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首页> 外文期刊>European Journal of Agronomy >Nitrogen mineralization in sandy loam soils under an intensivedouble-cropping forage system with dairy-cattle slurry applications
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Nitrogen mineralization in sandy loam soils under an intensivedouble-cropping forage system with dairy-cattle slurry applications

机译:集约双作饲草系统下牛砂壤土中的氮矿化作用

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Nitrogen (N) mineralization and soil mineral N contents were measured at 2-week intervals over a 2-year period (June 1994-May 1996) on two different sites in the North West region of Portugal. The experiment was established in fields, which had for many years been under a double-cropping forage system with maize from May to September and a winter crop (mixture of cereals and Italian ryegrass) during the rest of the year. In addition to N fertilizers, dairy-cattle slurry was applied regularly at the sowing of each crop. On this intensive forage system, quantification of N released from slurry, crop residues and soil organic matter becomes important when better N use efficiency and reduced environmental impact from agricultural practices are required. Net N mineralization rates of the 0-10 cm soil layer fluctuated considerably between consecutive incubation periods and ranged from - 0.88 to 1.87 mg N kg(-1) day(-1) with annual average rates of between 0.41 and 0.65 mg N kg(-1) day(-1). The total N mineralized in the 10 cm depth soil layer reached values between 122 and 224 kg N ha(-1) year(-1), showing that mineralization was a very important N source for the crops. The amounts of N released during the cold season (November-February) were equivalent to 27-48% of the yearly total. Regression analysis indicated that seasonal variation in N mineralization was only poorly explained by soil moisture and temperature. The changing balance during the year between soil moisture and temperature will contribute to the relatively constant N mineralization rates. Soil mineral N contents during the maize crop were high and exceeded the nutrient requirements for the optimum yield of this crop. Under the climatic conditions of the region and due to the poor development of the winter crop plants at the time, the mineral N left in the soil after the maize crop and released by mineralization during the cold season is particularly vulnerable to nitrate leaching losses.
机译:在葡萄牙西北部两个不同地点的两年(1994年6月至1996年5月)中,每隔2周测量一次氮(N)矿化和土壤矿物质N含量。该试验是在多年的田间进行的,该田采用双季饲草系统,从5月至9月使用玉米,并在该年其余时间使用冬季作物(谷物和意大利黑麦草的混合物)。除氮肥外,还定期在每种作物的播种中施用牛乳浆。在这种集约化饲草系统上,当需要更高的氮利用效率和减少农业实践对环境的影响时,量化从泥浆,农作物残留物和土壤有机物中释放的氮就变得很重要。 0-10厘米土壤层的净氮矿化率在连续潜伏期之间波动很大,范围为-0.88至1.87 mg N kg(-1)天(-1),年平均比率在0.41至0.65 mg N kg( -1)天(-1)。在10厘米深的土壤层中矿化的总N达到122至224 kg N ha(-1)年(-1),表明矿化是农作物非常重要的氮源。寒冷季节(11月至2月)释放的氮量相当​​于每年总量的27-48%。回归分析表明,氮矿化的季节性变化仅能通过土壤水分和温度来很好地解释。一年中土壤湿度和温度之间不断变化的平衡将有助于相对恒定的氮矿化速率。玉米作物中的土壤矿质氮含量很高,超过了该作物最佳产量所需的养分。在该地区的气候条件下,由于当时冬季农作物的生长不良,玉米作物生长后留在土壤中并在寒冷季节因矿化而释放的矿物质氮特别容易遭受硝酸盐淋失的损失。

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