To understand maize- and N-induced diel variations in CO 2 emission, we examined hourly CO 2 emissions during the three typical growth stages of maize in sandy loam soil. There was a distinct diel pattern in soil CO 2 emissions, with the peak occurring between 14:00 and 18:00 and the trough occurring between 0:00 and 4:00. Maize presence delayed the time of the peak. The absolute amount and diel fluctuation of CO 2 emissions tended to diminish with time in the bare soil fertilized with 150 kg N ha −1 (BS). In contrast, N-fertilized maize (N150) significantly enhanced the total amount of CO 2 emissions and the peak-trough differences in CO 2 emissions, which reached a maximum at the pollination stage and then decreased. Control soil (CK) containing maize but no N fertilizer had highest overall CO 2 emissions but reduced diel fluctuation because rhizosphere respiration was elevated in the nighttime. Soil temperature accounted for 61–71% of diel variation in the BS treatment but for only 44–59% and 38–58% in the N150 and CK treatments, respectively. Photosynthesis rates affected diel variation at the seedling and pollination stages. Both temperature and photosynthesis rates together explained up to 67–84% of diel variation at the seedling and pollination stages in the N150 treatment, but only 61% at the seedling stage in the CK treatment due to more CO 2 released in the nighttime. The increased nighttime CO 2 release, in turn, decreased the effect of temperature and even reduced the influence of photosynthesis rate on diel variations in CO 2 release. Based on the present results, the best time for obtaining a representative daily CO 2 measurement was found to be approximately 8:00 at the seedling stage and 9:00–11:00 at the other growth stages. The current findings indicate that N addition reduces soil CO 2 emissions and its diel fluctuation.
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