Characteristics of flow production and sediment production of Pinus tabulaeformis through artificial rainfall simulation

Abstract

In order to know well the relationship between vegetation and water in North China, especially Beijing, with exceptional water resources, we studied the characteristics of flow production and sediment production under different rainfall intensities by artificial rainfall simulation device. Results showed that increase of rainfall intensity would prolong the whole process of flow production, and vegetation on the slope would delay that process. Within the same duration, total runoff volume of each runoff plot and rainfall intensity had significant linear relationship. When vegetation kept unchanged, runoff velocity increased significantly with the increase of rainfall intensity, and owing to the formation of low permeable layer, the velocity increased fiercely during the early 3 minutes, reached stable at 10 - 15 minute. With the same rain intensity, total sediment yield decreased with rise of vegetation coverage, but increased obviously with rise of rain intensity and effectiveness of controlling sediment about 1 m x 1 m Pinus tabulaeformis stand decreased firstly and then increased, while that about 1.5 m x 1.5 m Pinus tabulaeformis stand kept decreasing. Since the tags with A, B and C for 0.42 mm/min, 0.83 mm/min, 1.29 mm/min, order of sediment concentration of wasteland plot was B > C > A, and 1 m x 1 m Pinus tabulaeformis plot B > A > C. Through this study, some suggestions were expected to be provided for water balance of Beijing area and certain basis for construction of shelter forest.

Share and Cite:

Zhao, Y. , Niu, J. , Li, J. , Tan, J. , Han, Y. and Zhang, Y. (2012) Characteristics of flow production and sediment production of Pinus tabulaeformis through artificial rainfall simulation. Open Journal of Ecology, 2, 74-78. doi: 10.4236/oje.2012.22009.

Conflicts of Interest

The authors declare no conflicts of interest.

References

[1] Yang, X.-B., Song, Q.-F., Cao, Y.-S., et al. (2009) Study on management models of typical small watershed in mountain and rocky area of North China—Based on beizhuang small watershed. Journal of Soil and Water Con- servation in China, 7, 10-12.
[2] Jin, H.-C. (2002) Soil and water loss and its prevention in Beijing. Journal of Beijing Water Resources, 2, 16-19.
[3] Xiao, Z.-X., Zhu, W.-L., Niu, J.-Z., et al. (2011) Soil preferential flow under different forest stands in Jiufeng National Forestry Park. Journal of Hunan Agricultural Sciences, 17, 118-121.
[4] Yan, M. (2005) Studies on ecological benefits evaluation in Jiufeng National Forest Park. PhD Thesis, Beijing Forestry University, Beijing.
[5] Wang, Y., Qiao, Y. and Sun, X.-Y. (2010) Soil taxonomy in Jiufeng National Forest Park. Beijing. Journal of Beijing Forestry University, 32, 217-220.
[6] Zhang, G.-H., Liu, B.-Y. and Li, P.-K. (2007) Principles and properties of artificial trough rainfall simulator. Journal of Bulletin of Soil and Water Conservation, 27, 56-60.
[7] Li, S.-Y. and Ma, J.-J. (2011) Impact of urbanization on precipitation in Beijing area. Journal of the Meteorological Sciences, 31, 414-421.
[8] Luo, D. (2008) Studies on the dynamic characteristics of rainfall under the forest in Beijing mountainous area. PhD Thesis, Beijing Forestry University, Beijing.
[9] Chen, H.-S., Shao, M.-A., Zhang, X.-C., et al. (2005) Field experiment on hillslope rainfall infiltration and run- off under simulated rainfall conditions. Journal of Soil Water Conservation, 19, 5-8.
[10] Wang, Y.-L., et al. (2011) Sediment and runoff yield characteristics of slope lands under different intensity of rainfall in southern region of Ningxia. Ningxia Journal of Agriculture and Forestry Science and Technology, 52, 64-67.
[11] Duan, W.-B. and Liu, S.-C. (2006) Analysis on runoff and sediment yields of water conservation forests in Lianhua Lake reservoir area. Journal of Soil and Water Conservation, 20, 12-15.
[12] Zhou, H.-F., Wang, D.-Q., Ma J., et al. (2009) Impacts of grass coverage and rainfall intensity on runoff and sedi- ment yield in Tianshan Mountains of China—A case study of the Tianchi Natural Lake reserve area. Journal of Bulletin of Soil and Water Conservation, 29, 26-29.
[13] Martínez Raya, A., Durán Zuazo, V.H. and Francia- Martínez, J.R. (2006) Soil erosion and runoff response to plant-cover strips on semiarid slopes (SE Spain). Land Degradation and Development, 17, 1-11. doi:10.1002/ldr.674
[14] Xu, X.-L., Ma, K.-M., Fu, B.-J., et al. (2006) Research review of the relationship between vegetation and soil loss. Journal of Acta Ecologica Sinica, 26, 3137-3143.
[15] Assouline, S. (2004) Rainfall-induced soil surface sealing: A critical review of observations, conceptual models, and solutions. Vadose Zone Journal, 3, 570-591. doi:10.2113/3.2.570
[16] Hudson, N.W. and Jackson, D.C. (1959) Results achieved in the measurement of erosion and runoff in Southern Rhodesia. Proceedings of the 3rd Inter-African Soils Conference, Dalaba, 2-11 November 1959, 1-15.
[17] Lu, S.-W., Feng, Q., Yu, X.-X., et al. (2008) Studies on the configuration and function of different density pine in Rocky Mountain area of Beijing. Journal of Research of Soil and Water Conservation, 15, 117-121.
[18] Li, P., Cai, W.-B., Zheng, L.-Y., et al. (2006) Effects of vegetative cover on runoff hydraulic characteristics and erosion. Journal of Science of Soil and Water Conservation, 4, 55-59.
[19] Qiao, G.-J., Tan, L.-G. and Chen, E.-Y. (2009) Experi- mental study on deceleration of soil erosion by watershed vegetation. Journal of Water Resources Protection, 25, 52-56.
[20] Huang, M.-B. and Liu, X.-Z. (2002) Regulation effect of forest vegetation on watershed runoff in the Loss Plateau. Chinese Journal of Applied Ecology, 13, 1057-1060.
[21] Li, M., Yao, W.-Y., Ding, W.-F., et al. (2005) Effect of grass coverage on sediment yield in the hillslope-gully side erosion system. Journal of Geographical Sciences, 60, 25-732.

Copyright © 2024 by authors and Scientific Research Publishing Inc.

Creative Commons License

This work and the related PDF file are licensed under a Creative Commons Attribution 4.0 International License.