Decomposition of organic matter in peat soil in a minerotrophic mire

被引:24
|
作者
Haraguchi, A
Kojima, H
Hasegawa, C
Takahashi, Y
Iyobe, T
机构
[1] Univ Kitakyushu, Kitakyushu, Fukuoka 8080135, Japan
[2] Niigata Univ, Fac Sci, Dept Environm Sci, Niigata 9502181, Japan
[3] Niigata Univ, Grad Sch Sci & Technol, Niigata 9502181, Japan
关键词
Alnus japonica; carbon dioxide emission; cellulolysis; Masukata mire; oxygen consumption; Phragmites australis; Sphagnum;
D O I
10.1016/S1164-5563(01)01112-8
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Decomposition of organic materials, oxygen consumption, and carbon dioxide emission were investigated in Masukata raire, a small minerotrophic mire in central Japan. We selected three dominant community types in the mire, a Sphagnum palustre community, a Phragmites australis community, and an Alnus japonica community, for the decomposition study sites. Decomposition rates were measured in the field by examining mass loss of peat and cellulose for 6 months. The oxygen consumption rate was measured in the field using a closed chamber equipped with an oxygen electrode. The carbon dioxide emission rate of the peat was measured by an infrared gas analyser in the laboratory under controlled conditions. Results of these measurements were tested by correlation analysis. The rate of mass loss of peat positively correlated with the CO2 emission rate. The cellulose decomposition rate showed significant differences among community types, and it had significant positive correlation with the oxygen consumption rate. Although oxygen consumption measurement is not generally used to estimate peatland soil respiration, the oxygen consumption method can be used for predicting long-term decomposition rate according to different vegetation types within a short time. (C) 2002 Editions scientifiques et medicales Elsevier SAS. All rights reserved.
引用
收藏
页码:89 / 95
页数:7
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