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Mapping gully erosion patterns in foothills of lower Shiwaliks


Table 3. Number of different ordered gullies in study catchments
Catchment 1st 2nd 3rd Total
I 91 22 1 114
II 90 16 -- 106
III 65 21 --- 86
IV 108 63 19 190

Table 4. Length of different ordered gullies in study catchments
Catchment 1st 2nd 3rd Total
I 3006 688 90 3784
II 2810 383.5 ---- 3193.5
III 1070.6 356.9 ----- 1427.5
IV 2214.5 994.8 506 3715.3

The study thus shows that the knowledge on gully network is a pre-requisite for their successful control. These being the continuous network need to be treated as a whole system rather than the individual gullies more so the lower order gullies. However, further studies are continuing so as to reach a logical conclusion.

References
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  • Burkard, M.B. and Kostaschuk, R.A. 1997. Patterns and control of gully growth along the shoreline of lake Huron. Earth Surf Process and Landforms, 22: 901-911.
  • Grissinger, E. M. and Murphy, J. B. 1989. Ephimeral gully erosion in the loess uplands, Gardwin Creek watershed, Northern Missisipi, USA. Proc. 4th Int. River Sedimentation Symp., Beijing, China, IASH Pub 236: 251-266.
  • Kukal, S.S. and Sur, H.S. 1992. Soil erosion hazards in the foothills of lower Shiwaliks. J. Indian Soc. Soil Sci., 40: 162-167.
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  • Meyer, A. and Martinez-Casasnovas, J.A. 1999. Prediction of existing gully erosion in Vineyard parcels of the NE Spain: a logistic modeling approach. Soil Tillage Res., 50: 319-331.
  • Stocking, M.A. 1980. Examination of the factors controlling gully growth. In: Boodt, M. de and Gabriels, D. (eds.) Assessment of Erosion, John Wiley and Sons, UK, pp. 505-520.
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