Warming Shapes and -Type Denitrifier Communities and Stimulates NO Emission in Acidic Paddy Soil.

Warming strongly stimulates soil nitrous oxide (NO) emission, contributing to the global warming trend. Submerged paddy soils exhibit huge NO emission potential; however, the NO emission pathway and underlying mechanisms for warming are not clearly understood. We conducted an incubation experiment using N to investigate the dynamics of NO emission at controlled temperatures (5, 15, 25, and 35°C) in 125% water-filled pore space.

[Effect of short-time drought process on denitrifying bacteria abundance and N2O emission in paddy soil].

In order to investigate the impact of drying process on greenhouse gas emissions and denitrifying microorganisms in paddy soil, wetting-drying process was simulated in laboratory conditions. N2O flux, redox potential (Eh) were monitored and narG- and nosZ-containing denitrifiers abundances were determined by real-time PCR. N2O emission was significantly increased only 4 h after drying process began, and it was more than 6 times of continuous flooding (CF) at 24 h.

[Effects of different nitrogen, phosphorous, and potassium fertilization modes on carbon- and nitrogen accumulation and allocation in rice plant].

Based on a 20-year field site-specific fertilization experiment in Taoyuan Experimental Station of Agriculture Ecosystems under Chinese Ecosystem Research Network (CERN), this paper studied the effects of different fertilization modes of N, P, and K on the accumulation and allocation of C and N in rice plant. The fertilization mode N-only showed the highest C and N contents (433 g kg(-1) and 18.9 g kg(-1), respectively) in rice grain, whereas the modes balanced fertilization of chemical N, P and K (NPK) and its combination with organic mature recycling (NPKC) showed the highest storage of C and N in rice plant.

[Effect of long-term fertilization on soil plough layer carbon storage in a reddish paddy soil].

With a reddish paddy soil as test materials, soil profile nitrogen storage in long-term different fertilization system (1990-2006) have been investigated. The result indicated that recycling of organic matter significantly increased the soil profile C storage (ranged from 57.7 to 66.

[Responses of microbial biomass P to the changes of organic C and P in paddy soils under different fertilization systems].

Based on a fifteen years field experiment in double rice-cropping region of subtropical China, the responses of microbial biomass P (MB-P) to organic C and P in red paddy soils under different fertilization systems were investigated. The results indicated that a long-term input of organic carbon sources and the increasing soil organic carbon made soil microbial biomass remain at a high level (MB-C > 800 mg x kg(-1)), being a main reason of the increase of MB-P. Under long-term zero chemical P fertilization, there was a significant decrease in soil total P (P < 0.