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黔中喀斯特石漠化地区土壤温室气体浓度的时空分布特征
摘要点击 1938  全文点击 1742  投稿时间:2008-12-25  修订日期:2009-06-02
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中文关键词  喀斯特  土壤  温室气体浓度  时空变化  黔中地区
英文关键词  Karst  soil  greenhouse gas concentration  temporal and spatial variation  central part of Guizhou Province
作者单位
刘芳 中国科学院地球化学研究所环境地球化学国家重点实验室贵阳550002 
刘丛强 中国科学院地球化学研究所环境地球化学国家重点实验室贵阳550002 
王仕禄 中国科学院地球化学研究所环境地球化学国家重点实验室贵阳550002 
吕迎春 中国科学院烟台海岸带可持续发展研究所烟台264003 
中文摘要
      2006~2007年对喀斯特石漠化地区土壤剖面中CO2、N2O和CH4的浓度分布进行观测.结果表明,土壤剖面中CO2、N2O和CH4浓度分别介于530.2~31512.6、 0.27~0.67和0.1~3.5μL·L-1.总体上,自地表向下,CO2和N2O浓度逐渐增大,CH4浓度则为逐渐减小,但在阴冷潮湿的10、11月和1月,15cm以下土层中CO2和N2O浓度随着深度的增加逐渐减小,CH4浓度则明显增加.土壤温度、水分同时影响剖面中CO2、N2O和CH4的时空分布,但影响效应以及作用的土层深度有所不同.相关分析结果表明,土壤中CO2 和N2O浓度的时空分布显著正相关(r为0.780~0.894, p<0.05~0.01),相关关系受环境因子的影响;CO2和CH4的时空分布则呈显著负相关关系(r=330, p<0.01);N2O和CH4的空间分布为互逆关系,但只在土壤水分较大月份达到显著水平(r为-0.829~-0.956, p<0.05~0.01).
英文摘要
      Concentrations of CO2,N2O and CH4 of soil profile in Karst Stone Desertification Areas were measured monthly from June of 2006 to May of 2007. The results indicated that the concentrations of CO2,N2O and CH4varied from 530.2 to 31512.6, 0.27 to 0.67 and 0.1 to 3.5 μL·L-1.On the whole, with the increase of soil depth, the concentrations of CO2 and N2O increased, while CH4 decreased. However, in the cold and wet October, November and January, the concentrations of CO2 and N2O decreased with the depth below 15 cm. In contrast, CH4 had the inverse trend. Soil temperature and moisture were the main factors which had impacts on the temporal and spatial variations of CO2, N2O and CH4concentrations in soil profile, but the influence impacts were different. The correlation analysis showed that there was positive correlation between CO2 and N2O(r 0.780-0.894, p<0.05-0.01), while correlation degree was controlled by environmental factors in different months.CH4 concentrations in soil had significantly negative correlation with CO2 concentrations(r=330, p<0.01), but correlated with N2O concentrations just in moisture months(r -0.829--0.956, p<0.05-0.01).

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