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    刘思琪, 满秀玲, 张頔, 徐志鹏. 寒温带4种乔木树种不同径级根系分解及碳氮释放动态[J]. 北京林业大学学报, 2023, 45(7): 36-46. DOI: 10.12171/j.1000-1522.20210490
    引用本文: 刘思琪, 满秀玲, 张頔, 徐志鹏. 寒温带4种乔木树种不同径级根系分解及碳氮释放动态[J]. 北京林业大学学报, 2023, 45(7): 36-46. DOI: 10.12171/j.1000-1522.20210490
    Liu Siqi, Man Xiuling, Zhang Di, Xu Zhipeng. Dynamics of root decomposition and carbon and nitrogen release of four tree species with different diameter classes in the cold temperate zone[J]. Journal of Beijing Forestry University, 2023, 45(7): 36-46. DOI: 10.12171/j.1000-1522.20210490
    Citation: Liu Siqi, Man Xiuling, Zhang Di, Xu Zhipeng. Dynamics of root decomposition and carbon and nitrogen release of four tree species with different diameter classes in the cold temperate zone[J]. Journal of Beijing Forestry University, 2023, 45(7): 36-46. DOI: 10.12171/j.1000-1522.20210490

    寒温带4种乔木树种不同径级根系分解及碳氮释放动态

    Dynamics of root decomposition and carbon and nitrogen release of four tree species with different diameter classes in the cold temperate zone

    • 摘要:
        目的  探讨我国寒温带地区不同树种不同径级根系分解及碳、氮养分释放特征,为了解我国寒温带地区乔木树种根系分解和碳、氮养分循环提供科学参考。
        方法  在2020年8月—2021年8月采用网袋分解法,连续1年对我国大兴安岭地区主要乔木树种白桦、山杨、兴安落叶松和樟子松的(细根(≤ 2 mm)、中根(2 ~ 5 mm)和粗根(5 ~ 10 mm))的分解速率及碳、氮元素动态进行研究。
        结果  (1)分解1年后,白桦、山杨、兴安落叶松和樟子松各径级根系年分解率分别波动在(29.75% ~ 39.92%)、(33.90% ~ 39.45%)、(22.08% ~ 28.80%)和(22.62% ~ 33.75%)之间,且不同径级间根系分解率表现为细根 > 中根 > 粗根,白桦和山杨高于兴安落叶松和樟子松,且分解初期(0 ~ 61 d)分解速率较高,243 ~ 365 d分解速率较低。(2)利用Olson指数衰减模型计算各树种根系年分解系数k发现:同一树种根系年分解系数均随直径增大而减小,白桦细根分解系数最高,为0.508 5。同一径级不同树种间,白桦和山杨根系年分解系数显著高于兴安落叶松和樟子松,且樟子松中根和粗根年分解系数仅为山杨的50%左右。(3)不同分解时期,4个树种各径级根系碳和氮表现出不同程度的释放或富集,碳和氮释放率均在分解初期(0 ~ 61 d)表现为最大,碳释放率在分解243 ~ 273 d时较小,分解304 ~ 365 d时氮富集较多。分解1年时间,4个树种各径级根系均表现为碳和氮的释放,释放率分别在(18.68% ~ 34.21%)和(14.90% ~ 28.92%)之间,且白桦和山杨碳和氮的释放率高于兴安落叶松和樟子松,细根碳释放率最大,而中根和粗根氮释放率相对较高。
        结论  不同树种、不同径级根系在不同分解时期分解速率及碳、氮养分释放率存在较大差异,白桦和山杨分解速率及碳、氮释放率均高于兴安落叶松和樟子松。

       

      Abstract:
        Objective  The root decomposition and carbon and nitrogen nutrient release characteristics of different tree species in cold temperate zone were discussed in order to provide scientific reference for understanding the root decomposition and carbon and nitrogen nutrient cycling of tree species in cold temperate zone.
        Method  Mesh bag decomposition method was adopted from August 2020 to August 2021. The decomposition rates and the dynamics of carbon and nitrogen elements of fine roots (≤ 2 mm), middle roots (2−5 mm) and coarse roots (5−10 mm) of Betula platyphylla, Populus davidiana, Larix gmelinii and Pinus sylvestris var. mongolica were studied for one consecutive year in the Daxing’an Mountains region of northeastern China.
        Result  (1) After 365 d of decomposition, the annual root decomposition rates of Betula platyphylla, Populus davidiana, Larix gmelinii and Pinus sylvestris var. mongolica varied in 29.75%−39.92%, 33.90%−39.45%, 22.08%−28.80% and 22.62%−33.75%, respectively. The root decomposition rate of different diameter classes was fine root > medium root > coarse root, Betula platyphylla and Populus davidiana were higher than those of Larix gmelinii and Pinus sylvestris var. mongolica. The decomposition rates were higher at the initial stage of decomposition (0−61 d) and lower at 243−365 d. (2) Olson exponential decay model was used to calculate the annual root decomposition coefficient (k) of each tree species. It was found that: the decomposition coefficient of fine root of Betula platyphylla was the highest, which was 0.508 5. The decomposition coefficient of fine root of Betula platyphylla and Populus davidiana was significantly higher than that of Larix gmelinii and Pinus sylvestris var. mongolica in the same diameter class, and the decomposition coefficient of middle root and coarse root of Pinus sylvestris var. mongolica was only about 50% of that of Populus davidiana. (3) At different decomposition stages, root carbon and nitrogen of all diameter sizes of the four tree species showed different degrees of release or enrichment. The release rate of carbon and nitrogen was the highest at the initial stage of decomposition (0−61 d), the release rate of carbon was lower at 243−273 d decomposition stage, and the enrichment of nitrogen was higher at 304−365 d decomposition stage. After one year of decomposition, the release rates of carbon and nitrogen were in the range of 18.68%−34.21% and 14.90%−28.92%, respectively. The total carbon and nitrogen release rates of Betula platyphylla and Populus davidiana were higher than those of Larix gmelinii and Pinus sylvestris var. mongolica. The release rate of carbon from fine roots was the highest, while the release rate of nitrogen from medium and coarse roots was relatively low.
        Conclusion  The decomposition rate and nutrient release rate of carbon and nitrogen of roots of different tree species and diameters differ greatly in different stages. The decomposition rates and carbon and nitrogen nutrient release rates of Betula platyphylla and Populus davidiana are higher than those of Larix gmelinii and Pinus sylvestris var. mongolica.

       

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