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[1]ZHANG Jiaqiong,LIU Zhang,YANG Mingyi,et al.Soil Erosion and Its Influence Factors on a Slope in the Wind-Water Erosion Crisscross Region on the Loess Plateau[J].Research of Soil and Water Conservation,2018,25(01):1-6,22.

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Soil Erosion and Its Influence Factors on a Slope in the Wind-Water Erosion Crisscross Region on the Loess Plateau

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 25 Number of periods: 2018 01 Page number: 1-6,22 Column: Public date: 2018-02-28

Title:: Soil Erosion and Its Influence Factors on a Slope in the Wind-Water Erosion Crisscross Region on the Loess Plateau

Author(s):: ZHANG Jiaqiong^1,2, LIU Zhang³, YANG Mingyi^1,2, ZHANG Fengbao^1,2, WANG Yongji^1,2, DENG Xinxin^1,2; 1. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A & F University, Yangling, Shaanxi 712100, China;
2. Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100, China;
3. Rare Earth Research Institute of Baotou, Baotou, Inner Mongolia 014030, China

Keywords:: soil erosion; slope variation; ¹³⁷Cs tracing; wind-water erosion crisscross region; grain-size distribution

CLC:: S157

DOI:: -

Abstract:: The alternating effect of wind and water erosion intensified soil loss in the wind-water erosion crisscross region, and formed a complicated erosion environment on the Loess Plateau. This study selected a hill going from northwest to east in the Liudaogou watershed of Shenmu County as the site to collect soil samples used for measuring ¹³⁷Cs and grain size. The distribution of soil grain size, erosion rate and the influence factors were studied. The results showed that grain-size and soil erosion had significant variations (p < 0.05) on two slopes with obvious undulation. The change of soil erosion was affected by conditions of underlying surface including slope position, gradient, vegetation, soils and land use type besides erosion forces (wind and rainfall). The results of principal component analysis showed that there were two components including all underlying surface factors. They explained that the variations of soil erosion ranged from 69.6% to 82.1%. The linear regression between soil erosion rate and these four factors (slope position, gradient, vegetation, soil and land use types) implied the importance of erosion forces besides underlying surface conditions. Unfortunately, spatial distribution of soil erosion on a single slope is unlikely to represent the general erosion pattern in this region, the ¹³⁷Cs tracing technique and grain-size analysis were far away from quantitatively dividing the contribution of wind erosion and water erosion in the total erosion on the slope scale. Further study with better methods and techniques is necessary.

References:: [1] Field J P, Breshears D D, Whicker J J. Toward a more holistic perspective of soil erosion:Why aeolian research needs to explicitly consider fluvial processes and interactions[J]. Aeolian Research, 2009,1:9-17.
[2] Bullard J E, Livingstone I. Interactions between aeolian and fluvial systems in dryland environments[J]. Area, 2002,34(1):8-16.
[3] 唐克丽,侯庆春,王斌科,等.黄土高原水蚀风蚀交错带和神木试区的环境背景及整治方向[J].西北水土保持研究所集刊,1993,18:1-15.
[4] 唐克丽.黄河流域的侵蚀与径流泥沙变化[M].北京:中国科学技术出版社,1993.
[5] 査轩,王斌科,唐克丽.神木六道沟气候及地面组成物质特征对侵蚀产沙的影响分析[J].西北水土保持研究所集刊,1993,18(2):67-74.
[6] 蒋冲,陈爱芳,喻小勇,等.黄土高原风蚀和风水蚀复合区的风蚀气候侵蚀力变化[J].干旱区研究,2013,30(3):477-484.
[7] 海春兴,史培军,刘宝元,等.风水两相侵蚀研究现状及我国今后风水蚀的主要研究内容[J].水土保持学报,2000,16(2):50-56.
[8] 李秋艳,蔡强国,方海燕.风水复合侵蚀与生态恢复研究进展[J].地理科学进展,2010,29(1):65-72.
[9] Menzel R G. Transport of strontium-90 in runoff[J]. Science, 1960,131:499-500.
[10] Du J Z, Zhang J, Baskaran M. Applications of short-lived radionuclides(⁷Be, ²¹⁰Pb, ²¹⁰Po, ¹³⁷Cs and ²³⁴Th) to trace the sources, transport pathways and deposition of particles/sediments in rivers, estuaries and coasts[C]//Handbook of Environmental Isotope Geochemistry. Springer Berlin Heidelberg, 2012:305-329.
[11] Petrovi? J, Dragovi? S, Dragovi? R, et al. Using ¹³⁷Cs measurements to estimate soil erosion rates in the P?inja and South Morava River Basins, southeastern Serbia[J]. Journal of Environmental Radioactivity, 2016,158/159:71-80.
[12] Krmar M, Veloji? M, Hansman J, et al. Wind erosion on Deliblato (the largest European continental sandy terrain) studied using ²¹⁰Pbex and ¹³⁷Cs measurements[J]. Journal of Radioanalytical and Nuclear Chemistry, 2015,303(3):2511-2515.
[13] 刘巍,曹月娥,杨建军,等.准东煤田露天矿区土壤¹³⁷Cs剖面分布特征及侵蚀速率估算[J].水土保持学报,2015,29(3):52-55.
[14] 张加琼,周学雷,张春来,等.张家口坝上地区农田土壤风蚀的¹³⁷Cs示踪研究[J].北京师范大学学报:自然科学版,2010,46(6):724-728.
[15] 成都地质学院陕北队.沉积岩(物)粒度分析及其应用[M].北京:地质出版社,1976.
[16] Palchan D, Stein M, Almogi-Labin A, et al. Dust transport and synoptic conditions over the Sahara-Arabia desert during the MIS 6/5 and 2/1 transitions from grain-size, chemical and isotopic properties of Red Sea cores[J]. Planetary Science Letters, 2013,382(6):125-139.
[17] Pye K. Aeolian Dust and Dust Deposits[M]. Elsevier:Academic Press, 1987.
[18] 穆桂金,吉启慧.塔克拉玛干地区第四纪沉积物的机械组成特征及其意义[J].干旱区地理,1990,13(2):9-18.
[19] Zhang X D, Ji Y, Yang Z S, et al. End member inversion of surface sediment grain size in the South Yellow Sea and its implications for dynamic sedimentary environments[J]. Science China Earth Sciences, 2016,59(2):258-267.
[20] Liu X X, Jef V, An Z S, et al. Grain size of Lake Qinghai sediments:Implications for riverine input and Holocene monsoon variability[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2016,449:41-51.
[21] 邓智瑞,何青,邢超锋,等.长江口北槽柱状沉积物粒度分布特征及沉积环境指示意义[J].海洋科学,2016,40(1):112-122.
[22] 李小妹,严平,吴伟,等.克里雅河中下游流域地表沉积物的粒度与化学元素空间分布[J].地理科学,2016,36(8):1269-1276.
[23] 杨明义,田均良.坡面侵蚀过程定量研究进展[J].地球科学进展,2000,15(6):649-653.
[24] Folk R L, Ward W C. Brazos River bar, a study in the significance of grain-size parameters[J]. Journal of Sedimentary Petrology, 1957,27(1):3-26.
[25] Wentworth C K. A scale of grade and class terms for clastic sediments[J]. Journal of Geology, 1922,30:377-392.
[26] Zhang X B, Higgitt D L, Walling D E. A preliminary assessment of the potential for using Caesium-137 to estimate rates of soil erosion in the Loess Plateau of China[J]. Hydrological Sciences Journal, 1990,35(3):243-252.
[27] 孙喜军.黄土高原水蚀风蚀交错带土壤侵蚀速率的⁷Be和¹³⁷Cs示踪研究[D].北京:中国科学院研究生院,2012.
[28] 张威,潘少明,张克新,等.中国大陆Cs-137背景值研究[J].地理学报,2015,70(9):1477-1490.
[29] 张平仓.水蚀风蚀交错带风水两相侵蚀的时空特征研究:以神木六道沟小流域为例[D].陕西杨凌:中国科学院水利部水土保持研究所,1997.
[30] 张平仓,唐克丽.六道沟流域有效水蚀风蚀能量及其特征研究[J].土壤侵蚀与水土保持学报,1997,3(2):32-40.
[31] 魏振海,董治宝,胡光印,等.若尔盖盆地沙丘形成分布影响因素探讨[J].中国沙漠,2009,29(6):1035-1042.
[32] 葛云龙,逯径铁,廖保方,等.辫状河相储集层地质模型:"泛连通体"[J].石油勘探与开发,1998,25(5):77-79.

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