期刊文献+

河北临城白云洞洞穴旅游对洞穴CO_2浓度及温度的影响 被引量:33

EFFECT OF SPELEO-TOURISM ON THE CO_2 CONTENT AND TEMPERATURE IN BAIYUN CAVE, LINCHENG, HEBEI
下载PDF
导出
摘要 河北临城白云洞碳酸钙景观极其丰富但风化严重。2000年"五一"黄金周对白云洞的客流量、温度、洞穴空气中的CO2浓度进行了系统的观测研究,并在8月、10月旅游淡季进行了对比观测。研究结果表明,洞穴旅游活动对洞穴的温度和CO2浓度的变化有主控作用。白云洞在"五一"长假游开始前最低CO2浓度为600ppm,"五一"这一天当游客量达到5800人时,大洞厅中的CO2达到4400ppm,温度提高了1.1℃,而狭小洞厅中CO2浓度可达到5800ppm,温度提高了2.3℃。当洞穴旅游高峰连续维持多日时,洞穴中的CO2还会累积增加。如5月2日的游客达到4000多人时,狭小洞厅CO2达到7000ppm。旅游高峰期,洞穴CO2往往经过一个晚上的扩散和流动后,也回不到本底值。但洞穴温度的累积不很明显。 The speleothem scene is very abundant but some of them are very strongly weathered in Baiyun Cave, Lincheng County, Hebei Province. During the 'Gold May Long Holidays' in 2000, the visitor flow, temperature and CO2 concentration in Baiyun Cave were monitored, the comparison work were done in August and October in 2000. The testing result shows that the temperature and CO2 content of the cave atmosphere are mainly controlled by the visitor flow. The lowest content of CO2 is 600ppm before May Day Holiday when there was small account of visitors. When the visitor flow reached 5800 people on May Day, the CO2 content went up to the maximum, 4400 ppm and temperature increased by 1.1℃ in the largest Hall, while the peak value is 5800ppm and temperature increased by 2.3℃ in small and narrow rooms. In the conditions of large number of visitors for several days, the CO2 concentration will be accumulated. For example, when the visitors got to about 4000 people on May 2, CO2 content of cave atmosphere in the small narrow room rose to 7000ppm. Though there were no visitors from 20:00 on May Day to 8:00 on May 2, the CO2 content did not get down to the background value, but still at the level 2600ppm. The accumulation of temperature was not so obvious. On October 1, the total visitors were 1000, the maximum value of CO2 was only 1690ppm. To protect cave environment, reducing the CO2 content in cave atmosphere should be paid attention to.
出处 《中国岩溶》 CAS CSCD 2003年第3期230-235,共6页 Carsologica Sinica
基金 本项目得到国家自然科学基金委资助(410071017)
关键词 白云洞 旅游 CO2浓度 温度 Baiyun Cave Visitor flow CO_2 content Temperature
  • 相关文献

参考文献4

二级参考文献8

  • 1朱文孝,李坡,潘高潮.织金洞的气候环境及空气中二氧化碳[J].中国岩溶,1993,12(4):407-417. 被引量:48
  • 2宋林华 中国地带学会地貌专业委员会.pH的喀斯特水文地球化学意义.喀斯特地貌与洞穴[M].北京:科学出版社,1985.184-193.
  • 3[1]河北省地矿局.河北省北京市天津市区域地质志[M].地质出版社,1989.
  • 4[2]Carot Hill, Paolo Forti. Cave minerals of the world[M]. National Speleological Society,1997.
  • 5[3]Song Linhua, Yang Jingrong & Wang Laihong et al. The potential corrosion of speleothems by condensation[J]. Acta Carsologica,1998, Vol.27, 215-229.
  • 6Song L,J Chin Geogr,1997年,7卷,3期,26页
  • 7刘再华,贵州乌江渡水电站灌浆帷幕老化问题的研究,1996年
  • 8宋林华,喀斯特地貌与洞穴,1985年,184页

共引文献59

同被引文献280

引证文献33

二级引证文献140

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部