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首页> 外文期刊>Plant and Soil >Contrasting diurnal variations in soil organic carbon decomposition and root respiration due to a hysteresis effect with soil temperature in a Gossypium s. (cotton) plantation
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Contrasting diurnal variations in soil organic carbon decomposition and root respiration due to a hysteresis effect with soil temperature in a Gossypium s. (cotton) plantation

机译:棉铃虫对土壤温度的滞后效应引起的土壤有机碳分解和根系呼吸的昼夜变化。 (棉花)种植园

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To understand the characteristics of the diurnal variation in soil respiration and its response to temperature, we used root exclusion plots, and buried CO2 sensors in situ during the late growing season in northwestern China. Soil organic carbon (SOC) decomposition and root respiration dynamics were quantified. In our study, we found that the diurnal variations in root respiration and soil organic carbon (SOC) decomposition showed a contrasting diurnal pattern. SOC decomposition peaked in the afternoon and was in phase with an increase in soil temperature at 10 cm; whereas root respiration decreased from similar to 08:00-09:00 and was minimal at similar to 17:00-18:00 despite an increase in soil temperature. Furthermore, an exponential function explained the diurnal variation in total soil respiration and SOC decomposition (r(2) > 0.6, n = 504), but not so for root respiration (r(2) < 0.3, n = 504). The fitted Q (10) value of 4.3 for SOC decomposition was significantly higher than the Q (10) value of 3.1 for root respiration. This result suggested that the root respiration rate had a different temperature sensitivity to the microbial respiration rate. In addition, we observed a significant (p < 0.001) clockwise hysteretic effect for SOC decomposition with respect to soil temperature at 10 cm over a 24 h period, with higher rates when soil temperature was increasing and lower rates when soil temperature was decreasing. By contrast, the diurnal hysteresis in root respiration with soil temperature at 10 cm was always counter-clockwise, with lower rates when soil temperature was increasing than when soil temperature was decreasing. This study emphasizes that root respiration and SOC decomposition have different responses to changing soil temperature. Therefore, modeling the impact of global climate change on soil carbon efflux should consider simultaneously, but separately, the impact of the two components.
机译:为了了解土壤呼吸的昼夜变化特征及其对温度的响应,我们使用了根系排斥图,并在中国西北部的生长期后期使用了埋藏式CO2传感器。量化土壤有机碳(SOC)的分解和根系呼吸动力学。在我们的研究中,我们发现根系呼吸作用和土壤有机碳(SOC)的昼夜变化表现出相反的昼夜模式。 SOC的分解在下午达到顶峰,并与土壤温度在10 cm的升高阶段同步。尽管土壤温度升高,但根呼吸作用却从大约08:00-09:00降低到17:00-18:00,最小。此外,指数函数解释了土壤总呼吸和SOC分解的日变化(r(2)> 0.6,n = 504),但对于根系呼吸却不是这样(r(2)<0.3,n = 504)。 SOC分解的拟合Q(10)值为4.3,明显高于根部呼吸的3.1(Q)值。该结果表明根呼吸速率对微生物呼吸速率具有不同的温度敏感性。此外,我们观察到在24小时内相对于10 cm的土壤温度,SOC分解具有明显的(p <0.001)顺时针滞后效应,当土壤温度升高时速率较高,而当土壤温度降低时速率较低。相反,当土壤温度为10 cm时,根部呼吸的昼夜滞后总是逆时针方向,土壤温度升高时的速率比土壤温度降低时的速率低。这项研究强调,根系呼吸作用和SOC分解对土壤温度变化的反应不同。因此,对全球气候变化对土壤碳外流的影响进行建模时,应同时(但分别)考虑这两个因素的影响。

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