[1]魏育超,陈姿宇,王子吟,等.基于REE示踪法的工程堆积体坡面泥沙来源研究[J].水土保持研究,2024,31(05):9-17.[doi:10.13869/j.cnki.rswc.2024.05.038]
　Wei Yuchao,Chen Ziyu,Wang Ziyin,et al.A Study on the Sediment Source on Slope of Engineering Deposits by Rare Earth Element Tracer Method[J].Research of Soil and Water Conservation,2024,31(05):9-17.[doi:10.13869/j.cnki.rswc.2024.05.038]
点击复制

基于REE示踪法的工程堆积体坡面泥沙来源研究

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 31 期数: 2024年05期 页码: 9-17 栏目: 出版日期: 2024-08-10
Title:
A Study on the Sediment Source on Slope of Engineering Deposits by Rare Earth Element Tracer Method
文章编号:
1005-3409(2024)05-0009-09
作者:
魏育超1,2,3, 陈姿宇4, 王子吟4, 魏宇航4, 张一博4, 王达未1,2,3, 谢永生2,4, 骆 汉2,4
(1.中国科学院 教育部水土保持与生态环境研究中心, 陕西 杨凌 712100; 2.中国科学院 水利部 水土保持研究所, 陕西 杨凌 712100; 3.中国科学院大学, 北京 100049; 4.西北农林科技大学 水土保持科学与工程学院, 陕西 杨凌 712100)
Author(s):
Wei Yuchao1,2,3, Chen Ziyu4, Wang Ziyin4, Wei Yuhang4, Zhang Yibo4, Wang Dawei1,2,3, Xie Yongsheng2,4, Luo Han2,4
(1.Research Center of Soil and Water Conservation and Ecological Environment, Chinese Academy of Sciences and Ministry of Education, Yangling, Shaanxi712100, China; 2.Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi712100, China; 3.University of Chinese Academy of Sciences, Beijing100049, China; 4.College of Soil and Water Conservation Science and Engineering, Northwest A&F University, Yangling, Shaanxi712100, China)
关键词:
土壤侵蚀;  REE;  砾石含量;  贡献率;  坡位
Keywords:
soil erosion;  rare earth element;  gravel content;  contribution rate;  slope position
分类号:
S157.1
DOI:
10.13869/j.cnki.rswc.2024.05.038
文献标志码:
A
摘要:
[目的]探究生产建设项目工程堆积体坡面侵蚀的泥沙来源,更有针对性地布设水土流失防治措施,减少人为扰动造成的水土流失。[方法]结合室内人工模拟降雨试验与REE(Rare Earth Elements)示踪技术,研究90 mm/h雨强下不同砾石含量〔0(纯土),10%,20%,30%〕工程堆积体坡面不同坡位的侵蚀特征及侵蚀贡献率。[结果](1)不同砾石含量堆积体各坡位侵蚀量均为下坡位最大,同时下坡位平均侵蚀贡献率(57.40%)大于上坡位和中坡位,表明下坡位是坡面泥沙的主要来源。(2)含砾石堆积体坡面中坡位和下坡位的侵蚀量显著小于纯土堆积体。含砾石堆积体坡面上坡位和中坡位的侵蚀贡献率显著+大于纯土堆积体坡面,下坡位侵蚀贡献率显著小于纯土堆积体坡面。(3)砾石含量对下坡位侵蚀量和贡献率的影响更显著(p<0.05)。含砾石堆积体中,20%砾石含量堆积体坡面上坡位和下坡位的侵蚀量显著大于10%,30%砾石含量堆积体。10%砾石含量堆积体坡面上坡位侵蚀贡献率显著大于20%,30%砾石含量堆积体坡面,下坡位侵蚀贡献率显著小于20%,30%砾石含量堆积体坡面。[结论]各砾石含量工程堆积体坡面中,下坡位侵蚀贡献率均最大,表明下坡位是工程堆积体坡面泥沙的主要来源,要加强工程堆积体下坡位的防护和治理。
Abstract:
[Objective]The aims of this study are to investigate the sediment sources of slope erosion in production and construction projects, and to implement the targeted soil and water conservation measures to mitigate soil and water loss caused by human disturbance. [Methods]Indoor simulated rainfall tests combined with REE tracer technique were conducted to examine the erosion characteristics and contributions from different areas of engineering deposits with varying gravel contents 〔0(pure soil), 10%, 20%, 30%〕 under the rainfall intensity of 90 mm/h. [Results](1)The amount of soil erosion of all areas of different gravel-containing engineering deposits was the largest in the down slope area, while the average erosion contribution of the down slope area(57.40%)was larger than that of the upper slope area and the middle slope area, which indicated that the down slope area was the main source of sediment.(2)The erosion contribution of the middle and down slope areas of the gravel-containing engineering deposits was significantly smaller than that of the pure soil deposits. The erosion contribution of the upper and middle slope areas of the gravel-containing engineering deposits was significantly greater than that of the pure soil deposits, and the erosion contribution of the down slope area of the gravel-containing engineering deposits was significantly less than that of the pure soil deposits.(3)The effect of gravel content on the amount and contribution of erosion at the down slope area was more significant(p<0.05). In the gravel-containing engineering deposits, the amount of erosion at the upper and down slope areas of the 20% gravel content engineering deposits was significantly greater than that of engineering deposits with 10% and 30% gravel contents. The contribution of erosion at the upper slope area of the engineering deposit with 10% gravel content was significantly greater than that engineering deposits with 20% and 30% gravel contents, and the contribution of erosion at the down slope area was significantly less than that engineering deposits with 20% and 30% gravel contents. [Conclusion]Among all the engineering deposits with gravel content, the erosion contribution rate of the down slope area is the largest, which indicates that the down slope area is the main source of sediment on the slope of the engineering deposits, and the protection and treatment of the down slope area should be strengthened.

参考文献/References:

[1]邹小阳,周旺,孙文俊,等.工程堆积体土壤侵蚀影响因素国内研究进展[J].东北农业科学,2021,46(1):57-61.
Zou X Y, Zhou W, Sun W J, et al. Research progress on influencing factors of soil erosion of engineering accumulation body in China[J]. Journal of Northeast Agricultural Sciences, 2021,46(1):57-61.
[2]刘衡秋,胡瑞林.大型复杂松散堆积体形成机制的内外动力耦合作用初探[J].工程地质学报,2008,16(3):291-297.
Liu H Q, Hu R L. Coupling of earth's endogenic and exogenic geological processes on formation mechanism of large-scale loose complex quaternary deposits in western China[J]. Journal of Engineering Geology, 2008,16(3):291-297.
[3]康宏亮,王文龙,薛智德,等.陕北风沙区含砾石工程堆积体坡面产流产沙试验[J].水科学进展,2016,27(2):256-265.
Kang H L, Wang W L, Xue Z D, et al. Experimental study on runoff and sediment yield from engineering deposition with gravel in the northern windy-sandy region, Shaanxi[J]. Advances in Water Science, 2016,27(2):256-265.
[4]吕佼容,张文博,胡锦昇,等.连续降雨下不同砾石含量工程堆积体土壤侵蚀[J].水科学进展,2019,30(2):210-219.
Lyu J R, Zhang W B, Hu J S, et al. Effects of rock fragment content on erosion characteristics of spoil heaps under multiple rainfall events[J]. Advances in Water Science, 2019,30(2):210-219.
[5]Wang X Y, Li Z X, Cai C F, et al. Effects of rock fragment cover on hydrological response and soil loss from Regosols in a semi-humid environment in South-West China[J]. Geomorphology, 2012,151/152:234-242.
[6]史倩华,王文龙,郭明明,等.模拟降雨条件下含砾石红壤工程堆积体产流产沙过程[J].应用生态学报,2015,26(9):2673-2680.
Shi Q H, Wang W L, Guo M M, et al. Runoff and sediment yielding processes on red soil engineering accumulation containing gravels by a simulated rainfall experiment[J]. Chinese Journal of Applied Ecology, 2015,26(9):2673-2680.
[7]李瑞栋,王文龙,娄义宝,等.模拟降雨条件下砾石含量对塿土工程堆积体坡面产流产沙的影响[J].应用生态学报,2022,33(11):3027-3036.
Li R D, Wang W L, Lou Y B, et al. Effects of gravel content on runoff and sediment yield on Lou soil engineering accumulation slopes under simulated rainfall conditions[J]. Chinese Journal of Applied Ecology, 2022,33(11):3027-3036.
[8]张文博,吕佼容,谢永生,等.不同形态工程堆积体产流产沙对比研究[J].水土保持学报,2020,34(3):49-54.
Zhang W B, Lü J R, Xie Y S, et al. Comparative study on runoff and sediment yielding in different morphological engineering accumulations[J]. Journal of Soil and Water Conservation, 2020,34(3):49-54.
[9]丁亚东,谢永生,景民晓,等.轻壤土散乱锥状堆置体侵蚀产沙规律研究[J].水土保持学报,2014,28(5):31-36.
Ding Y D, Xie Y S, Jing M X, et al. Study on sediment erosion law of conical scattered spoilbank of light loam[J]. Journal of Soil and Water Conservation, 2014,28(5):31-36.
[10]戎玉博,白玉洁,王森,等.含砾石锥状工程堆积体坡面径流侵蚀特征[J].水土保持学报,2018,32(1):109-115.
Rong Y B, Bai Y J, Wang S, et al. Characteristics of slope runoff erosion on the cone shaped engineering accumulation with gravel[J]. Journal of Soil and Water Conservation, 2018,32(1):109-115.
[11]王雪松,谢永生,陈曦,等.模拟降雨条件下工程堆积体产流产沙特征研究[J].泥沙研究,2015(4):74-80.
Wang X S, Xie Y S, Chen X, et al. Study on runoff and sediment yield of a spoil pile under simulated rainfall condition[J]. Journal of Sediment Research, 2015(4):74-80.
[12]陈卓鑫,王文龙,康宏亮,等.砾石对红壤工程堆积体边坡径流产沙的影响[J].生态学报,2019,39(17):6545-6556.
Chen Z X, Wang W L, Kang H L, et al. Effects of gravel on runoff and sediment yield of red soil engineering accumulation slopes[J]. Acta Ecologica Sinica, 2019,39(17):6545-6556.
[13]汤振权,刘刚,许文年.稀土元素示踪技术及其在土壤侵蚀研究中的应用[J].中国稀土学报,2011,29(5):515-522.
Tang Z Q, Liu G, Xu W N. REE tracing method and application in soil erosion[J]. Journal of the Chinese Society of Rare Earths, 2011,29(5):515-522.
[14]王瑄,李占斌,尚佰晓.利用REE示踪法分析坡面放水冲刷的侵蚀过程[J].沈阳农业大学学报,2008,39(2):218-222.
Wang X, Li Z B, Shang B X. Soil erosion process of the slope scouring with REE tracer method[J]. Journal of Shenyang Agricultural University, 2008,39(2):218-222.
[15]Zhu M Y, Tan S D, Dang H S, et al. Rare earth elements tracing the soil erosion processes on slope surface under natural rainfall[J]. Journal of Environmental Radioactivity, 2011,102(12):1078-1084.
[16]Zhang X C, Friedrich J M, Nearing M A, et al. Potential use of Rare Earth Oxides as Tracers for Soil Erosion and Aggregation Studies[J]. Soil Science Society of America Journal, 2001,65(5):1508-1515.
[17]田均良.侵蚀泥沙坡面沉积研究初报[J].水土保持研究,1997,4(2):57-63.
Tian J L. A primary report for a study on deposition of erosion sediments on slope[J]. Research of Soil and Water Conservation, 1997,4(2):57-63.
[18]武春龙,刘普灵,郑世清,等.坡面土壤侵蚀垂直分布定量分析研究[J].水土保持研究,1997,4(2):34-40.
Wu C L, Liu P L, Zheng S Q, et al. Study on vertical distribution of soil erosion on loess slope[J]. Research of Soil and Water Conservation, 1997,4(2):34-40.
[19]赵晓光,石辉.用稀土元素示踪方法研究裸露坡面沿程侵蚀与沉积[J].林业科学,2003,39(2):98-101.
Zhao X G, Shi H. Study on erosion and sediment along the bare sloping surfact with ree method[J]. Scientia Silvae Sinicae, 2003,39(2):98-101.
[20]唐泽军,雷廷武,张晴雯,等.稀土元素(REE)示踪土壤侵蚀动态过程的降雨模拟试验研究[J].农业工程学报,2006,22(3):32-35.
Tang Z J, Lei T W, Zhang Q W, et al. Rain simulation of dynamic soil erosion processes with rare earth element tracers[J]. Transactions of the Chinese Society of Agricultural Engineering, 2006,22(3):32-35.
[21]肖海,刘刚,许文年,等.利用稀土元素示踪三峡库区小流域模型泥沙来源[J].水土保持学报,2014,28(1):47-52.
Xiao H, Liu G, Xu W N, et al. Using REE to trace sediment source from simulated watershed in Three Gorges Reservoir region[J]. Journal of Soil and Water Conservation, 2014,28(1):47-52.
[22]刘普灵,田均良,周佩华,等.土壤侵蚀稀土元素示踪法实验研究[J].稀土,2001,22(2):37-40.
Liu P L, Tian J L, Zhou P H, et al. Experimental study on soil erosion by stable rare earth element tracer method[J]. Chinese Rare Earths, 2001,22(2):37-40.
[23]董亮.基于REE示踪法的露天煤矿排土场土壤侵蚀过程研究[D].阜新:辽宁工程技术大学,2020.
Dong L. A Study on Soil Erosion Process in Open-Pit Coal Mine Dump Based on REE Trace Method[D].Fuxin, Liaoning:Liaoning Technical University, 2020.
[24]李雅琦,吴普特,刘普灵,等.REE示踪法研究土壤侵蚀的室内模拟试验[J].水土保持研究,1997,4(2):26-33.
Li Y Q, Wu P T, Liu P L, et al. Simulation experiments to study soil erosion by REE tracer method[J]. Research of Soil and Water Conservation, 1997,4(2):26-33.
[25]Fang H Y, Sun L Y, Tang Z H. Effects of rainfall and slope on runoff, soil erosion and rill development:An experimental study using two loess soils[J]. Hydrological Processes, 2015,29(11):2649-2658.
[26]Lv J R, Luo H, Xie Y S. Effects of rock fragment content, size and cover on soil erosion dynamics of spoil heaps through multiple rainfall events[J]. Catena, 2019,172:179-189.
[27]王宁,杨春雨,张刚,等.黑土区土壤侵蚀的REE示踪法研究[J].地理科学,2008,28(4):565-570.
Wang N, Yang C Y, Zhang G, et al. Soil erosion of soil REE tracer study[J]. Scientia Geographica Sinica, 2008,28(4):565-570.
[28]Kimoto A, Nearing M A, Zhang X C, et al. Applicability of rare earth element oxides as a sediment tracer for coarse-textured soils[J]. Catena, 2006,65(3):214-221.
[29]余海龙,黄菊莹.砂田砾石覆盖对土壤大孔隙特征及其土壤水文过程的影响研究进展[J].水土保持研究,2012,19(4):284-288.
Yu H L, Huang J Y. Research progress on influence of mulching gravel and sand on soil macropore characteristics and soil hydrological process of gravel-sand mulch field[J]. Research of Soil and Water Conservation, 2012,19(4):284-288.
[30]薛亚洲,刘普灵,杨明义,等.REE示踪研究坡面侵蚀时空演变过程[J].中国稀土学报,2004,22(5):698-703.
Xue Y Z, Liu P L, Yang M Y, et al. Using rare earth element as tracers for studying spatial and temporal process of soil erosion in sloping land[J]. Journal of the Chinese Rare Earth Society, 2004,22(5):698-703.
[31]Liu P L, Tian J L, Zhou P H, et al. Stable rare earth element tracers to evaluate soil erosion[J]. Soil and Tillage Research, 2004,76(2):147-155.
[32]魏天兴,朱金兆.黄土残塬沟壑区坡度和坡长对土壤侵蚀的影响分析[J].北京林业大学学报,2002,24(1):59-62.
Wei T X, Zhu J Z. Effects of slope length and grade on soil erosion in the Gully Regions in Loess Plateau[J]. Journal of Beijing Forestry University, 2002,24(1):59-62.
[33]杨苗苗,杨勤科,张科利,等.砾石含量对土壤可蚀性因子估算的影响[J].土壤学报,2021,58(5):1157-1168.
Yang M M, Yang Q K, Zhang K L, et al. Effects of content of soil rock fragments on calculating of soil erodibility[J]. Acta Pedologica Sinica, 2021,58(5):1157-1168.
[34]马晨雷,戴翠婷,刘窑军,等.砾石覆盖对紫色土坡面流水动力学参数的影响[J].水土保持学报,2019,33(6):150-155,161.
Ma C L, Dai C T, Liu Y J, et al. Effects of gravel covering on hydraulic characteristics of slope flow on purple soil[J]. Journal of Soil and Water Conservation, 2019,33(6):150-155,161.
[35]周蓓蓓,邵明安.不同碎石含量及直径对土壤水分入渗过程的影响[J].土壤学报,2007,44(5):801-807.
Zhou B B, Shao M A. Effect of content and size of rock detritus on infiltration[J]. Acta Pedologica Sinica, 2007,44(5):801-807.

相似文献/References:

[1]宋玥,张忠学.不同耕作措施对黑土坡耕地土壤侵蚀的影响[J].水土保持研究,2011,18(02):14.
　SONG Yue,ZHANG Zhong-xue.The Effect of Different Tillage Measures on Soil Erosion in Slope Farmland in Black Soil Region[J].Research of Soil and Water Conservation,2011,18(05):14.
[2]裴会敏,许明祥,李强,等.侵蚀条件下土壤有机碳流失研究进展[J].水土保持研究,2012,19(06):269.
　PEI Hui-min,XU Ming-xiang,LI Qiang,et al.Advances in Soil Organic Carbon Losses under Erosion[J].Research of Soil and Water Conservation,2012,19(05):269.
[3]赵玉明,刘宝元,姜洪涛.东北黑土区垄向的分布及其对土壤侵蚀的影响[J].水土保持研究,2012,19(05):1.
　ZHAO Yu-ming,LIU Bao-yuan,JIANG Hong-tao.Distribution of Tillage-induced Direction and Its Effect on Soil Erosion in Black Soil Area of Northeast China[J].Research of Soil and Water Conservation,2012,19(05):1.
[4]袁靓,高华端,张旭贤,等.基于土壤侵蚀的贵阳市喀斯特地区基岩层间节理研究[J].水土保持研究,2012,19(05):167.
　YUAN Jing,GAO Hua-duan,ZHANG Xu-xian,et al.Research on the Interlayer Joints of Bedrock in the Karst Region of Guiyang City Based on Soil Erosion[J].Research of Soil and Water Conservation,2012,19(05):167.
[5]泮雪芹,刘占仁,孟晓云,等.云蒙湖流域不同土地利用类型的土壤侵蚀特征分析[J].水土保持研究,2012,19(04):6.
　PAN Xue-qin,LIU Zhan-ren,MENG Xiao-yun,et al.Analysis on Features of Soil Erosion with Different Land Uses in the Yunmeng Lake Watershed[J].Research of Soil and Water Conservation,2012,19(05):6.
[6]朱志玲,吴咏梅,张敏.基于GIS的宁夏生态环境敏感性综合评价[J].水土保持研究,2012,19(04):101.
　ZHU Zhi-ling,WU Yong-mei,ZHANG Min.Comprehensive Evaluation on Eco-environment Sensibility of Ningxia Hui Autonomous Region Based on GIS[J].Research of Soil and Water Conservation,2012,19(05):101.
[7]李瑞,李勇,刘云芳.贵州喀斯特地区降雨与坡面土壤侵蚀关系研究[J].水土保持研究,2012,19(03):7.
　LI Rui,LI Yong,LIU Yun-fang.Study of Rainfall and Soil Erosion on Slope in Karst Region of Guizhou Province[J].Research of Soil and Water Conservation,2012,19(05):7.
[8]程峥,姚志宏,张婧,等.南方红壤农作区数字流域建立和应用[J].水土保持研究,2012,19(03):12.
　CHENG Zheng,YAO Zhi-hong,ZHANG Jing,et al.Establishment and Application of Digital Watershed in the Red Earth Areas, Southern China[J].Research of Soil and Water Conservation,2012,19(05):12.
[9]董磊,彭明春,王崇云,等.基于USLE和GIS/RS的滇池流域土壤侵蚀研究[J].水土保持研究,2012,19(02):11.
　DONG Lei,PENG Ming-chun,WANG Chong-yun,et al.Research on Soil Erosion Based on the USLE Model and RS/GIS in the Dianchi Lake Watershed[J].Research of Soil and Water Conservation,2012,19(05):11.
[10]陈宇,焦菊英,王宁,等.黄土丘陵区撂荒地不同侵蚀带土壤种子库特征[J].水土保持研究,2012,19(01):1.
　CHEN Yu,JIAO Ju-ying,WANG Ning,et al.Characteristics of Soil Seed Banks under Different Erosion Zones on Abandoned Land in the Hilly-gullied Loess Plateau[J].Research of Soil and Water Conservation,2012,19(05):1.

备注/Memo

收稿日期:2023-12-02 修回日期:2024-01-02
资助项目:四川省交通运输科技项目(2018-ZL-15); 国家自然科学基金(41601300)
第一作者:魏育超(1996—),男,陕西渭南人,硕士研究生,研究方向为水土保持工程。E-mail:yuc21_pa@163.com
通信作者:骆汉(1985—),男,山东淄博人,副研究员,博士生导师,主要从事水土保持工程研究。E-mail:hanl@ms.iswc.ac.cn

更新日期/Last Update: 2024-08-10