Log in

Scale effect on sediment yield from slo** surfaces to basins in hilly loess region on the Loess Plateau in China

  • Original Article
  • Published:
Environmental Geology

Abstract

Based on data from two runoff plots and ten stations in hilly loess region Dalihe drainage basin ranging in area from 0.0006 to 3983 km2 on the Loess Plateau, the relationship between mean annual specific sediment yield (Y s) and drainage area (A) is studied, which is different from those for many other drainage areas of the world, neither at the scale of whole basin nor at local scale on the Loess Plateau. With increasing drainage area, the mean annual specific sediment yield experiences two peak values: the first peak value appears at 0.00408 km2 in area corresponding to the whole slope surface, and the second peak value appears at 96.1 km2 in area. The non-linear variation in the Y sA can be explained as follows: the first peak value can be explained by the abrupt increase in slope gradient and flow shear stress resulting in highly increased sediment concentration and specific sediment yield. And the second peak value can be explained by the combined influence of flow shear stress and drainage density, represented by dimensionless variable Ω.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Subscribe and save

Springer+ Basic
EUR 32.99 /Month
  • Get 10 units per month
  • Download Article/Chapter or Ebook
  • 1 Unit = 1 Article or 1 Chapter
  • Cancel anytime
Subscribe now

Buy Now

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7

Similar content being viewed by others

References

  • Andrle R (1996) Complexity and scale in geomorphology: statistical self-similarity vs. characteristic scales. Math Geol 28(3):275–293

    Article  Google Scholar 

  • Cai MY (1994) Estimate model for sediment transport process of Dali river region on the middle reaches of the Yellow River (in Chinese). J Hehai Univ 22:14–20

    Google Scholar 

  • Chen H, Wang KZ (1999) A study on the slope gully erosion relationship on small basins in the loess areas at the middle reaches of the Yellow River (in Chinese). Geogr Res 18:363–372

    Google Scholar 

  • Chen H, Fang HY, Cai QG, Liang GL, Yue ZQ (2006) Landform morphologic relations between inter-gullied and gullied land areas-a case study of the Wangjiagou Watershed in the west of Shanxi Province. Int J Sediment Res 21:62–73

    Google Scholar 

  • Chorley RJ, Schumm SA, Sugden DE (1984) Geomorphology. Methuen, London

    Google Scholar 

  • Church M, Slaymaker O (1989) Disequilibrium of Holocene sediment yield in glaciated British Columbia. Nature 337:452–454

    Article  Google Scholar 

  • Desmet PJJ, Poesen J, Govers G, Vandaele K (1999) Importance of slope gradient and contributing area for optimal prediction of the initiation and trajectory of ephemeral gullies. Catena 37:377–292

    Article  Google Scholar 

  • Fei XJ, Shao XJ (2004) Sediment transport capacity of gullies in small watersheds (in Chinese). J Sediment Res 1:1–8

    Google Scholar 

  • Fox DM, Bryan RB (1999) The relationship of soil loss by interrill erosion to slope gradient. Catena 38:211–222

    Article  Google Scholar 

  • Fu BJ (2006) A multiscale soil loss evaluation index. Sci Bull 51:448–456

    Article  Google Scholar 

  • Fu BJ, Zhang QJ, Chen LD, Zhao WW, Gulinck H, Liu GB, Yang QK, Zhu YG (2006) Temporal change in land use and its relationship to slope degree and soil type in a small catchment on the Loess Plateau of China. Catena 65:41–48

    Article  Google Scholar 

  • Hovius N (1998) Controls on sediment supply by large rivers. In: Relative Role of Eustasy, Climate, and Tectonism in Continental Rocks. SEPM (Society of Sedimentary Geology) Special Publication No. 59, pp 3–16

  • Hovius N, Stark CP, Allen PA (1997) Sediment flux from a mountain belt derived by landslide map**. Geology 25:231–234

    Article  Google Scholar 

  • Imeson AC, Lavee H (1998) Soil erosion and climate change: the transect approach and the influence of scale. Geomorphology 23:219–227

    Article  Google Scholar 

  • Jetten V, Roo AD, Mortlock DF (1999) Evaluation of field-scale and catchment-scale soil erosion models. Catena 37:521–541

    Article  Google Scholar 

  • Kimura R, Liu Y, Takayama N, Zhang X, Kamichika M, Matsuoka N (2005) Heat and water balances of the bare soil surface and the potential distribution of vegetation in the Loess Plateau, China. J Arid Environ 63:439–457

    Article  Google Scholar 

  • Kirkby MJ, Morgan RPC (1980) Soil erosion. A Weley-Interscience Publication, New York, pp 158–160

    Google Scholar 

  • Lane LJ, Hernandez M, Nichols M (1997) Processes controlling sediment yield from watersheds as functions of spatial scale. Environ Modell Softw 12:355–369

    Article  Google Scholar 

  • Nearing MA, Jetten V, Baffaut C, Cerdan O, Couturier A, Hernandez M, Bissonnais YL, Nichols MH, Nunes JP, Renschler CS, Souchere V, Oost KV (2005) Modeling response of soil erosion and runoff to changes in precipitation and cover. Catena 61:131–154

    Article  Google Scholar 

  • Owens P, Slaymaker O (1992) Late Holocene sediment yields in small alpine and subalpine drainage basins, British Columbia, IASH Publications No. 209, pp 147–154

  • Shi H, Shao (2000) Soil and water loss from the Loess Plateau in China. J Arid Environ 45:9–20

    Article  Google Scholar 

  • Syvitski JPM (2003) Supply and flux of sediment along hydrological pathways: research for the 21st century. Glob Planet Change 39:1–11

    Article  Google Scholar 

  • Syvitsky JPM, Burrel DC, Skei JM (eds) (1987) Fjords: processes and products. Springer, Berlin Heidelberg New York, pp 379

  • Valentin C, Poesen J, Li Y (2005) Gully erosion: impacts, factors and control. Catena 63:132–153

    Article  Google Scholar 

  • Wang NB (1991) Dataset by remote sense for resource and environment in the Loess Plateau region. **’an Press for Maps, **’an, pp 147–157

    Google Scholar 

  • Wang XK, Qian N, Hu WD (1982) The formation and process of confluence of the flow with hyperconcentration in the gullied-hilly loss areas of the Yellow River basin (in Chinese). Shuili Xuebao 7:26–35

    Google Scholar 

  • Woodward DE (1999) Method to predict cropland ephemeral gully erosion. Catena 37:393–399

    Article  Google Scholar 

  • Xu JX (1999) Erosion caused by hyperconcentrated flow on the Loess Plateau of China. Catena 36:1–19

    Article  Google Scholar 

  • Xu JX, Cheng DS (2002) Relationship between the erosion and sedimentation zones in the Yellow River, China. Geomorphology 48:365–382

    Article  Google Scholar 

  • Xu JX, Yan YX (2005) Scale effects on specific sediment yield in the Yellow River basin and geomorphological explains. J Hydrol 307:219–232

    Article  Google Scholar 

  • Yan YX, Xu JX (2006) Primary research on scale effect on specific sediment yield on the Loess Plateau. Sci China 36:1–10

    Google Scholar 

  • Yellow River Water Conservancy Commission (1961–1969) Hydrometric data in the Zizhou runoff experimental station (1959–1969). Zhengzhou: Ministry Water Conservancy and Electric Power Press

  • Yin ZY, Wang X (1999) A cross-scale comparison of drainage basin characteristics derived from digital elevation models. Earth Surf Process Landf 245:57–562

    Google Scholar 

  • Zhao WW, Fu BJ, Chen LD (2003) Correlations between topographical factors and soil and water loss in Hilly and Gully Area of Loess Plateau in Northern Shaanxi (in Chinese). J Soil Water Conserv 17:66–69

    Google Scholar 

  • Zheng FL, He XB, Gao XT, Zhang CE, Tang KL (2005) Effect of erosion patterns on nutrient loss following deforestation on the Loess Plateau of China. Agric Ecosyst Environ 108:85–97

    Article  Google Scholar 

Download references

Acknowledgment

The authors wish to acknowledge the projects of the National Grand Fundamental Research 973 Program of China under Grant No. 2007CB407207 and the National Natural Science Foundation of China under Grant No. 40471085 and 40471084 for their financial support of this work.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Hao Chen.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Fang, H., Chen, H., Cai, Q. et al. Scale effect on sediment yield from slo** surfaces to basins in hilly loess region on the Loess Plateau in China. Environ Geol 52, 753–760 (2007). https://doi.org/10.1007/s00254-006-0513-9

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00254-006-0513-9

Keywords

Navigation