1. Response of Water and Nitrogen Losses to Water Management Practices and Green Manure Application in Lowland Paddy Fields.
- Author
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Baoli Xu, Dongguo Shao, Shu Chen, Haoxin Li, and Longzhang Fang
- Subjects
WATER management ,NITROGEN in water ,IRRIGATION ,WATER shortages ,GREEN manure crops ,PADDY fields ,PREVENTION - Abstract
The complexity of agricultural water management practices has challenged researchers attempting to determine how hydrological pathways affect water and nitrogen (N) losses. Field experiments in a typical rice agricultural catchment in the Zhanghe Irrigation District in China were conducted in 2014 and 2015 to evaluate and quantify the connections between hydrological pathways and water and N losses. Four water management periods--namely, the irrigation period (IP), the rainfall period (RP), the normal-drainage period (DP), and the nonirrigation-drainage period (NP)--were defined based on climate conditions and artificial irrigation and drainage periods. The experimental results indicated that most water and N losses occurred in DP and RP and that lateral seepage and tailwater were the main sources of the observed drainage. Low average concentrations of ammonia N (NH
4 + --N, 0.373 mg L-1 ) and nitrate N (NO3 - --N, 0.285 mg L-1 ) and low proportions of dissolved N (42.2-54.0%) were detected in association with green manure application, whereas the average concentration of total N (TN, 1.376 mg L-1 ) was relatively high, which resulted in slight N pollution in the studied agricultural area. The concentrations and proportions of dissolved N were greastest in DP and RP. The average daily mass fluxes of NH4 + --N, NO3 - --N, and TN were 0.027, 0.020, and 0.095 kg ha-1 day-1 , respectively, and the magnitudes in DP and RP were significantly greater than those in IP and NP. The average concentrations of NH4 + --N, NO3 - --N, and TN were not correlated to drainage discharge according to a Pearson correlation analysis, whereas a power function can quantify the relationship between N mass fluxes and discharge during various water management periods. The average thresholds of drainage discharge, at which N export from paddy fields equalled to zero, were 45.2 m³ day-1 ha-1 for NH4 + --N,51.9 m³ day-1 ha-1 for NO3 - --N, and 55.5 m³ day-1 ha-1 for TN. These findings indicate that controlling drainage discharge is important for the reduction of water loss and N loss from paddy fields. [ABSTRACT FROM AUTHOR]- Published
- 2017
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