Seasonal Variation of Emission Fluxes of CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O from Different Larch Forests in the Daxing’An Mountains of China

Using a static chamber-gas chromatography method, we investigate the characteristics of soil CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O fluxes and their relationships with environmental factors during the growing season in four typical <i>Larix gmeli...

Full description

Bibliographic Details
Main Authors: Jinbo Li, Yining Wu, Jianbo Wang, Jiawen Liang, Haipeng Dong, Qing Chen, Haixiu Zhong
Format: Article
Language:English
Published: MDPI AG 2023-07-01
Series:Forests
Subjects:
Online Access:https://www.mdpi.com/1999-4907/14/7/1470
_version_ 1797589263183773696
author Jinbo Li
Yining Wu
Jianbo Wang
Jiawen Liang
Haipeng Dong
Qing Chen
Haixiu Zhong
author_facet Jinbo Li
Yining Wu
Jianbo Wang
Jiawen Liang
Haipeng Dong
Qing Chen
Haixiu Zhong
author_sort Jinbo Li
collection DOAJ
description Using a static chamber-gas chromatography method, we investigate the characteristics of soil CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O fluxes and their relationships with environmental factors during the growing season in four typical <i>Larix gmelinii</i> forests (moss–<i>Larix gmelinii</i> forest, <i>Ledum palustre</i>–<i>Larix gmelinii</i> forest, herbage–<i>Larix gmelinii</i> forest, and <i>Rhododendron dauricum</i>–<i>Larix gmelinii</i> forest) in the Greater Khingan Mountains. Our results show that all four forest types are sources of CO<sub>2</sub> emissions, with similar average emission fluxes (146.71 mg·m<sup>−2</sup> h<sup>−1</sup>–211.81 mg·m<sup>−2</sup> h<sup>−1</sup>) and no significant differences. The soil in the moss–<i>Larix gmelinii</i> forest emitted CH<sub>4</sub> (43.78 μg·m<sup>−2</sup> h<sup>−1</sup>), while all other forest types acted as CH<sub>4</sub> sinks (−56.02 μg·m<sup>−2</sup> h<sup>−1</sup>–−28.07 μg·m<sup>−2</sup> h<sup>−1</sup>). Although all forest types showed N<sub>2</sub>O uptake at the beginning of the growing season, the N<sub>2</sub>O fluxes (4.03 μg·m<sup>−2</sup> h<sup>−1</sup>–5.74 μg·m<sup>−2</sup> h<sup>−1</sup>) did not differ significantly among the four forest types for the entire growing season, and all acted as sources of N<sub>2</sub>O emissions. The fluxes of CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O were significantly correlated with soil temperature and soil pH for all four forest types. Multiple regression analysis shows that considering the interactive effects of soil temperature and moisture could better explain the changes in greenhouse gas emissions among different forest types. The average <i>Q</i><sub>10</sub> value (8.81) of the moss–<i>Larix gmelinii</i> forest is significantly higher than that of the other three forest types (3.16–3.54) (<i>p</i> < 0.05), indicating that the soil respiration in this forest type is more sensitive to temperature changes.
first_indexed 2024-03-11T01:04:02Z
format Article
id doaj.art-c3c2ef2030e14db2a34c87e9572059bf
institution Directory Open Access Journal
issn 1999-4907
language English
last_indexed 2024-03-11T01:04:02Z
publishDate 2023-07-01
publisher MDPI AG
record_format Article
series Forests
spelling doaj.art-c3c2ef2030e14db2a34c87e9572059bf2023-11-18T19:24:49ZengMDPI AGForests1999-49072023-07-01147147010.3390/f14071470Seasonal Variation of Emission Fluxes of CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O from Different Larch Forests in the Daxing’An Mountains of ChinaJinbo Li0Yining Wu1Jianbo Wang2Jiawen Liang3Haipeng Dong4Qing Chen5Haixiu Zhong6National and Local Joint Laboratory of Wetland and Ecological Conservation, Institute of Natural Resources and Ecology, Heilongjiang Academy of Sciences, Harbin 150040, ChinaNational and Local Joint Laboratory of Wetland and Ecological Conservation, Institute of Natural Resources and Ecology, Heilongjiang Academy of Sciences, Harbin 150040, ChinaNational and Local Joint Laboratory of Wetland and Ecological Conservation, Institute of Natural Resources and Ecology, Heilongjiang Academy of Sciences, Harbin 150040, ChinaNational and Local Joint Laboratory of Wetland and Ecological Conservation, Institute of Natural Resources and Ecology, Heilongjiang Academy of Sciences, Harbin 150040, ChinaNational and Local Joint Laboratory of Wetland and Ecological Conservation, Institute of Natural Resources and Ecology, Heilongjiang Academy of Sciences, Harbin 150040, ChinaHeilongjiang Forest and Grassland Fire Prevention Early Warning Monitoring Center, Harbin 150090, ChinaNational and Local Joint Laboratory of Wetland and Ecological Conservation, Institute of Natural Resources and Ecology, Heilongjiang Academy of Sciences, Harbin 150040, ChinaUsing a static chamber-gas chromatography method, we investigate the characteristics of soil CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O fluxes and their relationships with environmental factors during the growing season in four typical <i>Larix gmelinii</i> forests (moss–<i>Larix gmelinii</i> forest, <i>Ledum palustre</i>–<i>Larix gmelinii</i> forest, herbage–<i>Larix gmelinii</i> forest, and <i>Rhododendron dauricum</i>–<i>Larix gmelinii</i> forest) in the Greater Khingan Mountains. Our results show that all four forest types are sources of CO<sub>2</sub> emissions, with similar average emission fluxes (146.71 mg·m<sup>−2</sup> h<sup>−1</sup>–211.81 mg·m<sup>−2</sup> h<sup>−1</sup>) and no significant differences. The soil in the moss–<i>Larix gmelinii</i> forest emitted CH<sub>4</sub> (43.78 μg·m<sup>−2</sup> h<sup>−1</sup>), while all other forest types acted as CH<sub>4</sub> sinks (−56.02 μg·m<sup>−2</sup> h<sup>−1</sup>–−28.07 μg·m<sup>−2</sup> h<sup>−1</sup>). Although all forest types showed N<sub>2</sub>O uptake at the beginning of the growing season, the N<sub>2</sub>O fluxes (4.03 μg·m<sup>−2</sup> h<sup>−1</sup>–5.74 μg·m<sup>−2</sup> h<sup>−1</sup>) did not differ significantly among the four forest types for the entire growing season, and all acted as sources of N<sub>2</sub>O emissions. The fluxes of CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O were significantly correlated with soil temperature and soil pH for all four forest types. Multiple regression analysis shows that considering the interactive effects of soil temperature and moisture could better explain the changes in greenhouse gas emissions among different forest types. The average <i>Q</i><sub>10</sub> value (8.81) of the moss–<i>Larix gmelinii</i> forest is significantly higher than that of the other three forest types (3.16–3.54) (<i>p</i> < 0.05), indicating that the soil respiration in this forest type is more sensitive to temperature changes.https://www.mdpi.com/1999-4907/14/7/1470greenhouse gases<i>Larix gmelinii</i>temperature sensitivityGreater Khingan Mountains
spellingShingle Jinbo Li
Yining Wu
Jianbo Wang
Jiawen Liang
Haipeng Dong
Qing Chen
Haixiu Zhong
Seasonal Variation of Emission Fluxes of CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O from Different Larch Forests in the Daxing’An Mountains of China
Forests
greenhouse gases
<i>Larix gmelinii</i>
temperature sensitivity
Greater Khingan Mountains
title Seasonal Variation of Emission Fluxes of CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O from Different Larch Forests in the Daxing’An Mountains of China
title_full Seasonal Variation of Emission Fluxes of CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O from Different Larch Forests in the Daxing’An Mountains of China
title_fullStr Seasonal Variation of Emission Fluxes of CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O from Different Larch Forests in the Daxing’An Mountains of China
title_full_unstemmed Seasonal Variation of Emission Fluxes of CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O from Different Larch Forests in the Daxing’An Mountains of China
title_short Seasonal Variation of Emission Fluxes of CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O from Different Larch Forests in the Daxing’An Mountains of China
title_sort seasonal variation of emission fluxes of co sub 2 sub ch sub 4 sub and n sub 2 sub o from different larch forests in the daxing an mountains of china
topic greenhouse gases
<i>Larix gmelinii</i>
temperature sensitivity
Greater Khingan Mountains
url https://www.mdpi.com/1999-4907/14/7/1470
work_keys_str_mv AT jinboli seasonalvariationofemissionfluxesofcosub2subchsub4subandnsub2subofromdifferentlarchforestsinthedaxinganmountainsofchina
AT yiningwu seasonalvariationofemissionfluxesofcosub2subchsub4subandnsub2subofromdifferentlarchforestsinthedaxinganmountainsofchina
AT jianbowang seasonalvariationofemissionfluxesofcosub2subchsub4subandnsub2subofromdifferentlarchforestsinthedaxinganmountainsofchina
AT jiawenliang seasonalvariationofemissionfluxesofcosub2subchsub4subandnsub2subofromdifferentlarchforestsinthedaxinganmountainsofchina
AT haipengdong seasonalvariationofemissionfluxesofcosub2subchsub4subandnsub2subofromdifferentlarchforestsinthedaxinganmountainsofchina
AT qingchen seasonalvariationofemissionfluxesofcosub2subchsub4subandnsub2subofromdifferentlarchforestsinthedaxinganmountainsofchina
AT haixiuzhong seasonalvariationofemissionfluxesofcosub2subchsub4subandnsub2subofromdifferentlarchforestsinthedaxinganmountainsofchina