东北黑土区土地利用方式对土壤酶活性及其化学计量比的影响

Effects of different land use types on soil enzyme activities and their stoichiometric ratios in the black soil region of Northeast China

  • 摘要: 土壤酶活性是表征土壤生态系统养分循环过程的关键生物化学指标。解析东北黑土区土壤酶活性、化学计量比和微生物养分限制对土地利用方式改变的响应特征, 可为区域土壤管理模式优化和土壤养分循环效率提高提供理论依据。本研究选取东北黑土区典型农田和林地, 采用系统网格取样法采集78个土壤样品, 分析不同土地利用方式下土壤理化性质、β-1,4-葡萄糖苷酶(BG)、β-N-乙酰氨基葡萄糖苷酶(NAG)、亮氨酸氨基肽酶(LAP)和酸性磷酸酶(AP)活性以及酶的化学计量比特征, 并采用冗余分析探究土壤酶活性和微生物养分限制及其与土壤理化性质和气候因子的关联。结果显示, 林地土壤BG、NAG、LAP和AP活性均显著高于农田, 分别高74.35% (P<0.05)、108.70% (P<0.01)、80.12% (P<0.05)和31.87% (P<0.05)。冗余分析发现, 土壤pH对区域土壤酶活性变异的解释度最高(R2=0.74), 其次为年平均降水量(R2=0.31)和铵态氮含量(R2=0.30)。土壤碳氮磷相关酶化学计量比为1∶1.34∶1.58, 农田和林地土壤均表现出磷限制, 农田土壤的微生物磷限制更为突出, 可能是因为农田长期不合理耕作施肥, 碳氮相对富集, 同时微生物群落结构发生改变降低了磷的有效性, 并抑制了微生物代谢及生态功能。pH、年平均降水量和铵态氮含量是影响土壤酶活性的主要环境因子。建议未来采取基于生态原理的土壤管理策略, 如合理施用磷肥、优化水分管理并减少人为扰动, 以提高土壤养分循环效率, 促进区域生态系统的可持续发展。

     

    Abstract: Soil enzyme activity is a fundamental biochemical indicator that reflects microbial metabolic functioning and the intensity of nutrient cycling processes within soil ecosystems. Understanding how soil enzyme activity, enzymatic stoichiometry, and microbial nutrient limitation respond to land-use change is essential for developing effective soil management strategies, particularly in the black soil region of Northeast China, where maintaining soil fertility and ecological stability is of critical importance. In this study, a total of 78 soil samples were collected from representative farmland and forest sites using a systematic grid sampling design to ensure comprehensive spatial coverage. The activities of β-1,4-glucosidase (BG), β-N-acetylglucosaminidase (NAG), leucine aminopeptidase (LAP), and acid phosphatase (AP) were quantified, and their stoichiometric characteristics were analyzed to assess microbial nutrient-acquisition strategies. Redundancy analysis was further conducted to explore the interactive relationships among enzyme activities, microbial nutrient limitation, soil physicochemical properties, and climatic variables. The results showed that forest soils exhibited significantly higher activities of BG, NAG, LAP, and AP compared with farmland soils. Specifically, the activities of BG, NAG, LAP, and AP increased by 74.35% (P<0.05), 108.70% (P<0.01), 80.12% (P<0.05), and 31.87% (P<0.05), respectively, indicating that forest ecosystems generally support more active microbial metabolism and stronger nutrient cycling potentials. Redundancy analysis demonstrated that soil pH was the most important factor explaining the spatial variation in enzyme activities, with an explanatory power of R2=0.74. Mean annual precipitation and ammonium-nitrogen content were also influential, accounting for 31% (R2=0.31) and 30% (R2=0.30) of the total variation, respectively. The enzymatic stoichiometric ratio associated with microbial acquisition of carbon, nitrogen, and phosphorus was 1∶1.34∶1.58, indicating disproportionate microbial investment toward nitrogen- and especially phosphorus-acquiring enzymes. Both farmland and forest soils exhibited clear microbial phosphorus limitation, while the limitation was more pronounced in farmland soils. This stronger phosphorus limitation in farmland likely results from long-term tillage intensity and unbalanced fertilization practices, which cause relative enrichment of carbon and nitrogen, alter microbial community structure, reduce soil phosphorus availability, and constrain microbial functional potential. Soil pH, mean annual precipitation, and ammonium-nitrogen content were identified as the key environmental drivers regulating soil enzyme activity at the regional scale. Overall, the findings suggest that ecologically informed soil management strategies, including rational phosphorus fertilization, optimized water management, and reduced soil disturbance, are essential for alleviating microbial phosphorus limitation, enhancing soil nutrient cycling efficiency, and promoting long-term ecological sustainability in the black soil region of Northeast China.

     

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