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A detailed reconstruction of changes in the factors and parameters of soil erosion over the past 250 years in the forest zone of European Russia(Moscow region)

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International Soil and Water Conservation Research 2022年第1期10卷 149-160页

作者： Andrey Zhidkin Daria Fomicheva Nadezhda Ivanova Tomas Dostal Alla Yurova Mikhail Komissarov Josef Krasa V.V.dokuchaev soil science institute pyzhevskiy pereulok 7moscow119017russian federation Faculty of geography lomonosov moscow state universityleninskie gorygsp-1moscow119991russian federation Department of landscape water conservation faculty of civil engineeringczech technical university in praguethakurova 7prague16629czech republic Ufa institute of biology ufrc russian academy of sciencespr.oktyabrya 69ufa450054russian federation

Accelerated soil erosion is a major threat to soil,and there are great variations in the rate of soil erosion over time due to natural and human-induced *** temperate forest zone of Russia is character-ized by complex stages of land-use history(*** urbanization,agricultural development,land abandonment,etc.).We have for the first time estimated the rates of soil erosion by the watem/sedem model(rainfall erosion)and by a regional model(snowmelt erosion)over the past 250 years(from 1780 to 2019)for a 100-km2 study site in the Moscow region of *** calculations were made on the basis of a detailed historical reconstruction of the following factors:the location of the arable land,crop rotation,the rain erosivity factor,and the maximum snow water *** area of arable land has decreased more than 3.5-fold over the past 250 *** the end of the 20th century,the rates of gross erosion had declined more than 5.5-fold(from 28×10^(3) to 5×10^(3) t·ha^(-1)yr^(-1))in comparison with the end of the 18th *** in the boundaries of arable land and also the relief features had led to a significant intra-slope accumulation of *** a result of sediment redeposition within the arable land,the variation in net soil erosion was significantly lower than the variation in gross soil *** changes in arable land area and in crop composition are the factors that have to the greatest extent determined the changes in soil erosion in this territory.

关键词： Anthropogenic soil erosion Soil erosion history Crop rotation Magnetic tracer method watem/sedem

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Impact of land use changes on catchment soil erosion and sediment yield in the northeastern China:A panel data model application

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International Journal of Sediment Research 2020年第5期35卷 540-549页

作者： Haiyan Fang College of Resources and Environment University of Chinese Academy of Sciences Key Laboratory of Water Cycle and Related Land Surface Processes Institute of Geographic Sciences and Natural Resources ResearchChinese Academy of Sciences

Land use is an important factor influencing soil erosion and sediment yield(SESY).Regressing soil erosion intensity(SEI) and sediment yield(SY) to land use characteristics can provide necessary information for controlling soil ***,current simple regression methods emphasize cross sectional parameters,with less emphasis on temporal variability of relevant land use parameters so that the derived effects of land use change on SESY can be ***,a panel data method was applied to quantify the impact of land use change on SESY in 1954,1975,and 2015,based on the watem/sedem model and seven landscape metrics for 25 reservoir catchments in northeastern *** results indicate that SEI and area-specific SY(SSY) continuously decreased from 1954 to 2015,which were significantly correlated with landscape metrics such as area-edge metrics of mean patch area(AREAN),shape index of the mean related circumscribing circle(CIRCLEN),aggregation index of effective mesh size(MESH),patch cohesion index(COHESION),and diversity metrics such as Shannon’s diversity index(SHDI),patch richness density(PRD),and modified Simpson’s evenness index(MSIEI).The results suggested that catchment SESY can be reduced through decreasing mean patch area,patch mesh size,and physical connectivity of patches,enriching landscape types,and elongating land use *** findings are helpful to effectively implement soil conservation measures in northeastern China and similar regions *** current study also implies that the panel data approach will have beneficial potential applications in earth-science research fields.

关键词： watem/sedem Soil erosion Sediment yield Landscape metrics Panel data model

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景观指数耦合景观格局与土壤侵蚀的有效性

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生态学报 2017年第15期37卷 4923-4935页

作者：刘宇中国科学院地理科学与资源研究所、生态系统网络观测与模拟重点实验室北京100101

景观格局分析是景观生态学中揭示景观变化及其生态效应的主要方法,而景观指数是景观格局分析中广泛使用的工具。土壤侵蚀是土壤物质在景观中的迁移和再分配过程,受地形、植被和人类活动及其空间格局的调控。运用景观格局分析揭示景观格... 详细信息

景观格局分析是景观生态学中揭示景观变化及其生态效应的主要方法,而景观指数是景观格局分析中广泛使用的工具。土壤侵蚀是土壤物质在景观中的迁移和再分配过程,受地形、植被和人类活动及其空间格局的调控。运用景观格局分析揭示景观格局变化特别是土地利用/覆被格局变化对土壤侵蚀的影响是土壤侵蚀研究中应用景观生态学原理和方法的典型。在当前的研究中,斑块-廊道-基质范式下建立的景观指数对侵蚀过程的解释能力不断受到质疑,建立筛选适用的景观指数的原则和方法十分必要。以延河流域碾庄沟小流域为例,利用watem/sedem模型模拟多个年份流域侵蚀产沙和输沙量;基于土地利用/覆被数据,利用Fragstat4.2软件,计算了相应年份流域斑块、边界密度、形状、集聚与分散和斑块类型多样性4个方面的代表性景观指数。在此基础上,分析了景观指数与流域侵蚀产沙和输沙之间的关系,讨论了景观指数在土壤侵蚀研究中的有效性,在景观和斑块类型水平上分析了景观指数表达"源"、"汇"两大类景观类型的空间格局与侵蚀产沙和输沙之间的关系的一致性。结果表明:斑块-廊道-基底范式下发展的景观指数在指示景观格局的土壤侵蚀效应时存在局限。相对而言,斑块类型尺度的景观指数更能有效表达景观格局与土壤侵蚀的关系。基于景观类型在土壤侵蚀过程中的"源"、"汇"功能,提出了在土壤侵蚀研究中筛选适用的景观指数的原则:(1)对"源"、"汇"两类景观类型,景观指数与土壤侵蚀状况表征变量的相关系数符号相反;(2)对同为"源"或"汇"景观类型的多个景观类型,景观指数与土壤侵蚀表征变量的相关系数应具有符号一致性。尽管景观指数在斑块类型水平上具有一定的有效性,但用其预测景观格局变化的侵蚀效应有很大的不确定性。因此,基于土壤侵蚀过程与景观格局的作用机制发展新型的景观指数是增强景观格局分析预测土壤侵蚀过程的能力的途径。

关键词：景观指数景观格局分析土壤侵蚀 watem/sedem 景观指数有效性

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