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[1]WEI Ning,WEI Xia,HUANG Chihua.Influence of Freeze-Thaw Effects on Soil Critical Shear Stress and Soil Rill Erodibility[J].Research of Soil and Water Conservation,2021,28(03):19-24.

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Influence of Freeze-Thaw Effects on Soil Critical Shear Stress and Soil Rill Erodibility

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 28 Number of periods: 2021 03 Page number: 19-24 Column: Public date: 2021-04-20

Title:: Influence of Freeze-Thaw Effects on Soil Critical Shear Stress and Soil Rill Erodibility

Author(s):: WEI Ning¹, WEI Xia^2,3, HUANG Chihua³; (1.College of Science, Northwest A&F University, Yangling, Shaanxi 712100, China; 2.College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China; 3.Agronomy Department, Purdue University, USDA-ARS National Soil Erosion Research Laboratory, West Lafayette, IN 47907-2077, USA)

Keywords:: effects of freeze-thaw; variable flow scouring; soil critical shear stress; soil erodibility

CLC:: S157

DOI:: -

Abstract:: In order to reveal the influence of freeze-thaw effects on soil erosion by water, effects of freeze-thaw on the variation of critical shear stress under the influence of effects of freeze-thaw were studied by alternately freezing-thawing tests and scouring tests. Three kinds of freeze-thaw cycles(1, 3 and 6), two kinds of soil moisture mass fractions(10% and 20%)and control test(CK)were involved. The results show that different experimental treatments have different impact degrees and different impact tendency on soil critical shear stress and soil erodibility; when test soil experiences one freeze-thaw cycle, soil critical shear stress and soil erodibilty show the increasing trend compared to the control experiment; when the freeze-thaw cycle continues to increase to 3 and 6, the soil critical shear stress and soil erodibility show the decreasing trend compared to the control experiment, and when freeze-thaw cycle is equal to 3, soil critical shear stress and soil erodibility were minimum; Soil moisture mass fraction has the significant effect on soil critical shear stress and soil erodibility; when freeze-thaw cycles are same, soil critical shear stress and soil erodibility under 10% soil moisture mass fraction are bigger than the corresponding values under 20% soil moisture mass fraction. These results can provide the support for soil erosion prediction in the context of freeze-thaw cycle.

References:: [1] 李述训,南卓铜,赵林.冻融作用对系统与环境间能量交换的影响[J].冰川冻土,2002,24(2):109-115.
[2] 杨梅学,姚檀栋.青藏高原表层土壤的日冻融循环[J].科学通报,2006,51(16):1974-1976.
[3] Henry H A L. Soil freeze-thaw cycle experiments:trends, methodological weaknesses and suggested improvements [J]. Soil Biology and Biochemistry, 2007,39(5):977-986.
[4] 范昊明,蔡强国.冻融侵蚀研究进展[J].中国水土保持科学,2003,1(4):50-55.
[5] 魏霞,丁永建,李勋贵.冻融侵蚀研究的回顾与展望[J].水土保持研究,2012,19(2):271-275.
[6] Harmon R S, William W, DoeⅢ. Landscape erosion and evolution modeling[M]. Springer Us, 2001.
[7] Halvorson J J, Gatto L W, McCool D K. Overwinter changes to near-surface bulk density, penetration resistance and infiltration rates in compacted soil[J]. Journal of Terramechanics, 2003,40(1):1-24.
[8] Kværnø S H, Øygarden L. The influence of freeze-thaw cycles and soil moisture on aggregate stability of three soils in Norway [J]. Catena, 2006,67(3):175-182.
[9] Wei X, Huang C, Wei N, et al. The impact of freeze-thaw cycles and soil moisture content at freezing on runoff and soil loss[J]. Land Degradation and Development, 2019,30(5):515-523.
[10] Anetaabenská, Miroslav Dumbrovsk'/y. Changes of Soil Aggregate Stability as a Result of the Effect of Freeze-thaw Cycles[J]. Acta Universitatis Agriculturae Et Silviculturae Mendelianae Brunensis, 2015,63(4):1211-1218.
[11] Oztas T, Fayetorbay F. Effect of freezing and thawing processes on soil aggregate stability[J]. Catena, 2003,52(1):1-8.
[12] Sahin U, Anapali O. Short communication. The effect of freeze-thaw cycles on soil aggregate stability in different salinity and sodicity conditions[J]. Spanish Journal of Agricultural Research, 2007,5(3):431-434.
[13] Sahin U, Angin I, Kiziloglu F M. Effect of freezing and thawing processes on some physical properties of saline-sodic soils mixed with sewage sludge or fly ash[J]. Soil & Tillage Research, 2008,99(2):254-260.
[14] 刘佳,范昊明,周丽丽,等.冻融循环对黑土容重和孔隙度影响的试验研究[J].水土保持学报,2009,23(6):186-189.
[15] 李强,刘国彬,许明祥,等.黄土丘陵区冻融对土壤抗冲性及相关物理性质的影响[J].农业工程学报,2013,29(17):105-112.
[16] 刘宝元,张科利,焦菊英.土壤可蚀性及其在侵蚀预报中的应用[J].自然资源学报,1999,14(4):345-350.
[17] 朱冰冰,李占斌,李鹏,等.土地退化/恢复中土壤可蚀性动态变化[J].农业工程学报,2009,25(2):56-61.
[18] 宋阳,刘连友,严平,等.土壤可蚀性研究评述[J].干旱区地理,2006,29(1):124-131.
[19] Léonard J, Richard G. Estimation of runoff critical shear stress for soil erosion from soil shear strength[J]. Catena, 2004,57(3):233-249.
[20] Moody, J A. Critical shear stress for erosion of cohesive soils subjected to temperatures typical of wildfires [J]. Journal of Geophysical Research, 2005,110(1):1-13.
[21] Hanson G J, Cook K R. Apparatus, test procedures, and analytical methods to measure soil erodibility in situ [J]. Applied Engineering in Agriculture, 2004,20(4):455-462.
[22] Nouwakpo S K, Huang C H, Bowling L, et al. Impact of vertical hydraulic gradient on rill erodibility and critical shear stress[J]. Soil Science Society of America Journal, 2010,74(6):1914-1921.
[23] Nouwakpo S K, Huang C H. A fluidized bed technique for estimating soil critical shear stress [J]. Soil Ence Society of America Journal, 2012,76(4):1192-1196.
[24] 唐泽军,雷廷武,张晴雯,等.确定侵蚀细沟土壤临界抗剪应力的REE示踪方法[J].土壤学报,2004,41(1):28-34.
[25] 张晴雯,雷廷武,潘英华,等.细沟侵蚀可蚀性参数及土壤临界抗剪应力的有理(试验)求解方法[J].中国科学院研究生院学报,2004,21(4):468-475.
[26] Thoman R W, Niezgoda S L. Determining erodibility, critical shear stress, and allowable discharge estimates for cohesive channels:Case study in the powder river basin of wyoming [J]. Journal of Hydraulic Engineering, 2008,134(12):1677-1687.
[27] Zhang G H, Liu G B, Tang K M, et al. Flow detachment of soils under different land uses in the Loess Plateau of China [J]. Transactions of the American Society of Agricultural and Biological Engineers, 2008,51(3):883-890.
[28] Zhang G H, Tang M K, Zhang X C. Temporal variation in soil detachment under land uses in the Loess Plateau of China [J]. Earth Surface Processes & Landforms, 2009,34(9):1302-1309.
[29] Zhang X C, Liu W Z. Simulating potential response of hydrology, soil erosion, and crop productivity to climate change in Changwu tableland region on the Loess Plateau of China[J]. Agricultural & Forest Meteorology, 2005,131(3/4):127-142.
[30] Fu B J, Liu Y, Lu Y H, et al. Assessing the soil erosion control service of ecosystems change in the Loess Plateau of China [J]. Ecological Complexity, 2011,8(4):284-293.

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Last Update: 2021-04-20