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。