首页|短花针茅荒漠草原土壤呼吸对载畜率的响应

短花针茅荒漠草原土壤呼吸对载畜率的响应

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土壤碳通量是陆地生态系统中碳循环的重要组成部分.为了揭示放牧对荒漠草原土壤呼吸速率的影响,我们采取完全随机区组设计比较研究了不同载畜率下草地土壤的呼吸速率.试验包括4个处理,3次重复.4个处理分别是对照(CK)、轻度放牧(LG)、中度放牧(MG)和重度放牧(HG),相应的载畜率分别为0,0.91,1.82 和2.71只羊*hm-2*半年-1.在2004年和2006年8月,采用LI-6400-09土壤呼吸室与LI-6400连接对每个样地的土壤呼吸速率进行了测定,在测定过程中,同时获取了土壤温度及土壤呼吸室中的相对湿度等相关指标.通过对测定数据的分析表明,内蒙古荒漠草原土壤呼吸速率介于0.80 μmol·m-2·s-1与5.00 μmol·m-2·s-1之间.随着载畜率的增加,土壤呼吸速率明显增加(P<0.05).另外,土壤呼吸速率也随着土壤呼吸室中相对湿度的增加而增大,但是二者的相关关系不太明显(P>0.05).经过2年放牧后,重度放牧条件下的土壤呼吸速率明显低于对照区和轻度放牧区,不同载畜率下土壤呼吸速率随时间的变化并没有明显的差异.高载畜率下土壤呼吸速率明显降低可能与该条件下土壤水分和草地生物量的明显降低有关,土壤水分对土壤和大气之间CO2的交换起着非常重要的作用.
Soil Respiration Response to Different Stocking Rates on Stipa breviflora Griseb. Desert Steppe
Soil surface carbon dioxide flux is a very important component of carbon cycle of terrestrial ecosystems.In order to determine grazing impact on soil respiration rates under different stocking rates,a comparative study of soil respiration was conducted in a Desert Steppe in Inner Mongolia,P.R.China.A randomized complete block design was used with three replications and four grazing treatments:Control (CK),lightly grazed (LG), moderately grazed (MG) and heavily grazed (HG).The stocking rates were 0,0.91,1.82 and 2.71 sheep\5hm-2·half-year-1,for control,LG,MG and HG treatments, respectively.Soil respiration rate,soil temperature,and soil moisture were obtained in each plot by enclosed chamber method in 2004 and 2006.The results showed that soil respiration rate fluctuated from 0.80 μmol·m-2·s-1 to 5.00 μmol·m-2·s-1.Soil respiration rate was sharply decreased with increase of stocking rate (P<0.05).Meanwhile,soil respiration rate increased with increase of relative humidity in an enclosed chamber,but the regression relationship was not significant (P>0.05).Soil respiration rate has a significant decrease in HG treatment compared to CK and LG treatments through two years' treatment.There is no significant effect of time change on soil respiration in different stocking rates.Soil respiration rate was decreased significantly in a high stocking rate,which might be related to low soil moisture and biomass in these sites.Soil moisture plays an important role in CO2 exchange between soil and atmosphere.

carbon dioxidegrazinggrasslandsoil moisturesoil respirationsoil temperature

王忠武、焦树英、韩国栋、赵萌莉、Walter D Willms

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内蒙古农业大学生态环境学院,呼和浩特,010018

加拿大农业与农业食品部列桥研究中心,列桥 T1J 4B1

山东农业大学资源与环境学院,山东,泰安,271018

加拿大农业与农业食品部列桥研究中心,列桥, T1J 4B1

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CO2 放牧 草地 土壤湿度 土壤呼吸 土壤温度

国家重点基础研究发展规划(973计划)教育部高校优秀教师教学科研奖励计划国家科技支撑项目

2007CB1068002006BAD16B01

2009

内蒙古大学学报(自然科学版)
内蒙古大学

内蒙古大学学报(自然科学版)

CSTPCDCSCD北大核心
影响因子:0.346
ISSN:1000-1638
年,卷(期):2009.40(2)
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