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Carbon Sources and Sinks of China Costal Farmland Ecosystem

机译:中国沿海农田生态系统的碳源与汇

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This article estimated the size of carbon sink, emission, net carbon sink farmland ecosystem in China costal regions (including ten provinces) with statistic data from 1990 to 2010(which include crop yield and agricultural consumptions). Conclusions are as following: (1) the total carbon sink, emission and net sink of farmland ecosystem in China costal regions all increased since 1990. Carbon sink is obviously more than carbon emission, for example, total carbon sink in 2010 is 3 times more than carbon emission, which showed that the costal region is generally a "sink" region. While, because the increasing rate of carbon emission (265%) exceeded that of carbon sink (44%), the carbon sink function of farmland ecosystem in China costal regions will be saturated within several decades. (2) There were significant temporal-spatial differences in carbon sink, emission and net sink among different costal regions. Further, there are also differences in per area carbon sink, emission and net sink among different costal regions. The total and per area carbon emission increased year by year from 1990, while that of carbon sink and net sink changed drastically. The total carbon sink and net sink in relative developed regions has a down trend from 1990 to 2010. a special example: carbon emission exceeded carbon sink and caused that net carbon sink and per area net carbon sink was negative in 2010 in Shanghai, which indicated that Shanghai has been a carbon "source" region in 2010 because the decrease of cropland and increase of agricultural consumptions. (3) The proportion of carbon sinks in the main crops of farmland ecosystem in China costal regions compared with that of the whole nation decreased since 1990, which indicate that with the decrease of cropland and increase of agricultural consumptions, the carbon sink function of costal farmland is weaken.
机译:本文利用1990年至2010年的统计数据(包括作物产量和农业消费量)估算了中国沿海地区(包括十个省)的碳汇,排放量和净碳汇农田生态系统的规模。结论如下:(1)自1990年以来,中国沿海地区农田生态系统的总碳汇,排放和净汇都增加了。碳汇明显大于碳排放,例如,2010年的总碳汇是碳汇的3倍以上。碳排放量,这表明沿海地区通常是一个“下沉”地区。同时,由于碳排放的增长速度(265%)超过了碳汇的增长速度(44%),中国沿海地区农田生态系统的碳汇功能将在几十年内达到饱和。 (2)不同沿海地区的碳汇,碳排放和净汇存在明显的时空差异。此外,不同沿海地区的单位面积碳汇,排放和净汇也存在差异。从1990年开始,总的碳排放量和单位面积的碳排放量逐年增加,而碳汇和净汇的碳排放量则急剧变化。从1990年到2010年,相对发达地区的总碳汇和净汇呈下降趋势。一个特殊的例子:2010年上海的碳排放量超过碳汇,导致净碳汇和单位面积净碳汇为负数,这表明上海由于减少耕地和增加农业消费而成为2010年的碳“源”地区。 (3)1990年以来,中国沿海地区农田生态系统主要作物碳汇的比例与全国相比有所下降,表明随着农田的减少和农业消费的增加,沿海地区碳汇的功能耕地被削弱。

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