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Earth's Critical Zone and hydropedology: concepts, characteristics, and advances

机译:地球的关键地带和水文学:概念,特征和进步

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The Critical Zone (CZ) is a holistic framework for integrated studies of water with soil, rock, air, and biotic resources in the near-surface terrestrial environment. This most heterogeneous and complex region of the Earth ranges from the vegetation top to the aquifer bottom, with a highly variable thickness globally and a yet-to-be clearly defined lower boundary of active water cycle. Interfaces among different compartments in the CZ are critical, which provide fertile ground for interdisciplinary research. The reconciliation of coupled geological and biological cycles (vastly different in space and time scales) is essential to understanding the complexity and evolution of the CZ. Irreversible evolution, coupled cycling, interactive layers, and hierarchical heterogeneity are the characteristics of the CZ, suggesting that forcing, coupling, interfacing, and scaling are grand challenges for advancing CZ science. Hydropedology a?? the science of the behaviour and distribution of soil-water interactions in contact with mineral and biological materials in the CZ a?? is an important contributor to CZ study. The pedosphere is the foundation of the CZ, which represents a geomembrance across which water and solutes, as well as energy, gases, solids, and organisms are actively exchanged with the atmosphere, biosphere, hydrosphere, and lithosphere, thereby creating a life-sustaining environment. Hydropedology emphasizes in situ soils in the landscape setting, where distinct pedogenic features and soil-landscape relationships are essential to understanding interactive pedologic and hydrologic processes. Both CZ science and hydropedology embrace an evolutionary and holistic worldview, which offers stimulating opportunities through steps such as integrated systems approach, evolutionary mapping-monitoring-modeling framework, and fostering a global alliance. Our capability to predict the behaviour and evolution of the CZ in response to changing environment can be significantly improved if cross-site scientific comparisons, evolutionary treatment of organized complex systems, and deeper insights into the CZ can be made.
机译:关键区域(CZ)是一个整体框架,用于对近地表地球环境中的水与土壤,岩石,空气和生物资源进行综合研究。地球上这个最不均匀,最复杂的区域范围从植被顶部到含水层底部,全球范围内厚度变化很大,并且活跃水循环的下界尚未明确定义。 CZ中不同隔室之间的界面至关重要,这为跨学科研究提供了沃土。地质和生物循环耦合(在时空尺度上有很大不同)的和解对于理解CZ的复杂性和演化至关重要。不可逆的演化,耦合循环,交互层和分层异质性是CZ的特征,这表明,强制,耦合,接口和扩展是推进CZ科学的巨大挑战。水文学一?? CZ中与矿物和生物材料接触的土壤-水相互作用的行为和分布的科学?是CZ研究的重要贡献者。地层是CZ的基础,它代表了一种土膜,水和溶质以及能量,气体,固体和生物通过其与大气,生物圈,水圈和岩石圈进行积极的交换,从而维持生命环境。水文生态学强调景观环境中的原位土壤,其中独特的成岩特征和土壤-景观关系对于理解互动的土壤学和水文过程至关重要。 CZ科学和水文学学都包含一种进化和整体的世界观,它通过诸如集成系统方法,进化测绘-监视-建模框架以及建立全球联盟之类的步骤提供了令人兴奋的机会。如果可以进行跨站点的科学比较,对组织的复杂系统进行进化处理以及对CZ进行更深入的了解,那么我们预测CZ行为和环境变化的能力将大大提高。

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