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Published online 20 February 2008
Published in J Environ Qual 37:712-717 (2008)
DOI: 10.2134/jeq2007.0073
© 2008 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
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Nitrogen Loss through Lateral Seepage in Near-Trench Paddy Fields

Xin-Qiang Liang, Hua Li*, Ying-Xu Chen, Miao-Miao He, Guang-Ming Tian and Zhi-Jian Zhang

Dep. of Environmental Engineering, College of Natural Resources and Environmental Science, Zhejiang Univ., Hangzhou, 310029,China


Figure 1
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Fig. 1. The collection system for water samples of lateral seepage. B is a gravel-packed buffer zone between the bund and the trench, C is a container for collecting lateral seepage, R is a bucket with a pipe for collecting runoff, and T is a 1-m-deep trench. Lateral seepage water is pumped out from tube 1 using a syringe, and tube 2 is for air connection.

 

Figure 2
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Fig. 2. Dynamics of lateral seepage during three rice-growing seasons. Vertical bars above each data column indicate SE.

 

Figure 3
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Fig. 3. Dynamics of rainfall, irrigation, and floodwater level during three rice-growing periods.

 

Figure 4
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Fig. 4. Relationship between lateral seepage and floodwater level in flooded period of three rice seasons.

 

Figure 5
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Fig. 5. Temporal variations of total-N, NH4+–N, and NO3–N concentrations in lateral seepage water during three rice seasons. Vertical bars above each data point indicate SE. Arrows represent N fertilizer application dates.

 

Figure 6
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Fig. 6. Comparison of mean seasonal flux of total nitrogen in lateral seepage and surface runoff under a series of urea fertilizer application rates. *Significant differences (P = 0.05) between lateral seepage and surface runoff at each N rate. Error bars represent 1 SD.

 

Figure 7
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Fig. 7. Mean rice grain yield at different urea application rates in 2003, 2004, and 2005. Vertical bars above each data column indicate SE. Yields labeled with the same letter are not significantly different (P = 0.05).

 





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