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长期有机无机配施对喀斯特玉米根际与非根际土壤碳氮养分及胞外酶活性的影响

Effects of long-term combined organic and inorganic fertilization on carbon and nitrogen nutrients and extracellular enzyme activities in rhizosphere and bulk soils of maize in karst cropland

  • 摘要: 依托中国科学院环江喀斯特农业生态试验站长期定位试验,设置不施肥(CK)、单施化肥(NPK)及4种有机无机配施处理(秸秆还田STNPK、牛粪配施MNPK、滤泥配施SLNPK、甘蔗灰配施BANPK),研究不同施肥措施下玉米根际与非根际土壤碳氮养分及胞外酶活性特征。结果表明,有机无机配施整体显著提升土壤有机碳(SOC)和全氮(TN)水平。与CK相比,BANPK处理使根际SOC提高19.4%,MNPK处理使根际TN提高11.3%,而NPK处理显著降低根际SOC(11.4%)(P < 0.05)。在胞外酶方面,根际N-乙酰葡萄糖苷酶(NAG)活性显著高于非根际,而β-葡萄糖苷酶(BG)和亮氨酸氨基肽酶(LAP)的根际差异不显著(P>0.05)。双因素方差分析表明,施肥处理仅对BG活性产生显著影响,土壤位置仅对NAG活性具有显著作用。相关及多元统计分析显示,β-木糖苷酶(BX)、MBC/MBN及NAG对土壤综合变异贡献较高,可较好表征不同施肥处理下土壤养分与微生物功能变化。非根际土壤中胞外酶活性与养分指标整体呈正相关,而根际土壤中NAG与DOC呈负相关趋势,但未达显著水平。综上,长期有机无机配施有助于改善喀斯特农田土壤碳氮养分状况,其中牛粪配施(MNPK)与甘蔗灰配施(BANPK)表现相对较优。但不同施肥措施对胞外酶活性及微生物功能的影响具有选择性,其机制仍需结合多生育时期观测与更全面微生物指标进一步验证。

     

    Abstract: Based on a long-term field experiment at the Huanjiang observation and research station for karst ecosystems of the Chinese Academy of Sciences in Guangxi, six fertilization treatments were established, including no fertilization (CK), chemical fertilizer alone (NPK), and four combined organic and inorganic fertilization treatments: straw returning plus NPK (STNPK), cattle manure plus NPK (MNPK), filter mud plus NPK (SLNPK), and sugarcane ash plus NPK (BANPK). This study investigated the characteristics of soil carbon and nitrogen nutrients and extracellular enzyme activities in the rhizosphere and bulk soils of maize under different fertilization regimes. The results showed that combined organic and inorganic fertilization generally increased soil organic carbon (SOC) and total nitrogen (TN) contents. Compared with CK, the BANPK treatment significantly increased rhizosphere SOC by 19.4%, while the MNPK treatment significantly increased rhizosphere TN by 11.3%. In contrast, the NPK treatment significantly decreased rhizosphere SOC by 11.4% (P < 0.05). The activity of N-acetyl-β-D-glucosaminidase (NAG) was significantly higher in the rhizosphere than in the bulk soil, whereas no significant rhizosphere effects were observed for β-glucosidase (BG) or leucine aminopeptidase (LAP) activities (P > 0.05). Two-way analysis of variance showed that fertilization treatment significantly affected only BG activity, whereas soil position significantly influenced only NAG activity. Correlation and multivariate analyses further indicated that β-xylosidase (BX), the microbial biomass carbon to microbial biomass nitrogen ratio (MBC/MBN), and NAG contributed most to the overall variation in soil properties, indicating that these variables effectively characterize changes in soil nutrient status and microbial functions under different fertilization regimes. Extracellular enzyme activities in the bulk soil were generally positively correlated with nutrient indicators, whereas NAG activity showed a negative, although non-significant, correlation with dissolved organic carbon (DOC) in the rhizosphere. Overall, long-term combined organic and inorganic fertilization improved soil carbon and nitrogen nutrient status in karst croplands, with the MNPK and BANPK treatments showing relatively superior performance. However, the effects of different fertilization regimes on extracellular enzyme activities and microbial functions were selective, and the underlying mechanisms require further verification through observations across multiple crop growth stages combined with more comprehensive microbial indicators.

     

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