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Spatial and temporal patterns of CO(2) and CH(4) fluxes in China's croplands in response to multifactor environmental changes

机译:中国农田CO(2)和CH(4)通量对多因素环境变化的响应时空格局

摘要

The spatial and temporal patterns of CO(2) and CH(4) fluxes in China's croplands were investigated and attributed to multifactor environmental changes using the agricultural module of the Dynamic Land Ecosystem Model (DLEM), a highly integrated process-based ecosystem model. During 1980-2005 modelled results indicated that China's croplands acted as a carbon sink with an average carbon sequestration rate of 33.4 TgC yr-1 (1 Tg = 1012 g). Both the highest net CO(2) uptake rate and the largest CH(4) emission rate were found in southeast region of China's croplands. Of primary influences were land-cover and land-use change, atmospheric CO(2) and nitrogen deposition, which accounted for 76%, 42% and 17% of the total carbon sequestration in China's croplands during the study period, respectively. The total carbon losses due to elevated ozone and climate variability/change were equivalent to 27% and 9% of the total carbon sequestration, respectively. Our further analysis indicated that nitrogen fertilizer application accounted for 60% of total national carbon uptake in cropland, whereas changes in paddy field areas mainly determined the variability of CH(4) emissions. Our results suggest that improving air quality by means such as reducing ozone concentration and optimizing agronomic practices can enhance carbon sequestration capacity of China's croplands.
机译:使用高度集成的基于过程的生态系统模型动态土地生态系统模型(DLEM)的农业模块,对中国农田中CO(2)和CH(4)通量的时空格局进行了调查,并将其归因于多因素环境变化。在1980年至2005年期间,模拟结果表明,中国的农田是一个碳汇,平均碳固存率为33.4 TgC yr-1(1 Tg = 1012 g)。最高的净CO(2)吸收率和最大的CH(4)排放率都在中国农田的东南部地区发现。在研究期间,主要影响因素是土地覆盖和土地利用变化,大气中的CO(2)和氮沉降,分别占中国农田中固碳总量的76%,42%和17%。由于臭氧升高和气候变化/变化造成的总碳损失分别相当于总固碳的27%和9%。我们的进一步分析表明,氮肥的使用占农田中全国碳吸收总量的60%,而水田的变化主要决定了CH(4)排放的变化性。我们的结果表明,通过降低臭氧浓度和优化农艺方法等改善空气质量可以提高中国农田的固碳能力。

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