• 褐土 - 引用次数：4

  There were some significant differences between soil types in CO2 flux. The order of CO2 flux from large to small in different soil types was fragmental soil (351.82 μmol/(m2·h))>gray-cinnamonic soil(347.33 μmol/(m2·h))>chestnut soil (193.36 μmol/(m2·h)) >sierozem (162.37 μmol/(m2·h)).

  结果表明:森林土壤(粗骨土和山地灰褐土)的通量显著大于草原土壤(栗钙土和灰钙土)。

  参考来源 - 北温带干旱地区土壤

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