Number of microorganisms of soils of subtropic zones in a vegetable-fodder and vegetable-bean crop rotations compared with permanent cultivation of these cultures has been studied. The results of the analyses have sho...Number of microorganisms of soils of subtropic zones in a vegetable-fodder and vegetable-bean crop rotations compared with permanent cultivation of these cultures has been studied. The results of the analyses have shown that character of change of number of the basic physiological groups of microorganisms （a bacteria, sporeforming bacteria, actinomysetes and microscopic fungies） depends not only on soil-ecological conditions but also on the kind and biological features of cultivated cultures. In soils of subtropical zones the greatest number of organisms using organic nitrogen in food was observed on alluvial meadow-forestry soils and yellowish-gley soils. Gray-brown soils are rich in actinomycetes in comparison with alluvial meadow-forestry soils, but meadow-serozem is rich in spore-forming bacteria forms. A number of microscopic fungi of the studied soils were the least. High intensity of processes of mineralization was marked in meadow-serozem soils, the least in alluvial meadow-forestry and yellowish-gley soils. Under permanent cultures the quantity of microorganisms was less, and factor of mineralization is higher above, than in crop rotation.展开更多
Soil has been identified as a possible carbon （C） sink for sequestering atmospheric carbon dioxide （CO2）. However, soil organic carbon （SOC） dynamics in agro-ecosystems is affected by complex interactions of var...Soil has been identified as a possible carbon （C） sink for sequestering atmospheric carbon dioxide （CO2）. However, soil organic carbon （SOC） dynamics in agro-ecosystems is affected by complex interactions of various factors including climate, soil and agricultural management practices, which hinders our understanding of the underlying mechanisms. The objectives of this study were to use the Agricultural Production Systems simulator （APSIM） model to simulate the long-term SOC dynamics under different management practices at four long-term experimental sites, Zhengzhou and Xuzhou with double cropping systems and Gongzhuling and Urtimqi with single cropping systems, located in northern China. Firstly, the model was calibrated using information from the sites and literature, and its performance to predict crop growth and SOC dynamics was examined. The calibrated model was then used to assess the impacts of different management practices, including fertilizer application, irrigation, and residue retention, on C dynamics in the top 30 cm of the soil by scenario modelling. Results indicate a significant SOC sequestration potential through improved management practices of nitrogen （N） fertilizer application, stubble retention, and irrigation. Optimal N fertilization （Nopt） and 100% stubble retention （R100） increased SOC by about 11.2%, 208.29%, and 283.67% under irrigation at Gongzhuling, Zhengzhou, and Xuzhou, respectively. Soil organic carbon decreased rapidly at lJriimqi under irrigation, which was due to the enhanced decomposition by increased soil moisture. Under rainfed condition, SOC remained at a higher level. The combination of Nopt and R100 increased SOC by about 0.46% under rainfed condition at /Jr/imqi. Generally, agricultural soils with double cropping systems （Zhengzhou and Xuzhou） showed a greater potential to sequester C than those with single cropping systems （Gongzhuling and Urumqi）.展开更多
文摘Number of microorganisms of soils of subtropic zones in a vegetable-fodder and vegetable-bean crop rotations compared with permanent cultivation of these cultures has been studied. The results of the analyses have shown that character of change of number of the basic physiological groups of microorganisms （a bacteria, sporeforming bacteria, actinomysetes and microscopic fungies） depends not only on soil-ecological conditions but also on the kind and biological features of cultivated cultures. In soils of subtropical zones the greatest number of organisms using organic nitrogen in food was observed on alluvial meadow-forestry soils and yellowish-gley soils. Gray-brown soils are rich in actinomycetes in comparison with alluvial meadow-forestry soils, but meadow-serozem is rich in spore-forming bacteria forms. A number of microscopic fungi of the studied soils were the least. High intensity of processes of mineralization was marked in meadow-serozem soils, the least in alluvial meadow-forestry and yellowish-gley soils. Under permanent cultures the quantity of microorganisms was less, and factor of mineralization is higher above, than in crop rotation.
基金Supported by the National Basic Research Program(973 Program)of China(No.2010CB950604)the National Natural Science Foundation of China(No.41075108)
文摘Soil has been identified as a possible carbon （C） sink for sequestering atmospheric carbon dioxide （CO2）. However, soil organic carbon （SOC） dynamics in agro-ecosystems is affected by complex interactions of various factors including climate, soil and agricultural management practices, which hinders our understanding of the underlying mechanisms. The objectives of this study were to use the Agricultural Production Systems simulator （APSIM） model to simulate the long-term SOC dynamics under different management practices at four long-term experimental sites, Zhengzhou and Xuzhou with double cropping systems and Gongzhuling and Urtimqi with single cropping systems, located in northern China. Firstly, the model was calibrated using information from the sites and literature, and its performance to predict crop growth and SOC dynamics was examined. The calibrated model was then used to assess the impacts of different management practices, including fertilizer application, irrigation, and residue retention, on C dynamics in the top 30 cm of the soil by scenario modelling. Results indicate a significant SOC sequestration potential through improved management practices of nitrogen （N） fertilizer application, stubble retention, and irrigation. Optimal N fertilization （Nopt） and 100% stubble retention （R100） increased SOC by about 11.2%, 208.29%, and 283.67% under irrigation at Gongzhuling, Zhengzhou, and Xuzhou, respectively. Soil organic carbon decreased rapidly at lJriimqi under irrigation, which was due to the enhanced decomposition by increased soil moisture. Under rainfed condition, SOC remained at a higher level. The combination of Nopt and R100 increased SOC by about 0.46% under rainfed condition at /Jr/imqi. Generally, agricultural soils with double cropping systems （Zhengzhou and Xuzhou） showed a greater potential to sequester C than those with single cropping systems （Gongzhuling and Urumqi）.
