利用计量学和酶计量学揭示长期施肥对土壤微生物养分限制状况的影响

Revealing the effect of long–term fertilizer application on microbial nutrient limitation in Mollisols through soil stoichiometry and enzyme metrology

  • 摘要: 本研究旨在运用生态化学计量学和酶化学计量学的方法, 探讨长期施肥对黑土区土壤微生物养分限制状况的影响。研究于中国科学院东北地理与农业生态研究所黑土水土流失监测研究站开展, 通过比较玉米大豆轮作制度中种植大豆年的常规施肥(CF)、减施化肥(1/2CF)以及有机肥替代化肥(DM)处理与不施化肥(NOF)处理, 分析了与土壤碳、氮、磷转化相关的酶活性变化特征。与NOF处理相比, 施用化肥和有机肥显著增加了鼓粒期和成熟期土壤全碳(TC)、全氮(TN)和全磷(TP)含量, 鼓粒期增幅为14.4%~20.9%, 成熟期增幅为28.3%~34.8%, 其中有机肥施用对土壤养分含量的提升作用最为显著。在鼓粒期和成熟期, 与NOF处理相比, DM处理土壤pH分别显著提高了0.69和0.82个单位。与NOF相比, CF和1/2CF处理显著提高了土壤蔗糖酶(SC)活性, 而氮分解酶活性(LAP、NAG以及LAP+NAG)则呈下降趋势。DM处理普遍提高了土壤酶活性, 这可能归因于有机肥提供的丰富有机碳源和营养物质。此外, 在长期施肥处理下, 不同时期的BG和SC活性与土壤TC、TN以及TP的变化趋势相一致, 呈显著正相关性。土壤微生物养分限制对不同施肥处理的响应表明, 黑土微生物养分获取处于不平衡状态。与NOF相比, 在鼓粒期和成熟期, 化肥施用分别受碳和磷的共同限制以及磷的限制, 而有机肥施用在两个时期均仅受磷的限制。

     

    Abstract: This study aims to investigate the effect of long–term fertilizer application on microbial nutrient limitation in Mollisols through ecological stoichiometry and enzyme metrology. The study was conducted at the Monitoring and Research Station of Black Soil Erosion, affiliated with the Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences. We compared the effects of normal chemical fertilizer application (CF), reduced chemical fertilizer application (1/2CF), substitution of chemical fertilizer with organic manure (DM) and no fertilization (NOF) in a rotational corn–soybean system. Our analysis focused on the characteristics of enzyme activity changes associated with soil carbon, nitrogen, and phosphorus transformation. Compared to no fertilization (NOF), the application of chemical and organic fertilizers substantially increased the total carbon (TC), total nitrogen (TN), and total phosphorus (TP) content in Mollisols during both the seed filling and mature stages. Specifically, TC, TN and TP levels rose by 14.4%–20.9% during the seed filling stage and 28.3% to 34.8% during the mature stage. Organic manure application had the most substantial effect on enhancing soil nutrient content levels. Furthermore, soil pH in DM treatment increased significantly, rising by 0.69 units at the seed filling stage and 0.82 units at the mature stages, respectively compared to NOF. Compared to NOF, the CF and 1/2CF treatments significantly increased soil sucrase (SC) activity, whereas nitrogen-decomposition enzyme activities (LAP, NAG, and LAP+NAG) exhibited a decreasing trend. The DM treatment generally enhanced soil enzyme activities, which can be attributed to the abundant organic carbon sources and nutrients provided by organic manure. Additionally, the activities of β-glucosidase (BG) and SC at different stages were consistent with the trends of soil TC, TN, and TP changes, and showed significant positive correlations. The response of soil microbial nutrient limitation to different fertilizer application treatments indicated that Mollisols microbial nutrient acquisition is in an imbalanced state. Compared to NOF, chemical fertilizer application was limited by C and P, while organic manure application was only P limited at seed filling and mature stages.

     

/

返回文章
返回