Hydropedology: Interactions between pedologic and hydrologic processes across spatiotemporal scales
Ma, Yu-jun1,2,3; Li, Xiao-yan1,2; Guo, Li3; Lin, Henry3,4,5
2017-08-01
发表期刊EARTH-SCIENCE REVIEWS
卷号171期号:2017页码:181-195
文章类型Article
摘要Hydropedology is an emerging intertwined branch of soil science and hydrology that studies interactive pedologic and hydrologic processes and properties in the Earth's Critical Zone. It aims to bridge disciplines, scales, and data, connect soils with the landscape, link fast and slow processes, and integrate mapping with monitoring and modeling to provide a holistic understanding of the interactions between the pedosphere and the hydrosphere. This paper reviews major research findings in this field achieved in the past decade (mostly since 2012). A three-dimensional framework (spatial, temporal, and methodological) is used to synthesize recent hydropedological investigations over a broad range of spatiotemporal scales. In spatial dimension, soil architecture, ranging from the microscopic to the megascopic levels, exerts an important control on hydrologic processes and biogeochemical dynamics. In temporal dimension, both short-term soil functioning processes and long-term soil pedogenic processes are impacted by hydrologic processes, and vice versa. In methodological dimension, linking mapping with monitoring, modeling, and managing can accelerate integrated and sustainable use of soil and water resources. Three major challenges are identified for advancing the frontiers of hydropedology, including 1) hierarchical framework for 3-D spatial scale bridging, 2) quantitive linkage for multiple temporal scales, and 3) comprehensive integration for methodological breakthrough. It is hoped that this review can stimulate continuous efforts in advancing hydropedology and integrated soil and water sciences.
关键词Hydropedology Soil Architecture Soil Function Soil Formation Hydrologic Process
WOS标题词Science & Technology ; Physical Sciences
DOI10.1016/j.earscirev.2017.05.014
关键词[WOS]BIOGEOCHEMICAL HOT-SPOTS ; CELLULAR-AUTOMATA MODEL ; SOIL-MOISTURE ; SURFACE RUNOFF ; PREFERENTIAL FLOW ; CLIMATE-CHANGE ; CONSERVATION AGRICULTURE ; HYDRAULIC CONDUCTIVITY ; HEADWATER CATCHMENT ; LANDSCAPE EVOLUTION
收录类别SCI
语种英语
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
WOS记录号WOS:000408289500008
引用统计
被引频次:43[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.ieecas.cn/handle/361006/5404
专题黄土与第四纪地质国家重点实验室(2010~)
作者单位1.Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China
2.Beijing Normal Univ, Sch Nat Resources, 19 Xinjiekouwai St, Beijing 100875, Peoples R China
3.Penn State Univ, Dept Ecosyst Sci & Management, University Pk, PA 16802 USA
4.Chinese Acad Sci, State Key Lab Loess & Quaternary Geol, Inst Earth Environm, Xian 710061, Shaanxi, Peoples R China
5.Xian AMS Ctr, Shaanxi Key Lab Accelerator Mass Spectrometry Tec, Xian 710061, Shaanxi, Peoples R China
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Ma, Yu-jun,Li, Xiao-yan,Guo, Li,et al. Hydropedology: Interactions between pedologic and hydrologic processes across spatiotemporal scales[J]. EARTH-SCIENCE REVIEWS,2017,171(2017):181-195.
APA Ma, Yu-jun,Li, Xiao-yan,Guo, Li,&Lin, Henry.(2017).Hydropedology: Interactions between pedologic and hydrologic processes across spatiotemporal scales.EARTH-SCIENCE REVIEWS,171(2017),181-195.
MLA Ma, Yu-jun,et al."Hydropedology: Interactions between pedologic and hydrologic processes across spatiotemporal scales".EARTH-SCIENCE REVIEWS 171.2017(2017):181-195.
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