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Comparative Study on Characteristics and Influencing Factors of Soil Respiration of Reed Wetlands in Yellow River Estuary and Liaohe River Estuary

机译:黄河口与辽河河口芦苇湿地土壤呼吸特征及影响因素比较研究

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Soil respiration rates of reed wetlands in the Yellow River Estuary and in the Liaohe River Estuary were determined with a Li-8100 Automated Soil CO2 Flux System in May and November, 2009, respectively, and reasons were analyzed for the difference in respiration rates between the two wetlands. Analytical results showed that: 1) Average soil respiration rate of the Yellow River Estuary was 1.06 μmol·m~(-2)·s~(-1) in May and 0.24 μmol·m~(-2)·s~(-1) in November, which was 17 times and twice as much as those in the Liaohe River Estuary, respectively. And main reasons leading to the difference included temperature, moisture and texture of soil, while nutrient elements were not a major influencing factors. 2) Soil respiration rate of the Yellow River Estuary decreased with the rising of soil temperature in May when soil temperature was relatively high, and exhibited no significant diurnal variation in November; the rate in May was 4 times than that in November, mainly influenced by soil temperature and variation in vegetation growth period. In the Liaohe River Estuary, the rate was severely inhibited by the high soil moisture and exhibited insignificant diurnal variation in May, while it increased with the rising of soil temperature in November; the rate in May was merely half that in November.
机译:在2009年5月和11月,2009年5月和11000年的自动化土壤二氧化碳通量系统确定了黄河口和辽河河口中芦苇湿地的土壤呼吸率,并分析了呼吸率之间的原因两个湿地。分析结果表明:1)黄河口的平均土壤呼吸率为5月和0.24μmol·m〜(-2)·s〜(-1)·s〜(-2)·s〜( - 1)11月,分别为17倍,分别是辽河河口的两倍。主要原因是导致差异的主要原因包括温度,水分和土壤质地,而营养素元素不是主要的影响因素。 2)黄河口的土壤呼吸率随着土壤温度较高的土壤温度升高而下降,11月份没有显着的昼夜变化; 5月份的速度是11月的4次,主要是受土壤温度的影响和植被生长期的变化。在辽河河口中,率受到高土壤水分的严重抑制,并在5月份出现了微不足道的昼夜变异,而11月土壤温度的上升则增加; 5月份的速度仅仅是11月的一半。

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