Measuring frequently during peak soil N<sub>2</sub>O emissions is more important than choosing the time of day to sample

Abstract

<p><strong>Abstract.</strong> Manual gas sampling from static soil chambers is commonly used to measure the flux of nitrous oxide (N<sub>2</sub>O) from soil. Because manual sampling is labour intensive, sampling frequencies are often insufficient to fully capture daily variability of N<sub>2</sub>O soil flux, which compromises the accuracy of estimates of daily and cumulative emissions. Knowledge of the diurnal fluctuation of N<sub>2</sub>O flux has been used to choose a flux sampling time that maximizes the accuracy of N<sub>2</sub>O flux estimates and thereby reduces the required frequency of flux measurements, but results of previous studies have been inconsistent. We analysed N<sub>2</sub>O soils emissions measured quasi-continuously over three years from a highly fertilized (> 200 kg N ha<sup>−1</sup>) maize system grown in southern Wisconsin, USA. This is the first study of N<sub>2</sub>O flux temporal variability that includes multiple difficult-to-measure peak emission events (<q>hot moments</q>) and estimates the relative contribution of hot moments to cumulative emissions. Analysis of diurnal fluctuation in N<sub>2</sub>O flux was performed using all measured data (≈ 22 000 fluxes) as well as using subsets of the data grouped by flux magnitude. The relationship between the observed hourly average flux and the mean daily flux was assessed using linear regression. Results show that diurnal variation in N<sub>2</sub>O soil flux was closely associated with normalized flux size. During low emission periods, N<sub>2</sub>O soil fluxes exhibited a diurnal pattern such that N<sub>2</sub>O flux measured at particular times of day, <q>Preferred Measuring Times</q> (PMTs), were not significantly different from the mean daily flux. During high emissions periods N<sub>2</sub>O flux did not exhibit a diurnal pattern and there was no PMT. High emissions periods included difficult-to-measure hot moments that did not exhibit a PMT and contributed up to 50 % of the cumulative emissions. We conclude that in order to accurately measure soil N<sub>2</sub>O flux in this type of system, it is necessary to sample frequently, particularly during peak flux events, and that constraining sampling to particular times of day provides little benefit.</p>