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西安黄土塬区土壤碳释放规律研究

Change of CO2 Emission from Soil in Loess Tableland Areas of Xi’an

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【作者】 张晓龙赵景波马润花

【Author】 ZHANG Xiao long1, ZHAO Jing bo2,3, MA Run hua4(1. College of Environmental Science and Engineering, Ocean University of China, Qingdao 266003,China; 2. Geographical Department, Shaanxi Normal University, Xi’an 710062, China; 3. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS, Xi’an, 710075, China; 4. Geographical Department, Yantai Normal College of Shandong, Yantai 264025, China)

【机构】 中国海洋大学环境科学与工程学院陕西师范大学旅游与环境学院山东烟台师范学院地理系 山东青岛266003陕西西安710062中国科学院地球环境研究所黄土与第四纪地质国家重点实验室陕西西安710075山东烟台264025

【摘要】 采用现场观测方法,研究了西安黄土塬区土壤碳释放规律。结果表明,不同条件下土壤CO2释放量具有明显的日变化。土壤CO2释放量的变化与温度的变化趋势基本一致,但时间上有一定的滞后,释放量白昼低于夜间。温度是影响土壤CO2释放量变化最重要的因素。CO2释放量对土质变化敏感土质疏松,释放量大;致密的土壤,释放量小。土壤CO2释放量的大小可作为评价土质的一项重要指标。

【Abstract】 Through using alkali aqua absorption method, the amount of CO2 emission from soil was observed round the clock in Bailu tableland and Shaoling tableland of xi’an, whose topsoil layer was usually composed of Malan loess. The results showed that there existed apparent diurnal courses of CO2 emission amount in soil under different conditions. CO2 emission amount tended to change similarly with the temperature, but had a retardation time. The amount of CO2 emission in the daytime was less than that at night in loess tableland Soil of Xi’an. Temperature was the most important factor affecting CO2 emission. The emission of CO2 in the soil was sensitive to the texture and structure of soil and More CO2 emitted from loose layers than solid ones, which suggested that the amount of CO2 emission could be regarded as an important index of soil evaluation.

【关键词】 土壤CO2释放量黄土塬温度西安
【Key words】 CO2 from soilemission amountloess tablelandtemperatureXi’an
【基金】 国际地质对比计划项目(IGCP448);中国科学院地球环境研究所黄土与第四纪地质国家重点实验室项目(SKLLQG0007);国家资源部岩动力开放研究实验室项目(9901)
  • 【文献出处】 农业环境科学学报 ,Journal of Agro-environmental Science , 编辑部邮箱 ,2004年02期
  • 【分类号】S153
  • 【被引频次】9
  • 【下载频次】155
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