文摘
Methane (CH4) uptake by dryland soils is an important part in the global CH4 budget and is sensitive to the management practice. This research measured the annual CH4 flux over 2 years at the rain-fed maize fields in semiarid northwestern China using the static chamber technique. Methane uptake was measured under three mulching practices with the same nitrogen (N) application: no mulching (NM), gravel mulching (GM), and plastic film mulching (FM). In addition, methane uptake was also measured under film mulching management and three different N fertilizer rates: 0 (N0), 250 (N250), and 380 (N380) kg N ha−1. The results showed that the rain-fed maize fields acted as a sink for CH4, with the annual mean uptake rate of 21.3–40.8 μg CH4-C m−2 h−1. The soil CH4 uptake was positively correlated with soil temperature, but negatively correlated with soil moisture; these two factors together explained 35.5–50.9 % of the variance in CH4 uptake. Compared to the NM treatment, the mulching treatments markedly increased the topsoil temperature, but the annual CH4 uptake was significantly reduced by 5.2–6.7 % in the GM treatment and by 26.3 % in the FM treatment, most likely because the increased soil moisture restricted CH4 oxidation and diffusion. The CH4 uptake showed an increasing tendency with the N rate, probably because N fertilization decreased soil moisture and increased soil NO3− content. These results help in understanding the effects of agricultural managements on CH4 uptake and to properly assess the role of dryland soils in the global CH4 budget.