东北黑土区融雪径流侵蚀力时空分布

王鑫雨; 范昊明

doi:10.13870/j.cnki.stbcxb.2024.01.029

您当前的位置：

首页 >

文章列表页 >

东北黑土区融雪径流侵蚀力时空分布

更新时间：2025-03-12

- 东北黑土区融雪径流侵蚀力时空分布
- Spatial and Temporal Distribution of Snowmelt Runoff Erosivity in the Black Soil Area of Northeast China
- 水土保持学报 2024年38卷第1期页码：40-48
- 作者机构：
  
  沈阳农业大学水利学院,沈阳,110866
- 作者简介：
  
  [ "王鑫雨(1997—),女,硕士研究生,主要从事土壤侵蚀规律研究。E-mail:Eroswang33@163.com" ]
- 基金信息：
  
  国家重点研发计划项目(2021YFD1500701);国家自然科学基金项目(41371272)
- DOI：10.13870/j.cnki.stbcxb.2024.01.029
  中图分类号： S157.1
- 纸质出版：2024
- 稿件说明：
移动端阅览
王鑫雨, 范昊明. 东北黑土区融雪径流侵蚀力时空分布[J]. 水土保持学报, 2024,38(1):40-48.

WANG Xinyu, FAN Haoming. Spatial and Temporal Distribution of Snowmelt Runoff Erosivity in the Black Soil Area of Northeast China[J]. 2024, 38(1): 40-48.
王鑫雨, 范昊明. 东北黑土区融雪径流侵蚀力时空分布[J]. 水土保持学报, 2024,38(1):40-48. DOI： 10.13870/j.cnki.stbcxb.2024.01.029.

WANG Xinyu, FAN Haoming. Spatial and Temporal Distribution of Snowmelt Runoff Erosivity in the Black Soil Area of Northeast China[J]. 2024, 38(1): 40-48. DOI： 10.13870/j.cnki.stbcxb.2024.01.029.

摘要

[目的] 融雪侵蚀是东北黑土区主要土壤侵蚀形式之一

是该区土地退化的重要作用力

融雪径流侵蚀力是计算融雪径流侵蚀量的关键因子

因此研究融雪径流侵蚀力具有重要意义。融雪径流侵蚀力主要受积雪深度、辐射强度及升温速率影响

其主要驱动力包括融雪速率和地表径流作用。[方法] 通过计算近31年日均融雪径流侵蚀力

分析东北黑土区融雪径流侵蚀力时空分布特征

并利用地理探测器辨析各区域融雪径流侵蚀力的主要影响因子。[结果] 3个黑土亚区1990—2020年日均融雪径流侵蚀力均呈现先增大后减小态势

近些年逐步趋于稳定

多年日均融雪径流侵蚀力为0.01 (MJ·mm)/(hm2·h·a);空间上多年日均融雪径流侵蚀力在0~0.21 (MJ·mm)/(hm2·h·a)范围内

基本呈现中间小、四周大规律。融雪径流侵蚀力影响因子空间上表现为积雪深度北部大、南部小

太阳辐射强度呈现由西向东递减

升温速率值从北部向南部递减。通过地探测器辨析融雪径流侵蚀力影响因子作用强弱发现

升温速率对蒙东黑土亚区作用最强

而积雪深度对松嫩黑土亚区及三江黑土亚区作用最强。[结论] 通过分析1990—2020年东北黑土区融雪径流侵蚀力时空特征及其影响因子

对于深化研究区融雪径流侵蚀特征及融雪侵蚀防控具有一定的理论和实践意义。

Abstract

[Objective] Snowmelt erosion is one of the main forms of soil erosion in the black soil area of Northeast China

which plays an important role in land degradation in the area. The erosivity of snowmelt runoff is the key factor for calculating the erosion amount of snowmelt runoff

so it is of great significance to study the erosivity of snowmelt runoff. The erosivity of snowmelt runoff is mainly affected by snow depth

radiation intensity and warming rate

and its main driving forces include snowmelt rate and surface runoff. [Methods] The erosivity of daily average snowmelt runoff in the past 31 years was calculated

the temporal and spatial distribution characteristics of snowmelt runoff erosivity in the black soil area of Northeast China were analyzed

and the main influence factors of snowmelt runoff erosivity in each region were analyzed by using geographic detectors. [Results] The daily average snowmelt runoff erosivity in the three black soil subregions from 1990 to 2020 showed a trend of first increasing and then decreasing

and gradually stabilized in recent years

and the erosivity of daily average snowmelt runoff for many years was 0.01 (MJ·mm)/(hm2·h·a). Spatially

the erosivity of multi-year daily average snowmelt runoff was in the range of 0~0.21 (MJ·mm)/(hm2·h·a)

showing a pattern of small in the middle and large in the surrounding areas. The influence factors of snowmelt runoff erosivity in spatial were as follows

the snow depth was large in the north and small in the south

the solar radiation intensity decreased from west to east

and the warming rate decreased from north to south. The influence factor of snowmelt runoff erosivity were analyzed by ground detector

and it was found that the warming rate had the strongest effect in the Mengdong black soil subregion

while the snow depth had the strongest effect in the Songnen black soil subregion and the Sanjiang black soil subregion. [Conclusion] Analyzing the spatiotemporal characteristics and influence factors of snowmelt runoff erosivity in the black soil region of Northeast China from 1990 to 2020 had certain theoretical and practical significance for deepening the study of snowmelt runoff erosivity characteristics and snowmelt erosion prevention in the study area.

关键词

Keywords

references

ZHANG Y, LI P, LIU X J, et al. Tracer elements revealed the soil organic carbon sources in a dam-controlled watershed[J].Soil and Tillage Research,2022,216:e105184.

李占斌,朱冰冰,李鹏.土壤侵蚀与水土保持研究进展[J].土壤学报,2008,45(5):802-809. LI Z B, ZHU B B, LI P. Advancement in study on soil erosion and soil and water conservation[J].Acta Pedologica Sinica, 2008,45(5):802-809.

陈英,魏兴萍,张爱国,等.基于复合指纹法的岩溶洼地小流域泥沙来源解析[J].水土保持学报,2020,34(5):131-136,144. CHEN Y, WEI X P, ZHANG A G, et al. Analysis of sediment source in small watershed of Karst depression based on composite fingerprint method[J].Journal of Soil and Water Conservation,2020,34(5):131-136,144.

史玮玥,岳荣,方怒放.黄土高原地区泥沙来源复合指纹示踪研究进展[J].水土保持通报,2019,39(3):276-285. SHI W Y, YUE R, FANG N F. A review of researches on sediment sources discrimination with composite fingerprinting techniques in loess plateau[J].Bulletin of Soil and Water Conservation, 2019,39(3):276-285.

WALLING D E, WOODWARD J C, NICHOLAS A P. A multi-parameter approach to fingerprinting suspended-sediment sources[J].IAHS Publication,1993,215:329-338.

COLLINS A L, WALLING D E, LEEKS G J L. Source type ascription for fluvial suspended sediment based on a quantitative composite fingerprinting technique[J].Catena,1997,29(1):1-27.

HADDADCHI A, RYDER D S, EVRARD O, et al. Sediment fingerprinting in fluvial systems: Review of tracers, sediment sources and mixing models[J]. International Journal of Sediment Research, 2013,28(4):560-578.

COLLINS A L, ZHANG Y, WALLING D E, et al. Tracing sediment loss from eroding farm tracks using a geochemical fingerprinting procedure combining local and genetic algorithm optimisation[J].Science of The Total Environment, 2010,408(22):5461-5471.

周慧平,陈玉东,常维娜.指纹技术识别泥沙来源: 进展与展望[J].水土保持学报,2018,32(5):1-7. ZHOU H P, CHEN Y D, CHANG W N. Sediment source fingerprinting: Progresses and prospects[J].Journal of Soil and Water Conservation,2018,32(5):1-7.

肖成芳, 魏兴萍, 李慧, 等. 西南典型岩溶槽谷小流域地表和地下河悬浮泥沙来源[J]. 农业工程学报, 2022,38(12):154-162. XIAO C F, WEI X P, LI H, et al. Suspended sediment sources of surface and underground rivers in small watersheds of typical Karst valleys in Southwest China[J].Transactions of the Chinese Society of Agricultural Engineering,2022,38(12):154-162.

陈飞.青藏高原纳木错流域融水侵蚀强度评价及产沙特性研究[D].北京:中国农业大学,2016. CHEN F.Study on evaluation of erosion intensity and sediment characteristics by meltwater flow in the Nam Co Basin on the Tibetan Plateau[D].Beijing: China Agricultural University,2016.

王晓彤,张加琼,杨明义,等.榆神府矿区典型小流域侵蚀产沙对退耕还林(草)及煤矿开采的响应[J].应用生态学报,2020,31(6):1971-1979. WANG X T, ZHANG J Q, YANG M Y, et al. Effects of "Grain for Green" program and coal mining on sediment production in a typical small watershed of Yushenfu Mining Region, Northwest China[J].Chinese Journal of Applied Ecology,2020,31(6):1971-1979.

张风宝,薛凯,杨明义,等.坝地沉积旋回泥沙养分变化及其对小流域泥沙来源的解释[J].农业工程学报,2012,28(20):143-149. ZHANG F B, XUE K, YANG M Y, et al. Variations of sediment nutrient in check dam and its implication for small catchment sediment resources[J].Transactions of the Chinese Society of Agricultural Engineering, 2012,28(20):143-149.

陈鸿,刘刚,刘普灵,等.退耕还林背景下的小流域侵蚀产沙研究[J].泥沙研究,2020,45(2):52-58. CHEN H, LIU G, LIU P L, et al. Processes of erosion and sediment yield in a small watershed under the influence of the grain for green project[J].Journal of Sediment Research, 2020,45(2):52-58.

侯建才,李占斌,李勉,等.基于淤地坝淤积信息的小流域泥沙来源及产沙强度研究[J].西安理工大学学报,2007,23(2):118-122. HOU J C, LI Z B, LI M, et al. Research on the sediment source and sediment yield intensity in a small watershed based on the alluvium information of soil-saving dam[J]. Journal of Xi'an University of Technology, 2007,23(2):118-122.

ZHAO T Y, YANG M Y, WALLING D E, et al. Using check dam deposits to investigate recent changes in sediment yield in the Loess Plateau, China[J].Global and Planetary Change,2017,152:88-98.

KOITER A J, OWENS P N, PETTICREW E L, et al. The behavioural characteristics of sediment properties and their implications for sediment fingerprinting as an approach for identifying sediment sources in river basins[J].Earth-Science Reviews,2013,125:24-42.

毛骁.桑干河流域生态脆弱性评价[D].北京:北京林业大学,2020. MAO X. Evaluation of ecological vulnerability in the Sanggan River[D].Beijing: Beijing Forestry University,2020.

余绍文,孙自永,马瑞.基于遥感和GIS的桑干河流域土壤侵蚀评价[J].安全与环境工程,2008,15(2):8-12. YU S W, SUN Z Y, MA R. Using remote sense and GIS techniques to assess soil erosion in sanggan river watershed[J].Safety and Environmental Engineering, 2008,15(2):8-12.

张灵.桑干河上游流域径流泥沙对气候要素与土地利用变化的响应研究[D].北京:中国地质大学,2017. ZHANG L. Response of runoff and sediment to climatic variabilities and land use change on the upper Sang-kan River Basin[D].Beijing: China University of Geosciences,2017.

ZHANG X B, WEN Z M, FENG M Y, et al. Application of

137

Cs fingerprinting technique to interpreting sediment production records from reservoir deposits in a small catchment of the Hilly Loess Plateau, China[J].Science in China Series D: Earth Sciences, 2007,50(2):254-260.

SU Z G, WANG L J, LIU Y H, et al.

137

Cs tracing of the spatial patterns in soil redistribution, organic carbon and total nitrogen in the southeastern Tibetan Plateau[J].International Soil and Water Conservation Research,2023,11(1):86-96.

LLOYD C D. Assessing the effect of integrating elevation data into the estimation of monthly precipitation in Great Britain[J].Journal of Hydrology, 2005,308(1/2/3/4):128-150.

蒋凯鑫,于坤霞,李鹏,等.砒砂岩区典型淤地坝沉积泥沙特征及来源分析[J].水土保持学报,2020,34(1):47-53. JIANG K X, YU K X, LI P, et al. Sediment characteristics and sources analysis of typical check dam in pisha sandstone area[J]. Journal of Soil and Water Conservation,2020,34(1):47-53.

谢云,刘宝元,章文波.侵蚀性降雨标准研究[J].水土保持学报,2000,14(4):6-11. XIE Y, LIU B Y, ZHANG W B. Study on standard of erosive rainfall[J]. Journal of Soil Water Conservation, 2000,14(4):6-11.

章文波,谢云,刘宝元.利用日雨量计算降雨侵蚀力的方法研究[J].地理科学,2002,22(6):705-711. ZHANG W B, XIE Y, LIU B Y. Rainfall erosivity estimation using daily rainfall amounts[J].Scientia Geographica Sinica, 2002,22(6):705-711.

WALLING D E. Tracing suspended sediment sources in catchments and river systems[J].Science of the Total Environment,2005,344(1/3):159-184.

陈太丽,史忠林,王永艳,等.三峡水库典型支流消落带泥沙颗粒态磷复合指纹示踪研究[J]. 农业工程学报, 2019,35(20):118-124. CHEN T L, SHI Z L, WANG Y Y, et al. Fingerprinting particulate phosphorus absorbed by sediments for riparian zone deposits in tributary of Three Gorges Reservoir[J].Transactions of the Chinese Society of Agricultural Engineering,2019,35(20):118-124.

杨明义,田均良,刘普灵.应用

137

Cs研究小流域泥沙来源[J].土壤侵蚀与水土保持学报,1999,13(3):49-53. YANG M Y, TIAN J L, LIU P L. Studying sediment sources in small watershed using

137

Cs tracing[J].Journal of Soil Water Conservation,1999,13(3):49-53.

文安邦,张信宝,王玉宽,等.长江上游云贵高原区泥沙来源的

137

Cs法研究[J].水土保持学报,2000,14(2):25-27,103. WEN A B, ZHANG X B, WANG Y K, et al. Study on sedimentation source using caesium 137 technique in Yungui Plateau region of Upper Yangtze River[J].Journal of Soil Water Conservation,2000,14(2):25-27,103.

张信宝,贺秀斌,文安邦,等.侵蚀泥沙研究的

137

Cs核示踪技术[J].水土保持研究,2007,14(2):152-154,157. ZHANG X B, HE X B, WEN A B, et al. The

137

Cs nuclear tracing technique for soil erosion and sedimentation studies[J]. Research of Soil and Water Conservation, 2007,14(2):152-154,157.

魏霞,李占斌,李鹏,等.黄土高原典型淤地坝淤积机理研究[J].水土保持通报,2006,26(6):10-13,31. WEI X, LI Z B, LI P, et al. Study on depositing process of check dam on the loess plateau[J]. Bulletin of Soil and Water Conservation, 2006,26(6):10-13,31.

王永吉.基于淤地坝沉积解译水蚀风蚀交错带小流域侵蚀特征演变[D].陕西杨凌:西北农林科技大学,2017. WANG Y J.Using the sediment deposits behind a check dam to interpret the evolution of erosion characteristics in a small catchment of the wind-water erosion crisscross region[D].Yangling Shaanxi: Northwest A&F University,2017.

文安邦,张信宝,沃林.黄土丘陵区小流域泥沙来源及其动态变化的

137

Cs法研究[J].地理学报,1998,53(增刊1):124-133. WEN A B, ZHANG X B,WO L. A study on soil erosion rates and sediment sources using caesium-137 technique in a small drainage of the loess hills[J].Acta Geographica Sinica,1998,53(S1):124-133.

周仕轩,夏彬,郝旺林,等.黄土高原坝地深层土壤有机碳稳定性研究[J].水土保持学报,2022,36(4):284-289,298. ZHOU S X, XIA B, HAO W L, et al. Stability of deep soil organic carbon of dam land on the loess plateau[J].Journal of Soil and Water Conservation,2022,36(4):284-289,298.

贾松伟,韦方强.利用磁性参数诊断泥石流沟道沉积物来源:以云南蒋家沟流域为例[J].泥沙研究,2009(1):54-59. JIA S W, WEI F Q. Tracing sediment sources using magnetic measurements: A case study of Jiangjiagou valley, Yunnan Province[J].Journal of Sediment Research,2009(1):54-59.

焦菊英,刘元保,唐克丽.小流域沟间与沟谷地径流泥沙来量的探讨[J].水土保持学报,1992,6(2):24-28. JIAO J Y, LIU Y B, TANG K L. An approach to runoff and sediment generation of gully and intergully land in small watershed[J].Journal of Soil and Water Conservation,1992,6(2):24-28.

ZHANG X C, ZHANG G L, LIU B L, et al. Using cesium-137 to quantify sediment source contribution and uncertainty in a small watershed[J].Catena,2016,140:116-124.

刘冰,王友胜,张磊,等.黑龙江省老莱河流域河漫滩沉积泥沙来源研究[J].泥沙研究,2022,47(6):59-65. LIU B, WANG Y S, ZHANG L, et al. Study on the sources of floodplain sediment in Laolai River Basin of Heilongjiang Province[J]. Journal of Sediment Research, 2022,47(6):59-65.

郭进,文安邦,严冬春,等.复合指纹识别技术定量示踪流域泥沙来源[J].农业工程学报,2014,30(2):94-104. GUO J, WEN A B, YAN D C, et al. Quantifying catchment scale sediment source using composite fingerprinting technique[J].Transactions of the Chinese Society of Agricultural Engineering,2014,30(2):94-104.

李占斌.黄土地区小流域次暴雨侵蚀产沙研究[J].西安理工大学学报,1996,12(3):177-183. LI Z B. Study on small watershed single storm erosion sediment yield in loess region[J].Journal of Xi'an University of Technology, 1996,12(3): 177-183.

ZHANG J Q, YANG M Y, ZHANG F B, et al. Fingerprinting sediment sources after an extreme rainstorm event in a small catchment on the loess plateau, PR China[J].Land Degradation and Development,2017,28(8):2527-2539.

万赐航,周慧平,王强,等.植被覆盖度和降雨侵蚀力变化对小流域泥沙连通性的影响[J].农业工程学报,2022,38(12):127-134. WAN C H, ZHOU H P, WANG Q, et al. Effects of vegetation coverage and rainfall erosivity changes on sediment connectivity in small watersheds[J].Transactions of the Chinese Society of Agricultural Engineering,2022,38(12):127-134.

周涛,苏正安,刘刚才,等.工程堆积体典型生态修复措施对土壤侵蚀水动力过程的影响[J].农业工程学报,2022,38(9):91-100. ZHOU T, SU Z A, LIU G, et al. Effects of typical ecological restoration measures for engineering accumulation on sediment yield and hydrodynamic process[J].Transactions of the Chinese Society of Agricultural Engineering, 2022,38(9):91-100.

刘定辉,李勇.植物根系提高土壤抗侵蚀性机理研究[J].水土保持学报,2003,17(3):34-37,117. LIU D H, LI Y. Mechanism of plant roots improving resistance of soil to concentrated flow erosion[J].Journal of Soil Water Conservation, 2003,17(3):34-37,117.

刘翊涵,苏正安,潘洪义,等.张家口市土地利用和土壤保持功能的变化特征[J].草业科学,2020,37(7):1281-1292. LIU Y H, SU Z A, PAN H Y, et al. Changes in land use and soil retention functions in Zhangjiakou City[J].Pratacultural Science,2020,37(7):1281-1292.

浏览量

941

下载量

CSCD

文章被引用时，请邮件提醒。

提交

工具集

关联资源

河流筑坝对南盘江流域局地旱涝特征变化的驱动

宁夏水源涵养功能时空演变格局及其归因分析

滇西北云龙县2000—2020年土壤侵蚀时空演变特征及影响因素

黄河中游多沙粗沙区土壤水蚀时空变化及动态驱动力分析

基于RUSLE模型和地理探测器的鄂西南土壤侵蚀脆弱性评价