Soil Carbon Discharge Dynamics of Different Vegetation Types in Datong Reclamation District Filled with Coal Gangue
|更新时间:2025-03-12
|
Soil Carbon Discharge Dynamics of Different Vegetation Types in Datong Reclamation District Filled with Coal Gangue
Bulletin of Soiland Water ConservationVol. 32, Issue 2, Pages: 30-34(2013)
作者机构:
1. 安徽理工大学地球与环境学院,安徽,淮南,232001
2. 淮南煤炭工程技术研究院生态环境研究室,安徽,淮南,232001
作者简介:
基金信息:
DOI:
CLC:
Published:2013
稿件说明:
移动端阅览
YAO Duo-xi, ZHAO Kui, ZHANG Zhi-guo, et al. Soil Carbon Discharge Dynamics of Different Vegetation Types in Datong Reclamation District Filled with Coal Gangue[J]. Bulletin of Soiland Water Conservation, 2013, 32(2): 30-34.
DOI:
YAO Duo-xi, ZHAO Kui, ZHANG Zhi-guo, et al. Soil Carbon Discharge Dynamics of Different Vegetation Types in Datong Reclamation District Filled with Coal Gangue[J]. Bulletin of Soiland Water Conservation, 2013, 32(2): 30-34.DOI:
Soil Carbon Discharge Dynamics of Different Vegetation Types in Datong Reclamation District Filled with Coal Gangue
Soil respiration rates as well as soil temperature and moisture for four types of vegetation(grassland
bushes
small arbors
arbors)were monitored with Li-8100automated soil CO2flux systems at the reclamation district filled with coal gangue
which is located in Datong district of Huainan City
from July 2011to March 2012.The results indicated that diurnal variations of soil respiration for the four types of vegetationshowed a mode of single peak curve with the maximum value appearing in summer between 12:00and 16:00and the minimum value appearing in winter around 4:00AM.The soil respiration under different vegetationtypes differed significantly(p<0.05)
and its rates followed a decreasing order in vegetation types as grassland
shrubs
small arbors and arbors.The annual emission of soil CO2for four types of vegetation were999.74±62.26
small arbors and shrubs instead of grassland should be plantedin the study area.In addition to vegetation types
soil respiration of the area were affected by soil temperature at the depth of 10cm.The relationship between soil respiration and soil temperature was described well by anexponential equation
which explains more than 88%of the variance of soil respiration.The Q10(index of sensitvity)values of grassland