| On the loess plateau, summer fallow season is a hot rainy time with intensive soil microbe activities. To evaluate the response of soil respiration to soil moisture, temporature, and N fertilization during this period is helpful for a deep understanding about the temporal and spatial variability of soil respiration and its impact factors, then a field experiment was conducted in the Changwu State Key Agro-Ecological Experimental Station, Shaanxi, China. The experiment included five N application rates: unfertilized 0(N0), 45 (N45), 90 (N90), 135(N135), and 180 (N180) kg·hm-2. The results showed that at the fallow stage, soil respiration rate significantly enhanced from 1.24 to 1.91 μmol·（m2 ·s）-1and the average of soil respiration during this period ［6.20 g·（m2 ·d）-1］ was close to the growing season ［6.95 g·（m2 ·d）-1］.The bivariate model of soil respiration with soil water and soil temperature was better than the single-variable model, but not so well as the three-factor model when explaining the actual changes of soil respiration. Nitrogen fertilization alone accounted for 8% of the variation soil respiration. Unlike the single-variable model, the results could provide crucial information for further research of multiple factors on soil respiration and its simulation. |
