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Impacts of typical rainfall processes on nitrogen in typical rainfield of black soil region in Northeast China

机译:东北黑土区典型雨场典型降雨过程对氮素的影响

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In recent years, non-point source (NPS) pollution has become the main contributor to water quality problems. Research on nitrogen (N) losses from farmland and the factors that influence these losses are very meaningful both in terms of increasing the crop yield and for improving environmental water quality. Hydrological processes are the vector of NPS pollution processes. In this study, 15 different natural rainfalls in the northeast area were monitored to analyze the lost characteristics of nitrogen under different rainfall conditions and the field management measures from July to August of 2013. The results show that total N (TN) content in the rainfalls of 2013 in the drainage area of the Runjin River is 0.18-4.89 mg/L. Judging from the mean flow output of various runoff zones in each rainfall, transverse tilling mode (TTT) < ecological recovery mode (VVR) < no-tillage mode (TNT) < reduced tillage system (TRT) < traditional tilling type (TCT) < bare land (VB). Judging from the mean sand output of various runoff zones in each rainfall, ecological recovery mode (VVR) < no-tillage mode (TNT) < traditional tilling type (TCT) < reduced tillage system (TRT) < traditional tilling type (TCT) < bare land (VB). Moreover, various experimental zones with different tilling systems are distinctively different in the concentration of losses of water-soluble nitrogen and particulate nitrogen and the loss of water-soluble nitrogen and particulate nitrogen per unit area. In the study area, particulate nitrogen carried by runoff sands was the primary forms of nitrogen losses under typical rainfall conditions. The four rainfalls have caused the downward eluviation of nitrogen along the depth of soils to different extents.
机译:近年来,面源污染已成为造成水质问题的主要因素。从增加作物产量和改善环境水质方面,研究农田中氮(N)的损失以及影响这些损失的因素都是非常有意义的。水文过程是NPS污染过程的媒介。在这项研究中,监测了东北地区的15种不同自然降雨,以分析不同降雨条件下氮素的损失特征以及2013年7月至8月的田间管理措施。结果表明,降雨中的总N(TN)含量润金河流域2013年的排放量为0.18-4.89 mg / L。从各降雨区径流的平均流量输出来看,横向耕作方式(TTT)<生态恢复方式(VVR)<免耕方式(TNT)<耕作方式(TRT)<传统耕作方式(TCT)<裸地(VB)。从每个降雨过程中各个径流区的平均出砂量来看,生态恢复模式(VVR)<免耕模式(TNT)<传统耕作类型(TCT)<耕作制度(TRT)<传统耕作类型(TCT)<裸地(VB)。而且,具有不同耕作系统的各个实验区在单位面积上水溶性氮和颗粒态氮的损失浓度以及水溶性氮和颗粒态氮的损失浓度上明显不同。在研究区,径流沙携带的颗粒氮是典型降雨条件下氮损失的主要形式。四次降雨导致氮素沿土壤深度的不同程度下降。

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