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应用生态学报 ›› 2026, Vol. 37 ›› Issue (1): 43-51.doi: 10.13287/j.1001-9332.202601.002

• 研究论文 • 上一篇    下一篇

降水对樟子松人工林根际土壤微生物碳氮磷养分限制特征的影响

赵帅明, 王蕊, 李诚浩, 刘金花, 孟亚馨, 苏海瑶, 徐学华*   

  1. 河北农业大学林学院, 河北保定 071000
  • 收稿日期:2025-08-24 修回日期:2025-11-04 发布日期:2026-07-18
  • 通讯作者: *E-mail: xuehuaxu2001@163.com
  • 作者简介:赵帅明, 女, 2000年生, 硕士研究生。主要从事森林土壤微生物研究。E-mail: zsm123mm@163.com
  • 基金资助:
    河北省科技计划项目(17236801D-2)和河北省林草关键技术创新与示范揭榜挂帅项目(2025JBGS0001-5)

Effects of precipitation on soil microbial carbon, nitrogen, phosphorus nutrient limitation characteristics in rhizosphere of Pinus sylvestris var. mongolica plantations

ZHAO Shuaiming, WANG Rui, LI Chenghao, LIU Jinhua, MENG Yaxin, SU Haiyao, XU Xuehua*   

  1. College of Forestry, Hebei Agricultural University, Baoding 071000, Hebei, China
  • Received:2025-08-24 Revised:2025-11-04 Published:2026-07-18

摘要: 本研究以北方防沙带东部区樟子松人工林为对象,研究不同降水量(≤350、350~450和≥450 mm)下土壤理化性质及6种与碳、氮、磷元素循环相关的酶活性,分析根际土壤微生物碳、氮、磷养分限制特征。结果表明: 与降水量≤350 mm处理相比,降水量≥450 mm处理土壤自然含水率、有机碳、全氮含量分别增加38.7%、64.3%、58.9%,而pH和全磷含量分别下降23.4%、40.3%。β-1,4-葡萄糖苷酶、β-木糖苷酶、亮氨酸氨基肽酶、碱性磷酸酶活性及土壤微生物生物量碳、氮、磷在降水量为350~450 mm时达峰值。矢量模型表明,根际土壤微生物普遍受到碳和氮的共同限制,随降水量的增加,微生物养分限制特征由强的氮限制逐渐转变为弱的碳氮限制,最后表现为强的碳限制。冗余分析显示,降水量≤350 mm和≥450 mm处理下影响酶活性及其计量特征的主要因素分别为土壤微生物生物量氮(53.5%)和土壤有机碳(72.7%)。本研究揭示了不同降水量下樟子松人工林根际土壤微生物碳、氮、磷养分限制的变化规律及其主要影响因素,为该地区樟子松人工林的养分调控提供科学依据。

关键词: 降水, 樟子松, 土壤酶活性, 酶化学计量, 微生物养分限制

Abstract: We investigated soil physicochemical properties and the activities of six enzymes related to carbon, nitrogen, and phosphorus cycling under three precipitation treatments (≤350, 350-450, and ≥450 mm) in Pinus sylvestris var. mongolica plantations in the eastern part of the Northern Sand Prevention Belt. We further analyzed soil microbial nutrient carbon, nitrogen, phosphorus limitation characteristics in rhizosphere. The results showed that compared with that under precipitation ≤350 mm, soil water content, organic carbon and total nitrogen contents under precipitation ≥450 mm increased by 38.7%, 64.3% and 58.9%, respectively, while soil pH and total phosphorus content decreased by 23.4% and 40.3%. Activities of β-1,4-glucosidase, β-xylosidase, L-leucine amino-peptidase, and alkaline phosphatase, as well as soil microbial biomass carbon, nitrogen, and phosphorus peaked under the 350-450 mm precipitation condition. The vector model indicated that rhizosphere soil microorganisms were generally co-limited by soil carbon (C) and nitrogen (N) availability. With increasing precipitation, the pattern of microbial nutrient limitation gradually shifted from strong N limitation to the weak limitation by C and N, and eventually to the strong C limitation. Redundancy analysis showed that soil microbial biomass nitrogen was the primary factor influencing enzyme activities and stoichiometric ratios at ≤350 mm precipitation (53.5%), while soil organic carbon became the dominant factor at ≥450 mm precipitation (72.7%). Our results highlighted the variations and driving factors of microbial carbon, nitrogen, phosphorus nutrient limitations in the rhizosphere of P. sylvestris plantations across different precipitations, providing a scientific basis for nutrient regulation in P. sylvestris plantations.

Key words: precipitation, Pinus sylvestris var. mongolica, soil enzyme activity, enzymatic stoichiometry, microbial nutrient limitation