Influence of bare soil and cultivated land use types upstream of a bank gully on soil erosion rates and energy consumption for different gully erosion zones in the dry-hot valley region, Southwest China
- 388 Downloads
This study assessed temporal variation in soil erosion rates in response to energy consumption of flow (ΔE). It employed an in situ bank gully field flume experiment with upstream catchment areas with bare (BLG) or cultivated land (CLG) that drained down to bare gully headcuts. Water discharge treatments ranged from 30 to 120 L Min−1. Concentrated flow discharge clearly affected bank gully soil erosion rates. Excluding minimal discharge in the CLG upstream catchment area (30 L min−1), a declining power function trend (p ≤ 0.1) was observed with time in soil erosion rates for both BLG and CLG upstream catchment areas and downstream gully beds. Non-steady state soil erosion rates were observed after an abrupt collapse along the headcut slope after prolonged scouring treatments. However, as the experiment progressed, ΔE and energy consumption of flow per unit soil loss (ΔEu) exhibited a logarithmic growth trend (p < 0.1) at each BLG and CLG position. Although similar temporal trends in soil erosion and infiltration rates were observed, values clearly differed between BLG and CLG upstream catchment areas. Furthermore, Darcy–Weisbach friction factor (f) values in the CLG upstream catchment area were higher than the corresponding BLG area. In contrast to the BLG upstream catchment area, lower ΔEu and higher soil erosion rates were observed in the CLG upstream catchment area as a result of soil disturbances. This indicated that intensive land use changes accelerate soil erosion rates in upstream catchment areas of bank gullies and increase soil sediment transport to downstream gullies. Accordingly, reducing tillage disturbances and increasing vegetation cover in upstream catchment areas of bank gullies are essential in the dry-hot valley region of Southwest China.
KeywordsBank gully Headcut erosion Energy consumption of flow Land use Dry-hot valley
Financial support for this study was provided by the National Basic Research Program (973 Program) of China (2015CB452704), the “Western Light” Talents Cultivation program, CAS (2011, 2014), the 100 Talents Program of IMHE, CAS (SDSQB-2011-01), the Special Foundation of the President of CAS (2011), and the Youth Foundation of IMHE, CAS (2012). We are grateful for comments from Professor Thomas Glade and two anonymous reviewers.
Conflict of interest
The authors declare that they have no conflict of interest.
- Dong YF, Xiong DH, Su ZA, Li JJ, Yang D, Zhai J, Lu XN, Liu GC, Shi LT (2013) Critical topographic threshold of gully erosion in Yuanmou Dry-hot Valley in Southwestern China. Phys Geogr 34:50–59Google Scholar
- FAO (1988) Soil map of the world (revised legend). In: World Soil Resources Report 60, RomeGoogle Scholar
- Kostiakov AN (1932) On the dynamics of the coefficient of water percolation in soils and on the necessity for studying it from a dynamic point of view for purposes of amelioration. In: Transaction 6th Congress of the International Society of Soil Science. Moscow: Russian Part A, pp. 7–21Google Scholar
- Li Z, Lu K, Ding W (2002) Experimental study on dynamic processes of soil erosion on loess slope. J Soil Water Conserv 16(5–7):49 (in chinese)Google Scholar
- Li P, Li Z, Zheng L, Lu K (2005) Comparisons of dynamic mechanics of soil erosion and sediment yield by runoff on Loess slope. J Soil Water Conserv 19:66–69 (in Chinese)Google Scholar
- Li P, Li Z, Zheng L (2010) Experimental study on the critical relation between water erosion dynamics and soil erosion on steep loess slope. J Basic Sci Eng 18:435–441 (in Chinese)Google Scholar
- Soil Physics Laboratory, Institute of Soil Science, Chinese Academy of Sciences (1978) Soil Physical Characteristic Measuring Methods. Chinese Science Press, Beijing (in Chinese)Google Scholar
- Su ZA, Xiong DH, Dong YF, Zhang BJ, Zhang S, Zheng XY, Yang D, Zhang JH, Fang JR, Fang HD (2015) Hydraulic properties of concentrated flow for a bank gully in the dry-hot valley region of southwest China. Earth Surf Process Landf. doi: 10.1002/esp.3724
- Yang D, Xiong D, Juan Z, Li J, Su Z, Dong Y (2012) Morphological characteristics and causes of gullies in Yuanmou Dry-hot Vally Region. Sci Soil Water Conserv 10:38–45 (in Chinese)Google Scholar
- Yang D, Xiong DH, Guo M, Su ZA, Zhang BJ, Zheng XY, Zhang S, Fang HD (2015) Impact of grass belt position on the hydraulic properties of runoff in gully beds in the Yuanmou dry-hot valley region of Southwest China. Phys Geogr (accepted)Google Scholar
- Zhang X, Yang Z, Zhang J (2003) Lithologic types on hill slopes and revegetation zoning in the Yuanmou hot and dry valley. Scientia Silvae Sinicae 39:16–22 (in Chinese)Google Scholar
- Zhong XH (2000) Degradation of ecosystem and ways of its rehabilitation and reconstruction in dry and hot valley. Resour Environ Yangtze Basin 9:336–383 (in Chinese)Google Scholar