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DenNit – Experimental analysis and modelling of soil N2O efflux in response on changes of soil water content, soil temperature, soil pH, nutrient availability and the time after rain event

机译:DenNit –响应土壤水分,土壤温度,土壤pH,养分有效性和雨后时间的变化,对土壤N2 O流出进行实验分析和建模

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摘要

To quantify the effects of soil temperature (T soil), and relative soil water content (RSWC) on soil N2O emission we measured N2O soil efflux with a closed dynamic chamber in situ in the field and from soil cores in a controlled climate chamber experiment. Additionally we analysed the effect of soil acidity, ammonium, and nitrate concentration in the field. The analysis was performed on three meadows, two bare soils and in one forest. We identified soil water content, soil temperature, soil nitrogen content, and pH as the main parameters influencing soil N2O emission. The response of N2O emission to soil temperature and relative soil water content was analysed for the field and climate chamber measurements. A non-linear regression model (DenNit) was developed for the field data to describe soil N2O efflux as a function of soil temperature, soil moisture, pH value, and ammonium and nitrate concentration. The model could explain 81% of the variability in soil N2O emission of all individual field measurements, except for data with short-term soil water changes, namely during and up to 2 h after rain stopped. We validated the model with an independent dataset. For this additional meadow site 73% of the flux variation could be explained with the model.
机译:为了定量分析土壤温度(T土)和土壤相对含水量(RSWC)对土壤N2 O排放的影响,我们在一个封闭的动态室内就地测量了N2 土的外排量。在田间和土壤核心中进行受控气候室实验。此外,我们分析了田间土壤酸度,铵盐和硝酸盐浓度的影响。分析在三个草甸,两个裸露的土壤和一个森林中进行。我们确定了土壤水分,土壤温度,土壤氮含量和pH值是影响土壤N2 O排放的主要参数。分析了N2O排放对土壤温度和土壤相对含水量的响应,以进行田间和气候室测量。针对田间数据,建立了非线性回归模型(DenNit),以描述土壤N2O流量与土壤温度,土壤湿度,pH值以及铵和硝酸盐浓度的关系。该模型可以解释所有田间测量的土壤N2O排放量的81%变异性,但短期土壤水分变化的数据除外,即降雨停止期间和降雨之后最多2小时。我们使用独立的数据集验证了该模型。对于这个额外的草地场,可以用模型解释73%的通量变化。

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