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61.
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Topsoil organic carbon mineralization and CO2 evolution of three paddy soils from South China and the temperature dependence 总被引:11,自引:0,他引:11
Carbon mineralization and its response to climatic warming have been receiving global attention for the last decade. Although the virtual influence of temperature effect is still in great debate, little is known on the mineralization of organic carbon (SOC) of paddy soils of China under warming. SOC mineralization of three major types of China's paddy soils is studied through laboratory incubation for 114 d under soil moisture regime of 70% water holding capacity at 20℃ and 25℃ respectively. The carbon that mineralized as CO2 evolved was measured every day in the first 32 d and every two days in the following days. Carbon mineralized during the 114 d incubation ranged from 3.51 to 9.22 mg CO2-C/gC at 20℃ and from 4.24 to 11.35 mg CO2-C/gC at 25℃ respectively; and a mineralizable C pool in the range of 0.24 to 0.59 gC/kg, varying with different soils. The whole course of C mineralization in the 114 d incubation could be divided into three stages of varying rates, representing the three subpools of the total mineralizable C: very actively mineralized C at 1-23 d, actively tnineralized C at 24--74 d and a slowly mineralized pool with low and more or less stabilized C mineralization rate at 75-114 d. The calculated Q10 values ranged from 1.0 to 2.4, varying with the soil types and N status. Neither the total SOC pool nor the labile C pool could account for the total mineralization potential of the soils studied, despite a well correlation of labile C with the shortly and actively mineralized C, which were shown in sensitive response to soil warming. However, the portion of microbial C pool and the soil C/N ratio controlled the C mineralization and the temperature dependence. Therefore, C sequestration may not result in an increase of C mineralization proportionally. The relative control of C bioavailability and microbial metabolic activity on C mineralization with respect to stabilization of sequestered C in the paddy soils of China is to be further studied. 相似文献
63.
三峡库区小江回水区二氧化碳分压的时空变化特征分析 总被引:3,自引:0,他引:3
2009年9月~2010年4月在三峡库区与小江交汇的回水区的典型段面测量了该区域水体表层水和水体内部两部分水体中的有关物理化学参数,并利用这些水化学特征值通过水化学平衡模型计算出该区域水体CO2的分压。得出该区域水体中的CO2分压在一定时空范围内的变化特征。并对该区域有关水质参数与CO2的分压进行了相关性分析,得出其相关系数。指出了水体CO2分压与水体碳循环的关系。通过对三峡库区小江流域这一典型回水区域水体的CO2分压的分析研究,可望为三峡库区及其它同类型区域水体的二氧化碳分压研究提供一个分析案例,也为今后进一步从事水库温室效应的研究提供参考 相似文献
64.
刘丽萍 《中国人口.资源与环境》2011,(Z1)
根据云南省能源消费量,计算了由能源消费产生的CO2排放量及单位GDP碳排放强度。结果表明:近10年来,随着社会经济的快速发展,云南省能源消费及能源消费导致的CO2排放总量也呈现出显著上升的趋势。云南的碳排放强度高于全国平均水平,但人均碳排放量低于全国平均水平。以工业为主的第二产业是能源消费及碳排放的主体,其碳排放占总量的75%。 相似文献
65.
Household consumption is one of the important factors that induce COL emission. Based on input-output model, this article calculated the intensity of CO2 emission of different income groups and seven provinces in China, and then estimated total CO2 emission induced by urban household consumption from 1995 to 2004 in China based on statistic data of household living expenditure. The results show that CO2 emission per capita induced by household consumption had increased from 1583 to 2498 kg CO2 during 1995-2004. The ratio of consumption-induced CO2 emission to total CO2 emission had risen from 19% to 30% in the past decade. Indirect CO2 emission accounted for an important part of the consumption-induced emission, the ratio of indirect emission to consumption-induced emission had risen from 69% to 79% during the same period. A significant difference in consumption-induced CO2 emission across different income groups and different regions has been observed. COs emission per capita of higher income groups and developed regions increased faster than that of lower income groups and developing regions. Changing lifestyle has driven significant increase in CO2 emission. Especially, increases in private transport expenditure (for example, vehicle expenditure) and house building expenditure are key driving factors of growth in consumption-induced COL emission. There are big differences in the amount of CO2 emission induced by change in lifestyle across different income groups and provinces. It can be expected that lower income households and developing regions will increase consumption to improve their livings with income growth in the future, which may induce much more CO2 emission. A reasonable level of CO2 emission is necessary to satisfy human needs and to improve living standard, but a noticeable fact is that CO2 emission per capita induced by household consumption in developed areas of China had reached a quite high level. Adjustment in lifestyle towards a low-carbon society is in urgent need. 相似文献
66.
67.
碳捕捉与封存(CCS)技术的发展现状与前景 总被引:2,自引:0,他引:2
文章评述了国外CO2封存的潜力和利用封存CO2技术提高油田采收率的发展趋势以及中国CO2驱油的现状及前景. 相似文献
68.
69.
环丁砜-哌嗪溶液吸收烟道气中二氧化碳 总被引:2,自引:0,他引:2
采用搅拌实验装置,研究环丁砜溶液及不同配比的环丁砜-PZ复合溶液对烟道气中二氧化碳的吸收和解吸性能,揭示了吸收容量与酸碱度、时间之间的内在联系,并对CO2初始逸出温度、试液再生温度、试液再生率、再生pH下降率进行了细致记录分析。实验结果表明,环丁砜-PZ复合溶液配比为0.4∶0.6时:吸收效果最佳,吸收量约为0.126 mol;再生温度最高,为105℃;再生率最高,为90.34%。同时与相同配比的MEA、DEA相比具有较大再生优势。实验结果还表明,环丁砜-PZ复合体系之间存在负交互作用。 相似文献
70.