PDF Download

[1]Zhang Chengbo,Zhang Shaoliang,Feng Lanqian,et al.Response of fractal characteristics of various soil particle types to wind erosion in a typical wind erosion area of western Northeast China[J].Research of Soil and Water Conservation,2025,32(06):57-67.[doi:10.13869/j.cnki.rswc.2025.06.010]

Copy

Response of fractal characteristics of various soil particle types to wind erosion in a typical wind erosion area of western Northeast China

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 32 Number of periods: 2025 06 Page number: 57-67 Column: Public date: 2025-10-20

Title:: Response of fractal characteristics of various soil particle types to wind erosion in a typical wind erosion area of western Northeast China

Author(s):: Zhang Chengbo^1,2,Zhang Shaoliang^1,2,Feng Lanqian^1,2,Wang Hao^1,2,Xu Weitao^1,2,Zhuang Yaru^1,2,Yan Pengke^1,2; (1.School of Resources and Environment,Northeast Agricultural University,Harbin 150030,China;2.Research Centerfor Key Substances Transport and Regulation in Mollisols(Northeast Agricultural University),Harbin 150030,China)

Keywords:: soil types; soil particle composition; fractal dimension; soil wind erosion; wind erosion area of Northeast China

CLC:: S812.2

DOI:: 10.13869/j.cnki.rswc.2025.06.010

Abstract:: [Objective] To clarify the response mechanism of different types of soil particle characteristics to wind erosion in the black soil region of Northeast China, and provide a scientific basis for soil conservation in wind erosion areas. [Methods] A typical area in the wind erosion belt of western Northeast China(5 800 km²) was taken as the research object. A total of 122 sampling points were randomly set across the entire area, covering four soil types： aeolian sandy soil, meadow soil, chernozem, and saline-alkali soil, and soil samples were collected from the 0—20 cm and 20—30 cm layers. The soil volume fractal dimension was used to characterize the comprehensive distribution features of soil particles. The wind erosion modulus was estimated using the revised wind erosion equation (RWEQ) model. Environmental factors were obtained by combining field surveys with remote sensing images to comprehensively analyze the response of soil particle fractal characteristics to wind erosion. [Results](1) The content of particles smaller than 50 μm in the surface soil could to some extent reflect the impact degree of wind erosion on the soil in the past. Chernozem had the highest volume percentage of particles smaller than 50 μm(75.45%), indicating a relatively low degree of wind erosion impact, while aeolian sandy soil had the lowest content of particles smaller than 50 μm(52.64%), indicating the greatest degree of wind erosion impact.(2) Aeolian sandy soil had a relatively low vegetation coverage(67.43%) and was the most sensitive to wind erosion. Saline-alkali soil had the highest vegetation coverage(75.46%) and the weakest sensitivity to wind erosion.(3) Wind erosion decreased the fractal dimension of the soil surface layer, reducing the complexity and stability of soil particles, which further reduced the fractal dimension of the plow pan soil.(4) When vegetation coverage and soil moisture decreased, saline-alkali soil and chernozem with higher soil fractal dimension faced a higher risk of wind erosion. [Conclusion] Different types of soil particle fractal characteristics respond differently to wind erosion. The soil fractal dimension can well reflect the past wind erosion risk and the degree of wind erosion impact on soil in the study area.

References:: [1]王醒，方荣杰，张帅普，等.广西龙脊梯田区森林类型对土壤水力特性的影响[J]. 水土保持通报，2021，41（5）：92-98，106. Wang X，Fang R J，Zhang S P，et al.Soil hydraulic characteristics of different forest types in a Longji terraced field in Guangxi Region[J]. Bulletin of Soil and Water Conservation，2021，41（5）：92-98，106.
[2]戴磊，王贵玲，何雨江.基于分形理论研究土壤结构及其水分特征关系[J]. 地球科学，2021，46（9）：3410-3420. Dai L，Wang G L，He Y J.The relationship between soil structure and water characteristics based on fractal theory[J]. Earth Science，2021，46（9）：3410-3420.
[3]杜姣姣.马尾松人工林物种调控下土壤团聚体稳定性及养分特征研究[D]. 贵阳：贵州大学，2021. Du J J.Study on the stability and nutrient characteristics of soil aggregates under the regulation of species in Pinus massoniana plantation[D]. Guiyang：Guizhou University，2021.
[4]Rakhsh F，Golchin A，Beheshti Al Agha A，et al.Mineralization of organic carbon and formation of microbial biomass in soil：Effects of clay content and composition and the mechanisms involved[J]. Soil Biology and Biochemistry，2020，151：108036.
[5]Matus F J.Fine silt and clay content is the main factor defining maximal C and N accumulations in soils：a metaanalysis [J]. Scientific Reports，2021，11（1）：6438.
[6]王烁.土地整治下黑土区坡耕地不同耕作措施田间差异分析与产能提升研究[D]. 哈尔滨：东北农业大学，2023. Wang S.Field difference analysis andproductivity improvement of slopingfarmland under different tillagemeasures in black soil area underlandconsolidation[D]. Harbin： Northeast Agricultural University，2023.
[7]孙嘉豪.东北地区骤旱动态演变的驱动机制及其生态效应研究[D]. 哈尔滨：黑龙江大学，2024. Sun J H.Flash droughts in Northeast China：spatiotemporal patterns，possible climatic drivings and ecological impacts[D]. Harbin：Heilongjiang University，2024.
[8]巩国丽.中国北方土壤风蚀时空变化特征及影响因素分析[D]. 北京：中国科学院大学，2014. Gong G L.Temporal and spatial variation characteristics and influencing factors of soil wind erosion in northern China[D]. Beijing：University of Chinese Academy of Sciences，2014.
[9]蔺阿荣，周冬梅，马静，等.基于RWEQ模型的疏勒河流域防风固沙功能价值评估[J]. 干旱区地理，2024，47（1）：58-67. Lin A R，Zhou D M，Ma J，et al.Evaluation of wind prevention and sand fixation function in Shule River Basin based on RWEQ mode[l J]. Arid Land Geography，2024，47（1）：58-67.
[10]Kaplan S，Basaran M，Erpul G.Assessing the performance of wind erosion prediction models of RWEQ and SWEEP by direct measurements in an arid region[J]. Soil and Tillage Research，2024，240：106086.
[11]陈小磊，舒强，田欢，等.浙北平原区土壤分形特征及其与土壤肥力的关系：以水稻土为例[J]. 江苏农业科学，2021，49（22）：247-252. Chen X L，Shu Q，Tian H，et al.Soil fractal characteristics and its relationship with soil fertility in plain area of northern Zhejiang：taking paddy soil as an example[J]. Jiangsu Agricultural Sciences，2021，49（22）：247-252.
[12]He F，Mohamadzadeh N，Sadeghnejad M，et al.Fractal features of soil particles as an index of land degradation under different land-use patterns and slope-aspects [J]. Land，2023，12（3）：615.
[13]Shahabinejad N，Mahmoodabadi M，Jalalian A，et al. The fractionation of soil aggregates associated with primary particles influencing wind erosion rates in arid to semiarid environments[J]. Geoderma，2019，356：113936.
[14]Yan Y C，Wang X，Guo Z J，et al.Influence of wind erosion on dry aggregate size distribution and nutrients in three steppe soils in northern China[J]. Catena，2018，170：159-168.
[15]Hou R J，Li T X，Fu Q，et al.Research on the distribution of soil water，heat，salt and their response mechanisms under freezing conditions[J]. Soil and Tillage Research，2020，196：104486.
[16]Zhang Y L，Chun X，Zhou H J，et al.Particle size characteristics of surface sediments and their environmental significance：a comparative study of deserts in arid western Inner Mongolia，China[J]. Environmental Earth Sciences，2020，79（10）：203.
[17]Wu X G，Fan J Q，Sun L，et al.Wind erosion and its ecological effects on soil in the northern piedmont of the Yinshan Mountains[J]. Ecological Indicators，2021，128：107825.
[18]白玉锋，孙静，李秀军，等.松嫩平原西部典型盐生景观土壤分形维数及盐碱化特征[J]. 水土保持学报，2021，35（3）：163-169. Bai Y F，Sun J，Li X J，et al.Fractal dimension and salinization characteristics of typical halophytic landscape soil in western Songnen Plain[J]. Journal of Soil and Water Conservation，2021，35（3）：163-169.
[19]Zhao Y，Feng Q，Yang H D.Soil salinity distribution and its relationship with soil particle size in the lower reaches of Heihe River，Northwestern China[J]. Environmental Earth Sciences，2016，75（9）：1-18.
[20]顾汪明，周金星，王彬，等.冻融循环作用对黑土水稳性团聚体特征的影响[J]. 中国水土保持科学，2020，18（4）：45-52. Gu W M，Zhou J X，Wang B，et al.Effects of freezethaw cycle on the characteristics of black soil waterstable aggregates[J]. Science of Soil and Water Conservation，2020，18（4）：45-52.
[21]陈家欢，袁立敏，高永，等.风沙区不同种植制度下的土壤风蚀效果研究[J]. 土壤通报，2021，52（2）：408-415. Chen J H，Yuan L M，Gao Y，et al.Influence of different planting system on soil grain size distribution characteristics in sandstorm area[J]. Chinese Journal of Soil Science，2021，52（2）：408-415.
[22]Zhou W X，Li C J，Zhao W W，et al.Spatial distributions of soil nutrients affected by land use，topography and their interactions，in the Loess Plateau of China[J]. International Soil and Water Conservation Research，2024，12（1）：227-239.
[23]苗涵博.激光粒度仪法与湿筛—沉降法测定土壤颗粒组成的比较研究[D]. 沈阳：沈阳农业大学，2019. Miao H B.Comparative study on the determination of soil particle composition by laser particle sizeanalyzerand wet sieve-sedimentation method[D]. Shenyang：Shenyang Agricultural University，2019.
[24]邓时琴.土壤矿质颗粒及土壤质地[J]. 土壤，1983（2）：77-80. Deng S Q.Soil mineral particles and soil texture[J]. Soil，1983（2）：77-80.
[25]鲍士旦.土壤农化分析[M]. 3版.北京：中国农业出版社，2000. Bao S D.Soil and Agricultural Chemistry Analysis[M]. 3rd.Beijing：China Agriculture Press，2000.
[26]孙传龙，张卓栋，邱倩倩，等.锡林郭勒草地表层土壤粒度分形特征及其与风蚀的关系[J]. 中国沙漠，2017，37（5）：978-985. Sun C L，Zhang Z D，Qiu Q Q，et al.Fractal characteristics of surface soils in the Xilinguole grassland landscape system and its relationship to wind erosion[J]. Journal of Desert Research，2017，37（5）：978-985.
[27]王燕.武川县旱作农区土壤风蚀特征研究及风蚀量估算[D]. 呼和浩特：内蒙古农业大学，2019. Wang Y.Soil wind erosion characteristics and wind erosion estimation in dry farming area of Wuchuan County [D]. Hohhot：Inner Mongolia Agricultural University，2019.
[28]张泽宇.东北黑土区土壤团聚体地球化学控制因素与调控研究[D]. 长春：吉林大学，2024. Zhang Z Y.Study on geochemical control factors and regulation of soil aggregates in Northeast China's black soil region[D]. Changchun：Jilin University，2024.
[29]Cao C Y，Tao S，Cui Z B，et al.Response of soil properties and microbial communities to increasing salinization in the meadow grassland of NorthEast China[J]. Microbial Ecology，2021，82（3）：722-735.
[30]Meysam M，Mahmoud S，Mohammad Hossein M，et al. Characterizing spatial variability of soil textural fractions and fractal parameters derived from particle size distributions[J]. Pedosphere，2019，29（2）：224-234.

Similar References:

Memo

Last Update: 2025-12-10