Norra Stefan
Institute of Mineralogy and Geochemistry, University of Karlsruhe, 76131 Karlsruhe, Germany.
Environ Sci Pollut Res Int. 2009 Jul;16(5):539-45. doi: 10.1007/s11356-009-0183-8. Epub 2009 Jun 9.
BACKGROUND, AIM, AND SCOPE: In 1875, the geoscientist Walter Suess introduced several spheres, such as the lithosphere and the atmosphere to promote a comprehensive understanding of the system earth. Since then, this idea became the dominating concept for the understanding of the distribution of chemical elements in the system earth. Meanwhile, due to the importance of human beings on global element fluxes, the term anthroposphere was introduced. Nevertheless, in face of the ongoing urbanization of the earth, this concept is not any more adequate enough to develop a comprehensive understanding of global element fluxes in and between solid, liquid, and gaseous phases. This article discusses a new concept integrating urbanization into the geoscientific concept of spheres.
No geological exogenic force has altered the earth's surface during the last centuries in such an extent as human activity. Humans have altered the morphology and element balances of the earth by establishing agrosystems first and urban systems later. Currently, urban systems happen to become the main regulators for fluxes of many elements on a global scale due to ongoing industrial and economic development and a growing number of inhabitants. Additionally, urban systems are constantly expanding and cover more and more former natural and agricultural areas. For nature, urban systems are new phenomena, which never existed in previous geological eras. The process of the globe's urbanization concurrently is active with the global climate change. In fact, urban systems are a major emitter for climate active gases. Thus, beside the global changes in economy and society, urbanization is an important factor within the global change of nature as is already accepted for climate, ecosystems, and biodiversity.
Due to the fact that urbanization has become a global process shaping the earth and that the urban systems are globally cross-linked among each other, a new geoscientific sphere has to be introduced: the astysphere. This sphere comprises the parts of the earth influenced by urban systems. Accepting urbanization as global ongoing process forming the astysphere comprehensively copes with the growing importance of urbanization on the creation of present geologic formations.
Anthropogenic activities occur mainly in rural and urban environments. For long lasting periods of human history, human activities mainly were focused on hunting and agriculture, but since industrialization, urbanized areas became increasingly important for the material and energy fluxes of earth. Thus, it seems appropriate to classify the anthroposphere into an agriculturally and an urban-dominated sphere, which are the agrosphere (Krishna 2003) and the astysphere (introduced by Norra 2007).
We have to realize that urban systems are deposits, consumers, and transformers of resources interacting among each other and forming a network around the globe. Since the future of human mankind depends on the sustainable use of available resources, only a global and holistic view of the cross-linked urban systems forming together the astysphere provide the necessary geoscientific background understanding for global urban material and energy fluxes. If we want to ensure worth-living conditions for future generations of mankind, we have to develop global models of the future needs for resources by the global metasystem of urban systems, called astysphere.
The final vision for geoscientific research on the astysphere must be to design models describing the global process of urbanization of the earth and the development of the astysphere with respect to fluxes of materials, elements, and energy as well as with respect to the forming of the earth's face. Besides that, just from the viewpoint of fundamental research, the geoscientific concept of spheres has to be complemented by the astysphere if this concept shall fully represent the system earth.
背景、目的与范围:1875年,地球科学家沃尔特·聚斯提出了几个圈层概念,如岩石圈和大气圈,以促进对地球系统的全面理解。从那时起,这一理念成为理解地球系统中化学元素分布的主导概念。与此同时,由于人类在全球元素通量方面的重要性,“人类圈”这一术语被引入。然而,面对地球持续的城市化进程,这一概念已不足以全面理解固体、液体和气体相中以及它们之间的全球元素通量。本文讨论了一个将城市化纳入地球科学圈层概念的新观念。
在过去几个世纪里,没有任何地质外力能像人类活动那样对地球表面产生如此大的改变。人类先是建立了农业系统,后来又建立了城市系统,从而改变了地球的形态和元素平衡。由于持续的工业和经济发展以及人口增长,城市系统目前已成为全球范围内许多元素通量的主要调节者。此外,城市系统在不断扩张,覆盖了越来越多以前的自然和农业区域。对自然界而言,城市系统是新现象,在以前的地质时代从未存在过。全球城市化进程与全球气候变化同时进行。事实上,城市系统是气候活性气体的主要排放源。因此,除了全球经济和社会变化外,城市化是自然全球变化中的一个重要因素,这一点在气候、生态系统和生物多样性方面已得到认可。
由于城市化已成为塑造地球的全球进程,且城市系统在全球范围内相互关联,因此必须引入一个新的地球科学圈层:城市圈。这个圈层包括受城市系统影响的地球部分。将城市化视为形成城市圈的全球持续进程,能全面应对城市化在当前地质构造形成过程中日益增长的重要性。
人类活动主要发生在农村和城市环境中。在人类历史的很长一段时间里,人类活动主要集中在狩猎和农业上,但自工业化以来,城市化地区对地球的物质和能量通量变得越来越重要。因此,将人类圈分为农业主导圈和城市主导圈似乎是合适的,即农业圈(克里希纳,2003年)和城市圈(诺拉于2007年提出)。
我们必须认识到,城市系统是资源的储存者、消费者和转化者,它们相互作用,在全球形成一个网络。由于人类的未来取决于对可用资源的可持续利用,只有对共同构成城市圈的相互关联的城市系统有一个全球整体的认识,才能为全球城市物质和能量通量提供必要的地球科学背景理解。如果我们想确保人类后代有值得生活的条件,就必须通过称为城市圈的全球城市系统元系统来建立全球未来资源需求模型。
关于城市圈的地球科学研究的最终愿景必须是设计模型,描述地球城市化的全球进程以及城市圈在物质、元素和能量通量以及地球表面形成方面的发展。除此之外,仅从基础研究的角度来看,如果要让圈层的地球科学概念充分代表地球系统,就必须用城市圈对其进行补充。