造林后土壤有机碳储量随林分年龄和土壤深度的变化而变化

IF 1.7 3区 农林科学 Q2 FORESTRY Annals of Forest Research Pub Date : 2019-07-30 DOI:10.15287/AFR.2018.1294
Guolong Hou, C. O. Delang, Xixi Lu, Lei Gao
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引用次数: 20

摘要

土壤有机碳(SOC)是陆地生物圈碳库的最大组成部分。造林是减少碳(C)排放和将C固存到土壤中的有效解决方案。然而,造林对土壤有机碳储量变化的影响方式和影响程度尚不清楚。本研究通过对90篇论文中261个站点544个数据点的定量分析,探讨了造林对0-20 cm、20-40 cm和40-60 cm三个土层有机碳变化的影响。通过标准化和/或外推获得212个数据点,可靠性高。结果表明,林龄对不同土地利用类型、植物功能类型、温度和降水条件下土壤有机碳储量动态均有显著影响。在表层0 ~ 20 cm土层效果最大。以往土地利用类型对土壤有机碳积累有显著影响,但造林前10年和造林后30年的影响不显著。此外,从长期来看,草地造林似乎比农田造林吸收更多的有机碳。植物功能类型对土壤有机碳动态也有显著影响,在整个造林期内,落叶阔叶林在0 ~ 60 cm土壤深度的有机碳含量持续增加。另一方面,常绿阔叶林和常绿针叶林的有机碳积累从第30年开始。常绿阔叶林土壤有机碳积累速率较高,而落叶阔叶林与常绿针叶林在造林后较长时间内(20 ~ 20 a)无显著差异。年平均气温和降水对土壤有机碳积累在造林前20年呈负向影响,造林后20年呈正向影响。我们还发现,初始碳储量在碳固存中并不起主要作用。换句话说,低有机碳土壤在重新造林后也可以吸收大量的有机碳。
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Soil organic carbon storage varies with stand ages and soil depths following afforestation
Soil organic carbon (SOC) is the largest component of the terrestrial biosphere carbon pool. Afforestation is an effective solution to mitigate Carbon (C) emission and sequester C into soils. However, how and to which extent afforestation influences SOC stock changes are not well understood. This study conducts a quantitative review that synthesizes 544 data points from 261 sites from 90 papers, to examine the impact of afforestation on SOC changes in three soil layers (0-20 cm, 20-40 cm and 40-60 cm). 212 data points are obtained by standardization and/or extrapolationwith high reliability. The results indicate that stand age has significant effects on the SOC stock dynamics under different conditions of previous land use types, plant functional types, temperature or precipitation. The effect is greatest at the topsoil layer of 0-20 cm. Previous land use types significantly influence SOC accumulations, but these effects are not significant in the first 10 years or after 30 years of afforestation. Besides, afforestation on grassland seems to sequester more SOC than that of cropland in the long term. Plant functional types also significantly affect SOC dynamics, with deciduous hardwood reporting a continuous increase of SOC contents at soil depth of 0-60 cm during the whole afforestation period. On the other hand, the accumulation of SOC in evergreen hardwood and evergreen softwood start from the third decades. Higher SOC accumulation rates are observed under evergreen hardwood but no significant differences were found between deciduous hardwood and evergreen softwood for the longer period after afforestation (>20 years). Mean annual temperature and precipitation negatively affect SOC accumulation in the first two decades of afforestation, however, the effects become positive in the later years.We also found that initial SOC stocks did not play a major role in SOC sequestration. In other words, lower SOC soils could also sequestrate a significant amount of SOC after reforestation.
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来源期刊
CiteScore
2.20
自引率
11.10%
发文量
11
审稿时长
12 weeks
期刊介绍: Annals of Forest Research is a semestrial open access journal, which publishes research articles, research notes and critical review papers, exclusively in English, on topics dealing with forestry and environmental sciences. The journal promotes high scientific level articles, by following international editorial conventions and by applying a peer-review selection process.
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