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[积雪深度变化对水曲柳和兴安落叶松凋落物分解的影响]

[Influence of snow depth changes on leaf litter decomposition of Fraxinus mandshurica and Larix gmelinii].

作者信息

Dou Jia, Wang Chuan Kuan, Wu Qi Qian

机构信息

Center for Ecological Research, Northeast Forestry University, Harbin 150040, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2019 Jan 20;30(1):77-84. doi: 10.13287/j.1001-9332.201901.038.

Abstract

Changes in snowpack induced by climate change can profoundly affect forest litter decomposition. A snow depth manipulation experiment with three treatments (i.e.,control,snow addition, and snow removal) was conducted to assess the effects of snow depth changes on leaf litter decomposition of two temperate tree species [Manchurian ash (Fraxinus mandshurica) and Dahurian larch (Larix gmelinii)]. The annual loss of the litter mass after one year decomposition varied between 51.3% and 57.4% for the ash and between 21.7% and 31.4% for the larch. The decomposition constants (k) ranged from 0.048 to 0.057 and from 0.022 to 0.030 for these two species respectively.The greatest k value occurred under the snow addition treatment, while the least occurred under the snow removal treatment.Snow addition treatment shortened the 50% and 95% decomposition time by 1.1 months and 4.2 months for the ash, respectively, and by 3.7 months and 15.5 months for the larch, respectively. The snow removal treatment lengthened those decomposition time by 1.8 months and 6.4 months for the ash,and by 5.0 months and 21.1 months for the larch, respectively. Litter decomposition rate was significantly correlated with tree species, snow depth, decomposition time, and soil temperature, but its major influencing factors varied with decomposition stage. Soil temperature and the initial litter quality were the major factors affecting decomposition rates during the snow covered and following snow free periods, respectively. Our findings highlight that changes in snow depth exert significantly instantaneous and prolonged effects on forest litter decomposition.

摘要

气候变化引起的积雪变化会深刻影响森林凋落物分解。开展了一项积雪深度控制实验,设置了三种处理方式(即对照、增加积雪和去除积雪),以评估积雪深度变化对两种温带树种(水曲柳和落叶松)落叶分解的影响。经过一年的分解,水曲柳凋落物质量的年损失率在51.3%至57.4%之间,落叶松在21.7%至31.4%之间。这两个树种的分解常数(k)分别在0.048至0.057和0.022至0.030之间。最大的k值出现在增加积雪处理下,最小的出现在去除积雪处理下。增加积雪处理使水曲柳的50%和95%分解时间分别缩短了1.1个月和4.2个月,使落叶松分别缩短了3.7个月和15.5个月。去除积雪处理使水曲柳的这些分解时间分别延长了1.8个月和6.4个月,使落叶松分别延长了5.0个月和21.1个月。凋落物分解速率与树种、积雪深度、分解时间和土壤温度显著相关,但其主要影响因素随分解阶段而变化。土壤温度和初始凋落物质量分别是积雪覆盖期和融雪期后影响分解速率的主要因素。我们的研究结果突出表明,积雪深度变化对森林凋落物分解具有显著的即时和长期影响。

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