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Changes in soil bacterial community and enzyme activity under five years straw returning in paddy soil

机译:水稻土壤秸秆秸秆秸秆秸秆秸秆秸秆还稻秸秆还稻的变化

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摘要

Soil biological properties are essential for sustainable agriculture development. A five-year field experiment was conducted to understand the effects of mineral fertilizers combined with straw returning on bacterial community composition and enzyme activities in paddy soil. Treatments included three fertilizer rates of unfertilized (FO), half and full of conventional mineral fertilization (F1: 138.0 kg N ha(-1) y(-1), 67.5 kg P2O5 ha(-1) y(-1) and 39 kg K2O ha(-1) y(-1) and F2: 276.0 kg N ha(-1) y(-1), 135.0 kg P2O5 ha(-1) y(-1) and 78 kg K2O ha(-1) y(-1)) and combined with (S1: 9.0 Mg ha(-1)) or without straw (SO). Organic matter content increased by 62.8% in S1F1 and 67.2% in 51F2 in the 0-10 cm soil compared to S0F0. Compared with S0F0, S1F0 treatment increased the soil available nitrogen (AN), phosphorus (AP) and potassium (AK) content by 8.8% 9.7% and 30.0%, respectively, in 0-10 cm soil. The soil phosphatase, urease and invertase activities were increased with straw returning. The treatments of S0F1 and S0F2 reduced the soil phosphatase and invertase activities. Compared with S0F0, the S1F2 treatment significantly decreased bacterial diversity, while the S1F1 alleviated the decrease of soil bacterial diversity. Bacterial of Proteobacteria, Acidobacteria and Chloroftexi were the dominated phyla, and RDA identified that soil AN and SOM were closely correlated with bacterial community composition in both 0-10 cm and 10-20 cm soil, respectively. The higher carbon:nitrogen ratio was also observed in the S1F1, which was better for bacterial diversity. Overall, the continuous application of straw with mineral fertilizer improved soil enzyme activities and altered soil bacterial community composition. This suggests that the bacterial community respond differently to the long-term straw returning combined with mineral fertilization, which may result from different effects of C and N content or C: N ratio of soil on the composition of bacterial community.
机译:土壤生物学属性对于可持续农业发展至关重要。进行了五年的田间实验,了解矿物肥料与稻草返回的稻草返回稻草土壤中的秸秆还生进行。治疗包括三种未受精(FO)的肥料率,半成一半,常规矿物施肥(F1:138.0 kg n(-1)y(-1),67.5kg p2O5 ha(-1)y(-1)和39 Kg K2O ha(-1)y(-1)和f2:276.0kg n(-1)y(-1)y(-1),135.0kg p2O5 ha(-1)y(-1)和78kg K2O ha(-1 )y(-1))并结合(S1:9.0mg HA(-1))或没有吸管(SO)。与S0F0相比,有机质含量在0-10厘米的土壤中增加了62.8%,在0-10cm的土壤中为51f2。与S0F0相比,S1F0处理将土壤可用的氮(AN),磷(AP)和钾(AK)含量分别在0-10cm的土壤中增加了8.8%9.7%和30.0%。用秸秆返回增加土壤磷酸酶,脲酶和转化酶活性。 S0F1和SOF2的处理减少了土壤磷酸酶和转化酶活性。与S0F0相比,S1F2治疗显着降低了细菌多样性,而S1F1减轻了土壤细菌多样性的降低。蛋白细胞的细菌,抗酸杆菌和氯食粒是主导的培养基,RDA鉴定出土壤A和SOM分别与0-10cm和10-20cm的土壤中的细菌群落组合物密切相关。在S1F1中也观察到较高的碳:氮比,这对细菌多样性更好。总体而言,秸秆与矿物肥料的连续应用改善了土壤酶活性,改变了土壤细菌群落组成。这表明细菌群体与长期秸秆返回结合矿物施肥,这可能因细菌群落组成的土壤中的不同效应或C:n比例而不同。

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