Skip to main content
Log in

The enrichments of organic matter and total nitrogen in sediment as affected by relavant factors

  • Soil Geography
  • Published:
Journal of Geographical Sciences Aims and scope Submit manuscript

Abstract

Serious soil erosion has already resulted in degradation of the Loess Plateau of China. Soil erosion is commonly accompanied by extensive soil nutrient loss. Because of enrichment processes, sediment nutrient content is often higher than that of natural soil. The objective of this study is to determine the enrichments of organic matter and total nitrogen in sediment in hilly and gully loess areas on the Loess Plateau of China. Measurements of enrichment ratios (ER) of organic matter (EROM) and total nitrogen (ERTN) in sediment as affected by rainfall, slope gradient, tillage, and fertilization were made in the field under natural rainfall conditions. The results showed that the enrichment of clay in sediment resulted in the enrichment of organic matter (OM) and total nitrogen (TN) in sediment. The averages of sediment clay ER, EROM and ERTN for the various slope gradients were 1.77, 2.09 and 1.61, respectively. The soil erosive module was negatively correlated with EROM and ERTN. Our results indicate that measures to reduce soil erosion, i.e. reducing rainfall erosivity, decreasing soil slope gradient, decreasing fertilizer use, and using level trenches, may increase EROM and ERTN. Both quantity and quality of sediment yield should be considered when implementing erosion control measures.

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

Access this article

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

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Alberts E E, Wendt R C, Piest R F, 1983. Physical and chemical properties of erosion.Adv. Agron., 15: 303–316.

    Google Scholar 

  • Anderson D W, Saggar S, 1981. Particle size fractions and their use in studies of soil organic matter: I. the nature and distribution of forms of carbon, nitrogen, and sulfur.Soil Sci. Soc. Am. J., 45: 767–772.

    Article  Google Scholar 

  • Burwell R E, Timmons D R, Holt R F, 1975. Nutrient transport in surface runoff as effected by soil cover and seasonal periods.Soil Sci. Soc. Am. Proc., 37: 523–538.

    Article  Google Scholar 

  • Catroux G, Schnitzer M, 1987. Chemical, spectroscopic, and biological characteristics of the organic matter in particle size fractions separated from an Aquoll.Soil Sci. Soc. Am. J., 51: 1200–1207.

    Article  Google Scholar 

  • Chichester F W, 1969. Nitrogen in organa-mineral sedimentation fractions.Soil Sci., 107: 356–363.

    Article  Google Scholar 

  • Cogo N P, 1983. Tillage-induced roughness and runoff velocity on size distribution of eroded soil aggregates.Soil Sci. Soc. Am. J., 47(5): 1005–1008.

    Article  Google Scholar 

  • Gregory F, 1991. Nitrogen and phosphorus in eroded sediment from corn and soybean tillage system.J. Enviorn. Qual., 20: 663–670.

    Google Scholar 

  • Jiang Z S, 1995. The Surveillance on the Sediment-reduced Benefits of the Comprehensive Management and Loss of Soil and Water in Small Catchment. Beijing: Science Press, 186–242. (in Chinese)

    Google Scholar 

  • Hinds A A, Lowe L E, 1980. The use of an ultrasonic probe in soil dispersion and in the bulk isolation of organo-mineral complexes.Can. J. Soil Sci., 60: 389–392.

    Article  Google Scholar 

  • Huang L, Zhang G Y, Ding S Wet al., 1999. The research on soil particle loss in purple soil.J. Soil and Water Conserv., 13(1): 35–39. (in Chinese)

    Google Scholar 

  • Loch R Jet al., 1982. Field rainfall simulator studies on two clay soils of the Darling Downs, Queensland: II. aggregate breakdown, sediment properties and soil erodibility.Ast. J. Soil Res., 21: 47–58.

    Article  Google Scholar 

  • McKeague J A, 1971. Organic matter in particle size and specific gravity fractions of some Ah Horizons.Can. J. Soil Sci., 51: 299–505.

    Google Scholar 

  • Meyer L D, Foster G R, 1975. Effect of flow rate and canopy on rill erosion.Trans. ASAE, 18: 905–911.

    Google Scholar 

  • Neibling W H, Moldenhauer W C, Holmes B M, 1983. Evaluation and comparison of two methods for characterization of sediment size distribution.Trans. ASAE, 26: 472–480.

    Google Scholar 

  • Schnitzer M, Ivarson K C, 1982. Different forms of nitrogen in particle size fractions separated from two soils.Plant and Soil, 69: 383–389.

    Article  Google Scholar 

  • Sharpley A N, 1985. The selective erosion of plant nutrient in runoff.Soil Sci. Soc. Am. J., 49: 1527–1534.

    Article  Google Scholar 

  • Sowden F J, Chen Y, Schnitzer M, 1977. The nitrogen distribution in soils formed under widely differing climate conditions.Geochim. Cosmochim. Acta, 41: 1524–1526.

    Article  Google Scholar 

  • Tiessen H, Stewart J W B, 1983. Particle size fractions and their use in soil organic matter: II. cultivation effects on organic matter composition in size fractions.Soil Sci. Soc. Am. J., 47: 509–514.

    Article  Google Scholar 

  • Wan Y, El-Swaify S A, 1998. Sediment enrichment mechanisms of organic carbon and phosphorus in a well-aggregated Oxisol.J. Environ. Qual., 27: 132–138.

    Article  Google Scholar 

  • Waston J R, Parsons U W, 1974. Studies of soil organo-mineral fractions: I. isolation by ultrasonic dispersion.J. Soil Sci., 25: 1–8.

    Article  Google Scholar 

  • Zhou P H, Wu C L, 1993. The study on the research methods of soil anti-storability in Loess Plateau.J. Soil and Water Conserv., 13(1): 29–34. (in Chinese)

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Xingchang, Z., Jiyong, Z. & Shiqing, L. The enrichments of organic matter and total nitrogen in sediment as affected by relavant factors. J. Geogr. Sci. 14, 495–502 (2004). https://doi.org/10.1007/BF02837494

Download citation

  • Received:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02837494

Key words

Navigation