{"title":"模拟不同管理策略和环境条件下荷兰草地的碳循环。","authors":"A. Dasselaar, E. Lantinga","doi":"10.18174/njas.v43i2.575","DOIUrl":null,"url":null,"abstract":"A simulation model of the grassland carbon cycle (CCGRASS) was developed to evaluate the long-term effects of different management strategies and various environmental conditions on carbon sequestration in a loam soil under permanent grassland in the Netherlands. The model predicted that the rate of increase in the amount of soil organic carbon will be greatest at low to moderate application rates of nitrogen (100-250 kg N/ha per year). This is because the annual gross photosynthetic uptake of CO2 in permanent grassland is hardly influenced by the level of N supply. Since N shortage stimulates the growth of the unharvested plant parts (roots and stubble) the carbon supply to the soil is highest at low to moderate N application rates. The rate of increase in soil organic carbon will be greater under grazing than under mowing as a result of a greater amount of carbon added to the soil. Increase of atmospheric CO2 concn may induce an increase in decomposition rate of soil organic matter due to simultaneously increased temperatures. At the same time, plant productivity and thus carbon supply to the soil will be stimulated due to the CO2-fertilization effect. Assuming a temperature increase of 3 degrees C if the present atmospheric CO2 concn doubles, the model predicted that the combined effect of elevated CO2 and temperature will slightly reduce the rate of increase in the amount of organic carbon in grassland soils compared to that under unchanged environmental conditions. There was 2% less carbon sequestration by grassland at the end of a 100 year period as a result of these changes in environmental conditions. The separate effects of increased temperature or elevated CO2 were 10% less and 10% more carbon storage after 100 years, resp.","PeriodicalId":324908,"journal":{"name":"Netherlands Journal of Agricultural Science","volume":"7 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1995-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"33","resultStr":"{\"title\":\"Modelling the carbon cycle of grassland in the Netherlands under various management strategies and environmental conditions.\",\"authors\":\"A. Dasselaar, E. Lantinga\",\"doi\":\"10.18174/njas.v43i2.575\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"A simulation model of the grassland carbon cycle (CCGRASS) was developed to evaluate the long-term effects of different management strategies and various environmental conditions on carbon sequestration in a loam soil under permanent grassland in the Netherlands. The model predicted that the rate of increase in the amount of soil organic carbon will be greatest at low to moderate application rates of nitrogen (100-250 kg N/ha per year). This is because the annual gross photosynthetic uptake of CO2 in permanent grassland is hardly influenced by the level of N supply. Since N shortage stimulates the growth of the unharvested plant parts (roots and stubble) the carbon supply to the soil is highest at low to moderate N application rates. The rate of increase in soil organic carbon will be greater under grazing than under mowing as a result of a greater amount of carbon added to the soil. Increase of atmospheric CO2 concn may induce an increase in decomposition rate of soil organic matter due to simultaneously increased temperatures. At the same time, plant productivity and thus carbon supply to the soil will be stimulated due to the CO2-fertilization effect. Assuming a temperature increase of 3 degrees C if the present atmospheric CO2 concn doubles, the model predicted that the combined effect of elevated CO2 and temperature will slightly reduce the rate of increase in the amount of organic carbon in grassland soils compared to that under unchanged environmental conditions. There was 2% less carbon sequestration by grassland at the end of a 100 year period as a result of these changes in environmental conditions. 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引用次数: 33
摘要
建立了草地碳循环(CCGRASS)模拟模型,以评估荷兰永久草地下不同管理策略和不同环境条件对壤土碳固存的长期影响。模型预测,低至中等施氮量(100 ~ 250 kg N/ hm2 /年)土壤有机碳增加速率最大。这是因为永久草地的年总光合吸收CO2几乎不受氮供应水平的影响。由于氮素短缺刺激了未收获植物部分(根和残茬)的生长,因此在低至中等施氮量下,土壤的碳供应最高。放牧条件下土壤有机碳的增加速度比刈割条件下要快,因为土壤中添加了更多的碳。大气CO2浓度的增加可能会引起土壤有机质分解速率的增加,因为同时温度升高。同时,由于二氧化碳的施肥效应,植物的生产力和对土壤的碳供应将受到刺激。模型预测,如果当前大气CO2浓度增加一倍,温度升高3℃,与环境不变条件下相比,CO2和温度升高的共同作用将略微降低草地土壤中有机碳量的增长率。由于这些环境条件的变化,在100年的周期结束时,草地的碳固存减少了2%。温度升高或二氧化碳浓度升高的单独影响分别是100年后碳储量减少10%和增加10%。
Modelling the carbon cycle of grassland in the Netherlands under various management strategies and environmental conditions.
A simulation model of the grassland carbon cycle (CCGRASS) was developed to evaluate the long-term effects of different management strategies and various environmental conditions on carbon sequestration in a loam soil under permanent grassland in the Netherlands. The model predicted that the rate of increase in the amount of soil organic carbon will be greatest at low to moderate application rates of nitrogen (100-250 kg N/ha per year). This is because the annual gross photosynthetic uptake of CO2 in permanent grassland is hardly influenced by the level of N supply. Since N shortage stimulates the growth of the unharvested plant parts (roots and stubble) the carbon supply to the soil is highest at low to moderate N application rates. The rate of increase in soil organic carbon will be greater under grazing than under mowing as a result of a greater amount of carbon added to the soil. Increase of atmospheric CO2 concn may induce an increase in decomposition rate of soil organic matter due to simultaneously increased temperatures. At the same time, plant productivity and thus carbon supply to the soil will be stimulated due to the CO2-fertilization effect. Assuming a temperature increase of 3 degrees C if the present atmospheric CO2 concn doubles, the model predicted that the combined effect of elevated CO2 and temperature will slightly reduce the rate of increase in the amount of organic carbon in grassland soils compared to that under unchanged environmental conditions. There was 2% less carbon sequestration by grassland at the end of a 100 year period as a result of these changes in environmental conditions. The separate effects of increased temperature or elevated CO2 were 10% less and 10% more carbon storage after 100 years, resp.