Schönwitz Roswitha, Stichler Willibald, Ziegler Hubert
Institut für Botanik und Mikrobiologie der Technischen Universität, D-8000, München 2, Federal Republic of Germany.
Institut für Radiohydrometrie der Gesellschaft für Strahlen- und Umweltforschung mbH München, D-8042, Neuherberg, Federal Republic of Germany.
Oecologia. 1986 May;69(2):305-308. doi: 10.1007/BF00377638.
Based on the differential discrimination between CO and CO during photosynthetic CO fixation by C3 and C4 plants, the relative contribution of organic soil material of varying age can be checked by measuring the δC value of CO evolved during soil respiration.The CO from a soil cropped only with C3 plants for at least 7 years showed a δC value very close to that of C3 plant tissue. Correspondingly, a soil bearing the C4 plant maize for at least 6 years had a δC value for the respiratory CO quite near to that of a typical C4 plant. A soil cropped with maize in the year of study only showed intermediate δC values, with a tendency towards C4. With soil standardised for cultivation and cropping, a quantification of the part that fresh organic matter and especially the last year plant residues play in soil respiration, can be achieved.
基于C3和C4植物在光合固定二氧化碳过程中对13C和12C的差异辨别,通过测量土壤呼吸过程中释放的二氧化碳的δC值,可以检测不同年份有机土壤物质的相对贡献。仅种植C3植物至少7年的土壤释放的二氧化碳的δC值与C3植物组织的δC值非常接近。相应地,种植C4植物玉米至少6年的土壤,其呼吸二氧化碳的δC值与典型C4植物的δC值相当接近。在研究当年种植玉米的土壤仅显示出中间的δC值,有偏向C4的趋势。对于经过标准化种植和作物轮作的土壤,可以对新鲜有机物质尤其是去年的植物残体在土壤呼吸中所起的作用进行量化。