with the concentration of negative oxygen ions.

Key words: negative oxygen ion, tourist attractions, distribution characteristics

中图分类号:

谭静, 陈正洪, 罗学荣, 阳威, 舒斯, 徐金华. 湖北省旅游景区大气负氧离子浓度分布特征以及气象条件的影响[J]. 长江流域资源与环境, 2017, 26(02): 314-323.

TAN Jing, CHEN Zheng-hong, LUO Xue-rong, YANG Wei, SHU Si, XU Jin-hua. DISTRIBUTION CHARACTERISTICS OF AIR NEGATIVE OXYGEN ION CONCENTRATION AND THE INFLUENCE OF METEOROLOGICAL CONDITIONS IN TOURIST ATTRACTIONS IN HUBEI PROVINCE[J]. RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN, 2017, 26(02): 314-323.

参考文献

[1] 钟林生, 吴楚才, 肖笃宁. 森林旅游资源评价中的空气负离子研究[J]. 生态学杂志, 1998, 17(6):56-60.[ZHONG L S, WU C C, XIAO D N. Aeroanion researches in evaluation of forest recreation resources[J]. Chinese Journal of Ecology, 1998, 17(6):56-60.]
[2] 刘和俊. 安徽主要旅游景区空气负离子效应研究[D]. 合肥:安徽农业大学硕士学位论文, 2013.[LIU H J. The research on air anion effect of major tourist attractions in Anhui[D]. Hefei:Master Dissertation of Anhui Agricultural University, 2013.]
[3] 叶彩华, 王晓云, 郭文利. 空气中负离子浓度与气象条件关系初探[J]. 气象科技, 2000, 28(4):51-52.
[4] 冯鹏飞, 于新文, 张旭. 北京地区不同植被类型空气负离子浓度及其影响因素分析[J]. 生态环境学报, 2015, 24(5):818-824.[FENG P F, YU X W, ZHANG X. Variations in negative air ion concentrations associated with different vegetation types and influencing factors in Beijing[J]. Ecology and Environmental Sciences, 2015, 24(5):818-824.]
[5] 韦朝领, 王敬涛, 蒋跃林, 等. 合肥市不同生态功能区空气负离子浓度分布特征及其与气象因子的关系[J]. 应用生态学报, 2006, 17(11):2158-2162.[WEI C L, WANG J T, JIANG Y L, et al. Air negative charge ion concentration and its relationships with meteorological factors in different ecological functional zones of Hefei City[J]. Chinese Journal of Applied Ecology, 2006, 17(11):2158-2162.]
[6] 陈前江, 延军平. 1970年以来湖北省气候变化与旱涝灾害响应分析[J]. 江汉大学学报(自然科学版), 2015, 43(4):308-316.[CHEN Q J, YAN J P. Analysis on climatic change and responses to drought-flood disasters in Hubei from 1970[J]. Journal of Jianghan University (Natural Science Edition), 2015, 43(4):308-316.]
[7] 王学良, 余田野, 汪姿荷. 近52年湖北雷暴气候特征及其变化研究[C]//第31届中国气象学会年会. 北京:中国气象学会, 2015:1-15.[WANG X L, YU T Y, WANG Z H. A study on thunderstorms' climatic features and its variation in 52 years in Hubei[C]. Beijing:Chinese Meteorological Society, 2015:1-15.]
[8] 曹小雪, 黄建武, 揭毅. 近52年来武汉市气候变化特征分析[J]. 江西农业学报, 2014, 26(9):80-85, 89.[CAO X X, HUANG J W, JIE Y. Analysis of characteristics of climate changes in Wuhan City in recent 52 years[J]. Acta Agriculturae Jiangxi, 2014, 26(9):80-85, 89.]
[9] 吴楚材, 郑群明, 钟林生. 森林游憩区空气负离子水平的研究[J]. 林业科学, 2001, 37(5):76-81.[WU C C, ZHENG Q M, ZHONG L S. A study of the aero-anion concentration in forest recreation area[J]. Scientia Silvae Sinicae, 200137(5):75-81.]
[10] 穆丹, 梁英辉. 佳木斯绿地空气负离子浓度及其与气象因子的关系[J]. 应用生态学报, 2009, 20(8):2038-2041.[MU D, LIANG Y H. Air negative ion concentration and its relationships with meteorological factors in greenbelts of Jiamusi, Heilongjiang Province[J]. Chinese Journal of Applied Ecology, 2009, 20(8):2038-2041.]
[11] 吴甫成, 姚成胜, 郭建平, 等. 岳麓山空气负离子及空气质量变化研究[J]. 环境科学学报, 2006, 26(10):1737-1744.[WU F C, YAO C S, GUO J P, et al. Distribution of negative air ions and its relation to air quality of the Yuelu mountain[J]. Acta Scientiae Circumstantiae, 2006, 26(10):1737-1744.]
[12] 金琪, 严婧, 杨志彪, 等. 湖北春季大气负氧离子浓度分布特征及与环境因子的关系[J]. 气象科技, 2015, 43(4):728-733.[JIN Q, YAN J, YANG Z B, et al. Spatial-temporal characteristics of spring air negative oxygen ions and its relationship with environmental factors in Hubei[J]. Meteorological Science and Technology, 2015, 43(4):728-733.]
[13] 段炳奇. 空气离子及其与气象因子的相关研究[D]. 上海:上海师范大学硕士学位论文, 2007.
[14] 黄世成, 徐春阳, 周嘉陵. 城市和森林空气负离子浓度与气象环境关系的通径分析[J]. 气象, 2012, 38(11):1417-1422.[HUANG S C, XU C Y, ZHOU J L. Path analysis on negative air ion concentration and the meteorological environment in urban and forest zones[J]. Meteorological Monthly, 2012, 38(11):1417-1422.]

Metrics

Viewed

Full text

Abstract

Cited

Shared

Discussed

湖北省旅游景区大气负氧离子浓度分布特征以及气象条件的影响

DISTRIBUTION CHARACTERISTICS OF AIR NEGATIVE OXYGEN ION CONCENTRATION AND THE INFLUENCE OF METEOROLOGICAL CONDITIONS IN TOURIST ATTRACTIONS IN HUBEI PROVINCE

PDF (PC)

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 8

Metrics

推荐阅读 10

[1]	徐建霞, 彭刚志, 王建柱. 三峡库区香溪河消落带植被多样性及分布格局研究[J]. 长江流域资源与环境, 2015, 24(08): 1345-1350.
[2]	齐莉娜, 吴必虎, 俞曦. 基于中部崛起背景旅游景区发展战略研究[J]. 长江流域资源与环境, 2009, 18(8): 732-.
[3]	张翅鹏 \|刘丛强 \|吴攀\|汪福顺\|王宝利. 乌江中上游水库—河流体系夏秋季N、Si分布特征[J]. 长江流域资源与环境, 2009, 18(4): 331-.
[4]	吴成基,胡炜霞,. 旅游景区周边环境及范围界定[J]. 长江流域资源与环境, 2008, 17(3): 401-401.
[5]	苏春利, 王焰新. 墨水湖上覆水与沉积物间隙水中重金属的分布特征[J]. 长江流域资源与环境, 2008, 17(2): 285-285.
[6]	万红友,周生路,赵其国,廖启林,华明. 苏南经济快速发展区土壤有效态镉含量影响因素及分布特征[J]. 长江流域资源与环境, 2006, 15(2): 213-218.
[7]	唐将, 李勇, 邓富银, 雷家立. 三峡库区土壤中硒、碘、氟分布特征与规律研究[J]. 长江流域资源与环境, 2005, 14(4): 491-495.
[8]	郭晓东,牛叔文. 长江流域资源环境与区域发展研究的回顾及展望[J]. 长江流域资源与环境, 2005, 14(3): 392-396.