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首页> 外文期刊>Global Ecology and Conservation >Increasing soil organic carbon and nitrogen stocks along with secondary forest succession in permafrost region of the Daxing’an mountains, northeast China
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Increasing soil organic carbon and nitrogen stocks along with secondary forest succession in permafrost region of the Daxing’an mountains, northeast China

机译:中国东北地区大兴安州山脉永久冻土地区的二级森林连续,增加土壤有机碳和氮股

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摘要

Secondary forest succession plays a vital role in the dynamics of soil organic carbon and nitrogen and is recognized as an important driving force for the recovery of soil properties. In order to explore the effect of forest succession on the stocks of soil organic carbon and nitrogen in permafrost region of the Daxing’an Mountains, northeast China, the Betula platyphylla forest at the early succession stage; the Betula platyphylla - Larix gmelinii mixed forest at the middle succession stage and the pure Larix gmelinii forest at the climax forest stage were selected to compare soil organic carbon and soil nitrogen stocks along forest succession stage. The results showed that the concentration of soil organic carbon (SOC) and total soil nitrogen (SN) all increased during forest succession, particularly in 0–40?cm depth. However, the C:N ratio changed slightly. The concentration of SOC and SN and the ratio of C/N significantly decreased with increasing of soil depth along forest succession. The stocks of total soil organic carbon (TSOC) and total soil nitrogen (TSN) increased from 77.69?Mg?hasup?1/sup to 130.50?Mg?hasup?1/sup and from 7.46?Mg?hasup?1/sup to 13.90?Mg?hasup?1/sup, respectively, during forest succession, but the accumulation were mainly in later stage of succession from Betula platyphylla - Larix gmelinii forest to Larix gmelinii forest. TSOC and TSN showed obvious surface aggregation, with more than 58% of TSOC in the soil of 0–20?cm depth and more than 50% of TSN in the soil of 0–40?cm depth. TSOC and TSN decreased with increasing soil depth. To sum up, our study highlighted that secondary forest succession greatly increased the sequestration capacity of SOC and SN of forest soil in the future Daxing’an Mountains, northeast China. The result is of great significance for understanding the simultaneous effects of forest succession and climate change, and improving forest resource management measures and strategies in permafrost region.
机译:二次森林继承在土壤有机碳和氮的动态中起着至关重要的作用,并且被认为是恢复土壤性质的重要推动力。为了探讨森林继承森林冻土土壤有机碳和氮素股股市的影响,东北地区东北地区,桦树铂林早期连续阶段;桦木蛋白酶 - Larix Gmelinii混合森林在中继阶段和纯Larix Gmelinii森林的高潮森林阶段进行了选择,以比较森林连续阶段的土壤有机碳和土壤氮股。结果表明,在森林继承期间,土壤有机碳(SoC)和总土壤氮(Sn)的浓度均增加,特别是在0-40Ωcm深处。但是,C:n比例略有变化。随着森林继承的土壤深度的增加,SoC和Sn的浓度和C / N的比例显着降低。总土壤有机碳(Tsoc)和总土壤氮气(Tsn)的股增加到77.69Ω·mg?ha α1至130.50?mg?ha ?1 7.46?mg?ha α1到13.90?mg?ha ?1 ,在森林继承期间,但积累主要是在Betula platyphylla连续的后期继承阶段 - Larix Gmelinii森林到Larix Gmelinii森林。 TSOC和TSN显示出​​明显的表面聚集,在0-20℃的土壤中,超过58%的TSOC深度,50%以上的土壤中的0-40厘米深度。随着土壤深度的增加,TSOC和TSN减少。总而言之,我们的研究强调,二次森林继承大大提高了中国东北地区未来大兴安山区森林土壤的SoC和Sn的隔离能力。结果对于了解森林继承和气候变化的同时效果以及改善永久冻土地区的森林资源管理措施和战略的重要意义。

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