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Journal of Paleolimnology

, Volume 61, Issue 1, pp 17–35 | Cite as

Recent soil erosion in the Hongfeng catchment on the Guizhou Plateau, SW China revealed by analysis of reservoir sediments and soil loss modeling

  • Yao Luo
  • Minghui Lu
  • Hongya WangEmail author
  • Anan Qiu
Original paper
  • 101 Downloads

Abstract

The Guizhou Plateau in SW China is dominated by carbonate rocks and karst landforms. Erosion rates are low, but soils are thin and soil erosion remains a serious problem. Hongfeng Lake is the largest reservoir on the Guizhou Plateau. A 35-cm-long sediment core was retrieved from the reservoir and six soil profiles were sampled in the catchment. 137Cs activity was measured in the core to establish a chronological framework. Sediments and soils were analyzed for particle size, TOC, TN and mineral magnetism. Soil erosion that occurred between 1960 and 2003 was inferred from stratigraphic variations in particle size, TOC, C/N and magnetism of the sediments, aided by similar analyses on soils. Erosion was generally low from 1960 to 1987, but intensified thereafter, until about 1996. Between ca. 1996 and 2003, erosion declined. Land use data were derived from remote sensing images for 1973, 1990, 1993, 1996, 2000, 2003, 2006, 2010 and 2013, and running the Conversion of Land Use and its Effects at Small Region Extent (CLUE-S) model for 1976, 1979, 1982, 1985 and 1988. Precipitation, Digital Elevation Model (DEM) and soil-property data were also collected. Using these data, we determined input variables [rainfall erosivity (R), soil erodibility (K), slope length and gradient (LS), vegetation cover and management (C) and erosion control practices (P) for the Revised Universal Soil Loss Equation (RUSLE) Model]. Annual soil loss (A) was estimated for the Hongfeng Reservoir catchment for each year using the RUSLE model. Annual soil loss for 1973, 1976, 1979, 1982 and 1985 was generally low, with an average of 38.5 t ha−1 a−1. For 1988, 1990, 1993 and 1996, average annual soil loss increased to 57.7 t ha−1 a−1. The average for 2000 and 2003 declined to 46.6 t ha−1 a−1. Variations in the modeled annual soil loss are consistent with what was measured in the sediment record, implying that erosion events were recorded in the sediments despite temporary storage of sediments in the large, relatively flat catchment. Erosion was low and may have declined even more from 2003 to 2013. Despite the temporal variability, erosion was generally more intense in the west and east than in the central part of the catchment. Topography, rainfall and vegetation are the main factors that influenced soil erosion in the catchment.

Keywords

Soil erosion Reservoir sediments RUSLE modeling Guizhou Plateau Southwest China 

Notes

Acknowledgements

This research was supported by National Natural Science Foundation of China (Grant 41571130044 and 40335046). We are very grateful to Dr. Wenbo Wang, Dr. Qianqiong Zhu, Prof. Lin Xu, Ms. Ju Yuan and Prof. Ronggui Huang who helped sample sediments and soils from Hongfeng Reservoir and its catchment. We would also like to give our special thanks to the anonymous reviewers, Dr. Mark Brenner and the Associate Editor whose comments and suggestions have improved the manuscript.

References

  1. An YL, Cai GP, Xiong SY (1999) Soil erosion and its affective factors in Guizhou Upland. Bull Soil Water Conserv 19:47–52 (in Chinese with English abstract) Google Scholar
  2. Arnoldus HMJ (1977) Methodology used to determine the maximum potential average annual soil loss due to sheet and rill erosion in Morocco. FAO Soils Bull 34:39–51Google Scholar
  3. Bai ZG, Wan GJ, Huang RG, Liu TS (2002) A comparison on the accumulation characteristics of 7Be and 137Cs in lake sediments and surface soils in western Yunnan and central Guizhou, China. CATENA 49:253–270CrossRefGoogle Scholar
  4. Boar RR, Harper DM (2002) Magnetic susceptibilities of lake sediment and soils on the shoreline of Lake Naivasha, Kenya. Hydrobiologia 488:81–88CrossRefGoogle Scholar
  5. Boardman J (2006) Soil erosion science: reflections on the limitations of current approaches. CATENA 68:73–86CrossRefGoogle Scholar
  6. Boyle JF, Plater AJ, Mayers C, Turner SD, Straud RW, Weber JE (2011) Land use, soil erosion, and sediment yield at Pinto Lake, California: comparison of a simplified USLE model with the lake sediment record. J Paleolimnol 45:199–212CrossRefGoogle Scholar
  7. Chen JA, Wan GJ, Zhang F, Zhang DD, Huang RG (2004) Environmental records of lacustrine sediments in different time scales: sediment grain size as an example. Sci China Ser D 47:954–960CrossRefGoogle Scholar
  8. Chen H, Takashi O, Wu P (2017) Assessment for soil loss by using a scheme of alterative sub-models based on the RUSLE in a Karst Basin of Southwest China. J Integr Agr 16:377–388CrossRefGoogle Scholar
  9. De Boer DH (1997) Changing contributions of suspended sediment sources in small basins resulting from European settlement on the Canadian Prairies. Earth Surf Proc Land 22:623–639CrossRefGoogle Scholar
  10. Dearing JA (1991) Lake sediment records of erosional processes. Hydrobiologia 214:99–106CrossRefGoogle Scholar
  11. Dearing JA (1999) Holocene environmental change from magnetic proxies in lake sediments. In: Maher BA, Thompson R (eds) Quaternary climates, environments and magnetism. Cambridge University Press, Cambridge, pp 231–278CrossRefGoogle Scholar
  12. Dearing JA, Foster IDL (1993) Lake sediments and geomorphological processes: some thoughts. In: McManus J, Duck RW (eds) Geomorphology and sedimentology of lakes and reservoirs. Wiley, Chichester, pp 5–14Google Scholar
  13. Enters D, Lücke A, Zolitschka B (2006) Effects of land-use change on deposition and composition of organic matter in Frickenhauser See, northern Bavaria, Germany. Sci Total Environ 369:178–187CrossRefGoogle Scholar
  14. Eriksson MG, Sandgren P (1999) Mineral magnetic analyses of sediment cores recording recent soil erosion history in central Tanzania. Palaeogeogr Palaeocl Palaeoecol 152:365–383CrossRefGoogle Scholar
  15. Evans ME, Heller F (2003) Environmental magnetism: principles and applications of enviromagnetics. Academic Press, LondonGoogle Scholar
  16. Foster IDL, Owens PN, Walling DE (1996) Sediment yields and sediment delivery in the catchment of Slapton Lower Ley, south Devon, UK. Field Stud 8:629–661Google Scholar
  17. Gaillard MJ, Dearing JA, El-Daoushy F, Enell M, Hakansson H (1991) A late Holocene record of land use history, lake trophy and lake-level fluctuations at Lake Bjaresjo (south Sweden). J Paleolimnol 6:51–81CrossRefGoogle Scholar
  18. Hickey R, Smith A, Jankowski P (1994) Slope length calculations from a DEM within ARC/INFO grid. Comput Environ Urban 18:365–380CrossRefGoogle Scholar
  19. Huang CC, O’Connell M (2000) Recent land-use and soil-erosion history within a small catchment in Connemara, western Ireland: evidence from lake sediments and documentary sources. CATENA 41:293–335CrossRefGoogle Scholar
  20. Kansanen PH, Seppälä J (1992) Interpretation of mixed sediment profiles by means of a sediment-mixing model and radioactive fallout. Hydrobiologia 243–244:371–379CrossRefGoogle Scholar
  21. Kaushal S, Binford MW (1999) Relationship between C:N ratios of lake sediments, organic matter sources, and historical deforestation in Lake Pleasant, Massachusetts, USA. J Paleolimnol 22:439–442CrossRefGoogle Scholar
  22. Li CM, Wang HY (2010) 137Cs and 210Pb dating and inference of sedimentation rate for Maigang Reservoir in Southwest Guizhou Province. Bull Soil Water Conserv 30:215–219 (in Chinese with English abstract) Google Scholar
  23. Lu SG (2000) Lithological factors affecting magnetic susceptibility of subtropical soils, Zhejiang Province, China. CATENA 40:359–373CrossRefGoogle Scholar
  24. Lu MH (2007) The study on soil erosion based on analyses of sediments from lakes/reservoirs—a case study of the catchment of Hongfeng Lake in the Karst Area, Guizhou Province, Ph.D. thesis, Peking University, Beijing, ChinaGoogle Scholar
  25. Lu MH, Wang HY, Cai YL, Wang WB, Xu L (2008) Magnetic properties of core HF1-2 from Lake Hongfeng in Guizhou Province and its implications for soil erosion. J Lake Sci 20:298–305 (in Chinese with English abstract) CrossRefGoogle Scholar
  26. Lu SG, Chen DJ, Wang SY, Liu YD (2012) Rock magnetism investigation of highly magnetic soil developed on calcareous rock in Yun-Gui Plateau, China: evidence for pedogenic magnetic minerals. J Appl Geophys 77:39–50CrossRefGoogle Scholar
  27. Meyers PA, Lallier-Verges E (1999) Lacustrine sedimentary organic matter records of Later Quaternary paleoclimates. J Paleolimnol 21:345–372CrossRefGoogle Scholar
  28. Ministry of Water Resources of the People’s Republic of China (MWR of PRC) (2007) Classification criterions of soil erosion intensities (SL190-2007). China Water Power Press, Beijing (in Chinese) Google Scholar
  29. Oldfield F (1991) Environmental magnetism-a personal perspective. Quat Sci Rev 10:73–85CrossRefGoogle Scholar
  30. Oldfield F (1999) Environmental magnetism: the range of applications. In: Walden J, Oldfield F, Smith J (eds) Environmental magnetism: a practical guide, technical guide No 6. Quaternary Research Association, London, pp 212–222Google Scholar
  31. Olsson S, Regnéll J, Persson A, Sandgren P (1997) Sediment-chemistry response to land-use change and pollutant loading in a hypertrophic lake, southern Sweden. J Paleolimnol 17:275–294CrossRefGoogle Scholar
  32. Owens PN, Walling DE, He Q, Shanahan J, Foster IDL (1997) The use of caesium-137 measurements to establish a sediment budget for the Start catchment, Devon, UK. Hydrol Sci 42:405–423CrossRefGoogle Scholar
  33. Perseghin P, Incontri A (1998) The derivation of the green vegetation fraction from NOAA/AVHRR data for use in numerical weather prediction models. Int J Remote Sens 19:1533–1543CrossRefGoogle Scholar
  34. Ranzi R, Le TH, Rulli MC (2012) A RUSLE approach to model suspended sediment load in the Lo river (Vietnam): effects of reservoirs and land use changes. J Hydrol 422–423:17–29CrossRefGoogle Scholar
  35. Ritchie JC, McHenry JR (1990) Application of radioactive fallout 137Cs for measuring soil erosion and sediment accumulation rates and patterns: a review. Environ Qual 19:215–233CrossRefGoogle Scholar
  36. Royall D (2004) Particle-size and analytical considerations in the mineral-magnetic interpretation of soil loss from cultivated landscape. CATENA 57:198–207CrossRefGoogle Scholar
  37. Royall D (2007) A comparison of mineral-magnetic and distributed RUSLE modeling in the assessment of soil loss on a southeastern US cropland. CATENA 69:170–180CrossRefGoogle Scholar
  38. Schmidt RK, Koinig A, Thompson R, Kamenik C (2002) A multi proxy core study of the last 7000 years of climate and alpine land-use impacts on an Austrian mountain lake (Unterer Landschitzsee Niedere Tauern). Palaeogeogr Palaeoclimatol 187:101–120CrossRefGoogle Scholar
  39. Sharpley AN, Williams JR (1990) EPIC-erosion/productivity impact calculator: 1 model documentation. USDA Technical Bulletin No 1768, WashingtonGoogle Scholar
  40. Snowball IF (1991) Magnetic hysteresis properties of greigite (Fe3S4) and a new occurrence in Holocene sediments from Swedish Lappland. Phys Earth Planet Inter 68:32–40CrossRefGoogle Scholar
  41. Trimble SW (2009) Fluvial processes, morphology and sediment budgets in the Coon Creek Basin, WI, USA, 1975–1993. Geomorphology 108:8–23CrossRefGoogle Scholar
  42. Walden J, Slattery MC, Burt TP (1997) Use of mineral magnetic measurements to fingerprint suspended sediment sources: approaches and techniques for data analysis. J Hydrol 202:353–372CrossRefGoogle Scholar
  43. Walden J, White KH, Kilcoyne SH, Bentley PM (2000) Analyses of iron oxide assemblage within Namib dune sediments using high field remanence measurements (9T) and Mossbauer analysis. J Quat Sci 15:185–195CrossRefGoogle Scholar
  44. Walling DE (1983) The sediment delivery problem. J Hydrol 65:209–237CrossRefGoogle Scholar
  45. Walling DE (1990) Linking the field to the river: sediment delivery from agricultural land. In: Boardman J, Foster IDL, Dearing JA (eds) Soil erosion on agricultural land. Wiley, Chichester, pp 129–152Google Scholar
  46. Wan GJ (1999) 137Cs dating by annual distinguish for recent sedimentation: samples from Erhai Lake and Hongfeng Lake. Quat Sci 1:73–80 (in Chinese with English abstract) Google Scholar
  47. Wan GJ, Lin WZ, Huang RG, Chen ZL (1991) Dating characteristics and erosion traces of 137Cs vertical profiles in Hongfeng Lake sediments. Chin Sci Bull 36:674–677Google Scholar
  48. Wang SJ, Liu QM, Zhang DF (2004) Karst rocky desertification in southwestern China: geomorphology, landuse, impact and rehabilitation. Land Degrad Dev 15:115–121CrossRefGoogle Scholar
  49. Wang HY, Huo YY, Zeng LY, Wu XQ, Cai YL (2008) A 42-yr soil erosion record inferred from mineral magnetism of reservoir sediments in a small carbonate-rock catchment, Guizhou Plateau, southwest China. J Paleolimnol 40:897–921CrossRefGoogle Scholar
  50. Wang HY, Xu L, Sun XB, Lu MH, Du XY, Huo YY, Snowball I (2011) Comparing mineral magnetic properties of sediments in two reservoirs in “strongly” and “mildly” eroded regions on the Guizhou Plateau, southwest China: a tool for inferring differences in sediment sources and soil erosion. Geomorphology 130:255–271CrossRefGoogle Scholar
  51. Warren SD, Mitasova H, Hohmann MG, Landsberger S, Iskander FY, Ruzycki TS, Senseman GM (2005) Validation of a 3-D enhancement of the Universal Soil Loss Equation for prediction of soil erosion and sediment deposition. CATENA 64:281–296CrossRefGoogle Scholar
  52. Wischmeier WH, Smith DD (1978) Predicting rainfall erosion losses-a guide to conservation planning. United States Department of Agriculture, WashingtonGoogle Scholar
  53. Xiang L, Wu RJ, Ji L (1996) 137Cs and 241Am profiles and dating of sediments from two lakes in Yunnan Province, China. J Lake Sci 8:27–34 (in Chinese with English abstract) CrossRefGoogle Scholar
  54. Zhou ZF, An YL (2000) Remote sensing investigation of soil erosion present conditions and analyzing of spatial changeable in Guizhou Province. Bull Soil Water Conserv 20(23–25):41 (in Chinese with English abstract) Google Scholar
  55. Zhu LJ, Fu P, Wan GJ (1997) Magnetic characteristics and genesis of soils derived from carbonate rocks in Guizhou. Acta Pedol Sin 34:212–220 (in Chinese with English abstract) Google Scholar

Copyright information

© Springer Nature B.V. 2018

Authors and Affiliations

  1. 1.MOE Laboratory for Earth Surface Processes, School of Urban and Environmental SciencesPeking UniversityBeijingChina
  2. 2.Public Weather Service CenterChina Meteorological AdministrationBeijingChina

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