土壤碳固定是当前有关陆地生态系统碳循环与全球变化的地球表层过程研究的重要优先领域。国际社会对全球农业温室气体减排的需求,驱动着土壤学对土壤固碳容量与潜力、固碳与减排的过程与机理的前沿探索,并越来越呈现为一个独特的土壤学...土壤碳固定是当前有关陆地生态系统碳循环与全球变化的地球表层过程研究的重要优先领域。国际社会对全球农业温室气体减排的需求,驱动着土壤学对土壤固碳容量与潜力、固碳与减排的过程与机理的前沿探索,并越来越呈现为一个独特的土壤学新兴分支学科——固碳土壤学(Soil Science of C Sequestration)。本文围绕固碳土壤学的基本科学问题,回顾了最近10多年来,特别是最近5年来国内外关于土壤固碳研究的主要进展,讨论了固碳土壤学中的核心科学问题是土壤固碳容量与固碳作用的机理,论述了土壤物理保护、碳化学结合与碳化学转化稳定与固碳容量及稳定化的关系,提出了土壤-植物(作物)-微生物相互作用是当前固碳土壤学的前沿领域和深化方向,并结合国内对水稻土固碳的研究进展,提出了固碳土壤学的概念性框架,认为我国亟待加强固碳土壤学研究,深入探索我国农业经营管理特色下土壤固碳容量、过程、机理,丰富和发展农业土壤碳循环理论,并服务于全球变化生物学和国家碳管理。展开更多
Paludalfs under different crop rotation systems in North Huai region,China were sampled and soil aggregates were separated by ultra sonic dispersion followed by sedimentation and centrifuging.The particle size distrib...Paludalfs under different crop rotation systems in North Huai region,China were sampled and soil aggregates were separated by ultra sonic dispersion followed by sedimentation and centrifuging.The particle size distribution,SOC (Soil organic matter) contents and the natural abundance of 13 C in these aggregates were studied.Significant difference in size of the aggregates and organic carbon storage in the studied soils were found after 5 years of the crop rotation on the soil.SOC was mainly found in 0.02～0.25mm fraction of aggregates in the soils.The aggregates in layers deeper than 35cm became coarse and richer in SOC under corn peanut sweet potato rotation.Young carbon derived from corn tended to be accumulated in the coarse fractions as revealed by heavier stable carbon composition in those aggregates from deep layer under the rotation system containing corn crop.Compared to the soil under think pine forest,All soils under crop rotation system showed rapid increase of SOC at rates ranging from 0.14C g·kg -1 ·a -1 to 0 22C g·kg -1 ·a -1 ,with the highest under corn peanut sweet potato system.Thus,the significance was indicated for increasing SOC storage by crop rotation in paludalfs and for reinforcing terrestrial carbon retention of atmospheric CO 2.展开更多
文摘土壤碳固定是当前有关陆地生态系统碳循环与全球变化的地球表层过程研究的重要优先领域。国际社会对全球农业温室气体减排的需求,驱动着土壤学对土壤固碳容量与潜力、固碳与减排的过程与机理的前沿探索,并越来越呈现为一个独特的土壤学新兴分支学科——固碳土壤学(Soil Science of C Sequestration)。本文围绕固碳土壤学的基本科学问题,回顾了最近10多年来,特别是最近5年来国内外关于土壤固碳研究的主要进展,讨论了固碳土壤学中的核心科学问题是土壤固碳容量与固碳作用的机理,论述了土壤物理保护、碳化学结合与碳化学转化稳定与固碳容量及稳定化的关系,提出了土壤-植物(作物)-微生物相互作用是当前固碳土壤学的前沿领域和深化方向,并结合国内对水稻土固碳的研究进展,提出了固碳土壤学的概念性框架,认为我国亟待加强固碳土壤学研究,深入探索我国农业经营管理特色下土壤固碳容量、过程、机理,丰富和发展农业土壤碳循环理论,并服务于全球变化生物学和国家碳管理。
文摘Paludalfs under different crop rotation systems in North Huai region,China were sampled and soil aggregates were separated by ultra sonic dispersion followed by sedimentation and centrifuging.The particle size distribution,SOC (Soil organic matter) contents and the natural abundance of 13 C in these aggregates were studied.Significant difference in size of the aggregates and organic carbon storage in the studied soils were found after 5 years of the crop rotation on the soil.SOC was mainly found in 0.02～0.25mm fraction of aggregates in the soils.The aggregates in layers deeper than 35cm became coarse and richer in SOC under corn peanut sweet potato rotation.Young carbon derived from corn tended to be accumulated in the coarse fractions as revealed by heavier stable carbon composition in those aggregates from deep layer under the rotation system containing corn crop.Compared to the soil under think pine forest,All soils under crop rotation system showed rapid increase of SOC at rates ranging from 0.14C g·kg -1 ·a -1 to 0 22C g·kg -1 ·a -1 ,with the highest under corn peanut sweet potato system.Thus,the significance was indicated for increasing SOC storage by crop rotation in paludalfs and for reinforcing terrestrial carbon retention of atmospheric CO 2.
