首页> 外文会议>International Nitrogen Conference; 20041012-16; Nanjing(CN) >NITROGEN MOVEMENT IN THE SOIL PROFILE AS INFLUENCED BY LONG-TERM DIFFERENT FERTILIZATION
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NITROGEN MOVEMENT IN THE SOIL PROFILE AS INFLUENCED BY LONG-TERM DIFFERENT FERTILIZATION

机译:长期不同施肥对土壤剖面氮素运动的影响

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Nitrate contamination of surface and ground waters in Shaanxi province, China, has made it necessary to evaluate the impact of fertilizer N management on the accumulation and movement of NO_3-N in the soil. A long-term winter wheat - summer maize experiment with different fertilizer treatments was conducted to determine (ⅰ) the distribution and accumulation of NO_3-N in the soil profile, down to 400 cm depth, and (ⅱ) to estimate the movement of NO_3-N in different years. The results show that recovery of fertilizer N by 23 successive crops plus inorganic N in the soil profile ranging from 37.1 to 61.7%. The application of fertilizer N and NK without P resulted in a much larger NO_3-N concentration in the soil profile compared to the application of N with P or PK. With an annual application of 352 kg N·ha~(-1) alone or with K, peaks in NO_3-N accumulation occurred at 280 cm or 160 cm soil depth. However, with the application of NP or NPK, no peaks in NO_3-N distribution were discernible, with the exception of the surface 20 cm, NO_3-N concentrations were smaller at each sampling depth compared to the concentrations measured in the N and NK treatments. The annual application of 4500 kg·ha~(-1) maize stalk along with NPK led to a smaller NO_3-N content in the sub- soil. The amount of NO_3-N accumulation in the soil profile decreased as the cumulative N uptake by the crops increased. There were discernible movements of NO_3-N in the treatments of N and NK within a four-year interval, but not in the treatments of NP, NPK or NPK with organic materials. To minimize N leaching losses, fertilizer management must be balanced in a way that meets the needs of the growing crop.
机译:陕西省地表水和地下水的硝酸盐污染,使得有必要评估氮肥管理对土壤中NO_3-N积累和移动的影响。进行了长期冬小麦-夏季玉米不同肥料处理的试验,以确定(ⅰ)NO_3-N在土壤剖面中的分布和累积,深度低至400 cm,并且(ⅱ)估算NO_3的运动-N在不同的年份。结果表明,土壤中连续23种作物的氮肥利用率加上无机氮含量在37.1%至61.7%之间。与施用P或PK的N相比,施用不施用P的N和NK肥料导致土壤剖面中的NO_3-N浓度高得多。单独或与钾一起施用,每年施用352 kg N·ha〜(-1)时,在280 cm或160 cm的土壤深度出现NO_3-N积累峰值。但是,使用NP或NPK时,NO_3-N分布没有峰值,除了表面20 cm以外,与N和NK处理中测得的浓度相比,每个采样深度的NO_3-N浓度均较小。 。每年施用4500 kg·ha〜(-1)玉米秸秆和NPK导致土壤中NO_3-N含量降低。随着作物对氮的累积吸收增加,土壤剖面中NO_3-N的积累量减少。在四年的时间间隔内,N和NK处理中NO_3-N的运动明显,而有机材料处理NP,NPK或NPK则没有。为了最大程度地减少氮的淋失,肥料管理必须以能够满足作物生长需要的方式进行平衡。

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