College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, Zhejiang, China.
College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, Zhejiang, China.
Sci Total Environ. 2021 Feb 25;757:143817. doi: 10.1016/j.scitotenv.2020.143817. Epub 2020 Nov 19.
The effect of biochar additions on N leaching and retention in tea soils and its microbial mechanism are still unclear. In this study, effects of biochar additions at rates of 0, 3% and 6% on N leaching, N retention and microbial responses in two tea soils with 20- and 60-year plantation ages were investigated under application with N-labeled urea. The results showed that cumulative mass of leached NH-N, NO-N and TN was reduced by 20.9%-91.9%, 35.1%-66.9% and 40.0%-72.8% under biochar additions, respectively. The retention of TN in soil was increased by 1.2%-5.8% under biochar amendment. Fertilizer-N in the leachate was reduced by 28.8%-62.1%, while fertilizer-N retention in the soils was enhanced by 3.2%-23.9% with biochar application. Biochar addition of 6% showed the highest mitigation of N leaching and enhancement of TN retention across the two soils. Biochar additions increased soil microbial biomass and enzyme activities and changed the bacterial community composition, indicating that biochar addition increased the microbial N requirement, stimulated soil N cycling, including nitrification and denitrification processes, and enhanced microbial N immobilization in the tea soils. Those microbial responses to biochar addition were higher in 60-year-old soil relative to 20-year-old soil, leading to a higher enhancement of N retention and mitigation of N leaching. Soil pH was the prime factor that influenced soil microbes, and it strongly correlated with microbial biomass, enzyme activity, the relative abundance of dominant phyla and α-diversity indices. Therefore, the enhancement of microbial biomass, activity and shifts of bacterial community composition related to N cycling in response to biochar additions that increased the soil pH could be an important mechanism to better understand the biochar-induced N leaching mitigation and N retention enhancement in tea soils under different plantation ages.
生物炭添加对茶园土壤中氮淋失和氮素保持及其微生物机制的影响仍不清楚。本研究采用氮标记尿素,研究了生物炭添加量为 0、3%和 6%对 20 年和 60 年种植茶园土壤氮淋失、氮素保持和微生物响应的影响。结果表明,生物炭添加分别减少了 NH4-N、NO3-N 和 TN 的累积淋失量 20.9%-91.9%、35.1%-66.9%和 40.0%-72.8%。生物炭添加可使土壤 TN 保持率增加 1.2%-5.8%。生物炭添加使淋出液中肥料氮减少 28.8%-62.1%,而土壤中肥料氮保持率增加 3.2%-23.9%。在两种土壤中,6%的生物炭添加对氮淋失的抑制和 TN 保持的增强效果最佳。生物炭添加增加了土壤微生物生物量和酶活性,并改变了细菌群落组成,表明生物炭添加增加了微生物对氮的需求,刺激了土壤氮循环,包括硝化和反硝化过程,并增强了茶园土壤中微生物对氮的固定。与 20 年种植茶园土壤相比,60 年种植茶园土壤中生物炭添加对土壤微生物的促进作用更高,从而提高了氮的保持率,减少了氮的淋失。土壤 pH 是影响土壤微生物的主要因素,它与微生物生物量、酶活性、优势门相对丰度和 α-多样性指数密切相关。因此,生物炭添加增加土壤 pH,从而增强微生物生物量、活性和与氮循环相关的细菌群落组成的变化,可能是理解不同种植年限茶园土壤中生物炭诱导氮淋失减少和氮保持增强的重要机制。