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Fates of slurry-nitrogen applied to mountain grasslands: the importance of dinitrogen emissions versus plant N uptake
Biology and Fertility of Soils ( IF 5.1 ) Pub Date : 2024-05-10 , DOI: 10.1007/s00374-024-01826-9
Michael Dannenmann , Irina Yankelzon , Svenja Wähling , Elisabeth Ramm , Mirella Schreiber , Ulrike Ostler , Marcus Schlingmann , Claus Florian Stange , Ralf Kiese , Klaus Butterbach-Bahl , Johannes Friedl , Clemens Scheer

Intensive fertilization of grasslands with cattle slurry can cause high environmental nitrogen (N) losses in form of ammonia (NH3), nitrous oxide (N2O), and nitrate (NO3) leaching. Still, knowledge on short-term fertilizer N partitioning between plants and dinitrogen (N2) emissions is lacking. Therefore, we applied highly 15N-enriched cattle slurry (97 kg N ha−1) to pre-alpine grassland field mesocosms. We traced the slurry 15N in the plant-soil system and to denitrification losses (N2, N2O) over 29 days in high temporal resolution. Gaseous ammonia (NH3), N2 as well N2O losses at about 20 kg N ha−1 were observed only within the first 3 days after fertilization and were dominated by NH3. Nitrous oxide emissions (0.1 kg N ha−1) were negligible, while N2 emissions accounted for 3 kg of fertilizer N ha−1. The relatively low denitrification losses can be explained by the rapid plant uptake of fertilizer N, particularly from 0–4 cm depth, with plant N uptake exceeding denitrification N losses by an order of magnitude already after 3 days. After 17 days, total aboveground plant N uptake reached 100 kg N ha−1, with 33% of N derived from the applied N fertilizer. Half of the fertilizer N was found in above and belowground biomass, while at about 25% was recovered in the soil and 25% was lost, mainly in form of gaseous emissions, with minor N leaching. Overall, this study shows that plant N uptake plays a dominant role in controlling denitrification losses at high N application rates in pre-alpine grassland soils.



中文翻译:

山地草原施用泥浆氮的命运:氮排放与植物氮吸收的重要性

用牛粪对草原进行密集施肥会导致环境氮(N)以氨(NH 3)、一氧化二氮(N 2 O)和硝酸盐(NO 3 -)浸出的形式大量损失。尽管如此,关于植物之间短期肥料氮分配和二氮(N 2)排放的知识仍然缺乏。因此,我们将高度15 N 富集的牛泥(97 kg N ha -1)应用于高山前草原田间环境。我们在 29 天内以高时间分辨率追踪了植物-土壤系统中的泥浆15 N 和反硝化损失(N 2、N 2 O)。仅在受精后的前3天内观察到气态氨(NH 3 )、N 2以及约20kg N ha -1的N 2 O损失,并且主要是NH 3。一氧化二氮排放量(0.1 kg N ha −1)可以忽略不计,而N 2排放量占肥料N ha −1 3 kg 。相对较低的反硝化损失可以通过植物对肥料氮的快速吸收来解释,特别是在0-4厘米深度,植物氮吸收在3天后就已经超过反硝化氮损失一个数量级。 17天后,地上植物总氮吸收量达到100 kg N ha -1,其中33%的氮来自施用的氮肥。肥料氮的一半存在于地上和地下生物量中,约25%在土壤中回收,25%流失,主要以气态排放形式存在,少量氮淋失。总体而言,本研究表明,高山前草原土壤在高施氮量下,植物氮吸收在控制反硝化损失方面发挥着主导作用。

更新日期:2024-05-10
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