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Soil particle-size distribution and aggregate stability of new reconstructed purple soil affected by soil erosion in overland flow

  • Soils, Sec 2 • Global Change, Environ Risk Assess, Sustainable Land Use • Research Article
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Abstract

Purpose

Artificial soil erosion caused by engineering practices is becoming increasingly severe worldwide. However, little is known about the change of soil structure of new reconstructed purple soil after erosion in the hilly areas of Southwest China. This study aims to analyze the effects of erosion on the soil particle-size distribution (PSD) and aggregate stability of new reconstructed purple soil in the overland flow under different flow discharges, slope lengths, and slope positions.

Materials and methods

A series of field scouring experiments was conducted. Flow discharges of 5, 15, and 30 L/min were applied in the new reconstructed purple soil plots with different slope lengths (5, 10, 20, 30, 40, and 50 m). Sediment samples were collected in 550-mL bottles. Soil sampling was conducted from the 0–10-cm layers before and after the field scouring experiments. In the laboratory, the pipette method was used to measure the soil PSD and microaggregates. The macroaggregates were determined by the dry and wet sieving method.

Results and discussion

Silt particles were eroded most at 30 L/min, by 2.11%. The average maximal reduction rate of the mean weight diameter of soil aggregates (MWD) was 20.23% at 15 L/min. Clay loss was maximal at 1.04%, and the average maximal increasing rate of the > 0.25 mm percentage of aggregate disruption (PAD0.25) was 0.86% at 5 L/min. The silt and MWD maximally decreased by 7.72% and 1.86%, and the maximal sand and PAD0.25 increased by 16.70% and 25.18%, which were all observed in the 10-m plot. The percentage of soil aggregates destroyed by the change in the MWD was − 14.32% on the upslope. Silt sediment showed an increasing rate of 6.36% and microaggregate destruction showed a decreasing rate of 13.00% on the middle slope. Microaggregates and clay particles were mainly deposited on the lower slope and the reduction rates of the silt and sand content were smaller than those on the middle slope.

Conclusions

The effects of erosion on the soil PSD and aggregate stability of new reconstructed purple soil in the overland flow under different flow discharges, slope lengths, and slope positions were obviously different. Soil and water conservation measures should be effectively implemented on the upper slope and a slope length of 10-m soil. The soil PSD and MWD could be used as parameters for prediction of soil erosion on new reconstructed purple soil.

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References

  • Ampontuah EO, Robinson JS, Nortcliff S (2006) Assessment of soil particle redistribution on two contrasting cultivated hillslopes. Geoderma 132:324–343

    Google Scholar 

  • Asadi H, Moussavi A, Ghadiri H, Rose CW (2011) Flow–driven soil erosion processes and the size selectivity of sediment. J Hydrol 406:73–81

    Google Scholar 

  • Barthès B, Roose E (2002) Aggregate stability as an indicator of soil susceptibility to runoff and erosion; validation at several levels. Catena 47:133–149

    Google Scholar 

  • Boonamnuayvitaya V, Chaiya C, Tanthapanichakoon W, Jarudilokkul S (2004) Removal of heavy metals by adsorbent prepared from pyrolyzed coffee residues and clay. Sep Purif Technol 35:11–22

    CAS  Google Scholar 

  • Bronick CJ, Lal R (2005) Soil structure and management: a review. Geoderma 124:3–22

    CAS  Google Scholar 

  • Cerdà A, Bodí MB, Hevilla-Cucarella E (2007) Erosión del suelo en plantaciones de cítricos en ladera. Valle del riu Canyoles, Valencia. Agroecología 2:85–91

    Google Scholar 

  • Chen XY, Niu QX, Zhou J, Wei CF, Xie DT, He BH (2010) Study on spatial variability characters of steep purple soil particles under rainfall simulation condition. J Soil Water Conserv 24(5):163–168

    Google Scholar 

  • Chen SN, Ai XY, Dong TY, Li BB, Luo RH, Ai YW, Chen ZQ, Li CR (2016) The physico-chemical properties and structural characteristics of artificial soil for cut slope restoration in Southwestern China. Sci Rep 6:20565

    CAS  Google Scholar 

  • Chongqing Land Development and Consolidation Project Construction Standard (Trial) (2007)

  • Curtaz F, Stanchi S, D’Amico ME, Filippa G, Zanini E, Freppaz M (2015) Soil evolution after land-reshaping in mountains areas (Aosta Valley, NW Italy). Argic Ecosyst Environ 199:238–248

    Google Scholar 

  • Deng JL (1987) Grey system basic method. Huazhong University of Science and Technology Press, Wuhan, pp 17–34

    Google Scholar 

  • Ding W, Huang C (2017) Effects of soil surface roughness on interrill erosion processes and sediment particle size distribution. Geomorphology 295:801–810

    Google Scholar 

  • FAO/Unesco (1988) Soil map of the world, revised legend. FAO, Rome

  • Fiès JC, Bruand A (1998) Particle packing and organization of the textural porosity in clay-silt-sand mixtures. Eur J Soil Sci 49:557–567

    Google Scholar 

  • Fox DM, Bryan RB, Fox CA (2004) Changes in pore characteristics with depth for structural crusts. Geoderma 120:0–120

    Google Scholar 

  • Gholami V, Booij MJ, Nikzad Tehrani E, Hadian MA (2018) Spatial soil erosion estimation using an artificial neural network (ANN) and field plot data. Catena 163:210–218

    Google Scholar 

  • Hamed Y, Jean A, Pepin Y, Asseline J, Nasri S, Zante P, Berndtsson R, El-Niazy M, Balah M (2002) Comparison between rainfall simulator erosion and observed reservoir sedimentation in an erosion-sensitive semiarid catchment. Catena 50:1–16

    Google Scholar 

  • Hao HX, Wang JG, Guo ZL, Hua L (2019) Water erosion processes and dynamic changes of sediment size distribution under the combined effects of rainfall and overland flow. Catena 173:494–504

    Google Scholar 

  • He XB, Bao YH, Nan HW, Xiong DH, Wang L, Liu YF, Zhao JB (2009) Tillage pedogenesis of purple soils in southwestern China. J Mt Sci 6:205–210

    Google Scholar 

  • Kang HL, Wang WL, Xue ZD, Guo MM, Shi QH, Li JM, Guo JQ (2016) Erosion morphology and runoff generation and sediment yield on ephemeral gully in loess hilly region in field scouring experiment. Transactions of the Chinese Society of Agricultural Engineering 32:161–170 (in Chinese)

    Google Scholar 

  • Kara O, Sensoy H, Bolat I (2010) Slope length effects on microbial biomass and activity of eroded sediments. J Soils Sediments 10:434–439

    CAS  Google Scholar 

  • Kosmas C, Gerontidis ST, Marathianou M, Detsis B, Zafiriou TH, Muysen WN, Govers G, Quine T, Vanoost K (2001) The effects of tillage displaced soil on soil properties and wheat biomass. Soil Tillage Res 58:31–44

    Google Scholar 

  • Le Bissonnais Y (2005) Aggregate breakdown mechanisms and erodibility. Encyclopedia of soil science CRC Press pp 40–44

  • Li ZW, Zhang GH, Geng R, Wang H (2015) Spatial heterogeneity of soil detachment capacity by overland flow at a hillslope with ephemeral gullies on the Loess Plateau. Geomorphology 248:264–272

    Google Scholar 

  • Liao YS, Cai QG, Cheng QJ (2008) Critical topographic condition for slope erosion in hilly-gully region of Loess Plateau. Science of Soil and Water Conservation 6:32–38

    Google Scholar 

  • Liu J (2015) Soil engineering effect of farming plots reconstruction in hilly–mountainous region of Chongqing. PhD thesis, Southwest University (in Chinese)

  • Liu BY, Nearing MA, Shi PJ, Jia ZW (2000) Slope length effects on soil loss for steep slopes. Soil Sci Soc Am J 64:1759–1763

    CAS  Google Scholar 

  • Liu J, Du J, Wei C, Zhong M, Liu B (2015) Effects of land consolidation period of farmland on soil properties in purple region. Transactions of the Chinese Society of Agricultural Engineering 31:254–261 (in Chinese)

    Google Scholar 

  • López-Tarazón JA, Batalla RJ, Vericat D, Balasch JC (2010) Rainfall, runoff and sediment transport relations in a mesoscale mountainous catchment: the river Isábena (Ebro basin). Catena 82:23–34

    Google Scholar 

  • Lu J, Zheng F, Li G, Bian F, An J (2016) The effects of raindrop impact and runoff detachment on hillslope soil erosion and soil aggregate loss in the mollisol region of northeast China. Soil Tillage Res 161:79–85

    Google Scholar 

  • Meyer LD, Monke EJ (1965) Mechanics of soil erosion by rainfall and overland flow. Trans ASAE 8:572–580

    Google Scholar 

  • Meyer LD, Line DE, Harmon WC (1992) Size characteristics of sediment from agricultural soils. J Soil Water Conserv 47:107–111

    Google Scholar 

  • Nadeu E, Boix-Fayos C, De Vente J, López J, Martínez-Mena M (2010) Organic carbon mobilization by different erosive processes in the slope-channel connection. Movilización de carbono orgánico por distintos procesos erosivos en la conexión laderacauce. Pirineos 165:157–177

    Google Scholar 

  • Oades JM, Waters AG (1991) Aggregate hierarchy in soils. Aust J Soil Res 29:815–828

    Google Scholar 

  • Oztas T, Fayetorbay F (2003) Effect of freezing and thawing processes on soil aggregate stability. Catena 52:1–8

    CAS  Google Scholar 

  • Peng XD, Shi DM, Dong J, Wang SS, Li YX (2014) Runoff erosion process on different underlying surfaces from disturbed soils in the Three Gorges Reservoir Area, China. Catena 123:215–224

    Google Scholar 

  • Piccarreta M, Faulkner H, Bentivenga M, Bentivengac M, Capolongo D (2006) The influence of physico-chemical material properties on erosion processes in the badlands of Basilicata, Southern Italy. Geomorphology 81:235–251

    Google Scholar 

  • Poesen J (1984) The influence of slope angle on infiltration rate and Hortonian overland flow. Z. Geomorphol., Supplement Band 49:117–131

  • Prosdocimi M, Cerdà A, Tarolli P (2016) Soil water erosion on Mediterranean vineyards: a review. Catena 141:1–21

    Google Scholar 

  • Ramos MC, Cots-Folch R, Martínez-Casasnovas JA (2007) Effects of land terracing on soil properties in the Priorat region in northeastern Spain: a multivariate analysis. Geoderma 142:251–261

    Google Scholar 

  • Refahi HGh (2000). Water erosion and conservation. Tehran University Press, pp. 551 (in Persian)

  • Shen Y, Zhang XP, Liang AZ, Li WF, Yang XM (2008) Study on properties of soil loss from sloping farmland of black soil based on a runoff event. Agric Res Arid Areas 26:224–229 (in Chinese)

    Google Scholar 

  • Shi ZH, Fang NF, Wu FZ, Wang L, Yue BJ, Wu GL (2012) Soil erosion processes and sediment sorting associated with transport mechanisms on steep slopes. J Hydrol 454:123–130

    Google Scholar 

  • Six J, Elliott ET, Paustian K (2000) Soil structure and soil organic matter II. A normalized stability index and the effect of mineralogy. Soil Sci Soc Am J 64:1042–1049

    CAS  Google Scholar 

  • Sklenicka P (2006) Applying evaluation criteria for the land consolidation effect to three contrasting study areas in the Czech Republic. Land Use Policy 23:502–510

    Google Scholar 

  • Starr GC, Lal R, Malone R, Hothem D, Owens L, Kimble J (2000) Modeling soil carbon transported by water erosion processes. Land Degrad Dev 11:83–91

    Google Scholar 

  • Stomph TJ, Ridder N, Steenhuis TS, Giesen NCVD (2002) Scale effects of Hortonian overland flow and rainfall-runoff dynamics: laboratory validation of a process-based model. Earth Surf Process Landf 27:847–855

    Google Scholar 

  • Thomaz EL (2018) Interaction between ash and soil microaggregates reduces runoff and soil loss. Sci Total Envrion 625:1257–1263

    CAS  Google Scholar 

  • Tian X, Gao K, Zhang LJ, Yu YQ, Han GD (2015) Effect of slope position on spatial distribution of soil water and vegetation in sandy land. Bulletin of Soil and Water Conservation 35:12–16 (in Chinese)

    Google Scholar 

  • Wakindiki IIC, Ben–Hur M (2002) Soil mineralogy and texture effects on crust micromorphology, infiltration, and erosion. Soil Sci Soc Am J 66:897–905

    CAS  Google Scholar 

  • Wang WL, Lei AL, Li ZB, Tang KL (2004) Numerical simulation of multiple submerged jets on multilevel dicharged into plunge pool. J Hydraul Eng 35:25–30 38

    CAS  Google Scholar 

  • Wang AL, Zhao GX, Wang QF, Liu WP (2011) Effects of land consolidation on soil physical and chemical characteristics of hilly region. Transactions of the Chinese Society of Agricultural Engineering 27:311–315

    Google Scholar 

  • Wang L, Shi ZH, Wang J, Fang NF, Wu GL, Zhang HY (2014) Rainfall kinetic energy controlling erosion processes and sediment sorting on steep hillslopes: a case study of clay loam soil from the Loess Plateau, China. J Hydrol 512:168–176

    Google Scholar 

  • Wang Y, Ran L, Fang N, Shi Z (2018) Aggregate stability and associated organic carbon and nitrogen as affected by soil erosion and vegetation rehabilitation on the Loess Plateau. Catena 167:257–265

    CAS  Google Scholar 

  • Wei CF, Xie DT, Yang JH, Wang QK, He JL (1994) Study on soil fertility evolution of purple hilly sloping land. Mountain development 5:61–66

    Google Scholar 

  • Wei CF, Gao M, Che FC, Qu M, Yang JH, Xie DT (2000) Study on the fertility characteristics of soils in immigration’s reclamation area of ErTan hydropower station. Acta Pedol Sin 27:536–544

    Google Scholar 

  • Wei CF, Ni JP, Gao M, Xie DT, Hasegawa S (2006) Anthropic pedogenesis of purple rock fragments in Sichuan Basin, China. Catena 68:51–58

    Google Scholar 

  • Wei S, Zhang X, McLaughlin NB, Chen X, Jia S, Liang A (2017) Impact of soil water erosion processes on catchment export of soil aggregates and associated SOC. Geoderma 294:63–69

    CAS  Google Scholar 

  • Wu XL, Wei YJ, Wang JG, Xia JW, Cai CF, Wu LL, Fu ZY, Wei ZY (2017) Effects of erosion degree and rainfall intensity on erosion processes for Ultisols derived from quaternary red clay. Agric Ecosyst Environ 249:226–236

    Google Scholar 

  • Xie JQ, Tang CJ, Li XW (2005) China’s sloping farmland. Beijing. China Earth Press 29–31:49–55 (in Chinese)

  • Xu C, Gao M, Xie DT, Jiang T, Li S, Wei CF (2009) Effect of land consolidation history on soil quality of purple hilly region. Transactions of the Chinese Society of Agricultural Engineering 25:242–248 (in Chinese)

    CAS  Google Scholar 

  • Yu G, Feng J, Che Y, Lin X, Hu L, Yang S (2010) The identification and assessment of ecological risks for land consolidation based on the anticipation of ecosystem stabilization: a case study in Hubei province, China. Land Use Policy 27:293–303

    Google Scholar 

  • Zhang P, Wei T, Jia Z, Han Q, Ren X (2014) Soil aggregate and crop yield changes with different rates of straw incorporation in semiarid areas of northwest China. Geoderma 230–231:41–49

    Google Scholar 

  • Zheng BZ (2013) Technical guide to soil analysis. Beijing, pp 36–37

  • Zuo FL, Zhong SQ, Ran ZL, Wei CF (2018) Characteristics of sediment and hydrodynamic parameters of new reconstructed slope soil in the hill area with purple soils. J Soil Water Conserv 32:59–66 (in Chinese)

    Google Scholar 

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Funding

This work was financially supported by the National Natural Science Foundation of China (NSFC: 41730854, 91425301), Ten Thousand Talent Program for leading young scientist, and the state key development program in China “Constructing an efficient ecological interception technology system by combining source reduction,-biological isolation and-wetland disposal” (2017YFD0800505).

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Author notes

  1. Yu-Jun Ma

    Present address: School of Geography and Planning, Sun Yat-sen University, Guangzhou, China

Authors and Affiliations

  1. State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing, 100875, China

    Feng-Lin Zuo, Xiao-Yan Li, Xiao-Fan Yang, Yang Wang & Yu-Jun Ma

  2. School of Natural Resources, Faculty of Geographical Science, Beijing Normal University, Beijing, 100875, China

    Feng-Lin Zuo, Xiao-Yan Li, Xiao-Fan Yang, Yang Wang & Yu-Jun Ma

  3. College of Water Resources and Civil Engineering, China Agricultural University, Beijing, 100083, China

    Yu-Han Huang

  4. College of Resources and Environment, Southwest University, Chongqing, 400716, China

    Chao-Fu Wei

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  1. Feng-Lin Zuo
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Zuo, FL., Li, XY., Yang, XF. et al. Soil particle-size distribution and aggregate stability of new reconstructed purple soil affected by soil erosion in overland flow. J Soils Sediments 20, 272–283 (2020). https://doi.org/10.1007/s11368-019-02408-1

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