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Seasonal dynamics of fine root respiration in the degraded and successional primary Korean pine forests in the Lesser Khingan mountains of Northern China

机译:中国北方小兴安岭退化和演替的原始红松林细根呼吸的季节动态

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The broad-leaved and Korean pine mixed forests in the Liangshui National Natural Reserve, China, are important components of boreal forests in areas that are sensitive to global climate change. Respiration rates of excised roots were measured using an oxygen electrode (Hansatech Oxy-Lab 2, UK) to examine the variation in and identify the controlling factors of fine root respiration (Rr) during the growing period (May-October) in 2016. The relationships between Rr and biotic/abiotic factors [e.g., soil temperature, live fine root biomass (LFRB), and the soil carbon index] were subsequently analyzed. The results showed that Rr was significantly higher in the secondary broad-leaved forest (SF) than that in the primary Korean pine forest (PK) (p 0.001); whereas soil carbon sequestration showed the opposite trend (p 0.05). Rr tended to exponentially increase with soil temperature (p 0.001) in both forest types. The Q(10) value of the PK was significantly higher than that of the SF (p 0.01). Pearson correlation and regression analyses revealed that Rr was significantly linearly correlated with LFRB, total soil organic carbon, soil soluble organic carbon, and soil microbial biomass carbon (p 0.01). Stepwise regression was used to further explain that LFRB and soil microbial biomass carbon were the major contributors to changes in Rr (F = 53.97, p 0.001, R-2 = 0.75). The findings of the present study offer insights into the variability of the soil carbon sink function in the degraded and successional primary Korean pine forests.
机译:中国凉水国家自然保护区的阔叶和红松混交林是对全球气候变化敏感地区的北方森林的重要组成部分。使用氧气电极(Hansatech Oxy-Lab 2,英国)测量了被切除的根的呼吸速率,以检查2016年生长期(5月至10月)细根呼吸(Rr)的变化并确定其控制因素。随后分析了Rr与生物/非生物因素(例如,土壤温度,细根活生物量(LFRB)和土壤碳指数)之间的关系。结果表明,次生阔叶林(SF)的Rr明显高于主要红松林(PK)的Rr(p <0.001)。而土壤固碳显示出相反的趋势(p <0.05)。在两种森林类型中,Rr均随土壤温度呈指数增长(p <0.001)。 PK的Q(10)值显着高于SF(p <0.01)。 Pearson相关和回归分析显示,Rr与LFRB,土壤总有机碳,土壤可溶性有机碳和土壤微生物生物量碳呈线性相关(p <0.01)。使用逐步回归进一步解释了LFRB和土壤微生物生物量碳是Rr变化的主要因素(F = 53.97,p <0.001,R-2 = 0.75)。本研究的发现为退化和演替的红松原始森林土壤碳汇功能的变化提供了见识。

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