Li Huixin, Hu Feng, Shen Qirong, Chen Xiaoyun, Cang Long, Wang Xia
College of Resources and Environmental Sciences, Institute of Agricultural Resources and Eco-environment, Nanjing Agricultural University, Nanjing 210095.
Ying Yong Sheng Tai Xue Bao. 2002 Dec;13(12):1637-41.
This study was carried out in the Experimental Station of Nanjing Agricultural University, which is in a subtropical monsoon region characterized by a warm-wet spring and a hot-dry summer. The annual average temperature, precipitation and evaporation are 15.6 degrees C, 1010 mm and 1560 mm, respectively. In 1999, the experimental plots (2.8 m x 1.0 m x 0.6 m) were established by concrete frame. Soil in the plots was orthic aquisols collected from Rugao County, Jiangsu Province. Crop rotation was upland rice and winter wheat. At the beginning of the first crop (rice) season, earthworms (Pheretima sp.) were inoculated at a density of 10.m-2 and 20.m-2, respectively, in the plots with an application of corn residues at the rate of 1500 g.m-2(750 g.m-2 in the following seasons). The responses of soil carbon and nitrogen and crop yield to earthworm activity were investigated from 1999 to 2001. The results showed that earthworms had no significant influences on total soil carbon and nitrogen content, which implied that there was no depletion of soil carbon and nitrogen pools in the presence of earthworms. The maintenance of soil carbon might be explained by low assimilation efficiency of organic matter by earthworms, and by the compensation of carbon returning from plant production enhancement. Soil mineral nitrogen, soil microbial biomass carbon and microbial biomass nitrogen were increased, and nitrogen mineralization was strengthened by earthworm activities, which was more obvious at jointing/booting and heading stages. In comparison with no-worm treatments, the yield of rice wheat increased by 9.3% and 5.1%, respectively, in the treatments inoculated with earthworms. It was concluded that earthworm was very important in promoting nitrogen recycling of crop residues and plant productivity, and in keeping the balance of soil carbon pool as well.
本研究在南京农业大学实验站开展,该实验站位于亚热带季风区,其特点是春季温暖湿润,夏季炎热干燥。年平均气温、降水量和蒸发量分别为15.6摄氏度、1010毫米和1560毫米。1999年,用混凝土框架构建了实验小区(2.8米×1.0米×0.6米)。小区土壤为取自江苏省如皋县的雏形富铁土。作物轮作为旱稻和冬小麦。在第一季作物(水稻)季开始时,分别以每平方米10条和20条的密度在小区接种蚯蚓,并以每平方米1500克的用量施用玉米残体(在随后的季节为每平方米750克)。研究了1999年至2001年蚯蚓活动对土壤碳氮和作物产量的影响。结果表明,蚯蚓对土壤总碳氮含量没有显著影响,这意味着在有蚯蚓存在的情况下,土壤碳氮库没有消耗。土壤碳的维持可能是由于蚯蚓对有机质的同化效率低,以及植物生产增强带来的碳返还补偿。蚯蚓活动增加了土壤矿质氮、土壤微生物生物量碳和微生物生物量氮,并增强了氮矿化作用,在拔节/孕穗期和抽穗期更为明显。与不接种蚯蚓的处理相比,接种蚯蚓的处理中水稻和小麦产量分别提高了9.3%和5.1%。得出的结论是,蚯蚓在促进作物残体的氮循环和植物生产力以及保持土壤碳库平衡方面非常重要。