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Li, Peng
- Study on the Influential Factors of SCS-CN Model Parameter S in the Loess Plateau Area
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Authors
Affiliations
1 Institute of Water Resources and Hydro-Electric Engineering, Xi'an University of Technology, Xi'an 710048, CN
1 Institute of Water Resources and Hydro-Electric Engineering, Xi'an University of Technology, Xi'an 710048, CN
Source
Nature Environment and Pollution Technology, Vol 15, No 2 (2016), Pagination: 707-714Abstract
SCS-CN method, developed by the U.S. Department of Agriculture, is simple, effective and can be used in the area having lack of rainfall process data, thus has been widely used to estimate the runoff. In this study, 213 runoff events from 9 plots at Zizhou located on the Loess Plateau area, were studied and applied to calibrate water storage capability of soil which is donated as S in the SCS-CN method. The influence factors of S parameter were then analysed. The results show that the main influence factor of S is initial abstraction Ia. The initial abstraction ratio (Ia/S) at Tuanshangou watershed is 0.03. The maximum 30-minute rainfall intensity, 5-day prior rainfall amount and soil moisture in the top 20 cm soil layer has no influence on the S parameter.Keywords
SCS-CN Model, Retention Parameter (S), Runoff, Loess Plateau Area.References
- Andrews, R. G. 1954. The use of relative infiltration indices in computing runoff. Cited in Rainfall-Runoff Relation, Singh V. P. (ed.), Water Resources Publications, Littletion, Colo.
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- Auerswald, K. and Haider, J. 1996. Runoff curve numbers for small grain under German cropping conditions. Journal of Environmental Management, 47: 223-228.
- Bosznay M. 1989. Generalization of SCS curve number method. Irrig. and Drain. Engineer, ASCE, 115(1): 139-144.
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- Huang, M.B., Gallichand, J., Dong, C.Y., Wang, Z.L. and Shao, M.G. 2007. Use of soil moisture data and curve number method for estimating runoff in the Loess Plateau of China. Hydrological Processes, 21: 1471-1481.
- Knisel, W. 1980. CREAMS-A field scale model for chemicals, runoff, and erosion from agricultural management systems. USDA Conservation Research Report 26. Upper Sarby, Pennsylvania, USDA.
- Luo, L.F., Zhang, K.L. and Fu, S.H. 2002. Application of runoff curve number method on Loess Plateau. Bulletin of Soil and Water Conservation, 22(3): 58-61. (in Chinese)
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- Mack, M.J. 1995. HER-hydrologic evaluation of runoff; the soil conservation service curve number technique as an interactive computer model. Computer & Geosciences, 21(8): 929-935.
- Mishra, K. S. and Singh, V. P. 1999. Another look at SCS-CN method. Journal of Hydrologic Engineering, 4(3): 257-264.
- Mockus, V. 1949. Estimation of total (and peak rates of) surface runoff for individual storms. In “Interim survey report grand (neosho) Rivershed”. Exhibit A of Appendix B. U>S> Dep. Agric. (U.S. Gov. Print. Office, Washington, D.C.).
- Soil Conservation Service (SCS). 1956,1964,1972,1985. “Section 4, hydrology”. National Engineering Handbook, U.S. Department of Agriculture, Washington, D.C.
- Wang, Y. and Huang, M.B. 2008. Optimizing parameters of SCS-CN method for application on the Loess Plateau. Bulletin of Soil and Water Conservation, 28(1): 54-58. (in Chinese)
- Wang, Z.L., Shao, M. and Chang, Q.R. 1995. Effects of rainfall factors on soil erosion in Loess Plateau. Journal of Northwest A & F University, 26(4): 101-105. (in Chinese)
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- Zhang, Y.X., Mu, X.M. and Wang, F. 2008. Calibration and validation to parameter γ of soil conservation service curve number method in hilly region of the loess plateau. Agricultural Research in the Arid Areas. 26(5): 124-128. (in Chinese).
- Effects of Perennial Vegetation on Runoff and Erosion for Field Plots on Loess Plateau in China
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Authors
Affiliations
1 Key Lab of Northwest Water Resources and Environment Ecology of MOE, Xi’an University of Technology, Xi’an, Shaanxi, CN
2 Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Education, Yangling, Shaanxi, 712100, CN
3 Department of Military Economy, Engineering University of CAPF, Xi’an Shaanxi, 710086, CN
1 Key Lab of Northwest Water Resources and Environment Ecology of MOE, Xi’an University of Technology, Xi’an, Shaanxi, CN
2 Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Education, Yangling, Shaanxi, 712100, CN
3 Department of Military Economy, Engineering University of CAPF, Xi’an Shaanxi, 710086, CN
Source
Nature Environment and Pollution Technology, Vol 12, No 1 (2013), Pagination: 63-68Abstract
Vegetation is one of effective methods for soil and water conservation. How to select suitable vegetation species is a key problem in the practice. In this study. through 7 years observations on the rainfall, vegetation cover, total runoff and sediment in the plots, results indicated that the benefit of the vegetative cover on runoff and sediment dominated on all plots. The accumulative sediment yield from bare plot was 7 times to that from Astragalus absurgens + Caragana korshindkii plots, also over 4 times to that from the Medicago sativa, Medicago sativa + Caragana korshindkii and Astragalus absurgens plots. Among all the vegetation types, Caragana korshindkii was the most efficient in reducing the runoff, and the combination of shrub and grass also had better effect in reducing the runoff. The accumulative runoff from bare plot was 2.57 times to that from the C. korshindkii, and over 2 times to that from M. sativa, M. sativa + C. korshindkii, A. absurgens + C. korshindkii and Vicia amucena + C. korshindkii. This study is of great importance for the selection of suitable species for vegetation reconstruction in arid and semi-arid areas.Keywords
Vegetation Coverage, Runoff, Erosion, Sediment, Shrubs and Grasses, Loess Plateau.- Dynamic Mechanics of Soil Erosion by Runoff on Loess Slope
Abstract Views :158 |
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Authors
Affiliations
1 Xi'an University of Technology, Xi'an Shaanxi, 710048, CN
1 Xi'an University of Technology, Xi'an Shaanxi, 710048, CN
Source
Nature Environment and Pollution Technology, Vol 12, No 2 (2013), Pagination: 297-301Abstract
In this research, soil erosion and sediment yield were calculated by runoff shear stress, runoff energy consumption and runoff power theory. Results indicated that a linear relationship existed between the average runoff shear stress and sediment yield. Soil erodibility in the experiment was 178.5g/(Pa·min), and the critical shear stress value was 0.54 Pa. Results from energy consumption implied that there was also a linear relationship between sediment transportation and energy consumption of runoff unit width: Dr = 14.61 (ΔE-0.37), which indicated that the soil erodibility was 14.61g/J, with a critical energy consumption of 0.37J/(min·cm). Results from runoff power theory showed that sediment transportation increased with increase in runoff power, and the simple linear relationship was also regressed: Y = 8942.2x - 68.676. Generally, these three theories each showed certain advantages in describing the soil erosion processes on the slope, among which the results from energy consumption theory were simpler, more accurate, and proved more convenient in describing soil erosion on the slope.Keywords
Loess Slope, Runoff Energy, Runoff Power, Shear Stress, Soil Erosion.- Adsorption of Dye in Aqueous Solution by the Waste Polymer Activated Carbon
Abstract Views :152 |
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Authors
Affiliations
1 College of Life Science, Shaoxing University, Shaoxing, 312000, CN
2 Department of Life Science, Shaoxing University, Yuanpei College, Shaoxing, 312000, CN
1 College of Life Science, Shaoxing University, Shaoxing, 312000, CN
2 Department of Life Science, Shaoxing University, Yuanpei College, Shaoxing, 312000, CN
Source
Nature Environment and Pollution Technology, Vol 15, No 4 (2016), Pagination: 1227-1230Abstract
The waste polymer activated carbon was prepared from tyre by NaOH activation, which was used for the adsorption of dye Direct Scarlet 4BS in aqueous solution. The influences of pH value, activated carbon dosage, adsorption time and reaction temperature on adsorption rate were discussed in details. It was shown that the activated carbon dosage, adsorption time and reaction temperature had an important effect on the removal of dye Direct Scarlet 4BS in aqueous solution. However, the removal of dye Direct Scarlet 4BS was little dependent on pH value in solution. At 0.6g of activated carbon, 60mg/L of initial dye concentration, 60min, 35°C and pH 4.0, the removal of dye Direct Scarlet 4BS reached 85.14%.Keywords
Waste Polymer, Activated Carbon, Direct Scarlet 4BS Dye, Adsorption.References
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- Baêta, B.E.L., Luna, H.J., Sanson, A.L., Silva, S.Q. and Aquino, S.F. 2013. Degradation of a model azo dye in submerged anaerobic membrane bioreactor (SAMBR) operated with powdered activated carbon (PAC). J. Environ. Manage., 128(15): 462-470.
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- Chan, O.S., Cheung, W.H. and McKay, G. 2012. Single and multicomponent acid dye adsorption equilibrium studies on tyre demineralised activated carbon. Chem. Eng. J., 191(15): 162-170.
- Duan, X.H., Srinivasakannan, C. and Liang, J.S. 2014. Process optimization of thermal regeneration of spent coal based activated carbon using steam and application to methylene blue dye adsorption. J. Taiwan Inst. Chem. Eng., 45(4): 1618-1627.
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- Application of Sliding-Block Reverse-Circulation Drilling Bit in Multi-Layer Goaf Detection
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Authors
Affiliations
1 College of Construction Engineering, Jilin University, Changchun 130026, CN
2 Xian Research Institute of China Coal Research Institute, Xian 710043, CN
3 Changchun Institute of Technology, Jilin University, Changchun 130021, CN
1 College of Construction Engineering, Jilin University, Changchun 130026, CN
2 Xian Research Institute of China Coal Research Institute, Xian 710043, CN
3 Changchun Institute of Technology, Jilin University, Changchun 130021, CN