摘要
通过对采自北京石花洞石笋近500年来分辨率为3~5年的δ13C记录的研究,我们发现水动力条件的改变和近代大气CO2浓度的改变均对石笋的δ13C值有影响,当气候湿润,降雨量增加时,洞穴包气带水的下渗速度加快,在石灰岩裂隙中滞留的时间缩短,CaCO3的溶解量减少,造成渗出δ13C水的值变轻。包气带水的补给速度增加,也可能使得溶液的CO2分压降低,造成石灰岩CaCO3溶解减少。另外,洞内滴水和渗出水中CO2的逸出量与供水速度呈反比。滴水速度加快,CO2逸出量相对降低,沉淀出来的CaCO3的δ13C值偏轻。通过与δ18O记录的对比,δ13C记录也反映30~40年降雨量变化的周期,为这一地区夏风变化的规律提供佐证。近50年来的δ13C记录,反映了人类活动造成大气CO2浓度升高的现象。从1940年到现今,石笋的δ13C值从-6.7‰降低到-8.1‰,降低速率每年为-0.028‰,直接反映了这一时期大气CO2的δ13C值的变化。这一结果与其它研究相吻合。利用精细的、分辨率高达几年的δ13C记录可以为岩溶作用与碳循环的研究提供有效手段。
Using a computercontrolled microsampling device, we have obtained a δ13C record from a stalagmite collected from Shihua Cave, Beijing, with a resolution of 3 ̄5 years. This 500year δ13C record exhibits apparent 30/40year cycles which correlate well with the δ18O record.The variation in δ13C on the 30/40year time scale is mainly influenced by the changes in the surface water supply rather than in C3 /C4 ratio. When precipitation increases inferred by the decreasing δ18O peaks, the δ13C of stalagmites can be decreased by the following reasons: (1)reduced residence time of seepage water in the overlying limestone leading to decreased amount of dissolved bedrock CaCO3; (2) reduced PCO2 in seepage water resetting less CaCO3 dissolution; and (3) increased drip rate of drip water in cave atmophere causing less CO2degassing from the solution. Therefore, highresolution δ13C recorded in speleothems may also provide information on the variability of precipitation. The changes in the δ13C record for the last 50 years reveal the effect of increased atmospheric CO2 concentration resulted from the consumption of fossil fuel on the δ13C of soil CO2. Since 1940, the δ13C values of the stalagmite was decreased from -6.7‰ to -81‰, with a rate of -0.028‰/yr, which is in excellent agreement with the previous studies. The imprint of such δ13C decreasing event may be useful for the study on the relationship of karst processes and carbon cycle in the future.
出处
《中国岩溶》
CAS
CSCD
1997年第4期285-295,共11页
Carsologica Sinica
基金
北京石花洞研究项目
国际地质对比计划IGCP379项目
美国自然科学基金
关键词
碳同位素
洞穴石笋
古气候
大气
二氧化碳浓度
Carbon isotopes Stalagmite Paleoclimate Atmopheric CO2 Carbon cycle Shihua Cave
Beijing