- 1、本文档共16页,可阅读全部内容。
- 2、原创力文档(book118)网站文档一经付费(服务费),不意味着购买了该文档的版权,仅供个人/单位学习、研究之用,不得用于商业用途,未经授权,严禁复制、发行、汇编、翻译或者网络传播等,侵权必究。
- 3、本站所有内容均由合作方或网友上传,本站不对文档的完整性、权威性及其观点立场正确性做任何保证或承诺!文档内容仅供研究参考,付费前请自行鉴别。如您付费,意味着您自己接受本站规则且自行承担风险,本站不退款、不进行额外附加服务;查看《如何避免下载的几个坑》。如果您已付费下载过本站文档,您可以点击 这里二次下载。
- 4、如文档侵犯商业秘密、侵犯著作权、侵犯人身权等,请点击“版权申诉”(推荐),也可以打举报电话:400-050-0827(电话支持时间:9:00-18:30)。
查看更多
Lab: Vostok Ice Core
Map showing Antarctica and location of Vostok Ice Core. Colors indicate elevation.
I. Introduction
Snow falling in the polar regions of the earth (e.g. Greenland and Antarctica) sometimes is preserved as annual layers within the ice sheets, provided that they are not destroyed by flow of the ice. These annual layers provide a record of the earths climate that reaches back as much as 200,000 years.
Several different climate indicators can be measured from samples of the ice:
The amount of dust in each annual layer is indicative of the environment at the time that the dust was deposited. Various kinds of fallout from the atmosphere, including airborne continental dust and biological material, volcanic debris, sea salts, cosmic particles, and isotopes produced by cosmic radiation, are deposited on the ice sheet surface along with the snow, thus mixing with the snow and also acting as a distinctive barrier between different ice layers.
The composition of bubbles of air trapped in the ice is a measure of the composition of the atmosphere in ancient times. With increasing pressure from subsequent snow deposition on an ice cap or glacier, the snow becomes compacted and, consequently, air is trapped within the deposited layer. This entrapment of air occurs essentially with no differentiation of the atmospheric gas components. However, carbon dioxide has different chemical properties from other atmospheric gases, thus, the carbon dioxide concentration in the air-filled spaces might be affected by interaction with the ice itself or with trapped impurities.
The isotopic composition of water, and in particular the concentration of the heavy isotope of oxygen, 18O, relative to 16O, as well as 2H (deuterium) relative to 1H, is indicative of the temperatures of the environment. During cold periods, the concentration of less volatile 2H (18O) in the ice is lower than during warm periods. The reason for this is that at lower temperature, the moisture has
您可能关注的文档
- chapter3 the simple keynesian theoryof income determination(chapter 3 the simple theoryof keynesian income determination).doc
- chapter7- componentsof optical instruments(chapter 7 - componentsof optical instruments).doc
- chapter377 r e v i e w o f r o a d s u n d e r t h e s i t e l o c a t i o n o f(chapter377 r e v i e w o f r o a d s u n d e r t h e s i t e l o c a t i o n o f).doc
- chemical thermodynamics-- chapter13(chemical thermodynamics——chapter13).doc
- chemistry331-paceuniversitywebspace.doc
- chpater8 climatic zonesand types- u c c s home(chpater 8 climatic zonesand types - u c c s home).doc
- climate change- middlebury vermont community network(community climate change - vermont middlebury network).doc
- climate change- royal geographical society(climate change - royal geographical工厂).doc
- climatechangehowitimpactscanadiansandwhatwecando.doc
- codebook survey13(codebook survey13).doc
文档评论(0)