An in situ incubation technique to measure the contribution of organic nitrogen to potatoes

Agronomie Pub Date : 2004-07-01 DOI:10.1051/AGRO:2004022
M. Rodrigues
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引用次数: 16

Abstract

Field experiments which consisted of the incubation of soil within polyvinylchloride (PVC) tubes inserted in glass jars previously buried in potato crop rows were conducted in order to measure the contribution of soil organic matter and organic amendments to the N nutrition of the crop. The experiments were carried out in Braganca, NE Portugal, in the summer seasons of 1996-1998. Five treatments including farmyard manure, poultry manure, municipal solid wastes, urea and the control were used. Manures and urea were applied in rates which correspond to 100 kg N/ha. Nitrogen released from soil organic matter and manures was checked through crop N recovered and petiole nitrate concentrations. In the plots of urea treatments 80.1, 68.4 and 98.8 mg NO 3 -N kg -1 were released during the entire growing seasons of 1996, 1997 and 1998, respectively. In the control treatments 64.1, 41.5 and 55.4 mg NO 3 -N kg -1 were recorded. The mean values of NO 3 -N yielded from amended plots were not statistically different than control, excluding the plots of poultry manure on the initial sampling dates at the start of incubation. The measured amounts of inorganic N mineralized in the field from native soil organic matter were five to eight times higher than previous laboratory estimates from soil analysis. These results demonstrated that soils with low levels of organic matter could release significant amounts of inorganic N during a cropping season. Soil N availability estimated from the incubation technique was confirmed by petiole nitrate concentrations and closely related to the crop N recovered. However, in the plots of urea treatments some inconsistencies were found, probably originating from the leaching of urea as a molecular form to layers below the limit of soil coring. Soil N balance showed that more than 82% of inorganic N released from organic matter came from the 14-cm soil surface layer.
一种测定马铃薯有机氮贡献的原位培养技术
为了测量土壤有机质和有机改型对作物氮营养的贡献,进行了田间试验,将聚氯乙烯(PVC)管插入先前埋在马铃薯作物行的玻璃罐中。实验于1996-1998年夏季在葡萄牙东北部的布拉干卡进行。采用农家肥、禽粪、城市生活垃圾、尿素和对照5种处理。粪肥和尿素按100 kg N/ha施用。通过作物氮素恢复量和叶柄硝酸盐浓度测定土壤有机质和粪便中氮的释放量。1996年、1997年和1998年全生育期氮素释放量分别为80.1、68.4和98.8 mg。对照处理分别为64.1、41.5和55.4 mg no3 -N kg -1。除孵育开始时取样日期的禽粪样地外,改良样地的硝态氮产量均值与对照无统计学差异。从原生土壤有机质中测量到的无机氮矿化量比以前实验室土壤分析估计的高5到8倍。这些结果表明,低有机质水平的土壤在一个种植季节可以释放大量的无机氮。利用培养技术估算的土壤氮素有效性与叶柄硝酸盐浓度一致,且与作物氮素恢复密切相关。然而,在尿素处理的地块中发现了一些不一致,可能是由于尿素以分子形式淋滤到低于土壤取心极限的层。土壤氮平衡表明,有机质释放的无机氮82%以上来自14 cm土壤表层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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