Sorting Characteristics of Black Soil Splash Erosion Aggregates Under Intermittent Rainfall Conditions

HANG Xiaoya; XUJinzhong; YANG Qingnan; LEI Hanzhe; ZHAO Yikai; LI Yu; ZHANG Yupeng; FU Yu

doi:10.13870/j.cnki.stbcxb.2024.05.018

您当前的位置：

首页 >

文章列表页 >

Sorting Characteristics of Black Soil Splash Erosion Aggregates Under Intermittent Rainfall Conditions

更新时间：2025-02-18

- Sorting Characteristics of Black Soil Splash Erosion Aggregates Under Intermittent Rainfall Conditions
- Vol. 38, Issue 5, Pages: 31-39(2024)
- 作者机构：
  
  1. 东北林业大学林学院,哈尔滨,150040
  2. 黑龙江省水利科学研究院水土保持研究所,哈尔滨,150070
  3. 黑龙江省水土保持重点实验室,哈尔滨,150070
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2024.05.018
  CLC： S157.1
- Published：2024
- 稿件说明：
移动端阅览
HANG Xiaoya, XUJinzhong, YANG Qingnan, et al. Sorting Characteristics of Black Soil Splash Erosion Aggregates Under Intermittent Rainfall Conditions[J]. 2024, 38(5): 31-39.
DOI：

HANG Xiaoya, XUJinzhong, YANG Qingnan, et al. Sorting Characteristics of Black Soil Splash Erosion Aggregates Under Intermittent Rainfall Conditions[J]. 2024, 38(5): 31-39. DOI： 10.13870/j.cnki.stbcxb.2024.05.018.

摘要

[目的] 为探究间歇性降雨对黑土溅蚀量和溅蚀分选特征的影响。[方法] 基于人工模拟降雨试验

设计2个降雨强度(40

70 mm/h)

每个降雨强度5场降雨

分析不同降雨条件下黑土溅蚀量和溅蚀团聚体粒径分布特征。[结果] 2种降雨强度下

不同降雨场次土壤表层存在“无结皮—弱结皮—强结皮—弱结皮—新结皮”强弱交替的结皮动态发育过程。2种降雨强度下

溅蚀团聚体MWD和GMD均在第4场降雨出现最大值

在第1次降雨出现最小值。每场降雨5~2 mm粒级的团聚体均基本未发生迁移

溅蚀团聚体均以2~0.25 mm粒径为主

分别占2种降雨强度溅蚀量的36.49%~58.61%和49.10%~60.09%。5场降雨的溅蚀量随粒径减小呈先增加后减小的变化趋势

而粒径<0.053 mm质量百分数随间歇次数增加的变化趋势为先降低再增加

粒径<0.053 mm质量百分数均在第3场降雨出现最小值

分别为18.21%和17.63%。[结论] 降雨导致土壤结皮的形成

且随降雨次数的增加结皮厚度呈现动态变化

在第3场降雨土壤结皮厚度最大

此时溅蚀量有最小值

且主要以>0.053 mm为主。研究结果为东北黑土区土壤水蚀机理研究提供参考。

Abstract

[Objective] To investigate the impact of intermittent rainfall on the amount and sorting characteristics of black soil splash erosion. [Methods] This study is based on artificial simulated rainfall experiments

with two rainfall intensities (40

70 mm/h) designed

each with 5 rainfall events

to analyze the splashing erosion amount and particle size distribution characteristics of black soil under different rainfall conditions. [Results] Under two different rainfall intensities

there is a dynamic development process of alternating strength between "no crust weak crust strong crust weak crust new crust" in the soil surface layer of different rainfall sites. Under two different rainfall intensities

the maximum values of splashed aggregate MWD and GMD appeared in the fourth rainfall

and the minimum values appeared in the first rainfall. The agglomerates with a particle size of 5~2 mm did not migrate in each rainfall

and the splashed agglomerates were mainly composed of particles with a size of 2~0.25 mm

accounting for 36.49%~58.61% and 49.10%~60.09% of the splashed erosion amounts of the two rainfall intensities

respectively. The erosion amount of the five rainfall events showed a trend of first increasing and then decreasing with the decrease of particle size

while the mass percentage with particle size <0.053 mm showed a trend of first decreasing and then increasing with the increase of intermittent frequency. The mass percentage with particle size <0.053 mm all showed the minimum value in the third rainfall event

which was 18.21% and 17.63%

respectively. [Conclusion]Rainfall can lead to the formation of soil crust

and the thickness of soil crust shows dynamic changes with the increase of rainfall frequency. In the third rainfall

the soil crust thickness is the highest

and at this time

the splash erosion amount has the minimum value

mainly greater than 0.053 mm. The research results provide reference for the study of soil water erosion mechanism in the black soil area of Northeast China.

关键词

Keywords

references

LADO M, BEN-HUR M, SHAINBERG I. Soil wetting and texture effects on aggregate stability, seal formation, and erosion[J].Soil Science Society of America Journal,2004,68(6):1992-1999.

赵勇钢,赵世伟,曹丽花,等.半干旱典型草原区退耕地土壤结构特征及其对入渗的影响[J].农业工程学报,2008,24(6):14-20. ZHAO Y G, ZHAO S W, CAO L H, et al. Soil structural characteristics and its effect on infiltration on abandoned lands in semi-arid typical grassland areas[J].Transactions of the Chinese Society of Agricultural Engineering,2008,24(6):14-20.

韦自强,伊怀虎,任鹏,等.大兴安岭重度火烧迹地植被恢复后土壤团聚体稳定性及有机碳特征[J].森林工程,2023,39(4):19-28. WEI Z Q, YI H H, REN P, et al. Soil aggregates stability and organic carbon characteristics after vegetation restoration of burned areas in greater khingan mountains[J].Forest Engineering,2023,39(4):19-28.

郑粉莉,高学田.坡面土壤侵蚀过程研究进展[J].地理科学,2003,23(2):230-235. ZHENG F L, GAO X T. Research progresses in hillslope soil erosion processes[J].Scientia Geographica Sinica,2003,23(2):230-235.

肖海,刘刚,赵金凡,等.雨滴机械打击和消散作用对土壤团聚体的破坏特征[J].土壤学报,2017,54(4):827-835. XIAO H, LIU G, ZHAO J F, et al. Characteristics of mechanical impact and slaking effect of rain drops on soil aggregates[J].Acta Pedologica Sinica,2017,54(4):827-835.

阎百兴,杨育红,刘兴土,等.东北黑土区土壤侵蚀现状与演变趋势[J].中国水土保持,2008(12):26-30. YAN B X, YANG Y H, LIU X T, et al. Present status of soil erosion and evolution tendency of black soil region of northeast[J].Soil and Water Conservation in China,2008(12):26-30.

温磊磊,郑粉莉,沈海鸥,等.东北典型黑土区农耕土壤团聚体流失特征[J].土壤学报,2015,52(3):489-498. WEN L L, ZHENG F L, SHEN H O, et al. Characteristics of soil aggregate loss in croplands in the typical black soil region of Northeast China[J].Acta Pedologica Sinica,2015,52(3):489-498.

ZHAO Y K, WANG H, CHEN X W, et al. Effect of rainfall on soil aggregate breakdown and transportation on cultivated land in the black soil region of Northeast China[J].Sustainability,2022,14(17):e11028.

程金花,秦越,张洪江,等.华北土石山区模拟降雨下土壤溅蚀研究[J].农业机械学报,2015,46(2):153-161. CHENG J H, QIN Y, ZHANG H J, et al. Splash erosion under artificial rainfall in rocky mountain area of Northern China[J].Transactions of the Chinese Society for Agricultural Machinery,2015,46(2):153-161.

FU S H, LIU B Y, LIU H P, et al. The effect of slope on interrill erosion at short slopes[J].Catena,2011,84(1/2):29-34.

FU Y, LI G L, ZHENG T H, et al. Splash detachment and transport of loess aggregate fragments by raindrop action[J].Catena,2017,150:154-160.

HU F N, LIU J F, XU C Y, et al. Soil internal forces initiate aggregate breakdown and splash erosion[J].Geoderma,2018,320:43-51.

李叶鑫,吕刚,王道涵,等.煤矿复垦排土场裂缝区土壤团聚体分布及稳定性[J].灌溉排水学报,2023,42(6):104-110. LI Y X, LYU G, WANG D H, et al. Distribution and stability of soil aggregates over the fissure zones in reclaimed coal mining waste dumpsite[J].Journal of Irrigation and Drainage,2023,42(6):104-110.

吴发启,范文波.土壤结皮与降雨溅蚀的关系研究[J].水土保持学报,2001,15(3):1-3. WU F Q, FAN W B. Study on relationship of soil crust and rainfall splash[J].Journal of Soil Water Conservation,2001,15(3):1-3.

王辉,王全九,邵明安,等.表土结皮影响坡地产流产沙及养分流失的试验研究[J].水土保持学报,2008,22(4):35-38. WANG H, WANG Q J, SHAO M A, et al. Impact of soil crust on runoff, sediment and nutrient loss from sloping land[J].Journal of Soil and Water Conservation,2008,22(4):35-38.

蒋芳市,黄炎和,林金石,等.不同结皮条件对崩岗崩积体坡面侵蚀的影响[J].水土保持学报,2014,28(3):1-6. JIANG F S, HUANG Y H, LIN J S, et al. Effects of soil crust on the erosion of colluvial deposits in granite Benggang[J].Journal of Soil and Water Conservation,2014,28(3):1-6.

秦越,程金花,张洪江,等.北京市褐土区降雨参数对土壤溅蚀的影响[J].水土保持学报,2013,27(6):16-20. QIN Y, CHENG J H, ZHANG H J, et al. Effect of rainfall parameters on splash erosion in loamy soil of Beijing[J].Journal of Soil and Water Conservation,2013,27(6):16-20.

詹敏,厉占才,信玉林.黑土侵蚀区降雨参数与土壤流失关系[J].黑龙江水专学报,1998(1):40-43. ZHAN M, LI Z C, XIN Y L. On the relationship between precipitation parameter and soil erosion[J].Journal of Heilongjiang Hydraulic Engineering College,1998(1):40-43.

张宪奎,许靖华,卢秀琴,等.黑龙江省土壤流失方程的研究[J].水土保持通报,1992,12(4):1-9. ZHANG X K, XU J H, LU X Q, et al. A study on the soil loss equation in Heilongjiang Province[J].Bulletin of Soil and Water Conservation,1992,12(4):1-9.

宁静,周杰,周芳琪.基于变权物元模型的黑土区土壤侵蚀风险评价[J].江苏农业科学,2022,50(15):203-209. NING J, ZHOU J, ZHOU F Q. Risk assessment of soil erosion in black soil area based on variable weight matter element[J].Jiangsu Agricultural Sciences,2022,50(15):203-209.

姜义亮,郑粉莉,温磊磊,等.降雨和汇流对黑土区坡面土壤侵蚀的影响试验研究[J].生态学报,2017,37(24):8207-8215. JIANG Y L, ZHENG F L, WEN L L, et al. An experimental study on the impacts of rainfall and inflow on hillslope soil erosion in typical black soil regions[J].Acta Ecologica Sinica,2017,37(24):8207-8215.

周一杨.典型黑土击溅侵蚀特征的研究[D].哈尔滨:东北林业大学,2009. ZHOU Y Y.Characters of soil splash erosion of typical black soil region[D].Harbin: Northeast Forestry University,2009.

石璞, YANG C,赵鹏志.间歇性降雨对土壤团聚体粒级及磷、铜、锌富集的影响[J].土壤学报,2021,58(4):948-956. SHI P, YANG C, ZHAO P Z. Effect of intermittent rainfall on size distribution and phosphorus, copper and zinc enrichment of soil aggregates[J].Acta Pedologica Sinica,2021,58(4):948-956.

张晓平,梁爱珍,申艳,等.东北黑土水土流失特点[J].地理科学,2006,26(6):687-692. ZHANG X P, LIANG A Z, SHEN Y, et al. Erosion characteristics of black soils in Northeast China[J].Scientia Geographica Sinica,2006,26(6):687-692.

ZHU X C, LIANG Y, CAO L X, et al. Pore characteristics of physical crust samples from two typical erodible soils in Southern China[J].European Journal of Soil Science,2022,73(2):e13234.

FU Y, LI G L, ZHENG T H, et al. Fragmentation of soil aggregates induced by secondary raindrop splash erosion[J].Catena,2020,185:e104342.

张兴义,乔宝玲,李健宇,等.降雨强度和坡度对东北黑土区顺坡垄体溅蚀特征的影响[J].农业工程学报,2020,36(16):110-117. ZHANG X Y, QIAO B L, LI J Y, et al. Effects of rainfall intensity and slope on splash erosion characteristics of downslope ridge on farmland in black soil areas of Northeast China[J].Transactions of the Chinese Society of Agricultural Engineering,2020,36(16):110-117.

LI Y X, LV G, FU X Y, et al. Effects of rainfall characteristics and slope on splash erosion of cinnamon soil on slope farmland in low mountain and hilly region of western Liaoning Province[J].Journal of Soil and Water Conservation,2019,33(4):37-43.

HU W, ZHENG F L, BIAN F. The directional components of splash erosion at different raindrop kinetic energy in the Chinese mollisol region[J].Soil Science Society of America Journal,2016,80(5):1329-1340.

刘窑军,杨广勇,徐铭泽,等.鄱阳湖流域3种典型母质发育红壤溅蚀特征[J].水土保持学报,2019,33(2):55-59. LIU Y J, YANG G Y, XU M Z, et al. Splash erosion features of three red soils in Poyang Lake basin[J].Journal of Soil and Water Conservation,2019,33(2):55-59.

张转敏,王彬,饶伟,等.初始含水率和降雨能量对黑土团聚体溅蚀特征的影响[J].水土保持学报,2024,38(2):68-75. ZHANG Z M, WANG B, RAO W, et al. Impact of initial soil moisture and rainfall energy on splash erosion characteristics of black soil aggregate[J].Journal of Soil and Water Conservation,2024,38(2):68-75.

张媛静.基于能量分析的不同类型土壤抗侵蚀特征研究[D].武汉:长江科学院,2010. ZHANG Y J. Study on anti-erosion characteristics of different types of soils based on energy analysis[D].Wuhan: Changjiang River Scientiffic Research Institute,2010.

FALSONE G, BONIFACIO E, ZANINI E. Structure development in aggregates of poorly developed soils through the analysis of the pore system[J].Catena,2012,95:169-176.

ARJMAND SAJJADI S, MAHMOODABADI M. Aggregate breakdown and surface seal development influenced by rain intensity, slope gradient and soil particle size[J].Solid Earth,2015,6(1):311-321.

陈正发,夏清,史东梅,等.基于模拟降雨的土壤表土结皮特征及坡面侵蚀响应[J].水土保持学报,2011,25(4):6-11. CHEN Z F, XIA Q, SHI D M, et al. Soil surface crust characteristic and response feature to slope erosion base on simulation rainfall[J].Journal of Soil and Water Conservation,2011,25(4):6-11.

卜崇峰. 黄土水蚀风蚀区土壤结皮的发育特征及其侵蚀效应研究[D].陕西杨凌:西北农林科技大学,2010. BU C F. Research on the development characteristics and erosion effects of soil crust in loess water and wind erosion areas[D].Yangling, Shaanxi: Northwest A&F University,2010.

朱远达,蔡强国,胡霞,等.土壤理化性质对结皮形成的影响[J].土壤学报,2004,41(1):13-19. ZHU Y D, CAI Q G, HU X, et al. Effects of soil physical and chemical properties on soil crusting[J].Acta Pedologica Sinica,2004,41(1):13-19.

马仁明,王军光,李朝霞,等.降雨过程中红壤团聚体粒径变化对溅蚀的影响[J].长江流域资源与环境,2013,22(6):779-785. MA R M, WANG J G, LI Z X, et al. Effects of dynamic distribution of aggregate size on splash erosion under rainfall in red soils[J].Resources and Environment in the Yangtze Basin,2013,22(6):779-785.

范文波.坡耕地土壤结皮的成因及其作用研究[D].陕西杨凌:西北农林科技大学,2001. FAN W B. Study on the causes and functions of soil crust on sloping farmland[D].Yangling, Shaanxi: Northwest A&F University,2001.

乔宝玲.典型黑土农田垄体溅蚀特征研究[D].哈尔滨:东北农业大学,2021. QIAO B L. Splash erosion characteristics of ridge body on farmland in the typical black soil region of northeast China[D].Harbin: Northeast Agricultural University,2021.

郭伟,史志华,陈利顶,等.不同湿润速率对三种红壤坡面侵蚀过程的影响[J].土壤学报,2008,45(1):26-31. GUO W, SHI Z H, CHEN L D, et al. Effects of wetting rate on erosion processes on hillslopes of red soil[J].Acta Pedologica Sinica,2008,45(1):26-31.

张逸飞,汪零,徐玲,等.降雨驱动下红壤团聚体的溅蚀特征及周转过程[J].水土保持研究,2023,30(4):27-33. ZHANG Y F, WANG L, XU L, et al. Splash erosion characteristics and turnover process of red soil aggregates driven by rainfall[J].Research of Soil and Water Conservation,2023,30(4):27-33.

SAEDI T, SHORAFA M, GORJI M, et al. Indirect and direct effects of soil properties on soil splash erosion rate in calcareous soils of the central Zagross, Iran: A laboratory study[J].Geoderma,2016,271:1-9.

景可, 黄河中游侵蚀环境特征和变化趋势. 北京市, 中国科学院地理科学与资源研究所, 2005-01-01.

LI G L, FU Y, LI B Q, et al. Micro-characteristics of soil aggregate breakdown under raindrop action[J].Catena,2018,162:354-359.

CHEN L, YANG C, ZHANG Q W, et al. Variations in the disintegration rate of physical crusts induced by artificial rainfall in different alcohol concentrations[J].International Soil and Water Conservation Research,2022,10(4):565-573.

LIU B L, CAI Q G, SHI Z H, et al. Rain-simulated experiment study on the splash erosion characteristics of lou soil[J].Journal of Soil and Water Conservation,2016,31(5):29-33.

程琴娟,蔡强国,李家永.表土结皮发育过程及其侵蚀响应研究进展[J].地理科学进展,2005,24(4):114-122. CHENG Q J, CAI Q G, LI J Y. Summarization on study of soil surface crust or sealing and its effects on erosion[J].Progress In Geography,2005,24(4):114-122.

吴新亮,魏玉杰,李朝霞,等.亚热带地区几种红壤坡面侵蚀泥沙的物质组成特性[J].土壤学报,2014,51(6):1223-1233. WU X L, WEI Y J, LI Z X, et al. Composition of sediments of erosion from different red soil slopes in subtropical area[J].Acta Pedologica Sinica,2014,51(6):1223-1233.

赵迎松.雨滴击溅下薄层径流对土壤团聚体破碎、迁移的影响[D].陕西杨凌:西北农林科技大学,2019. ZHAO Y S. The effect of shallow overland flow on breakdown and transport of soil aggregates under raindrop action[D].Yangling, Shaanxi: Northwest A&F University,2019.

路培, 王林华, 吴发启. 不同降雨强度下土壤结皮强度对侵蚀的影响[J]. 农业工程学报, 2017, 33(8): 141-146. LU P, WANG L H, WU F Q. Effect of soil crust strength on erosion under different rainfall intensity[J].Transactions of the Chinese Society of Agricultural Engineering,2017,33(8):141-146.

胡伟.我国主要侵蚀土壤溅蚀和片蚀特征与机理研究[D].北京:中国科学院研究生院(教育部水土保持与生态环境研究中心),2016. HU W. Characteristics and mechanisms of splash eroison and sheet erosion on hillslope of main typical eroded soils in China[D].Beijing: Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences,2016.

Views

175

下载量

CSCD

Alert me when the article has been cited

提交

Tools

Publicity Resources

Effects of Maize Intercropping with Hairy Vetch and Rye on Soil Organic Carbon and Its Fractions

Response of Velocity and Sediment Production Characteristics of Spoil Heaps to Slope Length and Gravel Action

Response of Enzyme Activity Characteristics of Forest Soil Aggregates to Nitrogen Deposition in Central Yunnan Based on Dry and Wet Screening Metho

Splash Erosion of Aggregate in Different Particle-size under Simulated Rainfall in Red Soils

Effects of Freeze-thaw Cycles on Brown Soil Aggregates and Cadmium Transformations Within Particle Size Fractions

Related Author

BAO Xuelian

BA Xiaobo

YU Yang

NING Peng

LUO Jiaqiao

YANG Lu

LIAO Pan

LI Jianming

Related Institution

University of Chinese Academy of Sciences

Institute of Applied Ecology， Chinese Academy of Sciences

Oil Crops Research Institute， Chinese Academy of Agricultural Sciences， Key Laboratory of Biology and Genetic Improvement of Oil Crops， Ministry of Agriculture and Rural Affairs

College of Resources and Environment， China Agricultural University

Yangtze River Academy of Sciences of Yangtze River Water Resources Commission

⁰