Carbon dioxide and methane fluxes by a forest soil under laboratory-controlled moisture and temperature conditions

被引:223
|
作者
Bowden, RD [1 ]
Newkirk, KM
Rullo, GM
机构
[1] Allegheny Coll, Dept Environm Sci, Meadville, PA 16335 USA
[2] Marine Biol Lab, Ctr Ecosyst, Woods Hole, MA 02543 USA
来源
SOIL BIOLOGY & BIOCHEMISTRY | 1998年 / 30卷 / 12期
关键词
D O I
10.1016/S0038-0717(97)00228-9
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Carbon dioxide and methane are important greenhouse gases whose exchange rates between soils and the atmosphere are controlled strongly by soil temperature and moisture. We made a laboratory investigation to quantify the relative importance of soil moisture and temperature on fluxes of CO(2) and CH(4) between forest soils and the atmosphere. Forest floor and mineral soil material were collected from a mixed hardwood forest at the Harvard Forest. Long-Term Ecological Research Site (MA) and were incubated in the laboratory under a range of moisture (air-dry to nearly saturated) and temperature conditions (5-25 degrees C). Carbon dioxide emissions increased exponentially with increasing temperature in forest floor material, with emissions reduced at the lowest and highest soil moisture contents. The forest floor Q(10) of 2.03 (from 15-25 degrees C) suggests that CO(2) emissions were controlled primarily by soil biological activity. Forest floor CO(2) emissions were predicted with a multiple polynomial regression model (r(2) = 0.88) of temperature and moisture, but the fit predicting mineral soil respiration was weaker (r(2) = 0.59). Methane uptake was controlled strongly by soil moisture, with reduced fluxes under conditions of very low or very high soil moisture contents. A multiple polynomial model accurately described CH(4) uptake by mineral soil material (r(2) = 0.81), but only weakly (r(2) = 0.45) predicted uptake by forest floor material. The mineral soil Q(10) of 1.11 for CH(4) uptake indicates that methane uptake is controlled primarily by physical processes. Our work suggests that inclusion of both moisture and temperature can improve predictions of soil CO(2) and CH(4) exchanges between soils and the atmosphere. Additionally, global change models need to consider interactions of temperature and moisture in evaluating effects of global climate change on trace gas fluxes. (C) 1998 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:1591 / 1597
页数:7
相关论文
共 50 条
  • [31] Rainfall frequency and soil water availability regulate soil methane and nitrous oxide fluxes from a native forest exposed to elevated carbon dioxide
    Martins, Catarina S. C.
    Nazaries, Loic
    Delgado-Baquerizo, Manuel
    Macdonald, Catriona A.
    Anderson, Ian C.
    Singh, Brajesh K.
    FUNCTIONAL ECOLOGY, 2021, 35 (08) : 1833 - 1847
  • [32] Responses of ecosystem carbon dioxide fluxes to soil moisture fluctuations in a moist Kenyan savanna
    Otieno, D. O.
    K'Otuto, G. O.
    Maina, J. N.
    Kuzyakov, Y.
    Onyango, J. C.
    JOURNAL OF TROPICAL ECOLOGY, 2010, 26 : 605 - 618
  • [33] Model-empirical Calculation of Methane and Carbon Dioxide Fluxes from Peatbog Soil
    A. V. Zinchenko
    V. I. Privalov
    V. M. Ivakhov
    N. N. Paramonova
    Russian Meteorology and Hydrology, 2022, 47 : 767 - 780
  • [34] Model-empirical Calculation of Methane and Carbon Dioxide Fluxes from Peatbog Soil
    Zinchenko, A. V.
    Privalov, V. I.
    Ivakhov, V. M.
    Paramonova, N. N.
    RUSSIAN METEOROLOGY AND HYDROLOGY, 2022, 47 (10) : 767 - 780
  • [35] Temperature regulation of soil carbon dioxide production in the Humid Pampa of Argentina: estimation of carbon fluxes under climate change
    Alvarez, R
    Alvarez, CR
    BIOLOGY AND FERTILITY OF SOILS, 2001, 34 (04) : 282 - 285
  • [36] Temperature regulation of soil carbon dioxide production in the humid pampa of Argentina: Estimation of carbon fluxes under climate change
    Alvarez R.
    Alvarez C.
    Biology and Fertility of Soils, 2001, 34 (4) : 282 - 285
  • [37] A LABORATORY STUDY OF LYSIMETER DRAINAGE UNDER CONTROLLED SOIL MOISTURE TENSION
    COLMAN, EA
    SOIL SCIENCE, 1946, 62 (05) : 365 - 382
  • [38] Radiative forcing of methane fluxes offsets net carbon dioxide uptake for a tropical flooded forest
    Dalmagro, Higo J.
    Zanella de Arruda, Paulo H.
    Vourlitis, George L.
    Lathuilliere, Michael J.
    Nogueira, Jose de S.
    Couto, Eduardo G.
    Johnson, Mark S.
    GLOBAL CHANGE BIOLOGY, 2019, 25 (06) : 1967 - 1981
  • [39] Changes in fluxes of carbon dioxide and methane caused by fire in Siberian boreal forest with continuous permafrost
    Koster, Egle
    Koster, Kajar
    Berninger, Frank
    Prokushkin, Anatoly
    Aaltonen, Heidi
    Zhou, Xuan
    Pumpanen, Jukka
    JOURNAL OF ENVIRONMENTAL MANAGEMENT, 2018, 228 : 405 - 415
  • [40] METHANE AND CARBON-DIOXIDE FLUXES FROM POORLY DRAINED ADJACENT CULTIVATED AND FOREST SITES
    LESSARD, R
    ROCHETTE, P
    TOPP, E
    PATTEY, E
    DESJARDINS, RL
    BEAUMONT, G
    CANADIAN JOURNAL OF SOIL SCIENCE, 1994, 74 (02) : 139 - 146