Advanced Search

Indexed by SCI、CA、РЖ、PA、CSA、ZR、etc .

Volume 26 Issue 3
Jul 2015
Turn off MathJax
Article Contents
Qinghua Wu, Chunlei Liu, Wenjing Lin, Meng Zhang, Guiling Wang, Fawang Zhang. Quantifying the preferential flow by dye tracer in the North China Plain. Journal of Earth Science, 2015, 26(3): 435-444. doi: 10.1007/s12583-014-0489-4
Citation: Qinghua Wu, Chunlei Liu, Wenjing Lin, Meng Zhang, Guiling Wang, Fawang Zhang. Quantifying the preferential flow by dye tracer in the North China Plain. Journal of Earth Science, 2015, 26(3): 435-444. doi: 10.1007/s12583-014-0489-4

Quantifying the preferential flow by dye tracer in the North China Plain

doi: 10.1007/s12583-014-0489-4
More Information
  • Corresponding author: Qinghua Wu, wqh0505@126.com; Guiling Wang, Guilingw@163.com
  • Received Date: 15 May 2014
  • Accepted Date: 11 Sep 2014
  • Publish Date: 01 Jun 2015
  • The preferential flow plays a vital role on the infiltration of irrigation or rainfall. The objective of this study was to quantify preferential flow in the processing of irrigation infiltration in the field scale. Tests of different initial soil water contents and irrigation intensities were conducted using Brilliant Blue FCF (C.I.42090) dye tracer in Luancheng County of the North China Plain. The results showed that the percentages of infiltration by the preferential flow for irrigation depth of 25, 50, and 75 mm were 16.67%, 43.67%, and 34.17%, with 19.72%, 61.42%, 66.64% of dyed areas in the soil profile, respectively, which indicated that preferential flow was enhanced with increasing irrigation intensity, but reduced when the irrigation intensity was over 50 mm. The percentages of preferential flow for 75 and 180 mm previous irrigation producing different initial soil water contents were 23.26% and 18.97%, with 53.23% and 39.94% of dyed areas in the soil profile, respectively. Compared with the 75 mm without previous irrigation, the results indicated that higher initial soil water contents restrained the preferential flow in the field. Therefore, intermittent irrigation and low irrigation intensity patterns, and larger depth of plowing would be suggested to reduce the preferential flow which would increase the soil water utilization efficiency and reduce pollution risk of pesticide and fertilizer to groundwater.

     

  • loading
  • Alaoui, A., Caduff, U., Gerke, H. H., et al., 2011. Preferential Flow Effects on Infiltration and Runoff in Grassland and Forest Soils. Vadose Zone Journal, 10(1): 367-377 doi: 10.2136/vzj2010.0076
    Beven, K., Germann, P., 1982. Macropores and Water Flow in Soils. Water Resources Research, 18(5): 1311-1325 doi: 10.1029/WR018i005p01311
    Bu, N., Shang, S. H., Mao, X. M., et al., 2012. Fractal Characteristics of Finger Flow and Infiltration Laws in Layered Soil. Chinese Journal of Hydrodynamics, 27(2): 183-190 http://d.wanfangdata.com.cn/Periodical_sdlxyjyjz201202010.aspx
    Bundt, M., Widmer, F., Pesaro, M., et al., 2001. Preferential Flow Paths: Biological "Hot Spots" in Soils. Soil Biology and Biochemistry, 33(1): 729-738
    Chen, F. Q., Hui, S., 2006. A Study on Preferential Flow under Three Vegetations in the Upper Reach of Minjiang River by Brilliant Blue Dye Tracer. Journal of Ecological Science, 25(1): 69-73 (in Chinese with English Abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-STKX200601017.htm
    Cheng, Z. H., Zhang, J. B., 1998. Research Progress in Soil Preferential Flow. Soils, 6: 315-331 (in Chinese with English Abstract)
    Fei, Y. H., Zhang, Z. J., Zhang, F. E., et al., 2007. An Analysis of the Influence of Human Activity and Climate Change on Water Resources of the North China Plain. Acta Geoscientica Sinica, 28(7): 567-571 (in Chinese with English Abstract)
    Feng, J., Hao, Z. C., 2001. Research Process in Fractal Dimension Applied on Soil Macropore Flow. Hydrogeology & Engineering Geology, (9): 9-13 (in Chinese with English Abstract)
    Feng, J., Hao, Z. C., 2002. Distribution of Soil Macropores Characterized by CT. Advances in Water Resources, 13(5): 611-617 (in Chinese with English Abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-SKXJ200205013.htm
    Forrer, I., Papritz, A., Kasteel, R., et al., 2000. Quantifying Dye Tracers in Soil Profile by Image Processing. European Journal of Soil Science, 51: 313-322 doi: 10.1046/j.1365-2389.2000.00315.x
    Guo, H. R., 2008. The Experimental Study and Numerical Simulation of Groundwater Recharge Processes and Preferential Solute Transport in Soils: [Dissertation]. China University of Geosciences, Wuhan (in Chinese with English Abstract)
    Jarvis, N., Etana, A., Stagnitti, F., 2008. Water Repellency, Near-Saturated Infiltration and Preferential Solute Transport in a Macroporous Clay Soil. Geoderma, 143(3-4): 223-230 doi: 10.1016/j.geoderma.2007.11.015
    Jian, S. Q., Zhao, C. Y., Peng, H. H., et al., 2011. Root Influence on Soil Macropores by Dye Tracing and Image Processing Technology. Journal of Lanzhou University (Natural Sciences), 47(5): 62-66 (in Chinese with English Abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-LDZK201105012.htm
    Jørgensen, P. R., Hoffmann, M., Kistrup, J. P., et al., 2002. Preferential Flow and Pesticide Transport in a Clay-Rich Till: Field, Laboratory, and Modeling Analysis. Water Resources Research, 38(11): 28-1-28-15 doi: 10.1029/2001WR000494
    Larsson, M. H., Jarvis, N. J., Torstensson, G., et al., 1999. Quantifying the Impact of Preferential Flow on Solute Transport to Tile Drains in a Sandy Field Soil. Journal of Hydrology, 215(1-4): 116-134 doi: 10.1016/S0022-1694(98)00265-0
    Li, W. L., Jin, C. J., Wang, A. Z., et al., 2007. Research Progress in Soil Macropore Flow. Chinese Journal of Applied Ecology, 18(4): 888-894 (in Chinese with English Abstract) http://www.oalib.com/paper/1479990
    Lü, G., Wang, H. L., Huang, L., 2012. A Study on Macropore Properties of Forest Soil in Semi-Arid Region of Western Liaoning Province. Bulletin of Soil and Water Conservation, 32(5): 176-181 (in Chinese with English Abstract) http://search.cnki.net/down/default.aspx?filename=STTB201205037&dbcode=CJFD&year=2012&dflag=pdfdown
    Mooney, S. J., Nipattasuk, W., 2003. Quantification of the Effects of Soil Compaction on Water Flow Using Dye Tracers and Image Analysis. Soil Use and Management, 19(4): 356-363 doi: 10.1079/SUM2003210
    Morris, C., Mooney, S. J., Young, S. D., 2008. Sorption and Desorption Characteristics of the Dye Tracer, Brilliant Blue FCF, in Sandy and Clay Soils. Geoderma, 146(3-4): 434-438 doi: 10.1016/j.geoderma.2008.06.021
    Qi, D. H., Jin, M. G., Liu, Y. F., 2007. Determination of Preferential Flow in Precipitation Infiltration Recharge. Earth Science--Journal of China University of Geosciences, 32(3): 421-424 (in Chinese with English Abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200703016.htm
    Qin, Y. D., Ren, L., Wang, J., 2000. Review on the Study of Macropore Flow in Soil. Advances in Water Science, 11(2): 203-207 (in Chinese with English Abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-SKXJ200002016.htm
    Renaud, M., Thierry, B., 1996. An Isotopic Study (2H and 18O) of Water Movements in Clayey Soils under a Semiarid Climate. Water Resources Research, 32(4): 779-789 doi: 10.1029/96WR00074
    Sheng, F., Fang. Y., 2012. Study on Preferential Soil Water Flow Using Iodine-Starch Staining Method. Soils, 44(1): 144-148 (in Chinese with English Abstract)
    Shi, H., Wang, F., Li, Y. Y., 2007. Quantitative Studies on Soil Macropores under Artificial Chinese Pine Forest in Loess Hilly Region. Chinese Journal of Eco-Agriculture, 15(1): 9-13 (in Chinese with English Abstract)
    Shurbaji, A. R., Campbell, A. R., 1997. Study of Evaporation and Recharge in Desert Soil Using Environmental Tracers, New Mexico, USA. Environmental Geology, 29(3-4): 147-151 doi: 10.1007/s002540050112
    Subramanian, S. K., Li, Y., Cathles, L. M., 2013. Assessing Preferential Flow by Simultaneously Injecting Nanoparticle and Chemical Tracers. Water Resources Research, 49(1): 29-42 doi: 10.1029/2012WR012148
    Sun, L., Zhang, H. L., Cheng, J. H., et al., 2012. Relationship between Soil Macropore and Preferential Flow in Citrus Graden. Bulletin of Soil and Water Conservation, 32(6): 75-79 (in Chinese with English Abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-STTB201206016.htm
    Wang, K., Zhang, R. D., Wang, F. Q., et al., 2007. Characterizing Scale-Dependent Heterogeneity of Soil Water Movement through Dying Infiltration Experiments. Advances in Water Science, 18(2): 158-163 (in Chinese with English Abstract) http://www.researchgate.net/publication/295356856_Characterizing_scale-dependent_heterogeneity_of_soil_water_movement_through_dying_infiltration_experiments
    Weiler, M., Flühler, H., 2004. Inferring Flow Types from Dye Patterns in Macroporous Soils. Geoderma, 120(1-2): 137-153 doi: 10.1016/j.geoderma.2003.08.014
    Wu, J. Q., Zhang, J. F., Gao, R., 2009. Physical Simulation Experiments of Effects of Macropores on Soil Water Infiltration Characteristics. Transactions of the CSAE, 25(10): 13-18 (in Chinese with English Abstract) http://www.ingentaconnect.com/content/tcsae/tcsae/2009/00000025/00000010/art00003
    Wu, Q. H., 2008. Soil Water Dynamic Evolvement and High Efficiency Utilization under the Influence of Human Activity: [Dissertation]. Chinese Academy of Geological Sciences, Beijing (in Chinese with English Abstract)
    Wuest, S. B., 2009. Comparison of Preferential Flow Paths to Bulk Soil in a Weakly Aggregated Silt Loam Soil. Vadose Zone Journal, 8(3): 623-627 doi: 10.2136/vzj2008.0126
    Xiao, Z. X., Zhu, W. L., Niu, J. Z., et al., 2011. Soil Preferential Flow under Different Forest Stands in Jiufeng National Forestry Park. Hunan Agricultureal Sciences, (17): 118-121 (in Chinese with English Abstract) http://d.wanfangdata.com.cn/Periodical/hunannykx201117036
    Yu, H. L., Huang, J. Y., 2012. Research Progress on Influence of Mulching Gravel and Sand on Soil Macropore Characteristics and Soil Hydrological Process of Gravel- Sand Mulch Field. Research of Soil and Water Conservation, 19(4): 284-288 (in Chinese with English Abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-STBY201204061.htm
    Zhang, C. B., Liu, M. X., Wang, D. L., et al., 2012. Dyeing Characteristic of Preferential Flow under Forestland in the Three Gorges Reservoir Area. Journal of Soil and Water Conservation, 26(2): 80-84 (in Chinese with English Abstract) http://d.wanfangdata.com.cn/Periodical/trqsystbcxb201202018
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Figures(9)  / Tables(4)

    Article Metrics

    Article views(719) PDF downloads(195) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return