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Response of water and nitrogen losses to water management practices and green manure application in lowland paddy fields

机译:水和氮流失对低水田水管理实践和绿肥应用的响应

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摘要

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 (NO~- _3 -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 NH~+ _4 -N, NO~- _3 -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 NH~+ _4 -N, NO~- _3 -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 NH~+ _4 -N, 51.9 m3 day~(-1) ha~(-1) for NO~- _3 -N, and 55.5 m~3 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.
机译:农业用水管理实践的复杂性给试图确定水文途径如何影响水和氮(N)损失的研究人员提出了挑战。 2014年和2015年在中国漳河灌区一个典型的水稻农业流域进行了田间试验,以评估和量化水文路径与水和氮素损失之间的联系。根据气候条件和人工灌溉,确定了四个水管理时期,即灌溉时期(IP),降雨时期(RP),正常排水时期(DP)和非灌溉排水时期(NP)。排水期。实验结果表明,大部分水和氮流失发生在DP和RP上,侧向渗漏和尾水是观测到的排水的主要来源。氨氮(NH〜+ _4- -N,0.373 mg L〜(-1))和硝酸盐N(NO〜-_3- -N,0.285 mg L〜(-1))的平均浓度低,溶解氮(与绿肥施用相关的检出率为42.2-54.0%,而总氮的平均浓度(TN,1.376 mg L〜(-1))相对较高,在所研究的农业地区造成了轻微的氮污染。 DP和RP中溶解氮的浓度和比例最高。 NH〜+ _4-N,NO〜-_3-N和TN的平均日质量通量分别为0.027、0.020和0.095 kg ha〜(-1)day〜(-1),DP的大小和RP显着大于IP和NP。根据皮尔逊相关分析,NH〜+ _4-N,NO〜-_3-N和TN的平均浓度与排水量不相关,而幂函数可以量化各种水量下N质量通量与排水量之间的关系。管理期。 NH〜+ _4 -N的稻田N排放为零的平均排水阈值为45.2 m3 day〜(-1)ha〜(-1),51.9 m3 day〜(-1)ha NO〜-_3-N为〜(-1),TN为55.5 m〜3天〜(-1)ha〜(-1)。这些发现表明,控制排水流量对于减少稻田的水分流失和氮素损失非常重要。

著录项

  • 来源
    《Journal of irrigation and drainage engineering》 |2017年第12期|05017007.1-05017007.11|共11页
  • 作者单位

    State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan Univ, Wuhan, China;

    State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan Univ, Wuhan, China;

    State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan Univ, Wuhan, China;

    State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan Univ, Wuhan, China;

    State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan Univ, Wuhan, China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Drainage; Green manure; Irrigation; Nitrogen;

    机译:引流;绿肥灌溉;氮;

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