Evaluation of Sediment Transport Rate of the Kizilirmak River Basin on the Tectonically Active North Anatolian Fault Zone (NAFZ), Turkey

  • Gulcan SarpEmail author
Conference paper
Part of the Advances in Science, Technology & Innovation book series (ASTI)


In this study, sediment transport rate of the Kizilirmak River basin located in the tectonically active North Anatolian Fault Zone (NAFZ) is evaluated in order to determine the effects of the NAFZ on the Kizilirmak basin sediment transport rate. Vegetation covers the basin area is extracted from the LANDSAT ETM data by using Normalized Difference Vegetation Index (NDVI). On the other hand, topographic attributes (elevation, slope, curvature, and water catchment) were obtained from Digital Elevation Model (DEM) to detect areas associated with sediment transport and accumulation. GIS was used to extract topographic profiles along with the Kizilirmak River and attributes as well as for the implementation of the stream power index (SPI), topographic wetness index (TWI), sediment transport index (STI) and channel width. The relation with the derived indices and NAFZ is determined by integrating hot and cold spot clusters of indices values mapped with Getis-Ord Gi* statistics. According to the derived results which highlighted hot and cold spots of the index values helped to identify the relation between sediment transport rate of the basin area and NAFZ.


Sediment transport rate Kizilirmak River NAFZ Getis-Ord Gi* statistics 


  1. 1.
    Keller, E.A., Pinter, N.: Active Tectonics. Earthquakes, Uplift and Landscape, 2nd edn. Prentice Hall, Upper Saddle River (2002). (E.E.U.U.)Google Scholar
  2. 2.
    Nag, S.K., Chakraborty, S.: Influence of rock types and structures in the development of drainage network in hard rock area. J. Indian Soc. Remote Sens. 31(1), 25–35 (2003)CrossRefGoogle Scholar
  3. 3.
    Magesh, N.S., Chandrasekar, N., Kaliraj, S., A GIS based automated extraction tool for the analysis of basin morphometry. Bonfring Int. J. Ind. Eng. Manag. Sci. 2(1), 32–35 (2012)Google Scholar
  4. 4.
    Strahler, A.N.: Hypsometric (area-altitude) analysis of erosional topography. Geol. Soc. Am. Bull. 63, 1117–1142 (1952)CrossRefGoogle Scholar
  5. 5.
    Cox, R.T.: Analysis of drainage-basin symmetry as a rapid technique to identify areas of possible quaternary tilt-block tectonics: an example from the Mississippi Embayment. Geol. Soc. Am. Bull. 106, 571–581 (1994)CrossRefGoogle Scholar
  6. 6.
    Hurtrez, J.E., Sol, C., Lucazeau, F.: Effect of drainage area on hypsometry from an analysis of small-scale drainage basins in the Siwalik hills (central Nepal). Earth Surf. Process. Landform 24, 799–808 (1999)CrossRefGoogle Scholar
  7. 7.
    Sørensen, R., Zinko, U., Seibert, J.: On the calculation of the topographic wetness index: evaluation of different methods based on field observations. Hydrol. Earth Syst. Sci. 10, 101–112 (2006)CrossRefGoogle Scholar

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© Springer Nature Switzerland AG 2019

Authors and Affiliations

  1. 1.Department of GeographySüleyman Demirel UniversityIspartaTurkey

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