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首页> 外文期刊>Journal of plant nutrition and soil science >Nitrogen turnover in bare soil planted subsequently with grass as investigated by electro-ultrafiltration (EUF)
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Nitrogen turnover in bare soil planted subsequently with grass as investigated by electro-ultrafiltration (EUF)

机译:电超滤(EUF)研究了随后种植草的裸露土壤中的氮素转化

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摘要

Changes of EUF-extractable nitrogen (N) (nitrate, ammonium, organic N) in 20 arable bare soils, subsequently planted with ryegrass (Lolium multiflorum L.) and cutting three times were investigated in pot experiments. All 20 soils responded qualitatively in the same way. During the period of bare soil, there was a significant increase of EUF-extractable nitrate (EUF NO3-), while extractable ammonium (EUF NH4+) remained on the same level and organic N (EUF N-org) decreased. This decrease, however, was not significant. From sowing until the first cutting of the grass, EUF-NO3- concentration decreased to almost zero. This low EUF-NO3- 3 level was maintained throughout the subsequent experimental period (three cuttings of grass). During the growth of the first cutting, EUF N-org decreased while EUF NH4+ remained constant, however, on a low level. EUF NH4+ fell during the growth of the second and third cutting. In this period, how-ever, the N supply of the grass was insufficient. EUF N-org decreased during the growth of the second cutting, but increased during the growth of the third cutting. This shows that the EUF-N-org fraction represents a transient pool, which M. EUF NO3-, EUF NH4+ and EUF N-org gains and loses 3 41 correlated with the N-org uptake of the grass. Strongest correlation for EUF NO3- was found for the first cutting (p < 0.001), and for EUF Q and EUF N-org for the second and third cutting (p < 0.001). Total soil N was not correlated with the N uptake of the grass. EUF N was only about 2% of the total N. This relatively small EUF-N-org fraction, however, is relevant for the mineralization of organic soil N, and the N quantity indicated by EUF N-org is in the range of the N amount mineralized in arable soils within a growing season.
机译:在盆栽试验中研究了EUF可提取的氮(N)(硝酸盐,铵,有机氮)在20种耕地裸露土壤中的变化,随后种植了黑麦草(Lolium multiflorum L.),并砍了三遍。所有20种土壤都以相同的方式对定性做出反应。在光秃秃的土壤时期,可提取的EUF硝酸盐(EUF NO3-)显着增加,而可提取的铵盐(EUF NH4 +)保持在相同水平,而有机氮(EUF N-org)下降。但是,这种下降并不明显。从播种到第一次割草,EUF-NO3-的浓度几乎降至零。在随后的整个实验期间(三棵草),都保持了较低的EUF-NO3- 3水平。在第一次切割的增长过程中,EUF的N-org下降,而EUF的NH4 +保持恒定,但是处于较低水平。 EUF NH4 +在第二次和第三次切割的增长期间下降。然而,在此期间,草的氮供应不足。 EUF N-org在第二次切割的增长期间减少,但在第三次切割的增长期间增加。这表明EUF-N-org分数代表了一个瞬时池,M。EUF NO3-,EUF NH4 +和EUF N-org得失3,与草的N-org吸收有关。第一次切割的EUF NO3-相关性最强(p <0.001),第二次和第三次切割的EUF Q和EUF N-org相关性最强(p <0.001)。土壤总氮与草的氮吸收无关。 EUF N仅占总N的2%。但是,EUF-N-org相对较小,与有机土壤N的矿化有关,EUF N-org指示的N量在N的范围内。在生长季节中,N含量在可耕土壤中矿化。

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