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减雨对三江平原蒙古栎林土壤呼吸的初期影响

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[目的]研究土壤呼吸对干旱的响应,阐明全球气候变化与土壤碳排放之间的反馈关系.[方法]本研究以三江平原蒙古栎次生林为研究对象,采用林内穿透雨减少技术模拟干旱,通过LI-8100 土壤CO2 通量测定系统对2023年5-9月土壤呼吸速率进行观测,研究土壤温度、土壤体积含水量及不同土壤呼吸组分对减雨的响应.[结果]减雨处理后土壤温度、土壤体积含水量均呈现降低的趋势,减雨处理未对土壤异养呼吸速率造成显著影响,显著降低了土壤总呼吸速率.土壤呼吸速率的季节变化与土壤温度的季节变化较为一致.土壤呼吸速率与土壤温度呈极显著指数相关关系(P<0.01),与土壤体积含水量成显著二项式线性相关关系(P<0.05).减雨导致土壤总呼吸温度敏感性下降,双因素方差分析说明,以减雨为自变量时主效应存在(P<0.05),二者无显著交互作用(P>0.05).[结论]减雨显著抑制了三江平原蒙古栎林土壤呼吸,模拟干旱初期三江平原地区蒙古栎天然次生林的土壤碳排放速率可能会降低.该研究结果可为蒙古栎林的经营及管理提供理论依据,为精准评估气候变化背景下我国东北蒙古栎林的土壤碳汇提供数据支撑.
Initial Effects of Rainfall Reduction on Soil Respiration in Quercus mongolica Forest in Sanjiang Plain
[Objective]This study investigated the response of soil respiration to drought conditions and elucidated the feedback relationship between global climate change and soil carbon emissions.[Method]The research focused on the secondary Quercus mongolica forest in the Sanjiang plain,employing an in forest rain reduction technique to simulate drought scenarios.The LI-8100 soil CO2 flux measurement system was utilized to monitor soil respiration rates from May to September 2023,examining how soil temperature,soil volumetric water content,and various components of soil respiration respond to reduced rainfall.[Result]The soil temperature and soil volumetric water content showed a decreasing trend after rain reduction treatment,and the soil heterotrophic respiration rate was not significantly affected by rain reduction treatment,but the total soil respiration rate was significantly decreased.The seasonal variation of soil respiration rate was consistent with that of soil temperature.Soil respiration rate had a significant exponential correlation with soil temperature(P<0.01),and a significant binomial linear correlation with soil volumetric water content(P<0.05).The sensitivity of soil total respiration temperature decreased due to rainfall reduction.Two-factor ANOVA analysis of variance showed that the main effect existed when rainfall reduction was taken as independent variable(P<0.05),but there was no significant interaction between them(P>0.05).[Conclusion]Short-term reductions in rainfall markedly suppressed soil respiration within the Quercus mongolica forest of the Sanjiang plain,consequently,during early simulated drought conditions,carbon emission rates from this natural secondary forest may decline significantly.The results can provide a theoretical framework for managing Quercus mongolica forests while offering data support for accurately assessing carbon sequestration potential under climate change scenarios in northeastern China.

simulated droughtQuercus mongolicasoil respirationsoil carbon emissionsoil respiration sensitivity

王剑南、董立本、池成林、韩大校、崔嵘、赵博坤、骆媛媛、张吉利

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国家林业和草原局哈尔滨林业机械研究所,黑龙江 哈尔滨 150086

中国林业科学研究院寒温带林业研究中心,黑龙江 哈尔滨 150086

黑龙江抚远森林生态系统定位观测研究站,黑龙江 抚远 156500

抚远市林业和草原局,黑龙江 抚远 156500

黑河市林业科学院,黑龙江 黑河 164300

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减雨 蒙古栎林 土壤呼吸 土壤碳排放 土壤呼吸敏感性

2024

温带林业研究
国家林业局哈尔滨林业机械研究所

温带林业研究

影响因子:0.198
ISSN:2096-4900
年,卷(期):2024.7(4)