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SOIL MICROMORPHOLOGY IN ARCHAEOLOGY 考古学中的土壤微观形态
Pub Date : 1999-04-01 DOI: 10.11867/j.issn.1001-8166.1999.02.0197
Jin Guiyun
Soil micromorphology is a discipline to interpret the development of soil based on its microscopic features.There are two advantages of its use in archaeology,one is to analyse the relationship between environmental change and cultural development,the other is to analyse the characteristics of archaeological features and the human activity reflected in it.
土壤微形态学是一门根据土壤微观特征来解释土壤发展的学科。在考古学中使用它有两个优点,一是分析环境变化与文化发展的关系,二是分析考古特征的特点及其所反映的人类活动。
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引用次数: 0
DEVELOPMENT OF STUDY ON OZONE VARIATION AND ITS CLIMATIC EFFECT 臭氧变化及其气候效应研究进展
Pub Date : 1999-02-01 DOI: 10.11867/J.ISSN.1001-8166.1999.01.0037
Wang Tijian, Sun Zhaobo
In this paper,the developments of study on characteristics and mechanism of ozone variation and its climate effect are reviewed.The amount of tropospheric O 3(in North Hemisphere)is increasing,that of stratospheric O 3 is decreasing and the total ozone amount also is decreasing which show the trend of global ozone variation.The main reason is that the O 3 precusors,such as NOx,NMHC,CO,CH 4,are increasing due to human activities and the species(NOx,H 2O,N 2O,CFCs)which can destroy stratospheric O 3 are increasing.The enhancement of tropospheric O 3 will warm the ground surface and the lower atmosphere and the depletion of stratospheric O 3 may warm or cool the ground surface and lower atmosphere.It is a very effective way to use the global or regional climate model coupled with a atmospheric chemistry model for study on ozone variation and its climate effect.
本文综述了近年来臭氧变化的特征、机理及其气候效应的研究进展。对流层(北半球)臭氧量呈增加趋势,平流层臭氧量呈减少趋势,臭氧总量呈减少趋势,显示出全球臭氧变化的趋势。主要原因是由于人类活动导致NOx、NMHC、CO、ch4等o3前体物质增加,破坏平流层o3的物质(NOx、h2o、n2o、cfc)增加。对流层臭氧的增强会使地表和低层大气变暖,而平流层臭氧的耗竭会使地表和低层大气变暖或变冷。将全球或区域气候模式与大气化学模式相结合是研究臭氧变化及其气候效应的一种非常有效的方法。
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引用次数: 5
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Advance in Earth Sciences
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