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农田土壤中N2O释放的水温特征研究

Characteristics of N2O Emissions from Farmland Responding to Water and Temperature

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【作者】 韩建刚李占斌朱咏莉白红英李世清

【Author】 HAN Jian-gang~1, LI Zhan-bin~(2, 3), ZHU Yong-li~2, BAI Hong-ying~1, LI Shi-qing~1 (1.College of Resources and Environment al Science, Northwestern Sci-tech University of Agriculture & Forestry, ShaanXi Yangling 712100, China; 2.Research Center of Soil and Water Conservation and Ecological Environment, Chinese Academy of Sciences,and the Education Ministry, ShaanXi Yangling 712100, China;3.Xi’an University of Technology, Xi’an 710048).

【机构】 西北农林科技大学资源环境学院中国科学院教育部水土保持与生态环境研究中心西北农林科技大学资源环境学院 陕西杨凌712100陕西杨凌712100西安理工大学陕西西安710048陕西杨凌712100陕西杨凌712100

【摘要】 室内模拟研究不同水热条件下土壤中N2O的释放特征,有助于阐明N2O释放的水热效应机理。本文通过室内试验研究了西北地区的典型耕种土壤土娄土中N2O在不同水温变化下的释放特征,借助化学反应动力学理论对其释放机理进行了初步的探讨。结果表明:10℃和30℃下,不同含水量的土壤中N2O的浓度变化随着培养时间的延长呈"S"型曲线。可用方程C=1/[A+Bexp(-t)]来描述。随着温度的升高(10℃到30℃),N2O释放的快速期,减速期,稳定期的启动时间明显提前。在较低的土壤湿度范围内(27%至58%wfps),土壤中N2O释放的稳定浓度与土壤湿度呈正相关;田间持水量(58%wfps)时,N2O释放的稳定浓度达到最大;超过田间持水量时,其逐渐变小。当土壤湿度从27%-42%wfps增加时,30℃下土壤中N2O释放的稳定浓度大于10℃下的;当土壤湿度等于或大于田间持水量(58%wfps)时,30℃下土壤中N2O释放的稳定浓度小于10℃下的。低温下(10℃)的风干土壤(8%wfps)存在吸收N2O的现象。不同水热条件下土壤硝化和反硝化过程中N2O释放的表观化学反应速率常数和对应活化能的大小决定了土壤中N2O的释放量及难易程度。

【Abstract】 Model experiment provides possibilities for the study of N2O emission from soil under different water and temperature regimes. Effects of water and temperature on the N2O emission and the preliminary mechanism of the soil N2O emission were studied in terms of the kinetic theory of chemical reactions in the Lou soil-a typically cultivated soil in arid and semiarid region in the Northwester of China. Results showed: the curve of soil N2O concentration with incubation time under the different water regime is "S-shaped" and can be described by the equation C=1/[A+Bexp(-t)] when the incubation temperatures are 10℃and 30℃. The startup time of fast-stage, deceleration-stage and stable stage of soil N2O emission were advanced clearly with the increase of incubation temperature from 10℃to 30℃.The stable concentration of N2O increased with the increase of soil water contents (from 27 to 58% wfps), and it became smaller gradually when water content was above the field water capacity. The highest concentration occurred at the field water capacity (58%wfps). The stable concentration at the 30℃ was higher than that at the 10℃ when the soil moisture varied from 27 to 42%wfps. However, the trend was opposite when water content was above the field water capacity (58%wfps). Also, the air-dried soil (8%wfps) could absorb N2O weakly at the lower temperature (10℃).The apparent rate constant and activation energy of soil nitrification and denitrification process dominated the soil N2O emission in the different water and temperature regime.

【基金】 中国科学院知识创新工程资助项目"黄土高原区域水土保持环境效应与生态环境建设对策"(KZCX1-10-04)
  • 【文献出处】 土壤通报 ,Chinese Journal of Soil Science , 编辑部邮箱 ,2004年03期
  • 【分类号】S152
  • 【被引频次】31
  • 【下载频次】251
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