首页> 外文期刊>Acta Agriculturae Scandinavica. Section B, Soil and Plant Science >Conversion of forest to agricultural land affects the relative contribution of bacteria and fungi to nitrification in humid subtropical soils
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Conversion of forest to agricultural land affects the relative contribution of bacteria and fungi to nitrification in humid subtropical soils

机译:森林向农用地的转化会影响细菌和真菌对亚热带湿润土壤硝化的相对贡献

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摘要

Land-use and management practices can affect soil nitrification. However, nitrifying microorganisms responsible for specific nitrification process under different land-use soils remains unknown. Thus, we investigated the relative contribution of bacteria and fungi to specific soil nitrification in different land-use soils (coniferous forest, upland fields planted with corn and rice paddy) in humid subtropical region in China. N-15 dilution technique in combination with selective biomass inhibitors and C2H2 inhibition method were used to estimate the relative contribution of bacteria and fungi to heterotrophic nitrification and autotrophic nitrification in the different land-use soils in humid subtropical region. The results showed that autotrophic nitrification was the predominant nitrification process in the two agricultural soils (upland and paddy), while the nitrate production was mainly from heterotrophic nitrification in the acid forest soil. In the upland soils, streptomycin reduced autotrophic nitrification by 94%, whereas cycloheximide had no effect on autotrophic nitrification, indicating that autotrophic nitrification was mainly driven by bacteria. However, the opposite was true in another agricultural soil (paddy), indicating that fungi contributed to the oxidation of NH4+ to NO3-. In the acid forest soil, cycloheximide, but not streptomycin, inhibited heterotrophic nitrification, demonstrating that fungi controlled the heterotrophic nitrification. The conversion of forest to agricultural soils resulted in a shift from fungi-dominated heterotrophic nitrification to bacteria- or fungi-dominated autotrophic nitrification. Our results suggest that land-use and management practices, such as the application of N fertilizer and lime, the long-term waterflooding during rice growth, straw return after harvest, and cultivation could markedly influence the relative contribution of bacteria and fungi to specific soil nitrification processes.
机译:土地使用和管理做法会影响土壤硝化作用。然而,在不同土地利用的土壤下,负责特定硝化过程的硝化微生物仍然未知。因此,我们调查了中国亚热带湿润地区不同土地利用土壤(针叶林,种植玉米和水稻的旱地)中细菌和真菌对特定土壤硝化的相对贡献。采用N-15稀释技术结合选择性生物量抑制剂和C2H2抑制方法,估算了亚热带湿润地区不同土地利用土壤中细菌和真菌对异养硝化和自养硝化的相对贡献。结果表明,自养硝化是两种农业土壤(旱地和稻田)的主要硝化过程,而硝酸盐的产生主要来自酸性森林土壤中的异养硝化。在旱地土壤中,链霉素将自养硝化作用降低了94%,而环己酰亚胺对自养硝化作用没有影响,表明自养硝化作用主要由细菌驱动。但是,在另一种农业土壤(水稻)中情况恰恰相反,表明真菌促进了NH4 +氧化为NO3-。在酸性森林土壤中,环己酰亚胺(而非环霉素)抑制异养硝化作用,表明真菌控制了异养硝化作用。森林向农业土壤的转化导致了从以真菌为主的异养硝化向以细菌或真菌为主的自养硝化的转变。我们的结果表明,土地使用和管理实践(例如氮肥和石灰的施用,水稻生长期间的长期注水,收割后的秸秆还田和耕种)会显着影响细菌和真菌对特定土壤的相对贡献。硝化过程。

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