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国家自然科学基金(40930528)

作品数:7 被引量:396H指数:6
相关作者:吕一河傅伯杰徐延达姚雪玲高光耀更多>>
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Spatial Scale Effects of Water Erosion Dynamics:Complexities, Variabilities, and Uncertainties被引量:2
2012年
Severe water erosion is notorious for its harmful effects on land-water resources as well as local societies. The scale effects of water erosion, however, greatly exacerbate the difficulties of accurate erosion evaluation and hazard control in the real world. Analyzing the related scale issues is thus urgent for a better understanding of erosion variations as well as reducing such erosion. In this review article, water erosion dynamics across three spatial scales including plot, watershed, and regional scales were selected and discussed. For the study purposes and objectives, the advantages and disadvantages of these scales all demonstrate clear spatial-scale dependence. Plot scale studies are primarily focused on abundant data collection and mechanism discrimination of erosion generation, while watershed scale studies provide valuable information for watershed management and hazard control as well as the development of quantitatively distributed models. Regional studies concentrate more on large-scale erosion assessment, and serve policymakers and stakeholders in achieving the basis for regulatory policy for comprehensive land uses. The results of this study show that the driving forces and mechanisms of water erosion variations among the scales are quite different. As a result, several major aspects contributing to variations in water erosion across the scales are stressed: differences in the methodologies across various scales, different sink-source roles on water erosion processes, and diverse climatic zones and morphological regions. This variability becomes more complex in the context of accelerated global change. The changing climatic factors and earth surface features are considered the fourth key reason responsible for the increased variability of water erosion across spatial scales.
WEI WeiCHEN LidingYANG LeiFU BojieSUN Ranhao
关键词:UNCERTAINTYCOMPLEXITY
Landscape Ecology:Coupling of Pattern,Process,and Scale被引量:27
2011年
Landscape ecology provides new theoretical frameworks and methodologies for understanding complex ecological phenomena at multiple scales.Studies of landscape ecology focus on understanding the dynamics of eco-logical patterns and processes,and highlight the integration of multiple disciplines.In this paper,we discussed the problems and challenges that landscape ecology is currently facing,emphasizing the limitations of current methods used to describe dynamic landscape patterns and processes.We suggested that the focus should be on the integration of ground-based observation,mobile monitoring,transect survey,and remote-sensing monitoring,as well as improved coupling of experimental and model simulations.In addition,we outlined the research frontiers in landscape ecology,including scaling,integrated pattern and process modeling,and regional synthesis.Lastly,a brief review of pat-tern-process-scale coupling studies in China was provided.We concluded by pointing out that pattern-process-scale interactions,correlations between natural,economic,and social processes,and the coupling of human and natural systems will be major research areas in landscape ecology in the future.
FU BojieLIANG DiLU Nan
关键词:SCALE
景观格局与水土流失的尺度特征与耦合方法被引量:101
2010年
景观格局与生态过程的耦合研究是景观生态学研究的核心科学问题,也是综合自然地理学深化和发展的关键。尺度广泛存在于生态学现象中,尺度效应与尺度转换是景观生态学研究面临的挑战,探讨格局与过程之间相互作用机理与尺度特征是为解决尺度问题提供理论依据的必然途径。水土流失作为一种生态过程,是国内外颇为关注的生态问题。依据多种研究手段,在不同尺度上开展景观格局与水土流失的相互关系与尺度特征的研究,在分析景观格局的时空异质性、水土流失的影响因子与尺度效应的基础上,揭示流域景观格局与水土流失的耦合机理,发展尺度转换方法和景观格局—水土流失过程耦合模型,是完善景观生态学的理论基础,是为水土流失区生态建设提供科学依据的重要途径。
傅伯杰徐延达吕一河
关键词:水土流失
Land Use Change and Anthropogenic Driving Forces:A Case Study in Yanhe River Basin被引量:18
2011年
Human activities alter land use patterns and affect landscape sustainability. It is therefore very important to investigate the relationship between land use change and human activities. This study focuses on the detection of changing land use patterns in the Yanhe River Basin in northern Loess Plateau of China between 1995 and 2008. Landscape metrics were used to analyze the changing land use patterns and to explore the related anthropogenic driving forces. Results show that:1) Totally, 186 590 ha of croplands were converted into alternate land-use types (equivalent to 61.7% of the original cropland area). The majority of cropland areas were found to be converted into grassland and woodland areas (accounting for 55.9% and 4.9% respectively of the original cropland areas). 2) Both cropland and woodland demonstrated an increasing fragmentation tendency while grasslands showed a decreasing fragmentation tendency. 3) Multiple driving forces of land use change were thought to act together to changes in landscape metrics in the Yanhe River Basin. The anthropogenic driving forces were analyzed from four perspectives:ecological conservation policy, labor force transfer, industrial development, and rural settlement. The policy of the GfG (Grain for Green) project was the main driving factor which expedited the conversion from cropland to woodland and grassland. Industrial development was also found to affect land use change through the direct impact of economic activities such as oil exploration and agricultural production, or through indirect impacts such as the industrial structures readjustment. Labor force transfer from rural to urban areas was found to follow the industrial structure readjustment and further drove land use change from cropland to off-farm land use. Establishment of new tile-roofed houses instead of cave-type dwellings in rural settlements has helped to aggregate the original scattered land-use type of construction.
SU ChanghongFU BojieLU YiheLU NanZENG YuanHE AnnaHalina LAMPARSKI
黄土丘陵沟壑区坡面尺度土壤水分空间变异及影响因子被引量:105
2012年
土壤水分空间分布特征及其影响因子是土壤前期含水量模拟和小流域产流机制研究的重要内容,也是半干旱地区进行生态建设的重要参考。通过对黄土高原典型坡面雨季前后100 cm深度内土壤含水量进行观测,分析地形、植被和雨季对土壤水分空间分布的影响。基本统计分析显示,土壤水分的空间异质性在上层(<20 cm)较小,在下层(>40 cm)较大。坡面尺度上,土壤含水量的空间差异主要表现在不同植被类型之间,而不是坡位之间。各覆被类型的土壤含水量相对大小为荒草地>8年生刺槐林>20年生刺槐林>沙棘林。即使沙棘林和刺槐林位于更利于获取土壤水分的地形条件下,其土壤含水量仍然明显低于荒草地。地形对土壤水分的影响被植被类型的影响所掩盖。上述规律在雨季前后都有明显表现。因此,完全基于地形指数的土壤水分预测模型在黄土高原应该慎用,植被类型应该作为土壤水分空间预测的一个重要参数。雨季使土壤含水量整体提高,但是土壤水分空间分布格局并没有根本改变,高处仍高,低处仍低,各样点处的土壤含水量在雨季前后达到显著相关水平,说明土壤水分空间格局并不是瞬时状态,而具有明显的时间稳定性。
姚雪玲傅伯杰吕一河
关键词:土壤水分植被黄土高原
干旱半干旱区坡面覆被格局的水土流失效应研究进展被引量:74
2013年
植被恢复与建设是控制水土流失的重要措施。在干旱半干旱地区,植被在空间上的分布呈现离散特征,在坡面上形成的裸地-植被镶嵌和植被条带分布等覆被格局对水土流失过程具有重要影响。覆被格局与水土流失关系研究是景观生态学格局与过程研究的重要内容。从植被斑块、坡面覆被格局对水土流失的影响与耦合覆被格局与水土流失的手段和方法三个方面对国内外相关研究进行总结分析。从中发现,植被类型、层次结构和形态特征是植被斑块尺度上影响径流泥沙的关键因素;不同覆被类型的产流产沙特征与覆被格局的准确描述是研究覆被格局水土流失效应的重要基础;坡面覆被格局对水土流失的影响关键在于其改变了径流泥沙运移和汇集的连续性,应重点关注径流泥沙源汇区的连通性和空间分布在水土流失中的作用;以坡面的精确覆被制图为基础,建立基于水土流失过程的覆被格局指数和耦合格局信息的径流与侵蚀模型是定量研究覆被格局影响的有效手段。今后应加强以下研究:以动态系统的观点研究覆被格局的变化对水土流失的影响,系统理解覆被格局与水土流失之间的相互联系与反馈机制,探讨两者间动态关系随尺度变化的规律性并发展尺度上推方法;构建过程意义明确且简单实用的格局指数,将覆被格局与水土流失过程有机联系起来;发展覆被格局的动态信息与产流产沙过程相结合的水文模型,加强对格局与径流泥沙反馈系统的耦合,建立真正意义上的覆被格局-水土流失过程耦合模型。
高光耀傅伯杰吕一河刘宇王帅周继
关键词:干旱半干旱区水土流失
基于模型的景观格局与生态过程研究被引量:83
2010年
景观格局与生态过程关系的研究是景观生态学的主要特色和理论核心之一。模型可以充分利用实验和观测数据并综合不同时间和空间尺度上的信息提炼规律或揭示内在机制,模拟景观格局与生态过程的动态与相互关系,成为景观生态学研究的有力工具。结合研究实例,总结了基于模型的景观格局研究、生态过程研究和格局-过程关系研究的发展现状和薄弱环节,同时探讨了通过构建耦合模型研究格局-过程相互关系的途径。总结了景观模型研究亟待发展的领域与发展趋势。
徐延达傅伯杰吕一河
关键词:生态过程
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