大气CO_2浓度升高对农田土壤线虫的影响

大气CO_2浓度升高能够对生态系统产生一系列的影响。土壤线虫在农田生态系统腐屑食物网中占有重要的地位，能够对环境变化作出较迅速的反应。本文利用江苏省无锡市稻一麦轮作FACE系统研究平台，研究了大气CO_2浓度升高对农田土壤线虫群落的影响。在麦田生态系统中共观察到土壤线虫29科40属。研究发现大气CO_2浓度升高对土壤线虫的影响存在季节性的波动，不同营养类群的土壤线虫在不同生长关键期受大气CO2浓度升高影响的程度不同。在大气CO_2浓度升高（FACE）条件下，土壤线虫总数，食细菌线虫和食真菌线虫数量显著增加。由于土壤温湿条件的季节变化，只有在适宜的条件下，大气CO_2浓度升高对土壤线虫的影响才比较显著。在稻田生态系统中共观察到土壤线虫27科40属。研究发现，大气CO_2浓度升高能使土壤线虫总数和植物寄生线虫数量增加。在O-5cm土层，FACE系统中食真菌线虫数量显著低于对照。在5一10 cm土层，FACE系统中植物寄生线虫的潜根属（Hirschmanniella）和散香属（Boleodorus）线虫数量显著高于对照，对CO2浓度升高的反应较敏感。本研究试图为在全球变化条件下进一步认识土壤动物对农田生态 系统生态过程产生的影响提供参考。

施用农用化学品及生防制剂对土壤线虫群落动态影响的研究

Dynamics of soil nematode communities amended with agrochemicals and bio control preparations were investigated in a soybean field. The results showed that the frequency of plant non parasitic nematodes were obviously higher in soil amended with bio control preparations (Doufeng 1) than with urea and herbicide, however, that of plant parasitic nematodes exhibited an inverse trend.

Effects of plateau zokors (Myospalax Fontanierii) on plant community and soil in an alpine meadow

Effects of plateau zokors (Myospalax fontanierii) on seasonal above- and belowground plant biomass, plant species diversity, and soil moisture and organic matter were examined at an alpine meadow site in Qinghai Province, People's Republic of China. Above- and belowground biomass increased significantly in areas where zokors were removed or burrow systems were abandoned for 5 years compared with areas that zokors had occupied for >10 years. Biomass of monocotyledons was reduced greatly, but biomass of nonpalatable dicotyledons increased significantly, in occupied areas. Diversity of dicotyledons, monocotyledons, and total plants in unoccupied areas was significantly greater than in occupied or abandoned areas. Vegetation cover and height in occupied areas were significantly less than in unoccupied and abandoned areas. No consistent effect by zokors on soil moisture and organic matter was observed.

Stable Carbon Isotopic Composition in Soil Organic Carbon and C3/C4 Source Variations at the Haibei Alpine Meadow

Stable carbon isotopes of organic matter originated from different soil layers (0～5 cm, 5～15 cm, 15～25 cm, 25～35 cm, 35～50 cm, 50～65 cm) were investigated in the Haibei Alpine Meadow Ecosystem Research Station of the Chinese Academy of Sciences. The preliminary results indicated that δ13C values of soil organic matter increased with increased soil depth. δ13C of soil organic carbon in 0～5 cm layer showed the lowest value, -25.09‰; while 50～65 cm soil layer possessed the lowerδ13C value, -13.87‰. Based on mass balance model of stable isotopes, it was proposed that the percentage of C4 carbon source tend to increase with increased soil depth. The preliminary study indicated that alpine meadow might have undergone a successive process from C4-dominated community to C3-dominated one. However, changing δ13C values in atmospheric CO2 overtime and different processes of soil organic carbon formation (or eluviation) might somewhat contribute to increasing δ13C values. In this case, mass balance model would underestimate C3 community and overestimate C4 community.