植物生态学报 ›› 2007, Vol. 31 ›› Issue (3): 355-362.DOI: 10.17521/cjpe.2007.0043
收稿日期:
2006-03-13
接受日期:
2006-04-14
出版日期:
2007-03-13
发布日期:
2007-05-30
通讯作者:
周广胜
作者简介:
* E-mail: gszhou@ibcas.ac.cn基金资助:
WANG Xu, ZHOU Guang-Sheng*(), JIANG Yan-Ling, CAO Ming-Chang, ZENG Wei, SONG Jian
Received:
2006-03-13
Accepted:
2006-04-14
Online:
2007-03-13
Published:
2007-05-30
Contact:
ZHOU Guang-Sheng
摘要:
利用静态箱式法测量长白山阔叶红松(Pinus koraiensis)林伐后13年的皆伐迹地土壤呼吸作用。分析表明,皆伐迹地土壤呼吸作用日变化趋势呈单峰曲线,峰谷值出现时间较林地提前2~4 h,与土壤5 cm深度温度变化趋势基本一致。整个生长季节皆伐迹地土壤呼吸速率约为林地的75%,土壤温度与土壤呼吸作用存在显著的指数关系。在降水量集中的生长季,土壤水分对土壤呼吸作用具有一定的抑制作用,利用温度和水分双因子模型可以较好地解释皆伐迹地土壤呼吸作用的变异。阔叶红松林皆伐后生物量减少和微环境变化是造成土壤呼吸作用强度和动态特征发生变化的重要原因。
王旭, 周广胜, 蒋延玲, 曹铭昌, 曾伟, 宋健. 长白山阔叶红松林皆伐迹地土壤呼吸作用. 植物生态学报, 2007, 31(3): 355-362. DOI: 10.17521/cjpe.2007.0043
WANG Xu, ZHOU Guang-Sheng, JIANG Yan-Ling, CAO Ming-Chang, ZENG Wei, SONG Jian. SOIL RESPIRATION IN A CLERA-CUT BROAD-LEAVED KOREAN PINE FOREST OF CAHNGBAI MOUNTAIN. Chinese Journal of Plant Ecology, 2007, 31(3): 355-362. DOI: 10.17521/cjpe.2007.0043
主要因子 Important factor | 阔叶红松林 Broad-leaved Korean pine forest | 皆伐迹地 Clear-cut field |
---|---|---|
主要优势植物种类 Dominant plant species | 红松(Pinus koraiensis)、水曲柳(Fraximus mandshurica)、糠椴(Tilia mandshurica) | 春榆(Ulmus davidiana)、大青杨(Populus ussuriensis)、柳属(Salix) |
地上生物量Aboveground biomass (103 kg·hm-2) | 287.2 ( | |
凋落物量 Litter mass (g·m-2) | 1 106.6 | 1 103.3 |
地下生物量 Belowground biomass (g·m-2) | 1 798.1 | 751.9 |
土壤容重 Bulk density (g·m-3) | 0.639 | 0.496 |
土壤有机碳 Organic C (mg·g-1) | 125.62 | 172.38 |
土壤全氮 Total N (mg·g-1) | 10.56 | 14.38 |
碳氮比 C:N proportion | 11.01 | 10.67 |
土壤pH值 Soil pH value | 4.91 | 5.13 |
表1 试验地概况
Table 1 Characteristics of the experimental fields
主要因子 Important factor | 阔叶红松林 Broad-leaved Korean pine forest | 皆伐迹地 Clear-cut field |
---|---|---|
主要优势植物种类 Dominant plant species | 红松(Pinus koraiensis)、水曲柳(Fraximus mandshurica)、糠椴(Tilia mandshurica) | 春榆(Ulmus davidiana)、大青杨(Populus ussuriensis)、柳属(Salix) |
地上生物量Aboveground biomass (103 kg·hm-2) | 287.2 ( | |
凋落物量 Litter mass (g·m-2) | 1 106.6 | 1 103.3 |
地下生物量 Belowground biomass (g·m-2) | 1 798.1 | 751.9 |
土壤容重 Bulk density (g·m-3) | 0.639 | 0.496 |
土壤有机碳 Organic C (mg·g-1) | 125.62 | 172.38 |
土壤全氮 Total N (mg·g-1) | 10.56 | 14.38 |
碳氮比 C:N proportion | 11.01 | 10.67 |
土壤pH值 Soil pH value | 4.91 | 5.13 |
图4 24 h土壤呼吸速率与土壤温度关系
Fig.4 Relationships between soil respiration rate and soil temperature during 24 hours a: 皆伐迹地 Clear-cut field b: 阔叶红松林 Korean pine forest
图7 土壤呼吸作用与土壤水分关系
Fig.7 Relationships between soil respiration and soil water content Q1: 阔叶红松林地土壤呼吸 Korean pine forest soil respiration Q2: 皆伐地土壤呼吸Clear-cut field soil respiration W: 土壤水分体积含量 Soil volumetric water content
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