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拉脱维亚造林地区土壤有机碳储量和整株树木生物量的变化

Changes in Organic Carbon Stock in Soil and Whole Tree Biomass in Afforested Areas in Latvia.

作者信息

Petaja Guna, Bārdule Arta, Zalmanis Juris, Lazdiņa Dagnija, Daugaviete Mudrīte, Skranda Ilona, Zvaigzne Zaiga Anna, Purviņa Dana

机构信息

Latvian State Forest Research Institute "Silava", Riga Street 111, LV-2169 Salaspils, Latvia.

Latvia University of Life Sciences and Technologies, Liela Street 2, LV-3001 Jelgava, Latvia.

出版信息

Plants (Basel). 2023 Jun 9;12(12):2264. doi: 10.3390/plants12122264.

DOI:10.3390/plants12122264
PMID:37375889
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10305317/
Abstract

This study investigates the soil organic carbon (SOC) and whole tree biomass carbon (C), soil bulk density (BD) as well as changes in these parameters in afforested areas in Latvia. The study covered 24 research sites in afforested areas-juvenile forest stands dominated by Scots pine, Norway spruce and Silver birch. The initial measurements were conducted in 2012 and repeated in 2021. The results show that afforestation mostly leads to a general decrease in soil BD and SOC stock in 0-40 cm soil layer and an increase in C stock in tree biomass across afforested areas with various tree species, soil types, and former land uses. The physical and chemical properties of the soil could explain the differences in changes in soil BD and SOC caused by afforestation, as well as the impact of past land use may have persisted. When comparing the changes in SOC stock with the increase in C stock in tree biomass due to afforestation, taking into account the decrease in soil BD and the resulting elevation of soil surface level, the afforested areas at juvenile development stage can be considered a net C sink.

摘要

本研究调查了拉脱维亚造林地区的土壤有机碳(SOC)、整树生物量碳(C)、土壤容重(BD)以及这些参数的变化。该研究涵盖了24个造林地区的研究地点——以苏格兰松、挪威云杉和银桦为主的幼龄林分。初始测量于2012年进行,并于2021年重复进行。结果表明,造林大多导致0至40厘米土层的土壤BD和SOC储量普遍下降,以及不同树种、土壤类型和以前土地利用方式的造林地区树木生物量中的C储量增加。土壤的物理和化学性质可以解释造林引起的土壤BD和SOC变化差异,以及过去土地利用的影响可能持续存在。在比较造林导致的SOC储量变化与树木生物量中C储量的增加时,考虑到土壤BD的下降以及由此导致的土壤表面水平升高,幼龄发育阶段的造林地区可被视为一个净碳汇。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/32e9/10305317/91b89610a683/plants-12-02264-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/32e9/10305317/0dae612826f3/plants-12-02264-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/32e9/10305317/3cda0577c0fa/plants-12-02264-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/32e9/10305317/c4069abf4604/plants-12-02264-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/32e9/10305317/b8bf5f030f5a/plants-12-02264-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/32e9/10305317/8599f8ac85ac/plants-12-02264-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/32e9/10305317/91b89610a683/plants-12-02264-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/32e9/10305317/0dae612826f3/plants-12-02264-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/32e9/10305317/3cda0577c0fa/plants-12-02264-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/32e9/10305317/c4069abf4604/plants-12-02264-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/32e9/10305317/b8bf5f030f5a/plants-12-02264-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/32e9/10305317/8599f8ac85ac/plants-12-02264-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/32e9/10305317/91b89610a683/plants-12-02264-g006.jpg

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本文引用的文献

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Soils with more clay and dense vegetation were rich in soil carbon along Wadi Al-Sharaea, Makkah, Saudi Arabia.在沙特阿拉伯麦加的瓦迪·沙拉亚地区,黏土含量更高且植被茂密的土壤富含土壤碳。
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Root Exudates Mediate the Processes of Soil Organic Carbon Input and Efflux.根系分泌物介导土壤有机碳的输入和流出过程。
Plants (Basel). 2023 Jan 31;12(3):630. doi: 10.3390/plants12030630.
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Afforestation influences soil organic carbon and its fractions associated with aggregates in a karst region of Southwest China.
造林对中国西南喀斯特地区土壤有机碳及其与团聚体相关的各组分的影响。
Sci Total Environ. 2022 Mar 25;814:152710. doi: 10.1016/j.scitotenv.2021.152710. Epub 2021 Dec 31.
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A systematic analysis and review of the impacts of afforestation on soil quality indicators as modified by climate zone, forest type and age.系统分析和综述了造林对土壤质量指标的影响,这些影响受气候带、森林类型和年龄的调节。
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