Irina Yankelzon, Georg Willibald, Michael Dannenmann, Francois Malique, Ulrike Ostler, Clemens Scheer, Klaus Butterbach-Bahl
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The system inherent leakage rate was about 55 µg N m<sup>− 2</sup> h<sup>− 1</sup> for N<sub>2</sub>, while N<sub>2</sub>O leakage rates were below the detection limit (< 1 µg N m<sup>− 2</sup> h<sup>− 1</sup>). In our experiment, we found higher cumulative gaseous N<sub>2</sub> + N<sub>2</sub>O losses in sown soil (0.34 ± 0.02 g N m<sup>− 2</sup>) as compared to bare soil (0.23 ± 0.01 g N m<sup>− 2</sup>). N<sub>2</sub> fluxes accounted for approximately 94–96% of total gaseous N losses in both planted and unplanted mesocosms. N losses, as determined by the <sup>15</sup>N mass balance approach, were found to be 1.7 ± 0.5 g N m<sup>− 2</sup> for the sown soil and 1.7 ± 0.6 g N m<sup>− 2</sup> for the bare soil, indicating an inconsistency between the two assessment methods. Soil respiration rates were also higher in sown mesocosms, with cumulative soil and aboveground biomass CO<sub>2</sub> respiration reaching 4.8 ± 0.1 and 4.0 ± 0.1 g C m<sup>− 2</sup> over the 33-day incubation period, in sown and bare soil, respectively. Overall, this study measured the effect of wheat growth on soil denitrification, highlighting the sensitivity and utility of this advanced incubation system for such studies.</p>","PeriodicalId":9210,"journal":{"name":"Biology and Fertility of Soils","volume":null,"pages":null},"PeriodicalIF":5.1000,"publicationDate":"2024-03-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"A new incubation system to simultaneously measure n2 as well as n2o and co2 fluxes from plant-soil mesocosms\",\"authors\":\"Irina Yankelzon, Georg Willibald, Michael Dannenmann, Francois Malique, Ulrike Ostler, Clemens Scheer, Klaus Butterbach-Bahl\",\"doi\":\"10.1007/s00374-024-01809-w\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>This study presents a novel plant-soil mesocosm system designed for cultivating plants over periods ranging from days to weeks while continuously measuring fluxes of N<sub>2</sub>, N<sub>2</sub>O and CO<sub>2</sub>. For proof of concept, we conducted a 33-day incubation experiment using six soil mesocosms, with three containing germinated wheat plants and three left plant-free. To validate the magnitude of N<sub>2</sub> and N<sub>2</sub>O fluxes, we used <sup>15</sup>N-enriched fertilizer and a <sup>15</sup>N mass balance approach. The system inherent leakage rate was about 55 µg N m<sup>− 2</sup> h<sup>− 1</sup> for N<sub>2</sub>, while N<sub>2</sub>O leakage rates were below the detection limit (< 1 µg N m<sup>− 2</sup> h<sup>− 1</sup>). In our experiment, we found higher cumulative gaseous N<sub>2</sub> + N<sub>2</sub>O losses in sown soil (0.34 ± 0.02 g N m<sup>− 2</sup>) as compared to bare soil (0.23 ± 0.01 g N m<sup>− 2</sup>). N<sub>2</sub> fluxes accounted for approximately 94–96% of total gaseous N losses in both planted and unplanted mesocosms. 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引用次数: 0
摘要
本研究介绍了一种新型植物-土壤介观模型系统,该系统设计用于在数天到数周的时间内培育植物,同时连续测量 N2、N2O 和 CO2 的通量。为了验证这一概念,我们使用六个土壤介观模型进行了为期 33 天的培养实验,其中三个介观模型中含有发芽的小麦植株,另外三个介观模型中没有植株。为了验证 N2 和 N2O 通量的大小,我们使用了富含 15N 的肥料和 15N 质量平衡法。系统固有的 N2 泄漏率约为 55 µg N m- 2 h- 1,而 N2O 泄漏率低于检测限(< 1 µg N m- 2 h- 1)。在我们的实验中,我们发现播种土壤(0.34 ± 0.02 g N m- 2)与裸露土壤(0.23 ± 0.01 g N m- 2)相比,气态 N2 + N2O 的累积损失更高。在已种植和未种植的中置池中,N2 通量约占气态氮损失总量的 94-96%。根据 15N 质量平衡法确定的氮损失量,播种土壤为 1.7 ± 0.5 g N m- 2,裸露土壤为 1.7 ± 0.6 g N m- 2,这表明两种评估方法不一致。播种介箱的土壤呼吸速率也更高,在 33 天的培养期内,播种土壤和裸土的土壤和地上生物量二氧化碳呼吸累积量分别达到 4.8 ± 0.1 和 4.0 ± 0.1 g C m- 2。总之,这项研究测量了小麦生长对土壤反硝化作用的影响,突出了这种先进培养系统对此类研究的敏感性和实用性。
A new incubation system to simultaneously measure n2 as well as n2o and co2 fluxes from plant-soil mesocosms
This study presents a novel plant-soil mesocosm system designed for cultivating plants over periods ranging from days to weeks while continuously measuring fluxes of N2, N2O and CO2. For proof of concept, we conducted a 33-day incubation experiment using six soil mesocosms, with three containing germinated wheat plants and three left plant-free. To validate the magnitude of N2 and N2O fluxes, we used 15N-enriched fertilizer and a 15N mass balance approach. The system inherent leakage rate was about 55 µg N m− 2 h− 1 for N2, while N2O leakage rates were below the detection limit (< 1 µg N m− 2 h− 1). In our experiment, we found higher cumulative gaseous N2 + N2O losses in sown soil (0.34 ± 0.02 g N m− 2) as compared to bare soil (0.23 ± 0.01 g N m− 2). N2 fluxes accounted for approximately 94–96% of total gaseous N losses in both planted and unplanted mesocosms. N losses, as determined by the 15N mass balance approach, were found to be 1.7 ± 0.5 g N m− 2 for the sown soil and 1.7 ± 0.6 g N m− 2 for the bare soil, indicating an inconsistency between the two assessment methods. Soil respiration rates were also higher in sown mesocosms, with cumulative soil and aboveground biomass CO2 respiration reaching 4.8 ± 0.1 and 4.0 ± 0.1 g C m− 2 over the 33-day incubation period, in sown and bare soil, respectively. Overall, this study measured the effect of wheat growth on soil denitrification, highlighting the sensitivity and utility of this advanced incubation system for such studies.
期刊介绍:
Biology and Fertility of Soils publishes in English original papers, reviews and short communications on all fundamental and applied aspects of biology – microflora and microfauna - and fertility of soils. It offers a forum for research aimed at broadening the understanding of biological functions, processes and interactions in soils, particularly concerning the increasing demands of agriculture, deforestation and industrialization. The journal includes articles on techniques and methods that evaluate processes, biogeochemical interactions and ecological stresses, and sometimes presents special issues on relevant topics.