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Estimation of baseflow nitrate loads by a recursive tracing source algorithm in a rainy agricultural watershed

机译:递归溯源算法估算多雨农业流域基流硝酸盐负荷

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Baseflow has become an important source of nitrate nonpoint source pollution in many intensive agricultural watersheds. Uncertainties in baseflow nutrient load separation are caused by the effects of hydrometeorological factors on both baseflow recession and baseflow nutrient load recession. These uncertainties have not been addressed well in the existing separating algorithms, which are based on simple baseflow rate-load relationships. In the present study, a recursive tracing source algorithm (RTSA) was developed based on a nonlinear reservoir algorithm and hydrometeorology-corrected baseflow nutrient load recession parameter. This approach was used to reduce the uncertainty of baseflow nitrate load estimation caused by variations in different load recessions under varying climate conditions. RTSA validation in a typical rainy agricultural watershed yielded Nash-Sutcliffe efficiency, root mean square error-observation standard deviation ratio, and R-2 values of 0.91, 0.30, and 0.91, respectively. The baseflow nitrate-nitrogen (NNO3-) loads from 2003 to 2012 in the Changle River watershed of eastern China were estimated with the RTSA. The results indicated that baseflow nitrate export accounted for 62.0% of the mean total annual NNO3- loads (18.0 kg/ha). The total baseflow NNO3- export was highest in spring (3.6 kg/ha), followed by summer (3.2 kg/ha), winter (2.3 kg/ha), and autumn (2.1 kg/ha). The contribution of baseflow to total nitrate in the stream decreased in the order of winter (69.88%) >spring (66.59%) >autumn (60.36%) >summer (54.04%). The monthly baseflow NNO3- loads and flow-weighted concentrations greatly increased during the research period (Mann-Kendall test, Z(s) > 2.56, p < .01). Without proper countermeasures, baseflow nitrate may represent a serious long-term risk for water surfaces in the future.
机译:在许多集约化农业流域中,基流已成为硝酸盐面源污染的重要来源。水文气象因素对底流营养物负荷衰退和底流营养物负荷衰退的影响,导致底流营养物负荷分离的不确定性。这些不确定性在现有的基于简单基流速率-负载关系的分离算法中没有得到很好的解决。在本研究中,基于非线性油藏算法和经水文校正的底流养分负荷降低参数,开发了一种递归跟踪源算法(RTSA)。该方法用于减少由于气候条件不同而造成的不同负荷衰退的变化而导致的基流硝酸盐负荷估算的不确定性。在一个典型的多雨农业流域中,RTSA验证产生了纳什-萨特克利夫效率,均方根误差观测标准差比和R-2值分别为0.91、0.30和0.91。利用RTSA估算了中国东部长乐河流域2003年至2012年的基流硝态氮(NNO3-)负荷。结果表明,基流硝酸盐出口量占年度NNO3平均总负荷(18.0 kg / ha)的62.0%。春季(3.6千克/公顷),春季(3.2千克/公顷),冬季(2.3千克/公顷)和秋季(2.1千克/公顷)的NNO3-总基流出口量最高。溪流对总硝酸盐的贡献按冬季(69.88%)>春季(66.59%)>秋季(60.36%)>夏季(54.04%)的顺序减小。在研究期间,每月的基本流量NNO3-负荷和流量加权浓度大大增加(Mann-Kendall检验,Z(s)> 2.56,p <.01)。如果没有适当的对策,将来硝酸基流硝酸盐可能会严重威胁水面。

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