The monthly variety of the daytime average apparent CO2 flux was obvious, and redox potential and temperature were two main factors impacting the diurnal apparent CO2 flux from intertidal sediments to the atmosphere.
裸露潮间带沉积物-大气间表观CO2通量日间平均值存在明显的月变化,而表层沉积物氧化还原电位和温度的月变化是造成表观CO2通量月变化的主要因素。
参考来源 - 裸露潮间带表观CO·2,447,543篇论文数据,部分数据来源于NoteExpress
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